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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Main Author: R. Mark Leckie
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access: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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spelling 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
institution Open Polar
collection Unknown
op_collection_id 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
author2 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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