FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2054734198> ?p ?o ?g. }

• W2054734198 endingPage "63" @default.
• W2054734198 startingPage "51" @default.
• W2054734198 abstract "We present oxygen and carbon isotope records of benthic foraminifera from the glacial stage 6 through interglacial substage 5e (Eemian) sections of several cores from the subpolar North Atlantic. The cores range in water depth from 1451 to 2658 m. In one core, we generated estimates of sea surface temperature (SST) and of ice‐rafted detritus (IRD) delivery for all of stage 5. We reconstruct bathymeric profiles of δ 13 C for stage 6, Termination II, and three time slices of substage 5e. The δ 13 C profiles indicate that local deep water geometry during stage 6 was similar to that of the last glaciation, with glacial North Atlantic Intermediate Water (GNAIW) overlying deeper waters partially of southern origin. An anomalously large peak in IRD, coupled with planktonic δ 18 O evidence for iceberg melting immediately precedes Termination II and is otherwise similar to stage 2 and 3 Heinrich events. During the termination, low δ 13 C values are observed in cores near and above 2 km, providing evidence of reduced GNAIW production in association with deglacial melting. In the shallowest cores, low δ 13 C values persist into early substage 5e, indicating that the southward retreat of southern‐source waters was not completed until well after the beginning of the substage. In contrast to Termination I, SSTs remained cold until the end of the deglaciation; this may be why there is little evidence from marine and terrestrial sequences for a pronounced climate reversal on Termination II despite what is now clear evidence of a significant reduction in ocean ventilation. The faunal data suggest that SSTs during early 5e were about 7°C warmer than during the glaciation. SST rose several degrees from early to middle substage 5e, peaked in middle substage 5e at about 10°C above glacial values, and then gradually declined by about 5°C. These changes were linked to variations in water mass configuration, as interpreted from benthic δ 13 C evidence. Most of the evidence suggests that oscillations superimposed on the gradual SST trend were 1°–2°C, in contrast to the larger SST changes (3°–4°C) documented for substage 5d." @default.
• W2054734198 created "2016-06-24" @default.
• W2054734198 creator A5001481194 @default.
• W2054734198 creator A5067819213 @default.
• W2054734198 creator A5069463167 @default.
• W2054734198 date "1997-02-01" @default.
• W2054734198 modified "2023-09-26" @default.
• W2054734198 title "Marine core evidence for reduced deep water production during Termination II followed by a relatively stable substage 5e (Eemian)" @default.
• W2054734198 cites W1485073635 @default.
• W2054734198 cites W1966146362 @default.
• W2054734198 cites W1968721411 @default.
• W2054734198 cites W1978582597 @default.
• W2054734198 cites W1980799929 @default.
• W2054734198 cites W1981089749 @default.
• W2054734198 cites W1988104688 @default.
• W2054734198 cites W1991127249 @default.
• W2054734198 cites W1992470362 @default.
• W2054734198 cites W2002897543 @default.
• W2054734198 cites W2005459749 @default.
• W2054734198 cites W2006652966 @default.
• W2054734198 cites W2007257396 @default.
• W2054734198 cites W2008633637 @default.
• W2054734198 cites W2008875043 @default.
• W2054734198 cites W2009992333 @default.
• W2054734198 cites W2012534141 @default.
• W2054734198 cites W2012680423 @default.
• W2054734198 cites W2014485394 @default.
• W2054734198 cites W2016684083 @default.
• W2054734198 cites W2020385915 @default.
• W2054734198 cites W2028588371 @default.
• W2054734198 cites W2038727541 @default.
• W2054734198 cites W2045105472 @default.
• W2054734198 cites W2047056119 @default.
• W2054734198 cites W2051973454 @default.
• W2054734198 cites W2054521717 @default.
• W2054734198 cites W2058718049 @default.
• W2054734198 cites W2063025390 @default.
• W2054734198 cites W2076848599 @default.
• W2054734198 cites W2079889491 @default.
• W2054734198 cites W2084428435 @default.
• W2054734198 cites W2086359165 @default.
• W2054734198 cites W2087621665 @default.
• W2054734198 cites W2087625531 @default.
• W2054734198 cites W2090183139 @default.
• W2054734198 cites W2090767277 @default.
• W2054734198 cites W2091735381 @default.
• W2054734198 cites W2093142430 @default.
• W2054734198 cites W2094394939 @default.
• W2054734198 cites W2124322151 @default.
• W2054734198 cites W2146605432 @default.
• W2054734198 cites W2216552843 @default.
• W2054734198 cites W27788122 @default.
• W2054734198 cites W4255341695 @default.
• W2054734198 doi "https://doi.org/10.1029/96pa03133" @default.
• W2054734198 hasPublicationYear "1997" @default.
• W2054734198 type Work @default.
• W2054734198 sameAs 2054734198 @default.
• W2054734198 citedByCount "109" @default.
• W2054734198 countsByYear W20547341982012 @default.
• W2054734198 countsByYear W20547341982013 @default.
• W2054734198 countsByYear W20547341982014 @default.
• W2054734198 countsByYear W20547341982015 @default.
• W2054734198 countsByYear W20547341982016 @default.
• W2054734198 countsByYear W20547341982017 @default.
• W2054734198 countsByYear W20547341982018 @default.
• W2054734198 countsByYear W20547341982019 @default.
• W2054734198 countsByYear W20547341982020 @default.
• W2054734198 countsByYear W20547341982022 @default.
• W2054734198 countsByYear W20547341982023 @default.
• W2054734198 crossrefType "journal-article" @default.
• W2054734198 hasAuthorship W2054734198A5001481194 @default.
• W2054734198 hasAuthorship W2054734198A5067819213 @default.
• W2054734198 hasAuthorship W2054734198A5069463167 @default.
• W2054734198 hasBestOaLocation W20547341981 @default.
• W2054734198 hasConcept C111368507 @default.
• W2054734198 hasConcept C127313418 @default.
• W2054734198 hasConcept C146357865 @default.
• W2054734198 hasConcept C151730666 @default.
• W2054734198 hasConcept C15739521 @default.
• W2054734198 hasConcept C180705331 @default.
• W2054734198 hasConcept C186240526 @default.
• W2054734198 hasConcept C21790881 @default.
• W2054734198 hasConcept C2780368712 @default.
• W2054734198 hasConcept C2780518792 @default.
• W2054734198 hasConcept C62611706 @default.
• W2054734198 hasConcept C63376196 @default.
• W2054734198 hasConcept C83042747 @default.
• W2054734198 hasConceptScore W2054734198C111368507 @default.
• W2054734198 hasConceptScore W2054734198C127313418 @default.
• W2054734198 hasConceptScore W2054734198C146357865 @default.
• W2054734198 hasConceptScore W2054734198C151730666 @default.
• W2054734198 hasConceptScore W2054734198C15739521 @default.
• W2054734198 hasConceptScore W2054734198C180705331 @default.
• W2054734198 hasConceptScore W2054734198C186240526 @default.
• W2054734198 hasConceptScore W2054734198C21790881 @default.
• W2054734198 hasConceptScore W2054734198C2780368712 @default.
• W2054734198 hasConceptScore W2054734198C2780518792 @default.
• W2054734198 hasConceptScore W2054734198C62611706 @default.

• next