Results 211 to 220 of about 38,197 (265)
Soil microbial diversity, succession, and greenhouse gas cycling across a Greenlandic glacial chronosequence. [PDF]
FEMS Microbiol EcolMarsh G +4 more
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A late-glacial and post-glacial history of amsoldingersee and vicinity, Switzerland
Schweizerische Zeitschrift für Hydrologie, 1984 A multidisciplinary approach was used to study the Late-Glacial and Post-Glacial history of a Swiss Plateau lake. Pollen analysis revealed thirteen major changes in vegetation. A series of coordinated fluctuations in vegetation and lacustrine trophic status were found, which were partially interpreted as the result of climatic changes.
Lotter, André Franz, Boucherle, Mary M.
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Late Glacial Multidisciplinary Studies
, 2007 Amplitudes and rates of climate changes and environmental responses were especially high during the Late Glacial (ca. 16,000–11,500 years BP). By applying several methods on the same material (if possible on the same core to avoid correlation problems ...
B AMMANN +3 more
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Last Glacial Maximum, Late Glacial and Holocene of Patagonia
2022Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas.
Rabassa, Jorge Oscar +3 more
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The late proterozoic glacial era
Palaeogeography, Palaeoclimatology, Palaeoecology, 1985Abstract The Late Proterozoic glacial record is reviewed on a global basis as a setting and introduction for that part of the symposium concerned with West African tillites. No unequivocal glacial deposits have yet been recorded in the interval 1.0–2.0 Ga.
M.J. Hambrey, W.B. Harland
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Glacial and Late Glacial Processes in Western Iceland
Geografiska Annaler: Series A, Physical Geography, 1975The presence of glacial marine drift, a hybrid deposit containing sub-fossil shells of age about 12,000 years B.P.
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A note on the glacial and late glacial history of caithness
Geological Journal, 1981AbstractIt is generally accepted that in the last glaciation Scottish ice from the Moray Firth flowed to the northwest across Caithness depositing shelly drift. Examination of striae along the east coast of Caithness shows that some were formed by ice flowing into and not out of the Moray Firth.
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Late glacial and post‐glacial shorelines in north‐east Antrim
Irish Geography, 1965Abstract not available...
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