Reconstructing the palaeoenvironment of the Middle Russian Sea during the Middle–Late Jurassic transition using stable isotope ratios of cephalopod shells and variations in faunal assemblages

Author:

Wierzbowski Hubert,Rogov Mikhail

Funder

RFBR

Presidium of the Russian Academy of Sciences

Institute of Geological Sciences, Polish Academy of Sciences

Publisher

Elsevier BV

Subject

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

Reference100 articles.

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2. The stable isotopic records of fossils from the Peterborough Member, Oxford Clay Formation (Jurassic), UK: palaeoenvironmental implications;Anderson;J. Geol. Soc. Lond.,1994

3. Allopatric speciation of the teuthid fauna on the shelf and slope of northwest Africa;Arkhipkin;Acta Universitatis Carolinae-Geologica,2006

4. Carbon and oxygen isotope composition of Nautilus macromphalus: a record of thermocline waters off New Caledonia;Auclair;Chem. Geol.,2004

5. Thermal regime variations in the Jurassic marine basin of the East European Platform at the Callovian/Oxfordian boundary: evidence from stable isotopes in belemnite rostra;Barskov;Dokl. Earth Sci.,2000

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