Open AccessThe last deglaciation (20,000 to 11,000 B. P.) on Andoya, northern Norway
Author(s) -
VORREN TORE O.,
VORREN KARLDAG,
ALM TORBJØRN,
GULLIKSEN STEINAR,
LØVLIE REIDAR
Publication year - 1988
Publication title -
boreas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.95
H-Index - 74
eISSN - 1502-3885
pISSN - 0300-9483
DOI - 10.1111/j.1502-3885.1988.tb00123.x
Subject(s) - deglaciation , geology , radiocarbon dating , macrofossil , paleontology , chronology , holocene , arctic , oceanography , physical geography , geography
Cores representing a 5.5m long sequence recovered from lake Æråsvatnet have been investigated for lithostratigraphy, micro‐ and macrofossils and radiocarbon chronology. For the first time in Fennoscandia the maximum Weichselian advance has been closely bracketed with radiocarbon datings (19,000–18,500 B.P.). A continuous stratigraphy from 18,500 B.P. and onwards, partly marine and partly lacustrine, discloses the local shoreline displacement, the palaeovegetation, the palaeoclimate and, together with other data, the deglaciation history. Two phases with a prevailing High Arctic climate have occurred: 18,000 to 16,000 B.P. and 13,700 to 12,800 B.P. Important climatic amelioration accelerating the deglacial recession occurred 16,000, 12,800 and 12,000 B.P. The continental ice sheet was situated close to its maximum position until about 16,000 B.P. The following deglaciation was interrupted by (a minor ?) readvance/halt about 15,000 B.P. (the Flesen event), 13,700‐13,000 B.P. (the D‐event), 12,500 B.P. (the Skarpnes event) and 11,000–10,000 B.P. (the TromsØ‐Lyngen event). The deglaciation chronology and pattern can be correlated with the suggested deep‐sea‐stratigraphy‐based stepwise pattern relying on the old age alternative for termination IA.