Microbial degradation of Pleistocene permafrost-sealed fossil mammal remains

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F23%3A00130003" target="_blank" >RIV/00216224:14310/23:00130003 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00094862:_____/22:N0000068 RIV/00216305:26310/22:PU147187

Výsledek na webu

<a href="https://www.cambridge.org/core/journals/quaternary-research/article/microbial-degradation-of-pleistocene-permafrostsealed-fossil-mammal-remains/36BFA00736486E77C4E4CECC58572ACE" target="_blank" >https://www.cambridge.org/core/journals/quaternary-research/article/microbial-degradation-of-pleistocene-permafrostsealed-fossil-mammal-remains/36BFA00736486E77C4E4CECC58572ACE</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1017/qua.2022.28" target="_blank" >10.1017/qua.2022.28</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Microbial degradation of Pleistocene permafrost-sealed fossil mammal remains

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

Microbial degradation of Pleistocene permafrost-sealed fossil mammal remains

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary Research

ISSN

0033-5894

e-ISSN

1096-0287

Svazek periodika

111

Číslo periodika v rámci svazku

January

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

23

Strana od-do

84-106

Kód UT WoS článku

000840361100001

EID výsledku v databázi Scopus

2-s2.0-85147520595