Oligocene mammals from Ethiopia and faunal exchange between Afro-Arabia and Eurasia

被引:110
作者
Kappelman, J [1 ]
Rasmussen, DT
Sanders, WJ
Feseha, M
Bown, T
Copeland, P
Crabaugh, J
Fleagle, J
Glantz, M
Gordon, A
Jacobs, B
Maga, M
Muldoon, K
Pan, A
Pyne, L
Richmond, B
Ryan, T
Seiffert, ER
Sen, S
Todd, L
Wiemann, MC
Winkler, A
机构
[1] Univ Texas, Dept Anthropol, Austin, TX 78712 USA
[2] Univ Texas, Dept Geol Sci, Austin, TX 78712 USA
[3] Washington Univ, Dept Anthropol, St Louis, MO 63130 USA
[4] Univ Michigan, Museum Paleontol, Ann Arbor, MI 48109 USA
[5] Univ Houston, Dept Geosci, Houston, TX 77204 USA
[6] Univ Wyoming, Dept Geol & Geophys, Laramie, WY 82071 USA
[7] SUNY Stony Brook, Dept Anat Sci, Stony Brook, NY 11794 USA
[8] Colorado State Univ, Dept Anthropol, Ft Collins, CO 80523 USA
[9] So Methodist Univ, Dept Geol Sci, Dallas, TX 75275 USA
[10] George Washington Univ, Dept Anthropol, Washington, DC 20052 USA
[11] Duke Univ, Dept Biol Anthropol & Anat, Durham, NC 27708 USA
[12] Museum Natl Hist Nat, Lab Paleontol, F-75005 Paris, France
[13] Forest Serv, Ctr Wood Anat Res, USDA, Forest Prod Lab, Madison, WI 53705 USA
[14] Univ Texas, SW Med Ctr, Dept Cell Biol, Dallas, TX 75390 USA
基金
美国国家科学基金会;
关键词
D O I
10.1038/nature02102
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
Afro-Arabian mammalian communities underwent a marked transition near the Oligocene/Miocene boundary at approximately 24 million years (Myr) ago. Although it is well documented that the endemic paenungulate taxa were replaced by migrants from the Northern Hemisphere, the timing and evolutionary dynamics of this transition have long been a mystery because faunas from about 32 to 24 Myr ago are largely unknown(1). Here we report a late Oligocene fossil assemblage from Ethiopia, which constrains the migration to postdate 27 Myr ago, and yields new insight into the indigenous faunal dynamics that preceded this event. The fauna is composed of large paenungulate herbivores and reveals not only which earlier taxa persisted into the late Oligocene epoch but also demonstrates that one group, the Proboscidea, underwent a marked diversification. When Eurasian immigrants entered Afro-Arabia, a pattern of winners and losers among the endemics emerged: less diverse taxa such as arsinoitheres became extinct, moderately species-rich groups such as hyracoids continued into the Miocene with reduced diversity, whereas the proboscideans successfully carried their adaptive radiation out of Afro-Arabia and across the world.
引用
收藏
页码:549 / 552
页数:4
相关论文
共 31 条
[1]  
[Anonymous], 1986, Munchner Geowiss Abh
[2]  
[Anonymous], 2006, ARSENIC CYCLING SPEC
[3]   A brief Oligocene period of flood volcanism in Yemen: Implications for the duration and rate of continental flood volcanism at the Afro-Arabian triple junction [J].
Baker, J ;
Snee, L ;
Menzies, M .
EARTH AND PLANETARY SCIENCE LETTERS, 1996, 138 (1-4) :39-55
[4]   STRATIGRAPHY OF THE LOTHIDOK RANGE, NORTHERN KENYA, AND K/AR AGES OF ITS MIOCENE PRIMATES [J].
BOSCHETTO, HB ;
BROWN, FH ;
MCDOUGALL, I .
JOURNAL OF HUMAN EVOLUTION, 1992, 22 (01) :47-71
[5]   REVISED CALIBRATION OF THE GEOMAGNETIC POLARITY TIMESCALE FOR THE LATE CRETACEOUS AND CENOZOIC [J].
CANDE, SC ;
KENT, DV .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B4) :6093-6095
[6]  
Coppens Y., 1978, P336
[7]   A new species of Numidotherium (Mammalia: Proboscidea) from the Eocene of Libya and the early phylogeny of the Proboscidea [J].
Court, N .
JOURNAL OF VERTEBRATE PALEONTOLOGY, 1995, 15 (03) :650-671
[8]  
FESEHA M, 2001, SEQUENCE STRATIGRAPH
[9]  
Gheerbrant E, 2002, ACTA PALAEONTOL POL, V47, P493
[10]   A Palaeocene proboscidean from Morocco [J].
Gheerbrant, E ;
Sudre, J ;
Cappetta, H .
NATURE, 1996, 383 (6595) :68-70