Late- and postglacial history of lakes of the Karelian Isthmus

  title={Late- and postglacial history of lakes of the Karelian Isthmus},
  author={Natalia N. Davydoval and Kh. A. Arslanov and Valentina I. Khomutova and I. I. Krasnov and Dmitry B. Malakhovsky and Matti Saarnisto and Alexander Saksa and Dmitry A. Subetto},
The Late Pleistocene and Holocene history of five lakes in the central part of Karelian Isthmus, south of the present Vuoksi River, are described on the basis of sediment stratigraphical investigations. Two of the Lakes, Michurinskoe (94 m a.s.l.) and Uzornoe (55 m a.s.l.) are situated in an upland area that remained dry land after the deglaciation even during the early high water stages of the Baltic Sea (Baltic Ice Lake until c. 10 000 yr BP and Ancylus Lake 9500–8800 BP). The low-lying… 
Late-Glacial and Early Holocene Environmental and Climatic Change at Lake Tambichozero, Southeastern Russian Karelia
Abstract High-resolution lithostratigraphy, mineral magnetic, carbon, pollen, and macrofossil analyses, and accelerator mass spectrometry 14C measurements were performed in the study of a sediment
Palaeoecological and palaeoclimatic conditions on the Karelian Isthmus (northwestern Russia) during the Holocene
Abstract The Holocene evolution of climate in easternmost Fennoscandia and adjoining regions is poorly known, compared with regions to the west. To address this, a 224-cm-long sediment core from Lake
Climate and environment on the Karelian Isthmus, northwestern Russia, 13000‐9000 cal. yrs BP
Sediment sequences retrieved from Lake Medvedevskoye (60°13'N; 29°54'E) and Lake Pastorskoye (60°13'N; 30°02'E), Karelian Isthmus, northwestern Russia, were analysed for lithology, pollen and diatom
Holocene hydrological variability of Lake Ladoga, northwest Russia, as inferred from diatom oxygen isotopes
This article presents a new comprehensive assessment of the Holocene hydrological variability of Lake Ladoga, northwest Russia. The reconstruction is based on oxygen isotopes of lacustrine diatom
Lake stratigraphy implies an 80 000 yr delayed melting of buried dead ice in northern Russia
Sediment cores from lakes Kormovoye and Oshkoty in the glaciated region of the Pechora Lowland, northern Russia, reveal sediment gravity flow deposits overlain by lacustrine mud and gyttja. The
Important Pre-requisites for the Existence of Lakes: Basin and Depression Forming Processes
Abstract for Sect. 2.1 All lakes are positioned in basin-like forms on continental surfaces. Many lakes are so large it is difficult to identify these depressions such as the Caspian Sea, Victoria
Lakes of the World with Google Earth: Understanding our Environment
Although continental water represents only a very small percentage of all our global water, it occurs in a multitude of different facets and whether hidden under the surface as groundwater, in the
Index to Hydrobiologia Volumes 251-384 (1993-1999)


Ayrapal njarven vesikasvillisuudesta
  • (German summary: Uber die Wasservegetation des Ayrapaanjarvi-Sees) . Ann. Bot. Soc . Zool . Bot . Fenn . Vanamo
  • 1933
The LateQuaternary land uplift in the Baltic sphere and the relation diagram of the reised and tilted shore levels
  • Ann . Acad . Sci . Fennica Ser . AIII
  • 1990
Novye dannye golotsenovoi istorii Ladozhskogo ozera
  • 1993
Ayrapal njarven vesikasvillisuudesta . ( German summary : Uber die Wasservegetation des AyrapaanjarviSees )
  • Ann . Bot . Soc . Zool . Bot . Fenn . Vanamo
  • 1933
The Late Weichselian and Flandrian history of the Saimaa lake complex
  • Soc . Sci . Fennica, Comment. Phys . Math
  • 1970
Yoldievoe more i problema pozdielednikovogo Belomorsko-Baltiiskogo soedineniya
  • Izv . Gos . Geogr. Obshestva
  • 1935