1920 Fig. 3. Comparison of paleoclimatic

(blue line) and from MD 90-917 versus cal yr B.P. Chronology of the SST record is obtained by linear fits between two successive AMS 14 C ages on tephra (red arrows) and within peaks of abundance of planktonic foraminifera (black arrows) (9, 11). The 14 C ages were corrected from the varying measure...

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Main Author: Records From Gisp
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Planktonic foraminifera
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.141.97
http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.141.97
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.141.97 2023-05-15T18:00:40+02:00 1920 Fig. 3. Comparison of paleoclimatic Records From Gisp The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.141.97 http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.141.97 http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf text ftciteseerx 2016-01-07T14:59:00Z (blue line) and from MD 90-917 versus cal yr B.P. Chronology of the SST record is obtained by linear fits between two successive AMS 14 C ages on tephra (red arrows) and within peaks of abundance of planktonic foraminifera (black arrows) (9, 11). The 14 C ages were corrected from the varying measured R surf (red line) (10) and using a constant R surf of 390 years (14) (green line), then converted to calendar ages (8). The use of the �520year R surf estimate at �8200 years (4), slightly older than the modern one during the sapropel event, permits a better correlation between the two records. δ 18 O (‰) Text Planktonic foraminifera Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description (blue line) and from MD 90-917 versus cal yr B.P. Chronology of the SST record is obtained by linear fits between two successive AMS 14 C ages on tephra (red arrows) and within peaks of abundance of planktonic foraminifera (black arrows) (9, 11). The 14 C ages were corrected from the varying measured R surf (red line) (10) and using a constant R surf of 390 years (14) (green line), then converted to calendar ages (8). The use of the �520year R surf estimate at �8200 years (4), slightly older than the modern one during the sapropel event, permits a better correlation between the two records. δ 18 O (‰)
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Records From Gisp
spellingShingle Records From Gisp
1920 Fig. 3. Comparison of paleoclimatic
author_facet Records From Gisp
author_sort Records From Gisp
title 1920 Fig. 3. Comparison of paleoclimatic
title_short 1920 Fig. 3. Comparison of paleoclimatic
title_full 1920 Fig. 3. Comparison of paleoclimatic
title_fullStr 1920 Fig. 3. Comparison of paleoclimatic
title_full_unstemmed 1920 Fig. 3. Comparison of paleoclimatic
title_sort 1920 fig. 3. comparison of paleoclimatic
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.141.97
http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.141.97
http://www.gatsby.ucl.ac.uk/~pel/environment/mpa.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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