Evolution of marine mammals: Back to the sea after 300 million years

被引:114
作者
Uhen, Mark D. [1 ]
机构
[1] Smithsonian Inst, Natl Museum Nat Hist, Dept Paleobiol, Washington, DC 20013 USA
来源
ANATOMICAL RECORD-ADVANCES IN INTEGRATIVE ANATOMY AND EVOLUTIONARY BIOLOGY | 2007年 / 290卷 / 06期
关键词
cetacea; sirenia; pinnipedia; carnirora; desmostylia; feeding ecology; aquatic adaptation;
D O I
10.1002/ar.20545
中图分类号
R602 [外科病理学、解剖学]; R32 [人体形态学];
学科分类号
100101 ;
摘要
The fossil record demonstrates that mammals re-entered the marine realm on at least seven separate occasions. Five of these clades are still extant, whereas two are extinct. This review presents a brief introduction to the phylogeny of each group of marine mammals, based on the latest studies using both morphological and molecular data. Evolutionary highlights are presented, focusing on changes affecting the sensory systems, locomotion, breathing, feeding, and reproduction in Cetacea, Sirenia, Desmostylia, and Pinnipedia. Aquatic adaptations are specifically cited, supported by data from morphological and geochemical studies. For example, analysis of oxygen isotopes incorporated into fossil tooth enamel indicates whether these mammals foraged in (and, therefore, ingested) fresh water or sea water. Comparisons between groups are made to see if there are any common patterns, particularly relating to adaptations to aquatic life. Results show that aquatic characteristics evolved in mosaic patterns and that different morphological solutions to aquatic conditions were achieved separately in each of these groups. Changes in the axial and appendicular skeleton assist with locomotion for aquatic foraging. Nostril and eye placement modifications accommodate wading versus underwater foraging needs. All groups exhibit aquatic adaptations directly related to feeding, particularly changes in the dentition and rostrum. The earliest representatives of these clades all show morphological features that indicate they were feeding while in the water, suggesting that feeding ecology is a key factor in the evolution of marine mammals.
引用
收藏
页码:514 / 522
页数:9
相关论文
共 69 条
[1]  
[Anonymous], 1986, Smithsonian Contributions to Paleobiology, DOI DOI 10.5479/SI.00810266.59.1
[2]   Mitogenomic analyses provide new insights into cetacean origin and evolution [J].
Arnason, U ;
Gullberg, A ;
Janke, A .
GENE, 2004, 333 :27-34
[3]  
Barnes Lawrence G., 2001, Bulletin of Ashoro Museum of Paleontology, V2, P7
[4]   SKELETON OF THE OLDEST KNOWN PINNIPED, ENALIARCTOS-MEALSI [J].
BERTA, A ;
RAY, CE ;
WYSS, AR .
SCIENCE, 1989, 244 (4900) :60-62
[5]  
Berta A., 2006, MARINE MAMMALS EVOLU
[6]  
Berta A., 1991, Smithsonian Contributions to Paleobiology, V69, P1, DOI [10.5479/si.00810266.69.1, DOI 10.5479/SI.00810266.69.1]
[7]  
Berta Annalisa, 1994, Proceedings of the San Diego Society of Natural History, V29, P33
[8]   Fossil whale preservation implies high diatom accumulation rate in the Miocene-Pliocene Pisco Formation of Peru [J].
Brand, LR ;
Esperante, R ;
Chadwick, AV ;
Porras, OP ;
Alomía, M .
GEOLOGY, 2004, 32 (02) :165-168
[9]   Independent adaptation to riverine habitats allowed survival of ancient cetacean lineages [J].
Cassens, I ;
Vicario, S ;
Waddell, VG ;
Balchowsky, H ;
Van Belle, D ;
Ding, W ;
Fan, C ;
Mohan, RSL ;
Simoes-Lopes, PC ;
Bastida, R ;
Meyer, A ;
Stanhope, MJ ;
Milinkovitch, MC .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2000, 97 (21) :11343-11347
[10]  
Clementz MT, 2003, PALEOBIOLOGY, V29, P506, DOI 10.1666/0094-8373(2003)029<0506:APPTHA>2.0.CO