Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...

A record of carbon and oxygen isotopes in benthic and planktonic foraminifers has been obtained from the interval corresponding to the last 2.4 m.y. of Site 610, Holes 610 and 610A, with a sample resolution of about 30 kyr. The record from the late Quaternary (<0.9 Ma) shows large amplitudes and...

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Main Authors: Jansen, Eystein, Sejrup, Hans Petter
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1987
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.788583
https://doi.pangaea.de/10.1594/PANGAEA.788583
id ftdatacite:10.1594/pangaea.788583
record_format openpolar
spelling ftdatacite:10.1594/pangaea.788583 2024-09-15T18:25:24+00:00 Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ... Jansen, Eystein Sejrup, Hans Petter 1987 application/zip https://dx.doi.org/10.1594/pangaea.788583 https://doi.pangaea.de/10.1594/PANGAEA.788583 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.94.123.1987 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1987 ftdatacite https://doi.org/10.1594/pangaea.78858310.2973/dsdp.proc.94.123.1987 2024-08-01T10:57:41Z A record of carbon and oxygen isotopes in benthic and planktonic foraminifers has been obtained from the interval corresponding to the last 2.4 m.y. of Site 610, Holes 610 and 610A, with a sample resolution of about 30 kyr. The record from the late Quaternary (<0.9 Ma) shows large amplitudes and high frequencies in oxygen isotopic variation. Prior to 0.9 Ma the isotopic variability record is reduced in amplitude (but not in frequency) compared with the late Quaternary, suggesting lower ice-volume and climatic fluctuations, and higher average eustatic sea level.Left-coiling (L, polar) Neogloboquadrinapachyderma were not found in samples between 1.0 and 2.2 Ma, indicating less influence of polar front migrations in the Northeast Atlantic. Both polar planktonic faunas and larger isotope fluctuations reappear in the lowermost samples (2.3 to 2.4 Ma), pointing toward a period of larger climatic variability in the late Pliocene than in the early Quaternary.The variation in benthic d13C and hence in deep-water ... : Supplement to: Jansen, Eystein; Sejrup, Hans Petter (1987): Stable isotope stratigraphy and amino-acid empimerization for the last 2.4 m.y. at Site 610, Holes 610 and 610A. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 879-888 ... Article in Journal/Newspaper Northeast Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Deep Sea Drilling Project DSDP
spellingShingle Deep Sea Drilling Project DSDP
Jansen, Eystein
Sejrup, Hans Petter
Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
topic_facet Deep Sea Drilling Project DSDP
description A record of carbon and oxygen isotopes in benthic and planktonic foraminifers has been obtained from the interval corresponding to the last 2.4 m.y. of Site 610, Holes 610 and 610A, with a sample resolution of about 30 kyr. The record from the late Quaternary (<0.9 Ma) shows large amplitudes and high frequencies in oxygen isotopic variation. Prior to 0.9 Ma the isotopic variability record is reduced in amplitude (but not in frequency) compared with the late Quaternary, suggesting lower ice-volume and climatic fluctuations, and higher average eustatic sea level.Left-coiling (L, polar) Neogloboquadrinapachyderma were not found in samples between 1.0 and 2.2 Ma, indicating less influence of polar front migrations in the Northeast Atlantic. Both polar planktonic faunas and larger isotope fluctuations reappear in the lowermost samples (2.3 to 2.4 Ma), pointing toward a period of larger climatic variability in the late Pliocene than in the early Quaternary.The variation in benthic d13C and hence in deep-water ... : Supplement to: Jansen, Eystein; Sejrup, Hans Petter (1987): Stable isotope stratigraphy and amino-acid empimerization for the last 2.4 m.y. at Site 610, Holes 610 and 610A. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 879-888 ...
format Article in Journal/Newspaper
author Jansen, Eystein
Sejrup, Hans Petter
author_facet Jansen, Eystein
Sejrup, Hans Petter
author_sort Jansen, Eystein
title Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
title_short Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
title_full Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
title_fullStr Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
title_full_unstemmed Oxygen and carbon isotopic composition of benthic and planktonic foraminifers at DSDP Site 610 ...
title_sort oxygen and carbon isotopic composition of benthic and planktonic foraminifers at dsdp site 610 ...
publisher PANGAEA
publishDate 1987
url https://dx.doi.org/10.1594/pangaea.788583
https://doi.pangaea.de/10.1594/PANGAEA.788583
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_relation https://dx.doi.org/10.2973/dsdp.proc.94.123.1987
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.78858310.2973/dsdp.proc.94.123.1987
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