The late Eocene hyracodontid perissodactyl Ardynia from Saint Jacques, Inner Mongolia, China and its implications for the potential Eocene–Oligocene boundary-Reference-Cited by-同舟云学术

The late Eocene hyracodontid perissodactyl Ardynia from Saint Jacques, Inner Mongolia, China and its implications for the potential Eocene–Oligocene boundary

Published:2018-06 Issue:2 Volume:27 Page:247-257
ISSN:1871-174X
Container-title:Palaeoworld
language:en
Short-container-title:Palaeoworld

Author:

Bai Bin,Wang Yuan-Qing,Zhang Zhao-Qun

Funder

National Natural Science Foundation of China

Special Fund for Fossil Excavation and Preparation, CAS, Macroevolutionary Processes and Paleoenvironments of Major Historical Biota

State Key Laboratory of Palaeobiology and Stratigraphy

Youth Innovation Promotion Association, CAS

Publisher

Elsevier BV

Subject

Paleontology,Stratigraphy,Ecology, Evolution, Behavior and Systematics

Reference43 articles.

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3. Eocene–Oligocene climatic and biotic evolution: an overview;Berggren,1992

4. Exploration in Inner Mongolia — a preliminary account of the 1959 field work of the Sino-Soviet Paleontological Expedition (SSPE);Chow;Vertebrata PalAsiatica,1960

5. New primitive true rhinoceroses from the Eocene of Iliang, Yunnan;Chow;Vertebrata PalAsiatica,1961

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