Late and Middle Weichselian stratigraphy of Andøya, north Norway

• Published in: Boreas
• Main Author: VORREN, KARL‐DAG
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1978
• Subjects: Geology; Archeology; Ecology, Evolution, Behavior and Systematics; Andøya; Arctic; Boreas; Norway; North Norway
• Online Access: http://dx.doi.org/10.1111/j.1502-3885.1978.tb00047.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00047.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00047.x

BOREAS Vorren, K.‐D. 1978 03 01: Late and Middle Weichselian stratigraphy of Andøya, north Norway, Boreas, Vol. 7, pp. 19–38. Oslo. ISSN 0300–9483. Bio‐stratigraphy and 14 C datings from Lake Endletvatn, 69 o 44'N and 19 o 05'E, approx. 35 m above sea level, suggest that the lacustrine sedimentation started about 18,000 B.P. The Middle Weichselian vegetation was probably a dry arctic, partly barren, grassland type with abundant Draba spp. and perhaps also Braya spp. Two climatic ameliorations of this chronal substage, named Endletvatn thermomers 1 and 2 (ET 1 and 2), have been recorded. During ET 2, the beginning of which has been dated at about 15,000 B.P., a humid climate prevailed, with a July temperature probably not deviating much from the present one. The colonization by low alpine and subalpine species probably started in the Bølling Chronozone. During the early Allerød Chronozone, protocratic conditions with grasses RumexlOxyria, Papaver and Sagina of. saginoides prevailed. During the middle of the Allerød, stable soil and continuous vegetation was established at sheltered places. At the transition to the Younger Dryas Chronozone a climate favouring Artemisia changed this vegetational development. The middle of the Younger Dryas was cool and humid, probably with an upper low alpine vegetation. The end of this chronozone was characterized by a vegetation of low alpine heaths with Empetrum and Dryas. Diatom analysis (Foged 1978) suggests that there has been no direct marine influence in the basin. The marginal moraine stratigraphy, the marine limit and the climatic development are discussed.