Grusha and 12 for Akkol) were used to reconstruct the vegetational history since the last glaciation. The core from Grusha contains about 50 cm of Late Glacial sediment of relatively low organic content, mostly correlated with the Younger Dryas episode because Palaeogeography, Palaeoclimatology, Pal...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.1461
http://www.botany.unibe.ch/paleo/publications/reprints/PaleogeogrPaleocl_245_518.pdf