The hot spring deposits near Magyarkút and their paleobotanical analysis (Börzsöny Mountains, Hungary)
to the researches based on geomorphological and paleobotanical methods, the study assumes that a hot spring activity of postvolcanic origin took place in a time interval during the Middle to Late Miocene, in a subtropical environment. Besides the already known
The A. examines ecological theory, existing maps, and explorer journals, with the support of data on contemporary grass patterns and interpretation of the grassland paleobotanical record built from anlyses of opal phytoliths that were contained
Paleobotanical analyses indicate that the mastodont diet included significant amounts of low, herbaceous vegetation. Enteric bacteria (Enterobacter clocae), isolated from a sample of this material, are believed to represent survivors or descendants
As a result of investigations of paleobotanical materials taken from Cretaceous deposits of Kul'dzhuktau mountains in the Kyzylkum 3 different floras are determined : the Early Albian, the Late-Albian-Cenoman and Turon ones. Ferns prevailed
Reported here is the significance of 2 new Pleistocene plant records for western Europe resulting from a paleobotanical investigation of a French Middle Pleistocene temperate stage site at Trez Rouz, Brittany, by western European paleobotanists
-year-B.P. model results also suggest trends opposite to the paleobotanical data, with simulated cooler winter temperatures and drier conditions than present during the climatic optimum.
The results of geomorphological research in the Labský Důl Valley Giant Mts. New evidence regarding landscape development during the Pleistocene glaciations and the Holocene. Paleobotanical evidence prove the existence of a lake in the cirque floor
of these different deposits and their stratigraphical correlations from paleobotanical data and from 14C datations are discussed. The complete stratigraphical series is believed to include the Riss-Würm, the Mesowürm and the Neowürm.
A paleogeographic reconstruction of the region has been carried out based on the new data obtained due to complex investigations of ancient Sarykamysh basin (Northern Turkmenistan). Paleobotanical and geomorphological materials used
mats around Nagqu, 4 profiles were subjected to pedological, paleobotanical and geochronological analyses concentrating on soil properties, phytogenic composition and dating of the turf. The results show that the turfs result from the transformation
of the landscape was a late phenomenon, whose acceleration in both Provence and Languedoc, as paleobotanical research indicates can be dated to the 13th-14th centuries.
The study area, Axamilpa, is located close to the town of Tepexi de Rodríguez in the state of Puebla. The goal of this work is to reconstruct the past environmental conditions through the study of 3 proxies : paleosols, paleobotanical records
not yet been climatically subdivided. Correlation with the Netherlands is possible because of an abundance of paleobotanic and paleomagnetic evidence. In the Alpine foothills, stratigraphically useful indicators of warm climates are missing, but analogies