Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...

Planktonic foraminiferal assemblages from the upper Pleistocene part of Hole 1087A (0 to 12.1 meters below seafloor) are investigated to assess the role of global and local climate changes on surface circulation in the southern Benguela region. The benthic stable isotope record indicates that the st...

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Main Authors: Giraudeau, Jacques, Pierre, Catherine, Herve, Laurence
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735232
https://doi.pangaea.de/10.1594/PANGAEA.735232
id ftdatacite:10.1594/pangaea.735232
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735232 2024-09-15T18:19:31+00:00 Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ... Giraudeau, Jacques Pierre, Catherine Herve, Laurence 2001 application/zip https://dx.doi.org/10.1594/pangaea.735232 https://doi.pangaea.de/10.1594/PANGAEA.735232 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.175.225.2001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg175 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.73523210.2973/odp.proc.sr.175.225.2001 2024-08-01T10:53:32Z Planktonic foraminiferal assemblages from the upper Pleistocene part of Hole 1087A (0 to 12.1 meters below seafloor) are investigated to assess the role of global and local climate changes on surface circulation in the southern Benguela region. The benthic stable isotope record indicates that the studied interval is representative of the last four climatic cycles, that is, down to marine isotope Stage (MIS) 12. The species assemblages bear a clear transitional to subpolar character, with Neogloboquadrina pachyderma (d), Globorotalia inflata, and Globigerina bulloides, in order of decreasing abundance, as the dominant taxa. This species association presently characterizes the mixing domain of old upwelled and open ocean waters, seaward of the Benguela upwelling cells. Abundance variation of the dominant foraminiferal species roughly follows a glacial-interglacial pattern down to MIS 8, suggesting an alternation of upwelling strength and associated seaward extension of the belt of upwelled water as a response ... : Supplement to: Giraudeau, Jacques; Pierre, Catherine; Herve, Laurence (2001): A late Quaternary, high-resolution record of planktonic foraminiferal species distribution in the southern Benguela region: Site 1087. In: Wefer, G., Berger, W.H., and Richter, C. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-26 ... Article in Journal/Newspaper Neogloboquadrina pachyderma Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg175
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg175
Joides Resolution
Ocean Drilling Program ODP
Giraudeau, Jacques
Pierre, Catherine
Herve, Laurence
Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
topic_facet Drilling/drill rig
Leg175
Joides Resolution
Ocean Drilling Program ODP
description Planktonic foraminiferal assemblages from the upper Pleistocene part of Hole 1087A (0 to 12.1 meters below seafloor) are investigated to assess the role of global and local climate changes on surface circulation in the southern Benguela region. The benthic stable isotope record indicates that the studied interval is representative of the last four climatic cycles, that is, down to marine isotope Stage (MIS) 12. The species assemblages bear a clear transitional to subpolar character, with Neogloboquadrina pachyderma (d), Globorotalia inflata, and Globigerina bulloides, in order of decreasing abundance, as the dominant taxa. This species association presently characterizes the mixing domain of old upwelled and open ocean waters, seaward of the Benguela upwelling cells. Abundance variation of the dominant foraminiferal species roughly follows a glacial-interglacial pattern down to MIS 8, suggesting an alternation of upwelling strength and associated seaward extension of the belt of upwelled water as a response ... : Supplement to: Giraudeau, Jacques; Pierre, Catherine; Herve, Laurence (2001): A late Quaternary, high-resolution record of planktonic foraminiferal species distribution in the southern Benguela region: Site 1087. In: Wefer, G., Berger, W.H., and Richter, C. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-26 ...
format Article in Journal/Newspaper
author Giraudeau, Jacques
Pierre, Catherine
Herve, Laurence
author_facet Giraudeau, Jacques
Pierre, Catherine
Herve, Laurence
author_sort Giraudeau, Jacques
title Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
title_short Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
title_full Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
title_fullStr Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
title_full_unstemmed Late Quaternary planktonic foraminifera of ODP Hole 175-1087A ...
title_sort late quaternary planktonic foraminifera of odp hole 175-1087a ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.735232
https://doi.pangaea.de/10.1594/PANGAEA.735232
genre Neogloboquadrina pachyderma
Planktonic foraminifera
genre_facet Neogloboquadrina pachyderma
Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/odp.proc.sr.175.225.2001
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73523210.2973/odp.proc.sr.175.225.2001
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