Reconstruction holocene environmental changes in North-Western Pacific in relation to paleorecord from Shikotan Island

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Abstract


Results of a paleolimnological investigated of a well-dated lake sediment section from Shikotan Island (Southern Kurils) showed that from ca 8.0 to 5.8 cal ka BP warm and humid period corresponding to middle Holocene optimum took place. Cooling thereafter corresponds to Neoglacial. A reconstructed from ca 0.9 to ca 0.58 cal ka BP warm period can be correlated to a Medieval Warm Period. Cooling after 0.58 cal ka BP can be correlated with the LIA. Marine regression stages were identified at ca 6.2-5.9, 5.5-5.1 and 1.07-0.36 cal ka BP. The general chronology of major climatic events of Holocene in the island is in accordance with the climate records from the North Pacific region. Revealed spatial differences in timing and magnitude of the Late Holocene climatic episodes (LIA, MWP) within region needs further investigations.


About the authors

L. B. Nazarova

University of Potsdam, Institute of Earth and Environmental Science; Alfred-Wegener Institute, Helmholtz Centre for Polar and Marine Research, Research Unit Potsdam
 

Email: lyudmilalsd@gmail.com

Germany, 24-25 Karl-Liebknecht-Str., Potsdam-Golm, 14476; 12 Am Handelshafen, Bremerhaven, 27570

N. G. Razjigaeva

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 7, Radio Street, Vladivostok, 690041

B. Diekmann

University of Potsdam, Institute of Earth and Environmental Science; Alfred-Wegener Institute, Helmholtz Centre for Polar and Marine Research, Research Unit Potsdam
 

Email: lyudmilalsd@gmail.com

Germany, 24-25 Karl-Liebknecht-Str., Potsdam-Golm , 14476; 12 Am Handelshafen, Bremerhaven, 27570

Т. А. Grebennikova

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 7, Radio Street, Vladivostok, 690041

L. А. Ganzey

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 7, Radio Street, Vladivostok, 690041

N. I. Belyanina

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 7, Radio Street, Vladivostok, 690041

K. А. Arslanov

Saint-Petersburg State University

Email: lyudmilalsd@gmail.com

Russian Federation, 7/9, Universitetskaya embankment, Saint-Petersburg, 199034

V. М. Kaistrenko

Institute of Marine Geology and Geophysics, Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 1B, Nauka street, Yuzhno-Sakhalinsk, 693022

А. О. Gorbunov

Institute of Marine Geology and Geophysics, Far Eastern Branch of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 1B, Nauka street, Yuzhno-Sakhalinsk, 693022

А. А. Kharlamov

P.P. Shirshov Institute of Oceanology of Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 36, Nakhimovskii prospect, Moscow, 117997

L. V. Golovatyuk

Institute of Ecology of Volga Basin of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 10, Komzina street, Togliatti, 445003

L. S. Syrykh

Kazan Federal University; Herzen State Pedagogical University of Russia;
 

Author for correspondence.
Email: lyudmilalsd@gmail.com

Russian Federation, 18, Kremliovskaya street, Kazan, 420008; 48, Moika embankment, St.Petersburg, 191186;  

D. А. Subetto

Herzen State Pedagogical University of Russia; Karelian Research Center of the Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 48, Moika embankment, St.Petersburg, 191186; 11, Poushkinskaya street, Petrozavodsk, Karelia, 185910

A. P. Lisitsyn

P.P. Shirshov Institute of Oceanology of Russian Academy of Sciences

Email: lyudmilalsd@gmail.com

Russian Federation, 36, Nakhimovskii prospect, Moscow, 117997

Academician of the Russian Academy of Sciences

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