特别容易碎 发表于 2025-3-23 12:44:54
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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 发表于 2025-3-23 18:11:39
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.豪华 发表于 2025-3-23 22:18:20
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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 发表于 2025-3-24 15:19:32
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Grundlagen des Projektmanagements,undqvist, 1961; Nilson, 1968; Mörner, 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.藕床生厌倦 发表于 2025-3-24 23:29:10
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