FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1501544304> ?p ?o ?g. }

• W1501544304 endingPage "306" @default.
• W1501544304 startingPage "296" @default.
• W1501544304 abstract "[1] The initial rise in atmospheric CO2 during the last deglaciation was likely driven by input of carbon from a 13C-depleted reservoir. Here we show that high resolution benthic foraminiferal records from the mid-depth Brazil Margin display an abrupt drop in δ13C during Heinrich Stadial 1 (HS1) that is similar to but larger than in the atmosphere. Comparing the Brazil Margin results to published records from the North Atlantic, we are unable to account for the South Atlantic δ13C data with conservative mixing between northern and southern component water masses. Rapid input of abyssal water from the Southeast Atlantic could account for deglacial δ13C anomalies at the Brazil Margin but it would require a reversal in deep water flow direction compared to today. A new mid-depth water mass may explain similar HS1 δ13C values in both the North and South Atlantic, but contrasting oxygen isotopic values between the two basins do not support such a scenario. Instead, it appears that δ13C behaved non-conservatively during the deglaciation, possibly reflecting the input of carbon from an isotopically depleted source." @default.
• W1501544304 created "2016-06-24" @default.
• W1501544304 creator A5003682711 @default.
• W1501544304 creator A5043412788 @default.
• W1501544304 date "2013-06-01" @default.
• W1501544304 modified "2023-10-18" @default.
• W1501544304 title "Isotopically depleted carbon in the mid-depth South Atlantic during the last deglaciation" @default.
• W1501544304 cites W1482146370 @default.
• W1501544304 cites W1528818822 @default.
• W1501544304 cites W1566593795 @default.
• W1501544304 cites W1594282911 @default.
• W1501544304 cites W1608933594 @default.
• W1501544304 cites W1611443029 @default.
• W1501544304 cites W1639268213 @default.
• W1501544304 cites W1658156290 @default.
• W1501544304 cites W1852165277 @default.
• W1501544304 cites W1964806567 @default.
• W1501544304 cites W1968860571 @default.
• W1501544304 cites W1976509887 @default.
• W1501544304 cites W1980965759 @default.
• W1501544304 cites W1985246090 @default.
• W1501544304 cites W1987399250 @default.
• W1501544304 cites W1990753866 @default.
• W1501544304 cites W2031630167 @default.
• W1501544304 cites W2032396158 @default.
• W1501544304 cites W2033694700 @default.
• W1501544304 cites W2042377724 @default.
• W1501544304 cites W2051226623 @default.
• W1501544304 cites W2064368240 @default.
• W1501544304 cites W2074527287 @default.
• W1501544304 cites W2083519852 @default.
• W1501544304 cites W2083986366 @default.
• W1501544304 cites W2093031608 @default.
• W1501544304 cites W2107372061 @default.
• W1501544304 cites W2110373790 @default.
• W1501544304 cites W2127150857 @default.
• W1501544304 cites W2129040983 @default.
• W1501544304 cites W2147652131 @default.
• W1501544304 cites W2152188824 @default.
• W1501544304 cites W2157152584 @default.
• W1501544304 cites W4244847649 @default.
• W1501544304 doi "https://doi.org/10.1002/palo.20026" @default.
• W1501544304 hasPublicationYear "2013" @default.
• W1501544304 type Work @default.
• W1501544304 sameAs 1501544304 @default.
• W1501544304 citedByCount "40" @default.
• W1501544304 countsByYear W15015443042014 @default.
• W1501544304 countsByYear W15015443042015 @default.
• W1501544304 countsByYear W15015443042016 @default.
• W1501544304 countsByYear W15015443042017 @default.
• W1501544304 countsByYear W15015443042018 @default.
• W1501544304 countsByYear W15015443042019 @default.
• W1501544304 countsByYear W15015443042020 @default.
• W1501544304 countsByYear W15015443042021 @default.
• W1501544304 countsByYear W15015443042022 @default.
• W1501544304 countsByYear W15015443042023 @default.
• W1501544304 crossrefType "journal-article" @default.
• W1501544304 hasAuthorship W1501544304A5003682711 @default.
• W1501544304 hasAuthorship W1501544304A5043412788 @default.
• W1501544304 hasBestOaLocation W15015443042 @default.
• W1501544304 hasConcept C104779481 @default.
• W1501544304 hasConcept C111368507 @default.
• W1501544304 hasConcept C127313418 @default.
• W1501544304 hasConcept C140205800 @default.
• W1501544304 hasConcept C140345934 @default.
• W1501544304 hasConcept C159985019 @default.
• W1501544304 hasConcept C180705331 @default.
• W1501544304 hasConcept C192562407 @default.
• W1501544304 hasConcept C39432304 @default.
• W1501544304 hasConceptScore W1501544304C104779481 @default.
• W1501544304 hasConceptScore W1501544304C111368507 @default.
• W1501544304 hasConceptScore W1501544304C127313418 @default.
• W1501544304 hasConceptScore W1501544304C140205800 @default.
• W1501544304 hasConceptScore W1501544304C140345934 @default.
• W1501544304 hasConceptScore W1501544304C159985019 @default.
• W1501544304 hasConceptScore W1501544304C180705331 @default.
• W1501544304 hasConceptScore W1501544304C192562407 @default.
• W1501544304 hasConceptScore W1501544304C39432304 @default.
• W1501544304 hasIssue "2" @default.
• W1501544304 hasLocation W15015443041 @default.
• W1501544304 hasLocation W15015443042 @default.
• W1501544304 hasLocation W15015443043 @default.
• W1501544304 hasOpenAccess W1501544304 @default.
• W1501544304 hasPrimaryLocation W15015443041 @default.
• W1501544304 hasRelatedWork W1528621231 @default.
• W1501544304 hasRelatedWork W1977453258 @default.
• W1501544304 hasRelatedWork W2014303036 @default.
• W1501544304 hasRelatedWork W2048761473 @default.
• W1501544304 hasRelatedWork W2076805175 @default.
• W1501544304 hasRelatedWork W2079666306 @default.
• W1501544304 hasRelatedWork W2162457813 @default.
• W1501544304 hasRelatedWork W2491678165 @default.
• W1501544304 hasRelatedWork W2604403837 @default.
• W1501544304 hasRelatedWork W2990108707 @default.
• W1501544304 hasVolume "28" @default.
• W1501544304 isParatext "false" @default.
• W1501544304 isRetracted "false" @default.
• W1501544304 magId "1501544304" @default.

• next