中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Paleoecology of Pleistocene mammals and paleoclimatic change in South China: Evidence from stable carbon and oxygen isotopes

文献类型:期刊论文

作者Sun, Fajun1,2; Wang, Yang1,2,3,4; Wang, Yuan4; Jin, Chang-zhu4; Deng, Tao4; Wolff, Burt1,2
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2019-06-15
卷号524期号:0页码:1-12
关键词Fossils Stable isotopes Habitats Paleoclimate Yugong Cave Baxian Cave
ISSN号0031-0182
DOI10.1016/j.palaeo.2019.03.021
英文摘要The role of climate change in the evolution and diversification of hominoids remains a hotly debated issue. Stable isotope analyses of fossil mammals that coexisted with the hominoids can provide insights into hominoid palaeoenvironments and shed light on this debate. Here, we report results of stable carbon and oxygen isotope analyses of tooth enamel samples from a variety of Pleistocene mammals including pandas, deer, elephants, pigs, rhinos, and bovids from two hominoid fossil localities (Yugong Cave and Baxian Cave) in South China. Enamel delta C-13 values indicate that most of the mammals living in the study area during the late Middle Pleistocene had C-3-based diets but a small number of individuals consumed some C-4 grasses. This indicates the presence of C-4 plants in the region during the late Middle Pleistocene, most likely in patches of open areas in a predominantly forested environment. However, during the early Late Pleistocene, all of the mammals examined had C-3-based diets, except one bovid and one panda that may have ingested small amounts of C-4 plants. This indicates a dense forested environment with little C-4 grasses during the early Late Pleistocene. Like the Early Pleistocene pygmy panda (Ailuropoda microta) from Yanliang Cave, the late Middle Pleistocene Ailuropoda baconi from Yugong Cave and the early Late Pleistocene Ailuropoda melanoleuca from Baxian Cave had higher mean diet-delta C-13 values than other co-occurring herbivores, indicating they preferred relatively open forest habitats and had more restricted diets compared to other mammals. The reconstructed mean paleo-meteoric water delta O-18(w) values are lower than the annual average delta O-18(w) value of modern precipitation in the region, suggesting that the climatic conditions during the times when these Pleistocene mammals were alive were colder and/or wetter than today. In addition, delta O-18 values of the obligate drinkers (pigs, rhinos, bovids) display an overall decreasing trend, accompanied by increased range of delta O-18 variations, from the Early Pleistocene to the early Late Pleistocene. This suggests that the regional climate became colder and/or wetter, with increased seasonality, from the Early Pleistocene to the early Late Pleistocene, likely related to intensified glaciation. The change in climate to colder conditions may be responsible for the extinction of the Gigantopithecus in this region.
WOS关键词TIBETAN PLATEAU ; ENVIRONMENTAL-CHANGE ; DIET ; DISCRIMINATION ; ECOLOGY ; ARIDITY ; PLANTS ; TOOTH ; BONE ; RECONSTRUCTION
资助项目National Science Foundation[DMR-1644779] ; State of Florida
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
WOS记录号WOS:000469154700001
出版者ELSEVIER SCIENCE BV
源URL[http://119.78.100.205/handle/311034/10041]  
专题古脊椎动物与古人类研究所_图书馆1
通讯作者Sun, Fajun
作者单位1.Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA
2.Natl High Magnet Field Lab, Tallahassee, FL 32306 USA
3.Jinan Univ, Inst Groundwater & Earth Sci, Guangzhou 510632, Guangdong, Peoples R China
4.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing, Peoples R China
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Sun, Fajun,Wang, Yang,Wang, Yuan,et al. Paleoecology of Pleistocene mammals and paleoclimatic change in South China: Evidence from stable carbon and oxygen isotopes[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2019,524(0):1-12.
APA Sun, Fajun,Wang, Yang,Wang, Yuan,Jin, Chang-zhu,Deng, Tao,&Wolff, Burt.(2019).Paleoecology of Pleistocene mammals and paleoclimatic change in South China: Evidence from stable carbon and oxygen isotopes.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,524(0),1-12.
MLA Sun, Fajun,et al."Paleoecology of Pleistocene mammals and paleoclimatic change in South China: Evidence from stable carbon and oxygen isotopes".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 524.0(2019):1-12.

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来源:古脊椎动物与古人类研究所

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