FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2364782330> ?p ?o ?g. }

• W2364782330 abstract "ABSTRACT FINAL ID: PP31A-1838High concentrations of carbonate in surface sediments of the Nordic Seas are generally related to warm Atlantic Water (AW) inflow. This relationship was recently used to infer the Holocene dynamics of Atlantic-derived water off North-West Iceland (Giraudeau et al, 2010; QSR vol. 29) following suggestions that carbonate production in the vicinity of Denmark Strait is tightly linked with inputs of warm, nutrient-rich Irminger Current waters. The present study aims at testing this assumption in the two main passageways of AW to the Arctic Ocean: Fram Strait and the Barents Sea, with a focus on a high resolution Holocene sediment record collected off western Svalbard. Our datasets on extant coccolithophores, as well as estimates of coccolith-carbonate contents within the studied marine cores suggest that sedimentation of calcium carbonate in the northernmost North Atlantic essentially reflects production rates of coccolithophores, and that sedimentation of their fossil remains is driving to a high extent the Holocene variations in net CaCO3 accumulation in Fram Strait and the SW Barents Sea. Our coccolith-based proxy records are indicative of a complex regional dynamics of Holocene surface water changes in these two regions. With the exception of a ca. 2 000 years delayed recovery of surface AW influence to the SW Barents Sea in the early Holocene, both regions experienced the same history of surface water temperature changes until ca. 3 000 cal.yrs BP. A Holocene sea-surface thermal optimum is clearly recognized in both regions during the 8 000 to 7 000 cal. yrs BP interval, followed by a large scale surface cooling triggered by reduced poleward inflow of AW across the Iceland-Scotland Ridge. A decoupling in the pattern of coccolith-carbonate sedimentation between Fram Strait and the SW Barents Sea characterizes the late Holocene. While near continuous surface water warming impacted the southern Barents Sea throughout the last 3 000 years, the eastern Fram Strait was affected by the settling, during maximum AW inflow to the Arctic Ocean, of a strong stratification separating a fresh, sea-ice rich surface mixed-layer of polar origin from an AW-derived poleward water mass." @default.
• W2364782330 created "2016-06-24" @default.
• W2364782330 creator A5011837454 @default.
• W2364782330 creator A5020163951 @default.
• W2364782330 creator A5038325819 @default.
• W2364782330 creator A5059497409 @default.
• W2364782330 creator A5060495278 @default.
• W2364782330 creator A5066903407 @default.
• W2364782330 creator A5068412206 @default.
• W2364782330 creator A5074386991 @default.
• W2364782330 creator A5088835686 @default.
• W2364782330 date "2011-12-01" @default.
• W2364782330 modified "2023-09-27" @default.
• W2364782330 title "Coccolith-Carbonate Sedimentation in the Northern North Atlantic: an Holocene Perspective" @default.
• W2364782330 hasPublicationYear "2011" @default.
• W2364782330 type Work @default.
• W2364782330 sameAs 2364782330 @default.
• W2364782330 citedByCount "0" @default.
• W2364782330 crossrefType "journal-article" @default.
• W2364782330 hasAuthorship W2364782330A5011837454 @default.
• W2364782330 hasAuthorship W2364782330A5020163951 @default.
• W2364782330 hasAuthorship W2364782330A5038325819 @default.
• W2364782330 hasAuthorship W2364782330A5059497409 @default.
• W2364782330 hasAuthorship W2364782330A5060495278 @default.
• W2364782330 hasAuthorship W2364782330A5066903407 @default.
• W2364782330 hasAuthorship W2364782330A5068412206 @default.
• W2364782330 hasAuthorship W2364782330A5074386991 @default.
• W2364782330 hasAuthorship W2364782330A5088835686 @default.
• W2364782330 hasConcept C111368507 @default.
• W2364782330 hasConcept C127313418 @default.
• W2364782330 hasConcept C140345934 @default.
• W2364782330 hasConcept C191897082 @default.
• W2364782330 hasConcept C192562407 @default.
• W2364782330 hasConcept C2776926057 @default.
• W2364782330 hasConcept C2780659211 @default.
• W2364782330 hasConceptScore W2364782330C111368507 @default.
• W2364782330 hasConceptScore W2364782330C127313418 @default.
• W2364782330 hasConceptScore W2364782330C140345934 @default.
• W2364782330 hasConceptScore W2364782330C191897082 @default.
• W2364782330 hasConceptScore W2364782330C192562407 @default.
• W2364782330 hasConceptScore W2364782330C2776926057 @default.
• W2364782330 hasConceptScore W2364782330C2780659211 @default.
• W2364782330 hasLocation W23647823301 @default.
• W2364782330 hasOpenAccess W2364782330 @default.
• W2364782330 hasPrimaryLocation W23647823301 @default.
• W2364782330 hasRelatedWork W1005321287 @default.
• W2364782330 hasRelatedWork W110730617 @default.
• W2364782330 hasRelatedWork W1499565783 @default.
• W2364782330 hasRelatedWork W1789796658 @default.
• W2364782330 hasRelatedWork W1877758510 @default.
• W2364782330 hasRelatedWork W1966290157 @default.
• W2364782330 hasRelatedWork W1999027888 @default.
• W2364782330 hasRelatedWork W2022656501 @default.
• W2364782330 hasRelatedWork W2094302854 @default.
• W2364782330 hasRelatedWork W2105760390 @default.
• W2364782330 hasRelatedWork W2118541949 @default.
• W2364782330 hasRelatedWork W2126802881 @default.
• W2364782330 hasRelatedWork W2153315261 @default.
• W2364782330 hasRelatedWork W2175930730 @default.
• W2364782330 hasRelatedWork W2184853442 @default.
• W2364782330 hasRelatedWork W2473308253 @default.
• W2364782330 hasRelatedWork W2626100832 @default.
• W2364782330 hasRelatedWork W2900215920 @default.
• W2364782330 hasRelatedWork W598842153 @default.
• W2364782330 hasRelatedWork W601843022 @default.
• W2364782330 hasVolume "2011" @default.
• W2364782330 isParatext "false" @default.
• W2364782330 isRetracted "false" @default.
• W2364782330 magId "2364782330" @default.
• W2364782330 workType "article" @default.