Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ...
The middle Miocene delta18O increase represents a fundamental change in the ocean-atmosphere system which, like late Pleistocene climates, may be related to deepwater circulation patterns. There has been some debate concerning the early to early middle Miocene deepwater circulation patterns. Specifi...
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ftdatacite:10.1594/pangaea.728102 2024-09-30T14:44:07+00:00 Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... Wright, James D Miller, Kenneth G Fairbanks, Richard G 1992 application/zip https://dx.doi.org/10.1594/pangaea.728102 https://doi.pangaea.de/10.1594/PANGAEA.728102 en eng PANGAEA https://dx.doi.org/10.1029/92pa00760 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg40 Leg81 Leg82 Leg94 Leg114 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1992 ftdatacite https://doi.org/10.1594/pangaea.72810210.1029/92pa00760 2024-09-02T08:35:09Z The middle Miocene delta18O increase represents a fundamental change in the ocean-atmosphere system which, like late Pleistocene climates, may be related to deepwater circulation patterns. There has been some debate concerning the early to early middle Miocene deepwater circulation patterns. Specifically, recent discussions have focused on the relative roles of Northern Component Water (NCW) production and warm, saline deep water originating in the eastern Tethys. Our time series and time slice reconstructions indicate that NCW and Tethyan outflow water, two relatively warm deepwater masses, were produced from ~20 to 16 Ma. NCW was produced again from 12.5 to 10.5 Ma. Another feature of the early and middle Miocene oceans was the presence of a high delta13C intermediate water mass in the southern hemisphere, which apparently originated in the Southern Ocean. Miocene climates appear to be related directly to deepwater circulation changes. Deep-waters warmed in the early Miocene by ~3°C (?20 to 16 Ma) and ... : Supplement to: Wright, James D; Miller, Kenneth G; Fairbanks, Richard G (1992): Early and Middle Miocene stable isotopes: implications for deepwater circulation and climate. Paleoceanography, 7(3), 357-389 ... Article in Journal/Newspaper Southern Ocean DataCite Fairbanks Southern Ocean |
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Open Polar |
collection |
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op_collection_id |
ftdatacite |
language |
English |
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Drilling/drill rig Leg40 Leg81 Leg82 Leg94 Leg114 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg40 Leg81 Leg82 Leg94 Leg114 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Wright, James D Miller, Kenneth G Fairbanks, Richard G Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
topic_facet |
Drilling/drill rig Leg40 Leg81 Leg82 Leg94 Leg114 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
The middle Miocene delta18O increase represents a fundamental change in the ocean-atmosphere system which, like late Pleistocene climates, may be related to deepwater circulation patterns. There has been some debate concerning the early to early middle Miocene deepwater circulation patterns. Specifically, recent discussions have focused on the relative roles of Northern Component Water (NCW) production and warm, saline deep water originating in the eastern Tethys. Our time series and time slice reconstructions indicate that NCW and Tethyan outflow water, two relatively warm deepwater masses, were produced from ~20 to 16 Ma. NCW was produced again from 12.5 to 10.5 Ma. Another feature of the early and middle Miocene oceans was the presence of a high delta13C intermediate water mass in the southern hemisphere, which apparently originated in the Southern Ocean. Miocene climates appear to be related directly to deepwater circulation changes. Deep-waters warmed in the early Miocene by ~3°C (?20 to 16 Ma) and ... : Supplement to: Wright, James D; Miller, Kenneth G; Fairbanks, Richard G (1992): Early and Middle Miocene stable isotopes: implications for deepwater circulation and climate. Paleoceanography, 7(3), 357-389 ... |
format |
Article in Journal/Newspaper |
author |
Wright, James D Miller, Kenneth G Fairbanks, Richard G |
author_facet |
Wright, James D Miller, Kenneth G Fairbanks, Richard G |
author_sort |
Wright, James D |
title |
Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
title_short |
Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
title_full |
Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
title_fullStr |
Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
title_full_unstemmed |
Stable isotope record of Cibicidoides spp. from early and middle Miocene sediments ... |
title_sort |
stable isotope record of cibicidoides spp. from early and middle miocene sediments ... |
publisher |
PANGAEA |
publishDate |
1992 |
url |
https://dx.doi.org/10.1594/pangaea.728102 https://doi.pangaea.de/10.1594/PANGAEA.728102 |
geographic |
Fairbanks Southern Ocean |
geographic_facet |
Fairbanks Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://dx.doi.org/10.1029/92pa00760 |
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.72810210.1029/92pa00760 |
_version_ |
1811645597682237440 |