FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4282920658> ?p ?o ?g. }

• W4282920658 endingPage "1221" @default.
• W4282920658 startingPage "1207" @default.
• W4282920658 abstract "Abstract The interaction between ocean circulation and ice‐sheet dynamics plays a key role in the Quaternary climate. Compared with the surface and deep regions of the Atlantic Meridional Overturning Circulation (AMOC), the study of intermediate depths during key time periods, such as Heinrich Stadials (HSs), remains poorly documented, especially for the northeast Atlantic. Here we use benthic foraminiferal assemblage data to trace palaeoenvironmental changes from ~32 to 14 ka cal bp at ~1000 m depth in the Bay of Biscay. Our results highlight the high sensitivity of foraminifera, with species‐specific responses, to continental (European Ice Sheet dynamics) and marine (AMOC) forcing factors during the last three HSs. In general, HSs were characterised by the concomitant presence of meso‐oligotrophic and anoxia indicator species and the low abundance of high‐energy indicator species. This confirms an overall sluggish intermediate circulation during the three HSs in the northeast Atlantic. HS1 is distinctive for its abundance of high‐organic flux indicator species during its early phase. This is consistent with the fact that HS1 was by far the most important period of ice‐sheet retreat and meltwater release into the ocean over the studied time interval. Finally, foraminifera depict the mid‐HS2 reventilation event due to regional glacier instabilities." @default.
• W4282920658 created "2022-06-16" @default.
• W4282920658 creator A5009709500 @default.
• W4282920658 creator A5010577513 @default.
• W4282920658 creator A5039115288 @default.
• W4282920658 creator A5049369653 @default.
• W4282920658 creator A5058929466 @default.
• W4282920658 date "2022-06-14" @default.
• W4282920658 modified "2023-10-12" @default.
• W4282920658 title "Intermediate ocean circulation and cryosphere dynamics in the northeast Atlantic during Heinrich Stadials: benthic foraminiferal assemblage response" @default.
• W4282920658 cites W1482146370 @default.
• W4282920658 cites W1572099550 @default.
• W4282920658 cites W1681221880 @default.
• W4282920658 cites W1755662586 @default.
• W4282920658 cites W1859185656 @default.
• W4282920658 cites W1897950478 @default.
• W4282920658 cites W1911743236 @default.
• W4282920658 cites W1933102174 @default.
• W4282920658 cites W1963976762 @default.
• W4282920658 cites W1964202969 @default.
• W4282920658 cites W1965034294 @default.
• W4282920658 cites W1965681998 @default.
• W4282920658 cites W1965811169 @default.
• W4282920658 cites W1968860571 @default.
• W4282920658 cites W1973572242 @default.
• W4282920658 cites W1974416801 @default.
• W4282920658 cites W1974603678 @default.
• W4282920658 cites W1974728582 @default.
• W4282920658 cites W1976550053 @default.
• W4282920658 cites W1977355907 @default.
• W4282920658 cites W1977682658 @default.
• W4282920658 cites W1978704803 @default.
• W4282920658 cites W1980051883 @default.
• W4282920658 cites W1981309347 @default.
• W4282920658 cites W1981818426 @default.
• W4282920658 cites W1983097573 @default.
• W4282920658 cites W1985091074 @default.
• W4282920658 cites W1987207135 @default.
• W4282920658 cites W1987817580 @default.
• W4282920658 cites W1988767988 @default.
• W4282920658 cites W1992977196 @default.
• W4282920658 cites W1994452744 @default.
• W4282920658 cites W1996862213 @default.
• W4282920658 cites W1999094459 @default.
• W4282920658 cites W2000055654 @default.
• W4282920658 cites W2002717773 @default.
• W4282920658 cites W2007257396 @default.
• W4282920658 cites W2007331923 @default.
• W4282920658 cites W2011398650 @default.
• W4282920658 cites W2014565249 @default.
• W4282920658 cites W2016737438 @default.
• W4282920658 cites W2016893305 @default.
• W4282920658 cites W2018516398 @default.
• W4282920658 cites W2019498134 @default.
• W4282920658 cites W2020503094 @default.
• W4282920658 cites W2021564351 @default.
• W4282920658 cites W2021649536 @default.
• W4282920658 cites W2024368861 @default.
• W4282920658 cites W2027680699 @default.
• W4282920658 cites W2027861180 @default.
• W4282920658 cites W2028443916 @default.
• W4282920658 cites W2028556734 @default.
• W4282920658 cites W2029555224 @default.
• W4282920658 cites W2030421281 @default.
• W4282920658 cites W2040200888 @default.
• W4282920658 cites W2040997027 @default.
• W4282920658 cites W2049332465 @default.
• W4282920658 cites W2049760601 @default.
• W4282920658 cites W2051126029 @default.
• W4282920658 cites W2052681566 @default.
• W4282920658 cites W2053129218 @default.
• W4282920658 cites W2053668158 @default.
• W4282920658 cites W2059592586 @default.
• W4282920658 cites W2059598621 @default.
• W4282920658 cites W2060143450 @default.
• W4282920658 cites W2060359957 @default.
• W4282920658 cites W2062620507 @default.
• W4282920658 cites W2064163246 @default.
• W4282920658 cites W2065440175 @default.
• W4282920658 cites W2066755232 @default.
• W4282920658 cites W2067839278 @default.
• W4282920658 cites W2069215153 @default.
• W4282920658 cites W2071611350 @default.
• W4282920658 cites W2073758527 @default.
• W4282920658 cites W2074099824 @default.
• W4282920658 cites W2076827814 @default.
• W4282920658 cites W2076877001 @default.
• W4282920658 cites W2078313230 @default.
• W4282920658 cites W2080775544 @default.
• W4282920658 cites W2081115782 @default.
• W4282920658 cites W2081968403 @default.
• W4282920658 cites W2082243003 @default.
• W4282920658 cites W2083519852 @default.
• W4282920658 cites W2086192317 @default.
• W4282920658 cites W2088086245 @default.
• W4282920658 cites W2088592186 @default.
• W4282920658 cites W2089401146 @default.
• W4282920658 cites W2091672966 @default.

• next