Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ...
Oxygen and carbon isotope analyses show that the biserial forarniniferal genus Streptochilus, which was originally described from pelagic sediments on the Eauripik Rise and Ontong Java Plateau, lived deep in the upper water column within the oxygen minimum layer. The species of Streptochilus average...
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ftdatacite:10.1594/pangaea.682292 2024-09-15T18:30:52+00:00 Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... Resig, Johanna M Kroopnick, Peter M 1983 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.682292 https://doi.pangaea.de/10.1594/PANGAEA.682292 en eng PANGAEA https://dx.doi.org/10.1016/0377-8398(83)90026-9 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock AGE Sample code/label Epoch Planktic foraminifera zone Globigerinoides sacculifer, δ13C Globigerinoides sacculifer, δ18O Temperature, calculated Globorotalia tumida, δ13C Globorotalia tumida, δ18O Streptochilus globulosum, δ13C Streptochilus globulosum, δ18O Foraminifera, benthic δ13C Foraminifera, benthic δ18O Siphouvigerina sp., δ13C Siphouvigerina sp., δ18O Uvigerina spp., δ13C Uvigerina spp., δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Calculated from stable oxygen isotopes Leg7 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1983 ftdatacite https://doi.org/10.1594/pangaea.68229210.1016/0377-8398(83)90026-9 2024-08-01T10:57:41Z Oxygen and carbon isotope analyses show that the biserial forarniniferal genus Streptochilus, which was originally described from pelagic sediments on the Eauripik Rise and Ontong Java Plateau, lived deep in the upper water column within the oxygen minimum layer. The species of Streptochilus average from 4 to 19% of the foraminiferal assemblages in which benthic forms compose less than 1 or 2%. Specimens of Streptochilus are selectively dissolved when in contact with the bottom water mass. Their rapid evolutionary turnover of less than a few million years and their wide areal distribution in the equatorial Indo-Pacific are indicative of planktonic foraminifera. Aside from usefulness of the species of Streptochilus as stratigraphic indices, these Neogene biserial planktonic foraminifera are potential indices of paleoceanographic stratification. ... : Ages are approximated, Temperature calculation: T (∞C) = 16.5-4.3 * (deltaO18 O3) + 1.4 * (deltaO18 O3)**2, based on the revised paleotemperature equation of Epstein et al. (1953) ... Dataset Planktonic foraminifera DataCite |
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English |
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DEPTH, sediment/rock AGE Sample code/label Epoch Planktic foraminifera zone Globigerinoides sacculifer, δ13C Globigerinoides sacculifer, δ18O Temperature, calculated Globorotalia tumida, δ13C Globorotalia tumida, δ18O Streptochilus globulosum, δ13C Streptochilus globulosum, δ18O Foraminifera, benthic δ13C Foraminifera, benthic δ18O Siphouvigerina sp., δ13C Siphouvigerina sp., δ18O Uvigerina spp., δ13C Uvigerina spp., δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Calculated from stable oxygen isotopes Leg7 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
DEPTH, sediment/rock AGE Sample code/label Epoch Planktic foraminifera zone Globigerinoides sacculifer, δ13C Globigerinoides sacculifer, δ18O Temperature, calculated Globorotalia tumida, δ13C Globorotalia tumida, δ18O Streptochilus globulosum, δ13C Streptochilus globulosum, δ18O Foraminifera, benthic δ13C Foraminifera, benthic δ18O Siphouvigerina sp., δ13C Siphouvigerina sp., δ18O Uvigerina spp., δ13C Uvigerina spp., δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Calculated from stable oxygen isotopes Leg7 Glomar Challenger Deep Sea Drilling Project DSDP Resig, Johanna M Kroopnick, Peter M Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
topic_facet |
DEPTH, sediment/rock AGE Sample code/label Epoch Planktic foraminifera zone Globigerinoides sacculifer, δ13C Globigerinoides sacculifer, δ18O Temperature, calculated Globorotalia tumida, δ13C Globorotalia tumida, δ18O Streptochilus globulosum, δ13C Streptochilus globulosum, δ18O Foraminifera, benthic δ13C Foraminifera, benthic δ18O Siphouvigerina sp., δ13C Siphouvigerina sp., δ18O Uvigerina spp., δ13C Uvigerina spp., δ18O Drilling/drill rig DSDP/ODP/IODP sample designation Isotope ratio mass spectrometry Calculated from stable oxygen isotopes Leg7 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
Oxygen and carbon isotope analyses show that the biserial forarniniferal genus Streptochilus, which was originally described from pelagic sediments on the Eauripik Rise and Ontong Java Plateau, lived deep in the upper water column within the oxygen minimum layer. The species of Streptochilus average from 4 to 19% of the foraminiferal assemblages in which benthic forms compose less than 1 or 2%. Specimens of Streptochilus are selectively dissolved when in contact with the bottom water mass. Their rapid evolutionary turnover of less than a few million years and their wide areal distribution in the equatorial Indo-Pacific are indicative of planktonic foraminifera. Aside from usefulness of the species of Streptochilus as stratigraphic indices, these Neogene biserial planktonic foraminifera are potential indices of paleoceanographic stratification. ... : Ages are approximated, Temperature calculation: T (∞C) = 16.5-4.3 * (deltaO18 O3) + 1.4 * (deltaO18 O3)**2, based on the revised paleotemperature equation of Epstein et al. (1953) ... |
format |
Dataset |
author |
Resig, Johanna M Kroopnick, Peter M |
author_facet |
Resig, Johanna M Kroopnick, Peter M |
author_sort |
Resig, Johanna M |
title |
Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
title_short |
Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
title_full |
Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
title_fullStr |
Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
title_full_unstemmed |
Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) ... |
title_sort |
stable isotope ratios of benthic and planktonic foraminifera from miocene to pliocene sediments of dsdp hole 7-62a on the eauripik rise, pacific ocean (table 1) ... |
publisher |
PANGAEA |
publishDate |
1983 |
url |
https://dx.doi.org/10.1594/pangaea.682292 https://doi.pangaea.de/10.1594/PANGAEA.682292 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1016/0377-8398(83)90026-9 |
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.68229210.1016/0377-8398(83)90026-9 |
_version_ |
1810472409726189568 |