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- Volume 15 (1966)
Title: | Present achievments in a palynological study of the Quaternary period in the USSR |
Authors: | Neustadt, M.I. |
Issue Date: | 1966 |
Citation: | Palaeobotanist (1966) 15(1,2): 213-227 |
Abstract: | Enormous palynological data are accumulated
over the continental and marine deposits from the
various regions of the USSR.
Palynological data are usually applied together
with the geological ones. At a time diatoms and
large plant remains are analysed. The absolute
age determination by C 14 are in common use.
The general pattern of distribution and dynamic
of vegetation and natural zones in the Pleistocene
and Holocene are traced in large scale regions and
in all the country.
Palynological data serve usually as a main
criteria for the differentiation and subdivision of interglacials and interstadials with reference to their relative chronological estimates.
Palynological method is used also for the identification of the Pliocene-Pleistocene and Pleistocene-Holocene boundaries, for the sub-division of deposits into horizons and zones on the base of vegetational changes, for the determination of past climates, for the typization of interglacial, interstadial and holocene diagrams with reference to their geographical
position, time correlation, of marine transgressions etc.
There are found some sections representing
palynologically continuous vegetational development from the last interglacial to the present. The data from arid zone are very interesting to study pluvial and interpluvial periods.
Palynological data show the extremely complicated
development of the Pleistocene and Holocene
vegetation, the significant mobility and transformation of natural zones.
Only due to the use of palynological method it
became possible to study climatic conditions,
vegetational development and stratigraphical position of the Pleistocene and Holocene deposits. |
URI: | http://hdl.handle.net/123456789/528 |
Appears in Collections: | Volume 15 (1966)
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