First fossil record of Staphylea L. (Staphyleaceae) from North America, and its biogeographic implications

被引:15
|
作者
Huang, Yong-Jiang [1 ,2 ]
Liu, Yu-Sheng [1 ]
Wen, Jun [3 ]
Quan, Cheng [4 ]
机构
[1] E Tennessee State Univ, Dept Biol Sci, Johnson City, TN 37614 USA
[2] Chinese Acad Sci, Key Lab Plant Biodivers & Biogeog East Asia, Kunming Inst Bot, Kunming 650204, Peoples R China
[3] Natl Museum Nat Hist, Dept Bot, Smithsonian Inst, MRC 166, Washington, DC 20560 USA
[4] Jilin Univ, Res Ctr Paleontol & Stratig, Changchun 130026, Peoples R China
基金
中国国家自然科学基金;
关键词
Fossil seed; Gray Fossil Site; Late Neogene; North America; Staphylea; EARLIEST PLIOCENE; LATEST MIOCENE; TENNESSEE; EVOLUTION; FRUITS; GRAY; MORPHOLOGY; SEED;
D O I
10.1007/s00606-015-1224-z
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
The occurrences of Staphylea L. (Staphyleaceae) fossils have been abundantly documented from the Cenozoic of Eurasia, but none has been confirmed from North America to date. In this study, we describe Staphylea levisemia sp. nov. on the basis of seed remains from the latest Miocene to earliest Pliocene of northeastern Tennessee, southeastern USA. The seeds are characterized by a smoothly inflated body, a large hilar scar perforated by several vascular traces and bordered by a distinctive lip-like rim, a cuticle coating the seed coat interior, and seed coat section containing weakly developed tiny lumina. According to the paleogeographic distribution of the genus, it is hypothesized that Staphylea originated from western Eurasia no later than the late Oligocene, and arrived in eastern North America no later than the late Neogene, most possibly through the North Atlantic land bridges like many other seed plants.
引用
收藏
页码:2203 / 2218
页数:16
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