Holocene changes in deep-water circulation of the Western Mediterranean Basin, links to North Atlantic climate variability

dc.contributor.author
Frigola Ferrer, Jaime I.
dc.contributor.author
Cacho Lascorz, Isabel
dc.contributor.author
Herrera, G.
dc.contributor.author
Canals Artigas, Miquel
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Moreno Caballud, Ana
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Amblàs i Novellas, David
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Grimalt Obrador, Joan
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Masqué, Pere
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Esparza, M.
dc.date.issued
2020-05-30T06:54:10Z
dc.date.issued
2020-05-30T06:54:10Z
dc.date.issued
2010
dc.date.issued
2020-05-30T06:54:10Z
dc.identifier
1576-5172
dc.identifier
https://hdl.handle.net/2445/163194
dc.identifier
587958
dc.description.abstract
preliminary results from multicores recovered in the Minorca sediment drift, south of the Western Mediterranean Deep Water formation area, reveal changes in deep-water circulation during the last 2500 yr. Records of grain-size and SST Mg/Ca derived from G. bulloides show oscillations in deep-water current intensities that could be related to cool periods on land, i.e. the Little Ice Age, but also denote some relationship with changes in sea surface salinity likely associated with changes in continental humid conditions.
dc.format
2 p.
dc.format
application/pdf
dc.language
eng
dc.publisher
Sociedad Geológica de España
dc.relation
Reproducció del document publicat a:
dc.relation
Geo-Temas, 2010, vol. 11, p. 43-44
dc.rights
(c) Sociedad Geológica de España, 2010
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
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Geologia submarina
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Fons marins
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Paleoclimatologia
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Paleoceanografia
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Holocè
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Submarine geology
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Ocean bottom
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Paleoclimatology
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Paleoceanography
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Holocene
dc.title
Holocene changes in deep-water circulation of the Western Mediterranean Basin, links to North Atlantic climate variability
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion


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