A new species of Castanopsis (Fagaceae) from the upper Pliocene of West Yunnan, China and its biogeographical implications

被引:20
|
作者
Wu, Jing-Yu [1 ,2 ,3 ]
Ding, Su-Ting [1 ,2 ,3 ]
Li, Qi-Jia [1 ,2 ]
Zhao, Zhen-Rui [1 ,2 ]
Dong, Chong [1 ,2 ,3 ]
Sun, Bai-Nian [1 ,2 ,3 ]
机构
[1] Lanzhou Univ, Sch Earth Sci, Key Lab Mineral Resources Western China Gansu Pro, Lanzhou 730000, Peoples R China
[2] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China
[3] Chinese Acad Sci, Nanjing Inst Geol & Paleontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Castanopsis; Cuticle; Pliocene; Yunnan; Biogeography; TIBETAN PLATEAU; MIOCENE CLIMATE; EVOLUTION; GERMANY; UPLIFT; VEGETATION; RECONSTRUCTION; PALEOECOLOGY; PATTERNS; TERTIARY;
D O I
10.1016/j.palwor.2014.10.005
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Two focal leaves identified as Castanopsis presclerophylla n. sp. collected from a diatomite bed in the upper Pliocene (3.3-2.8 Ma) in Tengchong County, Yunnan Province, Southwest China, are characterized by elliptic laminar shapes with acuminate apex, convex base, simple trichome bases and cyclocytic stomata. The cuticles of extant leaves from six selected Castanopsis species that are similar to the Pliocene fossil leaves in laminar shape were examined in detail for the comparison. Based on the analysis of leaf architecture and cuticular characteristics, the present fossil leaves most closely resemble the extant leaves of Castanopsis sclerophylla (Lindl.) Schott., which prefers a subtropical climate. The published fossil records of Castanopsis also indicate that it was once widely distributed in North America, Europe and Asia before the Pliocene, and then rapidly retreated to the East and Southeast Asia as a result of the Pleistocene glaciation. (C) 2014 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
引用
收藏
页码:370 / 382
页数:13
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