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Subfossil cladocera from boreal lake gahkozero (The republic of Karelia, Russia) as paleoenvironmental proxies of macrophytes in the lake. The history of the development and the evolution of the lake is traced by the change

Late Pleistocene-Holocene and Recent Ostracoda of the Laptev Sea and their importance for paleoenvironmental reconstructions. Data on recent Ostracoda are used for paleoenvironmental reconstructions on the eastern shelf

CONTINUOUS PALEOENVIRONMENTAL SEDIMENT RECORD FROM TWO LAKES ON VALDAY ICE MARGINAL ZONE STARTED SHORTLY AFTER THE ICE RETREATCONTINUOUS PALEOENVIRONMENTAL SEDIMENT RECORD FROM TWO LAKES ON VALDAY ICE MARGINAL ZONE STARTED

Multi-proxy evidence of late-Holocene paleoenvironmental change at Princessvlei, South Africa: The effects of fire, herbivores, and humans, indicate vegetation disturbances caused by climatic changes, anthropogenic influences, fire, and herbivore

FERROMAGNETIC, DIA-/PARAMAGNETIC AND SUPERPARAMAGNETIC COMPONENTS OF ARAL SEA SEDIMENTS: SIGNIFICANCE FOR PALEOENVIRONMENTAL RECONSTRUCTION.-field susceptibility in order to better understand and to interpret environmental changes. This new method is based

Cladocera from bottom deposits as an indicator of changes in climate and ecological conditions
indicators in paleoenvironmental studies and paleoreconstructions of abiotic conditions of the past.

Subfossil cladocera from boreal lake gahkozero (The republic of Karelia, Russia) as paleoenvironmental proxies of macrophytes in the lake. The history of the development and the evolution of the lake is traced by the change

Upper Paleolithic site Tuyana – a multi-proxy record of sedimentation and environmental history during the Late Pleistocene and Holocene in the Tunka rift valley, Baikal region detailed record of the change in environment and climate of the ancient humans’ habitation in the Tunka

Geodatabase of buried soils for reconstruction of palaeoecologic conditions in the steppe zone of East European plain climatic changes and soil types during the Subboreal and Subatlantic ages of the Holocene has been

Reconstructions of Paleoecological and Paleoclimatic Conditions of the Late Pleistocene and Holocene according to the Results of Chironomid Analysis of Sediments from Medvedevskoe Lake (Karelian Isthmus)
of changes in natural and climatic settings allows one to reconstruct paleoclimatic and paleoenvironmental

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