抄録
Pollen analysis was conducted at the Maebashi peat bed, late Pleistocene, Takasaki, Gunma. Paleovegetation of approximately 13 to 21 Ka was reproduced and local pollen zones were determined. The paleo vegetation of this age was primarily comprised of conifer trees of the subarctic to temperature zone mixed with deciduous broard-leaved trees. The combined occurrence of Fagus and Quercus, which are major deciduous broad-leaved trees of the cool temperature zone, was subject to changes consistent with the paleoclimate change curve.
