Holocene climate variability of the Western Mediterranean: (Record no. 15064)

MARC details
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fixed length control field 02889nab a2200265 4500
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control field 20231029150803.0
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100 ## - MAIN ENTRY--PERSONAL NAME
Personal name Bazzicalupo, Pietro
245 ## - TITLE STATEMENT
Title Holocene climate variability of the Western Mediterranean:
Sub Title Surface water dynamics inferred from calcareous plankton assemblages/
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Name of publisher, distributor, etc Sage,
Date of publication, distribution, etc 2020.
300 ## - PHYSICAL DESCRIPTION
Pages Vol. 30, issue 5, 2020 ( 691–708 p.).
520 ## - SUMMARY, ETC.
Summary, etc A high-resolution study (centennial scale) has been performed on the calcareous plankton assemblage of the Holocene portion of the Ocean Drilling Program Site 976 (Alboran Sea) with the aim to identify the main changes in the surface water dynamic. The dataset also provided a seasonal foraminiferal sea surface water temperatures (SSTs), estimated using the modern analog technique SIMMAX 28, and it was compared with available geochemical and pollen data at the site. Three main climate shifts were identified as (1) the increase in abundance of Syracosphaera spp. and Turborotalita quinqueloba marks the early Holocene humid phase, during maximum summer insolation and enhanced river runoff. It is concomitant with the expansion of Quercus, supporting high humidity on land. It ends at 8.2 ka, registering a sudden temperature and humidity reduction; (2) the rise in the abundances of Florisphaera profunda and Globorotalia inflata, at ca. 8 ka, indicates the development of the modern geostrophic front, gyre circulation, and of a deep nutricline following the sea-level rise; and (3) the increase of small Gephyrocapsa and Globigerina bulloides at 5.3 ka suggests enhanced nutrient availability in surface waters, related to more persistent wind-induced upwelling conditions. Relatively higher winter SST in the last 3.5 ka favored the increase of Trilobatus sacculifer, likely connected to more stable surface water conditions. Over the main trends, a short-term cyclicity is registered in coccolithophore productivity during the last 8 ka. Short periods of increased productivity are in phase with Atlantic waters inflow, and more arid intervals on land. This cyclicity has been related with periods of positive North Atlantic Oscillation (NAO) circulations. Spectral analysis on coccolithophore productivity confirms the occurrence of millennial-scale cyclicity, suggesting an external (i.e. solar) and an internal (i.e. atmospheric/oceanic) forcing.
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Added Entry Personal Name Maiorano, Patrizia
700 ## - Added Entry Personal Name
Added Entry Personal Name Girone, Angela
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Added Entry Personal Name Marino, Maria
700 ## - Added Entry Personal Name
Added Entry Personal Name Combourieu-Nebout, Nathalie
700 ## - Added Entry Personal Name
Added Entry Personal Name Pelosi, Nicola
700 ## - Added Entry Personal Name
Added Entry Personal Name Salgueiro, Emilia
700 ## - Added Entry Personal Name
Added Entry Personal Name Incarbona, Alessandro
773 0# - HOST ITEM ENTRY
Host Biblionumber 12756
Host Itemnumber 17200
Place, publisher, and date of publication London: Sage Publication Ltd, 2019.
Title Holocene/
International Standard Serial Number 09596836
856 ## - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier https://doi.org/10.1177/0959683619895580
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type E-Journal
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-- 58990
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-- 58991
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-- 51966
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-- 58737
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-- 58992
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-- 58993
942 ## - ADDED ENTRY ELEMENTS (KOHA)
-- ddc

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