Vertebrate fossil-bearing paleosol units (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.): Implications for taphonomy, biostratigraphy, and assemblage analysis-Reference-Cited by-同舟云学术

Vertebrate fossil-bearing paleosol units (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.): Implications for taphonomy, biostratigraphy, and assemblage analysis

Published:1981-01 Issue: Volume:34 Page:31-56
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Bown Thomas M.,J. Kraus Mary

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference27 articles.

1. The taphonomy and paleoecology of Plio-Pleistocene vertebrate assemblages east of Lake Rudolf, Kenya;Behrensmeyer;Bull. Mus. Comp. Zool.,1975

2. Taphonomic and ecologic information from bone weathering;Behrensmeyer;Paleobiology,1978

3. New perspectives in vertebrate paleoecology from a recent bone assemblage;Behrensmeyer;Paleobiology,1979

4. The comparative ecology of rain forest mammals in Africa and tropical America: some introductory remarks;Bourliére,1972

5. Paleocene and lower Eocene rocks in the Sand Creek—No Water Creek area, Washakie County, Wyoming;Bown,1975

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