22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN:
A planktonic foraminiferal fauna of probable late Aptian age is recorded in Cores 113-693A-47R and-48R, located on the Antarctic continental margin. Moderate to highly productive surface waters and upper bathyal paleodepths are inferred from benthic and planktonic foraminifers, and other biotic and...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.698.3473 2023-05-15T13:48:28+02:00 22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: R. Mark Leckie The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.698.3473 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.698.3473 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf text ftciteseerx 2016-01-08T18:44:54Z A planktonic foraminiferal fauna of probable late Aptian age is recorded in Cores 113-693A-47R and-48R, located on the Antarctic continental margin. Moderate to highly productive surface waters and upper bathyal paleodepths are inferred from benthic and planktonic foraminifers, and other biotic and mineral components in the>63 fim size frac-tion. INTRODUCTION AND METHODS 10°E ODP Site 693 lies on a mid-slope bench (2370 m) along the east-ern continental margin of the Weddell Sea (70°49.9'S, 14°34.4'W) (Fig. 1). Five samples from Cores 113-693A-47R and-48R were examined. The samples span a 19 m interval within Unit VII Text Antarc* Antarctic Weddell Sea Unknown Antarctic The Antarctic Weddell Weddell Sea |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
A planktonic foraminiferal fauna of probable late Aptian age is recorded in Cores 113-693A-47R and-48R, located on the Antarctic continental margin. Moderate to highly productive surface waters and upper bathyal paleodepths are inferred from benthic and planktonic foraminifers, and other biotic and mineral components in the>63 fim size frac-tion. INTRODUCTION AND METHODS 10°E ODP Site 693 lies on a mid-slope bench (2370 m) along the east-ern continental margin of the Weddell Sea (70°49.9'S, 14°34.4'W) (Fig. 1). Five samples from Cores 113-693A-47R and-48R were examined. The samples span a 19 m interval within Unit VII |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R. Mark Leckie |
spellingShingle |
R. Mark Leckie 22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
author_facet |
R. Mark Leckie |
author_sort |
R. Mark Leckie |
title |
22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
title_short |
22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
title_full |
22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
title_fullStr |
22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
title_full_unstemmed |
22. MIDDLE CRETACEOUS PLANKTONIC FORAMINIFERS OF THE ANTARCTIC MARGIN: |
title_sort |
22. middle cretaceous planktonic foraminifers of the antarctic margin: |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.698.3473 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf |
geographic |
Antarctic The Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic The Antarctic Weddell Weddell Sea |
genre |
Antarc* Antarctic Weddell Sea |
genre_facet |
Antarc* Antarctic Weddell Sea |
op_source |
http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.698.3473 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_22.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766249303428300800 |