FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2890187576> ?p ?o ?g. }

• W2890187576 endingPage "1869" @default.
• W2890187576 startingPage "1855" @default.
• W2890187576 abstract "Subarctic permafrost peatlands are important soil organic carbon pools, and improved knowledge about peat properties and peatland sensitivity to past climate change is essential when predicting future response to a warmer climate and associated feedback mechanisms. In this study, Holocene peatland development and permafrost dynamics of four subarctic peat plateaus in Finnmark, northern Norway have been investigated through detailed analyses of plant macrofossils and geochemical properties. Peatland inception occurred around 9800 cal. yr BP and 9200 cal. yr BP at the two continental sites Suossjavri and Iskoras. Younger basal peat ages were found at the two coastal locations Lakselv and Karlebotn, at least partly caused by the time lag between deglaciation and emergence of land by isostatic uplift. Here, peatland development started around 6150 cal. yr BP and 5150 cal. yr BP, respectively. All four peatlands developed as wet fens throughout most of the Holocene. Permafrost aggradation, causing frost heave and a shift in the vegetation assemblage from wet fen to dry bog species, probably did not occur until during the last millennium, ca. 950 cal. yr BP in Karlebotn and ca. 800 cal. yr BP in Iskoras, and before ca. 150 cal. yr BP in Lakselv and ca. 100 cal. yr BP in Suossjavri. In Karlebotn, there are indications of a possible earlier permafrost phase around 2200 cal. yr BP due to climatic cooling at the late Subboreal to early Subatlantic transition. The mean long-term Holocene carbon accumulation rate at all four sites was 12.3 ± 4.1 gC m −2 yr −1 (±SD) and the mean soil organic carbon storage was 97 ± 46 kgC m −2 ." @default.
• W2890187576 created "2018-09-27" @default.
• W2890187576 creator A5024742380 @default.
• W2890187576 creator A5042632167 @default.
• W2890187576 creator A5045120084 @default.
• W2890187576 creator A5077504737 @default.
• W2890187576 creator A5088264629 @default.
• W2890187576 date "2018-09-10" @default.
• W2890187576 modified "2023-10-10" @default.
• W2890187576 title "Holocene development of subarctic permafrost peatlands in Finnmark, northern Norway" @default.
• W2890187576 cites W1515526034 @default.
• W2890187576 cites W1522489502 @default.
• W2890187576 cites W1578761803 @default.
• W2890187576 cites W1595107457 @default.
• W2890187576 cites W1893530606 @default.
• W2890187576 cites W1902944997 @default.
• W2890187576 cites W1956280464 @default.
• W2890187576 cites W1978040704 @default.
• W2890187576 cites W2004148179 @default.
• W2890187576 cites W2010917045 @default.
• W2890187576 cites W2012286900 @default.
• W2890187576 cites W2012939734 @default.
• W2890187576 cites W201461634 @default.
• W2890187576 cites W2017963652 @default.
• W2890187576 cites W2021372054 @default.
• W2890187576 cites W2023171854 @default.
• W2890187576 cites W2023906603 @default.
• W2890187576 cites W2035201317 @default.
• W2890187576 cites W2036837225 @default.
• W2890187576 cites W2046753504 @default.
• W2890187576 cites W2067058455 @default.
• W2890187576 cites W2076177619 @default.
• W2890187576 cites W2077813923 @default.
• W2890187576 cites W2077895701 @default.
• W2890187576 cites W2081098099 @default.
• W2890187576 cites W2086431105 @default.
• W2890187576 cites W2087563534 @default.
• W2890187576 cites W2096585821 @default.
• W2890187576 cites W2098627306 @default.
• W2890187576 cites W2104833230 @default.
• W2890187576 cites W2120538079 @default.
• W2890187576 cites W2136176561 @default.
• W2890187576 cites W2144794841 @default.
• W2890187576 cites W2152976421 @default.
• W2890187576 cites W2153651524 @default.
• W2890187576 cites W2155211093 @default.
• W2890187576 cites W2157468587 @default.
• W2890187576 cites W2159200641 @default.
• W2890187576 cites W2161110837 @default.
• W2890187576 cites W2164286940 @default.
• W2890187576 cites W2167452694 @default.
• W2890187576 cites W2170805169 @default.
• W2890187576 cites W2176932226 @default.
• W2890187576 cites W2230422110 @default.
• W2890187576 cites W2266381963 @default.
• W2890187576 cites W2287395412 @default.
• W2890187576 cites W2307890158 @default.
• W2890187576 cites W2552937981 @default.
• W2890187576 cites W2565402520 @default.
• W2890187576 cites W2750309510 @default.
• W2890187576 cites W4246027503 @default.
• W2890187576 cites W4249751050 @default.
• W2890187576 cites W4252596155 @default.
• W2890187576 cites W4256039743 @default.
• W2890187576 doi "https://doi.org/10.1177/0959683618798126" @default.
• W2890187576 hasPublicationYear "2018" @default.
• W2890187576 type Work @default.
• W2890187576 sameAs 2890187576 @default.
• W2890187576 citedByCount "15" @default.
• W2890187576 countsByYear W28901875762019 @default.
• W2890187576 countsByYear W28901875762020 @default.
• W2890187576 countsByYear W28901875762021 @default.
• W2890187576 countsByYear W28901875762022 @default.
• W2890187576 countsByYear W28901875762023 @default.
• W2890187576 crossrefType "journal-article" @default.
• W2890187576 hasAuthorship W2890187576A5024742380 @default.
• W2890187576 hasAuthorship W2890187576A5042632167 @default.
• W2890187576 hasAuthorship W2890187576A5045120084 @default.
• W2890187576 hasAuthorship W2890187576A5077504737 @default.
• W2890187576 hasAuthorship W2890187576A5088264629 @default.
• W2890187576 hasBestOaLocation W28901875762 @default.
• W2890187576 hasConcept C100970517 @default.
• W2890187576 hasConcept C109007969 @default.
• W2890187576 hasConcept C111368507 @default.
• W2890187576 hasConcept C112959462 @default.
• W2890187576 hasConcept C114793014 @default.
• W2890187576 hasConcept C122284674 @default.
• W2890187576 hasConcept C127313418 @default.
• W2890187576 hasConcept C132651083 @default.
• W2890187576 hasConcept C140345934 @default.
• W2890187576 hasConcept C142614818 @default.
• W2890187576 hasConcept C15098985 @default.
• W2890187576 hasConcept C180705331 @default.
• W2890187576 hasConcept C18903297 @default.
• W2890187576 hasConcept C205649164 @default.
• W2890187576 hasConcept C25868968 @default.
• W2890187576 hasConcept C2775933976 @default.
• W2890187576 hasConcept C53657456 @default.

• next