(Table 1) Age determination of sediment core MD99-2343

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Autores principales: Sierro, Francisco Javier, Hodell, David A, Curtis, Jason H, Flores, José-Abel, Reguera, Maria Isabel, Colmenero-Hidalgo, Elena, Bárcena, María Angeles, Grimalt, Joan O, Cacho, Isabel, Frigola, Jaime, Canals, Miquel
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2005
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author Sierro, Francisco Javier
Hodell, David A
Curtis, Jason H
Flores, José-Abel
Reguera, Maria Isabel
Colmenero-Hidalgo, Elena
Bárcena, María Angeles
Grimalt, Joan O
Cacho, Isabel
Frigola, Jaime
Canals, Miquel
author_facet Sierro, Francisco Javier
Hodell, David A
Curtis, Jason H
Flores, José-Abel
Reguera, Maria Isabel
Colmenero-Hidalgo, Elena
Bárcena, María Angeles
Grimalt, Joan O
Cacho, Isabel
Frigola, Jaime
Canals, Miquel
collection Datos científicos de ciencias marinas y ambientales
contents Down-core samples of planktonic and benthic foraminifera were analyzed for oxygen and carbon isotopes in International Marine Past Global Changes Study (IMAGES) core MD99-2343 in order to study the interactions between climate change in the Northern Hemisphere and the western Mediterranean thermohaline circulation at times of Heinrich events (HE). Our results confirm the antiphase correlation between enhanced North Atlantic Deep Water formation and low ventilation in the Mediterranean. However, this study reveals that this antiphase relationship in deepwater formation between the North Atlantic and Mediterranean was interrupted during times of HE when the injection of large volumes of water from melting icebergs reached the entrance to the Mediterranean. These events, which lasted less than 1000 years, are represented by pronounced decreases in both planktonic d18O and benthic d13C signals. Lower salinities of Mediterranean surface water resulted in a slowdown of western Mediterranean deepwater overturn even though cold sea surface temperatures and drier climate should have resulted in enhanced deepwater formation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_837083
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age determination of sediment core MD99-2343
Sierro, Francisco Javier
Hodell, David A
Curtis, Jason H
Flores, José-Abel
Reguera, Maria Isabel
Colmenero-Hidalgo, Elena
Bárcena, María Angeles
Grimalt, Joan O
Cacho, Isabel
Frigola, Jaime
Canals, Miquel
98; Age, 14C AMS; Age, comment; Age, dated; Age, dated, standard deviation; Calendar age; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES V; Marion Dufresne (1995); MD114; MD99-2343; North Minorca
Down-core samples of planktonic and benthic foraminifera were analyzed for oxygen and carbon isotopes in International Marine Past Global Changes Study (IMAGES) core MD99-2343 in order to study the interactions between climate change in the Northern Hemisphere and the western Mediterranean thermohaline circulation at times of Heinrich events (HE). Our results confirm the antiphase correlation between enhanced North Atlantic Deep Water formation and low ventilation in the Mediterranean. However, this study reveals that this antiphase relationship in deepwater formation between the North Atlantic and Mediterranean was interrupted during times of HE when the injection of large volumes of water from melting icebergs reached the entrance to the Mediterranean. These events, which lasted less than 1000 years, are represented by pronounced decreases in both planktonic d18O and benthic d13C signals. Lower salinities of Mediterranean surface water resulted in a slowdown of western Mediterranean deepwater overturn even though cold sea surface temperatures and drier climate should have resulted in enhanced deepwater formation.
title (Table 1) Age determination of sediment core MD99-2343
topic 98; Age, 14C AMS; Age, comment; Age, dated; Age, dated, standard deviation; Calendar age; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES V; Marion Dufresne (1995); MD114; MD99-2343; North Minorca
url https://doi.org/10.1594/PANGAEA.837083