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Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball...

Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_4b9ea44d0f664016b1b2a7482b73670d

Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth

About this item

Full title

Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth

Publisher

London: Nature Publishing Group UK

Journal title

Nature communications, 2016-07, Vol.7 (1), p.12192-12192, Article 12192

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

The terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pronounced positive sulfur isotope (
34
S/
32
S) excursions in Earth’s history, with strong variability and maximum values averaging δ
34
S∼+38‰. These excursions have been mostly interpreted in the framework of steady-state models, in which ocean sulfate co...

Alternative Titles

Full title

Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_4b9ea44d0f664016b1b2a7482b73670d

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_4b9ea44d0f664016b1b2a7482b73670d

Other Identifiers

ISSN

2041-1723

E-ISSN

2041-1723

DOI

10.1038/ncomms12192

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