Redox conditions across the Cambrian–Ordovician boundary: Elemental and isotopic signatures retained in the GSSP carbonates-Reference-Cited by-同舟云学术

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Redox conditions across the Cambrian–Ordovician boundary: Elemental and isotopic signatures retained in the GSSP carbonates

Published:2015-12 Issue: Volume:440 Page:440-454
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Azmy Karem,Kendall Brian,Brand Uwe,Stouge Svend,Gordon Gwyneth W.

Funder

NSERC

Carlsberg Foundation

Publisher

Elsevier BV

Subject

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

Reference77 articles.

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3. A modern framework for the interpretation of 238U/235U in studies of ancient ocean redox;Andersen;Earth Planet. Sci. Lett.,2014

4. Trace element indicators of increased primary production and decreased water-column ventilation during deposition of latest Pliocene sapropels at five locations across the Mediterranean Sea;Arnaboldi;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2007

5. Coupled molybdenum, iron and uranium stable isotopes as oceanic paleoredox proxies during the Paleoproterozoic Shunga Event;Asael;Chem. Geol.,2013

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