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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Bibliographic Details
Main Authors: Resig, Johanna M, Kroopnick, Peter M
Format: Dataset
Language:English
Published: PANGAEA 1983
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.682292
https://doi.pangaea.de/10.1594/PANGAEA.682292
id ftdatacite:10.1594/pangaea.682292
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic 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