Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake

© 2015 Elsevier B.V. Within the scope of Russian-German palaeoenvironmental research, Two-Yurts Lake (TYL, Dvuh-Yurtochnoe in Russian) was chosen as the main scientific target area to decipher Holocene climate variability on Kamchatka. The 5. ×. 2 km large and 26 m deep lake is of proglacial origin...

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Main Authors: Hoff U., Biskaborn B., Dirksen V., Dirksen O., Kuhn G., Meyer H., Nazarova L., Roth A., Diekmann B.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2014
Subjects:
Online Access:https://dspace.kpfu.ru/xmlui/handle/net/137212
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spelling ftkazanuniv:oai:dspace.kpfu.ru:net/137212 2023-05-15T16:58:33+02:00 Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake Hoff U. Biskaborn B. Dirksen V. Dirksen O. Kuhn G. Meyer H. Nazarova L. Roth A. Diekmann B. 2014 https://dspace.kpfu.ru/xmlui/handle/net/137212 unknown Global and Planetary Change 134 101 http://dspace.kpfu.ru/xmlui/bitstream/net/137212/-1/SCOPUS09218181-2014-134-SID84947047552-p1.pdf 0921-8181 https://dspace.kpfu.ru/xmlui/handle/net/137212 SCOPUS09218181-2014-134-SID84947047552 Diatoms Holocene Climate Kamchatka North Pacific Palaeolimnology Pollen Article 2014 ftkazanuniv 2022-01-01T09:46:43Z © 2015 Elsevier B.V. Within the scope of Russian-German palaeoenvironmental research, Two-Yurts Lake (TYL, Dvuh-Yurtochnoe in Russian) was chosen as the main scientific target area to decipher Holocene climate variability on Kamchatka. The 5. ×. 2 km large and 26 m deep lake is of proglacial origin and situated on the eastern flank of Sredinny Ridge at the northwestern end of the Central Kamchatka Valley, outside the direct influence of active volcanism. Here, we present results of a multi-proxy study on sediment cores, spanning about the last 7000 years. The general tenor of the TYL record is an increase in continentality and winter snow cover in conjunction with a decrease in temperature, humidity, and biological productivity after 5000-4500. cal. yrs. BP, inferred from pollen and diatom data and the isotopic composition of organic carbon. The TYL proxy data also show that the late Holocene was punctuated by two colder spells, roughly between 4500 and 3500 cal. yrs. BP and between 1000 and 200 cal. yrs. BP, as local expressions of the Neoglacial and Little Ice Age, respectively. These environmental changes can be regarded as direct and indirect responses to climate change, as also demonstrated by other records in the regional terrestrial and marine realm. Long-term climate deterioration was driven by decreasing insolation, while the short-term climate excursions are best explained by local climatic processes. The latter affect the configuration of atmospheric pressure systems that control the sources as well as the temperature and moisture of air masses reaching Kamchatka. Article in Journal/Newspaper Kamchatka Kazan Federal University Digital Repository Pacific
institution Open Polar
collection Kazan Federal University Digital Repository
op_collection_id ftkazanuniv
language unknown
topic Diatoms
Holocene Climate
Kamchatka
North Pacific
Palaeolimnology
Pollen
spellingShingle Diatoms
Holocene Climate
Kamchatka
North Pacific
Palaeolimnology
Pollen
Hoff U.
Biskaborn B.
Dirksen V.
Dirksen O.
Kuhn G.
Meyer H.
Nazarova L.
Roth A.
Diekmann B.
Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
topic_facet Diatoms
Holocene Climate
Kamchatka
North Pacific
Palaeolimnology
Pollen
description © 2015 Elsevier B.V. Within the scope of Russian-German palaeoenvironmental research, Two-Yurts Lake (TYL, Dvuh-Yurtochnoe in Russian) was chosen as the main scientific target area to decipher Holocene climate variability on Kamchatka. The 5. ×. 2 km large and 26 m deep lake is of proglacial origin and situated on the eastern flank of Sredinny Ridge at the northwestern end of the Central Kamchatka Valley, outside the direct influence of active volcanism. Here, we present results of a multi-proxy study on sediment cores, spanning about the last 7000 years. The general tenor of the TYL record is an increase in continentality and winter snow cover in conjunction with a decrease in temperature, humidity, and biological productivity after 5000-4500. cal. yrs. BP, inferred from pollen and diatom data and the isotopic composition of organic carbon. The TYL proxy data also show that the late Holocene was punctuated by two colder spells, roughly between 4500 and 3500 cal. yrs. BP and between 1000 and 200 cal. yrs. BP, as local expressions of the Neoglacial and Little Ice Age, respectively. These environmental changes can be regarded as direct and indirect responses to climate change, as also demonstrated by other records in the regional terrestrial and marine realm. Long-term climate deterioration was driven by decreasing insolation, while the short-term climate excursions are best explained by local climatic processes. The latter affect the configuration of atmospheric pressure systems that control the sources as well as the temperature and moisture of air masses reaching Kamchatka.
format Article in Journal/Newspaper
author Hoff U.
Biskaborn B.
Dirksen V.
Dirksen O.
Kuhn G.
Meyer H.
Nazarova L.
Roth A.
Diekmann B.
author_facet Hoff U.
Biskaborn B.
Dirksen V.
Dirksen O.
Kuhn G.
Meyer H.
Nazarova L.
Roth A.
Diekmann B.
author_sort Hoff U.
title Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
title_short Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
title_full Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
title_fullStr Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
title_full_unstemmed Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake
title_sort holocene environment of central kamchatka, russia: implications from a multi-proxy record of two-yurts lake
publishDate 2014
url https://dspace.kpfu.ru/xmlui/handle/net/137212
geographic Pacific
geographic_facet Pacific
genre Kamchatka
genre_facet Kamchatka
op_source SCOPUS09218181-2014-134-SID84947047552
op_relation Global and Planetary Change
134
101
http://dspace.kpfu.ru/xmlui/bitstream/net/137212/-1/SCOPUS09218181-2014-134-SID84947047552-p1.pdf
0921-8181
https://dspace.kpfu.ru/xmlui/handle/net/137212
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