FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2066239714> ?p ?o ?g. }

• W2066239714 endingPage "1492" @default.
• W2066239714 startingPage "1476" @default.
• W2066239714 abstract "Ocean circulation changes along the continental shelf of the Nordic and Barents Seas have been investigated in order to reconstruct regional changes in the inflow of Atlantic Water (AW) through the last 16,000 calibrated (cal) years (yr) B.P. We have selected five time-slices representing the late glacial (16,000–15,000 cal yr B.P.), the Bølling-Allerød warm interstadials (14,500–13,500 cal yr B.P.), the Younger Dryas cold stadial (12,500–11,500 cal yr B.P.), the early Holocene (9500–7500 cal yr B.P.) and the late Holocene (4000–2000 cal yr B.P.). Twelve previously published records of the distribution of benthic foraminifera faunas and ice-rafted debris have been compiled. The earliest sign of Atlantic Water inflow was recorded at the northern Iceland shelf at 16,000–15,000 cal yr B.P. The inflow of warm AW to the Nordic Seas shelf has been persistent since, but with variable strength and geographic pattern. An apparent zonal seesaw pattern in the strength of the Norwegian Atlantic Current (NwAC) and the Irminger Current (IC) during the late glacial, Bølling-Allerød and Younger Dryas periods was found. During the Holocene, no zonal differences in the inflows of NwAC and IC were found. A strong meridional gradient with warmer conditions at lower latitudes and relatively cold conditions at high northern latitudes existed." @default.
• W2066239714 created "2016-06-24" @default.
• W2066239714 creator A5006719258 @default.
• W2066239714 creator A5033322256 @default.
• W2066239714 creator A5041428463 @default.
• W2066239714 creator A5051823963 @default.
• W2066239714 creator A5060191244 @default.
• W2066239714 creator A5087017093 @default.
• W2066239714 date "2008-08-01" @default.
• W2066239714 modified "2023-10-07" @default.
• W2066239714 title "Time-slice reconstructions of ocean circulation changes on the continental shelf in the Nordic and Barents Seas during the last 16,000 cal yr B.P." @default.
• W2066239714 cites W1480882029 @default.
• W2066239714 cites W1484803647 @default.
• W2066239714 cites W1580202324 @default.
• W2066239714 cites W1909880476 @default.
• W2066239714 cites W1963483128 @default.
• W2066239714 cites W1965034294 @default.
• W2066239714 cites W1967286558 @default.
• W2066239714 cites W1971239741 @default.
• W2066239714 cites W1971250306 @default.
• W2066239714 cites W1974231217 @default.
• W2066239714 cites W1976840776 @default.
• W2066239714 cites W1982002268 @default.
• W2066239714 cites W1983162443 @default.
• W2066239714 cites W1986513960 @default.
• W2066239714 cites W1987337564 @default.
• W2066239714 cites W1987817580 @default.
• W2066239714 cites W1988196896 @default.
• W2066239714 cites W1990032129 @default.
• W2066239714 cites W2002517276 @default.
• W2066239714 cites W2002976815 @default.
• W2066239714 cites W2003534383 @default.
• W2066239714 cites W2010357033 @default.
• W2066239714 cites W2021303842 @default.
• W2066239714 cites W2027861180 @default.
• W2066239714 cites W2028671122 @default.
• W2066239714 cites W2029830870 @default.
• W2066239714 cites W2034639312 @default.
• W2066239714 cites W2036890859 @default.
• W2066239714 cites W2038848503 @default.
• W2066239714 cites W2039819271 @default.
• W2066239714 cites W2040564336 @default.
• W2066239714 cites W2045798746 @default.
• W2066239714 cites W2052318413 @default.
• W2066239714 cites W2053862746 @default.
• W2066239714 cites W2054410181 @default.
• W2066239714 cites W2061358089 @default.
• W2066239714 cites W2061658481 @default.
• W2066239714 cites W2062139129 @default.
• W2066239714 cites W2065963875 @default.
• W2066239714 cites W2066755232 @default.
• W2066239714 cites W2073893467 @default.
• W2066239714 cites W2074063375 @default.
• W2066239714 cites W2075604832 @default.
• W2066239714 cites W2076938907 @default.
• W2066239714 cites W2078863693 @default.
• W2066239714 cites W2081553192 @default.
• W2066239714 cites W2081801195 @default.
• W2066239714 cites W2088209548 @default.
• W2066239714 cites W2089193029 @default.
• W2066239714 cites W2091347044 @default.
• W2066239714 cites W2094302854 @default.
• W2066239714 cites W2095743368 @default.
• W2066239714 cites W2095910031 @default.
• W2066239714 cites W2102002872 @default.
• W2066239714 cites W2105163876 @default.
• W2066239714 cites W2106538606 @default.
• W2066239714 cites W2114919313 @default.
• W2066239714 cites W2125613162 @default.
• W2066239714 cites W2151352254 @default.
• W2066239714 cites W2158588727 @default.
• W2066239714 cites W2158672058 @default.
• W2066239714 cites W2166972083 @default.
• W2066239714 cites W2280624662 @default.
• W2066239714 cites W2314562218 @default.
• W2066239714 cites W2491872128 @default.
• W2066239714 cites W3178231311 @default.
• W2066239714 cites W4233816718 @default.
• W2066239714 cites W4238289388 @default.
• W2066239714 cites W4244516050 @default.
• W2066239714 cites W4253445574 @default.
• W2066239714 doi "https://doi.org/10.1016/j.quascirev.2008.04.015" @default.
• W2066239714 hasPublicationYear "2008" @default.
• W2066239714 type Work @default.
• W2066239714 sameAs 2066239714 @default.
• W2066239714 citedByCount "94" @default.
• W2066239714 countsByYear W20662397142012 @default.
• W2066239714 countsByYear W20662397142013 @default.
• W2066239714 countsByYear W20662397142014 @default.
• W2066239714 countsByYear W20662397142015 @default.
• W2066239714 countsByYear W20662397142016 @default.
• W2066239714 countsByYear W20662397142017 @default.
• W2066239714 countsByYear W20662397142018 @default.
• W2066239714 countsByYear W20662397142019 @default.
• W2066239714 countsByYear W20662397142020 @default.
• W2066239714 countsByYear W20662397142021 @default.
• W2066239714 countsByYear W20662397142022 @default.
• W2066239714 countsByYear W20662397142023 @default.

• next