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Lake Kotokel

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Journal Article
Published: 01 April 2011
Russ. Geol. Geophys. (2011) 52 (4): 458–465.
...E.V. Bezrukova; P.E. Tarasov; N.V. Kulagina; A.A. Abzaeva; P.P. Letunova; S.S. Kostrova Abstract Pollen and AMS 14 C analyses of bottom sediments from the upper nine meters of the Lake Kotokel’ section were carried out. The regional climate and landscape dynamics during the Late Glacial...
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Journal Article
Published: 01 December 2024
Russ. Geol. Geophys. (2024) 65 (12): 1446–1467.
...G.A. Leonova; A.E. Maltsev; L.M. Kondratieva; V.A. Bychinsky; L.V. Miroshnichenko; S.K. Krivonogov Chemical composition of bottom sediments and pore waters of organic-mineral sediments (sapropel) of Lake Kotokel (Eastern Baikal region) has been studied, based on long drilling cores, 14.5 and 16.5 m...
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Journal Article
Published: 01 August 2016
Russ. Geol. Geophys. (2016) 57 (8): 1239–1247.
...S.S. Kostrova; H. Meyer; P.E. Tarasov; E.V. Bezrukova; B. Chapligin; A. Kossler; L.A. Pavlova; M.I. Kuzmin Abstract This is a summary of new oxygen isotope record of diatoms from Lake Kotokel sediments, with implications for responses of the lake system and its environment to global change over...
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Scematic location map of <span class="search-highlight">Lake</span> <span class="search-highlight">Kotokel</span>, drilling and sampling sites.
Published: 01 December 2024
Fig. 1. Scematic location map of Lake Kotokel, drilling and sampling sites.
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Map of <span class="search-highlight">Lake</span> <span class="search-highlight">Kotokel</span> location.  1 , the KTK2 core;  2 , water sampling sites...
Published: 01 August 2016
Fig. 1. Map of Lake Kotokel location. 1 , the KTK2 core; 2 , water sampling sites.
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Lithology of KTK2 core from <span class="search-highlight">Lake</span> <span class="search-highlight">Kotokel</span>, assemblage composition and abunda...
Published: 01 August 2016
Fig. 2. Lithology of KTK2 core from Lake Kotokel, assemblage composition and abundances of diatoms ( Bezrukova et al., 2010 ), and δ 18 O, SiO 2 and Al 2 O 3 of diatom specimens. 1, black-brown gyttja; 2, gray-black silty clay; 3, laminated gray silty clay; 4, dark-gray silty clay; 5, position
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δ 18 O diatom  from <span class="search-highlight">Lake</span> <span class="search-highlight">Kotokel</span> sediments and landscapes vegetation (biome...
Published: 01 August 2016
Fig. 3. δ 18 O diatom from Lake Kotokel sediments and landscapes vegetation (biomes) in the lake basin reconstructed from pollen data ( Bezrukova et al., 2010 ), along with δ 18 O NGRIP variations as a proxy of Northern Hemisphere air temperature ( Svensson et al., 2008 ); δ 18 O variations
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Geographic location of <span class="search-highlight">Lake</span> <span class="search-highlight">Kotokel</span>’.
Published: 01 April 2011
Fig. 1. Geographic location of Lake Kotokel’.
Journal Article
Published: 01 November 2017
Russ. Geol. Geophys. (2017) 58 (11): 1401–1411.
..., concentration of biogenic silica, and sediment compaction indicate considerable variations of sedimentary environments during the Late Pleistocene and Holocene. Being compared with the previously reconstructed landscape and climate dynamics for the sedimentary succession of Lake Kotokel for this time interval...
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Production-macrophyte type of <span class="search-highlight">lake</span> ecosystems of the south of West Siberia ...
Published: 01 November 2019
Fig. 2. Production-macrophyte type of lake ecosystems of the south of West Siberia (Lake Minzelinskoe) ( A ), where macrophytes ( 1 ) are the main producers of OM. Production-phytoplankton type of lake ecosystems in the East Baikal region (Lake Kotokel’) ( B ), where phytoplankton ( 2
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Material composition of lacustrine sapropels: macrophytogenic of <span class="search-highlight">Lake</span> Bol’s...
Published: 01 November 2019
Fig. 4. Material composition of lacustrine sapropels: macrophytogenic of Lake Bol’shie Toroki ( A ) and Lake Minzelinskoe ( B ), peaty Lake Minzelinskoe ( C ), planktonogenic (Lake Kotokel’ ( D ) and Lake Dukhovoe ( E ), and planktonogenic-peaty (Lake Ochki: peat ( F ) and plankton ( G
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Lithological section and distribution curves of lithological, physical, and...
Published: 01 November 2017
Fig. 2. Lithological section and distribution curves of lithological, physical, and petromagnetic parameters of the sediments within the Baunt-2014 section, correlated with palynologically-derived dynamics of the natural landscapes of Lake Kotokel. 1, diatom ooze; 2, silty clay with diatoms; 3
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Correlation of the formation stages of carbonate coatings with regional and...
Published: 01 July 2020
) in the bottom sediments of Lake Kotokel’ ( Kostrova et al., 2016 ); c , NGRIP oxygen isotope scale as a proxy of atmospheric temperatures in the Northern Hemisphere (numbers show positive shifts in D–O events) ( Svensson et al., 2008 ); d , humidity dynamics in northern Mongolia (d1) and the Baikal region (d2
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SEM photo of bottom sediment of <span class="search-highlight">lakes</span> of the taiga zone of various regions:...
Published: 01 July 2023
Fig. 5. SEM photo of bottom sediment of lakes of the taiga zone of various regions: а – Lake Skazka (taiga zone, south of Eastern Siberia): 1 – quartz grain, 2 –micro-scale illite aggregate (Mg ≤ Fe), 3 – pyrite frambohedron; b – Lake Kotokel’ (taiga zone, south of Eastern Siberia): 1
Journal Article
Published: 01 November 2019
Russ. Geol. Geophys. (2019) 60 (11): 1278–1299.
...Fig. 2. Production-macrophyte type of lake ecosystems of the south of West Siberia (Lake Minzelinskoe) ( A ), where macrophytes ( 1 ) are the main producers of OM. Production-phytoplankton type of lake ecosystems in the East Baikal region (Lake Kotokel’) ( B ), where phytoplankton ( 2...
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Location map of the Baikal Rift. Numerals from 1 to 19 mark locations of re...
Published: 01 September 2012
and Babushka bays (18); Mindei Basin (19); Lake Kotokel (20). Dashed lines are major faults. Inset map in top left-hand corner shows distribution of heat-loving animals in the Pliocene–Eocene Sinian–Indian zoogeographic province ( Martinson, 1998 ). Numerals 1 to 4 mark regions of Arctic (1), Russian Far East
Journal Article
Published: 01 November 2018
Russ. Geol. Geophys. (2018) 59 (11): 1419–1432.
... – 66 . Bezrukova , E.V. , Krivonogov , S.K. , Takahara , H. , Letunova , P.P. , Shichi , K. , Abzaeva , A.A. , Kulagina , N.V. , Zabelina , Yu.S. , 2008 . Lake Kotokel as a stratotype for the Late Glacial and Holocene...
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Journal Article
Published: 01 January 1999
Russ. Geol. Geophys. (1999) 40 (1): 17–25.
... a different geodynamic framework. Both the underwater slope and the major marginal step above it are complexly structured, and their main elements are grouped into asynchronous genetic series. Neotectonic subsidence of step-like blocks (including the denuded pre-rift pediment like Lake Kotokel’ and Chivyrkui...
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Journal Article
Published: 01 April 2023
Russ. Geol. Geophys. (2023) 64 (4): 424–451.
... lakes studied by the authors of this paper, namely Lake Ochki and Lake Kotokel’, in which carbonate-free planktonogenic sapropel is formed ( Leonova and Bobrov, 2012 ; Leonova et al., 2014a , b , 2015 ; Bobrov et al., 2019 ; Maltsev et al., 2019a , b ). Table 7. Average chemical composition...
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Journal Article
Published: 01 July 2023
Russ. Geol. Geophys. (2023) 64 (7): 824–838.
...Fig. 5. SEM photo of bottom sediment of lakes of the taiga zone of various regions: а – Lake Skazka (taiga zone, south of Eastern Siberia): 1 – quartz grain, 2 –micro-scale illite aggregate (Mg ≤ Fe), 3 – pyrite frambohedron; b – Lake Kotokel’ (taiga zone, south of Eastern Siberia): 1...
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