Open AccessPALAEO-ECOLOGICAL CONDITIONSOF THE LEFT BANK OF THE KURA DURING NEOPLEISTOCENE
Author(s) -
Г. Халилов,
H. Khalilov,
Г. Мамедова,
G. Mammadova
Publication year - 2017
Publication title -
vestnik kemerovskogo gosudarstvennogo universiteta. seriâ: biologičeskie, tehničeskie nauki i nauki o zemle
Language(s) - English
Resource type - Journals
eISSN - 2542-2456
pISSN - 2542-2448
DOI - 10.21603/2542-2448-2017-1-60-66
Subject(s) - marine transgression , pollen , palaeogeography , sea level , oceanography , geology , ecology , paleontology , biology , tectonics , structural basin , volcanism
On the basis of litho-facial, chemical of the marine and continental sedimentanalyses, pollen spores assemblages were investigated on order to identify palaeogeography condition of the region. The research showed that during climatic changes, glaciations of the hill mountain and transgression of the Caspian Sea occurred during Turkan, the latestBaku, the earliest Khazar (second step), the late Khazar (second step), the early Khvalyn periods. The warming and transgression of the Caspian Sea in the area occurred during the earliestBaku, the earliest Khazar (first step), the early Khvalyn periods.