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Early angiosperms from the Lower Cretaceous of Jixi, eastern ...

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92<br />

G. Sun, D.L. Dilcher / Review <strong>of</strong> Palaeobotany and Palynology 121 (2002) 91^112<br />

However, a few pollen records <strong>from</strong> <strong>the</strong> lower<br />

<strong>Lower</strong> <strong>Cretaceous</strong> (e.g. Valanginian) support <strong>the</strong><br />

idea that <strong>the</strong> divergence <strong>of</strong> <strong>the</strong> <strong>angiosperms</strong> could<br />

be earlier (Hughes, 1994; Brenner, 1996).The recent<br />

discovery <strong>of</strong> early <strong>angiosperms</strong> (i.e. Archaefructus)<br />

<strong>from</strong> <strong>the</strong> western Liaoning, China could<br />

possibly even be traced to <strong>the</strong> Late Jurassic (Sun<br />

et al., 1998).Never<strong>the</strong>less, <strong>the</strong> middle <strong>Early</strong> <strong>Cretaceous</strong><br />

appears to be a very important period in<br />

<strong>the</strong> evolution and development <strong>of</strong> <strong>angiosperms</strong> in<br />

<strong>the</strong> world.Therefore, <strong>the</strong> recent ¢ndings <strong>of</strong> angiosperm<br />

megafossils as well as some micr<strong>of</strong>ossils<br />

<strong>from</strong> <strong>the</strong> early^middle <strong>Early</strong> <strong>Cretaceous</strong> Chengzihe<br />

Formation <strong>of</strong> <strong>Jixi</strong>, <strong>eastern</strong> Heilongjiang, China<br />

reported here (Fig.1), are very signi¢cant for<br />

<strong>the</strong> study <strong>of</strong> early <strong>angiosperms</strong> in <strong>the</strong> world and<br />

particularly in <strong>eastern</strong> Asia. Sun et al.(1992a) ¢rst<br />

reported <strong>the</strong> early angiosperm megafossils <strong>from</strong><br />

<strong>the</strong> Chengzihe Formation <strong>of</strong> <strong>Jixi</strong> and considered<br />

<strong>the</strong> age <strong>of</strong> <strong>the</strong> angiosperm fossils as Valanginian^<br />

Hauterivian or early Barremian based mainly on<br />

<strong>the</strong> associated marine dino£agellates in <strong>the</strong> formation.Later,<br />

Sun and Dilcher (1996, 1997) studied<br />

<strong>the</strong>se early angiosperm leaf remains and particularly<br />

<strong>the</strong> in£orescence and its pollen grains. He<br />

and Sun (2000) restudied <strong>the</strong> dino£agellates associated<br />

with <strong>the</strong> <strong>angiosperms</strong> <strong>of</strong> <strong>the</strong> Chengzihe<br />

Formation, and proposed <strong>the</strong>ir new determina-<br />

tions resulting in more precise dating as late Hauterivian<br />

in age.<br />

The early <strong>angiosperms</strong> <strong>from</strong> <strong>the</strong> Chengzihe<br />

Formation <strong>of</strong> <strong>Jixi</strong>, China described here all are<br />

dicotyledons with many leaf and reproductive<br />

characters new in <strong>the</strong> early history <strong>of</strong> <strong>the</strong> group<br />

and <strong>the</strong>se are presented so <strong>the</strong>y can be evaluated<br />

as primitive or derived angiosperm characters.At<br />

this locality, abundant fossil ferns and fern allies,<br />

cycadales, bennettitales, ginkgoales, conifers and<br />

caytoniales are associated with <strong>the</strong> <strong>angiosperms</strong>,<br />

including Equisetites burejensis, Coniopteris burejensis,<br />

Acanthopteris gothanii, Onychiopsis elongata,<br />

Acropteris sp., Cladophlebis sp., Nilssonia sinensis,<br />

Nilssonia angustissima, Pseudocycas sp.,<br />

Ginkgo sp., Sphenobaiera sp., Elatocladus submanchurica,<br />

Sphenolepis kurriana, Schizolepis sp.and<br />

Sagenopteris sp.(Sun et al., 1992a; Sun, 1995).<br />

2. Material and methods<br />

One important aspect <strong>of</strong> this investigation is <strong>the</strong><br />

validity <strong>of</strong> <strong>the</strong> age determination for <strong>the</strong> fossil<br />

<strong>angiosperms</strong> described in this paper.The determination<br />

<strong>of</strong> <strong>the</strong> age involved a great deal <strong>of</strong> ¢eld<br />

mapping <strong>of</strong> <strong>the</strong> Chengzihe Formation and associated<br />

Muling Formation exposed along <strong>the</strong> Muling<br />

Fig.1.Geographic position <strong>of</strong> <strong>the</strong> locality <strong>of</strong> <strong>the</strong> early <strong>angiosperms</strong> <strong>from</strong> <strong>Jixi</strong> <strong>of</strong> Heilongjiang, China.

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