Ocean water temperatures from ODP Site 130-806

Fuente: PANGAEA
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Autores principales: Lear, Caroline H, Coxall, Helen K, Foster, Gavin L, Lunt, Daniel J, Mawbey, Elaine M, Rosenthal, Yair, Sosdian, Sindia M, Thomas, Ellen, Wilson, Paul A
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2021
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author Lear, Caroline H
Coxall, Helen K
Foster, Gavin L
Lunt, Daniel J
Mawbey, Elaine M
Rosenthal, Yair
Sosdian, Sindia M
Thomas, Ellen
Wilson, Paul A
author_facet Lear, Caroline H
Coxall, Helen K
Foster, Gavin L
Lunt, Daniel J
Mawbey, Elaine M
Rosenthal, Yair
Sosdian, Sindia M
Thomas, Ellen
Wilson, Paul A
collection Datos científicos de ciencias marinas y ambientales
contents The dataset compiles reconstructed changes in bottom water temperature and global ice volume from 0 to 17 Ma using δ18O in conjunction with Mg/Ca records of the infaunal benthic foraminifer, O. umbonatus from Ocean Drilling Program (ODP) Site 130-806 (equatorial Pacific; ~2500 m). This dataset covers the middle Miocene to present (17-0 Ma) and has an average temporal resolution of ~0.2 Ma. Application of the new equations to the Site 130-806 record leads to the suggestion that global ice volume was greater than today after the Middle Miocene Climate Transition (~14 Ma). ODP Site 130-806 bottom waters cooled and freshened as the Pacific zonal sea surface temperature gradient increased, and climate cooled through the Pliocene, prior to the Plio‐Pleistocene glaciation of the Northern Hemisphere.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_931013
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Ocean water temperatures from ODP Site 130-806
Lear, Caroline H
Coxall, Helen K
Foster, Gavin L
Lunt, Daniel J
Mawbey, Elaine M
Rosenthal, Yair
Sosdian, Sindia M
Thomas, Ellen
Wilson, Paul A
130-806; AGE; Benthic foraminifera; Bottom water temperature; Calculated (LEAR 2002 Calibration); Calculated (LEAR 2010 Calibration); COMPCORE; Composite Core; Joides Resolution; Leg130; Mg/Ca; North Pacific Ocean; ocean drilling program; ocean temperatures; δ18O, seawater, reconstructed
The dataset compiles reconstructed changes in bottom water temperature and global ice volume from 0 to 17 Ma using δ18O in conjunction with Mg/Ca records of the infaunal benthic foraminifer, O. umbonatus from Ocean Drilling Program (ODP) Site 130-806 (equatorial Pacific; ~2500 m). This dataset covers the middle Miocene to present (17-0 Ma) and has an average temporal resolution of ~0.2 Ma. Application of the new equations to the Site 130-806 record leads to the suggestion that global ice volume was greater than today after the Middle Miocene Climate Transition (~14 Ma). ODP Site 130-806 bottom waters cooled and freshened as the Pacific zonal sea surface temperature gradient increased, and climate cooled through the Pliocene, prior to the Plio‐Pleistocene glaciation of the Northern Hemisphere.
title Ocean water temperatures from ODP Site 130-806
topic 130-806; AGE; Benthic foraminifera; Bottom water temperature; Calculated (LEAR 2002 Calibration); Calculated (LEAR 2010 Calibration); COMPCORE; Composite Core; Joides Resolution; Leg130; Mg/Ca; North Pacific Ocean; ocean drilling program; ocean temperatures; δ18O, seawater, reconstructed
url https://doi.org/10.1594/PANGAEA.931013