J 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
Name: Sedimentární záznam depozičních pánví Českého masívu a Západních Karpat (Acronym: SZDP)
Investor: Masaryk University
MUNI/A/1390/2020, interní kód MU
Name: Analytická a fyzikální chemie ve výzkumu biologických, geologických a syntetických materiálů (Acronym: BIOGEOSYNT)
Investor: Masaryk University