Climate variability of the last 2700 years in the Southern Adriatic Sea: (Record no. 15007)

MARC details
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fixed length control field 02353nab a2200253 4500
005 - DATE & TIME
control field 20231022152756.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 231022b |||||||| |||| 00| 0 eng d
100 ## - MAIN ENTRY--PERSONAL NAME
Personal name Cascella, Antonio
245 ## - TITLE STATEMENT
Title Climate variability of the last 2700 years in the Southern Adriatic Sea:
Sub Title Coccolithophore evidences/
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Name of publisher, distributor, etc Sage,
Date of publication, distribution, etc 2020.
300 ## - PHYSICAL DESCRIPTION
Pages Vol. 30, issue 1, 2020 ( 53–64 p.).
520 ## - SUMMARY, ETC.
Summary, etc New information on palaeoenvironmental conditions over the past ~2700 years in the Central Mediterranean Sea have been acquired through the high-resolution study of calcareous nannofossils preserved in the sediment core SW104-ND14Q recovered in the Southern Adriatic Sea (SAS) at 1013-m water depth. The surface water properties at this open SAS site are sensitive to atmospheric forcing (acting both at local and regional scale) and the North Ionian Sea driven inflowing waters. Our data show a relationship between reworked coccolith abundances, flood frequency across the Southern Alps and the North Atlantic Oscillation (NAO) confirming their value as indicator of runoff/precipitation. Changes in the abundance of the opportunistic (r-strategist) species Emiliania huxleyi and deep dweller taxa Florisphaera profunda were used to reconstruct the upper water column stratification and associated changes in coccolithophorid productivity. The negative correlation between reworked coccoliths and the N-Ratio (r = −0.44; p = 6−7) suggest that fresh water induced stratification is a controlling factor of the SAS coccolithophorid production. High coccolithophorid productivity levels occurred during dry periods and/or time intervals of inflowing salty and nutrient-rich Levantine Intermediate Waters favouring convection while lower levels took place during high freshwater discharge, mainly during the ‘Little Ice Age’ and two centennial scale intervals of weakest NAO around 200 BCE and 500 CE.
700 ## - Added Entry Personal Name
Added Entry Personal Name Bonomo, Sergio
700 ## - Added Entry Personal Name
Added Entry Personal Name Jalali, Bassem
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Added Entry Personal Name Sicre, Marie-Alexandrine
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Added Entry Personal Name Pelosi, Nicola
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Added Entry Personal Name Schmidt, Sabine
700 ## - Added Entry Personal Name
Added Entry Personal Name Lirer, Fabrizio
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/10.1177/0959683619865600
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type E-Journal
100 ## - MAIN ENTRY--PERSONAL NAME
-- 58733
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-- 58734
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-- 58735
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-- 58736
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-- 58737
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-- 58738
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-- 58739
942 ## - ADDED ENTRY ELEMENTS (KOHA)
-- ddc

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