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Record #192085:
Climatic influence on peatland formation and lateral expansion in sub-Arctic Fennoscandia / Jan Weckström, Heikki Seppä, Atte Korhola.
Title: | Climatic influence on peatland formation and lateral expansion in sub-Arctic Fennoscandia / Jan Weckström, Heikki Seppä, Atte Korhola. |
Author(s): | Weckström, Jan. Seppä, Heikki. Korhola, Atte. |
Date: | 2010. |
In: | Boreas. (2010.), Vol. 39(4) (2010) |
Abstract: | Investigates initiation and lateral expansion patterns of five small sub-Arctic peatlands in Fennoscandian tree-line region, using 21 accelerator mass spectrometry ¹⁴C-dated basal peat samples representing three to six dates per site. Radiocarbon dates were converted to calendar years and were based on median probability . Finds most extensive lateral expansion of peatlands to have occurred during beginning of cool and moist late Holocene period (c. 4000-3000 cal. yr BP). |
Notes: | Boreas. Vol. 39(4) :761-769 (2010). |
Keywords: | 551.58 -- Climatology. 551.583.2 -- Climatic changes, historic. 551.583.3 -- Climatic changes, Quaternary. 551.586 -- Climatology, biological aspects. 551.794 -- Holocene. 574.4 -- Ecology, terrestrial. 581.526.33/.35 -- Peatland plant formations. F -- Biological sciences. (*3) -- Arctic regions. (*548) -- Scandinavia. |
SPRI record no.: | 192085 |
LDR 01743naa#a2200000#a#4500 001 SPRI-192085 005 20240329100912.0 007 ta 008 240329s2010####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-192085 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aWeckström, Jan. 245 10 ‡aClimatic influence on peatland formation and lateral expansion in sub-Arctic Fennoscandia /‡cJan Weckström, Heikki Seppä, Atte Korhola. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2010. 300 ## ‡ap. 761-769 :‡bill., diag., table, map. 500 ## ‡aBoreas. Vol. 39(4) :761-769 (2010). 520 3# ‡aInvestigates initiation and lateral expansion patterns of five small sub-Arctic peatlands in Fennoscandian tree-line region, using 21 accelerator mass spectrometry ¹⁴C-dated basal peat samples representing three to six dates per site. Radiocarbon dates were converted to calendar years and were based on median probability . Finds most extensive lateral expansion of peatlands to have occurred during beginning of cool and moist late Holocene period (c. 4000-3000 cal. yr BP). 530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2010.00168.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2010.00168.x 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.583.2 -- Climatic changes, historic.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.586 -- Climatology, biological aspects.‡2udc 650 07 ‡a551.794 -- Holocene.‡2udc 650 07 ‡a574.4 -- Ecology, terrestrial.‡2udc 650 07 ‡a581.526.33/.35 -- Peatland plant formations.‡2udc 650 07 ‡aF -- Biological sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*548) -- Scandinavia.‡2udc 700 1# ‡aSeppä, Heikki. 700 1# ‡aKorhola, Atte. 773 0# ‡7nnas ‡tBoreas. ‡gVol. 39(4) (2010) ‡wSPRI-56035 916 ## ‡a2010/10/20 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329 ‡bJW