Radiocarbon dating holocene
proposed the designation Recent for the period that has elapsed since “the earth has been tenanted by man.” It is now known that humans have been in existence a great deal longer. The preceding and substantially longer sequence of alternating glacial and interglacial ages is the .
The term Holocene was proposed in 1867 and was formally submitted to the International Geological Congress at Bologna, Italy, in 1885. Because there is nothing to suggest that the Pleistocene has actually ended, certain authorities prefer to extend the Pleistocene up to the present time; this approach tends to ignore humans and their impact, however.
The mosaic picture of woodland and wetland, which covered this landscape during the Upper Holocene, contrasts with the present day monotonous open lowland.
Sediments of the peat bog provide information on the origin and vegetation evolution of this area.
Age determination with high accuracy as well as high resolution is a principal procedure in the research of Quaternary processes, such as volcanic eruptions, lacustrine and ocean sedimentation, and recent fault activation, for investigating past global environmental changes and predicting the realistic changes in the near future.
A progressive southward migration of the locus of crustal upwarping is demonstrated over a distance of 380 km within a period of about 3,500 years.
*Prices in US$ apply to orders placed in the Americas only.
Prices in GBP apply to orders placed in Great Britain only.
Prices in € represent the retail prices valid in Germany (unless otherwise indicated). Prices do not include postage and handling if applicable. The paper reports the results of a palynological study of a newly exposed section in the peat sediments of Bezděkov site and its correlation with the previous palaeobotanical studies.
The main goal was to elucidate the stratigraphic position and paleogeographic development of fossil peat bog and its environment in the Protected Landscape Area Žďárské vrchy and Železné hory in the Bohemian-Moravian Uplands.