(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ...
The sediment sequence at Ocean Drilling Program (ODP) Site 910 (556 m water depth) on the Yermak Plateau in the Arctic Ocean features a remarkable "overconsolidated section" from ~19 to 70-95 m below sea floor (m bsf), marked by large increases in bulk density and sediment strength. The OD...
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Online Access: | https://dx.doi.org/10.1594/pangaea.712046 https://doi.pangaea.de/10.1594/PANGAEA.712046 |
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ftdatacite:10.1594/pangaea.712046 2024-09-15T17:53:54+00:00 (Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... Flower, Benjamin P 1997 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.712046 https://doi.pangaea.de/10.1594/PANGAEA.712046 en eng PANGAEA https://dx.doi.org/10.1130/0091-7613(1997)025<0147:osotyp>2.3.co;2 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Depth, top/min Depth, bottom/max Sample code/label Strontium-87/Strontium-86 ratio Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Leg151 Joides Resolution Ocean Drilling Program ODP dataset Dataset 1997 ftdatacite https://doi.org/10.1594/pangaea.71204610.1130/0091-7613(1997)025<0147:osotyp>2.3.co;2 2024-08-01T10:54:59Z The sediment sequence at Ocean Drilling Program (ODP) Site 910 (556 m water depth) on the Yermak Plateau in the Arctic Ocean features a remarkable "overconsolidated section" from ~19 to 70-95 m below sea floor (m bsf), marked by large increases in bulk density and sediment strength. The ODP Leg 151 Shipboard Scientific Party interpreted the overconsolidated section to be caused by (1) grounding of a marine-based ice sheet, derived from Svalbard and perhaps the Barents Sea ice sheet, and/or (2) coarser-grained glacial sedimentation, which allowed increased compaction. Here I present planktonic foraminiferal d18O data based on Neogloboquadrina pachyderma (sinistrally coiling) that date the termination of overconsolidation near the boundary between isotope stages 16 and 17 (ca. 660 ka). No evidence is found for coarser grained sedimentation, because lithic fragments >150 µm exhibit similar mean concentrations throughout the upper 24.5 m bsf. The overconsolidated section may reflect more extensive ice-sheet ... : Values normalized to NBS987 (National Bureau of Standards) value of 0.710248. ... Dataset Arctic Ocean Barents Sea Foraminifera* Ice Sheet Neogloboquadrina pachyderma Sea ice Svalbard Yermak plateau DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Depth, top/min Depth, bottom/max Sample code/label Strontium-87/Strontium-86 ratio Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Leg151 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Depth, top/min Depth, bottom/max Sample code/label Strontium-87/Strontium-86 ratio Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Leg151 Joides Resolution Ocean Drilling Program ODP Flower, Benjamin P (Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
topic_facet |
Depth, top/min Depth, bottom/max Sample code/label Strontium-87/Strontium-86 ratio Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Leg151 Joides Resolution Ocean Drilling Program ODP |
description |
The sediment sequence at Ocean Drilling Program (ODP) Site 910 (556 m water depth) on the Yermak Plateau in the Arctic Ocean features a remarkable "overconsolidated section" from ~19 to 70-95 m below sea floor (m bsf), marked by large increases in bulk density and sediment strength. The ODP Leg 151 Shipboard Scientific Party interpreted the overconsolidated section to be caused by (1) grounding of a marine-based ice sheet, derived from Svalbard and perhaps the Barents Sea ice sheet, and/or (2) coarser-grained glacial sedimentation, which allowed increased compaction. Here I present planktonic foraminiferal d18O data based on Neogloboquadrina pachyderma (sinistrally coiling) that date the termination of overconsolidation near the boundary between isotope stages 16 and 17 (ca. 660 ka). No evidence is found for coarser grained sedimentation, because lithic fragments >150 µm exhibit similar mean concentrations throughout the upper 24.5 m bsf. The overconsolidated section may reflect more extensive ice-sheet ... : Values normalized to NBS987 (National Bureau of Standards) value of 0.710248. ... |
format |
Dataset |
author |
Flower, Benjamin P |
author_facet |
Flower, Benjamin P |
author_sort |
Flower, Benjamin P |
title |
(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
title_short |
(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
title_full |
(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
title_fullStr |
(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
title_full_unstemmed |
(Table 1) Strontium isotope ratios (87Sr/86Sr) of Neogloboquadrina pachyderma (sinistrally coiling) tests from ODP Hole 151-910A ... |
title_sort |
(table 1) strontium isotope ratios (87sr/86sr) of neogloboquadrina pachyderma (sinistrally coiling) tests from odp hole 151-910a ... |
publisher |
PANGAEA |
publishDate |
1997 |
url |
https://dx.doi.org/10.1594/pangaea.712046 https://doi.pangaea.de/10.1594/PANGAEA.712046 |
genre |
Arctic Ocean Barents Sea Foraminifera* Ice Sheet Neogloboquadrina pachyderma Sea ice Svalbard Yermak plateau |
genre_facet |
Arctic Ocean Barents Sea Foraminifera* Ice Sheet Neogloboquadrina pachyderma Sea ice Svalbard Yermak plateau |
op_relation |
https://dx.doi.org/10.1130/0091-7613(1997)025<0147:osotyp>2.3.co;2 |
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.71204610.1130/0091-7613(1997)025<0147:osotyp>2.3.co;2 |
_version_ |
1810430008272879616 |