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Late Holocene climate and environmental changes in Kamchatka inferred from the subfossil chironomid recordThis study presents a reconstruction of the Late Holocene climate in Kamchatka based on chironomid

Late Holocene climate and environmental changes in Kamchatka inferred from the subfossil chironomid recordThis study presents a reconstruction of the Late Holocene climate in Kamchatka based on chironomid

Quantitative reconstructions of mid- to late holocene climate and vegetation in the north-eastern altai mountains recorded in lake teletskoye© 2016 Elsevier B.V.We report the first high-resolution (20-50 years) mid- to late Holocene pollen

Development of surficial deposits on Belyi Island (Kara Sea) during the Last 40,000 Years of dates from the Late Glacial period and from the Early Holocene (MIS 1 - ca. 14-9 ka cal BP) point

Quaternary deposits and biostratigraphy in caves and grottoes located in the Southern Urals (Russia)-steppes were widespread during Late Neopleistocene – Holocene. The forest vegetation existed during the warm

Mid-late Holocene environmental history of Kulunda, southern West Siberia: Vegetation, climate and humansAn environmental reconstruction of mid-late Holocene vegetation, climate and lake dynamics

Transformation of the Bryansk paleosol in microdepressions in the center of the East European forest-steppe during the maximum of valdai glaciation and in the HoloceneRecent and Late Pleistocene soils of the central forest-steppe in the East European Plain have been

Mid-late Holocene environmental history of Kulunda, southern West Siberia: Vegetation, climate and humansAn environmental reconstruction of mid-late Holocene vegetation, climate and lake dynamics

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)
) in the Late Pleistocene and Holocene and the evolution of the ecosystem of Medvedevskoe Lake have been

RECONSTRUCTION OF TERIBERKA (KOLA PENINSULA) PEATLAND FORMATION CONDITION IN LATE HOLOCENE ACCORDING POLLEN DATA of peat in the vicinity of the village of Teriberka (Kola Peninsula) in the Late Holocene according

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