Ph.D. thesis
Quaternary karst in the valley of Rusenski Lom River and its tributaries
The aim of this investigation is a
description of the young karst forms and establishing their
genesis and age in the valley of Rusenski Lom River and its
tributaries - Cherni Lom River, Beli Lom River and Malki Lom
River (NE Bulgaria). The last stage of karstifikation is
determined from Late Romanian Time until our days by study on
geological features and surfaces. The past conditions and
development of the valley during the last stage of karstification
are established by investigating alluvium, loess-paleosol
sequence and river terraces. Four units in the river deposits are
separated and they are correlated with sediments in the Late
Romanian - Young Pleistocene basin. Fourteen river terraces are
recorded.The ages of most of them are determinate.
The known 56 caves in the region are described in details and
systematized in a new classification on the base of their
morphogenetic features. The structural and hydraulic control on
forming the caves, their genesis and some regularities of karst
are recognized. A new genetic model for Orlova Chuka Cave is
propounded. The sediment sequences in five sites in the Orlova
Chuka Cave are analyzed and lithofacial types are set off.
Paleoclimatic record of one of the sites is studied by comparing
some physical parameters - grain size, carbonate content,
magnetic susceptibility and organic carbon content. 579 remnants
of micromammals and an individual of Ursus cf. deningeri have
been found into the sediments from the same site. The remnants of
micromammals present minimum 35 species of orders Insectovora,
Lagomorpha, Rodentia and Chiroptera. The results of
paleoecological analysis of micromammals conform the results of
comparing the physical parameters. They manifest alternation of
periods of cold and arid, cold and humid, and temperate climate
in general cold conditions during depostion.
Last Update: December 17, 2005
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