06.04.2013 Views

Middle Miocene palynoflora of the Legnica lignite deposit complex ...

Middle Miocene palynoflora of the Legnica lignite deposit complex ...

Middle Miocene palynoflora of the Legnica lignite deposit complex ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

32<br />

1974, Kohlman-Adamska 1993, Stuchlik et al.<br />

2009). They represent arctotertiary (A) element<br />

(Ziembińska-Tworzydło 1996).<br />

Today <strong>the</strong> family Polygonaceae contains<br />

about 30 genera and 750 species <strong>of</strong> herbaceous<br />

plants, rarely shrubs or trees, occurring<br />

all over <strong>the</strong> world, mainly in temperate zone<br />

<strong>of</strong> <strong>the</strong> nor<strong>the</strong>rn hemisphere. The genus Polygonum<br />

(about 150 species) contains mainly<br />

perennials, rarely climbers (Heywood 1978).<br />

P. densifl orum Meisn. and P. hydropiperoides<br />

Michaux occur e.g. in sawgrass marshes in<br />

Florida (Willard et al. 2004).<br />

(75) Rumex L. type<br />

Pl. 11, fi g. 5a–c<br />

1964 Rumex sp.; Stuchlik, p. 43, pl. 13, fi gs 9, 10.<br />

Pollen grains tri- and tetracolporate, round<br />

in shape, 20–28 μm in diameter. Colpi ra<strong>the</strong>r<br />

long, very narrow. Pores small, 1.5–2.0 μm<br />

in diameter, circular to slightly equatorially<br />

elongate. Exine 1.5 μm thick, surface microreticulate.<br />

R e m a r k s. Pollen grains <strong>of</strong> Rumex type are<br />

rarely found in <strong>the</strong> Tertiary <strong>deposit</strong>s. They are<br />

known from <strong>the</strong> Polish <strong>Miocene</strong> and Pliocene<br />

<strong>deposit</strong>s (Stuchlik 1964, Oszast 1967, 1973,<br />

Oszast & Stuchlik 1977, Jahn et al. 1984). Only<br />

3 specimens <strong>of</strong> this type were encountered in<br />

<strong>the</strong> analysed material.<br />

Today <strong>the</strong> genus Rumex (about 150 species)<br />

is distributed in nor<strong>the</strong>rn temperate zone<br />

(Heywood 1978).<br />

Ordo GARRYALES<br />

Familia EUCOMMIACEAE<br />

Eucommia Oliv.<br />

Eucommioipollis Ziembińska-Tworzydło in<br />

Ziembińska-Tworzydło et al. 1994<br />

(76) Eucommioipollis parmularius<br />

(Potonié 1934) Ziembińska-Tworzydło in<br />

Ziembińska-Tworzydło et al. 1994<br />

Pl. 11, fi g. 4<br />

1934 Pollenites parmularius n. sp., Potonié, p. 52,<br />

pl. 2, fi g. 7.<br />

1994b Eucommioipollis parmularius (Potonié) Ziembińska-Tworzydło<br />

comb. nov.; Ziembińska-<br />

Tworzydło et al., p. 24, pl. 13, fi g. 7a, b.<br />

R e m a r k s. These pollen grains represent<br />

warm-temperate element (A1). In Europe<br />

<strong>the</strong>y occur in <strong>the</strong> Lower Oligocene to Pliocene<br />

<strong>deposit</strong>s (Ziembińska-Tworzydło et al.<br />

1994a, b, Ziembińska-Tworzydło 1996). They<br />

were sporadically encountered in <strong>the</strong> studied<br />

material.<br />

In <strong>the</strong> recent days <strong>the</strong> monotypic genus<br />

Eucommia occurs in central China. E. ulmoides<br />

Oliv. is a tall tree which grows in mesophytic<br />

mountain forests (Wang 1961). The variability<br />

<strong>of</strong> fossil pollen grains, leaves, and fruits (Guo<br />

2000) indicates that <strong>the</strong>y could represent not<br />

<strong>the</strong> only one species.<br />

Ordo SAXIFRAGALES<br />

Familia CERCIDIPHYLLACEAE<br />

Cercidiphyllum Sieb. & Zucc.<br />

Cercidiphyllites Mtshedlishvili in<br />

Samoilovich & Mtshedlishvili 1961<br />

(77) Cercidiphyllites minimireticulatus<br />

(Trevisan 1967) Ziembińska-Tworzydło<br />

in Ziembińska-Tworzydło et al. 1994<br />

Pl. 11, fi gs 2, 3<br />

1967 Tricolpopollenites minimireticulatus n. fsp.,<br />

Trevisan, p. 38, pl. 24, fi gs 10–12.<br />

1994b Cercidiphyllites minimireticulatus (Trevisan)<br />

Ziembińska-Tworzydło comb. nov.; Ziembińska-<br />

Tworzydło et al., p. 21, pl. 13, fi gs 1a, b, 2.<br />

R e m a r k s. This species represents warmtemperate<br />

element (A1), and is known from<br />

<strong>the</strong> <strong>Middle</strong> and Upper <strong>Miocene</strong> (Ziembińska-<br />

Tworzydło et al. 1994a, b, Ziembińska-<br />

Tworzydło 1996) as well Pliocene localities<br />

(Jahn et al. 1984). Macro-remains <strong>of</strong> Cercidiphyllum<br />

occur in Poland in <strong>the</strong> Oligocene to<br />

Pliocene <strong>deposit</strong>s (Hummel 1970). These pollen<br />

grains were rarely encountered in <strong>the</strong><br />

studied material, in quantities not exceeding<br />

1%.<br />

Today relics <strong>of</strong> Cercidiphyllum (2 species)<br />

are wide-spread in <strong>the</strong> mountains <strong>of</strong> Japan<br />

and China. C. japonicum Sieb. & Zucc. is<br />

besides numbered among <strong>the</strong> oldest elements<br />

<strong>of</strong> <strong>the</strong> Japanese fl ora. This species grows in<br />

dense and wet forests, mainly on <strong>the</strong> altitudes<br />

above 1500 m a.s.l.; C. magnifi cum (Nakai)<br />

Nakai occurs in China (Wang 1961, Bugała<br />

1991).

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!