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Sökning: WFRF:(Salonen J. Sakari) > (2011-2014) > Scattered late-glac...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003947naa a2200445 4500
001oai:DiVA.org:su-68534
003SwePub
008120104s2011 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-685342 URI
024a https://doi.org/10.1111/j.1365-2699.2010.02448.x2 DOI
040 a (SwePub)su
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Valiranta, Minna4 aut
2451 0a Scattered late-glacial and early Holocene tree populations as dispersal nuclei for forest development in north-eastern European Russia
264 c 2010-12-09
264 1b Wiley,c 2011
338 a print2 rdacarrier
500 a authorCount :6
520 a Aim Concepts about patterns and rates of post-glacial tree population migration are changing as a result of the increasing amount of palaeobotanical information being provided by macroscopic plant remains. Here we combine macrofossil, pollen and stomata records from five sites in north-eastern European Russia and summarize the results for the late-glacial-early Holocene transition. The late-glacial-early Holocene transition encompasses the first indications of trees (tree-type Betula, Picea abies, Abies sibirica and Larix sibirica) and subsequent forest development. Considerable time-lags between the first macrobotanical and/or stomata finds of spruce (Picea abies) and the establishment of a closed forest are reconsidered. Location Pechora basin, north-eastern European Russia. Methods We used plant macrofossil, stomata, pollen and radiocarbon analyses to reconstruct late-glacial and early Holocene tree establishment and forest development. The data were derived from lake sediment and peat archives. Results Palaeobotanical data reveal an early Holocene presence (11,500-10,000 cal. yr bp) of arboreal taxa at all five sites. One site presently located in the northernmost taiga zone, shows the presence of spruce and reproducing tree birch during the late-glacial. Given the current view of post-glacial population dynamics and migration rates, it seems likely that the source area of these early tree populations in north-eastern European Russia was not located in southern Europe but that these populations had local origins. Results thus support the emerging view that the first post-glacial population expansions in non-glaciated regions at high latitudes do not reflect migration from the south but were a result of an increase in the size and density of small persisting outlying tree populations. Main conclusions Results suggest that the area east of the margin of the Scandinavian ice sheet to the Ural Mountains had isolated patches of trees during the late-glacial and early Holocene and that these small populations acted as initial nuclei for population expansion and forest development in the early Holocene.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Early Holocene
653 a forest development
653 a glacial refugia
653 a late-glacial
653 a north-eastern European Russia
653 a palaeobotany
653 a tree colonization
700a Kaakinen, Anu4 aut
700a Kuhry, Peteru Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)pkuhr
700a Kultti, Seija4 aut
700a Salonen, J. Sakari4 aut
700a Seppa, Heikki4 aut
710a Stockholms universitetb Institutionen för naturgeografi och kvartärgeologi (INK)4 org
773t Journal of Biogeographyd : Wileyg 38:5, s. 922-932q 38:5<922-932x 0305-0270x 1365-2699
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-68534
8564 8u https://doi.org/10.1111/j.1365-2699.2010.02448.x

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