Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...

Seawater 187Os/188Os ratios for the Middle Miocene were reconstructed by measuring the 187Os/188Os ratios of metalliferous carbonates from the Pacific (DSDP 598) and Atlantic (DSDP 521) oceans. Atlantic and Pacific 187Os/188Os measurements are nearly indistinguishable and are consistent with previou...

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Main Authors: Reusch, Douglas N, Ravizza, Gregory E, Maasch, Kirk A, Wright, James D
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1998
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.711533
https://doi.pangaea.de/10.1594/PANGAEA.711533
id ftdatacite:10.1594/pangaea.711533
record_format openpolar
spelling ftdatacite:10.1594/pangaea.711533 2024-09-30T14:36:40+00:00 Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ... Reusch, Douglas N Ravizza, Gregory E Maasch, Kirk A Wright, James D 1998 application/zip https://dx.doi.org/10.1594/pangaea.711533 https://doi.pangaea.de/10.1594/PANGAEA.711533 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(98)00082-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg73 Leg92 Glomar Challenger Deep Sea Drilling Project DSDP Collection Supplementary Publication Series of Datasets article 1998 ftdatacite https://doi.org/10.1594/pangaea.71153310.1016/s0012-821x(98)00082-x 2024-09-02T08:40:50Z Seawater 187Os/188Os ratios for the Middle Miocene were reconstructed by measuring the 187Os/188Os ratios of metalliferous carbonates from the Pacific (DSDP 598) and Atlantic (DSDP 521) oceans. Atlantic and Pacific 187Os/188Os measurements are nearly indistinguishable and are consistent with previously published Os isotope records from Pacific cores. The Atlantic data reported here provide the first direct evidence that the long-term sedimentary 187Os/188Os record reflects whole-ocean changes in the Os isotopic composition of seawater. The Pacific and the Atlantic Os measurements confirm a long-term 0.01/Myr increase in marine 187Os/188Os ratios that began no later than 16 Ma. The beginning of the Os isotopic increase coincided with a decrease in the rate of increase of marine 87Sr/86Sr ratios at 16 Ma. A large increase of 1 per mil in benthic foraminiferal delta18O values, interpreted to reflect global cooling and ice sheet growth, began approximately 1 million years later at 14.8 Ma, and the long-term ... : Supplement to: Reusch, Douglas N; Ravizza, Gregory E; Maasch, Kirk A; Wright, James D (1998): Miocene seawater 187Os/188Os ratios inferred from metalliferous carbonates. Earth and Planetary Science Letters, 160(1-2), 163-178 ... Article in Journal/Newspaper Ice Sheet DataCite Pacific
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg73
Leg92
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg73
Leg92
Glomar Challenger
Deep Sea Drilling Project DSDP
Reusch, Douglas N
Ravizza, Gregory E
Maasch, Kirk A
Wright, James D
Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
topic_facet Drilling/drill rig
Leg73
Leg92
Glomar Challenger
Deep Sea Drilling Project DSDP
description Seawater 187Os/188Os ratios for the Middle Miocene were reconstructed by measuring the 187Os/188Os ratios of metalliferous carbonates from the Pacific (DSDP 598) and Atlantic (DSDP 521) oceans. Atlantic and Pacific 187Os/188Os measurements are nearly indistinguishable and are consistent with previously published Os isotope records from Pacific cores. The Atlantic data reported here provide the first direct evidence that the long-term sedimentary 187Os/188Os record reflects whole-ocean changes in the Os isotopic composition of seawater. The Pacific and the Atlantic Os measurements confirm a long-term 0.01/Myr increase in marine 187Os/188Os ratios that began no later than 16 Ma. The beginning of the Os isotopic increase coincided with a decrease in the rate of increase of marine 87Sr/86Sr ratios at 16 Ma. A large increase of 1 per mil in benthic foraminiferal delta18O values, interpreted to reflect global cooling and ice sheet growth, began approximately 1 million years later at 14.8 Ma, and the long-term ... : Supplement to: Reusch, Douglas N; Ravizza, Gregory E; Maasch, Kirk A; Wright, James D (1998): Miocene seawater 187Os/188Os ratios inferred from metalliferous carbonates. Earth and Planetary Science Letters, 160(1-2), 163-178 ...
format Article in Journal/Newspaper
author Reusch, Douglas N
Ravizza, Gregory E
Maasch, Kirk A
Wright, James D
author_facet Reusch, Douglas N
Ravizza, Gregory E
Maasch, Kirk A
Wright, James D
author_sort Reusch, Douglas N
title Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
title_short Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
title_full Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
title_fullStr Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
title_full_unstemmed Isotope ratios of osmiun, carbon and oxygen of Miocene sediments and benthic foraminifera ...
title_sort isotope ratios of osmiun, carbon and oxygen of miocene sediments and benthic foraminifera ...
publisher PANGAEA
publishDate 1998
url https://dx.doi.org/10.1594/pangaea.711533
https://doi.pangaea.de/10.1594/PANGAEA.711533
geographic Pacific
geographic_facet Pacific
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://dx.doi.org/10.1016/s0012-821x(98)00082-x
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.71153310.1016/s0012-821x(98)00082-x
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