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Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

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Record title

Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

Record identifier

TN_cdi_proquest_miscellaneous_743205933

Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

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https://collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743205933

Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

Full title

Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

Publisher

Washington, DC: American Association for the Advancement of Science

Journal title

Science (American Association for the Advancement of Science), 2008, Vol.321 (5891), p.949-952

Record Identifier

TN_cdi_proquest_miscellaneous_743205933

Language

English

Formats

Publication information

Publisher

Washington, DC: American Association for the Advancement of Science

More information

SCOPE AND CONTENTS

Contents

Earth's surface chemical environment has evolved from an early anoxic condition to the oxic state we have today. Transitional between an earlier Proterozoic world with widespread deep-water anoxia and a Phanerozoic world with large oxygen-utilizing animals, the Neoproterozoic Era [1000 to 542 million years ago (Ma)] plays a key role in this history...

ALTERNATIVE TITLES

Full title

Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry

Identifiers

PRIMARY IDENTIFIERS

Record Identifier

TN_cdi_proquest_miscellaneous_743205933

Permalink

https://collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743205933

OTHER IDENTIFIERS

ISSN

0036-8075

E-ISSN

1095-9203

DOI

10.1126/science.1154499

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