Late Glacial erosion and pedogenesis dynamics: Evidence from high-resolution lacustrine archives and paleosols in south Bohemia (Czech Republic)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388980%3A_____%2F17%3A00480522" target="_blank" >RIV/61388980:_____/17:00480522 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/17:00480522 RIV/00216208:11310/17:10330484 RIV/00216208:11620/17:10330484 RIV/00025798:_____/17:00000011
Result on the web
<a href="http://dx.doi.org/10.1016/j.catena.2016.11.022" target="_blank" >http://dx.doi.org/10.1016/j.catena.2016.11.022</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.catena.2016.11.022" target="_blank" >10.1016/j.catena.2016.11.022</a>
Alternative languages
Result language
angličtina
Original language name
Late Glacial erosion and pedogenesis dynamics: Evidence from high-resolution lacustrine archives and paleosols in south Bohemia (Czech Republic)
Original language description
Sediments from three paleolakes and two paleosol horizons in south Bohemia, Czech Republic, provide evidence of climate change and landscape evolution in central-eastern Europe on millennial to centennial thhescales over the Late Glacial (similar to 16-11.5 ky). Based on a combination of geochemical, sedimentological and geophysical proxy indicators, along with the pollen record and soil micromorphology, we propose a relationship between vegetation cover, soil development, and erosional processes. Four major and two minor environmental stages, identified in all investigated paleo-lakes, were broadly correlated with the Late Glacial climatostratigraphy. Short-term (decadal to centennial) climatic deteriorations between the Bolling and Allerod, and within the Allerod, have been correlated with the Older Dryas and the Infra-Allerod Cold Period (IACP) respectively. B horizons of two (gleyic) podzols discovered under aeolian sand dunes in the lake catchments were dated to the Allerod interstadial and were parallelized with Usselo soils - pedostratigraphical marker horizons of west-and northern-central Europe. The upper parts of these soils have signs of colluvial processes. According to the radiocarbon dating, the erosion occurred at 13,155 150 cal. yr BP and can be associated with the IACP event, which is marked by a significant input of allogenic material into the lake basins. We attribute the significant increase in the iron and consequent phosphorus content in the lake sediments during the Allerod to the podzolization that occurred with the humid interstadial conditions.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/GA13-08169S" target="_blank" >GA13-08169S: Prior to the Neolithic: Contextual Analysis of Environmental Dynamics During Early Postglacial Transformation of Central Europe.</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
CATENA
ISSN
0341-8162
e-ISSN
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Volume of the periodical
150
Issue of the periodical within the volume
March 2017
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
18
Pages from-to
261-278
UT code for WoS article
000392686000027
EID of the result in the Scopus database
2-s2.0-84999289104