A cave response to environmental changes in the Late Pleistocene: a study of Budimirica Cave sediments, Macedonia
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F16%3A00464669" target="_blank" >RIV/67985831:_____/16:00464669 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.4154/gc.2016.29" target="_blank" >http://dx.doi.org/10.4154/gc.2016.29</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.4154/gc.2016.29" target="_blank" >10.4154/gc.2016.29</a>
Alternative languages
Result language
angličtina
Original language name
A cave response to environmental changes in the Late Pleistocene: a study of Budimirica Cave sediments, Macedonia
Original language description
Budimirica Cave is a small cave located in the southern part of the Republic of Macedonia, in the Kamenica Valley, a tributary to the Crna Reka and part of the Vardar river drainage network. The response of the cave to Late Pleistocene environmental changes is interpreted based on a detailed study of cave sediments, with previous data being supplemented, reinterpreted and compared to the Ohrid Lake palaeoclimate record. The oldest exposed speleothems in the Budimiricansediment profile were deposited during the MIS 5a (radiometric age of ca 83 ka). Sands to clays in the overburden are characterized by cycles separated by short-lived interruptions in deposition. They were deposited from a number of repeated flood events likely during the MIS 4 stage, the Weichselian (Wurmian) Glaciation, correlating to aggradation in the Kamenica Valley. The top flowstone is correlated with a warmer climate excursion at 45–50 ka (MIS 3) recordednfrom the Ohrid Lake deposits. The whole section was extensively eroded during the MIS 2 stage, due to strong incision in the Kamenica Valley, indicated by knickpoint retreat. The erosion surface is overlain by a fossil-bearing breccia (with Ursus spelaeus) derived from frost shattering of the cave walls close to the entrance due to climate deterioration and enlargement of the entrance by slope retreat during the MIS 2 stage. Budimirica Cave sediments reflect changes innthe Kamenica Valley, as well as the environmental changes during the last glacial-interglacial cycle, with clastic cave sediments deposited during glacial stadials, and erosion and flowstone deposition characteristic of the interstadials. They also allow reconstruction of the evolution of the Kamenica Valley during the Late Pleistocene, with a general trend of valley incision hindered by climate influenced river aggradation, but reinforced by river knickpoint retreat.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geologia Croatica
ISSN
1330-030X
e-ISSN
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Volume of the periodical
69
Issue of the periodical within the volume
3
Country of publishing house
HR - CROATIA
Number of pages
10
Pages from-to
307-316
UT code for WoS article
000386655500003
EID of the result in the Scopus database
2-s2.0-84991594122