Oribatid mites in a succession of permafrost soils in Central Yakutia
ABSTRACTThermokarst troughs formed on ice-rich ground in Central Yakutia harbor contrasting soils that have developed from lake silt through a marsh stage to meadow and steppe-like soils. Associated processes result in radical transformations of an important component of the decomposer community in...
Published in: | Arctic, Antarctic, and Alpine Research |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Taylor & Francis Group
2024
|
Subjects: | |
Online Access: | https://doi.org/10.1080/15230430.2024.2334815 https://doaj.org/article/d7daf7621ae247828424cc7cedb00439 |
id |
ftdoajarticles:oai:doaj.org/article:d7daf7621ae247828424cc7cedb00439 |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:d7daf7621ae247828424cc7cedb00439 2024-09-15T17:49:03+00:00 Oribatid mites in a succession of permafrost soils in Central Yakutia Mikhail V. Yakutin Vladislav S. Andrievskii Franz Conen Alexander N. Puchnin 2024-12-01T00:00:00Z https://doi.org/10.1080/15230430.2024.2334815 https://doaj.org/article/d7daf7621ae247828424cc7cedb00439 EN eng Taylor & Francis Group https://www.tandfonline.com/doi/10.1080/15230430.2024.2334815 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 doi:10.1080/15230430.2024.2334815 1938-4246 1523-0430 https://doaj.org/article/d7daf7621ae247828424cc7cedb00439 Arctic, Antarctic, and Alpine Research, Vol 56, Iss 1 (2024) Eastern Siberia Cryosol oribatid mites abundance species richness Environmental sciences GE1-350 Ecology QH540-549.5 article 2024 ftdoajarticles https://doi.org/10.1080/15230430.2024.2334815 2024-08-05T17:49:34Z ABSTRACTThermokarst troughs formed on ice-rich ground in Central Yakutia harbor contrasting soils that have developed from lake silt through a marsh stage to meadow and steppe-like soils. Associated processes result in radical transformations of an important component of the decomposer community in the biological cycle—the oribatid mites community. During the transition of soil from a Histic Reductaquic Cryosol to a Gleyic Cryosol and, finally, to a Turbic Chernic Cryosol, the number of species increased from three to six to thirteen. Total abundance of oribatid mites increased from 1,600 m−2 (±265) to 2,442 m−2 (±328) to 8,640 (±588) m−2. A characteristic feature of these permafrost soils was the considerable similarity of the populations in the Gleyic Cryosol and the Turbic Chernic Cryosol and their negligible overlap with the oribatids population of the Histic Reductaquic Cryosol. The peculiarity of the Histic Reductaquic Cryosol is manifested both in quantitative parameters of the communities and in their qualitative characteristics, such as the dominance structure and the sets of species with different ecological preferences. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Ice permafrost Yakutia Siberia Directory of Open Access Journals: DOAJ Articles Arctic, Antarctic, and Alpine Research 56 1 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Eastern Siberia Cryosol oribatid mites abundance species richness Environmental sciences GE1-350 Ecology QH540-549.5 |
spellingShingle |
Eastern Siberia Cryosol oribatid mites abundance species richness Environmental sciences GE1-350 Ecology QH540-549.5 Mikhail V. Yakutin Vladislav S. Andrievskii Franz Conen Alexander N. Puchnin Oribatid mites in a succession of permafrost soils in Central Yakutia |
topic_facet |
Eastern Siberia Cryosol oribatid mites abundance species richness Environmental sciences GE1-350 Ecology QH540-549.5 |
description |
ABSTRACTThermokarst troughs formed on ice-rich ground in Central Yakutia harbor contrasting soils that have developed from lake silt through a marsh stage to meadow and steppe-like soils. Associated processes result in radical transformations of an important component of the decomposer community in the biological cycle—the oribatid mites community. During the transition of soil from a Histic Reductaquic Cryosol to a Gleyic Cryosol and, finally, to a Turbic Chernic Cryosol, the number of species increased from three to six to thirteen. Total abundance of oribatid mites increased from 1,600 m−2 (±265) to 2,442 m−2 (±328) to 8,640 (±588) m−2. A characteristic feature of these permafrost soils was the considerable similarity of the populations in the Gleyic Cryosol and the Turbic Chernic Cryosol and their negligible overlap with the oribatids population of the Histic Reductaquic Cryosol. The peculiarity of the Histic Reductaquic Cryosol is manifested both in quantitative parameters of the communities and in their qualitative characteristics, such as the dominance structure and the sets of species with different ecological preferences. |
format |
Article in Journal/Newspaper |
author |
Mikhail V. Yakutin Vladislav S. Andrievskii Franz Conen Alexander N. Puchnin |
author_facet |
Mikhail V. Yakutin Vladislav S. Andrievskii Franz Conen Alexander N. Puchnin |
author_sort |
Mikhail V. Yakutin |
title |
Oribatid mites in a succession of permafrost soils in Central Yakutia |
title_short |
Oribatid mites in a succession of permafrost soils in Central Yakutia |
title_full |
Oribatid mites in a succession of permafrost soils in Central Yakutia |
title_fullStr |
Oribatid mites in a succession of permafrost soils in Central Yakutia |
title_full_unstemmed |
Oribatid mites in a succession of permafrost soils in Central Yakutia |
title_sort |
oribatid mites in a succession of permafrost soils in central yakutia |
publisher |
Taylor & Francis Group |
publishDate |
2024 |
url |
https://doi.org/10.1080/15230430.2024.2334815 https://doaj.org/article/d7daf7621ae247828424cc7cedb00439 |
genre |
Antarctic and Alpine Research Arctic Ice permafrost Yakutia Siberia |
genre_facet |
Antarctic and Alpine Research Arctic Ice permafrost Yakutia Siberia |
op_source |
Arctic, Antarctic, and Alpine Research, Vol 56, Iss 1 (2024) |
op_relation |
https://www.tandfonline.com/doi/10.1080/15230430.2024.2334815 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 doi:10.1080/15230430.2024.2334815 1938-4246 1523-0430 https://doaj.org/article/d7daf7621ae247828424cc7cedb00439 |
op_doi |
https://doi.org/10.1080/15230430.2024.2334815 |
container_title |
Arctic, Antarctic, and Alpine Research |
container_volume |
56 |
container_issue |
1 |
_version_ |
1810290747681800192 |