Relationship between δ13C and δ18O values of the RecentNautilus and brachiopod shells in the wild and the problem of reconstruction of fossil cephalopod habitat-Reference-Cited by-同舟云学术

Relationship between δ13C and δ18O values of the RecentNautilus and brachiopod shells in the wild and the problem of reconstruction of fossil cephalopod habitat

Published:2006-09 Issue:3 Volume:10 Page:331-345
ISSN:1226-4806
Container-title:Geosciences Journal
language:en
Short-container-title:Geosci J

Author:

Zakharov Yuri D.,Shigeta Yasunari,Smyshlyaeva Olga P.,Popov Alexander M.,Ignatiev Alexander V.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

http://link.springer.com/content/pdf/10.1007/BF02910374.pdf

Reference55 articles.

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2. Berthold, T. and Engeser, T., 1987, Phylogenetic analysis and systematization of the Cephalopoda. Verhandlungen des Naturwissenschaftlichen. Vereins in Hamburg, 29, 187–220.

3. Cochran, J.K., Rye, D.M. and Landman, N.H., 1981, Growth rate and habitat ofNautilus pompilius inferred from radioactive and stable isotope studies. Paleobiology, 7, 469–480.

4. Collins, D., Ward, P.D. and Westermann, G.E.G., 1980, Function of cameral water inNautilus. Paleobiology, 6(2), 168–172.

5. Craig, H. and Gordon, L.I., 1965, Deuterium and oxygen-18 variations in the ocean and marine atmosphere. In: E. Tongiorgi (Editor), Stable Isotopes in Oceanographic Studies and Paleo-Temperatures. Pisa, Lab. Geol. Nucl.: 9–130.

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