Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ...
Modern thermohaline circulation plays a role in latitudinal heat transport and in deep-ocean ventilation, yet ocean circulation may have functioned differently during past periods of extreme warmth, such as the Cretaceous. The Late Cretaceous (100-65 Ma) was an important period in the evolution of t...
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ftdatacite:10.1594/pangaea.817120 2023-05-15T17:30:33+02:00 Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... Robinson, Stuart A Vance, Derek 2012 application/zip https://dx.doi.org/10.1594/pangaea.817120 https://doi.pangaea.de/10.1594/PANGAEA.817120 en eng PANGAEA https://dx.doi.org/10.1029/2011pa002240 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.81712010.1029/2011pa002240 2023-04-03T13:11:41Z Modern thermohaline circulation plays a role in latitudinal heat transport and in deep-ocean ventilation, yet ocean circulation may have functioned differently during past periods of extreme warmth, such as the Cretaceous. The Late Cretaceous (100-65 Ma) was an important period in the evolution of the North Atlantic Ocean, characterized by opening ocean gateways, long-term climatic cooling and the cessation of intermittent periods of anoxia (oceanic anoxic events, OAEs). However, how these phenomena relate to deep-water circulation is unclear. We use a proxy for deep-water mass composition (neodymium isotopes; e-Nd) to show that, at North Atlantic ODP Site 1276, deep waters shifted in the early Campanian (~78-83 Ma) from e-Nd values of ~-7 to values of ~-9, consistent with a change in the style of deep-ocean circulation but >10 Myr after a change in bottom water oxygenation conditions. A similar, but more poorly dated, trend exists in e-Nd data from DSDP Site 386. The Campanian e-Nd transition observed in ... : Supplement to: Robinson, Stuart A; Vance, Derek (2012): Widespread and synchronous change in deep-ocean circulation in the North and South Atlantic during the Late Cretaceous. Paleoceanography, 27(1), PA1102 ... Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Vance ENVELOPE(-139.567,-139.567,-75.467,-75.467) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP Robinson, Stuart A Vance, Derek Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
topic_facet |
Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP |
description |
Modern thermohaline circulation plays a role in latitudinal heat transport and in deep-ocean ventilation, yet ocean circulation may have functioned differently during past periods of extreme warmth, such as the Cretaceous. The Late Cretaceous (100-65 Ma) was an important period in the evolution of the North Atlantic Ocean, characterized by opening ocean gateways, long-term climatic cooling and the cessation of intermittent periods of anoxia (oceanic anoxic events, OAEs). However, how these phenomena relate to deep-water circulation is unclear. We use a proxy for deep-water mass composition (neodymium isotopes; e-Nd) to show that, at North Atlantic ODP Site 1276, deep waters shifted in the early Campanian (~78-83 Ma) from e-Nd values of ~-7 to values of ~-9, consistent with a change in the style of deep-ocean circulation but >10 Myr after a change in bottom water oxygenation conditions. A similar, but more poorly dated, trend exists in e-Nd data from DSDP Site 386. The Campanian e-Nd transition observed in ... : Supplement to: Robinson, Stuart A; Vance, Derek (2012): Widespread and synchronous change in deep-ocean circulation in the North and South Atlantic during the Late Cretaceous. Paleoceanography, 27(1), PA1102 ... |
format |
Article in Journal/Newspaper |
author |
Robinson, Stuart A Vance, Derek |
author_facet |
Robinson, Stuart A Vance, Derek |
author_sort |
Robinson, Stuart A |
title |
Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
title_short |
Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
title_full |
Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
title_fullStr |
Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
title_full_unstemmed |
Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A ... |
title_sort |
age model and nd isotope ratios of dsdo hole 43-386 and odp hole 210-1276a ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.817120 https://doi.pangaea.de/10.1594/PANGAEA.817120 |
long_lat |
ENVELOPE(-139.567,-139.567,-75.467,-75.467) |
geographic |
Vance |
geographic_facet |
Vance |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2011pa002240 |
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.81712010.1029/2011pa002240 |
_version_ |
1766127391189499904 |