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• W1589384225 abstract "[1] The multidisciplinary study of planktic and benthic foraminifera, alkenone SST, and O and C stable isotope records allowed reconstruction of the paleoenvironmental history of the central Adriatic basin over the last 360 ka B.P. In general, the main paleoclimatic changes documented in the central Adriatic appear in phase with climate change in the North Atlantic realm, except for intervals which correspond to the deposition of sapropel levels in the eastern Mediterranean. In particular, the interval between Marine Isotope Stage (MIS) 7.5 and MIS 5 appears to be strongly influenced by the monsoonal regime. The comparison with other Mediterranean records also suggests that the Adriatic Basin was affected by very low sea surface temperature (SST) (down to 2°C for MIS 2) during glacial intervals, which is uncommon for the Mediterranean Basin. In addition, the SST record indicates that this basin was unable to maintain warm interglacial/interstadial conditions for durations similar to the western Mediterranean. This fact can be explained by the landlocked position and shallow depth of this basin, which make it particularly exposed to atmospheric forcing (e.g., Siberian High) and to the strong influence of the nearby landmass during glacial intervals, producing a lag in the demise of glacial intervals. Moreover, the progressively higher values of the δ18O records of glacial intervals, alongside the SST record and the foraminifera assemblage, imply an increasing impact of the formation of cold and dense water since the penultimate glacial." @default.
• W1589384225 created "2016-06-24" @default.
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• W1589384225 date "2008-03-01" @default.
• W1589384225 modified "2023-10-14" @default.
• W1589384225 title "Climatic cycles as expressed in sediments of the PROMESS1 borehole PRAD1-2, central Adriatic, for the last 370 ka: 2. Paleoenvironmental evolution" @default.
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• W1589384225 cites W1657962187 @default.
• W1589384225 cites W1919635784 @default.
• W1589384225 cites W1960757806 @default.
• W1589384225 cites W1965430736 @default.
• W1589384225 cites W1968227109 @default.
• W1589384225 cites W1971369540 @default.
• W1589384225 cites W1972298334 @default.
• W1589384225 cites W1975221307 @default.
• W1589384225 cites W1978347718 @default.
• W1589384225 cites W1980055870 @default.
• W1589384225 cites W1981709236 @default.
• W1589384225 cites W1982734254 @default.
• W1589384225 cites W1983526579 @default.
• W1589384225 cites W1984963091 @default.
• W1589384225 cites W1985475097 @default.
• W1589384225 cites W1986363924 @default.
• W1589384225 cites W1986655331 @default.
• W1589384225 cites W1996302852 @default.
• W1589384225 cites W1997582493 @default.
• W1589384225 cites W1998311555 @default.
• W1589384225 cites W2003885809 @default.
• W1589384225 cites W2006914011 @default.
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• W1589384225 cites W2008596475 @default.
• W1589384225 cites W2008875043 @default.
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• W1589384225 cites W2015515846 @default.
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• W1589384225 cites W2026935997 @default.
• W1589384225 cites W2028721282 @default.
• W1589384225 cites W2036503315 @default.
• W1589384225 cites W2041905636 @default.
• W1589384225 cites W2046727032 @default.
• W1589384225 cites W2047065728 @default.
• W1589384225 cites W2049144205 @default.
• W1589384225 cites W2057996409 @default.
• W1589384225 cites W2058184002 @default.
• W1589384225 cites W2058451620 @default.
• W1589384225 cites W2066755232 @default.
• W1589384225 cites W2073675853 @default.
• W1589384225 cites W2076198715 @default.
• W1589384225 cites W2077686034 @default.
• W1589384225 cites W2078167754 @default.
• W1589384225 cites W2080912283 @default.
• W1589384225 cites W2083519852 @default.
• W1589384225 cites W2086474520 @default.
• W1589384225 cites W2091284813 @default.
• W1589384225 cites W2094948284 @default.
• W1589384225 cites W2096341304 @default.
• W1589384225 cites W2101665356 @default.
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• W1589384225 cites W2135719445 @default.
• W1589384225 cites W2138990589 @default.
• W1589384225 cites W2142579039 @default.
• W1589384225 cites W2146159291 @default.
• W1589384225 cites W2146605432 @default.
• W1589384225 cites W2152146490 @default.
• W1589384225 cites W2154251676 @default.
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• W1589384225 cites W2155234362 @default.
• W1589384225 cites W2158831232 @default.
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• W1589384225 cites W2280624662 @default.
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• W1589384225 doi "https://doi.org/10.1029/2007gc001785" @default.
• W1589384225 hasPublicationYear "2008" @default.
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