Reply

The authors respond to Hoffman et al. (2001), who acknowledged that methane may have played an important role in unusual events associated with Neoproterozoic glaciation, but questioned the authors' permafrost gas hydrate hypothesis for 13C-depleted cap carbonate formation. The critique focused...

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Bibliographic Details
Main Authors: Kennedy, Martin J., Christie-Blick, Nicholas, Sohl, Linda E.
Format: Text
Language:unknown
Published: Columbia University 2002
Subjects:
Geology
Paleoclimatology
Geochemistry
permafrost
Online Access:https://dx.doi.org/10.7916/d8fb5d3q
https://academiccommons.columbia.edu/doi/10.7916/D8FB5D3Q
id ftdatacite:10.7916/d8fb5d3q
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spelling ftdatacite:10.7916/d8fb5d3q 2023-05-15T17:57:20+02:00 Reply Kennedy, Martin J. Christie-Blick, Nicholas Sohl, Linda E. 2002 https://dx.doi.org/10.7916/d8fb5d3q https://academiccommons.columbia.edu/doi/10.7916/D8FB5D3Q unknown Columbia University Geology Paleoclimatology Geochemistry Text Articles article-journal ScholarlyArticle 2002 ftdatacite https://doi.org/10.7916/d8fb5d3q 2021-11-05T12:55:41Z The authors respond to Hoffman et al. (2001), who acknowledged that methane may have played an important role in unusual events associated with Neoproterozoic glaciation, but questioned the authors' permafrost gas hydrate hypothesis for 13C-depleted cap carbonate formation. The critique focused on three issues: (1) an interpretation for tube structures in cap carbonates unrelated to gas migration; (2) the absence of a suitable source for methane gas; and (3) the degree of 13C depletion in sheet-crack cements. Text permafrost DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geology
Paleoclimatology
Geochemistry
spellingShingle Geology
Paleoclimatology
Geochemistry
Kennedy, Martin J.
Christie-Blick, Nicholas
Sohl, Linda E.
Reply
topic_facet Geology
Paleoclimatology
Geochemistry
description The authors respond to Hoffman et al. (2001), who acknowledged that methane may have played an important role in unusual events associated with Neoproterozoic glaciation, but questioned the authors' permafrost gas hydrate hypothesis for 13C-depleted cap carbonate formation. The critique focused on three issues: (1) an interpretation for tube structures in cap carbonates unrelated to gas migration; (2) the absence of a suitable source for methane gas; and (3) the degree of 13C depletion in sheet-crack cements.
format Text
author Kennedy, Martin J.
Christie-Blick, Nicholas
Sohl, Linda E.
author_facet Kennedy, Martin J.
Christie-Blick, Nicholas
Sohl, Linda E.
author_sort Kennedy, Martin J.
title Reply
title_short Reply
title_full Reply
title_fullStr Reply
title_full_unstemmed Reply
title_sort reply
publisher Columbia University
publishDate 2002
url https://dx.doi.org/10.7916/d8fb5d3q
https://academiccommons.columbia.edu/doi/10.7916/D8FB5D3Q
genre permafrost
genre_facet permafrost
op_doi https://doi.org/10.7916/d8fb5d3q
_version_ 1766165734904299520

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