Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

w10=
Найдено документов в текущей БД: 4

    Paleoecology and dynamics of forest ecosystems in Central Evenkia during the past 2400 years
[Text] / V. L. Koshkarova, A. D. Koshkarov // Russ. J. Ecol. - 2005. - Vol. 36, Is. 1. - P1-7. - Cited References: 21 . - 7. - ISSN 1067-4136
РУБ Ecology

Кл.слова (ненормированные):
plant macroremains -- the Holocene -- dynamics of forest ecosystems -- paleoclimate

Аннотация: New data on the composition of surface assemblages of plant macroremains from soil and swamp samples have been obtained in the study of geomorphologically different localities in the middle reaches of the Nizhnyaya Tunguska River. The results of paleocarpological analysis of forest soil sections supported by relevant palynological and geochronological data are presented. Natural changes of the forest cover over the past 2400 years and quantitative characteristics of the paleoclimate during each stage are described.

Полный текст,
WOS,
Scopus

Держатели документа:
Russian Acad Sci, Sukachev Inst Forest, Siberian Div, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Koshkarova, V.L.; Koshkarov, A.D.

    Is the 20th century warming unprecedented in the Siberian north?
/ O. V. Sidorova [et al.] // Quaternary Science Reviews. - 2013. - Vol. 73. - P93-102, DOI 10.1016/j.quascirev.2013.05.015 . - ISSN 0277-3791

Кл.слова (ненормированные):
Ice cores -- Pollen data -- Stable carbon and oxygen isotopes -- Taimyr -- Tree-rings -- Warming -- Ice core -- Pollen data -- Stable carbon -- Taimyr -- Tree rings -- Warming -- Carbon -- Cellulose -- Forestry -- Ice -- Isotopes -- Lakes -- Lasers -- Oxygen -- Trees (mathematics) -- carbon isotope -- coniferous forest -- data set -- dendrochronology -- Holocene -- ice core -- oxygen isotope -- paleoclimate -- paleoecology -- paleoenvironment -- palynology -- permafrost -- reconstruction -- stable isotope -- tree ring -- twentieth century -- warming -- Carbon -- Cellulose -- Forestry -- Ice -- Isotopes -- Lakes -- Lasers -- Oxygen -- Rings -- Trees -- Krasnoyarsk [Russian Federation] -- Lama Lake -- Russian Federation -- Siberia

Аннотация: To answer the question "Has the recent warming no analogues in the Siberian north?" we analyzed larch tree samples (. Larix gmelinii Rupr.) from permafrost zone in the eastern Taimyr (TAY) (72В°N, 102В°E) using tree-ring and stable isotope analyses for the Climatic Optimum Period (COP) 4111-3806 BC and Medieval Warm Period (MWP) 917-1150 AD, in comparison to the recent period (RP) 1791-2008 AD.We developed a description of the climatic and environmental changes in the eastern Taimyr using tree-ring width and stable isotope (?13C, ?18O) data based on statistical verification of the relationships to climatic parameters (temperature and precipitation).Additionally, we compared our new tree-ring and stable isotope data sets with earlier published July temperature and precipitation reconstructions inferred from pollen data of the Lama Lake, Taimyr Peninsula, ?18O ice core data from Akademii Nauk ice cap on Severnaya Zemlya (SZ) and ?18O ice core data from Greenland (GISP2), as well as tree-ring width and stable carbon and oxygen isotope data from northeastern Yakutia (YAK).We found that the COP in TAY was warmer and drier compared to the MWP but rather similar to the RP. Our results indicate that the MWP in TAY started earlier and was wetter than in YAK. July precipitation reconstructions obtained from pollen data of the Lama Lake, oxygen isotope data from SZ and our carbon isotopes in tree cellulose agree well and indicate wetter climate conditions during the MWP.Consistent large-scale patterns were reflected in significant links between oxygen isotope data in tree cellulose from TAY and YAK, and oxygen isotope data from SZ and GISP2 during the MWP and the RP.Finally, we showed that the recent warming is not unprecedented in the Siberian north. Similar climate conditions were recorded by tree-rings, stable isotopes, pollen, and ice core data 6000 years ago. В© 2013 Elsevier Ltd.

Scopus,
WOS,
Полный текст

Держатели документа:
Paul Scherrer Institute, 5232 Villigen, Switzerland
V.N. Sukachev Institute of Forest SB RAS, 660036 Krasnoyarsk, Akademgorodok, Russian Federation
Institute of Geology and Minerology, University of Koeln, 50674 Koln, Germany
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Research Unit Potsdam, 14473 Potsdam, Germany

Доп.точки доступа:
Sidorova, O.V.; Saurer, M.; Andreev, A.; Fritzsche, D.; Opel, T.; Naurzbaev, M.M.; Siegwolf, R.

    Ecologo-cenotic diversity of forests in the "Stolby" zapovednik (Eastern Sayan) in the Late Holocene
/ V. L. Koshkarova, A. D. Koshkarov // Geography and Natural Resources. - 2013. - Vol. 34, Is. 1. - P34-40, DOI 10.1134/S1875372813010058 . - ISSN 1875-3728
Аннотация: Results of paleocarpological analysis were used to reconstruct the dynamics of ecologo-phytocenotic diversity of forest cover on the territory of the "Stolby" zapovednik for the last 3500 years. В© 2013 Pleiades Publishing, Ltd.

Scopus,
Полный текст

Держатели документа:
Institute of Forest, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russian Federation
Krasnoyarsk State Pedagogical University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Koshkarova, V.L.; Koshkarov, A.D.

    Palaeoclimate chronology and aridization tendencies in the Transbaikalia for the last 1900 years
/ A. B. Ptitsyn [et al.] // Geography and Natural Resources. - 2010. - Vol. 31, Is. 2. - P144-147, DOI 10.1016/j.gnr.2010.06.009 . - ISSN 1875-3728
Аннотация: Within the long-term research program on reconstruction of palaeoclimatic characteristics of Central Asia, we carried out a palaeoreconstructions of climate aridity/humidity in the Transbaikalia, based on investigating layered palynological spectra and chemical composition of bottom sediments from Lake Arakhlei. It was found that the humid phases of climate on the time interval 90-2005 used in calculations exhibits a periodicity of 20-45 years, which roughly corresponds to the humidity cycles of Eurasia. В© 2010.

Scopus

Держатели документа:
Institute of Natural Resources, Ecology and Cryology SB RAS, Chita, Russian Federation
Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russian Federation
Institute of Forest SB RAS, Krasnoyarsk, Russian Federation
Environmental Change Research Centre, Department of Geography, University College London, United Kingdom
Siberian Federal University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Ptitsyn, A.B.; Reshetova, S.A.; Babich, V.V.; Daryin, A.V.; Kalugin, I.A.; Ovchinnikov, D.V.; Panizzo, V.; Myglan, V.S.