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Did the expansion of C-4 plants drive extinction and massive range contraction of micromammals? Inferences from food preference and historical biogeography of pikas
Ge, Deyan1; Zhang, Zhaoqun2; Xia, Lin1; Zhang, Qian1; Ma, Yong1; Yang, Qisen1; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]
2012-04-01
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
卷号326页码:160-171
文章类型Article
摘要The expansion of C-4 plants is thought to have profound effects on the faunal turnover of large mammals during the latest Miocene. However, it is unclear whether this event also induced extinction and range contraction of small mammals. Pikas (Ochotonidae) are highly adapted to arctic or alpine environments, and are considered ideal indicators in biochronology. Previous studies have demonstrated that large numbers of ochotonides were widely geographically distributed in the middle Miocene, although most went extinct in the late Miocene. It is uncertain whether their extinction was induced by the accelerated expansion of C-4 plants. A comprehensive review of the worldwide fossil occurrence in Ochotonidae and a detailed analysis of its historical biogeography are also lacking. Here, we categorize plants that are selected by extant pikas for food and hay piles according to their photosynthesis pathway. Fossil records of Ochotonidae are also reviewed. The divergence time within Ochotona is estimated using multiple fossil calibrators and the combined matrix of two mitochondrial genes. We also infer the historical biogeography of Ochotona using event based methods (S-DIVA, Bayes-DIVA and Maximum Parsimony). The expansion of C-4 plants in the late Miocene may have resulted in the extinction and range contraction of pikas. This hypothesis is supported by the prominent preference of C-3 plants in extant pikas. The Qinghai-Tibet Plateau is identified as the most likely ancestral center or origin of extant Ochotona. Evolution of the pikas' geographical range shows a strong concordance with the global climate and paleoecological change. Their historical extinction and recent range contraction, as well as future survival prospects, appear to be closely associated with climate-driven vegetation changes in their habitats. (C) 2012 Elsevier B.V. All rights reserved.
关键词C-4 Plants Expansion Dispersal-vicariance Analysis (Diva) Forage Selection Historical Biogeography Ochotonidae Qinghai-tibet Plateau (Qhtp)
WOS标题词Science & Technology ; Physical Sciences ; Life Sciences & Biomedicine
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关键词[WOS]DISPERSAL-VICARIANCE ANALYSIS ; OCHOTONA-PRINCEPS ; GLOBAL CHANGE ; AMERICAN PIKAS ; LATE MIOCENE ; GREAT-BASIN ; PHOTOSYNTHETIC PATHWAYS ; MAMMAL DIVERSIFICATION ; SECONDARY METABOLITES ; NORTHERN PAKISTAN
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology ; Paleontology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:000302851200014
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/4307
专题古低等脊椎动物研究室
通讯作者[email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]
作者单位1.Chinese Acad Sci, Inst Zool, Key Lab Zool Systemat & Evolut, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
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Ge, Deyan,Zhang, Zhaoqun,Xia, Lin,et al. Did the expansion of C-4 plants drive extinction and massive range contraction of micromammals? Inferences from food preference and historical biogeography of pikas[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2012,326:160-171.
APA Ge, Deyan.,Zhang, Zhaoqun.,Xia, Lin.,Zhang, Qian.,Ma, Yong.,[email protected].(2012).Did the expansion of C-4 plants drive extinction and massive range contraction of micromammals? Inferences from food preference and historical biogeography of pikas.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,326,160-171.
MLA Ge, Deyan,et al."Did the expansion of C-4 plants drive extinction and massive range contraction of micromammals? Inferences from food preference and historical biogeography of pikas".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 326(2012):160-171.
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