New species of fossil Dryopterites from the Lower Cretaceous in the Zhongkouzi Basin, Beishan area, Northwest China, and its geological significance
New species of fossil Dryopterites from the Lower Cretaceous in the Zhongkouzi Basin, Beishan area, Northwest China, and its geological significance
复制标题
DOI:
10.1080/08912963.2021.2022135
复制
发表时间:
2022-01
影响因子:
1.4
通讯作者:
Wenxiu Ren;Guang Wu;Lei Han;Yifan Hua;Bai-Nian Sun
中科院分区:
文献类型:
--
作者:
Wenxiu Ren;Guang Wu;Lei Han;Yifan Hua;Bai-Nian Sun
ABSTRACT Fossil remains of Dryopterites fern foliage were collected from the Lower Cretaceous Chijinbao Formation in the Zhongkouzi Basin, Beishan area, Northwest China. A new species, Dryopterites beishanensis Ren and Sun sp. nov., is described on the basis of gross morphological structure and details of reproductive characters. Fronds are tripinnate, the main rachis is broad, and pinnules are small, oval or long ovate, and attached at narrow angles to the rachis, with apices obtuse. Sporangia are rounded or rounded-reniform and borne on the lateral vein, with one to two pairs in number. Spores are suborbicular or oval and monolete, with laesura 28 to 41 µm long. The extine is not smooth. The new fossils represent the first record of Dryopterites from the Chijinbao Formation. Additionally, according to different fossil records, the genus Dryopterites most likely originated in East Asia in the Early Cretaceous (Hauterivian to Barremian age). The new fossil provides new evidence on concerning the origin of Dryopterites.