FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2021108822> ?p ?o ?g. }

• W2021108822 endingPage "502" @default.
• W2021108822 startingPage "489" @default.
• W2021108822 abstract "The bulk magnetic parameters of seven deep-sea cores distributed from the Nordic Seas (67°N) to the North Atlantic as far south as the Bermuda Rise (33°N) exhibit short-term variations which correlate with rapid climatic changes during marine isotopic stage 3 (MIS3). The magnetic mineralogy is uniformly dominated by well sorted low Ti-content magnetites indicating that these variations are due to variations in the relative amount of magnetic minerals. Because the magnetic minerals predominantly originate from one common source area (the Nordic basaltic province), these changes arise from changes in the efficiency of the transport of the magnetic particles by deep currents from the source to the site of deposition. These results therefore show that the fast climatic changes are related to coeval fast changes in the strength of the deep-sea circulation. The latter was active/reduced during the interstadials/stadials and Heinrich events transporting the magnetic particles from the Norwegian Sea into the North Atlantic ocean along a path similar to the present path of the NADW. It is tentatively suggested that the Faeroe-Shetland Channel and the Denmark Strait were the only two active paths for the overflow water during MIS3. The presence of magnetic oscillations in the Bermuda Rise core in phase with those from the North Atlantic indicates that the activity of the southern Newfoundland Basin gyre was linked to that of the NADW during MIS3." @default.
• W2021108822 created "2016-06-24" @default.
• W2021108822 creator A5003899211 @default.
• W2021108822 creator A5004906060 @default.
• W2021108822 creator A5026835054 @default.
• W2021108822 creator A5040795769 @default.
• W2021108822 creator A5055902382 @default.
• W2021108822 creator A5078998894 @default.
• W2021108822 date "1999-09-01" @default.
• W2021108822 modified "2023-10-16" @default.
• W2021108822 title "Rapid climatic variations during marine isotopic stage 3: magnetic analysis of sediments from Nordic Seas and North Atlantic" @default.
• W2021108822 cites W1639268213 @default.
• W2021108822 cites W1966329790 @default.
• W2021108822 cites W1967286558 @default.
• W2021108822 cites W1968721411 @default.
• W2021108822 cites W1971145772 @default.
• W2021108822 cites W1973227610 @default.
• W2021108822 cites W1976375472 @default.
• W2021108822 cites W1980818108 @default.
• W2021108822 cites W1984659383 @default.
• W2021108822 cites W1989427453 @default.
• W2021108822 cites W1991127249 @default.
• W2021108822 cites W1992799854 @default.
• W2021108822 cites W2000469323 @default.
• W2021108822 cites W2000719275 @default.
• W2021108822 cites W2001203090 @default.
• W2021108822 cites W2005459749 @default.
• W2021108822 cites W2008710874 @default.
• W2021108822 cites W2008875043 @default.
• W2021108822 cites W2014607005 @default.
• W2021108822 cites W2014925306 @default.
• W2021108822 cites W2015120422 @default.
• W2021108822 cites W2026669659 @default.
• W2021108822 cites W2040226379 @default.
• W2021108822 cites W2047577495 @default.
• W2021108822 cites W2051559013 @default.
• W2021108822 cites W2052128667 @default.
• W2021108822 cites W2066131692 @default.
• W2021108822 cites W2075173695 @default.
• W2021108822 cites W2075282717 @default.
• W2021108822 cites W2082955214 @default.
• W2021108822 cites W2101372386 @default.
• W2021108822 cites W2119689998 @default.
• W2021108822 cites W2138071182 @default.
• W2021108822 cites W2216966513 @default.
• W2021108822 doi "https://doi.org/10.1016/s0012-821x(99)00162-4" @default.
• W2021108822 hasPublicationYear "1999" @default.
• W2021108822 type Work @default.
• W2021108822 sameAs 2021108822 @default.
• W2021108822 citedByCount "184" @default.
• W2021108822 countsByYear W20211088222012 @default.
• W2021108822 countsByYear W20211088222013 @default.
• W2021108822 countsByYear W20211088222014 @default.
• W2021108822 countsByYear W20211088222015 @default.
• W2021108822 countsByYear W20211088222016 @default.
• W2021108822 countsByYear W20211088222017 @default.
• W2021108822 countsByYear W20211088222018 @default.
• W2021108822 countsByYear W20211088222019 @default.
• W2021108822 countsByYear W20211088222020 @default.
• W2021108822 countsByYear W20211088222021 @default.
• W2021108822 countsByYear W20211088222022 @default.
• W2021108822 countsByYear W20211088222023 @default.
• W2021108822 crossrefType "journal-article" @default.
• W2021108822 hasAuthorship W2021108822A5003899211 @default.
• W2021108822 hasAuthorship W2021108822A5004906060 @default.
• W2021108822 hasAuthorship W2021108822A5026835054 @default.
• W2021108822 hasAuthorship W2021108822A5040795769 @default.
• W2021108822 hasAuthorship W2021108822A5055902382 @default.
• W2021108822 hasAuthorship W2021108822A5078998894 @default.
• W2021108822 hasConcept C111368507 @default.
• W2021108822 hasConcept C127313418 @default.
• W2021108822 hasConcept C140345934 @default.
• W2021108822 hasConcept C14168384 @default.
• W2021108822 hasConcept C146357865 @default.
• W2021108822 hasConcept C151730666 @default.
• W2021108822 hasConcept C17093552 @default.
• W2021108822 hasConcept C2780978308 @default.
• W2021108822 hasConcept C30380174 @default.
• W2021108822 hasConcept C505870484 @default.
• W2021108822 hasConcept C65814071 @default.
• W2021108822 hasConcept C6582778 @default.
• W2021108822 hasConcept C78091846 @default.
• W2021108822 hasConcept C86803240 @default.
• W2021108822 hasConceptScore W2021108822C111368507 @default.
• W2021108822 hasConceptScore W2021108822C127313418 @default.
• W2021108822 hasConceptScore W2021108822C140345934 @default.
• W2021108822 hasConceptScore W2021108822C14168384 @default.
• W2021108822 hasConceptScore W2021108822C146357865 @default.
• W2021108822 hasConceptScore W2021108822C151730666 @default.
• W2021108822 hasConceptScore W2021108822C17093552 @default.
• W2021108822 hasConceptScore W2021108822C2780978308 @default.
• W2021108822 hasConceptScore W2021108822C30380174 @default.
• W2021108822 hasConceptScore W2021108822C505870484 @default.
• W2021108822 hasConceptScore W2021108822C65814071 @default.
• W2021108822 hasConceptScore W2021108822C6582778 @default.
• W2021108822 hasConceptScore W2021108822C78091846 @default.
• W2021108822 hasConceptScore W2021108822C86803240 @default.
• W2021108822 hasIssue "3" @default.

• next