Results 201 to 210 of about 4,058,105 (258)

Cryptomeria Japonica: Glacial Refugia and Late‐Glacial and Postglacial Migration

Ecology, 1982
Cryptomeria japonica had multiple refugia in Japan where relatively moist, cool climates prevailed during the last glacial period. Its expansion began from scattered full—glacial centers of distribution °15 000 yr ago, reaching its maximum abundance from °7000—2000 yr ago.
openaire   +1 more source

Animal Invasion of Glacial and Late Glacial Terrestrial Environments in Scandinavia

Oikos, 1966
The problem of geographic origin and immigration routes of biota occurring in north-western Scandinavia in the latter part of the Wiirm glaciation is intimately connected with the development of the environments after the culmination of the Full Glacial period. Analyses of environments in Antarctica and their biotic communities give certain clues.
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Extinctions in North America's Late Glacial landscapes

Quaternary International, 2013
Human-caused extinctions of terrestrial mammals in large parts of the world such as North America may have been side-effects of rapid long-distance dispersals (biogeographic range-change) by Homo sapiens moving outward from the Old World. The extinctions help explain how modern humans briskly explored and populated large, empty, and increasingly ...
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The Late Ordovician glacial record

2008
An outline of the North Gondwanan, Late Ordovician glacial record is proposed. The related palaeogeographic domain extended from southern high palaeo-latitudes (southeastern Mauritania, Niger) to northern lower palaeo-latitudes (Morocco, Turkey, Sardinia) and covered a more than 4000 km-wide section perpendicular to ice-flow lines. Glacial advances are
Ghienne, Jean-François, Loi, Alfredo, Paris, Florentin, Rubino, Jean-Loup   +3 more
openaire   +2 more sources

Late glacial foraminifera

Geological Society, London, Special Publications, 1996
Knudsen, Karen Luise, Austin, William E.N.   +1 more
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Palaeogeography of late glacial vegetation

Nederlandse, Geografische Studies, 1997
The Weichselian Late glacial is the transition period between two metastable conditions, that of the last Glacial and that of the present Interglacial and can be placed in time between 13 000 and 10 000 14C-yr BP (Mangerud et al., 1974). The modelling of vegetation, environment and climate during ghis time-interval, with very dynamic (rapid changing ...
openaire   +1 more source

The paths and timing of late Paleozoic ice revisited: New stratigraphic and paleo-ice flow interpretations from a glacial succession in the upper Itararé Group (Paraná Basin, Brazil)

, 2018
T. Mottin, F. Vesely, Mérolyn Camila Naves de Lima Rodrigues, Felipe Kipper, Paulo A. Souza   +4 more
semanticscholar   +1 more source

Cosmogenic 36Cl glacial chronologies of the Late Quaternary glaciers on Mount Geyikdağ in the Eastern Mediterranean

, 2017
M. Sarıkaya, A. Çiner, C. Yıldırım
semanticscholar   +1 more source

Climate, pCO2 and terrestrial carbon cycle linkages during late Palaeozoic glacial-interglacial cycles

, 2016
I. Montañez, J. McElwain, C. Poulsen, J. White, W. DiMichele, Jonathan P. Wilson, G. Griggs, M. Hren   +7 more
semanticscholar   +1 more source

Carbonate isotopes from high altitude Tso Moriri Lake (NW Himalayas) provide clues to late glacial and Holocene moisture source and atmospheric circulation changes

, 2015
P. Mishra, S. Prasad, A. Anoop, B. Plessen, A. Jehangir, B. Gaye, Philip Menzel, S. Weise, A. Yousuf   +8 more
semanticscholar   +1 more source