FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4214739306> ?p ?o ?g. }

• W4214739306 abstract "Abstract. Climate warming is amplified in the land-sea system of the East Siberian Arctic, which also holds large pools of vulnerable carbon in permafrost. This coastal area is strongly influenced by sediment and carbon transport from both its large rivers and extensive erosion of Pleistocene permafrost along its coastline. This study is investigating the coastal fate of the sediment and organic carbon delivered to the Buor-Khaya Gulf, which is the first recipient of the 16 overwhelming fluvial discharge from the Lena River and is additionally receiving large input from extensive erosion of the coastal ice-complex (permafrost a.k.a. Yedoma; loess soil with high organic carbon content). Both water column suspended particulate matter (SPM) and surface sediments were sampled at about 250 oceanographic stations in the Gulf in this multiyear effort, including one winter campaign, and analyzed for the distribution and sorting of sediment size, organic carbon content, and stable carbon isotope signals. The composition of the surface sediment suggests an overwhelmingly terrestrial contribution from both river and coastal erosion. Based on data collected during several years in the period 2000–2008, two different sedimentation regimes were revealed for the Buor-Khaya Gulf, the relative importance of each at a given time depend on hydrometeorological conditions, the Lena River water discharge and sea-ice regime: Type 1 erosion-accumulation and Type 2 accumulation. The Type 1 erosion-accumulation sedimentation regime is typical (2000–2006) for the ice-free period of the year (here considered in detail for August 2005). Under such conditions terrigenous sources of suspended particulate matter (SPM) and particulate organic carbon (POC) stem predominantly from river discharge, thermal erosion of coastal ice-complex and remobilized bottom sediments. The Type 2 accumulation sedimentation regime develops under ice-covered conditions, and only occasionally during the ice-free period (August 2008). In Type 2 winter, combined terrigenous and marine-biogenic SPM and POC sources are dominating due to relatively low overall terrigenous input (April 2007). In Type 2 summer, river alluvium becomes the major SPM and POC source (August 2008). The water column SPM and POC loadings vary by more than a factor of two between the two regimes. This study underscores the necessity of multi-year investigations to better understand the functioning of the primary recipient of terrestrially expulsed matter in the East Siberian Arctic." @default.
• W4214739306 created "2022-03-02" @default.
• W4214739306 creator A5004305973 @default.
• W4214739306 creator A5033298038 @default.
• W4214739306 creator A5037665769 @default.
• W4214739306 creator A5044975902 @default.
• W4214739306 creator A5050042588 @default.
• W4214739306 creator A5057777852 @default.
• W4214739306 creator A5062317991 @default.
• W4214739306 creator A5076707370 @default.
• W4214739306 date "2011-02-28" @default.
• W4214739306 modified "2023-10-18" @default.
• W4214739306 title "Seasonal and interannual variability of sedimentation and organic matter distribution in the Buor Khaya Gulf – the primary recipient of input from Lena River and coastal erosion in the SE Laptev Sea" @default.
• W4214739306 cites W1544486285 @default.
• W4214739306 cites W1964274869 @default.
• W4214739306 cites W1969266604 @default.
• W4214739306 cites W1972399256 @default.
• W4214739306 cites W1977727401 @default.
• W4214739306 cites W2032741748 @default.
• W4214739306 cites W2058918120 @default.
• W4214739306 cites W2059501475 @default.
• W4214739306 cites W206342875 @default.
• W4214739306 cites W2083690878 @default.
• W4214739306 cites W2090023837 @default.
• W4214739306 cites W2091974950 @default.
• W4214739306 cites W2110252117 @default.
• W4214739306 cites W2145250389 @default.
• W4214739306 cites W34391976 @default.
• W4214739306 doi "https://doi.org/10.5194/bgd-8-1917-2011" @default.
• W4214739306 hasPublicationYear "2011" @default.
• W4214739306 type Work @default.
• W4214739306 citedByCount "4" @default.
• W4214739306 countsByYear W42147393062013 @default.
• W4214739306 crossrefType "posted-content" @default.
• W4214739306 hasAuthorship W4214739306A5004305973 @default.
• W4214739306 hasAuthorship W4214739306A5033298038 @default.
• W4214739306 hasAuthorship W4214739306A5037665769 @default.
• W4214739306 hasAuthorship W4214739306A5044975902 @default.
• W4214739306 hasAuthorship W4214739306A5050042588 @default.
• W4214739306 hasAuthorship W4214739306A5057777852 @default.
• W4214739306 hasAuthorship W4214739306A5062317991 @default.
• W4214739306 hasAuthorship W4214739306A5076707370 @default.
• W4214739306 hasBestOaLocation W42147393061 @default.
• W4214739306 hasConcept C109007969 @default.
• W4214739306 hasConcept C111368507 @default.
• W4214739306 hasConcept C112959462 @default.
• W4214739306 hasConcept C114793014 @default.
• W4214739306 hasConcept C123157820 @default.
• W4214739306 hasConcept C127313418 @default.
• W4214739306 hasConcept C15098985 @default.
• W4214739306 hasConcept C154261466 @default.
• W4214739306 hasConcept C158787203 @default.
• W4214739306 hasConcept C187320778 @default.
• W4214739306 hasConcept C18903297 @default.
• W4214739306 hasConcept C199285206 @default.
• W4214739306 hasConcept C2816523 @default.
• W4214739306 hasConcept C29941650 @default.
• W4214739306 hasConcept C39432304 @default.
• W4214739306 hasConcept C518008717 @default.
• W4214739306 hasConcept C76886044 @default.
• W4214739306 hasConcept C86803240 @default.
• W4214739306 hasConceptScore W4214739306C109007969 @default.
• W4214739306 hasConceptScore W4214739306C111368507 @default.
• W4214739306 hasConceptScore W4214739306C112959462 @default.
• W4214739306 hasConceptScore W4214739306C114793014 @default.
• W4214739306 hasConceptScore W4214739306C123157820 @default.
• W4214739306 hasConceptScore W4214739306C127313418 @default.
• W4214739306 hasConceptScore W4214739306C15098985 @default.
• W4214739306 hasConceptScore W4214739306C154261466 @default.
• W4214739306 hasConceptScore W4214739306C158787203 @default.
• W4214739306 hasConceptScore W4214739306C187320778 @default.
• W4214739306 hasConceptScore W4214739306C18903297 @default.
• W4214739306 hasConceptScore W4214739306C199285206 @default.
• W4214739306 hasConceptScore W4214739306C2816523 @default.
• W4214739306 hasConceptScore W4214739306C29941650 @default.
• W4214739306 hasConceptScore W4214739306C39432304 @default.
• W4214739306 hasConceptScore W4214739306C518008717 @default.
• W4214739306 hasConceptScore W4214739306C76886044 @default.
• W4214739306 hasConceptScore W4214739306C86803240 @default.
• W4214739306 hasLocation W42147393061 @default.
• W4214739306 hasLocation W42147393062 @default.
• W4214739306 hasOpenAccess W4214739306 @default.
• W4214739306 hasPrimaryLocation W42147393061 @default.
• W4214739306 hasRelatedWork W1952025987 @default.
• W4214739306 hasRelatedWork W1981054635 @default.
• W4214739306 hasRelatedWork W1999484141 @default.
• W4214739306 hasRelatedWork W2130048334 @default.
• W4214739306 hasRelatedWork W2299794243 @default.
• W4214739306 hasRelatedWork W2528771795 @default.
• W4214739306 hasRelatedWork W3005969641 @default.
• W4214739306 hasRelatedWork W3032866170 @default.
• W4214739306 hasRelatedWork W3044554458 @default.
• W4214739306 hasRelatedWork W38660292 @default.
• W4214739306 isParatext "false" @default.
• W4214739306 isRetracted "false" @default.
• W4214739306 workType "article" @default.