Phylogeography of a pantropical plant with sea-drifted ... - åè大å¦
Phylogeography of a pantropical plant with sea-drifted ... - åè大å¦
Phylogeography of a pantropical plant with sea-drifted ... - åè大å¦
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( 千 葉 大 学 学 位 申 請 論 文 )<br />
<strong>Phylogeography</strong> <strong>of</strong> a <strong>pantropical</strong> <strong>plant</strong> <strong>with</strong><br />
<strong>sea</strong>‐<strong>drifted</strong> seeds; Canavalia ro<strong>sea</strong> (Sw.) DC.,<br />
(Fabaceae)<br />
汎 熱 帯 海 流 散 布 植 物 ナガミハマナタマメ<br />
(マメ 科 )の 系 統 地 理<br />
2010 年 7 月<br />
千 葉 大 学 大 学 院 理 学 研 究 科<br />
地 球 生 命 圏 科 学 専 攻 生 物 学 コース<br />
Mohammad Vatanparast
<strong>Phylogeography</strong> <strong>of</strong> a <strong>pantropical</strong> <strong>plant</strong> <strong>with</strong><br />
<strong>sea</strong>‐<strong>drifted</strong> seeds; Canavalia ro<strong>sea</strong> (Sw.) DC.,<br />
(Fabaceae)<br />
July 2010<br />
MOHAMMAD VATANPARAST<br />
Graduate School <strong>of</strong> Science<br />
CHIBA UNIVERSITY
TABLE OF CONTENTS PAGES<br />
ABSTRACT 1<br />
GENERAL INTRODUCTION 3<br />
Pantropical <strong>plant</strong>s <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds species (PPSS) 5<br />
A project on the phylogeography <strong>of</strong> the PPSS 6<br />
A case study <strong>of</strong> PPSS: Hibiscus tiliaceus L. 7<br />
Canavalia ro<strong>sea</strong>: a genuine <strong>pantropical</strong> <strong>plant</strong> <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds 8<br />
Overview <strong>of</strong> this study 10<br />
CHAPTER 1 12<br />
PHYLOGENETIC RELATIONSHIPS AMONG CANAVALIA ROSEA AND ITS<br />
ALLIED SPECIES 12<br />
1-1 Introduction 12<br />
1-2 Materials and Methods 15<br />
Taxon sampling 15<br />
DNA extraction, PCR, and sequencing 16<br />
Phylogenetic analyses based on cpDNA sequence data 18<br />
Phylogenetic analyses based on ITS sequence data 19<br />
1-3 Results 21<br />
Phylogenetic analyses based on cpDNA sequence data 21<br />
Phylogenetic analyses based on ITS sequence data 22<br />
1-4 Discussion 24<br />
Phylogenetic relationships among C. ro<strong>sea</strong> and its related species 24<br />
The phylogeographic break in the Atlantic Ocean 25<br />
Origin <strong>of</strong> the Hawaiian endemic species 26<br />
Future prospects for the evolutionary studies among C. ro<strong>sea</strong> and its allied<br />
species 27<br />
Tables and figures 29<br />
i
TABLE OF CONTENTS (CONTINUED) PAGES<br />
CHAPTER 2 40<br />
GLOBAL GENETIC STRUCTURE OF CANAVALIA ROSEA; EVIDENCE FROM<br />
CHLOROPLAST DNA SEQUENCES 40<br />
2-1 Introduction 40<br />
2-2 Materials and Methods 44<br />
Sampling 44<br />
DNA extraction, PCR, and sequencing 44<br />
Haplotype Composition and Network <strong>of</strong> C. ro<strong>sea</strong> and its allied species 44<br />
Population differentiation 45<br />
Historical migration rates between oceanic regions 46<br />
Estimates <strong>of</strong> recent migration rates 48<br />
2-3 Results 49<br />
Haplotype Composition and Network <strong>of</strong> C. ro<strong>sea</strong> and its allied species 49<br />
Population differentiation 50<br />
Historical migration rates between oceanic regions 51<br />
Estimates <strong>of</strong> recent migration rates 52<br />
2-4 Discussion 54<br />
Gene flow in Indo-Pacific Ocean through Long Distance Seed Dispersal 54<br />
A strong genetic difference between the Indo-Pacific and Atlantic populations<br />
<strong>of</strong> C. ro<strong>sea</strong> 56<br />
2-5 Conclusion 59<br />
Tables and figures 60<br />
GENERAL DISCUSSION 74<br />
REFERENCES 76<br />
ACKNOWLEDGEMENTS 82<br />
BIOGRAPHY 83<br />
ii
ABBREVIATIONS<br />
AEP<br />
AMOVA<br />
bp<br />
cpDNA<br />
CTAB<br />
ESS<br />
Atlantic East Pacific<br />
Analysis <strong>of</strong> molecular variance<br />
base pair<br />
chloroplast DNA<br />
cetyltrimethyl ammonium bromide<br />
Effective sample size<br />
F ST<br />
Fixation index (F-statistices)<br />
IGS<br />
ITS<br />
IWP<br />
MLE<br />
nrDNA<br />
PCR<br />
PCR-SSCP<br />
PCR-SSP<br />
PPSS<br />
RCA<br />
SAMOVA<br />
Intergenic Spacer<br />
Internal Transcribed Spacers<br />
Indo West Pacific<br />
Maximum likelihood estimates<br />
nuclear ribosomal DNA<br />
Polymerase Chain Reaction<br />
PCR amplification <strong>with</strong> single-strand conformation polymorphism<br />
PCR amplification <strong>with</strong> sequence specific primers<br />
Pantropical Plants <strong>with</strong> Sea-<strong>drifted</strong> Seeds<br />
Rolling Circle Amplification<br />
Spatial Analysis <strong>of</strong> Molecular Variance<br />
iii
ABSTRACT<br />
This study intends to examine the importance <strong>of</strong> long distance seed<br />
dispersal in the recurrent speciation and integration <strong>of</strong> <strong>pantropical</strong> <strong>plant</strong>s <strong>with</strong><br />
<strong>sea</strong>-<strong>drifted</strong> seeds (PPSS). I focused on one <strong>of</strong> genuine member <strong>of</strong> PPSS;<br />
Canavalia ro<strong>sea</strong> (Sw.) DC. and its allied species.<br />
Chapter 1 is concerned <strong>with</strong> the phylogenetic relationships among C.<br />
ro<strong>sea</strong> and its allied species as well as Hawaiian endemic species using<br />
chloroplast DNA (cpDNA) and internal transcribed spacers (ITS) <strong>of</strong> nuclear<br />
ribosomal DNA (nrDNA) sequences. Phylogenetic analyses using nucleotide<br />
sequences <strong>of</strong> 6 cpDNA regions (ca. 6000 bp) as well as nrDNA ITS for C. ro<strong>sea</strong><br />
and its related species suggested that rapid speciation might occurred among<br />
C. ro<strong>sea</strong> and its related species. The phylogenetic results also suggested that<br />
Hawaiian endemic subgenus Maunaloa, was monophyletic and closely related<br />
to subgenus Canavalia than to other subgenera (Wenderothia and Catodonia).<br />
The results suggests that the Hawaiian subgenus originated by single<br />
colonization to Hawaiian archipelagos by <strong>sea</strong>-dispersal.<br />
In chapter 2, spatial genetic structure <strong>of</strong> cpDNA sequences were studied<br />
for C. ro<strong>sea</strong> and its related species. In total 515 individuals from 48 populations<br />
were surveyed based on partial sequences <strong>of</strong> 6 cpDNA regions (ca. 2000 bp).<br />
Statistical analyses (F ST -based and coalescent-based methods) did not show<br />
significant genetic differentiation among the C. ro<strong>sea</strong> populations over whole<br />
Pacific and Indian Oceanic regions and also <strong>with</strong>in Atlantic region. This<br />
suggests that significant gene flow by long distance dispersal <strong>of</strong> <strong>sea</strong>-<strong>drifted</strong><br />
1
seeds occurs among these oceanic regions. On the other hand, the results <strong>of</strong><br />
phylogenetic and population genetic analyses confirm the genetic<br />
differentiation <strong>of</strong> the Atlantic populations. This suggests that African and<br />
American land masses played roles as geographical barriers to gene flow by<br />
<strong>sea</strong>-dispersal. However, partial gene flow was detected between Atlantic and<br />
Indian oceanic regions which suggest that the unity <strong>of</strong> the species in global<br />
scale is kept by long distance seed dispersal over the African continent.<br />
Directional gene flow <strong>with</strong>in Atlantic region might be corresponded to the<br />
variation <strong>of</strong> the strength <strong>of</strong> tropical Atlantic’s major currents which regarded as<br />
transatlantic dispersal in Atlantic region. Moreover, highly differentiated<br />
populations <strong>of</strong> C. ro<strong>sea</strong> were detected in the southern Brazil. The South<br />
Equatorial Current bifurcating at the north-eastern horn <strong>of</strong> Brazil to the<br />
northward and southward appears to be potential barrier to gene flow and<br />
may promote the genetic differentiation <strong>of</strong> the C. ro<strong>sea</strong> populations in<br />
southern Brazil.<br />
2
GENERAL INTRODUCTION<br />
“… mammals have not been able to migrate, whereas some <strong>plant</strong>s, from their<br />
varied means <strong>of</strong> dispersal, have migrated across the wide and broken interspaces.”<br />
(Darwin, 1859)<br />
The term dispersal has two different but interrelated functions in most<br />
species. The first one is, range expansion <strong>of</strong> species, and the second one, gene<br />
flow <strong>with</strong>in and among populations. Range expansion is necessary for almost<br />
all species, so they have various strategies to expand their distribution ranges<br />
(Linhart & Grant, 1996). However, the wider distribution range arisen from<br />
dispersal causes high genetic heterogeneity among populations because <strong>of</strong><br />
increased levels <strong>of</strong> selection <strong>with</strong>in local populations and/or because <strong>of</strong> limited<br />
levels <strong>of</strong> genetic exchange among the local populations (Heywood, 1991;<br />
Hamrick & Nason, 1996; Linhart & Grant, 1996). When genetic heterogeneity<br />
among populations becomes significantly enough, local populations can evolve<br />
and eventually form a distinct species (Wright, 1931; Ennos, 1994; Bohonak,<br />
3
1999). Gene flow is one <strong>of</strong> the most important processes for species to evolve<br />
as cohesive units in their distribution range (Mayr, 1963; Levin, 2000; Morjan &<br />
Rieseberg, 2004). In fact, if levels <strong>of</strong> gene flow <strong>with</strong>in and among populations<br />
become high (e.g. greater than four migrants per generation), it homogenize<br />
the species and prevents genetic divergence <strong>of</strong> local populations.<br />
In many <strong>plant</strong> species, populations are spatially isolated from each other,<br />
<strong>of</strong>ten by hundreds <strong>of</strong> meters or more and seed dispersal represents the only<br />
way by which populations can exchange individuals or to expand the<br />
distribution ranges (Cain et al., 2000). As there are geographical, ecological or<br />
behavioral barriers to seed dispersal, most <strong>plant</strong> species are not distributed<br />
globally (Howe & Smallwood, 1982; Cain et al., 1998; Willson & Traveset, 2000).<br />
The biggest barrier for land <strong>plant</strong>s will be the ocean, so that most <strong>of</strong> the<br />
floristic compositions are generally quite different among continents which are<br />
divided by oceans. However, there are a few <strong>plant</strong> species that characterized by<br />
their extremely wide distribution ranges across littoral areas in tropics and<br />
subtropics worldwide. They are called “<strong>pantropical</strong> <strong>plant</strong>s <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong><br />
seeds” (Takayama et al., 2006; 2008), referred to as PPSS. A few PPSS are known<br />
from various families which can roughly divide into 2 categories. One is<br />
genuine PPSS in which a single species distributes around the globe.<br />
Canavalia ro<strong>sea</strong> (Sw.) DC. (Fabaceae) and Ipomoea pes-caprae (L.) R. Br.<br />
(Convolvulaceae) are in this category. The other one is Sub-PPSS, in which<br />
small numbers <strong>of</strong> closely related species compose the global distribution in<br />
total. Hibiscus tiliaceus L., <strong>with</strong> H. pernambucensis Arruda (Malvaceae), Vigna<br />
marina (Burm.f.) Merr. <strong>with</strong> V. luteola (Jacq.) Benth. (Fabaceae), and species <strong>of</strong><br />
Rhizophora L. and Entada Adans. are in this category.<br />
4
Pantropical <strong>plant</strong>s <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds species (PPSS)<br />
The main dispersal mode <strong>of</strong> PPSS is <strong>sea</strong>-dispersal. Almost all PPSS have<br />
seeds or fruits that can float in <strong>sea</strong> water for long time. The seed coats <strong>of</strong> these<br />
species are hard <strong>with</strong> lightweight cotyledons and there are air spaces between<br />
the folds <strong>of</strong> the cotyledons which help the seeds to stay impermeable on <strong>sea</strong><br />
water (Nakanishi, 1988; Loewer, 2005; Thiel & Haye, 2006). Nakanishi (1988)<br />
investigated germination and buoyancy <strong>of</strong> seeds and fruits <strong>of</strong> seventeen<br />
maritime species (including most <strong>of</strong> PPSS), after immersion in artificial <strong>sea</strong>water.<br />
He revealed that all seeds and fruits tested in the study continued to float in<br />
<strong>sea</strong> water for at least three months (Nakanishi, 1988). These characteristics help<br />
PPSS to distribute in wide areas in equatorial belt around the globe. Their<br />
distribution ranges are consistent <strong>with</strong> the areas where the average<br />
temperature <strong>of</strong> Ocean water is around 20 ͦC. In the West Atlantic, they are<br />
distributed from Florida to the Uruguay in Southern West Atlantic. In East<br />
Atlantic they are distributed from Senegal to the Angola and in the Indian<br />
Ocean from Northern part <strong>of</strong> Indian Ocean to the East Cape <strong>of</strong> South Africa. In<br />
the West Pacific Ocean their northern limit is Ryukyu Islands in Japan and in the<br />
south west Pacific is the Brisbane in Australia. In central pacific, their<br />
distribution ranges are from Hawaii to Polynesia and in the East Pacific from<br />
Sinaloa in Mexico to the Northern part <strong>of</strong> Peru in the East Pacific <strong>sea</strong>shores (Fig.<br />
1-2A).<br />
The extremely wide distribution range <strong>of</strong> PPSS has been explained<br />
mainly by their high ability <strong>of</strong> seed dispersal (Sauer, 1988; Whistler, 1992). On<br />
the other hand, high dispersal ability <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds could raise the<br />
5
potential <strong>of</strong> population differentiation and speciation. New species could arise<br />
independently in remote populations following long-distance seed dispersal<br />
and/or adaptation to a new habitat. This kind <strong>of</strong> speciation process is assumed<br />
to occur in PPSS, as the most <strong>of</strong> the PPSS have some closely related species<br />
distributed in limited areas comparing to the mother PPSS (Levin, 2001;<br />
Takayama et al., 2006). However, until recently there were no empirical data to<br />
explain how PPSS keep the extremely wide range <strong>of</strong> distribution.<br />
A project on the phylogeography <strong>of</strong> the PPSS<br />
One <strong>of</strong> the major difficulties that prevent re<strong>sea</strong>rchers from performing<br />
comprehensive study in PPSS was their extremely wide distribution ranges. The<br />
project <strong>of</strong> PPSS was started more than 10 years ago <strong>with</strong> the leading <strong>of</strong> Dr.<br />
Tadashi Kajita and <strong>with</strong> propose <strong>of</strong> global population sampling as well as<br />
performing population genetic analyses using various molecular markers.<br />
Accomplishment <strong>of</strong> this project was facilitated because <strong>of</strong> development <strong>of</strong><br />
aviation and transportation systems in recent two decades. Cooperation <strong>with</strong><br />
over<strong>sea</strong> re<strong>sea</strong>rchers and institutes are also promoted the project to go ahead.<br />
Until now more than several thousand samples were collected from 30<br />
countries and is ongoing project to performing phylogeographic analyses to<br />
reveal the speciation and population differentiation <strong>of</strong> PPSS.<br />
<strong>Phylogeography</strong> is a relatively new discipline that deals <strong>with</strong> the spatial<br />
arrangements <strong>of</strong> genetic lineages, especially <strong>with</strong>in and among closely related<br />
species (Avise, 2009). It utilized molecular markers to reveal the evolutionary<br />
history <strong>of</strong> the species at the geographical scale. Novel analytical methods <strong>with</strong><br />
high output are also recently developed at the population level (e.g.,<br />
6
application <strong>of</strong> coalescent-based approaches and tree-based thinking) (Knowles<br />
& Maddison, 2002; Knowles, 2009). Using these methods will enable us to<br />
study phylogeographic patterns <strong>of</strong> PPSS.<br />
A case study <strong>of</strong> PPSS: Hibiscus tiliaceus L.<br />
Recently, one <strong>of</strong> our colleagues, Koji Takayama studied genetic structure<br />
<strong>of</strong> Hibiscus tiliaceus and its allied species using chloroplast DNA (cpDNA)<br />
polymorphisms and Microsatellite markers (Takayama et al., 2006; 2008).<br />
Hibiscus tiliaceus is distributed in the East Atlantic and Indo-West Pacific<br />
regions and its counterpart species, Hibiscus pernambucensis, is distributed in<br />
the East Pacific-West Atlantic regions. All together distribution range <strong>of</strong> H.<br />
tiliaceus and H. pernambucensis covers almost the entire littoral area <strong>of</strong> the<br />
tropics worldwide, a situation that could have been established through<br />
dispersal by <strong>sea</strong>-<strong>drifted</strong> seeds. Three morphologically similar species to H.<br />
tiliaceus are recognized in both the Old World (Hibiscus hamabo Siebold &<br />
Zucc.) and New World (Hibiscus glaber Matsum. and Hibiscus elatus Sw.). These<br />
three species have limited distribution ranges, which the two island endemic<br />
species, H. glaber and H. elatus grow in parallel at inland habitats <strong>of</strong> islands in<br />
both the Old and New Worlds respectively, and H. hamabo grows in temperate<br />
areas <strong>of</strong> West Pacific area beyond the northern limit <strong>of</strong> distribution <strong>of</strong> H.<br />
tiliaceus (Takayama et al., 2006). The main summary <strong>of</strong> their finding are as<br />
follows:<br />
I. Recurrent speciation from H. tiliaceus has given rise to all <strong>of</strong> its allied<br />
species.<br />
7
II.<br />
Frequent gene flow by long-distance seed dispersal is responsible for<br />
species integration <strong>of</strong> H. tiliaceus in the wide distribution range.<br />
III.<br />
American and African continents may be geographical barriers to gene<br />
flow by <strong>sea</strong>-<strong>drifted</strong> seeds among populations <strong>of</strong> H. pernambucensis and<br />
H. tiliaceus, respectively.<br />
IV.<br />
Introgression between the H. tiliaceus and H. pernambucensis was<br />
occurred in the Atlantic region.<br />
All these results are new for a sub-PPSS species and explain their wide<br />
distribution range; however we still do not know whether these results are<br />
applicable for other PPSS, especially for a genuine PPSS <strong>with</strong> global distribution.<br />
So, to answer this question, I focused on Canavalia ro<strong>sea</strong> (Beach bean), a<br />
genuine member <strong>of</strong> PPSS.<br />
Canavalia ro<strong>sea</strong>: a genuine PPSS<br />
Canavalia ro<strong>sea</strong> (Beach bean) is mostly prostrate herbaceous vine that<br />
trails along beach dunes, coastal strand and rocky shores and sometimes<br />
climbs into low vegetation (Whistler, 1992). The thick and fleshy stem can grow<br />
to 6 m or more in length and more than 2.5 cm in diameter. The stem is rather<br />
woody near the base and several branches radiate outward, forming mats <strong>of</strong><br />
light green semi-succulent foliage. Beach bean has compound leaves <strong>with</strong><br />
three thick, more or less rounded, fleshy leaflets, each about 5 -12 cm long. The<br />
leaflets fold up under the hot sun at midday and are coriaceous, oblong to<br />
nearly circular in outline, obtuse to emarginate, <strong>of</strong>ten minutely apiculate at tip.<br />
Bracteoles are 1.5 mm long. Pedicel is 3 mm long. Calyx 12 mm long;<br />
pubescence short, white, sparse to moderately dense; upper lip much shorter<br />
8
than tube, upper edge constricted behind non-apiculate tip; lowest tooth 2<br />
mm long, acute, slightly exceeding acute laterals. Standard is 3 cm long. The<br />
flowers are typical pea flowers, purplish pink, about 5 cm long and borne in<br />
erect spikes on long stalks. Beach bean blooms most <strong>of</strong> the summer and<br />
sporadically the rest <strong>of</strong> the year. The pods are commonly 10-15 cm long, flat,<br />
moderately compressed, spirally dehiscent; each valve <strong>with</strong> sutural ribs and an<br />
extra rib ca. 3 mm from ventral rib. They are prominently ridged and woody<br />
when mature. Seeds to 18 X 13 X 10 mm, elliptic, slightly compressed, brown<br />
<strong>with</strong> darker marbling, mostly buoyant and indefinitely impermeable to water, at<br />
least for a year; hilum ca. 7 mm long (Sauer, 1964). Occasionally it is cultivated<br />
experimentally as a sand binder or cover crop. Flowering time is in all <strong>sea</strong>sons,<br />
even in the subtropics. The species considered as self-compatible and it can<br />
also be pollinated by carpenter bee (Xylocopa) species (Arroyo, 1981; Gross,<br />
1993).<br />
Canavalia ro<strong>sea</strong> is distributed throughout littoral areas <strong>of</strong> the tropics and<br />
subtropics around the world. It is one <strong>of</strong> the common and most widespread<br />
tropical <strong>sea</strong>coast <strong>plant</strong>s, most commonly trailing on beaches at the outer limits<br />
<strong>of</strong> land vegetation, where it is usually associated <strong>with</strong> Ipomoea pes-caprae,<br />
occasionally climbing on littoral thickets, rarely slightly inland along roadsides<br />
or coastal plain lake shores. The seeds float because <strong>of</strong> a lightweight tissue and<br />
air space (Van Der Pijl, 1969; Loewer, 2005) and remain impermeable in water<br />
for years while drifting in the <strong>sea</strong> (Guppy, 1906; Nakanishi, 1988; Thiel & Gutow,<br />
2004). The extremely wide distribution <strong>of</strong> C. ro<strong>sea</strong> is considered to be a result<br />
<strong>of</strong> long distance seed dispersal by <strong>sea</strong>-<strong>drifted</strong> seeds; however, we do not have<br />
9
any empirical data and don't know whether the gene flow by seed dispersal is<br />
kept throughout the distribution range over the globe.<br />
There are three related species to C. ro<strong>sea</strong>; Canavalia cathartica Thouars,<br />
C. lineata L. and C. sericea A. Gray from the same subgenus Canavalia, which is<br />
distributed in coastal areas <strong>of</strong> Indo-Pacific Oceanic regions. Their<br />
morphological similarity suggests that they might be closely related to each<br />
other. Given the wide distribution <strong>of</strong> C. ro<strong>sea</strong> and the limited distribution <strong>of</strong> the<br />
other three species, the three species <strong>of</strong> more limited distribution might have<br />
diversified from the widely distributed species. Moreover, there are six endemic<br />
Canavalia species in Hawaiian Islands (subgenus Maunaloa). There is<br />
hypothesis that these species might originate from species which reach to the<br />
Hawaiian island by <strong>sea</strong> <strong>drifted</strong> seed dispersal (Sauer, 1964). Although the<br />
presence <strong>of</strong> several closely related species <strong>with</strong> limited distribution are likely to<br />
be explained by recurrent speciation from widely distributed species, as were<br />
shown in H. tiliaceus; the speciation process among C. ro<strong>sea</strong> and these species<br />
is still in question.<br />
The main questions addressed in this thesis are: (1) Have recurrent<br />
speciation occurred in the distribution range <strong>of</strong> C. ro<strong>sea</strong>? and (2) Can a single<br />
species keep gene flow over the extremely wide range <strong>of</strong> distribution?<br />
Overview <strong>of</strong> this study<br />
In chapter 1, I will study the phylogenetic relationships and evolutionary<br />
history among C. ro<strong>sea</strong> and its allied species as well as Hawaiian endemic<br />
species based on cpDNA and internal transcribed spacers (ITS) <strong>of</strong> nuclear<br />
ribosomal DNA (nrDNA) sequences, which enable to investigate multiple lines<br />
10
<strong>of</strong> evidence. In chapter 2, I will study global phylogeography and genetic<br />
structure <strong>of</strong> C. ro<strong>sea</strong> and its allied species based on the cpDNA sequences,<br />
which provide an ideal marker for studying gene flow through seed dispersal.<br />
Finally, based on the results obtained in this study, I will discuss importance <strong>of</strong><br />
<strong>sea</strong>-<strong>drifted</strong> seed dispersal for the speciation and integration <strong>of</strong> C. ro<strong>sea</strong>.<br />
11
CHAPTER 1<br />
PHYLOGENETIC RELATIONSHIPS AMONG CANAVALIA ROSEA AND<br />
ITS ALLIED SPECIES<br />
1-1 Introduction<br />
The genus Canavalia Adans, 1763, is distributed in tropics and subtropics<br />
<strong>of</strong> all over the world (Lackey, 1981; Schrire, 2005). According to the latest<br />
taxonomic revision, the genus are further divided into four subgenera, namely,<br />
Catodonia (7 species) and Wenderothia (16 species) mostly distributed in the<br />
New World, Canavalia (23 species) in both the Old and New World which<br />
includes some crop species, and Maunaloa (6 species) which is endemic to<br />
Hawaii Islands (Sauer, 1964). Sauer (1964) studied the morphological<br />
differences/similarities among species and considered that the most primitive<br />
subgenus would be Wenderothia, and subgenera Catodonia and Canavalia<br />
would be originated from it. He also considered that subgenus Maunaloa<br />
would be originated from subgenus Canavalia because <strong>of</strong> the presence <strong>of</strong> a<br />
<strong>pantropical</strong> species, Canavalia ro<strong>sea</strong>, in the subgenus.<br />
12
Canavalia ro<strong>sea</strong> is a typical member <strong>of</strong> the <strong>plant</strong> group called<br />
“Pantropical Plants <strong>with</strong> Sea-<strong>drifted</strong> Seeds (Takayama et al. 2006, 2008)";<br />
abbreviated as PPSS. These species are distributed in littoral areas <strong>of</strong> the<br />
tropics and subtropics all over the world and their main mode <strong>of</strong> seed dispersal<br />
is <strong>sea</strong>-dispersal. In addition, C. ro<strong>sea</strong> has some closely related species from<br />
subgenus Canavalia which have <strong>sea</strong>-dispersal, namely, C. cathartica which is<br />
distributed over Indo-West Pacific regions, C. lineata in South East Asia and C.<br />
sericea in South West Pacific. These species are distributed <strong>with</strong>in distribution<br />
range <strong>of</strong> C. ro<strong>sea</strong>. The other species which is known to have <strong>sea</strong>-<strong>drifted</strong> seeds is<br />
C. bonariensis <strong>of</strong> subgenus Catodonia. All other species <strong>of</strong> genus Canavalia do<br />
not have <strong>sea</strong>-<strong>drifted</strong> seeds and their main mode <strong>of</strong> seed dispersal is<br />
mechanical (thrown by dehiscent <strong>of</strong> pods) or gravity dispersal. Although the<br />
presence <strong>of</strong> several closely related species <strong>with</strong> limited distribution are likely to<br />
be explained by recurrent speciation from widely distributed species, as were<br />
shown in H. tiliaceus (Takayama et al., 2006); the speciation process among C.<br />
ro<strong>sea</strong> and its related species from subgenus Canavalia is still in question.<br />
Moreover, given the distribution ranges <strong>of</strong> the species and their modes <strong>of</strong> seed<br />
dispersal, Sauer (1964) and Carlquist (1966) suggested that the endemic<br />
species <strong>of</strong> Hawaii Islands might be originated from the species that reach to<br />
the Hawaiian Islands by <strong>sea</strong>-dispersal, and the species would plausibly be the<br />
<strong>pantropical</strong> species, Canavalia ro<strong>sea</strong>. However, this hypothesis has never been<br />
tested using modern molecular phylogenetic methods.<br />
13
To test the hypothesis about the origin <strong>of</strong> Hawaiian endemic species <strong>of</strong><br />
Canavalia and speciation process among C. ro<strong>sea</strong> and its related species, we<br />
employed both nuclear and chloroplast DNA markers. These markers have<br />
been successfully used to study the origin <strong>of</strong> Hawaiian endemic species in<br />
other <strong>plant</strong> groups (Baldwin & Wagner, 2010). Chloroplast DNA is regarded as<br />
single locus and maternally inherited through seeds in most angiosperms<br />
(Mogensen, 1996), and it has been utilized to discover phylogenetic<br />
relationships in many <strong>plant</strong> species (Soltis & Soltis, 1998). In addition, nuclear<br />
DNA markers can also be used in combination <strong>with</strong> cytoplasmic markers to<br />
decipher phylogenetic relationships among closely relates species, as using<br />
multiple lines <strong>of</strong> molecular markers <strong>with</strong> highly polymorphic loci could give<br />
resolved topologies than single locus (Small et al., 1998; Brito & Edwards, 2009;<br />
Calonje et al., 2009). Although a recent phylogenetic study on tribe Diocleinae<br />
based on nrDNA ITS sequences (Varela et al., 2004) showed that subgenus<br />
Canavalia was sister to Catedonia, taxon sampling <strong>of</strong> the study was not enough<br />
to reveal phylogenetic relationships <strong>of</strong> the four subgenera and the origin <strong>of</strong><br />
Hawaiian endemic species. I studied all species <strong>of</strong> subgenus Maunaloa together<br />
<strong>with</strong> other samples <strong>of</strong> C. ro<strong>sea</strong> and its closely related species, in addition to<br />
both representative species <strong>of</strong> subgenera Wenderothia and Catodonia.<br />
14
1-2 Materials and Methods<br />
Taxon sampling<br />
Leaf samples were collected in large-scale, covering almost all<br />
distribution ranges <strong>of</strong> the species. For cpDNA phylogenetic analyses, in total,<br />
62 individuals from Canavalia ro<strong>sea</strong>, 5 individuals from C. cathartica, 4<br />
individuals from C. lineata, and 3 individuals from C. sericea were included in<br />
phylogenetic study (Table 1-1). Moreover, an inland species, Canavalia virosa<br />
(Roxb.) Wight & Arn., two crop species, Canavalia ensiformis (L.) DC. (Common<br />
Jack bean) and Canavalia gladiata (Jacq.) DC. (Sword bean) from the subgenus<br />
Canavalia were added in the phylogenetic analyses (Table 1-1). For nrDNA ITS<br />
phylogenetic analyses selective samples from C. ro<strong>sea</strong> and its related species<br />
were included (Table 1-2). All Hawaiian endemic species from subgenus<br />
Maunaloa including Canavalia molokaiensis Degener & al., C. hawaiiensis<br />
Degener & al., C. napaliensis St. John, C. galeata Gaudich., C. pubescens Hook.<br />
& Arn., and C. kauaiensis J.D. Sauer (St. John H, 1970; Wagner et al., 1999) were<br />
also included in either cpDNA and ITS analyses. Canavalia parviflora Benth. was<br />
added in the phylogenetic analyses as a representative species from subgenus<br />
Catedonia. Canavalia hirsutissima J.D. Sauer and Canavalia villosa Benth. from<br />
15
subgenus Wenderothia were chosen as outgroups according to Sauer (1964)<br />
and Varella (2004). Voucher specimens were deposited in the herbarium <strong>of</strong><br />
University <strong>of</strong> the Ryukyus (RYU), Jardim Botânico, Rio de Janeiro (RBRJ) and<br />
Bishop Museum, Honolulu, Hawaii.<br />
DNA extraction, PCR, and sequencing<br />
Genomic DNA was extracted from dried leaves using modified CTAB<br />
(cetyltrimethyl ammonium bromide) method (Doyle & Doyle, 1987) and DNA<br />
concentration was measured by GeneQuant 100 electrophotometer (GE<br />
Healthcare, Life Sciences). After an initial screening <strong>of</strong> 15 cpDNA candidate<br />
non-coding regions (Shaw et al., 2007), six highly variable regions including<br />
intergenic spacers (IGS) and introns were chosen for further steps (Table 1-3).<br />
For nuclear genome, nuclear rDNA ITS was sequenced. Polymerase chain<br />
reactions (PCR) were performed in 10-25 µL volume reactions containing 1.25<br />
units ExTaq (TaKaRa), 0.2 mM <strong>of</strong> dNTPs, 10x PCR buffer contains 1.5 mM MgCl2,<br />
0.5–1 µM <strong>of</strong> each primer pairs, and 20 ng genomic DNA. The PCR conditions<br />
were as follows: 3 min for initial denaturation at 95 °C, followed by 35<br />
amplification cycles <strong>of</strong> 1 min denaturation at 95 °C, 1-2 min annealing at<br />
fragment-specific temperatures (see Table 1-3), 1-2 min extension at 72 °C, and<br />
a final 10 min extension at 72 °C. The PCR products were visualized by 0.8 %<br />
agarose gel electrophoresis and purified using either GENECLEAN III kit<br />
(Qiagen) or ExoSAP-IT (USB Corp., Cleveland, Ohio, USA) following the<br />
manufacturer's instructions.<br />
The cycle sequencing reactions were carried out using a BigDye<br />
Terminator v. 3.1 Cycle Sequencing Kit (Applied Biosystems) and sequencing<br />
16
eaction products were purified by ethanol precipitation method. All DNA<br />
sequences were determined <strong>with</strong> ABI 377 or ABI 3500 DNA sequencer (Applied<br />
Biosystems). For ITS sequences which direct sequencing yielded unreadable<br />
electropherograms, TOPO-TA cloning kit (Invitrogen) was subsequently used<br />
according to the manufacturer’s instructions. In total for 19 individuals from 14<br />
species cloning method were used. Twelve colonies from each sample were<br />
picked up, purified and amplified via TempliPhi DNA Sequencing Template<br />
Amplification Kits (GE Healthcare). This kit utilize bacteriophage Phi29 DNA<br />
polymerase and rolling circle amplification (RCA) technology (Polidoros et al.,<br />
2006) for rapid amplification <strong>of</strong> circular template DNA. The products were then<br />
sequenced using the ABI Big Dye Terminator v3.1 Cycle Sequencing Ready<br />
Reaction kit (Applied Biosystems). Both forward and reverse strands were<br />
assembled manually using the Autoassembler 2.1 (Applied Biosystems) <strong>with</strong><br />
default setting. Sequences manually edited and aligned <strong>with</strong> Se-Al v2.0a11<br />
(Rambaut, 2002). Seven Indels and inversions from cpDNA sequence data set<br />
were coded as separate binary characters according to Kelchner (2000)<br />
Simmons & Ochoterena (2000) and Ingvarsson (2003). However, length<br />
variations, all gaps containing homopolymers, AT-rich regions and two<br />
homoplasious inversions were excluded from all analyses. For the ITS sequence<br />
data set, cloned products were assembled and singleton mutations were<br />
excluded by comparing to the corresponding direct ITS sequence data <strong>of</strong> this<br />
study. These singletons were presumed as a result <strong>of</strong> Taq or PCR error in<br />
cloning method. I chose a threshold that less than two singletons from aligned<br />
sequence data were removed from the data set. After making final dataset,<br />
haplotype file in Nexus format was made by the program DNAsp v. 5.10.01<br />
17
(Librado & Rozas, 2009). Sequences were deposited to the GenBank under the<br />
accession numbers ### ###.<br />
Phylogenetic analyses based on cpDNA sequence data<br />
As the chloroplast genome is inherited as a single unit <strong>with</strong>out<br />
recombination, combining sequences from multiple cpDNA regions can be<br />
justified (Soltis & Soltis, 1998). Because all six cpDNA sequenced regions used<br />
in this study occur in the haploid chloroplast genome and their histories are<br />
linked, there is no priori reason to infer that their resulting gene trees will differ.<br />
However, their patterns <strong>of</strong> evolution might be different (e.g. differences in<br />
evolutionary rates and/or base compositions), leading to the incongruence<br />
among datasets (Bull et al., 1993; Wiens, 1998). Keeping these in mind, I<br />
concatenate all these regions to a single sequence data set.<br />
Maximum parsimony (MP), maximum likelihood (ML) and Bayesian<br />
phylogenetic inference were employed for phylogenetic analyses using a<br />
concatenate data set (Table 1-3). MP analyses were conducted in PAUP*<br />
v.4.0b10 (Sw<strong>of</strong>ford, 2002) using heuristic <strong>sea</strong>rches, tree-bisection–reconnection<br />
(TBR) branch swapping algorithm, and all characters were unweighted and<br />
unordered. Branch support was evaluated by bootstrapping method <strong>of</strong><br />
Felsenstein (Felsenstein, 1985) based on 1000 replicates.<br />
ML analysis was employed using the program RAxML (Randomized<br />
Axelerated Maximum Likelihood) version 7.2.6 which implements a rapid hill<br />
climbing algorithm (Stamatakis, 2006). The analysis was run <strong>with</strong> indel and<br />
inversion characters removed under the GTR+G model <strong>of</strong> evolution and best-<br />
18
scoring ML tree inferences. Rapid bootstrap analysis was conducted <strong>with</strong> 1000<br />
replications to assess branch support.<br />
Partitioned Bayesian inference were performed <strong>with</strong> MrBayes v.3.1.2<br />
(Ronquist & Huelsenbeck, 2003). The data set was divided into two partitions;<br />
aligned nucleotides and coded indels and inversions. For nucleotide sequences<br />
GTR+I model was selected as a best-fit model according to the Akaike<br />
information criterion (AIC) by MrModel Test v.2 (Nylander, 2004) and binary<br />
model was employed for coded indels and inversions. Two independent<br />
Markov Chain Monte Carlo (MCMC) analyses <strong>with</strong> four simultaneous chains<br />
and 5,000,000 generations were run. Trees were sampled every 100<br />
generations and the first 20000 trees were discarded as burn-in. MCMC chains<br />
convergence was visualized <strong>with</strong> Tracer v. 1.5 (Rambaut & Drummond, 2009)<br />
and likelihood scores for sampled trees were inspected.<br />
Phylogenetic analyses based on ITS sequence data<br />
For nrDNA ITS sequence data, small number <strong>of</strong> samples were surveyed<br />
comparing to the comprehensive cpDNA samples (36 vs. 88). Maximum<br />
parsimony (MP) and neighbor joining (NJ) analyses were performed <strong>with</strong><br />
PAUP* v.4.0b10 (Sw<strong>of</strong>ford, 2002) for nrDNA ITS sequences (Table 1-2). MP<br />
analyses were conducted using heuristic <strong>sea</strong>rches, tree-bisection–reconnection<br />
(TBR) branch swapping algorithm, and all characters were unweighted and<br />
unordered. Branch support was evaluated by bootstrapping method <strong>of</strong><br />
Felsenstein (Felsenstein, 1985) based on 1000 replicates. The NJ tree was<br />
constructed using the distance set to Kimura 2-parameter model (Kimura,<br />
19
1980) and bootstrap analysis based on 100 replicates. Combine sequence data<br />
set <strong>of</strong> cpDNA and nrDNA ITS was performed based on NJ method. In the both<br />
method Canavalia hirsutissima and Canavalia villosa from subgenus<br />
Wenderothia are defined as outgroups.<br />
Network analyses<br />
20
1-3 Results<br />
Phylogenetic analyses based on cpDNA sequence data<br />
The concatenate cpDNA aligned sequence, which consisted <strong>of</strong> 88<br />
sequences from 16 species, yielded 27 haplotypes (H1-27) <strong>with</strong> total length <strong>of</strong><br />
5654 characters after excluding all gaps and ambiguous characters. In total<br />
seven indels and inversions were coded as binary codes. MP analyses retained<br />
16112 most parsimonious trees <strong>with</strong> tree length <strong>of</strong> 145, consistency index (CI)<br />
<strong>of</strong> 0.862, retention index (RI) <strong>of</strong> 0.807 and rescaled consistency index (RC) <strong>of</strong><br />
0.696 (Fig. 1-3). One hundred twenty-two characters were variable, <strong>of</strong> which 57<br />
were parsimony-informative. MP analysis inferred monophyly <strong>of</strong> all ingroup<br />
taxa including members <strong>of</strong> subgenus Canavalia and subgenus Maunaloa all<br />
together <strong>with</strong> 100% bootstrap support. Although, C. ro<strong>sea</strong> is not monophyletic<br />
species, three major clades (I, II and III) were recognized <strong>with</strong> 93, 88 and 83<br />
bootstrap support, respectively (Fig. 1-3). Clade I consisted <strong>of</strong> C. ro<strong>sea</strong><br />
haplotypes, H5 from Java in Indian Ocean and H6 from Tanzania in Indian and<br />
Brazil in Atlantic Ocean. Clade II comprised 3 haplotypes (H16-18) <strong>of</strong> C. ro<strong>sea</strong><br />
which are exclusive to the Atlantic region samples. Haplotypes in this strongly<br />
supported clade are from both West and East Atlantic Ocean <strong>with</strong> longer<br />
21
anch length. Hawaiian endemic species <strong>of</strong> subgenus Maonalua (clade III)<br />
make monophyletic group <strong>with</strong> high bootstrap support (Fig. 1-3). A major<br />
haplotype (H8) was shared among 5 species (C. ro<strong>sea</strong>, C. lineata, C. cathartica,<br />
C. gladiata and C. ensiformis) and also shared among 24 samples <strong>of</strong> C. ro<strong>sea</strong><br />
from very wide distribution range in Indian and Pacific Oceans. Haplotype H2 is<br />
exclusive between C. sericea and C. cathartica from Pacific Ocean and 14<br />
haplotypes <strong>of</strong> C. ro<strong>sea</strong> (H1, H3-4, H7, H9-15 and H19-21) which are mainly<br />
from Atlantic Ocean made polytomies in all phylogenetic analyses. Canavalia<br />
lineata have only an identical haplotype (H8) <strong>with</strong> C. ro<strong>sea</strong>, but C. cathartica<br />
own two haplotypes (H2 and H8) which are shared <strong>with</strong> C. sericea and C. ro<strong>sea</strong>,<br />
respectively (Figs 1-3 and 2-1). Maximum likelihood tree (not shown) and<br />
Bayesian majority role consensus tree (Fig. 1-4) represented an identical<br />
topology for the main clades which was found in MP analyses.<br />
Phylogenetic analyses based on ITS sequence data<br />
Total sequence length <strong>of</strong> nrDNA ITS was 782 for 36 samples and aligned<br />
sequence after excluding all gaps and ambiguous characters yielded 674 bp<br />
(Table 1-2). The analyses inferred monophyly <strong>of</strong> all ingroup taxa including<br />
members <strong>of</strong> subgenus Canavalia and subgenus Maunaloa all together <strong>with</strong><br />
100% bootstrap support same as resultant trees from cpDNA sequences. The<br />
Hawaiian endemic subgenus Maunaloa was grouped <strong>with</strong> subgenus Canavalia<br />
rather than other subgenera (Wenderothia and Catadonia) (Fig. 1-5). MP<br />
analysis results were revealed that members <strong>of</strong> subgenus Maunaloa is<br />
polyphyletic. Although clear phylogenetic relationships among ingroup taxa<br />
22
were not obtained (polytomy), Hawaiian endemic species and some species<br />
have multiple copies <strong>of</strong> ITS sequences. A copy is shared among all species<br />
including C. ro<strong>sea</strong> and others species (haplotype H1).<br />
Resultant tree from combined dataset <strong>of</strong> cpDNA and nrDNA ITS show that<br />
subgenus Maunaloa is a monophyletic group <strong>with</strong> high statistical support<br />
(bootstrap value 88%; Fig. 1-6). Overall, in the nrDNA ITS trees, also same as<br />
cpDNA trees, clear relationships among C. ro<strong>sea</strong> and its allied species was not<br />
resolved.<br />
23
1-4 Discussion<br />
Phylogenetic relationships among C. ro<strong>sea</strong> and its related species<br />
Phylogenetic analyses based on ca. 6000 bp cpDNA sequences are revealed a<br />
monophyletic group including members <strong>of</strong> subgenus Canavalia and subgenus<br />
Maunaloa (Fig. 1-3) which is disclosed by morphological (Sauer, 1964) and<br />
cladistic surveys (De Queiroz et al., 2003). However, our results do not<br />
segregate clear species relationship among C. ro<strong>sea</strong> and its allied species even<br />
using high variable cpDNA regions (Fig. 1-3). Therefore understanding<br />
evolutionary history among these species is rather complicated, and additional<br />
sequences from nuclear genome and ecological surveys are essential to<br />
address such issues (Cronn et al., 2002). On the other hand, the genealogy <strong>of</strong><br />
the cpDNA haplotypes appears somewhat “star phylogeny” (Fig. 2-1), <strong>with</strong> a<br />
common ancestral-like haplotypes (e.g. H7 and H8) lie at the central position<br />
and recent derivatives (rare haplotypes) independently connected to it by short<br />
branches (Avise, 2000). In general, such gene genealogies are interpreted as a<br />
result <strong>of</strong> range expansion (Slatkin & Hudson, 1991; Exc<strong>of</strong>fier, 2004).<br />
Considering phylogenetic trees and haplotype network (Figs 1-3 and 2-1), its<br />
plausible to suppose that recurrent speciation happened among C. ro<strong>sea</strong> and<br />
its allies as reported in numerous <strong>plant</strong> species (Schaal et al., 1998; Kay et al.,<br />
2005; Mort et al., 2007).<br />
Shared haplotypes <strong>of</strong> C. cathartica <strong>with</strong> C. ro<strong>sea</strong> (H8) and C. sericea (H2)<br />
might be sign <strong>of</strong> retention <strong>of</strong> ancestral polymorphisms or traces <strong>of</strong> recent<br />
introgression events. Because I used relatively long cpDNA sequences, this<br />
24
event could not have been caused by lack <strong>of</strong> information on cpDNA regions.<br />
Therefore the possibility <strong>of</strong> introgressive hybridization is more likely, however,<br />
even extensive organelle sequence data sets may have not sufficient power to<br />
conclusively resolve between the ancestral retention and contemporary<br />
introgression (Donnelly et al., 2004).<br />
Interestingly, two well-known crop species Canavalia ensiformis<br />
(Common Jack bean) and Canavalia gladiata (Sword bean) have completely<br />
identical cpDNA sequence haplotype <strong>with</strong> C. ro<strong>sea</strong> (H8) <strong>with</strong> using ca. 6000<br />
highly variable regions. This case shows that cpDNA genome <strong>of</strong> these crop<br />
species is same <strong>with</strong> C. ro<strong>sea</strong> and might suggest that introgression happened<br />
among these species and/or they might be derived from C. ro<strong>sea</strong>, however<br />
further study is necessary.<br />
The phylogeographic break in the Atlantic Ocean<br />
Usually, when there is a sharp geographic boundary between widely<br />
distributed clades, re<strong>sea</strong>rchers assume that such breaks are the result <strong>of</strong><br />
geographic barriers to dispersal, cryptic species boundaries, or recent contacts<br />
between historically allopatric populations (Irwin & Gibbs, 2002). The<br />
haplotypes <strong>of</strong> clade II (H16-18) are specific to Atlantic region <strong>with</strong> high<br />
probability support and Long Branch length (Fig. 1-3). Although possibility <strong>of</strong><br />
cryptic species cannot be completely rejected and the populations in the<br />
African Oceanic regions are not kind <strong>of</strong> allopatric populations, I considered that<br />
long-term geographic barrier to dispersal is responsible to such kind <strong>of</strong><br />
phylogeographic break in the Atlantic Ocean (Fig. 2-2).<br />
25
Origin <strong>of</strong> the Hawaiian endemic species<br />
Volcanic oceanic islands such as Hawaii which have never been<br />
connected to the continents can be colonize by species which have dispersed<br />
to the islands from elsewhere. These islands which separated by thousands <strong>of</strong><br />
kilometers from a source population are usually colonized by water or animaldispersed<br />
<strong>plant</strong> species. According to phylogenetic analyses using nucleotide<br />
sequences <strong>of</strong> 6 chloroplast DNA regions (clade III, Fig. 1-3) and combined<br />
sequence data set <strong>of</strong> cpDNA and nrDNA ITS (Fig. 1-6), Hawaiian endemic<br />
subgenus, Maunaloa, was monophyletic <strong>with</strong> high bootstrap support (84% and<br />
88%, respectively) and it was closely related to subgenus Canavalia than to<br />
other subgenera. These results suggest that the Hawaiian subgenus is a result<br />
<strong>of</strong> single colonization event to the Hawaiian archipelagos.<br />
Although ancestral lineage <strong>of</strong> Hawaiian endemic Canavalia was not<br />
clearly solved but it is plausible to assume that an ancestral species <strong>of</strong> Hawaiian<br />
endemic species, was somewhat similar to C. ro<strong>sea</strong> which has <strong>sea</strong>-<strong>drifted</strong> seed<br />
dispersal ability to reach the Hawaiian Islands. Sauer (1964) and Carlquist<br />
(1966) reported loss <strong>of</strong> seed buoyancy for the members <strong>of</strong> subgenus Maunaloa.<br />
The loss <strong>of</strong> seed buoyancy in these species might be due to decreased air<br />
space in the seeds. In C. ro<strong>sea</strong>, air spaces between the folds <strong>of</strong> the cotyledons<br />
help long-term seed buoyancy on <strong>sea</strong> water (Nakanishi, 1988). Loss <strong>of</strong> seed<br />
buoyancy in oceanic island species is a common phenomenon and occurred in<br />
many species in Hawaiian endemic <strong>plant</strong>s (Carlquist, 1974). Loss <strong>of</strong> seed<br />
dispersal ability had occurred in response to the habitat shift toward inlands<br />
during the speciation process <strong>of</strong> members <strong>of</strong> subgenus Maunaloa.<br />
26
The important attribute <strong>of</strong> reduced seed dispersibility is expected to<br />
restrict gene flow among local populations <strong>with</strong>in the Islands, and may lead to<br />
genetic differentiation among populations. Further studies are required to<br />
assess gene flow and population genetic structure in inland species.<br />
Future prospects for the evolutionary studies among C. ro<strong>sea</strong> and its allied<br />
species<br />
Although <strong>with</strong> using more than 6000 bp cpDNA sequences I could get<br />
overall phylogenetic relationships among C. ro<strong>sea</strong> and its related species,<br />
however, clear evolutionary history among them is not resolved. This is not the<br />
only case which single locous is not able to decipher phylogenetic relationships<br />
among taxa (Cronn et al., 2002). Given the difficulties that closely related taxa<br />
such as the C. ro<strong>sea</strong> present in terms <strong>of</strong> phylogenetic resolution, and the low<br />
sequence divergence found in cpDNA and nrDNA ITS sequences, novel<br />
approaches are needed to integrate not only a combination <strong>of</strong> single copy<br />
genes, but also multiple molecular markers such as Microsatellite or AFLP<br />
markers (Scherson et al., 2005). The use <strong>of</strong> multiple and independent nuclear<br />
loci, promises not only to resolve phylogenetic relationships but also <strong>of</strong>fers a<br />
means by which speciation events may be solved in PPSS.<br />
The results <strong>of</strong> cpDNA phylogeny suggest that recurrent speciation might<br />
occur among C. ro<strong>sea</strong> and its allied species in oceanic islands. However,<br />
complete segregation has not been established between these species and<br />
also some crop species. As theory suggests, long distance dispersal play a role<br />
for range expansion <strong>of</strong> species and because <strong>of</strong> less flow in marginal<br />
27
populations, speciation might occur. Taking account the limited distribution<br />
range <strong>of</strong> allied species <strong>of</strong> C. ro<strong>sea</strong> and also endemic species <strong>of</strong> Hawaiian Islands,<br />
this kind <strong>of</strong> speciation might occurred among C. ro<strong>sea</strong> and its daughter species<br />
(C. cathartica, C. lineata and C. sericea) in Indo-West pacific region and also for<br />
Hawaiian endemic species at oceanic islands which produced an endemic<br />
subgenus. In terms <strong>of</strong> speciation, long distance seed dispersal clearly<br />
contributed in species diversity in oceanic islands.<br />
28
Subgenus Taxon Oceanic Region Locality N.<br />
Canavalia C. ro<strong>sea</strong> (Sw.) DC.<br />
Indian Ocean South Africa Umdloti 2<br />
Tanzania Dar es salaam 2<br />
Sri Lanka Wattala, Negambo 2<br />
Thailand Phuket, Kmala Beach 1<br />
Indonesia Bali 1<br />
Java 1<br />
Sumatra 1<br />
Australia Darwin 2<br />
Headland Harbour 1<br />
West Pacific Thailand Kho Samui 1<br />
Taiwan Houpihu 1<br />
Singapore Singapore 1<br />
Philippine Quezon, Luzon 1<br />
Australia Queensland 2<br />
Japan Iriomote 2<br />
New Caledonia Plage de poe 1<br />
Fiji Korotogo 1<br />
Tonga Sopu 1<br />
Samoa Samoa 1<br />
Marquises Taipivai, Nuku Hiva 1<br />
East Pacific Mexico Nayarit 2<br />
Sinaloa 1<br />
Oaxaca 1<br />
Costa Rica Jaco Beach 1<br />
Panama Veracruz 1<br />
Ecuador Isla Jambel 1<br />
West Atlantic Mexico Coatzcoalcos 2<br />
Costa Rica Puerto Viejo 1<br />
Panama Pina, Colon 4<br />
Cuango, Colon 3<br />
Brazil Para 2<br />
Gaibu Pernanbuco 1<br />
Rio De Janeiro, Arraial do Cabo 1<br />
Rio De Janeiro, Recreio 2<br />
East Atlantic Senegal Joal-Fadiout 8<br />
Ghana Busua beach 4<br />
Angola Musul, Luanda 1<br />
Subtotal 62<br />
Table 1‐1. List <strong>of</strong> Canavalia samples used for cpDNA phylogenetic analyses. N, number<br />
<strong>of</strong> individuals in each population. (to be continued)<br />
29
Subgenus Taxon Oceanic Region Locality N.<br />
C. cathartica Thouars Pacific Philippine Atimona 1<br />
Samoa Samoa 1<br />
Tonga Tonga 1<br />
Tahiti Tahiti 1<br />
Hawaii Kauai 1<br />
Subtotal 5<br />
C. lineata (Thunb.) DC. Pacific Taiwan Maopi Tao 1<br />
Japan Ishigaki 1<br />
Miyazaki 1<br />
Ogasawara 1<br />
Subtotal 4<br />
C. sericea A. Gray Pacific Tonga Haashini-Lavengatonga 2<br />
Hawaii Maui, Bishop Museum 1<br />
Subtotal 3<br />
C. virosa (Roxb.) Wight & Arn. Atlantic Africa Seed purchased 1<br />
C. gladiata (Jacq.) DC. Pacific Japan Seed purchased 1<br />
C. ensiformis (L.) DC. Pacific Japan Seed purchased 1<br />
Maunaloa C. hawaiiensis Degener & al. Pacific Hawaii Bishop Museum 1<br />
C. napaliensis St. John Pacific Hawaii Bishop Museum 1<br />
C. galeata Gaudich. Pacific Hawaii Bishop Museum 1<br />
C. pubescens Hook. & Arn. Pacific Hawaii Bishop Museum 1<br />
C. kauaiensis J.D. Sauer Pacific Hawaii Bishop Museum 1<br />
C. molokaiensis Degener & al. Pacific Hawaii Bishop Museum 1<br />
C. hawaiiensis Degener & al. Pacific Hawaii Center for Conservation Re<strong>sea</strong>rch and Training (CCRT) 1<br />
C. galeata Gaudich. Pacific Hawaii Center for Conservation Re<strong>sea</strong>rch and Training (CCRT) 1<br />
Catodonia Canavalia parviflora Benth. Atlantic Brazil Jardim Botanico (Rio de Janeiro) 1<br />
Wenderothia Canavalia villosa Benth. Atlantic Mexico MEXU 1<br />
Canavalia hirsutissima J.D. Sauer Atlantic Mexico MEXU 1<br />
Total 88<br />
Table 1‐1. continued<br />
30
N. Subgenus Taxon Oceanic region Locality DNA voucher Sequence method<br />
1 Canavalia C. ro<strong>sea</strong> (Sw.) DC. Indian Ocean South Africa Umdloti 98 Cloning<br />
2 Tanzania Dar es salaam 184 Cloning<br />
3 Sri Lanka Wattala, Negambo 31 Cloning<br />
4 Indonesia Sumatra 500 Direct<br />
5 Australia Headland Harbour 1 Direct<br />
6 West Pacific Marquises Taipivai, Nuku Hiva 31 Direct<br />
7 Tonga Sopu 171 Direct<br />
8 East Pacific Mexico Sinaloa 965 Direct<br />
9 Panama Veracruz 202 Direct<br />
10 Ecuador Isla Jambel 1205 Direct<br />
11 West Atlantic Panama Cuango, Colon 110 Direct<br />
12 Panama Pina, Colon 24 Cloning<br />
13 Costa Rica Puerto Viejo 346 Cloning<br />
14 Mexico Coatzcoalcos 71 Cloning<br />
15 Brazil Gaibu Pernanbuco 70 Cloning<br />
16 East Atlantic Senegal Joal-Fadiout 107 & 118 Cloning<br />
17 Ghana Busua beach 5 Direct<br />
18 Angola Musul, Luanda 0 Cloning<br />
Subtotal 19<br />
19 C. cathartica Thouars Pacific Philippine Atimona CH10 Cloning<br />
Subtotal 1<br />
20 C. lineata (Thunb.) DC. Pacific Taiwan Maopi Tao CL1 Direct<br />
21 Japan Miyazaki 74 Cloning<br />
Subtotal 2<br />
22 C. sericea A. Gray Pacific Tonga Haashini-Lavengatonga 42 Direct<br />
23 Pacific Tonga Haashini-Lavengatonga 138 Cloning<br />
Subtotal 2<br />
24 C. virosa (Roxb.) Wight & Arn. Atlantic Africa Seed purchased S3F8 Direct<br />
25 Maunaloa C. hawaiiensis Degener & al. Pacific Hawaii Bishop Museum 6 Clonig<br />
26 C. galeata Gaudich. Pacific Hawaii Bishop Museum 7 Clonig<br />
27 C. kauaiensis J.D. Sauer Pacific Hawaii Bishop Museum 9 Clonig<br />
28 C. molokaiensis Degener & al. Pacific Hawaii Bishop Museum 4 Clonig<br />
29 C. napaliensis St. John Pacific Hawaii Bishop Museum 5 Clonig<br />
30 C. pubescens Hook. & Arn. Pacific Hawaii Bishop Museum 8 Clonig<br />
31 C. hawaiiensis Degener & al. Pacific Hawaii Center for Conservation Re<strong>sea</strong>rch and Training (CCRT) C6 Direct<br />
32 C. galeata Gaudich. Pacific Hawaii Center for Conservation Re<strong>sea</strong>rch and Training (CCRT) C7 Direct<br />
33 Catodonia Canavalia parviflora Benth. Atlantic Brazil Jardim Botanico (Rio de Janeiro) 809 Direct<br />
34 Wenderothia Canavalia villosa Benth. Atlantic Mexico MEXU 23 Direct<br />
35 Canavalia hirsutissima J.D. Sauer Atlantic Mexico MEXU 11 Direct<br />
Total 36<br />
Table 1‐2 List <strong>of</strong> Canavalia samples used for nrDNA ITS phylogenetic analyses.<br />
31
Primer name Length (bp) Primer Pairs Sequence (5'- 3') Annealing Tm. Source<br />
atpB -rbcL IGS 518-742 atpB GTGGAAACCCCGGGACGAGAAGTAGT 52 °C Hodges and Arnold, 1994<br />
rbcL ACTTGCTTTAGTTTCTGTTTGTGGTGA Hodges and Arnold, 1994<br />
ndhD -ndhE 670 ndhD GAAAATTAAGGAACCCGCAA 48 °C Xu et. al 2000<br />
ndhE TCAACTCGTATCAACCAATC Xu et. al 2000<br />
psbA -trnH IGS 264-338 psbA CGAAGCTCCATCTACAAATGG 48 °C Hamilton 1998<br />
trnH ACTGCCTTGATCCACTTGGC Hamilton 1998<br />
rps16 Intron 781-850 rps16 F GTGGTAGAAAGCAACGTGCGACTT 52 °C Oxelman et al., 1997<br />
rps16 2R TCGGGATCGAACATCAATTGCAAC Oxelman et al., 1998<br />
trnD -trnT 1036-1055 trnD ACCAATTGAACTACAATCCC 52 °C Demesure et al. (1995)<br />
trnT CTACCACTGAGTTAAAAGGG Demesure et al. (1995)<br />
trnK 2485-2532 trnK 1L CTCAATGGTAGAGTACTCG 52 °C Lavin et al. (2000)<br />
trnK 685F GTATCGCACTATGTATCATTTGA Wojciechowski et al. (2004)<br />
matK 789R TAGGAAATCCTGGTGGCGAGATC Hu et al. (2000)<br />
matK 1777L TTCAGTGGTACGAAGTCAAATG Hu et al. (2000)<br />
matK 1932R CAGACCGACTTACTAATGGG Hu et al. (2000)<br />
trnK 2R AACTAGTCGGATGGAGTAG Johnson & Soltis (1994)<br />
nrDNA ITS 674 ITS5 GGAAGTAAAAGTCGTAACAAGG 54 °C White et al. 1990<br />
ITS4 TCCTCCGCTTATTGATATGC White et al. 1990<br />
Table 1‐3 List <strong>of</strong> primers used for amplifications and sequencing <strong>of</strong> chloroplast regions.<br />
PCR amplification primers are shown in bold.<br />
32
Figure 1‐1. Canavalia ro<strong>sea</strong> and its related species. A: Canavalia ro<strong>sea</strong>, B: C.<br />
cathartic, C: C. lineata, D: C. sericea, E: C. ensiformis, F: C. gladiata. G: C.<br />
villosa, H: C. pubescens,I: seed <strong>of</strong> C. ensiformis (1), C. gladiata (2), C. ro<strong>sea</strong><br />
(3), C. lineata (4).<br />
33
A<br />
B<br />
Figure 1‐2. A: Distribution range <strong>of</strong> PPSS species. B: Distribution range <strong>of</strong> Canavalia<br />
ro<strong>sea</strong> and its related species. In each <strong>of</strong> the encircled areas, C. ro<strong>sea</strong>, C. cathartica,<br />
C. lineata and C. sericea are distributed in the coastal areas and the members <strong>of</strong><br />
subgenus Maunaloa are distributed in inland areas.<br />
34
Figure 1‐3. Phylogram <strong>of</strong> strict consensus tree <strong>of</strong> 16112 shortest tree based on<br />
Maximum Parsimony (MP) analysis from 6 cpDNA regions <strong>with</strong> ca. 6000 bp for<br />
Canavalia species (Tree length=145, CI= 0.862, RI= 0.807 and RC= 0.696).<br />
Bootstrap values are shown above branches. Canavalia hirsutissima and<br />
Canavalia villosa from subgenus Wenderothia and Canavalia parviflora from<br />
subgenus Catedonia are defined as outgroups. Twenty seven haplotypes (H1‐29)<br />
were detected for C. ro<strong>sea</strong> and its allied species. Abbreviations in parenthesis are:<br />
P (Pacific Ocean); A (Atlantic Ocean); I (Indian Ocean); Numbers in the localities<br />
correspond to the number <strong>of</strong> sequenced individuals in that locality.<br />
36
Figure 1‐4. The Bayesian phylogram using 80 samples <strong>of</strong> Canavalia ro<strong>sea</strong> and other<br />
species based on concatenate cpDNA data set. Support for nodes is estimated<br />
from Bayesian posterior probabilities. Support values ≥70% is given. The legends<br />
are as follows: P (Pacific Ocean); A (Atlantic Ocean); I (Indian Ocean).<br />
37
Figure 1‐5. Phylogram <strong>of</strong> strict consensus tree <strong>of</strong> 28 shortest tree based on Maximum<br />
Parsimony (MP) analysis from nrDNA ITS for members <strong>of</strong> subgenus Canavalia and<br />
Maunaloa (bold) (Tree length=92, CI= 0.9457, RI= 0.9920 and RC= 0.9381).<br />
Bootstrap values are shown near branches. Canavalia hirsutissima and Canavalia<br />
villosa from subgenus Wenderothia are defined as outgroups. Abbreviations in<br />
parenthesis are DNA voucher numbers. Letters A and P correspond to Atlantic<br />
and Pacific Oceanic regions, respectively.<br />
38
Figure 1‐6. Strict consensus tree resulting from combined cpDNA and ITS sequence data<br />
for members <strong>of</strong> subgenus Canavalia and Maunaloa (bold). Numbers near<br />
branches indicate bootstrap values. Canavalia hirsutissima and Canavalia villosa<br />
from subgenus Wenderothia are defined as outgroups. Abbreviations in<br />
parenthesis are DNA voucher numbers. Letters A and P correspond to Atlantic<br />
and Pacific Oceanic regions, respectively.<br />
39
Figure 1‐7. Haplotype network among Canavalia ro<strong>sea</strong> and its related species based on<br />
statistical parsimony method. Each segment <strong>of</strong> branch shows the one step<br />
difference <strong>of</strong> molecular data. C. ro<strong>sea</strong> has the greatest diversity <strong>of</strong> haplotypes<br />
in the Atlantic region than Pacific and Indian Ocean. Hawaiian endemic<br />
species are more closely related to a haplotype from the Atlantic (Panama‐<br />
Angola) which may suggest that these species are diversified from Atlantic before<br />
closure <strong>of</strong> Panama Isthmus.<br />
40
CHAPTER 2<br />
GLOBAL GENETIC STRUCTURE OF CANAVALIA ROSEA; EVIDENCE<br />
FROM CHLOROPLAST DNA SEQUENCES<br />
2-1 Introduction<br />
Gene flow is considered as a main factor responsible for genetic<br />
cohesion among populations <strong>of</strong> a species (Olmstead & Palmer, 1994). In fact,<br />
when levels <strong>of</strong> gene flow <strong>with</strong>in and among populations become high (e.g.<br />
greater than four migrants per generation), it homogenize the species and<br />
prevents genetic divergence <strong>of</strong> populations; otherwise local populations can<br />
evolve and eventually form a distinct species (Wright, 1931; Ennos, 1994;<br />
Bohonak, 1999). Population differentiation can also results from environmental<br />
impediments or intrinsic barriers (Avise, 2000). Therefore sufficient amount <strong>of</strong><br />
genetic exchange among populations is expected to hold a species as a<br />
cohesive unit in spatially continuous populations.<br />
Populations <strong>of</strong> many <strong>plant</strong> species are spatially isolated from each other<br />
due to presence <strong>of</strong> physical or ecological barriers such as land masses or water<br />
barriers (Cain et al., 2000). As a result, the distribution range <strong>of</strong> many <strong>plant</strong><br />
species are structured to the specific localities like Indo West Pacific (IWP) and<br />
Atlantic East Pacific (AEP) in some <strong>plant</strong> species such as mangroves (Duke et al.,<br />
40
2002; Nettel & Dodd, 2007) and PPSS such as Hibiscus tiliaceus (Takayama et al.,<br />
2006). In H. tiliaceus, PCR-SSCP (PCR amplification <strong>with</strong> single-strand<br />
conformation polymorphism) and PCR-SSP (PCR amplification <strong>with</strong> sequence<br />
specific primers) analyses performed on more than 1100 samples from 65<br />
populations worldwide to illustrate genetic structure <strong>of</strong> populations in very<br />
wide distribution range. The results revealed that gene flow occurred among<br />
populations <strong>of</strong> H. tiliaceus in Indo-West Pacific region and also over the African<br />
continent due to <strong>sea</strong>-<strong>drifted</strong> seeds and introgression was happened between H.<br />
tiliaceus and H. pernambucensis populations in the Atlantic region. On the<br />
other hand, the American continent was the barrier to gene flow through <strong>sea</strong><strong>drifted</strong><br />
seed dispersal among populations <strong>of</strong> H. pernambucensis (Takayama et<br />
al., 2006; Takayama et al., 2008). These results suggest the importance <strong>of</strong> gene<br />
flow through <strong>sea</strong>-<strong>drifted</strong> seeds over the barriers to keep the unity <strong>of</strong> the<br />
species and also the role <strong>of</strong> American continent as a strong barrier to gene<br />
flow. For globally distributed single PPSS such as C. ro<strong>sea</strong> the existence <strong>of</strong> these<br />
barriers seems to be critical to keep gene flow over its distribution range as the<br />
possibilities <strong>of</strong> cryptic species would be expected.<br />
Presence <strong>of</strong> cryptic species is popular in many <strong>plant</strong>s species where<br />
morphological diversification might not be happened among lineages. In<br />
chapter 1, the result <strong>of</strong> phylogenetic analyses detected some distinct<br />
haplotypes which were specific to the Atlantic region (clade II, Fig. 1-3). As<br />
discussed in chapter 1, usually when there is such kind <strong>of</strong> sharp geographic<br />
boundary between widely distributed clades, it is assumes that it might be a<br />
result <strong>of</strong> geographic barriers to dispersal or possibility <strong>of</strong> cryptic species<br />
boundaries (Irwin & Gibbs, 2002). However, gross population data is necessary<br />
41
to infer the existence <strong>of</strong> gene flow over African and American continents to<br />
keep the unity <strong>of</strong> C. ro<strong>sea</strong> in distant populations. Therefore, the main question<br />
targeted in this chapter is: How can a single species keep gene flow over the<br />
extremely wide range <strong>of</strong> distribution?<br />
A variety <strong>of</strong> genetic markers can be used to quantify the gene flow<br />
through seed dispersal. As discussed by Parker (1998), Ouborg (1999) and<br />
others, these markers include allozymes, DNA sequences, microsatellites,<br />
restriction fragment length polymorphisms (RFLPs), and DNA randomly<br />
amplified from the genome (e.g., RAPDs and AFLPs). Many <strong>plant</strong>s species<br />
exchange genes among populations by the movement <strong>of</strong> pollen and seed.<br />
Only dispersal via seed directly bears on colonization <strong>of</strong> new populations.<br />
Movement <strong>of</strong> both pollen and seed, however, leaves a genetic signature <strong>with</strong>in<br />
and among populations. Therefore, estimating gene flow among <strong>plant</strong><br />
populations from nuclear DNA, which is transferred via pollen and seed, may<br />
tend to overestimate seed dispersal (Cain et al., 2000). Because <strong>of</strong> this effect,<br />
estimation <strong>of</strong> the seed dispersal requires appropriate markers inherited only<br />
through seeds. In most angiosperms, chloroplast DNA (cpDNA) is regarded as<br />
single locus and maternally inherited through seeds (Corriveau & Coleman,<br />
1988; Mogensen, 1996). So, it has been utilized to discover phylogenetic and<br />
phylogeographic patterns in many <strong>plant</strong> species (Schaal et al., 1998; Petit et al.,<br />
2005; Soltis et al., 2006; Avise, 2009). On the other hand, uniparentally inherited<br />
markers such as cpDNA may be informative at the interspecific and<br />
intraspecific level (Wakeley, 2003).<br />
There are many statistical methods for retrieving information from<br />
molecular markers to reveal evolutionary relationships among species and<br />
42
estimating important population parameters (Exc<strong>of</strong>fier & Heckel, 2006). A<br />
variety <strong>of</strong> analytical methods exists to estimates gene flow through seed<br />
dispersal such as F ST -based methods (Wright, 1951), Likelihood-based methods<br />
(Rannala & Hartigan, 1996) and Coalescent-based methods (Beerli &<br />
Felsenstein, 1999). Although the latter rely on more realistic parameters than<br />
the others (Kuhner, 2009).<br />
For this purpose, I employed molecular markers using short fragments <strong>of</strong><br />
6 cpDNA regions and performing population genetic analysis in global scale.<br />
Population genetic analyses based on pairwise F ST and coalescent-based<br />
methods, were conducted for 515 individuals from 48 populations using more<br />
than 2000 bp nucleotide sequences to elucidate the spatial genetic structure <strong>of</strong><br />
C. ro<strong>sea</strong> populations in its entire distribution range.<br />
43
2-2 Materials and Methods<br />
Sampling<br />
Leaf samples were collected in large-scale, covering almost all<br />
distribution ranges <strong>of</strong> the species. In total, 436 individuals (37 populations)<br />
from Canavalia ro<strong>sea</strong>, 25 individuals (5 populations) from C. cathartica, 42<br />
individuals (4 populations) from C. lineata, and 12 individuals (2 populations)<br />
from C. sericea were included in this study (Table 2-1). Voucher specimens<br />
were deposited in the herbarium <strong>of</strong> University <strong>of</strong> the Ryukyus (RYU), Jardim<br />
Botânico, Rio de Janeiro (RBRJ) and Bishop Museum, Honolulu, Hawaii.<br />
DNA extraction, PCR, and sequencing<br />
DNA extraction, PCR and sequencing methods are same as described<br />
methods in chapter 1.<br />
Haplotype Composition and Network <strong>of</strong> C. ro<strong>sea</strong> and its allied species<br />
In chapter 1, I surveyed more than 6000 bp cpDNA sequences for<br />
Canavalia samples from wide range <strong>of</strong> distribution. As sequencing <strong>of</strong> more<br />
than 6000 bp <strong>of</strong> cpDNA genome for all population samples (515 individuals) is<br />
required extra labor and cost, I targeted partial sequences <strong>of</strong> 6 cpDNA regions<br />
(Table 2-2) based on the results <strong>of</strong> phylogenetic analyses (cf. chapter 1). Several<br />
new internal primers were designed for these 6 short fragments and in total<br />
44
2012 base pairs were sequenced for all individuals. Sequences were edited and<br />
aligned as chapter 1 and haplotype composition <strong>of</strong> each population was<br />
recorded. The haplotypes frequency <strong>of</strong> populations was presented as pie charts<br />
on the world map. The genealogical relationships <strong>of</strong> haplotypes were<br />
constructed <strong>with</strong> TCS program (Clement et al., 2000) using statistical parsimony<br />
method <strong>with</strong> 95% confidence interval (Templeton et al., 1992). For population<br />
analyses, all populations <strong>of</strong> C. ro<strong>sea</strong> were divided into five regional groups<br />
(West-East Atlantic Ocean, Indian Ocean and West-East Pacific Ocean) based<br />
on geography, phylogenetic results (cf. chapter 1) and observed haplotypes.<br />
Populations <strong>of</strong> C. cathartica, C. lineata and C. sericea were excluded from all<br />
population analyses.<br />
Population differentiation<br />
To compare chloroplast genetic diversity among population <strong>of</strong> five oceanic<br />
regional groups, I calculated numbers <strong>of</strong> haplotypes (H), polymorphis site (S),<br />
Haplotype diversity (Hd) and nucleotide diversity (π) using the program DnaSP<br />
version 5.10 (Librado & Rozas, 2009). To determine the amount <strong>of</strong> genetic<br />
differentiation among populations <strong>of</strong> C. ro<strong>sea</strong>, F-statistics (F ST ) analysis (Wright,<br />
1951) performed by the program AREQUIN v. 3.11 (Exc<strong>of</strong>fier et al., 2005).<br />
Pairwise F ST was calculated following the method <strong>of</strong> Weir & Cockerham (1984)<br />
and statistical significance was assessed using 1000 permutations. An exact test<br />
<strong>of</strong> population differentiation was performed to examine the null hypothesis <strong>of</strong><br />
the random distribution <strong>of</strong> haplotypes across populations (Raymond & Rousset,<br />
1995).<br />
To clarify groups <strong>of</strong> C. ro<strong>sea</strong> populations which are geographically<br />
homogeneous and maximally differentiated from each other, spatial analysis <strong>of</strong><br />
45
molecular variance (SAMOVA; Dupanloup et al. 2002) was conducted. To<br />
ensure that the conformation <strong>of</strong> the groups (K) is not affected by the given<br />
initial conditions, the simulated annealing procedure is repeated 100 times<br />
(Dupanloup et al., 2002). The analyses were repeated for user-defined groups<br />
(K) from 2 to 12, and the highest FCT values was maintained as the best<br />
grouping <strong>of</strong> populations in case there are not included single population<br />
(Heuertz et al., 2004). Because SAMOVA analysis uses locality coordination and<br />
sampling scale in this study cover the whole equatorial belt, arbitrary<br />
coordinates were tried to avoid miscalculation <strong>of</strong> analyses.<br />
Historical migration rates between oceanic regions<br />
To assess migration rates, direction <strong>of</strong> gene flow and genetic diversity among<br />
populations <strong>of</strong> C. ro<strong>sea</strong>, I applied coalescent approach (Kingman, 1982a, b)<br />
using the Maximum likelihood and Bayesian inference methods implemented<br />
in MIGRATE-N version 3.1.3 (Beerli & Felsenstein, 1999; 2001; Beerli, 2008).<br />
Coalescent based genealogies provide more realistic estimates <strong>of</strong> population<br />
parameters than other summary statistics methods (Kuhner, 2009). I was<br />
specifically interested in contrasting the migration rate and direction <strong>of</strong> gene<br />
flow between geographic regions rather than between sampled populations.<br />
Hence, all populations were pooled into five regional groups (West-East<br />
Atlantic Ocean, Indian Ocean and West-East Pacific Ocean). Given the linear<br />
distribution <strong>of</strong> C. ro<strong>sea</strong> at coastal lines, the stepping stone migration model<br />
<strong>with</strong> asymmetric rates was employed (Kimura & Weiss, 1964).<br />
For each <strong>of</strong> the five regional groups, the genetic diversity (θ=Neμ, where<br />
Ne is the effective population size and µ is the mutation rate per site per<br />
generation), pairwise migration rate (M=m/μ, where m is the rate <strong>of</strong> migration<br />
46
for each locus) and number <strong>of</strong> migrants per generation (Nm=Mθ) were<br />
estimated. Starting parameters for migrant values and θ were generated from<br />
F ST calculation. For Maximum likelihood analysis, 20 short chains (length 5.0 x<br />
10 4 ) followed by 5 long chains (length 5.0 x 10 5 ) <strong>with</strong> sample increment <strong>of</strong> 100<br />
and for both run were conducted and the first 15000 generations were<br />
discarded as burn-in at the beginning <strong>of</strong> each chain. An adaptive heating<br />
scheme <strong>with</strong> 4 chains and a swapping interval <strong>of</strong> 1 was applied. Maximum<br />
likelihood estimates (MLE) were verified <strong>with</strong> three replicate Markov Chain<br />
Monte Carlo (MCMC) simulation runs to ensure convergence <strong>of</strong> similar values<br />
for θ.<br />
Bayesian MCMC coalescent modeling were also used which is provide<br />
parameter estimates based on full likelihood estimation and decreased<br />
computation time <strong>of</strong> approximation comparing to Maximum likelihood<br />
estimates. Bayesian parameters included an update frequency <strong>of</strong> 0.5, a<br />
Metropolis-Hastings sampling algorithm for both θ and M; uniform priors were<br />
placed on θ from 0 to 0.001 and M from 0 to 50000. Starting parameters for<br />
migrant values and θ were generated from F ST calculation. An adaptive heating<br />
scheme <strong>with</strong> 4 chains and a swapping interval <strong>of</strong> 1 was applied. I used the<br />
Felsenstein 84 model <strong>of</strong> evolution, and set the transition to transversion ratio<br />
to 2 as a default values in the program. Six independent MCMC runs <strong>of</strong> varying<br />
length and burn-in were conducted which produced similar results. Hence, I<br />
present results from the longest run which consisted a long chain <strong>of</strong> 50 million<br />
steps <strong>with</strong> sample increment <strong>of</strong> 100 and the first 5 million steps were discarded<br />
as burn-in. Using tracer v1.5 (Rambaut & Drummond, 2009) convergence <strong>of</strong><br />
the likelihood in MCMC chains and effective sample size (ESS) observed<br />
47
following the burn-in. The analyses were considered as converged upon a<br />
stationary distribution, if the different runs generated similar posterior density<br />
distributions <strong>with</strong> a minimum ESS <strong>of</strong> 100 (Hey, 2005; Kuhner & Smith, 2007).<br />
Estimates <strong>of</strong> recent migration rates<br />
Although estimating <strong>of</strong> gene flow and migration rates using MIGRATE-N based<br />
on coalescent methods have many advantages comparing to the other<br />
conventional methods, it also has drawback in separation <strong>of</strong> recurrent gene<br />
flow from ancestral polymorphism (Carbone et al., 2004; Brito, 2005; Bowie et<br />
al., 2006; Kane et al., 2009). To distinguish whether the estimated migration<br />
rates from MIGRATE-N are the result <strong>of</strong> the retention <strong>of</strong> ancestral<br />
polymorphism or recent gene flow, additional coalescent based analyses were<br />
conducted using the program MDIV which is implements both likelihood and<br />
Bayesian methods using MCMC coalescent simulations for jointly estimating <strong>of</strong><br />
the θ and M (Nielsen & Wakeley, 2001).<br />
Theta and M for pairwise comparisons <strong>of</strong> each <strong>of</strong> the five oceanic<br />
regional groups were estimated. Uniform prior Values for Mmax (maximum<br />
value for the scaled migration rate) and θ was set to the 10 and zero,<br />
respectively. The program ran under the default finite sites mutation model <strong>of</strong><br />
HKY (Hasegawa et al., 1985); <strong>with</strong> Markov chain simulation for 5000000 steps,<br />
where the first 500000 were discarded as burn-in. Multiple runs <strong>with</strong> different<br />
random seeds and prior distributions were conducted to determine if the<br />
analyses were reached to the convergence in the mode <strong>of</strong> the posterior<br />
distribution (Nielsen & Wakeley, 2001).<br />
48
2-3 Results<br />
Haplotype Composition and Network <strong>of</strong> C. ro<strong>sea</strong> and its allied species<br />
For population analyses 2012 bp aligned sequences were attained using partial<br />
sequence <strong>of</strong> 6 cpDNA regions which is including 12 substitutions, 2 indels and<br />
one inversion (Table 2-3). Through 21 haplotypes (H1-21) which were detected<br />
in chapter 1 by full sequence <strong>of</strong> 6 cpDNA regions among samples <strong>of</strong> four<br />
species (C. ro<strong>sea</strong>, C. lineata, C. cathartica and C. sericea), I detected 17<br />
haplotypes (H1-17) by partial sequences at population level (Fig. 2-1; Table 2-<br />
1). Four haplotypes, H18 and H19-21 <strong>of</strong> phylogenetic analyses (chapter 1)<br />
could not be detected by partial sequences and therefore they are identical to<br />
haplotypes H16 and H7 in population analyses (this chapter), respectively.<br />
Haplotype network based on full sequence length were shown in figure 2-1.<br />
Colors in the network correspond to the haplotypes which could detect by<br />
partial sequence <strong>of</strong> 6 short fragments (H1-17). All haplotypes were shared<br />
among C. ro<strong>sea</strong> populations except haplotype H2 which is exclusive to C.<br />
cathartica and C. sericea populations from Pacific Ocean (n= 18; Fig. 2-2; Table<br />
2-1). A major haplotype (H8) was shared among C. ro<strong>sea</strong>, C. lineata and C.<br />
cathartica populations from Indian and Pacific Oceanic regions (n=293), (Fig. 2-<br />
2). Notably, all samples <strong>of</strong> C. lineata (n=42) have an identical haplotype <strong>with</strong> C.<br />
ro<strong>sea</strong> haplotype (H8), however, C. cathartica shares haplotypes <strong>with</strong> C. ro<strong>sea</strong><br />
(H8, n=19) and <strong>with</strong> C. sericea (H2, n=6). Another major haplotypes <strong>of</strong> C. ro<strong>sea</strong><br />
were found in Atlantic and Indian Oceanic region including H7 (n=45), H6<br />
(n=32), H17 (n=29) and H16 (n=25), respectively (Table 2-1). Haplotype H1<br />
(n=7) shared between a population from southern Brazil (n=1) and Panama<br />
(n=6) in Atlantic Ocean. Haplotype H3 shared between a population from<br />
49
Mexico (n=2) and Senegal (n=7) in Atlantic Ocean; haplotype H4 shared<br />
between 2 populations from Mexico (Nayarit and Sinaloa, n=9) in Pacific Ocean<br />
and haplotypes H5, H9-15 are private haplotypes (haplotypes which is found<br />
only in one population) in oceanic regions (Fig. 2-2; Table 2-1).<br />
Population differentiation<br />
Total haplotype diversity (Hd) and nucleotide diversity (π) <strong>with</strong>in C. ro<strong>sea</strong><br />
populations were estimated to be 0.69124 and 0.00086, respectively (Table 2-4).<br />
The populations at West Atlantic and East Atlantic had the highest haplotype<br />
diversity (0.7809 and 0.74.34, Table 2-4) and populations <strong>of</strong> the West Pacific<br />
Ocean share a lowest haplotype diversity and nucleotide diversity (0.03418 and<br />
0.00002, respectively). Pairwise F ST analysis detected genetic differentiation in 6<br />
out <strong>of</strong> 10 pairs <strong>of</strong> C. ro<strong>sea</strong> populations (5 regional groups) from different<br />
oceanic regions (Table 2-5). The F ST values between the West and East Atlantic,<br />
Indian and West Pacific and between West and East pacific populations were<br />
0.13, 0.19 and 0.16 respectively. The F ST value between the Indian Ocean and<br />
East pacific was 0.08. On the other hand the F ST values between the East<br />
Atlantic and Indian and between East Pacific and West Atlantic and between<br />
and East pacific populations were 0.36 and 0.45 respectively. All differentiations<br />
were significant using an exact test (P < 0.05; Table 2-5).<br />
The results <strong>of</strong> SAMOVA are shown in figure 2-3 and Table 2-6. The<br />
SAMOVA method did not allow to unambiguously identifying the groups <strong>of</strong><br />
populations (K) displaying the highest differentiation among groups, F CT . This<br />
was because F CT values increased progressively as K was increased, reaching a<br />
plateau at K = 8 (Fig. 2-3). The number <strong>of</strong> K which has highest F CT <strong>with</strong>out<br />
single population was K=3 which is divide all populations to three groups<br />
50
(Table 2-6). First group comprise populations from Ghana, Mexico (A), Panama<br />
(colon2), Para and Senegal. Second group includes populations from<br />
Pernambuco, Rio De Janeiro (1 and 2) and Java and the last groups<br />
corresponds to the rests <strong>of</strong> populations (Table 2-6). The composition <strong>of</strong> these<br />
three groups is partially corresponding to the geographical distribution <strong>of</strong><br />
haplotypes visually identified on the haplotype frequency map (Fig. 2-2). From<br />
K=4 to K=10 all groups includes at least single population (populations which<br />
have private haplotypes) which is not appropriate to the analysis (Heuertz et al.,<br />
2004).<br />
Historical migration rates between oceanic regions<br />
Coalescent-based maximum likelihood estimates (MLE) from MIGRATE-N<br />
indicate asymmetric gene flow along the distribution range <strong>of</strong> the C. ro<strong>sea</strong><br />
populations (Table 2-7). The MLE showed that genetic diversity was highest in<br />
the West Atlantic region (θ = 0.0163), and lowest in the West Pacific region (θ<br />
= 0.0069). The most probable estimates <strong>of</strong> migration rates (M) ranged from 0<br />
to 395.7, <strong>with</strong> the highest migration observed out <strong>of</strong> the East Atlantic into the<br />
West Atlantic. In contrast, estimates <strong>of</strong> migration in the both side <strong>of</strong> Panama<br />
Isthmus as well as into the Indian Ocean from the East Atlantic were zero (Table<br />
2-7). Comparing <strong>with</strong> high migration rates between West-East Atlantic region<br />
and between Indian-West Pacific region, migration between the West and East<br />
Pacific was low but significantly greater than zero. The direction <strong>of</strong> migration<br />
was asymmetrical, <strong>with</strong> the West Atlantic region experiencing a greater input <strong>of</strong><br />
polymorphism due to migration (M EA to WA = 395.7) than the East Atlantic (M WA<br />
to EA = 166.4). Based on values <strong>of</strong> M and θ, I calculated a mean probability <strong>of</strong><br />
number <strong>of</strong> migrants per generation (Nm) among 5 regional groups (Table 2-7)<br />
51
which the highest was greater than 8 migrant per generation <strong>with</strong>in East-West<br />
Atlantic region and the lowest was zero between Western and eastern side <strong>of</strong><br />
American continent and Indian region to the Atlantic region. The estimated<br />
number <strong>of</strong> migrants between Indian-West Pacific pairs and between West-East<br />
Pacific pairs were 5.5 and near 1, respectively.<br />
Results <strong>of</strong> pairwise F ST and MIGRATE-N among Indian and West Pacific<br />
Oceanic regions show relatively low genetic differentiation (F ST = 0.19, Table 2-<br />
5) and high number <strong>of</strong> migrants (Nm >5 per generation), respectively (Table 2-<br />
7). Rates <strong>of</strong> gene flow between West and East Pacific regions (F ST = 0.16; Nm ≅<br />
1) were lower than that <strong>of</strong> between Indian and West Pacific which may<br />
consequence <strong>of</strong> very long distance between population in pacific Oceans.<br />
Bayesian inference <strong>of</strong> theta and Migration rates among five groups are<br />
plotted on figures 2-4 and 2-5 respectively. Although Bayesian estimation <strong>of</strong><br />
migration rates looks much bigger than Maximum likelihood estimation but in<br />
total estimates <strong>of</strong> number <strong>of</strong> migrants (Nm) are almost equal in ML and<br />
Bayesian estimation (see fig. 2-6 and Table 2-7). Highest number <strong>of</strong> migrants<br />
was from West Pacific to the Indian Ocean (Nm=10.98; fig. 2-6) and East<br />
Atlantic to West Atlantic region (Nm=9.01).<br />
Estimates <strong>of</strong> recent migration rates<br />
Figure 2-7 shows the posterior distributions for migration rates (M) and<br />
mutation rates (θ) obtained from MDIV program among population <strong>of</strong> C. ro<strong>sea</strong><br />
at different regional groups. Results are interestingly comparable <strong>with</strong> the<br />
results <strong>of</strong> MIGRATE-N (Figs. 2-4, 2-5 and Table 2-7). For example, migration<br />
rates between East Atlantic and Indian Oceanic region and also between East<br />
52
Pacific and West Atlantic region was definitely low among populations<br />
comparing to the populations at three other regional groups (Fig. 2-7). These<br />
results are concordant <strong>with</strong> MIGRATE-N results and reveal that observed gene<br />
flow <strong>with</strong>in East and West Atlantic, Indo-West Pacific and also between West<br />
and East Pacific is likely result <strong>of</strong> recent gene flow than retention <strong>of</strong> ancestral<br />
polymorphism.<br />
53
2-4 Discussion<br />
Gene flow in Indo-Pacific Ocean through Long Distance Seed Dispersal<br />
Geographical variation <strong>of</strong> cpDNA haplotypes is expected to indicate gene flow<br />
through seed dispersal as chloroplast genome is maternally inherited<br />
(Mogensen, 1996). When seed-mediated gene flow frequently occurs among<br />
populations, distribution <strong>of</strong> cpDNA haplotypes will be homogeneous in spatial<br />
scale. Population genetic analyses (Fig. 2-2, Tables 2-4 and 2-5) show high<br />
levels <strong>of</strong> gene flow and low levels <strong>of</strong> population structure both <strong>with</strong>in and<br />
between populations <strong>of</strong> C. ro<strong>sea</strong> across Pacific and Indian Oceanic regions. The<br />
major haplotype <strong>of</strong> C. ro<strong>sea</strong> (H8) has an extremely wide distribution range from<br />
South Africa in the West Indian Ocean to Panama in the East Pacific Ocean (Fig.<br />
2-2). Results <strong>of</strong> Fst, MIGRATE-N and MDIV also show low genetic<br />
differentiation among Indian and West Pacific Oceanic regions (F ST = 0.19) and<br />
high number <strong>of</strong> migrants (Nm > 5 per generation, Table 2-7), respectively.<br />
Rates <strong>of</strong> gene flow between West and East Pacific regions (F ST = 0.16; Nm ≅ 1)<br />
were lower than that <strong>of</strong> between Indian and West Pacific which may due to<br />
very long distance between populations in the Pacific Ocean. According to the<br />
theoretical thoughts such amount <strong>of</strong> migrants is enough to keep the unity <strong>of</strong><br />
species in such long distances (>25000 kilometers).<br />
If we consider the results <strong>of</strong> SAMOVA, the populations in the Atlantic<br />
region are differentiated from Indo-Pacific regions (table 2-6). In the number <strong>of</strong><br />
K=3 (Table 2-6), populations <strong>of</strong> most <strong>of</strong> Atlantic and one population from<br />
Indian Ocean (Java) is grouped in two groups and rest <strong>of</strong> populations from<br />
Indo-Pacific regions are making an integrate group. The result <strong>of</strong> coalescent<br />
methods from MIGRATE-N and MDIV programs are also coherent <strong>with</strong><br />
54
SAMOVA results, as significant differentiation between Indo-Pacific oceanic<br />
regions was not detected. Hence, long distance dispersal <strong>of</strong> <strong>drifted</strong> seeds by<br />
oceanic currents appears to be the most probable explanation for the present<br />
distribution patterns <strong>of</strong> C. ro<strong>sea</strong> haplotypes <strong>with</strong>in Indo-Pacific oceanic. Overall,<br />
these results suggest that substantial gene flow occurs among populations <strong>of</strong><br />
Indo-Pacific oceanic regions by <strong>sea</strong>-<strong>drifted</strong> seeds which are impermeable in<br />
water for years (Guppy, 1906; Thiel & Gutow, 2005).<br />
Although overall haplotype diversity and population differentiation is<br />
very low between the West and East Pacific Oceanic region, however migration<br />
rates between these oceanic regions is low comparing to the other regions like<br />
between Indian and West Pacific region (Fig. 2-6, Table 2-7). A possible<br />
explanation to this outcome can be presence <strong>of</strong> very long distance between<br />
West and East Pacific populations which makes difficult dispersal <strong>of</strong> seeds by<br />
oceanic currents (Figs., 2-2, 2-6 and Table 2-7). Another interpretation can be<br />
the role <strong>of</strong> the East Pacific barrier in this region as similar results have seen in<br />
another PPSS, Ipomea pes-caprae (Wakita, unpublished) and Hibiscus tiliaceus<br />
(Takayama et al., 2006). Thus, land masses such as African and American<br />
continents not only could be barriers to the seed dispersal for C. ro<strong>sea</strong> and also<br />
other PPSS but also Ocean currents itself are as intrinsic barriers to seed<br />
dispersal which naturally are main barrier to the terrestrial <strong>plant</strong>s (Murray, 1986;<br />
Sauer, 1988; Cox & Moore, 2005; Thiel & Haye, 2006).<br />
55
A strong genetic difference between the Indo-Pacific and Atlantic populations <strong>of</strong><br />
C. ro<strong>sea</strong><br />
The results <strong>of</strong> phylogenetic (chapter 1) and population genetic analyses<br />
clearly exhibit genetic structure in the populations <strong>of</strong> Atlantic region even very<br />
limited gene flow have occurred between the Atlantic and Indian Oceanic<br />
region (H6 shared between Brazil and Tanzania populations, Figs. 2-1 and 2-2).<br />
Pairwise F ST analysis revealed presence <strong>of</strong> genetic differentiation between the<br />
West Atlantic and East Pacific region (F ST = 0.45) and between the East Atlantic<br />
and Indian Oceanic region (F ST = 0.36). Results <strong>of</strong> migration analyses also unveil<br />
that migration to the in and out <strong>of</strong> Atlantic region is restricted except some<br />
migrants from East Atlantic to the Indian Ocean (Nm=1.6; see Table 2-7). These<br />
results confirm that African and American land masses are geographical<br />
barriers to gene flow through seed dispersal by oceanic currents among C.<br />
ro<strong>sea</strong> populations, as observed in another PPSS Hibiscus tiliaceus (Takayama et<br />
al., 2006) and Ipomea pes-caprae (N. Wakita, unpublished) and also in<br />
mangrove species (Dodd et al., 2002; Duke et al., 2002; Nettel & Dodd, 2007).<br />
Inference <strong>of</strong> patterns <strong>of</strong> current or historical gene flow from gene<br />
genealogies seems straightforward when there is a sharp geographic boundary<br />
between two widely distributed clades (Irwin & Gibbs, 2002). Usually,<br />
re<strong>sea</strong>rchers assume that such boundary is the result <strong>of</strong> geographic barriers to<br />
dispersal or cryptic species boundaries. The haplotypes H16-18 are specific to<br />
Atlantic region <strong>with</strong> high probability support and Long Branch length (Fig. 2-1).<br />
Although possibility <strong>of</strong> cryptic species cannot be completely rejected and the<br />
populations in the African Oceanic regions are not kind <strong>of</strong> allopatric<br />
populations, I considered that long-term geographic barrier to dispersal is<br />
56
esponsible to such kind <strong>of</strong> phylogeographic break in the Atlantic Ocean (Fig.<br />
2-2).<br />
Directional gene flow <strong>with</strong>in Atlantic region was suggested by MIGRATE-<br />
N; as migration rates from the East to the West Atlantic were two times larger<br />
than vice versa (M EA to WA = 395.65; M WA to EA = 166.42). These results might<br />
correspond to the variation <strong>of</strong> the strength <strong>of</strong> tropical Atlantic’s major currents<br />
which regarded as transatlantic dispersal in Atlantic region (Renner, 2004).<br />
Chloroplast DNA sequences detected highly differentiated populations <strong>of</strong> C.<br />
ro<strong>sea</strong> in southern Brazil (H6, Fig. 2-2). Although there are no known barriers,<br />
the bifurcating status <strong>of</strong> the South Equatorial Current at the north-eastern horn<br />
<strong>of</strong> Brazil to the northward and southward (Fratantoni et al., 2000; Renner, 2004),<br />
appears to be potential barrier to gene flow. These opposite ocean current<br />
directions may promote the genetic differentiation <strong>of</strong> the C. ro<strong>sea</strong> populations<br />
in southern Brazil which is also the case in H. pernambucensis populations<br />
(Takayama et al., 2008).<br />
Overall, same haplotypes are distributed in the all range <strong>of</strong> Indo-Pacific<br />
regions and also over Africa (Fig. 2-2). Similar results also were found in other<br />
PPSS such as Hibiscus tiliaceus and H. pernambucensis (Takayama et al., 2006;<br />
Takayama et al., 2008) and Ipomea pes-caprae (N. Wakita, unpublished). The<br />
results suggested that this kind <strong>of</strong> haplotype distribution patterns was occurred<br />
due to long distance dispersal <strong>of</strong> <strong>sea</strong>-<strong>drifted</strong> seeds which keep the unity <strong>of</strong><br />
these species over such a long distances. However, additional data using<br />
molecular markers is necessary to assess the possibility <strong>of</strong> cryptic species in the<br />
Atlantic region for C. ro<strong>sea</strong> populations and also verify presence <strong>of</strong> the gene<br />
57
flow over Isthmus <strong>of</strong> Panama which was restricted by <strong>sea</strong>-<strong>drifted</strong> seed dispersal<br />
according to the cpDNA sequence results.<br />
58
2-5 Conclusion<br />
Chloroplast DNA sequence revealed that frequent gene flow through longdistance<br />
seed dispersal occurs over the Pacific and Indian Oceanic regions and<br />
also <strong>with</strong>in Atlantic region. Chloroplast DNA sequence also revealed partial<br />
gene flow has detected between Atlantic and Indian oceanic regions which<br />
suggest that the unity <strong>of</strong> the species in global scale is kept by long distance<br />
seed dispersal by ocean currents. The results detected highly differentiated<br />
populations <strong>of</strong> C. ro<strong>sea</strong> overall Atlantic region. This suggests that African and<br />
American land masses played as geographical barriers to gene flow by <strong>sea</strong>dispersal.<br />
Gene flow across the extremely wide distribution range <strong>of</strong> C. ro<strong>sea</strong> was<br />
kept by long distance seed dispersal through oceanic currents. In terms <strong>of</strong> long<br />
distance dispersal, this scale <strong>of</strong> gene flow from such widely distributed range <strong>of</strong><br />
<strong>plant</strong> species is a new and unique case. And it shows the significance <strong>of</strong> long<br />
distance seed dispersal to keep species integration in worldwide distributed<br />
populations.<br />
Although <strong>sea</strong> currents enable gene flow over the global distribution<br />
range <strong>of</strong> <strong>plant</strong>s <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds, our study detected highly differentiated<br />
populations in southern Brazil which might be the result <strong>of</strong> bidirectional<br />
current <strong>of</strong> South Equatorial Current. Finally, the results provide good evidence<br />
for transatlantic long-distance seed dispersal by <strong>sea</strong> currents in Atlantic region.<br />
Seed dispersal prevented in the Isthmus <strong>of</strong> Panama and caused a distinct<br />
genetic difference in the cpDNA haplotype distribution between the Pacific and<br />
Atlantic populations <strong>of</strong> C. ro<strong>sea</strong>.<br />
59
Taxon Oceanic Region Locality N.<br />
C. ro<strong>sea</strong> (Sw.) DC. H1 H2 H3 H4 H5 H6 H7 H8 H9 H10 H11 H12 H13 H14 H15 H16 H17<br />
Indian Ocean South Africa Umdloti ‐29.67 31.12 22 8 14<br />
Tanzania Dar es salaam ‐6.82 39.32 25 4 21<br />
Sri Lanka Wattala, Negambo 6.97 79.89 11 10 1<br />
Thailand Phuket, Kmala Beach 7.99 98.29 10 10<br />
Indonesia Bali ‐1.08 100.42 3 3<br />
Java ‐8.73 115.17 10 10<br />
Sumatra ‐2.91 104.71 10 10<br />
Australia Darwin ‐12.44 130.83 10 10<br />
Headland Harbour ‐20.31 118.58 10 10<br />
West Pacific Thailand Kho Samui 9.51 100.06 9 9<br />
Taiwan Houpihu 38.99 117.56 15 15<br />
Singapore Singapore 1.35 103.99 9 9<br />
Philippine Quezon, Luzon 16.44 120.33 10 10<br />
Australia Queensland ‐16.73 145.66 10 8 2<br />
Japan Iriomote 24.40 123.76 15 15<br />
New Caledonia Plage de poe ‐21.61 165.39 10 10<br />
Fiji Korotogo ‐18.17 177.54 8 8<br />
Tonga Sopu ‐21.13 ‐175.21 10 10<br />
Samoa Samoa ‐13.86 ‐171.71 10 10<br />
Marquises Taipivai, Nuku Hiva ‐8.93 ‐140.09 10 10<br />
East Pacific Mexico Nayarit 21.58 ‐105.28 10 5 5<br />
Sinaloa 25.44 ‐108.73 4 4<br />
Oaxaca 15.94 ‐97.42 10 10<br />
Costa Rica Jaco Beach 9.61 ‐84.63 11 11<br />
Panama Veracruz 8.89 ‐79.62 10 10<br />
Ecuador Isla Jambel 0.74 ‐79.20 10 10<br />
West Atlantic Mexico Coatzcoalcos 18.14 ‐94.41 10 2 8<br />
Costa Rica Puerto Viejo 10.75 ‐83.56 5 5<br />
Panama Pina, Colon 1 9.28 ‐80.05 10 7 2 1<br />
Cuango, Colon 2 9.55 -79.31 10 6 4<br />
Brazil Para ‐1.32 ‐46.40 11 7 4<br />
Pernanbuco ‐8.34 ‐34.95 10 10<br />
Rio De Janeiro 1, Arraial do Cabo ‐22.97 ‐42.03 10 10<br />
Rio De Janeiro 2, Recreio ‐23.02 ‐43.44 9 1 8<br />
East Atlantic Senegal Joal-Fadiout 14.17 ‐16.85 31 7 3 4 17<br />
Ghana Busua beach 4.96 ‐1.73 18 5 10 3<br />
Angola Musul, Luanda ‐8.95 13.06 30 30<br />
Subtotal 436 7 0 9 9 10 32 45 232 5 10 14 1 2 4 2 25 29<br />
C. cathartica Thouars Pacific Philippine Atimona 10 10<br />
Samoa Samoa 2 2<br />
Tonga Tonga 5 5<br />
Tahiti Tahiti 1 1<br />
Hawaii Kauai 7 7<br />
Subtotal 25 6 19<br />
C. lineata (Thunb.) DC. Pacific Taiwan Maopi Tao 11 11<br />
Japan Ishigaki 11 11<br />
Miyazaki 10 10<br />
Ogasawara 10 10<br />
Subtotal 42 42<br />
C. sericea A. Gray Pacific Tonga Haashini-Lavengatonga 10 10<br />
Hawaii Maui, Bishop Museum 2 2<br />
Subtotal 12 12<br />
Table 2‐1. Chloroplast DNA haplotype composition and coordinates <strong>of</strong> populations for<br />
our study group. Haplotypes ranged from H1 to H17 and N, number <strong>of</strong> samples<br />
in each population.<br />
60
Primer name Length (bp) Primer Pairs Sequence (5'- 3') Source<br />
atpB partial 590 atpB-146 TTGGTACCATCCAACCAATTC This study<br />
ndhD partial 396 ndhD ACATCCGTCCCAAGGTATCA This study<br />
ndhE CAACTCGTATCAACCAATCGAA This study<br />
psbA 250 psbA CGAAGCTCCATCTACAAATGG Hamilton 1998<br />
rps16 partial 186 rps16-610 CCTTTGAGTTATCGGGTTGC This study<br />
trnK 5' flanking 250 trnK5' F GAATGGAAAAAGTAGCATGTCG This study<br />
trnK5' R TGCGATACGATCAAAACAGG This study<br />
trnK 3' flanking 340 trnK3' F AAAGGTCGGATTTGGTATTTAGA This study<br />
trnK3' R TCCTGAATCCCAACTCTTATTACAT This study<br />
Table 2‐2. List <strong>of</strong> primers used for sequencing <strong>of</strong> chloroplast regions in population<br />
samples. PCR amplification primers are shown in table 1‐2.<br />
61
Taxon<br />
Population's<br />
haplotypes Haplotype frequency atp B‐rbc L ndh D‐ndh E psb A‐trn H rps 16 trn K 5' trnK 3'<br />
256 510 267 644 23 155 183 308 682 733 748 155 156 2211 2290<br />
C. ro<strong>sea</strong> C1 7 C G G C 0 A T 2= 0 T T T C G A<br />
C. catharca, C. sericea C2 18 T . . . . . . 2= 0 C . . . T .<br />
C. ro<strong>sea</strong> C3 9 T . . . . . . 2= 0 . C . . . .<br />
C. ro<strong>sea</strong> C4 9 T . A . . . . 2= 0 . . . A . .<br />
C. ro<strong>sea</strong> C5 10 T . . . . . . 2= 0 . . G A T T<br />
C. ro<strong>sea</strong> C6 32 T . . . . . . 2= 0 . . . A T T<br />
C. ro<strong>sea</strong> C7 45 T . . . . . . 2= 0 . . . . . .<br />
C. ro<strong>sea</strong>, C. lineata, C. catharca C8 293 T . . . . . . 2= 0 . . . . T .<br />
C. ro<strong>sea</strong> C9 5 T . . T . . . 2= 0 . . . . . .<br />
C. ro<strong>sea</strong> C10 10 T . . . . T . 2= 0 . . . . T .<br />
C. ro<strong>sea</strong> C11 14 T . . . 1$ . . 2= 0 . . . . T .<br />
C. ro<strong>sea</strong> C12 1 T . . . . . . 2+ 0 . C . . . .<br />
C. ro<strong>sea</strong> C13 2 T . . . . . . 2+ 0 . . . . T .<br />
C. ro<strong>sea</strong> C14 4 T . . . . . G 2+ 0 . . . . . .<br />
C. ro<strong>sea</strong> C15 2 T . . . . . G 2= 0 . C . . . .<br />
C. ro<strong>sea</strong> C16 25 T T . . . . G 2= 0 . . . . . .<br />
C. ro<strong>sea</strong> C17 29 T T . . . . G 2= 1# . . . . . .<br />
$ AAAAT; = AGA; + TCT; # TTATT<br />
Table 2‐3. Variable sites <strong>of</strong> short fragments <strong>of</strong> 6 cpDNA regions used to determine<br />
haplotypes in Canavalia ro<strong>sea</strong> and its related species populations. Dots (•)<br />
indicate that character states are same as for C. ro<strong>sea</strong> haplotype C1. Numbers<br />
(0, 1 and 2) in sequences indicate indels, <strong>with</strong> ‘0’ indicating absence, ‘1’<br />
presence and ‘2’ inversion.<br />
62
Regions N (h) (S) (Hd) (π)<br />
West Atlantic 75 7 8 0.7809 0.0014<br />
East Atlantic 79 6 6 0.74034 0.00087<br />
Indian Ocean 111 6 8 0.5507 0.00053<br />
West Pacific 116 2 1 0.03418 0.00002<br />
East Pacific 55 2 3 0.27879 0.00042<br />
Total 436 16* 14 0.69124 0.00086<br />
*, number <strong>of</strong> haplotypes shared between C. ro<strong>sea</strong> populations<br />
Table 2‐4. Number <strong>of</strong> haplotypes (h), Polymorphic sites (S), Haplotype diversity (Hd),<br />
Nucleotide diversity (π).<br />
63
IN WP EP WA EA<br />
IN 0 0.1967 0.0826 0.3331 0.3605<br />
WP 0.1967 0 0.1684 0.6454 0.6577<br />
EP 0.0826 0.1684 0 0.4518 0.47<br />
WA 0.3331 0.6454 0.4518 0 0.1309<br />
EA 0.3605 0.6577 0.47 0.1309 0<br />
Table 2‐5. Pairwise FST comparison between 5 geographic regions. All differentiations<br />
are significant using an exact test (P < 0.05). (WA: West Atlantic, EA: East<br />
Atlantic, In: Indian Ocean, WP: West Pacific, EP: East Pacific).<br />
64
Grouping<br />
K FCT (P < 0.05)<br />
1 2 3 4 5 6 7 8 9 10<br />
Ghana (A)<br />
Mexico (A)<br />
2 0.57801 Panama-A2(A) Rests<br />
Para (A)<br />
Senegal (A)<br />
3 0.67019<br />
Ghana (A)<br />
Mexico (A)<br />
Panama-A2<br />
Para<br />
Senegal (A)<br />
4 0.68682 Mexico-Sin (P)<br />
5 0.71847 Java (I)<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Java (I)<br />
6 0.73819 Mexico-Nay Mexico-Sin Java (I)<br />
Ghana (A)<br />
Mexico (A)<br />
Panama-A1<br />
Panama-A2<br />
Para Senegal (A)<br />
Ghana (A)<br />
Mexico(A)<br />
Para Senegal (A)<br />
Panama-A2<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Java (I)<br />
Angola (A)<br />
Costa-A<br />
Panama-A1<br />
7 0.75362 Darwin (I) Mexico-Nay Mexico-Sin Java (I)<br />
Mexico-Sin<br />
Ghana (A) Mexico(A)<br />
Para Senegal (A)<br />
Panama-A2<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Angola (A)<br />
Costa-A<br />
Panama-A1<br />
8 0.76387 Panama-A2 Darwin (I) Mexico-Nay Mexico-Sin Java (I)<br />
Ghana (A) Mexico(A)<br />
Para Senegal (A)<br />
Panama-A2<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Angola (A) Costa-A<br />
Panama-A1<br />
Ghana (A) Mexico(A)<br />
Para Senegal (A)<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro3<br />
Angola (A) Costa-A<br />
Panama-A1<br />
9 0.76322 Angola (A) Panama-A2 Darwin (I) Mexico-Nay Mexico-Sin Java (I) Costa-A Panama-A1<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro3<br />
Ghana (A) Mexico(A)<br />
Para<br />
Senegal (A)<br />
10 0.77158 South Africa (A) Angola (A) Senegal (A) Panama-A2 Darwin (I) Mexico-Nay Mexico-Sin Java (I) Costa-A Panama-A1<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Ghana (A)<br />
Mexico(A)<br />
Para<br />
Rests<br />
Pernanbuco<br />
RDJaneiro1<br />
RDJaneiro2<br />
Rests<br />
Table 2‐6. Fixation indices (FCT) <strong>of</strong> C. ro<strong>sea</strong> population groupings obtained from SAMOVA (Dupanloup et<br />
al., 2002) as a function <strong>of</strong> the user‐defined number K <strong>of</strong> groups <strong>of</strong> populations. Bold populations in<br />
the grouping indicate the newly separated populations at a given level <strong>of</strong> K.<br />
65
0.05 MLE 0.95 Nm<br />
θWA 0.0133 0.0163 0.0202<br />
θEA 0.0122 0.0144 0.0171<br />
θIn 0.0131 0.0154 0.0184<br />
θWP 0.006 0.0069 0.0081<br />
θEP 0.0071 0.009 0.0119<br />
MEA to WA 302.43 395.65 506.36 6.4491<br />
MEP to WA 1.11E‐07 1.27E‐07 13.0875 0<br />
MWA to EA 119.79 166.42 223.96 2.3964<br />
M In to EA 1.75E‐08 1.99E‐08 8.0529 0<br />
MEA to In 52.7402 105.53 185.43 1.6252<br />
MWP to In 195.14 296.22 422.56 4.5618<br />
MIn to WP 82.1782 146.84 238.55 1.0132<br />
MEP to WP 14.2155 16.2463 58.7398 0.1121<br />
MWP to EP 41.8149 96.8064 186.78 0.8713<br />
MWA to EP 8.31E‐14 9.36E‐14 26.2257 0<br />
Table 2‐7. Maximum likelihood estimates (MLE) and 95% confidence interval <strong>of</strong> θ and<br />
migration rates (M) and number <strong>of</strong> migrants (Nm) obtained from MIGRATE‐N<br />
for 5 regional groups (WA: West Atlantic, EA: East Atlantic, In: Indian Ocean,<br />
WP: West Pacific, EP: East Pacific).<br />
66
Figure 2‐1. Statistical parsimony networks <strong>of</strong> 21 haplotypes (H1‐21) based on full<br />
length cpDNA sequences among C. ro<strong>sea</strong> and its allied species. Symbols, colors<br />
and size <strong>of</strong> each haplotype correspond to species, haplotypes could detect by<br />
partial sequence <strong>of</strong> 6 short fragments and frequencies <strong>of</strong> the corresponding<br />
haplotypes, respectively. The small white circles indicate the undetected<br />
intermediate haplotypes.<br />
67
Figure 2‐2. Distribution map <strong>of</strong> the cpDNA haplotypes identified by partial sequence<br />
(2012 bp) for 48 populations from five oceanic regional groups <strong>of</strong> C. ro<strong>sea</strong>. Pie<br />
charts represent the proportion <strong>of</strong> haplotypes in each locality and the size <strong>of</strong><br />
pie charts is proportional to sample size. Haplotypes H1‐21 corresponds to the<br />
figure 2‐1.<br />
68
1<br />
0.9<br />
0.8<br />
0.7<br />
0.6<br />
0.5<br />
0.4<br />
0.3<br />
0.2<br />
0.1<br />
0<br />
FST<br />
F<br />
FSC<br />
0 2 4 6 8 10 12<br />
Figure 2‐3. Fixation indices F obtained <strong>with</strong> the SAMOVA program (Dupanloup et al.<br />
2002) as a function <strong>of</strong> the user‐defined number K <strong>of</strong> groups <strong>of</strong> populations. F ST ,<br />
differentiation among populations; F CT , differentiation among groups <strong>of</strong><br />
populations; F SC , differentiation among populations <strong>with</strong>in groups. . All<br />
differentiations were significant (P < 0.01).<br />
69
Figure 2‐4. Posterior density distribution <strong>of</strong> Bayesian analysis from MIGRATE‐N for<br />
mutation rates (θ). Number 1‐5 corresponds to West Atlantic, East Atlantic,<br />
Indian Ocean, West Pacific and East Pacific regions.<br />
70
Figure 2‐5. Posterior density distribution <strong>of</strong> Bayesian analysis obtained from<br />
MIGRATE‐N for migration rates (M) <strong>with</strong>in C. ro<strong>sea</strong> populations.<br />
71
12<br />
Number <strong>of</strong> Migrants (Nm)<br />
10<br />
8<br />
6<br />
4<br />
2<br />
0<br />
Figure 2‐6. Estimated number <strong>of</strong> migrants (Nm) <strong>with</strong>in different Oceanic regions<br />
obtained from Bayesian method implemented in MIGRATE‐N program.<br />
Calculation was based on 95% credible interval <strong>of</strong> θ and M values.<br />
72
Figure 2‐7. The theta and migration rates (M) posterior probability<br />
distributions between five oceanic groups <strong>of</strong> C. ro<strong>sea</strong> populations using MDIV<br />
program (Nielsen & Wakeley, 2001). Legends are as follows: WA=West Atlantic,<br />
EA=East Atlantic, IN=Indian Ocean, WP= West Pacific and EP= East Pacific.<br />
73
GENERAL DISCUSSION<br />
In this study, I reported the results <strong>of</strong> phylogenetic analyses among Canavalia<br />
ro<strong>sea</strong>, a genuine member PPSS and its related species based on cpDNA and<br />
nrDNA ITS sequences and also the result <strong>of</strong> phylogeographic analyses from a<br />
large survey <strong>of</strong> cpDNA variations among populations <strong>of</strong> C. ro<strong>sea</strong>.<br />
This phylogeographic study <strong>of</strong> a genuine PPSS, suggested several<br />
interesting findings on a single species that keeps its distribution range by long<br />
distance seed dispersal by <strong>sea</strong>-<strong>drifted</strong> seeds. Comparing my results <strong>with</strong> the<br />
studies <strong>of</strong> sub PPSS, H. tiliaceus and its allies, will give us a comprehensive idea<br />
about the evolutionary history <strong>of</strong> PPSS.<br />
I. Closely related species are speciated in the wide distribution range<br />
<strong>of</strong> PPSS. Although we did not have strong evidence <strong>of</strong> speciation<br />
in Canavalia ro<strong>sea</strong>, the widest range <strong>of</strong> distribution and high<br />
haplotype diversity <strong>of</strong> this species may suggest that some species<br />
were speciated from C. ro<strong>sea</strong> as mother species. In the case <strong>of</strong> H.<br />
tiliaceus recurrent speciation from H. tiliaceus has given rise to all<br />
<strong>of</strong> its allied species.<br />
II.<br />
Substantial gene flow over wide range <strong>of</strong> distribution is common<br />
in both H. tiliaceus and C. ro<strong>sea</strong>, especially over Indo-Pacific region.<br />
III.<br />
In H. tiliaceus and H. pernambucensis, two species boundary are<br />
present: one is the East Pacific and the other is the Atlantic Ocean.<br />
It is interesting that both <strong>of</strong> them are oceanic barriers. In H.<br />
pernambucensis in addition, American continents are clear barrier<br />
74
to shape a clear geographic structure between Pacific and Atlantic<br />
regions. In C. ro<strong>sea</strong>, gene flow over East Pacific and Atlantic are<br />
observed. These would be caused by the difference <strong>of</strong> seed<br />
dispersibility between the two species group, which suggest that<br />
seed dispersibility is the key factor to be a genuine PPSS.<br />
IV.<br />
The land barriers <strong>of</strong> Africa and American Continents are common<br />
for the both PPSS species which support that <strong>sea</strong>-<strong>drifted</strong> seed<br />
dispersal is limited by land masses.<br />
V. The quite different point between the two studies was the genetic<br />
diversity among populations in Pacific and Atlantic regions.<br />
Haplotype diversity in the Pacific region for the H. tiliaceus was<br />
much higher than that for C. ro<strong>sea</strong>. On the other hand, in the<br />
Atlantic region haplotype diversity in C. ro<strong>sea</strong> populations was<br />
significantly higher than H. tiliaceus populations. Such interesting<br />
results show different evolutionary history <strong>of</strong> these species and<br />
require additional studies to clear up such fascinating patterns.<br />
75
REFERENCES<br />
Arroyo, M.T.K. (1981) Breeding systems and pollination biology in leguminosae. Advances in legume<br />
systematics (ed. by R.M.P.a.P.H. Raven), pp. 723–770. Royal Botanic Gardens, Kew, UK.<br />
Avise, J. (2000) <strong>Phylogeography</strong>: The history and formation <strong>of</strong> species. Harvard University Press.<br />
Avise, J. (2009) <strong>Phylogeography</strong>: Retrospect and prospect. Journal <strong>of</strong> Biogeography, 36, 3‐15<br />
Baldwin, B.G. & Wagner, W.L. (2010) Hawaiian angiosperm radiations <strong>of</strong> north american origin.<br />
Annals <strong>of</strong> Botany, 105, 849‐879<br />
Beerli, P. (2008) Migrate version 3.0: A maximum likelihood and bayesian estimator <strong>of</strong> gene flow<br />
using the coalescent. In: Distributed over the Internet at http://popgen.scs.edu/migrate.html<br />
Beerli, P. & Felsenstein, J. (1999) Maximum‐likelihood estimation <strong>of</strong> migration rates and effective<br />
population numbers in two populations using a coalescent approach. Genetics, 152, 763‐773<br />
Beerli, P. & Felsenstein, J. (2001) Maximum likelihood estimation <strong>of</strong> a migration matrix and effective<br />
population sizes in n subpopulations by using a coalescent approach. Proceedings <strong>of</strong> the<br />
National Academy <strong>of</strong> Sciences <strong>of</strong> the United States <strong>of</strong> America, 98, 4563‐4568<br />
Bohonak, A.J. (1999) Dispersal, gene flow, and population structure. The Quarterly Review <strong>of</strong> Biology,<br />
74, 21<br />
Bowie, R., Fjeldså, J., Hackett, S., Bates, J. & Crowe, T. (2006) Coalescent models reveal the relative<br />
roles <strong>of</strong> ancestral polymorphism, vicariance, and dispersal in shaping phylogeographical<br />
structure <strong>of</strong> an african montane forest robin. Molecular Phylogenetics and Evolution, 38, 171‐<br />
188<br />
Brito, P. & Edwards, S. (2009) Multilocus phylogeography and phylogenetics using sequence‐based<br />
markers. Genetica, 135, 439‐455<br />
Brito, P.H. (2005) The influence <strong>of</strong> pleistocene glacial refugia on tawny owl genetic diversity and<br />
phylogeography in western europe. Molecular Ecology, 14, 3077‐3094<br />
Bull, J.J., Huelsenbeck, J.P., Cunningham, C.W., Sw<strong>of</strong>ford, D.L. & Waddell, P.J. (1993) Partitioning and<br />
combining data in phylogenetic analysis. Systematic Biology, 42, 384‐397<br />
Cain, M., Damman, H. & Muir, A. (1998) Seed dispersal and the holocene migration <strong>of</strong> woodland<br />
herbs. Ecological Monographs, 68, 325‐347<br />
Cain, M.L., Milligan, B.G. & Strand, A.E. (2000) Long‐distance seed dispersal in <strong>plant</strong> populations.<br />
American Journal <strong>of</strong> Botany 87, 1217‐1227<br />
Calonje, M., Martín‐Bravo, S., Dobeš, C., Gong, W., Jordon‐Thaden, I., Kiefer, C., Kiefer, M., Paule, J.,<br />
Schmickl, R. & Koch, M. (2009) Non‐coding nuclear DNA markers in phylogenetic<br />
reconstruction. Plant Systematics and Evolution, 282, 257‐280<br />
Carbone, I., Liu, Y.‐C., Hillman, B.I. & Milgroom, M.G. (2004) Recombination and migration <strong>of</strong><br />
cryphonectria hypovirus 1 as inferred from gene genealogies and the coalescent. Genetics,<br />
166, 1611‐1629<br />
Carlquist, S. (1966) The biota <strong>of</strong> long‐distance dispersal. Iii. Loss <strong>of</strong> dispersibility in the hawaiian flora.<br />
Brittonia, 18, 310‐335<br />
Carlquist, S. (1974) Loss <strong>of</strong> dispersibility in island <strong>plant</strong>s. Island biology, pp. 429‐486. Columbia<br />
University Press, New York.<br />
Clement, M., Posada, D. & Crandall, K. (2000) Tcs: A computer program to estimate gene genealogies.<br />
Molecular Ecology, 9, 1657‐1659<br />
Corriveau, J.L. & Coleman, A.W. (1988) Rapid screening method to detect potential biparental<br />
inheritance <strong>of</strong> plastid DNA and results for over 200 angiosperm species. American Journal <strong>of</strong><br />
Botany, 75, 1443‐1458<br />
76
Cox, C. & Moore, P. (2005) Biogeography: An ecological and evolutionary approach (2005), Seventh<br />
edn. Blackwell Publishing Limited.<br />
Cronn, R.C., Small, R.L., Haselkorn, T. & Wendel, J.F. (2002) Rapid diversification <strong>of</strong> the cotton genus<br />
(gossypium: Malvaceae) revealed by analysis <strong>of</strong> sixteen nuclear and chloroplast genes.<br />
American Journal <strong>of</strong> Botany, 89, 707‐725<br />
Darwin, C. (1859) On the origin <strong>of</strong> species by means <strong>of</strong> natural selection, or the preservation <strong>of</strong><br />
favoured races in the struggle for life.<br />
De Queiroz, L., Fortunato, R. & Giulietti, A. (2003) Phylogeny <strong>of</strong> the diocleinae (papilionoideae:<br />
Phaseoleae) based on morphological characters. Advances in legume systematics, 10, 303–<br />
324<br />
Dodd, R.S., Afzal‐Rafii, Z., Kashani, N. & Budrick, J. (2002) Land barriers and open oceans: Effects on<br />
gene diversity and population structure in avicennia germinans l. (avicenniaceae). Molecular<br />
Ecology, 11, 1327‐1338<br />
Donnelly, M.J., Pinto, J., Girod, R., Besansky, N.J. & Lehmann, T. (2004) Revisiting the role <strong>of</strong><br />
introgression vs shared ancestral polymorphisms as key processes shaping genetic diversity in<br />
the recently separated sibling species <strong>of</strong> the anopheles gambiae complex. Heredity, 92, 61‐68<br />
Doyle, J. & Doyle, J. (1987) A rapid DNA isolation procedure for small quantities <strong>of</strong> fresh leaf tissue.<br />
Phytochemistry, 19, 11‐15<br />
Duke, N., Lo, E. & Sun, M. (2002) Global distribution and genetic discontinuities <strong>of</strong> mangrovesemerging<br />
patterns in the evolution <strong>of</strong> rhizophora. Trees‐Structure and Function, 16, 65‐79<br />
Dupanloup, I., Schneider, S. & Exc<strong>of</strong>fier, L. (2002) A simulated annealing approach to define the<br />
genetic structure <strong>of</strong> populations. Molecular Ecology, 11, 2571‐2581<br />
Ennos, R.A. (1994) Estimating the relative rates <strong>of</strong> pollen and seed migration among <strong>plant</strong><br />
populations. Heredity, 72, 250‐259<br />
Exc<strong>of</strong>fier, L. (2004) Patterns <strong>of</strong> DNA sequence diversity and genetic structure after a range expansion:<br />
Lessons from the infinite‐island model. Molecular Ecology, 13, 853‐864<br />
Exc<strong>of</strong>fier, L. & Heckel, G. (2006) Computer programs for population genetics data analysis: A survival<br />
guide. Nature Reviews Genetics, 7, 745‐758<br />
Exc<strong>of</strong>fier, L., Laval, G. & Schneider, S. (2005) Arlequin (version 3.0): An integrated s<strong>of</strong>tware package<br />
for population genetics data analysis. Evolutionary Bioinformatics Online, 1, 47–50<br />
Felsenstein, J. (1985) Confidence limits on phylogenies: An approach using the bootstrap. Evolution,<br />
39, 783‐791<br />
Fratantoni, D.M., Johns, W.E., Townsend, T.L. & Hurlburt, H.E. (2000) Low‐latitude circulation and<br />
mass transport pathways in a model <strong>of</strong> the tropical atlantic ocean. Journal <strong>of</strong> Physical<br />
Oceanography, 30, 1944‐1966<br />
Gross, C. (1993) The reproductive ecology <strong>of</strong> canavalia ro<strong>sea</strong> (fabaceae) on anak krakatau, indonesia.<br />
Australian Journal <strong>of</strong> Botany, 41, 591‐599<br />
Guppy, H.B. (1906) Observations <strong>of</strong> a naturalist in the pacific between 1896 and 1899 , vol. 2. Plant<br />
dispersal. MacMillan, London.<br />
Hamrick, J. & Nason, J. (1996) Consequences <strong>of</strong> dispersal in <strong>plant</strong>s. Population dynamics in ecological<br />
space and time, pp. 203–236. University <strong>of</strong> Chicago Press.<br />
Hasegawa, M., Kishino, H. & Yano, T. (1985) Dating <strong>of</strong> the human‐ape splitting by a molecular clock <strong>of</strong><br />
mitochondrial DNA. Journal <strong>of</strong> molecular evolution, 22, 160‐174<br />
Heuertz, M., Hausman, J., Hardy, O., Vendramin, G., Frascaria‐Lacoste, N. & Vekemans, X. (2004)<br />
Nuclear microsatellites reveal contrasting patterns <strong>of</strong> genetic structure between western and<br />
southeastern european populations <strong>of</strong> the common ash (fraxinus excelsior l.). Evolution, 58,<br />
976‐988<br />
77
Hey, J. (2005) On the number <strong>of</strong> new world founders: A population genetic portrait <strong>of</strong> the peopling <strong>of</strong><br />
the americas. PLoS Biology, 3, e193<br />
Heywood, J.S. (1991) Spatial analysis <strong>of</strong> genetic variation in <strong>plant</strong> populations. Annual Review <strong>of</strong><br />
Ecology and Systematics, 22, 335‐355<br />
Howe, H.F. & Smallwood, J. (1982) Ecology <strong>of</strong> seed dispersal. Annual Review <strong>of</strong> Ecology and<br />
Systematics, 13, 201‐228<br />
Ingvarsson, P.K., Ribstein, S. & Taylor, D.R. (2003) Molecular evolution <strong>of</strong> insertions and deletion in<br />
the chloroplast genome <strong>of</strong> silene. Molecular Biology and Evolution, 20, 1737‐1740<br />
Irwin, D.E. & Gibbs, H.L. (2002) Phylogeographic breaks <strong>with</strong>out geographic barriers to gene flow.<br />
Evolution, 56, 2383‐2394<br />
Kane, N., King, M., Barker, M., Raduski, A., Karrenberg, S., Yatabe, Y., Knapp, S. & Rieseberg, L. (2009)<br />
Comparative genomic and population genetic analyses indicate highly porous genomes and<br />
high levels <strong>of</strong> gene flow between divergent helianthus species. Evolution, 63, 2061‐2075<br />
Kay, K.M., Reeves, P.A., Olmstead, R.G. & Schemske, D.W. (2005) Rapid speciation and the evolution<br />
<strong>of</strong> hummingbird pollination in neotropical costus subgenus costus (costaceae): Evidence from<br />
nrdna its and ets sequences. American Journal <strong>of</strong> Botany, 92, 1899‐1910<br />
Kelchner, S.A. (2000) The evolution <strong>of</strong> non‐coding chloroplast DNA and its application in <strong>plant</strong><br />
systematics. Annals <strong>of</strong> the Missouri Botanical Garden, 87, 482‐498<br />
Kimura, M. (1980) A simple method for estimating evolutionary rates <strong>of</strong> base substitutions through<br />
comparative studies <strong>of</strong> nucleotide sequences. Journal <strong>of</strong> molecular evolution, 16, 111‐120<br />
Kimura, M. & Weiss, G. (1964) The stepping stone model <strong>of</strong> population structure and the decrease <strong>of</strong><br />
genetic correlation <strong>with</strong> distance. Genetics, 49, 561‐576<br />
Kingman, J. (1982a) The coalescent. Stochastic processes and their applications, 13, 235‐248<br />
Kingman, J. (1982b) On the genealogy <strong>of</strong> large populations. Journal <strong>of</strong> Applied Probability, 19, 27‐43<br />
Knowles, L.L. (2009) Statistical phylogeography. Annual Review <strong>of</strong> Ecology, Evolution, and Systematics,<br />
40, 593‐612<br />
Knowles, L.L. & Maddison, W.P. (2002) Statistical phylogeography. Molecular Ecology, 11, 2623‐2635<br />
Kuhner, M.K. (2009) Coalescent genealogy samplers: Windows into population history. Trends in<br />
Ecology & Evolution, 24, 86‐93<br />
Kuhner, M.K. & Smith, L.P. (2007) Comparing likelihood and bayesian coalescent estimation <strong>of</strong><br />
population parameters. Genetics, 175, 155‐165<br />
Lackey, J. (1981) Phaseoleae. Advances in legume systematics (ed. by R.P.a.P. Raven), pp. 301‐327.<br />
Royal Botanic Gardens, Kew, London.<br />
Levin, D.A. (2000) The origin, expansion and demise <strong>of</strong> <strong>plant</strong> species. Oxford University Press.<br />
Levin, D.A. (2001) The recurrent origin <strong>of</strong> <strong>plant</strong> races and species. Systematic Botany, 26, 197‐204<br />
Librado, P. & Rozas, J. (2009) Dnasp v5: A s<strong>of</strong>tware for comprehensive analysis <strong>of</strong> DNA polymorphism<br />
data. In: Bioinformatics, pp. 1451‐1452<br />
Linhart, Y.B. & Grant, M.C. (1996) Evolutionary significance <strong>of</strong> local genetic differentiation in <strong>plant</strong>s.<br />
Annual Review <strong>of</strong> Ecology and Systematics, 27, 237‐277<br />
Loewer, P. (2005) Seed dispersal. In: Seeds: The definitive guide to growing, history, and lore. Pp. 61‐<br />
74. Timber Press.<br />
Mayr, E. (1963) Animal species and evolution. Belknap Press.<br />
Mogensen, H.L. (1996) The hows and whys <strong>of</strong> cytoplasmic inheritance in seed <strong>plant</strong>s. American<br />
Journal <strong>of</strong> Botany, 83, 383‐404<br />
Morjan, C.L. & Rieseberg, L.H. (2004) How species evolve collectively: Implications <strong>of</strong> gene flow and<br />
selection for the spread <strong>of</strong> advantageous alleles. Molecular Ecology, 13, 1341‐1356<br />
78
Mort, M.E., Archibald, J.K., Randle, C.P., Levsen, N.D., O'leary, T.R., Topalov, K., Wiegand, C.M. &<br />
Crawford, D.J. (2007) Inferring phylogeny at low taxonomic levels: Utility <strong>of</strong> rapidly evolving<br />
cpdna and nuclear its loci. American Journal <strong>of</strong> Botany, 94, 173‐183<br />
Murray, D.R. (1986) Seed dispersal by water. Seed dispersal, pp. 49‐85. Academic Press, Sydney.<br />
Nakanishi, H. (1988) Dispersal ecology <strong>of</strong> the maritime <strong>plant</strong>s in the ryukyu islands, japan. Ecological<br />
Re<strong>sea</strong>rch, 3, 163‐173<br />
Nettel, A. & Dodd, R.S. (2007) Drifting propagules and receding swamps: Genetic footprints <strong>of</strong><br />
mangrove recolonization and dispersal along tropical coasts. Evolution, 61, 958‐971<br />
Nielsen, R. & Wakeley, J. (2001) Distinguishing migration from isolation: A markov chain monte carlo<br />
approach. Genetics, 158, 885‐896<br />
Nylander, J. (2004) Mrmodeltest v2. Program distributed by the author. In: Evolutionary Biology<br />
Centre, Uppsala University<br />
Olmstead, R. & Palmer, J. (1994) Chloroplast DNA systematics: A review <strong>of</strong> methods and data analysis.<br />
American Journal <strong>of</strong> Botany, 81, 1205‐1224<br />
Ouborg, N.J., Piquot Y. & Van Groenendael J. M. (1999) Population genetics, molecular markers and<br />
the study <strong>of</strong> dispersal in <strong>plant</strong>s. Journal <strong>of</strong> Ecology, 87, 551‐568<br />
Parker, P.G., Allison, A.S., Schug, M.D., Booton, G.C. & Fuerst, P.A. (1998) What molecules can tell us<br />
about populations: Choosing and using a molecular marker. Ecology, 79, 361‐382<br />
Petit, R., Duminil, J., Fineschi, S., Hampe, A., Salvini, D. & Vendramin, G. (2005) Comparative<br />
organization <strong>of</strong> chloroplast, mitochondrial and nuclear diversity in <strong>plant</strong> populations.<br />
Molecular Ecology, 14, 689‐701<br />
Polidoros, A., Pasentsis, K. & Tsaftaris, A. (2006) Rolling circle amplification‐race: A method for<br />
simultaneous isolation <strong>of</strong> 5'and 3'cdna ends from amplified cdna templates. BioTechniques,<br />
41, 35<br />
Rambaut, A. (2002) Se‐al: A manual sequence alignment editor v2.0a11.<br />
Rambaut, A. & Drummond, A. (2009) Tracer v1.5. Available<br />
from:. In:<br />
Rannala, B. & Hartigan, J.A. (1996) Estimating gene flow in island populations. Genetics Re<strong>sea</strong>rch, 67,<br />
147‐158<br />
Raymond, M. & Rousset, F. (1995) An exact test for population differentiation. Evolution, 49, 1280‐<br />
1283<br />
Renner, S. (2004) Plant dispersal across the tropical atlantic by wind and <strong>sea</strong> currents. International<br />
Journal <strong>of</strong> Plant Sciences, 165, S23‐S33<br />
Ronquist, F. & Huelsenbeck, J.P. (2003) Mrbayes 3: Bayesian phylogenetic inference under mixed<br />
models. Bioinformatics, 19, 1572‐1574<br />
Sauer, J. (1964) Revision <strong>of</strong> canavalia. Brittonia, 16, 106‐181<br />
Sauer, J. (1988) Plant migration: The dynamics <strong>of</strong> geographic patterning in seed <strong>plant</strong> species.<br />
University <strong>of</strong> California Press, Berkeley, California, USA.<br />
Schaal, B.A., Hayworth, D.A., Olsen, K.M., Rauscher, J.T. & Smith, W.A. (1998) Phylogeographic<br />
studies in <strong>plant</strong>s: Problems and prospects. Molecular Ecology, 7, 465‐474<br />
Scherson, R., Choi, H., Cook, D. & Sanderson, M. (2005) Phylogenetics <strong>of</strong> new world astragalus:<br />
Screening <strong>of</strong> novel nuclear loci for the reconstruction <strong>of</strong> phylogenies at low taxonomic levels.<br />
Brittonia, 57, 354‐366<br />
Schrire, B.D. (2005) Phaseoleae. Legumes <strong>of</strong> the world (ed. by B.S. Gwilym Lewis, Barbara Mackinder,<br />
and Mike Lock), pp. 393‐431. Kew Publishing.<br />
Shaw, J., Lickey, E.B., Schilling, E.E. & Small, R.L. (2007) Comparison <strong>of</strong> whole chloroplast genome<br />
sequences to choose noncoding regions for phylogenetic studies in angiosperms: The tortoise<br />
and the hare iii. American Journal <strong>of</strong> Botany, 94, 275‐288<br />
79
Simmons, M. & Ochoterena, H. (2000) Gaps as characters in sequence‐based phylogenetic analyses.<br />
Systematic Biology, 49, 369<br />
Slatkin, M. & Hudson, R. (1991) Pairwise comparisons <strong>of</strong> mitochondrial DNA sequences in stable and<br />
exponentially growing populations. Genetics, 129, 555<br />
Small, R.L., Ryburn, J.A., Cronn, R.C., Seelanan, T. & Wendel, J.F. (1998) The tortoise and the hare:<br />
Choosing between noncoding plastome and nuclear adh sequences for phylogeny<br />
reconstruction in a recently diverged <strong>plant</strong> group. American Journal <strong>of</strong> Botany, 85, 1301‐1315<br />
Soltis, D.E., Morris, A.B., Mclachlan, J.S., Manos, P.S. & Soltis, P.S. (2006) Comparative<br />
phylogeography <strong>of</strong> unglaciated eastern north america. Molecular Ecology, 15, 4261‐4293<br />
Soltis, D.E. & Soltis, P.S. (1998) Choosing an approach and appropriate gene for phylogenetic analysis.<br />
Molecular systematics <strong>of</strong> <strong>plant</strong>s ii. DNA sequencing (ed. by D.E. Soltis, P.S. Soltis and J.J.<br />
Doyle), pp. 1‐42. Kluwer Academic Publishers.<br />
St. John H (1970) Revision <strong>of</strong> the hawaiian species <strong>of</strong> canavalia (leguminosae). Hawaiian <strong>plant</strong> studies.<br />
Israel Journal <strong>of</strong> Botany, 19, 161‐219<br />
Stamatakis, A. (2006) Raxml‐vi‐hpc: Maximum likelihood‐based phylogenetic analyses <strong>with</strong> thousands<br />
<strong>of</strong> taxa and mixed models. Bioinformatics, 22, 2688‐2690<br />
Sw<strong>of</strong>ford, D. (2002) Paup* 4.0 beta 10: Phylogenetic analysis using parsimony (*and other methods).<br />
In. Sinauer Associates Sunderland, MA<br />
Takayama, K., Kajita, T., Murata, J. & Tateishi, Y. (2006) <strong>Phylogeography</strong> and genetic structure <strong>of</strong><br />
hibiscus tiliaceus‐ speciation <strong>of</strong> a <strong>pantropical</strong> <strong>plant</strong> <strong>with</strong> <strong>sea</strong>‐<strong>drifted</strong> seeds. Molecular Ecology,<br />
15, 2871‐2881<br />
Takayama, K., Tateishi, Y., Murata, J. & Kajita, T. (2008) Gene flow and population subdivision in a<br />
<strong>pantropical</strong> <strong>plant</strong> <strong>with</strong> <strong>sea</strong>‐<strong>drifted</strong> seeds hibiscus tiliaceus and its allied species: Evidence from<br />
microsatellite analyses. Molecular Ecology, 17, 2730‐2742<br />
Templeton, A., Crandall, K. & Sing, C. (1992) A cladistic analysis <strong>of</strong> phenotypic associations <strong>with</strong><br />
haplotypes inferred from restriction endonuclease mapping and DNA sequence data. Iii.<br />
Cladogram estimation. Genetics, 132, 619<br />
Thiel, M. & Gutow, L. (2005) The ecology <strong>of</strong> rafting in the marine environment: I. The floating<br />
substrata. Oceanography and Marine Biology: An Annual Review Volume 42, 42, 181‐264<br />
Thiel, M. & Haye, P.A. (2006) The ecology <strong>of</strong> rafting in the marine environment. Iii. Biogeographical<br />
and evolutionary consequences. Oceanography and marine biology: An annual review (ed. by<br />
R. Gibson, R. Atkinson and J. Gordon), pp. 323‐429. CRC Press.<br />
Varela, E.S., Lima, J.P.M.S., Galdino, A.S., Pinto, L.D.S., Bezerra, W.M., Nunes, E.P., Alves, M.a.O. &<br />
Grangeiro, T.B. (2004) Relationships in subtribe diocleinae (leguminosae; papilionoideae)<br />
inferred from internal transcribed spacer sequences from nuclear ribosomal DNA.<br />
Phytochemistry, 65, 59‐69<br />
Wagner, W., Herbst, D. & Sohmer, S. (1999) Manual <strong>of</strong> the flowering <strong>plant</strong>s <strong>of</strong> hawaii, revised edition.<br />
University <strong>of</strong> Hawaii Press.<br />
Wakeley, J. (2003) Inferences about the structure and history <strong>of</strong> populations: Coalescents and<br />
intraspecific phylogeography. The evolution <strong>of</strong> population biology (ed. by R. Singh and M.<br />
Uyenoyama), pp. 193–215. Cambridge University Press, Cambridge.<br />
Weir, B. & Cockerham, C. (1984) Estimating f‐statistics for the analysis <strong>of</strong> population structure.<br />
Evolution, 38, 1358‐1370<br />
Whistler, W. (1992) Flowers <strong>of</strong> the pacific island <strong>sea</strong>shore. Univ. <strong>of</strong> Hawaii Press.<br />
Wiens, J.J. (1998) Combining data sets <strong>with</strong> different phylogenetic histories. Systematic Biology, 47,<br />
568‐581<br />
Willson, M. & Traveset, A. (2000) The ecology <strong>of</strong> seed dispersal. Seeds the ecology <strong>of</strong> regeneration in<br />
<strong>plant</strong> communities 2nd edition (ed. by M. Fenner), pp. 85‐110. CAB International.<br />
80
Wright, S. (1931) Evolution in mendelian populations. Genetics, 16, 97‐159<br />
Wright, S. (1951) The genetical structure <strong>of</strong> populations. Annals <strong>of</strong> Eugenics, 15, 323‐354<br />
81
ACKNOWLEDGEMENTS<br />
I am deeply grateful to my supervisor, Pr<strong>of</strong>. Dr. Tadashi Kajita who<br />
encouraging me to do a good re<strong>sea</strong>rch, and challenge me to logical thinking.<br />
His efforts, support, and patience in accepting me as a PhD student, will never<br />
forget as my dream (study abroad) came true. I am also grateful to my cosupervisor,<br />
Pr<strong>of</strong>. Dr. Yasuyuki Watano who always remind me how to learn and<br />
Dr. Takeshi Asakawa for his valuable suggestions. I specially thank Pr<strong>of</strong>. Dr.<br />
Takayoshi Tsuchiya and Pr<strong>of</strong>. Dr. Sumiko Kimura for their suggestions and<br />
comments as referees. I also owe a great debt to Dr. Koji Takayama, who<br />
taught me molecular methods and for his valuable comments. I would like to<br />
thank Mr. Alvin Y. Yoshinaga from Center for Conservation Re<strong>sea</strong>rch and<br />
Training, Hawaii for sending materials. I would like to thank Pr<strong>of</strong>. Dr. Yoichi<br />
Tateishi for his helpful comments and allowing me to visit the herbarium <strong>of</strong><br />
University <strong>of</strong> the Ryukyus. I am also grateful to Pr<strong>of</strong>. Dr. Masaki Miya for<br />
valuable classes in phylogenetic analysis.<br />
I specially thank Dr. Akihisa Shirai, Dr. Norihisa Wakita, Dr. Bayu Adjie, for<br />
their help and suggestions. I would also like to thank to all students <strong>of</strong> Watano<br />
and Kajita laboratory for any helps during my re<strong>sea</strong>rches.<br />
And finally, thanks to my family and all friends for their love, support,<br />
and encouragement throughout the years.<br />
My study fully supported by Monbukagakusho (MEXT: Ministry <strong>of</strong><br />
Education, Culture, Sports, Science and Technology) scholarship.<br />
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BIOGRAPHY<br />
Mohammad Vatanparast was born in Urmia, central city <strong>of</strong> West Azerbaijan<br />
province in the North West <strong>of</strong> Iran in 20 February 1976. He finished his<br />
undergraduate level in <strong>plant</strong> biology from Urmia University in 1999. In 2000 he<br />
enter master course in the <strong>plant</strong> systematic field at Tarbiat Modarres University<br />
in Tehran and graduate in 2003. His master thesis was on biosystematics <strong>of</strong> the<br />
genus Trifolium a part <strong>of</strong> national project about Flora <strong>of</strong> Iran in Persian<br />
language. As his dreams and interest was study abroad to learn novel practical<br />
and analytical methods in the <strong>plant</strong> systematic and evolution, <strong>with</strong> efforts <strong>of</strong><br />
Pr<strong>of</strong>. Dr. Tadashi Kajita, he could enter to the PhD course in his laboratory in<br />
Chiba University, Japan. In October 2006 he entered Japan and after taking 6<br />
month re<strong>sea</strong>rch student course in April 2007 he started his PhD project<br />
focusing on “<strong>Phylogeography</strong> <strong>of</strong> a <strong>pantropical</strong> <strong>plant</strong>s <strong>with</strong> <strong>sea</strong>-<strong>drifted</strong> seeds,<br />
Canavalia ro<strong>sea</strong>” by applying large population sampling using molecular<br />
methods such as chloroplast DNA sequences and population genetic analyses.<br />
83