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Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
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Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Record identifier
TN_cdi_proquest_miscellaneous_743205933
Record permalink
https://collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743205933
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Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
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Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
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Author / Creator
Publisher
Washington, DC: American Association for the Advancement of Science
Journal title
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Language
English
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Publication information
Publisher
Washington, DC: American Association for the Advancement of Science
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— 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
— AUTHORS, ARTISTS AND CONTRIBUTORS
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— 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