Biostratigraphic evidence of the Allerod-Younger Dryas-Preboreal oscillation in northern Iceland

Basal sediments of Lake Torfadalsvatn, northern Iceland, record changes in terrestrial and limnic environments in the period 11,300-9000 C-14 yr B.P. These changes were probably forced by climate and connected with displacements of the marine polar front and sea-ice margin. Pollen, spores, green algae (Pediastrum), saturation isothermal remanent magnetization, and carbon content of the basal sediments provide the first detailed biostratigraphic record of the last glacial-interglacial transition in Iceland. During the first pioneer phase, beginning at ca. 11,300 C-14 yr B.P., grasses and fell-field herbs became established, and lake productivity was very low. At ca. 10,900 C-14 yr B.P., climatic and soil conditions became favorable for shrubs and dwarf shrubs. This change, together with increased limnic productivity, clearly indicates long seasons without ice-cover in the sea immediately north of Iceland. A return to a colder climate (Younger Dryas), probably in connection with a southward displacement of the marine polar front, occurred by 10,600 C-14 yr B.P. Shrub and dwarf-shrub vegetation disappeared, and limnic productivity diminished. A second pioneer vegetation phase, dominated by Oxyria/Rumex and grasses, was initiated by a change to longer seasons without sea ice at ca. 9900 C-14 yr B.P. This warming is also evident as a contemporaneous increase in lake productivity. After ca. 9400 C-14 yr B.P. the reestablishment of dwarf-shrub heaths and very high limnic productivity indicate further warming. (C) 1995 University of Washington.