Nannofossil, alkenone and oxygen isotopic data from sediment core HER-GC-T1

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Autores principales: Ausín, Blanca, Flores, José Abel, Sierro, Francisco Javier, Cacho, Isabel, Hernández-Almeida, Iván, Martrat, Belén, Grimalt, Joan O
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2018
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author Ausín, Blanca
Flores, José Abel
Sierro, Francisco Javier
Cacho, Isabel
Hernández-Almeida, Iván
Martrat, Belén
Grimalt, Joan O
author_facet Ausín, Blanca
Flores, José Abel
Sierro, Francisco Javier
Cacho, Isabel
Hernández-Almeida, Iván
Martrat, Belén
Grimalt, Joan O
collection Datos científicos de ciencias marinas y ambientales
contents High-resolution paleoproductivity variations have been reconstructed in a productive cell from core HER-GC-T1 in the Alboran Sea for the Holocene. Fossil coccolithophore assemblages have been studied along with the Uk′37-estimated sea surface temperature (SST) and oxygen isotope records. The appearance of this cell is suggested at 7.7 ka cal. BP and was linked to the establishment of the western anti-cyclonic gyre. From that time until the present, the nannofossil accumulation rate of Florisphaera profunda has revealed successive episodes of weakening and strengthening of upwelling conditions in the Alboran Sea that have been simultaneous to changes in Western Mediterranean Deep Water (WMDW) formation in the Gulf of Lions.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_895679
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Nannofossil, alkenone and oxygen isotopic data from sediment core HER-GC-T1
Ausín, Blanca
Flores, José Abel
Sierro, Francisco Javier
Cacho, Isabel
Hernández-Almeida, Iván
Martrat, Belén
Grimalt, Joan O
Alboran Sea; GC; Gravity corer; HER_GC_T1; HERMESIONE; Hespérides
High-resolution paleoproductivity variations have been reconstructed in a productive cell from core HER-GC-T1 in the Alboran Sea for the Holocene. Fossil coccolithophore assemblages have been studied along with the Uk′37-estimated sea surface temperature (SST) and oxygen isotope records. The appearance of this cell is suggested at 7.7 ka cal. BP and was linked to the establishment of the western anti-cyclonic gyre. From that time until the present, the nannofossil accumulation rate of Florisphaera profunda has revealed successive episodes of weakening and strengthening of upwelling conditions in the Alboran Sea that have been simultaneous to changes in Western Mediterranean Deep Water (WMDW) formation in the Gulf of Lions.
title Nannofossil, alkenone and oxygen isotopic data from sediment core HER-GC-T1
topic Alboran Sea; GC; Gravity corer; HER_GC_T1; HERMESIONE; Hespérides
url https://doi.org/10.1594/PANGAEA.895679