Detailed Information on Publication Record
2023
Microbial degradation of Pleistocene permafrost-sealed fossil mammal remains
CALÁBKOVÁ, Gabriela, Jiří CHLACHULA, Martin IVANOV, Michaela HLOŽKOVÁ, Jolanta CZERNIAWSKA et. al.Basic information
Original name
Microbial degradation of Pleistocene permafrost-sealed fossil mammal remains
Authors
CALÁBKOVÁ, Gabriela (203 Czech Republic, guarantor, belonging to the institution), Jiří CHLACHULA (203 Czech Republic), Martin IVANOV (203 Czech Republic, belonging to the institution), Michaela HLOŽKOVÁ (203 Czech Republic, belonging to the institution), Jolanta CZERNIAWSKA (616 Poland), Michaela VAŠINOVÁ GALIOVÁ (203 Czech Republic), Lubomír PROKEŠ (203 Czech Republic, belonging to the institution) and Petr GADAS (203 Czech Republic, belonging to the institution)
Edition
Quaternary Research, Cambridge University Press, 2023, 0033-5894
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10506 Paleontology
Country of publisher
United States of America
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 2.300 in 2022
RIV identification code
RIV/00216224:14310/23:00130003
Organization unit
Faculty of Science
UT WoS
000840361100001
Keywords in English
Pleistocene; Yakutia; Yana Basin; Batagay thermokarst sinkhole; Permafrost; Fossil osteological material; Diagenesis; MIS 3 environment; Fauna remains preservation
Tags
Tags
International impact, Reviewed
Změněno: 4/3/2024 16:03, Mgr. Marie Šípková, DiS.
Abstract
V originále
Paleontological remains retrieved from permafrost represent the most informative records of Pleistocene ecosystems. Different levels of past microbial activity affecting fossil material preservation are presented for two selected bone samples—an almost intact Bison sp. metacarpus (45.0 ± 5.0 14C ka BP) and a weathered Equus sp. metacarpus (37.8 ± 1.7 14C ka BP) from the recently exposed cryogenic geo-contexts in the Yana River basin, NE Yakutia. Diagenetic changes in bone porosity and chemical composition as a result of the past microbial activity were investigated by multiple analytical methods. In the bison bone, which was permafrost-sealed shortly after death of the animal and conserved for ca. 45 ka in a frozen state in a cryolithic formation, only superficial microbial degradation processes were detected. Progressive microbial attacks characterize the horse bone, which was exposed to MIS 3 sub-aerial biogenic decay and modern surficial weathering. This is evidenced by extensive bacterial micro-boring with the typical focal destructions, an increase in microbial porosity, and de-mineralized osseous zones due to waterlogged and poorly oxygenated past depositional conditions. New information contributes to better understanding of the diagenesis particularities and the associated chemical and biological agents of the fossil osteological assemblages with respect to their taphonomic and paleoenvironmental implications.
Links
MUNI/A/1263/2020, interní kód MU |
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MUNI/A/1390/2020, interní kód MU |
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