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  • Late Pleistocene–Holocene environmental changes in ultra-continental subarid permafrost-affected landscapes of the Terekhol' Basin, South Siberia
  • This study is an attempt to use closely related inter-complementary paleo-archives of a local landscape to access understanding of Late Pleistocene–Holocene environmental changes in the region. The study site is a small intermountain basin
  • permafrost sub–arid/arid conditions persist in the basin within the studied period. The following sequence of environmental changes was established : 11 000 and 4 000 cal yrs BP are characterized by well balanced climatic moistening; progressive aridization
  • 2014
  • Quaternary paleosols and sediments on the Balearic Islands as indicators of climate changes
  • 2014
  • (Ljubljansko barje). The past environment and vegetation changes were studied. The AA. reconstruct lifestyle of Eneolithic settlement. The palaeoenvironmental reconstruction before, during and after prehistoric settlement is presented.
  • 2014
  • shrinking through time and the grass areas increasing. Both isotope and phytolith records demonstrate a contrasting difference between Pleistocene and recent vegetation dominated by xerophytic shrubs and succulents. This vegetation change could play
  • 2014
  • and Stavropol regions in Russia, and Samara in Ukraine. This transect represents the changes of climate (MAP and MAT) and vegetation (increasing of C4-plants portion under the domination of C3-vegetation). Isotopic composition of soft carbonates, corresponding
  • 2014