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Record #188594:

Vegetation and climate c. 12 300-9000 cal. yr BP at Andøya, NW Norway / Karl-Dag Vorren, and 4 others.

Title: Vegetation and climate c. 12 300-9000 cal. yr BP at Andøya, NW Norway / Karl-Dag Vorren, and 4 others.
Author(s): Vorren, Karl-Dag.
Date: 2009.
In: Boreas. (2009.), Vol. 38(1) (2009)
Abstract: Reports investigation of palynological, macrofossil, loss-on-ignition, tephra and ¹⁴C data at three sites at northern part of island of Andøya. Aim is to trace response of Andøya biota to climate changes taking place after Weichselian glaciation. Period 12,300-11,950 cal. yr BP was characterised by polar desert vegetation, and period 11,950-11,050 cal. yr BP by moisture-demanding predominantly low-Arctic Oxyria vegetation. During period 11,050-10,650 cal. yr BP, there was climatic amelioration towards sub-Arctic climate and heaths dominated by Empetrium. After 10,650 cal. yr BP, Oxyria vegetation disappeared.
Notes:

Boreas. Vol. 38(1) :401-420 (2009).

Keywords: 551.336 -- Ice ages.
551.583.3 -- Climatic changes, Quaternary.
551.79 -- Quaternary.
574 -- Ecology.
56 -- Palaeontology.
581.081.3 -- Pollen analysis.
581.526 -- Ecology, formational.
581.526.34 -- Heathland plant formations.
581.526.42 -- Forest plant formations.
F -- Biological sciences.
(*3) -- Arctic regions.
(*58) -- Norway.
SPRI record no.: 188594

MARCXML

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100 1# ‡aVorren, Karl-Dag.
245 10 ‡aVegetation and climate c. 12 300-9000 cal. yr BP at Andøya, NW Norway /‡cKarl-Dag Vorren, and 4 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 401-420.
500 ## ‡aBoreas. Vol. 38(1) :401-420 (2009).
520 3# ‡aReports investigation of palynological, macrofossil, loss-on-ignition, tephra and ¹⁴C data at three sites at northern part of island of Andøya. Aim is to trace response of Andøya biota to climate changes taking place after Weichselian glaciation. Period 12,300-11,950 cal. yr BP was characterised by polar desert vegetation, and period 11,950-11,050 cal. yr BP by moisture-demanding predominantly low-Arctic Oxyria vegetation. During period 11,050-10,650 cal. yr BP, there was climatic amelioration towards sub-Arctic climate and heaths dominated by Empetrium. After 10,650 cal. yr BP, Oxyria vegetation disappeared.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2008.00081.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2008.00081.x
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a581.081.3 -- Pollen analysis.‡2udc
650 07 ‡a581.526 -- Ecology, formational.‡2udc
650 07 ‡a581.526.34 -- Heathland plant formations.‡2udc
650 07 ‡a581.526.42 -- Forest plant formations.‡2udc
650 07 ‡aF -- Biological sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*58) -- Norway.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 38(1) (2009) ‡wSPRI-56035
916 ## ‡a2010/01/21 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221002 ‡bJW