Quaternary correlations in Arctic Canada in Quaternary glaciations in the Northern Hemisphere.
In the Hudson Bay/James Bay Lowlands, along the coasts of Banks Island, and along the eastern coast of Baffin Island continuous and extensive sections in Quaternary sediments are rich in marine fossils, buried peats and soils and contain a wide
variety of glacigenic sediments together with glacial marine units and littoral deposits. Lake muds are also fairly common. All three areas possess very long records that may extend to the early Quaternary and Pliocene.
Glacial-marine sedimentation and Quaternary glacial history of Marguerite Bay, Antarctic Peninsula
Piston cores and single-channel seismic reflection data were collected during the Deep Freeze 85 and 86 expeditions to determine the late Quaternary history of the area. Seismic data in the bay show a rugged seafloor, with numerous deep troughs
Polar perspective of late-Quaternary climates in the southern hemisphere
Late-Quaternary paleoecological and glacial evidence from the higher latitudes of the Southern Hemisphere implies overall uniformity of large-scale glacial and interglacial climatic fluctuations for the past 40 000 yr. Climate of the last glacial
Zur Geomorphologie von S-Dickson Land (W-Spitzbergen) mit Schwerpunkt auf die quartären Vergletscherungsgeschichte. (Geomorphology of S. Dickson Land (W. Spitsbergen) with main emphasis on the Quaternary glacial history)
Jungquartäre Delta-und Flussentwicklung im glazialisostatischen Hebungsraum der Oobloyah Bay auf N-Ellesmere Island, N. W. T., Kanada = Delta and river history in the glacioisostatic uplift region of the Oobloyah Bay during the younger Quaternary
Bergs, barriers and Beringia: reflections on the peopling of the New World in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
The stages and routes of human occupation of the Beringian land bridge based on archaeological data in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
The AA. describe here late Quaternary paleoclimate, ice-volume change, and dynamics of the Ross ice drainage system using data from a powerful combination of drift sheets and ice cores.
The Holocene transgression on the Arctic flank of Beringia: Chukchi Valley to Chukchi Estuary to Chukchi Sea in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.