Zobrazeno 1 - 10
of 48
pro vyhledávání: '"E.M. Zelikson"'
Publikováno v:
Quaternary International. 237:65-73
Pollen analyses and radiocarbon dates from Zhukovskoye peat mire (56°20′N, 84°50′E), situated in the south-eastern part of the boreal forest (taiga) zone of West Siberia, suggest that climatic oscillations of the Lateglacial were well expressed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c1f4964be0c383983890eddc77d0229
https://doi.org/10.1016/j.quaint.2011.01.015
https://doi.org/10.1016/j.quaint.2011.01.015
Autor:
Elena Novenko, T. Boettger, Andrei A. Velichko, Valentina V. Pisareva, Frank W. Junge, E.M. Zelikson
Publikováno v:
Boreas. 34:207-219
Velichko, A. A., Novenko, E. Y., Pisareva, V. V., Zelikson, E. M., Boettger, T. & Junge, F. W. 2005 (May): Vegetation and climate changes during the Eemian interglacial in Central and Eastern Europe: comparative analysis of pollen data. Boreas, Vol.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c41e50c77b30a127376c75292a3c3f13
https://doi.org/10.1111/j.1502-3885.2005.tb01016.x
https://doi.org/10.1111/j.1502-3885.2005.tb01016.x
Publikováno v:
Boreas. 37:1-19
Main climatic indexes (mean January, July and annual temperatures; duration of the frost-free period; seasonal and annual precipitation; and annual potential evaporation) are estimated for the Last Interglacial Eemian–Mikulino–Kazantsevo–Oxygen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d2aed5c47e98500053224f294f03db4
https://doi.org/10.1111/j.1502-3885.2007.00001.x
https://doi.org/10.1111/j.1502-3885.2007.00001.x
Autor:
E.M. Zelikson, A.A. Velichko
Publikováno v:
Quaternary International. :137-151
Typical mammoth inhabited the East European Plain during the second half of the Late Pleistocene glaciation. Under conditions of extremely arid climate, periglacial, mostly open landscapes formed a vast hyperzone (cryohyperzone) that occupied the pla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::afaa0166decad4fa427d3526b572c35f
https://doi.org/10.1016/j.quaint.2004.04.019
https://doi.org/10.1016/j.quaint.2004.04.019
Publikováno v:
Chemical Geology. 159:191-204
The phytomass (the biomass of terrestrial vegetation) is one of the main reservoirs of carbon, as carbon makes up approximately 0.45 of the phytomass by weight [Ajtay, G.L., Ketner, P., Duvigneaud, P., 1979. Terrestrial primary production and phytoma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2e9aad45a5bf0cb9c84ae9377df8c9e
https://doi.org/10.1016/s0009-2541(99)00029-7
https://doi.org/10.1016/s0009-2541(99)00029-7
Autor:
T. D. Morozova, V. A. Klimanov, A. N. Drenova, Olga K. Borisova, Yu. M. Kononov, I. I. Spasskaya, Ye. I. Kurenkova, A.A. Velichko, E.M. Zelikson, V. P. Nechayev, M. A. Faustova
Publikováno v:
Scopus-Elsevier
The authors describe the evolution of a new field in cartography—the substantive basis of which is the preparation of a series of spatial reconstructions (climate, landscape components) of the past on the basis of principles of comprehensive mappin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::92953ae8d0483d91dcf7cd6e0fb47a71
https://doi.org/10.1080/07493878.1999.10642104
https://doi.org/10.1080/07493878.1999.10642104
Autor:
V. P. Nechaev, E.M. Zelikson, Olga K. Borisova, Constantine V. Kremenetski, A.A. Velichko, H. Faure
Publikováno v:
Global and Planetary Change. :159-180
The concentration of methane in the atmosphere has varied considerably during the last 125,000 years. Boreal wetlands represent one of the main sources of methane emissions into the atmosphere, the rate of which is largely controlled by climate. Chan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3034df3040733210bc241ba5e3a9fec0
https://doi.org/10.1016/s0921-8181(98)00032-0
https://doi.org/10.1016/s0921-8181(98)00032-0
Publikováno v:
Global and Planetary Change. :181-195
The phytomass stored in terrestrial vegetation at 5.5, 18 and 125 Ka BP, representing the environmental extremes of the Late Quaternary, was estimated for the Russian Plain, excluding the northern coast and adjacent piedmont. The estimates are based
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6400c88ad758ae8b65a9b1ce2a050d3b
https://doi.org/10.1016/s0921-8181(98)00031-9
https://doi.org/10.1016/s0921-8181(98)00031-9
Autor:
E.M. Zelikson
Publikováno v:
Quaternary International. :97-101
Tundra vegetation during the Allerod optimum was limited to the fringe of the Scandinavian ice sheet and the Kola Peninsula. In contrast, forest-tundra vegetation assemblages, including birch, pine and spruce, were much more extensive, reaching the A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfa874dd125fe93d68ee4c247e3b2ee0
https://doi.org/10.1016/s1040-6182(96)00040-7
https://doi.org/10.1016/s1040-6182(96)00040-7
Autor:
E.M. Zelikson
Publikováno v:
GeoJournal. 36:223-228
Basic climatic indexes for loess deposits may be determined by the floristic method of palaeoclimatic reconstruction. Spectra of loess pollen are selective, thus may or may not reflect adequately the original composition of the vegetation. Presence o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8164e1a239c4e40fb4c4b3465ff2421e
https://doi.org/10.1007/bf00813174
https://doi.org/10.1007/bf00813174