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Record #191641:

Re-dating the Pilgrimstad Interstadial with OSL: a warmer climate and a smaller ice sheet during the Swedish Middle Weichselian (MIS 3)? / Helena Alexanderson, Timothy Johnsen, Andrew S. Murray.

Title: Re-dating the Pilgrimstad Interstadial with OSL: a warmer climate and a smaller ice sheet during the Swedish Middle Weichselian (MIS 3)? / Helena Alexanderson, Timothy Johnsen, Andrew S. Murray.
Author(s): Alexanderson, Helena.
Johnsen, Timothy.
Murray, Andrew S.
Date: 2010.
In: Boreas. (2010.), Vol. 39(2) (2010)
Abstract: Presents and evaluates results of optically stimulated luminescence dating of 10 samples from mineral- and organic-rich sediments from new Pilgrimstad section. Site is considered important for reconstructing environmental changes during last (Weichselian) glacial period and has been assigned an Early Weichselian age (marine isotope stage (MIS) 5 a/c; > 74 ka). Since new results controversially place Pilgrimstad Interglacial in marine isotope stage MIS 3, paper focuses on methodology and reliability of OSL ages, rather than their palaeoglaciological and palaeoecological implications.
Notes:

Boreas. Vol. 39(2) :367-376 (2010).

Keywords: 551.33 -- Glacial geology.
551.336 -- Ice ages.
551.337 -- Chronology of the Pleistocene and recent periods.
550.93 -- Geochronology.
551.321 -- Glaciological methods and instruments.
551.583.3 -- Climatic changes, Quaternary.
551.324.24 -- Ice sheets and caps: Scandinavian Ice Sheet.
551.791 -- Pleistocene.
E7 -- Glaciology: glacial geology and ice ages.
(*57) -- Sweden.
(*571) -- Norrland.
SPRI record no.: 191641

MARCXML

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035 ## ‡aSPRI-191641
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aAlexanderson, Helena.
245 10 ‡aRe-dating the Pilgrimstad Interstadial with OSL :‡ba warmer climate and a smaller ice sheet during the Swedish Middle Weichselian (MIS 3)? /‡cHelena Alexanderson, Timothy Johnsen, Andrew S. Murray.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2010.
300 ## ‡ap. 367-376 :‡bill., diags., tables, map.
500 ## ‡aBoreas. Vol. 39(2) :367-376 (2010).
520 3# ‡aPresents and evaluates results of optically stimulated luminescence dating of 10 samples from mineral- and organic-rich sediments from new Pilgrimstad section. Site is considered important for reconstructing environmental changes during last (Weichselian) glacial period and has been assigned an Early Weichselian age (marine isotope stage (MIS) 5 a/c; > 74 ka). Since new results controversially place Pilgrimstad Interglacial in marine isotope stage MIS 3, paper focuses on methodology and reliability of OSL ages, rather than their palaeoglaciological and palaeoecological implications.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2009.00130.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2009.00130.x
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps: Scandinavian Ice Sheet.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*57) -- Sweden.‡2udc
651 #7 ‡a(*571) -- Norrland.‡2udc
700 1# ‡aJohnsen, Timothy.
700 1# ‡aMurray, Andrew S.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 39(2) (2010) ‡wSPRI-56035
916 ## ‡a2010/08/17 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231003 ‡bRF