The beginning of the Bølling is also the high-resolution date for the sharp temperature rise marking the end of the Oldest Dryas at 14,670 BP. Roberts (1998) uses 15,000. A range of 14,650–14,000 BP calibrated has been assigned to the Bølling layer of the excavation at Lake Neuchâtel, Switzerland, 1992–1993. The Oxygen isotope record from Greenland ice includes the Bølling warm peak between 14,600 and 14,100 BP. Most of the recent dates available fall within a few hundred years of these.
Of the two periods, Bølling and Allerød, Bølling is the warmer and came on more suddenly. During it sea level rose about 35 m due to glacial melt. Ice uncovered large parts of north Europe and temperate forests covered Europe from 29 deg. to 41 deg. north latitude. After some pioneer vegetation, such as Salix polaris and Dryas octopetala, hardwoods, such as Quercus, and softwoods, Betula and Pinus, spread northward for a brief few hundred years.
During this time late Pleistocene animals spread northward from refugia in the three peninsulas, Spain, Italy and the Balkans. Geneticists can identify the general location by studying degrees of consanguinity in the modern animals of Europe. The hunting camps of ancient humans remain a major source of faunal fossils.
Animals hunted by humans are predominantly the big-game mammals: reindeer, horse, saiga, antelope, bison, woolly mammoth and woolly rhinoceros. In the alpine regions ibex and chamois were hunted. Throughout the forest were red deer. Smaller animals, such as fox, wolf, hare and squirrel also appear. Salmon was fished. For more details, see also the references to fauna under Oldest Dryas and Older Dryas.
Whittow, John (1984). Dictionary of Physical Geography. London: Penguin, 1984, p. 67. ISBN 0-14-051094-X.