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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004508naa a2200529 4500
001oai:DiVA.org:su-174940
003SwePub
008191105s2019 | |||||||||||000 ||eng|
009oai:DiVA.org:uu-395920
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1749402 URI
0247 a https://doi.org/10.3390/quat20300292 DOI
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3959202 URI
040 a (SwePub)sud (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Finné, Martinu Uppsala universitet,Antikens kultur och samhällsliv,Stockholm Univ, Bolin Ctr Climate Res, SE-10691 Stockholm, Sweden;Univ Helsinki, Inst Atmospher & Earth Syst Res INAR Phys, Varrio Res Stn, POB 64, FI-00014 Helsinki, Finland4 aut0 (Swepub:uu)marfi619
2451 0a Last Interglacial Climate in Northern Sweden-Insights from a Speleothem Record
264 c 2019-08-20
264 1b MDPI AG,c 2019
338 a print2 rdacarrier
520 a Continental records with absolute dates of the timing and progression of climatic conditions during the Last Interglacial (LIG) from northern Europe are rare. Speleothems from northern Europe have a large potential as archives for LIG environmental conditions since they were formed in sheltered environments and may be preserved beneath ice sheets. Here, we present delta C-13 and delta O-18 values from speleothem Kf-21, from Korallgrottan in Jamtland (northwest Sweden). Kf-21 is dated with five MC-ICPMS U-Th dates with errors smaller than similar to 1 ka. Kf-21 started forming at similar to 130.2 ka and the main growth phase with relatively constant growth rates lasted from 127.3 ka to 124.4 ka, after which calcite formation ceased. Both delta C-13 and delta O-18 show rapid shifts but also trends, with a range of values within their Holocene counterparts from Korallgrottan. Our results indicate an early onset of the LIG in northern Europe with ice-free conditions at similar to 130 ka. Higher growth rates combined with more negative delta O-18 values between similar to 127.3 and 126.8 ka, interpreted here as warmer and more humid conditions, as well as indications of a millennial-scale cold spell centered at 126.2 ka, resemble findings from speleothem records from other parts of Europe, highlighting that these were regional scale climatic patterns.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Multidisciplinär geovetenskap0 (SwePub)105032 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geosciences, Multidisciplinary0 (SwePub)105032 hsv//eng
653 a Last Interglacial (LIG)
653 a speleothem
653 a stable carbon and oxygen isotope compositions
653 a climate variability
653 a Scandinavia
653 a Sweden
7001 a Salonen, Sakariu Univ Helsinki, Dept Geosci & Geog, POB 64, FI-00014 Helsinki, Finland;Univ Bordeaux, Environm & Paleoenvironm Ocean & Continentaux, UMR 5805, F-33615 Pessac, France4 aut
7001 a Frank, Norbertu Heidelberg Univ, Inst Environm Phys, D-69120 Heidelberg, Germany4 aut
7001 a Helmens, Karin F.u Stockholm Univ, Bolin Ctr Climate Res, SE-10691 Stockholm, Sweden4 aut
7001 a Schröder-Ritzrau, Andreau Heidelberg Univ, Inst Environm Phys, D-69120 Heidelberg, Germany4 aut
7001 a Deininger, Michaelu Johannes Gutenberg Univ Mainz, Inst Geosci, D-55128 Mainz, Germany4 aut
7001 a Holzkämper, Steffenu Stockholms universitet,Institutionen för naturgeografi,Stockholm Univ, Bolin Ctr Climate Res, SE-10691 Stockholm, Sweden;Stockholm Univ, Dept Phys Geog, SE-10691 Stockholm, Sweden4 aut0 (Swepub:su)sholz
7102 a Uppsala universitetb Antikens kultur och samhällsliv4 org
7730 t Quaternaryd : MDPI AGg 2:3q 2:3x 2571-550X
8564 u https://doi.org/10.3390/quat2030029y Fulltext
8564 u https://www.mdpi.com/2571-550X/2/3/29/pdf
8564 u https://uu.diva-portal.org/smash/get/diva2:1366677/FULLTEXT01.pdfx primaryx Raw objecty fulltext:print
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-174940
8564 8u https://doi.org/10.3390/quat2030029
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-395920

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