Kj. Willis et al., The role of sub-Milankovitch climatic forcing in the initiation of the Northern Hemisphere glaciation, SCIENCE, 285(5427), 1999, pp. 568-571
Mechanisms responsible for the initiation of major glaciation in the Northe
rn Hemisphere at about 2.75 million years ago are poorly understood. A Lami
nated terrestrial sequence from Pula maar, Hungary, containing about 320,00
0 years in annual Layers between 3.05 and 2.60 million years ago, provides
a detailed record of rates of climatic change across this dramatic transiti
on. An analysis of the record implies that climatic variations at sub-Milan
kovitch frequencies (less than or equal to 15,000 years) were an important
driving force during this transitional interval and that, as the threshold
was approached, these increased in frequency and amplitude, possibly provid
ing the final trigger for the amplification of Northern Hemisphere ice shee
ts.