FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2073982634> ?p ?o ?g. }

• W2073982634 endingPage "113" @default.
• W2073982634 startingPage "95" @default.
• W2073982634 abstract "Sr and Nd isotopic compositions have been measured on the lithic fraction of last climatic cycle sediments from the North Atlantic (≈40°N/≈60°N), in order to identify the origins of the particles. From the reconstruction of their transport pathways, we deduce the mechanisms that explain their distributions. The main source regions are the Canadian shield (mostly the area of Baffin Bay and western Greenland), the Scandinavian shield, the European region (British Isles and Bay of Biscay), and Iceland. We observe a significant glacial/interglacial contrast, characterized by a dominant Icelandic input via near‐bottom transport by North Atlantic Deep Water (NADW) during the interglacials and a largely continent‐derived contribution of surface‐transported, ice‐rafted detritus (IRD) during the glacial period. During the last glacial period, the Heinrich events (abrupt, massive discharges of IRD) originated not only from the Laurentide ice sheet as heretofore envisioned but also from other sources. Three other major North Atlantic ice sheets (Fennoscandian, British Isles, and Icelandic) probably surged simultaneously, discharging ice and IRD into the North Atlantic. As opposed to theories implying a unique, Laurentide origin [ Gwiazda et al., 1995] driven by an internal mechanism [ McAyeal , 1993], we confirm that the Icelandic and the Fennoscandian ice sheets also surged as recently proposed by other authors, and we here also distinguish a possible detrital contribution from the British Isles ice sheet. This pan‐North Atlantic phenomenon thus requires a common regional, external forcing." @default.
• W2073982634 created "2016-06-24" @default.
• W2073982634 creator A5004774480 @default.
• W2073982634 creator A5017480302 @default.
• W2073982634 creator A5027992695 @default.
• W2073982634 creator A5082310551 @default.
• W2073982634 date "1996-02-01" @default.
• W2073982634 modified "2023-10-16" @default.
• W2073982634 title "Sr and Nd isotopes as tracers of North Atlantic lithic particles: Paleoclimatic implications" @default.
• W2073982634 cites W1514394155 @default.
• W2073982634 cites W1968721411 @default.
• W2073982634 cites W1970242590 @default.
• W2073982634 cites W1973227610 @default.
• W2073982634 cites W1980461742 @default.
• W2073982634 cites W1981028614 @default.
• W2073982634 cites W1982903817 @default.
• W2073982634 cites W1986796119 @default.
• W2073982634 cites W1987276983 @default.
• W2073982634 cites W1991127249 @default.
• W2073982634 cites W1995613894 @default.
• W2073982634 cites W1996055672 @default.
• W2073982634 cites W1999997920 @default.
• W2073982634 cites W2001134294 @default.
• W2073982634 cites W2005459749 @default.
• W2073982634 cites W2007217700 @default.
• W2073982634 cites W2007257396 @default.
• W2073982634 cites W2014925306 @default.
• W2073982634 cites W2015120422 @default.
• W2073982634 cites W2018376581 @default.
• W2073982634 cites W2019558782 @default.
• W2073982634 cites W2020661715 @default.
• W2073982634 cites W2025956607 @default.
• W2073982634 cites W2026734417 @default.
• W2073982634 cites W2037041276 @default.
• W2073982634 cites W2037099081 @default.
• W2073982634 cites W2040574144 @default.
• W2073982634 cites W2047056119 @default.
• W2073982634 cites W2051559013 @default.
• W2073982634 cites W2055840853 @default.
• W2073982634 cites W2056400369 @default.
• W2073982634 cites W2057091716 @default.
• W2073982634 cites W2059041512 @default.
• W2073982634 cites W2061037721 @default.
• W2073982634 cites W2076651014 @default.
• W2073982634 cites W2076848599 @default.
• W2073982634 cites W2078689557 @default.
• W2073982634 cites W2079922028 @default.
• W2073982634 cites W2087625531 @default.
• W2073982634 cites W2091154424 @default.
• W2073982634 cites W2091735381 @default.
• W2073982634 cites W2097009984 @default.
• W2073982634 cites W2112628010 @default.
• W2073982634 cites W2127089758 @default.
• W2073982634 cites W2141580927 @default.
• W2073982634 cites W2146605432 @default.
• W2073982634 cites W2153040879 @default.
• W2073982634 cites W2155969003 @default.
• W2073982634 cites W2161926766 @default.
• W2073982634 cites W2201864556 @default.
• W2073982634 cites W2330716625 @default.
• W2073982634 doi "https://doi.org/10.1029/95pa03199" @default.
• W2073982634 hasPublicationYear "1996" @default.
• W2073982634 type Work @default.
• W2073982634 sameAs 2073982634 @default.
• W2073982634 citedByCount "135" @default.
• W2073982634 countsByYear W20739826342012 @default.
• W2073982634 countsByYear W20739826342013 @default.
• W2073982634 countsByYear W20739826342014 @default.
• W2073982634 countsByYear W20739826342015 @default.
• W2073982634 countsByYear W20739826342016 @default.
• W2073982634 countsByYear W20739826342017 @default.
• W2073982634 countsByYear W20739826342018 @default.
• W2073982634 countsByYear W20739826342019 @default.
• W2073982634 countsByYear W20739826342020 @default.
• W2073982634 countsByYear W20739826342021 @default.
• W2073982634 countsByYear W20739826342022 @default.
• W2073982634 crossrefType "journal-article" @default.
• W2073982634 hasAuthorship W2073982634A5004774480 @default.
• W2073982634 hasAuthorship W2073982634A5017480302 @default.
• W2073982634 hasAuthorship W2073982634A5027992695 @default.
• W2073982634 hasAuthorship W2073982634A5082310551 @default.
• W2073982634 hasConcept C111368507 @default.
• W2073982634 hasConcept C115880899 @default.
• W2073982634 hasConcept C123750103 @default.
• W2073982634 hasConcept C127313418 @default.
• W2073982634 hasConcept C151730666 @default.
• W2073982634 hasConcept C15739521 @default.
• W2073982634 hasConcept C180705331 @default.
• W2073982634 hasConcept C186240526 @default.
• W2073982634 hasConcept C2780518792 @default.
• W2073982634 hasConcept C39996641 @default.
• W2073982634 hasConcept C63376196 @default.
• W2073982634 hasConcept C6582778 @default.
• W2073982634 hasConcept C78091846 @default.
• W2073982634 hasConceptScore W2073982634C111368507 @default.
• W2073982634 hasConceptScore W2073982634C115880899 @default.
• W2073982634 hasConceptScore W2073982634C123750103 @default.
• W2073982634 hasConceptScore W2073982634C127313418 @default.

• next