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• W2534429609 abstract "Abstract A 25 m-thick outcrop section exposed at Torre Mucchia, on the sea-cliff north of Ortona, eastern central Italy, comprises a rare Middle Pleistocene succession of shallow-water and paralic sediments along the western Adriatic Sea. An integrated study of the section, including facies and microfacies analyses, and characterization of paleobiological associations (mollusks, fishes, ostracods, foraminifers and pollen), enable a detailed reconstruction of the paleoenvironmental and paleoclimatic conditions during deposition. The shallow-water deposits include a transgressive, deepening- and fining-upward shoreface to offshore-transition facies succession overlain by a regressive shoreface-foreshore sandstone body with an erosive base and a rooted and pedogenically altered horizon at the top that imply deposition during sea-level fall. This forced regressive unit is overlain by paralic strata forming a transgressive succession comprising palustrine carbonates and back-barrier lagoonal mudstones. The palustrine carbonates exhibit some of the typical features encountered in palustrine limestones deposited within seasonal freshwater wetlands (marl prairies). Following the sea-level rising trend, the freshwater marshes were abruptly replaced by a barrier-lagoon system that allowed deposition of the overlying mud-rich unit. Within these deposits, the faunal assemblages are consistent with a low-energy brackish environment characterized by a relatively high degree of confinement. The pollen record documents the development of open forest vegetation dominated by Pinus and accompanied by a number of mesophilous and thermophilous tree taxa, whose composition supports a tentative correlation with Marine Oxygen Isotope Stage 17. The new pollen record from Torre Mucchia improves our understanding of the vegetation development in the Italian Peninsula during the Middle Pleistocene and sheds new light on the role played by the most marked glacial periods in determining the history of tree taxa." @default.
• W2534429609 created "2016-10-28" @default.
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• W2534429609 date "2016-11-01" @default.
• W2534429609 modified "2023-09-30" @default.
• W2534429609 title "Sedimentology, faunal content and pollen record of Middle Pleistocene palustrine and lagoonal sediments from the Peri-Adriatic basin, Abruzzi, eastern central Italy" @default.
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• W2534429609 cites W1805070800 @default.
• W2534429609 cites W1898751829 @default.
• W2534429609 cites W1964919295 @default.
• W2534429609 cites W1971383041 @default.
• W2534429609 cites W1972960870 @default.
• W2534429609 cites W1978909173 @default.
• W2534429609 cites W1988559035 @default.
• W2534429609 cites W1994160242 @default.
• W2534429609 cites W1995854523 @default.
• W2534429609 cites W2013488210 @default.
• W2534429609 cites W2014090954 @default.
• W2534429609 cites W2014836091 @default.
• W2534429609 cites W2015727709 @default.
• W2534429609 cites W2018030188 @default.
• W2534429609 cites W2022864445 @default.
• W2534429609 cites W2025342239 @default.
• W2534429609 cites W2027773213 @default.
• W2534429609 cites W2031787194 @default.
• W2534429609 cites W2032891138 @default.
• W2534429609 cites W2033684032 @default.
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• W2534429609 cites W2037671020 @default.
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• W2534429609 cites W2044550285 @default.
• W2534429609 cites W2046121361 @default.
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• W2534429609 cites W2055537723 @default.
• W2534429609 cites W2055786492 @default.
• W2534429609 cites W2056211447 @default.
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• W2534429609 cites W2063946634 @default.
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• W2534429609 cites W2067894630 @default.
• W2534429609 cites W2072986148 @default.
• W2534429609 cites W2075040969 @default.
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• W2534429609 doi "https://doi.org/10.1016/j.yqres.2016.08.003" @default.
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