The origins and evolution of the North American grassland biome: the story from the hoofed mammals

被引:146
作者
Janis, CM [1 ]
Damuth, J
Theodor, JM
机构
[1] Brown Univ, Dept Ecol & Evolutionary Biol, Providence, RI 02912 USA
[2] Univ Calif Santa Barbara, Dept Ecol Evolut & Marine Biol, Santa Barbara, CA 93106 USA
关键词
grasslands; herbivores; mammals; Miocene; atmospheric carbon dioxide;
D O I
10.1016/S0031-0182(01)00359-5
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The North American grassland biome first appeared around 18 Ma in the mid Miocene. The familiar story of the Neogene evolution of this biome is of the replacement of ungulates (hoofed mammals) having a primarily browsing diet by the more derived grazing ungulates. However, new data show a more complicated pattern of faunal succession. There was a maximum taxonomic diversity of ungulates at 16-14 Ma, including a large number of grazers, and the subsequent decline in overall diversity was largely due to the decline of the browsers, with little corresponding increase in the grazers. Additionally the mid Miocene faunas (similar to18-12 Ma) contained a much greater number of browsers than any comparable present-day habitat. We discuss possible explanations for these non-analogous grassland faunas, including the possibility that the primary productivity of the vegetation was greater in the early to middle Miocene than it is today. One possible explanation for increased primary productivity is higher Miocene levels of atmospheric carbon dioxide than in the present day. The proposed difference in vegetational productivity also may explain why horses radiated as the main grazers in North America, in contrast to the radiation of antelope in the Plio-Pleistocene African grasslands. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:183 / 198
页数:16
相关论文
共 61 条
[1]  
[Anonymous], EOCENE OLIGOCENE CLI
[2]  
[Anonymous], GSA TODAY
[3]   RISE OF THE GRASSLAND BIOME, CENTRAL NORTH-AMERICA [J].
AXELROD, DI .
BOTANICAL REVIEW, 1985, 51 (02) :163-201
[4]   THE RESPONSE OF NATURAL ECOSYSTEMS TO THE RISING GLOBAL CO2 LEVELS [J].
BAZZAZ, FA .
ANNUAL REVIEW OF ECOLOGY AND SYSTEMATICS, 1990, 21 :167-196
[5]   A MODEL FOR ATMOSPHERIC CO2 OVER PHANEROZOIC TIME [J].
BERNER, RA .
AMERICAN JOURNAL OF SCIENCE, 1991, 291 (04) :339-376
[6]   3GEOCARB-II - A REVISED MODEL OF ATMOSPHERIC CO2 OVER PHANEROZOIC TIME [J].
BERNER, RA .
AMERICAN JOURNAL OF SCIENCE, 1994, 294 (01) :56-91
[8]   Carbon dioxide starvation, the development of C4 ecosystems, and mammalian evolution [J].
Cerling, TE ;
Ehleringer, JR ;
Harris, JM .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES, 1998, 353 (1365) :159-170
[9]   Global vegetation change through the Miocene/Pliocene boundary [J].
Cerling, TE ;
Harris, JM ;
MacFadden, BJ ;
Leakey, MG ;
Quade, J ;
Eisenmann, V ;
Ehleringer, JR .
NATURE, 1997, 389 (6647) :153-158
[10]  
Churcher C.S., 1978, P379