Ecological changes in Miocene mammalian record show impact of prolonged climatic forcing

被引:159
作者
Badgley, Catherine [1 ,2 ]
Barry, John C. [3 ]
Morgan, Michele E. [3 ]
Nelson, Sherry V. [4 ]
Behrensmeyer, Anna K. [5 ]
Cerling, Thure E. [6 ]
Pilbeam, David [3 ]
机构
[1] Univ Michigan, Museum Paleontol, Ann Arbor, MI 48109 USA
[2] Univ Michigan, Dept Ecol & Evolutionary Biol, Ann Arbor, MI 48109 USA
[3] Harvard Univ, Peabody Museum, Cambridge, MA 02138 USA
[4] Univ New Mexico, Dept Anthropol, Albuquerque, NM 87131 USA
[5] Smithsonian Inst, Natl Museum Nat Hist, Evolut Terr Ecosyst Program, Dept Paleobiol, Washington, DC 20560 USA
[6] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA
基金
美国国家科学基金会;
关键词
faunal turnover; isotope ecology; mammals; paleocommunities; flood plain paleoecology;
D O I
10.1073/pnas.0805592105
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Geohistorical records reveal the long-term impacts of climate change on ecosystem structure. A 5-myr record of mammalian faunas from floodplain ecosystems of South Asia shows substantial change in species richness and ecological structure in relation to vegetation change as documented by stable isotopes of C and 0 from paleosols. Between 8.5 and 6.0 Mal, C-4 savannah replaced C-3 forest and woodland. Isotopic historical trends for 27 mammalian herbivore species, in combination with ecomorphological data from teeth, show three patterns of response. Most forest frugivores and browsers maintained their dietary habits and disappeared. Other herbivores altered their dietary habits to include increasing amounts of C4 plants and persisted for >1 myr during the vegetation transition. The few lineages that persisted through the vegetation transition show isotopic enrichment of delta C-13 values over time. These results are evidence for long-term climatic forcing of vegetation structure and mammalian ecological diversity at the subcontinental scale.
引用
收藏
页码:12145 / 12149
页数:5
相关论文
共 35 条
[1]  
ALROY J, 2001, DEEP TIME PALEOBIOLO, P259
[2]   Evolution of Asian monsoons and phased uplift of the Himalayan Tibetan plateau since Late Miocene times [J].
An, ZS ;
Kutzbach, JE ;
Prell, WL ;
Porter, SC .
NATURE, 2001, 411 (6833) :62-66
[3]   Ecological biogeography of North American mammals: species density and ecological structure in relation to environmental gradients [J].
Badgley, C ;
Fox, DL .
JOURNAL OF BIOGEOGRAPHY, 2000, 27 (06) :1437-1467
[4]  
Badgley Catherine, 2005, P29
[5]  
Barnosky AD, 2002, EVOL ECOL RES, V4, P811
[6]   Effects of Quaternary Climatic Change on Speciation in Mammals [J].
Anthony D. Barnosky .
Journal of Mammalian Evolution, 2005, 12 (1-2) :247-264
[7]  
Barry JC, 2002, PALEOBIOLOGY, V28, P1, DOI 10.1666/0094-8373(2002)28[1:FAECIT]2.0.CO
[8]  
2
[9]   The structure and rate of late Miocene expansion of C4 plants:: Evidence from lateral variation in stable isotopes in paleosols of the Siwalik Group, northern Pakistan [J].
Behrensmeyer, Anna K. ;
Quade, Jay ;
Cerling, Thure E. ;
Kappelman, John ;
Khan, Imran A. ;
Copeland, Peter ;
Roe, Lois ;
Hicks, Jason ;
Stubblefield, Phoebe ;
Willis, Brian J. ;
Latorre, Claudio .
GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 2007, 119 (11-12) :1486-1505
[10]  
Belmaker M, 2007, J VERTEBR PALEONTOL, V27, p46A