in Jurassic and Cretaceous Stratigraphy
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in Jurassic and Cretaceous Stratigraphy
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Earth Science Frontiers, Vol. 17, Special Issue, Aug. 2010 ISSN 1005-2321<br />
228<br />
A Early <strong>Jurassic</strong> Flora from Southern Jil<strong>in</strong>, Ch<strong>in</strong>a<br />
Chunl<strong>in</strong> Sun 1 , Tao Li 2 , Lijun Zhang 3<br />
1. Key-Lab for Evolution of Past Life <strong>and</strong> Environment <strong>in</strong> Northeast Asia, M<strong>in</strong>istry of Education, Research Center of Paleontology <strong>and</strong><br />
<strong>Stratigraphy</strong> of Jil<strong>in</strong> University, Changchun 130026, Ch<strong>in</strong>a (E-mail: clsun@jlu.edu.cn)<br />
2. Geologic Museum of Jil<strong>in</strong> University, Changchun 130026, Ch<strong>in</strong>a<br />
3. Bureau of fossil protection <strong>and</strong> adm<strong>in</strong>istration of Liaon<strong>in</strong>g , Shenyang 110032, Ch<strong>in</strong>a<br />
A diversity Early <strong>Jurassic</strong> flora was preserved <strong>in</strong><br />
the f<strong>in</strong>e-gra<strong>in</strong>ed s<strong>and</strong>stone <strong>and</strong> siltstone beds from the<br />
middle-upper part of the Yihe Formation <strong>in</strong> the Yihe<br />
Bas<strong>in</strong>, southern Jil<strong>in</strong>, Ch<strong>in</strong>a. The Yihe Formation is<br />
represented by fluvial <strong>and</strong> swamp sediments, consist<strong>in</strong>g<br />
of conglomerates, s<strong>and</strong>stones, siltstlnes, <strong>and</strong> th<strong>in</strong> coal<br />
layers.<br />
The Yihe flora is composed of 35 species<br />
belong<strong>in</strong>g to 22 genera, conta<strong>in</strong><strong>in</strong>g Equisetales: Equi-<br />
setum laterale Phillips,Neocalamites carrerei (Zeiller)<br />
Halle, N. hoerrensis (Schimper) Halle, N. cf . rugousus<br />
Sze, Annulariopsis sp. Filicales: Marattiopsis hoerensis<br />
(schimper) Thomas, Coniopteris sp. 1, Coniopteris sp.<br />
2, Clathropteris obovata Öishi. Filices <strong>in</strong>certae sedis:<br />
Cladophlebis nebbensis (Brongniart) Nathorst, Clado-<br />
phlebis tersus Chang, Cladophlebis sulktensis var.<br />
crassa Brick, Cladophlebis sp. Bennettiales: Ptero-<br />
phyllum baotoum Zhang, Pterophyllum exhibens Li,<br />
Pterophyllum prop<strong>in</strong>quum Goeppert, Perophyllum cf.<br />
tietzei Schenk, Pterophyllum sp., Anomozamites sp.,<br />
Tyrmia? aequalis Liu et Mi, Cycadolepis corrugata<br />
Zeiller. Nilssoniales: Nilssonia <strong>in</strong>ouyei Yokyama, N.<br />
orientalis Heer N. sp. Cycadales: Ctenis ch<strong>in</strong>ensis Hsu,<br />
Ctenis sp. G<strong>in</strong>kgoales: G<strong>in</strong>kgo digitata (Brongniart)<br />
Heer, Baiera cf. conc<strong>in</strong>na (Heer)Kawasaki, Glosso-<br />
phyllum? sp. Czekanowskiales: Phoeniopsis sp. Coni-<br />
ferales: Storgaardia pityophylloides Liu et Mi,<br />
Podaozamitalis: Podaozamites sp., L<strong>in</strong>dleycladus<br />
lanceolatus (L<strong>in</strong>dley et Hutton.) Harris. Sem<strong>in</strong>a: Car-<br />
polithus sp. Form genus <strong>in</strong>certae sedis: Taeniopteris cf.<br />
tenu<strong>in</strong>ervis Braun.<br />
The flora is dom<strong>in</strong>ated by cycads <strong>and</strong> ferns.<br />
Among cycads, the most of genera have been found<br />
from the Early <strong>Jurassic</strong> foloras of the North <strong>and</strong> South<br />
Ch<strong>in</strong>a except for Siberia <strong>and</strong> the northern part of<br />
Northeastern Ch<strong>in</strong>a. Based on comparisons with sub-<br />
tropic or tropic floras from the southern Ch<strong>in</strong>a, some<br />
typical genera of cycads, for <strong>in</strong>stance Ptilophyllum,<br />
Otozamites, are absent <strong>in</strong> the present flora. Ferns<br />
possesses a higher percentage <strong>in</strong> the present flora,<br />
especially the occurrence of Clathropteris seems to<br />
<strong>in</strong>dicate a warm <strong>and</strong> humid climate, but compared with<br />
the those of the subtropic <strong>and</strong> tropic floras the com-<br />
ponents of Dipteridaceae are not abundant. G<strong>in</strong>kgos<br />
<strong>and</strong> Czekanowskiales with a low-diversity show<strong>in</strong>g<br />
seasonal change of climate also occur <strong>in</strong> the present<br />
flora. The more abundant Neocalamites of horsetail<br />
shows relatively complete fragmentation suggest<strong>in</strong>g it<br />
grew close to the depositional site. Sedimentological<br />
characteristics <strong>and</strong> the composition of the flora signifi-<br />
cantly <strong>in</strong>dicate a relatively warm <strong>and</strong> humid palaeo-<br />
climate for the Yihe Bas<strong>in</strong> Early <strong>Jurassic</strong>.<br />
The age of the Yihe flora has been generally<br />
accepted as Early <strong>Jurassic</strong> (Liu <strong>and</strong> Mi, 1981, Bureau of<br />
geology <strong>and</strong> m<strong>in</strong>eral resources of Jil<strong>in</strong>, 1982). Although<br />
the Yihe flora conta<strong>in</strong>s some taxa that are long rang<strong>in</strong>g<br />
through Late Triassic to the <strong>Jurassic</strong> <strong>in</strong> Eurasia, the<br />
occurrence <strong>and</strong> low-diversity of Coniopteris offers an<br />
evidence support<strong>in</strong>g a late Early <strong>Jurassic</strong> age. This<br />
genus is long rang<strong>in</strong>g (late Early <strong>Jurassic</strong> to Late<br />
<strong>Cretaceous</strong>) <strong>in</strong> the Northern Hemisphere, but it beg<strong>in</strong> to<br />
occur <strong>in</strong> the late Early <strong>Jurassic</strong> <strong>and</strong> diverse <strong>in</strong> the<br />
Middle <strong>Jurassic</strong>, absent <strong>in</strong> the early Early <strong>Jurassic</strong>. Only<br />
two <strong>in</strong>complete specimens of Coniopteris were<br />
collected from this flora. It is a significant component<br />
for us to regard the age of the present flora as late Early<br />
<strong>Jurassic</strong>.<br />
The present flora is similar to the those of Early<br />
<strong>Jurassic</strong> floras distributed <strong>in</strong> the North Ch<strong>in</strong>a <strong>and</strong><br />
Middle Asia, such as Fuxian flora from Northern<br />
Shanxi, Yongd<strong>in</strong>gzhuang flora from Datong, Shanxi,<br />
Wudanggou flora from Inner Mongolia, The flora of the<br />
upper mumber of Beipiao Formation from Western<br />
Liaon<strong>in</strong>g, Tianshuigou flora from Northeastern border<br />
of Qaidam Bas<strong>in</strong>, Q<strong>in</strong>ghai <strong>and</strong> Aksaisk flora from<br />
Issyk-kul Bas<strong>in</strong>, S<strong>and</strong>jia flora from Gissar, Kokkija<br />
flora from Eastern Fergana, Sarikamish flora from<br />
Northern Fergana, Dzhil flora from Northern Kirgizija.<br />
Acknowledgements: Supported by Project 111 of<br />
Ch<strong>in</strong>a.<br />
Key words: Southern Jil<strong>in</strong>; Early <strong>Jurassic</strong>; Flora<br />
References:<br />
Bureau of geology <strong>and</strong> m<strong>in</strong>eral resources of Jil<strong>in</strong><br />
Prov<strong>in</strong>ce. Regional geology of Jil<strong>in</strong> Prov<strong>in</strong>ce.<br />
Beij<strong>in</strong>g: Geological Publish<strong>in</strong>g House, 1988: 1-<br />
698 (<strong>in</strong> Ch<strong>in</strong>ese).<br />
Bureau of geology <strong>and</strong> m<strong>in</strong>eral resources of Jil<strong>in</strong><br />
Prov<strong>in</strong>ce. <strong>Stratigraphy</strong> (Lithostratic) of Jil<strong>in</strong><br />
Prov<strong>in</strong>ce. Wuhan: Ch<strong>in</strong>a University of Geo-<br />
sciences Press, 1997: 1-324 (<strong>in</strong> Ch<strong>in</strong>ese).<br />
Genk<strong>in</strong>a R.Z. Older Mesozoic flora <strong>and</strong> stratigraphy