FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2517587411> ?p ?o ?g. }

• W2517587411 endingPage "361" @default.
• W2517587411 startingPage "341" @default.
• W2517587411 abstract "A multi-proxy record based on calcareous plankton, dinocysts, pollen, mineralogy and grain size has been acquired from the “Ideale” section, the portion of Montalbano Jonico succession (Southern Italy) that could host the GSSP for the Middle Pleistocene. The direct correlation between marine and terrestrial proxies provides a valuable indication of atmospheric and oceanic connections. The record shows a distinct climate variability well expressed by the vegetational changes, sediment input into the basin and sea surface–water modifications. Biotic proxies indicate that, during the study interval, periods of prevailing subpolar/transitional surface–water conditions were concurrent with steppe and halophytic vegetation. Erosional processes on the hillslopes and terrigenous supply, during these periods, were likely favored due to reduced arboreal vegetation, as attested to by sediment composition and pollen assemblages. Temperate/subtropical surface water conditions were concomitant with prevalent expansions of thermophilous arboreal plants and moister conditions on land, which likely promoted chemical weathering leading to an enhanced supply of kaolinite and smectite in the basin. A relationship between mineral content and the nature of the outcropping units in the source area, as well as sea-level fluctuations, has also been considered. A well-defined period of polar–subpolar water incursion, ranging from 793.2 ka to 788.1 ka, matches the major expansion of steppic vegetation on land and the increase of terrigenous supply into the basin. It likely represents the local response to North Atlantic ice-rafted debris deposition. Short-lived warming/cooling episodes punctuate the latest part of MIS 20 and are tentatively correlated with analogue climate phases predating MIS 1 inception. Full interglacial conditions of MIS 19c, lasting 10.6 kyr, started at 784.3 ka and were characterized by warm, oligotrophic and stratified surface–waters coupled with forest expansion, suggesting prevalent warm and humid conditions on land. A potential sapropel-like interval is identified within MIS 19c and correlated to i-cycle 74. The MIS 19c/19b transition is marked, at 773.2 ka, by the reestablishment of millennial-scale variability, similarly to North Atlantic marine and ice-core records. The results improve the paleoclimate framework of a Middle Pleistocene reference section and add further insight regarding climate development across MIS 19 and on potential similarities with its closest Holocene analogue." @default.
• W2517587411 created "2016-09-16" @default.
• W2517587411 creator A5006336335 @default.
• W2517587411 creator A5021086145 @default.
• W2517587411 creator A5024937315 @default.
• W2517587411 creator A5033597892 @default.
• W2517587411 creator A5055934445 @default.
• W2517587411 creator A5057409460 @default.
• W2517587411 creator A5062927266 @default.
• W2517587411 creator A5073166910 @default.
• W2517587411 creator A5076021341 @default.
• W2517587411 creator A5085442949 @default.
• W2517587411 date "2016-11-01" @default.
• W2517587411 modified "2023-09-24" @default.
• W2517587411 title "Climate signatures through Marine Isotope Stage 19 in the Montalbano Jonico section (Southern Italy): A land–sea perspective" @default.
• W2517587411 cites W1073777694 @default.
• W2517587411 cites W1600196881 @default.
• W2517587411 cites W1652886781 @default.
• W2517587411 cites W1657962187 @default.
• W2517587411 cites W1667825627 @default.
• W2517587411 cites W1676501496 @default.
• W2517587411 cites W1832154245 @default.
• W2517587411 cites W1890121307 @default.
• W2517587411 cites W1929312068 @default.
• W2517587411 cites W1961220440 @default.
• W2517587411 cites W1966282214 @default.
• W2517587411 cites W1967188805 @default.
• W2517587411 cites W1971879569 @default.
• W2517587411 cites W1972321981 @default.
• W2517587411 cites W1976251153 @default.
• W2517587411 cites W1976403388 @default.
• W2517587411 cites W1977355907 @default.
• W2517587411 cites W1977865990 @default.
• W2517587411 cites W1978250019 @default.
• W2517587411 cites W1978347718 @default.
• W2517587411 cites W1980027739 @default.
• W2517587411 cites W1980352443 @default.
• W2517587411 cites W1980680517 @default.
• W2517587411 cites W1981135957 @default.
• W2517587411 cites W1982734254 @default.
• W2517587411 cites W1985294064 @default.
• W2517587411 cites W1985520359 @default.
• W2517587411 cites W1986785608 @default.
• W2517587411 cites W1988123755 @default.
• W2517587411 cites W1989040762 @default.
• W2517587411 cites W1990111902 @default.
• W2517587411 cites W1991028051 @default.
• W2517587411 cites W1993497033 @default.
• W2517587411 cites W1997869145 @default.
• W2517587411 cites W1997886158 @default.
• W2517587411 cites W2001175847 @default.
• W2517587411 cites W2001675220 @default.
• W2517587411 cites W2001682930 @default.
• W2517587411 cites W2002460650 @default.
• W2517587411 cites W2003477787 @default.
• W2517587411 cites W2005180019 @default.
• W2517587411 cites W2007568126 @default.
• W2517587411 cites W2007709723 @default.
• W2517587411 cites W2012006566 @default.
• W2517587411 cites W2012083531 @default.
• W2517587411 cites W2012223487 @default.
• W2517587411 cites W2014491351 @default.
• W2517587411 cites W2016225258 @default.
• W2517587411 cites W2020715324 @default.
• W2517587411 cites W2022473152 @default.
• W2517587411 cites W2022489877 @default.
• W2517587411 cites W2022898066 @default.
• W2517587411 cites W2024576546 @default.
• W2517587411 cites W2026880003 @default.
• W2517587411 cites W2027515845 @default.
• W2517587411 cites W2032303838 @default.
• W2517587411 cites W2033163352 @default.
• W2517587411 cites W2035427883 @default.
• W2517587411 cites W2035808643 @default.
• W2517587411 cites W2036627780 @default.
• W2517587411 cites W2038461879 @default.
• W2517587411 cites W2040309870 @default.
• W2517587411 cites W2042707373 @default.
• W2517587411 cites W2044921293 @default.
• W2517587411 cites W2047566574 @default.
• W2517587411 cites W2047717614 @default.
• W2517587411 cites W2048160147 @default.
• W2517587411 cites W2048602871 @default.
• W2517587411 cites W2049282716 @default.
• W2517587411 cites W2051147978 @default.
• W2517587411 cites W2052001254 @default.
• W2517587411 cites W2052542639 @default.
• W2517587411 cites W2053743714 @default.
• W2517587411 cites W2056822596 @default.
• W2517587411 cites W2056842509 @default.
• W2517587411 cites W2059010126 @default.
• W2517587411 cites W2062503928 @default.
• W2517587411 cites W2062996546 @default.
• W2517587411 cites W2063124686 @default.
• W2517587411 cites W2063535911 @default.
• W2517587411 cites W2064692729 @default.
• W2517587411 cites W2065927184 @default.
• W2517587411 cites W2066202902 @default.

• next