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

特別容易碎

dysphagia

The Classical Late Weichselian Climatic Fluctuations in Mexicontarctica). Recent investigations give more and more evidence that the classical West European chronostratigraphy of the Late Weichselian in many details is a . stratigraphy and cannot be transferred to other areas of the world.

left-ventricle

The Reflection of Abrupt Climatic Changes in the Relief and Sequence of Continental Depositsposits in the temperature zone. The following abrupt changes are discussed for the last 11000 years; 10.9–10.6 Ka, 8.4–8.0 Ka, 5.0–4.5 Ka, 2.8–2.4 Ka BP and the Little Ice Age. The following abrupt climatic changes have been distinguished: a/abrupt warmings and coolings and b/short waves of increased humidity and increased flood frequency.

豪華

Hyperplasia

Parallel

解脫

Biotic Response to Climatic Changes during the Time Span 13,000–10,000 B.P. — a Case Study from SW Ses 13,000–12,500 followed by a gradual deterioration until 11,000 when a sudden drop of temperature leads to a minimum between 11,000 and 10,500. A distinct rise of summer temperature around 10,500 is confirmed although the time lag in the vegetation response is ab. 300 years.

cleaver

憤慨一下

Grundlagen des Projektmanagements,undqvist, 1961; Nilson, 1968; M?rner, 1969; Berglund, 1979). We realize that there are still serious problems connected with the identification and correlation of deglaciation features and their proper dating and relation to biozonation and paleoclimatic cold/warm periods.

藕床生厭倦