Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian
The funded research was motivated by the earlier study of Burdett et al. (1990), who collected carbon and oxygen isotopic data from Paleoproterozoic rocks of the Northwest Territories from deep-and shallow-water facies of the Rocknest Platform. Their results displayed a possible decrease in (delta)C...
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1997
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ftnasantrs:oai:casi.ntrs.nasa.gov:19980031507 2023-05-15T17:46:33+02:00 Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian Kump, Lee R. Unclassified, Unlimited, Publicly available 1997 application/pdf http://hdl.handle.net/2060/19980031507 unknown Document ID: 19980031507 http://hdl.handle.net/2060/19980031507 No Copyright CASI Life Sciences (General) NASA/CR-97-206475 NAS 1.26:206475 1997 ftnasantrs 2019-08-31T23:06:14Z The funded research was motivated by the earlier study of Burdett et al. (1990), who collected carbon and oxygen isotopic data from Paleoproterozoic rocks of the Northwest Territories from deep-and shallow-water facies of the Rocknest Platform. Their results displayed a possible decrease in (delta)C-13 with depth when arranged by increasing distance from the paleoshore. The most C-13-depleted samples were seafloor cements and fans from the underlying siliciclastic Odjick Formation, and slope carbonates of the Rocknest platform. Other/Unknown Material Northwest Territories NASA Technical Reports Server (NTRS) Northwest Territories |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Life Sciences (General) |
spellingShingle |
Life Sciences (General) Kump, Lee R. Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
topic_facet |
Life Sciences (General) |
description |
The funded research was motivated by the earlier study of Burdett et al. (1990), who collected carbon and oxygen isotopic data from Paleoproterozoic rocks of the Northwest Territories from deep-and shallow-water facies of the Rocknest Platform. Their results displayed a possible decrease in (delta)C-13 with depth when arranged by increasing distance from the paleoshore. The most C-13-depleted samples were seafloor cements and fans from the underlying siliciclastic Odjick Formation, and slope carbonates of the Rocknest platform. |
format |
Other/Unknown Material |
author |
Kump, Lee R. |
author_facet |
Kump, Lee R. |
author_sort |
Kump, Lee R. |
title |
Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
title_short |
Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
title_full |
Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
title_fullStr |
Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
title_full_unstemmed |
Investigation of Isotopic and Geochemical Evidence for an Active Planktonic Biota in the Precambrian |
title_sort |
investigation of isotopic and geochemical evidence for an active planktonic biota in the precambrian |
publishDate |
1997 |
url |
http://hdl.handle.net/2060/19980031507 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Northwest Territories |
geographic_facet |
Northwest Territories |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_source |
CASI |
op_relation |
Document ID: 19980031507 http://hdl.handle.net/2060/19980031507 |
op_rights |
No Copyright |
_version_ |
1766150277851774976 |