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Bibliographic Details
Main Authors: Català, Albert, Cacho, Isabel, Frigola, Jaime, Pena, Leopoldo D, Lirer, Fabrizio
Format: Dataset Open Access
Language:en
Published: PANGAEA 2019
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Online Access:https://doi.org/10.1594/PANGAEA.901667
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author Català, Albert
Cacho, Isabel
Frigola, Jaime
Pena, Leopoldo D
Lirer, Fabrizio
author_facet Català, Albert
Cacho, Isabel
Frigola, Jaime
Pena, Leopoldo D
Lirer, Fabrizio
collection Datos científicos de ciencias marinas y ambientales
contents All data are based on the planktonic foraminifera Globigerina bulloides. SST are based on Mg/Ca ratios converted to SST by applying the calibration from Cisneros et al. (2016, doi:10.5194/cp-12-849-2016). Since this calibration was performed on non-reductive cleaned samples and, the Mg/Ca ratios from ALB-2 and MD99-2343 cores were obtained with the full reductive cleaning procedure, Mg/Ca ratios were increased by 12% prior to the calibration application. δ18O are also based in the same planktonic foraminifera Globigerina bulloides. ALB-2 record: A new deglacial and Holocene sea surface temperature (SST) and δ18O reconstructions are presented for the Alboran Sea (western Mediterranean) with its age-model. MD99-2343: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Menorca Drift (western Mediterranean). The age-model has been improved from the originally published by Frigola et al. (2007, doi:10.1029/2006PA001307) for the last 17 kyr. MD95-2043: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Alboran Sea (western Mediterranean).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_901667
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Deglacial and Holocene sea surface temperature (SST) and δ18O reconstruction from the western Mediterranean Sea
Català, Albert
Cacho, Isabel
Frigola, Jaime
Pena, Leopoldo D
Lirer, Fabrizio
Alboran Sea; Holocene; Mediterranean Sea; Sea Surface Tempertures; Stable isotopes
All data are based on the planktonic foraminifera Globigerina bulloides. SST are based on Mg/Ca ratios converted to SST by applying the calibration from Cisneros et al. (2016, doi:10.5194/cp-12-849-2016). Since this calibration was performed on non-reductive cleaned samples and, the Mg/Ca ratios from ALB-2 and MD99-2343 cores were obtained with the full reductive cleaning procedure, Mg/Ca ratios were increased by 12% prior to the calibration application. δ18O are also based in the same planktonic foraminifera Globigerina bulloides. ALB-2 record: A new deglacial and Holocene sea surface temperature (SST) and δ18O reconstructions are presented for the Alboran Sea (western Mediterranean) with its age-model. MD99-2343: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Menorca Drift (western Mediterranean). The age-model has been improved from the originally published by Frigola et al. (2007, doi:10.1029/2006PA001307) for the last 17 kyr. MD95-2043: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Alboran Sea (western Mediterranean).
title Deglacial and Holocene sea surface temperature (SST) and δ18O reconstruction from the western Mediterranean Sea
topic Alboran Sea; Holocene; Mediterranean Sea; Sea Surface Tempertures; Stable isotopes
url https://doi.org/10.1594/PANGAEA.901667