Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate

The article focuses on the results of analysis of more than 100 thousand animal fossils recovered from Chagyrskaya Cave in 2007–2011. Animal remains from strata 5 and 6a result mostly from the hunting activity of wolves and cave hyenas, which used the cave as a shelter or den for breeding their offs...

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Main Author: Vasiliev, S. K.
Format: Text
Language:unknown
Published: Digital Commons @ University of South Florida 1994
Subjects:
Online Access:https://digitalcommons.usf.edu/kip_articles/3302
https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2
id ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-4301
record_format openpolar
spelling ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-4301 2023-07-30T04:06:29+02:00 Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate Vasiliev, S. K. 1994-01-01T08:00:00Z https://digitalcommons.usf.edu/kip_articles/3302 https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/3302 https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2 KIP Articles Chagyrskaya Cave Bone Remains Taphocenosis Carnivores Paleolithic Man text 1994 ftusouthflorida https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2 2023-07-13T23:23:33Z The article focuses on the results of analysis of more than 100 thousand animal fossils recovered from Chagyrskaya Cave in 2007–2011. Animal remains from strata 5 and 6a result mostly from the hunting activity of wolves and cave hyenas, which used the cave as a shelter or den for breeding their offspring. In contrast, fauna remains from strata 6b and 6c at the cave's entrance zone primarily accumulated due to the hunting activities of Paleolithic humans, who mostly hunted bison (Bison priscus). To a lesser extent, they also hunted the Ovodov horse (Equus (Sussemionus) ovodovi), reindeer (Rangifer tarandus), Siberian mountain goat (Capra sibirica), and argali (Ovis ammon). Animal bones representing common taxa point to the existence of steppe landscapes during the formation of stratum 6. The sediment deposition of stratum 5 supposedly proceeded under arid climatic conditions. However, small forested areas existed in river valleys and mountain gorges throughout the entire sedimentation period. Text Rangifer tarandus University of South Florida St. Petersburg: Digital USFSP
institution Open Polar
collection University of South Florida St. Petersburg: Digital USFSP
op_collection_id ftusouthflorida
language unknown
topic Chagyrskaya Cave
Bone Remains
Taphocenosis
Carnivores
Paleolithic Man
spellingShingle Chagyrskaya Cave
Bone Remains
Taphocenosis
Carnivores
Paleolithic Man
Vasiliev, S. K.
Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
topic_facet Chagyrskaya Cave
Bone Remains
Taphocenosis
Carnivores
Paleolithic Man
description The article focuses on the results of analysis of more than 100 thousand animal fossils recovered from Chagyrskaya Cave in 2007–2011. Animal remains from strata 5 and 6a result mostly from the hunting activity of wolves and cave hyenas, which used the cave as a shelter or den for breeding their offspring. In contrast, fauna remains from strata 6b and 6c at the cave's entrance zone primarily accumulated due to the hunting activities of Paleolithic humans, who mostly hunted bison (Bison priscus). To a lesser extent, they also hunted the Ovodov horse (Equus (Sussemionus) ovodovi), reindeer (Rangifer tarandus), Siberian mountain goat (Capra sibirica), and argali (Ovis ammon). Animal bones representing common taxa point to the existence of steppe landscapes during the formation of stratum 6. The sediment deposition of stratum 5 supposedly proceeded under arid climatic conditions. However, small forested areas existed in river valleys and mountain gorges throughout the entire sedimentation period.
format Text
author Vasiliev, S. K.
author_facet Vasiliev, S. K.
author_sort Vasiliev, S. K.
title Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
title_short Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
title_full Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
title_fullStr Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
title_full_unstemmed Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate
title_sort luminescent microbanding in speleothems: high-resolution chronology and paleoclimate
publisher Digital Commons @ University of South Florida
publishDate 1994
url https://digitalcommons.usf.edu/kip_articles/3302
https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2
genre Rangifer tarandus
genre_facet Rangifer tarandus
op_source KIP Articles
op_relation https://digitalcommons.usf.edu/kip_articles/3302
https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2
op_doi https://doi.org/10.1130/0091-7613(1994)022<0407:LMISHR>2.3.CO;2
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