Titlebook: Climatic Changes on a Yearly to Millennial Basis; Geological, Historic N.-A. Mörner,W. Karlén Book 1984 Springer Science+Business Media Dor

Homocystinuria

发源

Flora, Fauna and Stable Isotopes in Late-Würm Deposits at Lobsigensee (Swiss Plateau)imum depth 2.5 m. It was chosen as one of the primary reference sites in the Swiss contribution to IGCP 158b (LANG 1983). The littoral site “150” was investigated by various methods (AMMANN & TOBOLSKI 1983, GAILLARD 1983, ELIAS & WILKINSON 1983, HOFMANN 1983, CHAIX 1983, EICHER & SIEGENTHALER 1983,

小木槌

Late Weichselian Fluctuations in the French Alps and Massif Central from Pollen Analysess species refuges, as was shown by Van Campo & Aymonin (1962), Lang (1970), Beug (1975), Van der Hammen (1979), but also the variations of climate. These regions were not much affected by the Scandinavian inland ice; therefore they may have registered the first oscillations that took place at the en

Custodian

Climatic and Glacial Fluctuations during the Late-Glacial and the Holocene in Oisans (Isere, France)nges. Emphasis is laid on the thick and long-lasting snow cover. Besides these two recurrence periods, the major events observed mainly evidence the influence of drought: glacial regression and formation of rock- glaciers.

neutrophils

The Classical Late Weichselian Climatic Fluctuations in Mexicoto establish similar chronostratigraphies of climatic variations for other parts of the world (e.g. Chile, Western North America, New Zealand, South Antarctica). Recent investigations give more and more evidence that the classical West European chronostratigraphy of the Late Weichselian in many deta