Silt grain-size analysis of ODP holes from the western equatorial Atlantic ...
Grain-size records of the terrigenous and calcareous silt fraction, preservation of planktic foraminifera, and benthic foraminiferal stable-isotope data (delta13C, delta18O values of C. wuellerstorfi) at ODP Site 927 on the Ceará Rise (5°27.7'N, 44°28.8'W), are used to reconstruct variatio...
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Online Access: | https://dx.doi.org/10.1594/pangaea.736009 https://doi.pangaea.de/10.1594/PANGAEA.736009 |
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ftdatacite:10.1594/pangaea.736009 2024-09-30T14:39:03+00:00 Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... Gröger, Matthias Henrich, Rüdiger Bickert, Torsten 2003 application/zip https://dx.doi.org/10.1594/pangaea.736009 https://doi.pangaea.de/10.1594/PANGAEA.736009 en eng PANGAEA https://dx.doi.org/10.1016/s0025-3227(03)00263-9 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg154 Joides Resolution Geosciences, University of Bremen GeoB Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2003 ftdatacite https://doi.org/10.1594/pangaea.73600910.1016/s0025-3227(03)00263-9 2024-09-02T08:35:09Z Grain-size records of the terrigenous and calcareous silt fraction, preservation of planktic foraminifera, and benthic foraminiferal stable-isotope data (delta13C, delta18O values of C. wuellerstorfi) at ODP Site 927 on the Ceará Rise (5°27.7'N, 44°28.8'W), are used to reconstruct variations in the history of bottom current strength, ventilation, and carbonate corrosiveness of deep waters during the time interval from 0.8 to 0.3 Ma. Glacial periods are characterized by generally smaller mean sizes of the terrigenous sortable silt fraction (mean(SS)), lower delta13C values, and poorer preservation of planktic foraminifera compared to interglacials. This indicates lower bottom current speeds, larger nutrient contents and more corrosive deep water. By contrast, larger mean(SS) sizes, higher delta13C values, and well preserved planktic foraminifera indicate strong circulation and a well ventilated deep-water mass during interglacials. The observed changes are most likely related to the weakening and ... : Supplement to: Gröger, Matthias; Henrich, Rüdiger; Bickert, Torsten (2003): Glacial-interglacial variability in lower North Atlantic deep water: inference from silt grain-size analysis and carbonate preservation in the western equatorial Atlantic. Marine Geology, 201(4), 321-332 ... Article in Journal/Newspaper North Atlantic Deep Water North Atlantic DataCite |
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Open Polar |
collection |
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op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg154 Joides Resolution Geosciences, University of Bremen GeoB Ocean Drilling Program ODP |
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Drilling/drill rig Leg154 Joides Resolution Geosciences, University of Bremen GeoB Ocean Drilling Program ODP Gröger, Matthias Henrich, Rüdiger Bickert, Torsten Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
topic_facet |
Drilling/drill rig Leg154 Joides Resolution Geosciences, University of Bremen GeoB Ocean Drilling Program ODP |
description |
Grain-size records of the terrigenous and calcareous silt fraction, preservation of planktic foraminifera, and benthic foraminiferal stable-isotope data (delta13C, delta18O values of C. wuellerstorfi) at ODP Site 927 on the Ceará Rise (5°27.7'N, 44°28.8'W), are used to reconstruct variations in the history of bottom current strength, ventilation, and carbonate corrosiveness of deep waters during the time interval from 0.8 to 0.3 Ma. Glacial periods are characterized by generally smaller mean sizes of the terrigenous sortable silt fraction (mean(SS)), lower delta13C values, and poorer preservation of planktic foraminifera compared to interglacials. This indicates lower bottom current speeds, larger nutrient contents and more corrosive deep water. By contrast, larger mean(SS) sizes, higher delta13C values, and well preserved planktic foraminifera indicate strong circulation and a well ventilated deep-water mass during interglacials. The observed changes are most likely related to the weakening and ... : Supplement to: Gröger, Matthias; Henrich, Rüdiger; Bickert, Torsten (2003): Glacial-interglacial variability in lower North Atlantic deep water: inference from silt grain-size analysis and carbonate preservation in the western equatorial Atlantic. Marine Geology, 201(4), 321-332 ... |
format |
Article in Journal/Newspaper |
author |
Gröger, Matthias Henrich, Rüdiger Bickert, Torsten |
author_facet |
Gröger, Matthias Henrich, Rüdiger Bickert, Torsten |
author_sort |
Gröger, Matthias |
title |
Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
title_short |
Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
title_full |
Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
title_fullStr |
Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
title_full_unstemmed |
Silt grain-size analysis of ODP holes from the western equatorial Atlantic ... |
title_sort |
silt grain-size analysis of odp holes from the western equatorial atlantic ... |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://dx.doi.org/10.1594/pangaea.736009 https://doi.pangaea.de/10.1594/PANGAEA.736009 |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_relation |
https://dx.doi.org/10.1016/s0025-3227(03)00263-9 |
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.73600910.1016/s0025-3227(03)00263-9 |
_version_ |
1811641594404667392 |