Highlights of the Didymellaceae - Studies in Mycology
Highlights of the Didymellaceae - Studies in Mycology
Highlights of the Didymellaceae - Studies in Mycology
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Group A – outgroup and basal l<strong>in</strong>eages:<br />
The tree presented <strong>in</strong> Fig. 2 is rooted to Ascochyta hordei and Ph.<br />
paspali, which proved to be ancestral to <strong>the</strong> <strong>Didymellaceae</strong> <strong>in</strong> Fig. 1.<br />
The latter species was described by Johnston (1981) as a species<br />
from grasses <strong>in</strong> New Zealand and Australia, but <strong>in</strong> recent years,<br />
isolates with similar genotypes were isolated from iron-rich volcanic<br />
soil from France (C. Gueidan, pers. comm.), and from common<br />
reed (Phragmites australis) <strong>in</strong> Germany (Wirsel et al. 2001). These<br />
isolates were, however, never studied morphologically.<br />
Ano<strong>the</strong>r species used as outgroup is Ascochyta hordei var.<br />
hordei (CBS 544.74), which was obta<strong>in</strong>ed from a South African<br />
Triticum aestivum, <strong>in</strong>dicat<strong>in</strong>g that also with<strong>in</strong> <strong>the</strong> <strong>Didymellaceae</strong>,<br />
species that are ascribed to Ascochyta do not form a monophyletic<br />
group. Also CBS 259.92, <strong>the</strong> isotype <strong>of</strong> Ph. matteuciicola, proved<br />
to be basal to most o<strong>the</strong>r Phoma species. Phoma matteuciicola is<br />
commonly known as a pathogen <strong>of</strong> many fern species (De Gruyter<br />
et al. 2002). With<strong>in</strong> <strong>the</strong> basal l<strong>in</strong>eages, also a group compris<strong>in</strong>g Ph.<br />
humicola and <strong>the</strong> novel species Ph. saxea is found, although this<br />
group is only supported by BI analysis (BPP = 0.92, RBS < 50 %).<br />
Although Phoma humicola is known as a saprobic soil fungus, it is<br />
sometimes mistaken for <strong>the</strong> notorious potato pathogen Ph. foveata<br />
(Group N), due to a similar biochemical reaction to NaOH and <strong>the</strong><br />
formation <strong>of</strong> citr<strong>in</strong>e green crystals on MEA (De Gruyter et al. 1998).<br />
However, conidia <strong>of</strong> Ph. humicola are always eguttulate <strong>in</strong> contrast<br />
to those <strong>of</strong> Ph. foveata. Phoma saxea has been found twice <strong>in</strong><br />
Germany on rock material, and will be fur<strong>the</strong>r described below.<br />
Phoma humicola J.C. Gilman & E.V. Abbott, Iowa St. Coll.<br />
J. Sci. 1(3): 266. 1927.<br />
Specimen exam<strong>in</strong>ed: U.S.A., Nevada, Death Valley, from a dead leaf <strong>of</strong> Franseria<br />
sp., 1971, G.H. Boerema, CBS H-16390, culture CBS 220.85.<br />
Phoma matteuciicola Aderkas, Gruyter, Noordel. &<br />
Strongman, Canad. J. Pl. Pathol. 14(3): 227. 1992.<br />
Specimen exam<strong>in</strong>ed: Canada, Nova Scotia, Five Mile River, from leaf base <strong>of</strong><br />
Matteuccia struthiopteris, May 1981, P. von Aderkas, holotype DAOM 183092,<br />
culture ex-holotype CBS 259.92 = IMI 286996 = PD 91/272.<br />
Notes: Gangrene <strong>in</strong> ostrich fern was orig<strong>in</strong>ally attributed to Ph.<br />
exigua var. foveata (von Aderkas & Brewer 1983), which is here<br />
recomb<strong>in</strong>ed as Boeremia foveata, but Von Aderkas et al. (1992)<br />
recognised a new species as causal agent <strong>of</strong> this disease. The<br />
phylogeny presented here supports <strong>the</strong>se observations, as Ph.<br />
matteuciicola is found ra<strong>the</strong>r dist<strong>in</strong>ct from B. foveata.<br />
Phoma paspali P.R. Johnst., New Zealand J. Bot. 19(2):<br />
181. 1981.<br />
Specimens exam<strong>in</strong>ed: New Zealand, Auckland, Kaikohe, from a dead leaf <strong>of</strong><br />
Paspalum dilatatum, Jan. 1979, P.K. Buchanan, isotype CBS H-7623, culture exisotype<br />
CBS 560.81 = PD 92/1569; Waikato District, Ruakura, from Lolium perenne,<br />
Jan. 1979, G.H. Boerema, CBS 561.81 = PDDCC 6615.<br />
Phoma saxea Aveskamp, Gruyter & Verkley, sp. nov.<br />
MycoBank MB515591. Fig. 3.<br />
Conidia dimorpha, <strong>in</strong>tra idem pycnidia formata. Conidia typus 1 (sub)globosa,<br />
glabra, hyal<strong>in</strong>a, cont<strong>in</strong>ua, (3–)3.5–5.5 μm diam., (0–)3–10(–15) guttulis praedita.<br />
Conidia typus 2 cyl<strong>in</strong>drica vel ellipsoidea, glabra, hyal<strong>in</strong>a, cont<strong>in</strong>ua, (3.5–)4.5–<br />
7(–7.5) × 2.5–3.5(–4) μm, plerumque eguttulata, vel 1–3 guttulis praedita. Matrix<br />
www.studies<strong>in</strong>mycology.org<br />
Phoma And relAted pleoSporAleAn generA<br />
conidiorum salmonea. Chlamydosporae cont<strong>in</strong>uae, globosae, viridulae, <strong>in</strong> catenas<br />
usque 35 positae, (8.5–)10–16.5(–17.5) × (6–)8–12.5(–14) μm.<br />
Etymology: Refers to <strong>the</strong> substratum on which both isolates <strong>of</strong> this<br />
species were found, stone material.<br />
Pycnidia solitary, (sub-)globose, glabrous or covered with hyphal<br />
outgrows, (90–)135–280(–310) × (90–)105–260(–275) μm. Ostioles<br />
s<strong>in</strong>gle, papillate, with wide open<strong>in</strong>gs, ca. 40–80 μm diam. Pycnidial<br />
wall pseudoparenchymatous, composed <strong>of</strong> oblong to isodiametric<br />
cells, 2–3 layers, 10–17 μm thick, outer cell layer brown pigmented.<br />
Conidiogenous cells phialidic, hyal<strong>in</strong>e, simple, smooth, variable <strong>in</strong><br />
appearance, flask-shaped, oblong or isodiametric ca. 5.5–7.5 × 3–4<br />
μm. Conidia <strong>of</strong> two types, both orig<strong>in</strong>at<strong>in</strong>g from <strong>the</strong> same pycnidia.<br />
Conidia <strong>of</strong> type 1: (sub-)globose, th<strong>in</strong>-walled, smooth, hyal<strong>in</strong>e,<br />
aseptate (3–)3.5–5.5 μm diam, with (0–)3–10(–15) guttules.<br />
Conidia <strong>of</strong> type 2: cyl<strong>in</strong>drical to ellipsoidal, th<strong>in</strong>-walled, smooth,<br />
hyal<strong>in</strong>e, aseptate, (3.5–)4.5–7(–7.5) × 2.5–3.5(–4) μm, ma<strong>in</strong>ly<br />
egutullate or with up to 3 m<strong>in</strong>ute guttules. Conidial matrix salmon.<br />
Chlamydospores ubiquitously present <strong>in</strong> <strong>the</strong> agar, unicellular,<br />
globose, <strong>in</strong> long cha<strong>in</strong>s <strong>of</strong> up to 35 elements, greenish pigmented,<br />
measur<strong>in</strong>g (8.5–)10–16.5(–17.5) × (6–)8–12.5(–14) μm.<br />
Culture characteristics: Colonies on OA, 45–50 mm diam after<br />
7 d, marg<strong>in</strong> regular. Immersed mycelium flat, olivaceous to<br />
greenish olivaceous, citr<strong>in</strong>e-green or coral near <strong>the</strong> colony marg<strong>in</strong>.<br />
Aerial mycelium absent, but sometimes some grey erect tufts<br />
are encountered near <strong>the</strong> colony centre; reverse concolourous.<br />
Colonies on MEA 20–25 mm diam after 7 d, marg<strong>in</strong> regular.<br />
Immersed mycelium violet-slate, but saffron near <strong>the</strong> colony marg<strong>in</strong>.<br />
Abundant pycnidia are present on <strong>the</strong> agar surface; reverse irongrey,<br />
saffron near <strong>the</strong> colony marg<strong>in</strong>. Colonies on CHA similar as on<br />
MEA, but somewhat slower grow<strong>in</strong>g, 10–15 mm diam. after 7 d, and<br />
some sparse white aerial mycelia hyphae are present <strong>in</strong> <strong>the</strong> colony.<br />
Application <strong>of</strong> NaOH results <strong>in</strong> a greenish yellow discolouration <strong>of</strong><br />
<strong>the</strong> agar, best to be observed on OA medium.<br />
Specimens exam<strong>in</strong>ed: Germany, Oldenburg, from corroded Mediterranean marble,<br />
June 1992, J. Kuroczk<strong>in</strong>, holotype designated here CBS H-20240, culture exholotype<br />
CBS 419.92; Oldenburg, from limestone, 1987, J. Kuroczk<strong>in</strong>, CBS 298.89.<br />
Notes: The pycnidial wall <strong>of</strong> Phoma saxea is extremely th<strong>in</strong> and<br />
almost hyal<strong>in</strong>e when <strong>the</strong> conidia have exuded. Older pycnidia<br />
collapse and rema<strong>in</strong> as a double-layered, disc-like structure on <strong>the</strong><br />
agar.<br />
Both stra<strong>in</strong>s <strong>of</strong> this species have been isolated from stone<br />
material, such as limestone (CBS 298.89) and corroded<br />
Mediterranean marble (CBS 419.92). Although <strong>the</strong> genus is<br />
known from all k<strong>in</strong>ds <strong>of</strong> substrates, <strong>the</strong> number <strong>of</strong> rock-<strong>in</strong>habit<strong>in</strong>g<br />
Phoma isolates is relatively low. Selbmann et al. (2002) report<br />
on Ph. herbarum from Antarctic rock, and Boerema et al. (2004)<br />
list several species from rock-like materials, such as cement (Ph.<br />
herbarum), wall-plaster (Ph. heteroderae – here recomb<strong>in</strong>ed <strong>in</strong>to<br />
Ph. calorpreferens) and crockery (Ph. pomorum). In addition,<br />
multiple species are recorded from rock-<strong>in</strong>habit<strong>in</strong>g lichens (Nelson<br />
et al. 2009, Ruibal et al. 2009). These species, listed by Hawksworth<br />
& Cole (2004) are, however, unculturable and could <strong>the</strong>refore not<br />
be compared with Ph. saxea <strong>in</strong> vitro. However, <strong>the</strong> morphological<br />
descriptions suggest that <strong>the</strong> mentioned species and Ph. saxea are<br />
different taxonomic entities.<br />
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