Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions

Thermokarst (alas) of Central Yakutia is an intrazonal dynamic landscape in the form of rounded depressions with peculiar soils and meadow vegetation, microclimate, and fauna that are very different from the surrounding typical taiga landscapes. During the formation of alas depression, complete proc...

Full description

Bibliographic Details
Published in:Geosciences
Main Authors: Alexey Desyatkin, Fumiaki Takakai, Maya Nikolaeva
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/geosciences8120439
id ftmdpi:oai:mdpi.com:/2076-3263/8/12/439/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2076-3263/8/12/439/ 2023-08-20T04:10:06+02:00 Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions Alexey Desyatkin Fumiaki Takakai Maya Nikolaeva agris 2018-11-27 application/pdf https://doi.org/10.3390/geosciences8120439 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/geosciences8120439 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 8; Issue 12; Pages: 439 thermokarst central yakutia thermokarst soils thermokarst vegetation hydrothermal regime physicochemical regime GHG emission thermokarst microzones Text 2018 ftmdpi https://doi.org/10.3390/geosciences8120439 2023-07-31T21:52:04Z Thermokarst (alas) of Central Yakutia is an intrazonal dynamic landscape in the form of rounded depressions with peculiar soils and meadow vegetation, microclimate, and fauna that are very different from the surrounding typical taiga landscapes. During the formation of alas depression, complete processing of thawed ground with the formation of new soils occurs and entirely changes the biogeochemical cycle. Because this system is closed, all water-soluble substances, such as N/C and soluble salts, etc., accumulate inside the depression. Using standard methods and instruments, we measured the main properties of alas soils. Depending on the hydrothermal and physicochemical regimes, thawing depth, and greenhouse gas (GHG) flux, three main belts of soils and vegetation were distinguished within the alas: (1) steppe meadow, located on most elevated places, not sufficiently moistened, with alas steppe soils and steppe vegetation; (2) middle meadow, located lower than stepped meadow in elevation, normally moist, with alas sod-meadow soils and highest productivity vegetation; and (3) wet meadow, located around the lake, excessively moistened, with alas marshy sod-meadow soils and marsh vegetation. Therefore, the soils of wet and real meadows, due to the abundance of organic matter, are significant sources of CO2 and CH4, especially in humid years. Under the climate warming observed over recent decades in this territory, the alas ecosystem has undergone considerable change. Thus, the classification and mapping of belts within the alas can have both applied and fundamental importance. Text taiga Thermokarst Yakutia MDPI Open Access Publishing Geosciences 8 12 439
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic thermokarst
central yakutia
thermokarst soils
thermokarst vegetation
hydrothermal regime
physicochemical regime
GHG emission
thermokarst microzones
spellingShingle thermokarst
central yakutia
thermokarst soils
thermokarst vegetation
hydrothermal regime
physicochemical regime
GHG emission
thermokarst microzones
Alexey Desyatkin
Fumiaki Takakai
Maya Nikolaeva
Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
topic_facet thermokarst
central yakutia
thermokarst soils
thermokarst vegetation
hydrothermal regime
physicochemical regime
GHG emission
thermokarst microzones
description Thermokarst (alas) of Central Yakutia is an intrazonal dynamic landscape in the form of rounded depressions with peculiar soils and meadow vegetation, microclimate, and fauna that are very different from the surrounding typical taiga landscapes. During the formation of alas depression, complete processing of thawed ground with the formation of new soils occurs and entirely changes the biogeochemical cycle. Because this system is closed, all water-soluble substances, such as N/C and soluble salts, etc., accumulate inside the depression. Using standard methods and instruments, we measured the main properties of alas soils. Depending on the hydrothermal and physicochemical regimes, thawing depth, and greenhouse gas (GHG) flux, three main belts of soils and vegetation were distinguished within the alas: (1) steppe meadow, located on most elevated places, not sufficiently moistened, with alas steppe soils and steppe vegetation; (2) middle meadow, located lower than stepped meadow in elevation, normally moist, with alas sod-meadow soils and highest productivity vegetation; and (3) wet meadow, located around the lake, excessively moistened, with alas marshy sod-meadow soils and marsh vegetation. Therefore, the soils of wet and real meadows, due to the abundance of organic matter, are significant sources of CO2 and CH4, especially in humid years. Under the climate warming observed over recent decades in this territory, the alas ecosystem has undergone considerable change. Thus, the classification and mapping of belts within the alas can have both applied and fundamental importance.
format Text
author Alexey Desyatkin
Fumiaki Takakai
Maya Nikolaeva
author_facet Alexey Desyatkin
Fumiaki Takakai
Maya Nikolaeva
author_sort Alexey Desyatkin
title Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
title_short Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
title_full Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
title_fullStr Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
title_full_unstemmed Landscape Microzones within Thermokarst Depressions of Central Yakutia under Present Climatic Conditions
title_sort landscape microzones within thermokarst depressions of central yakutia under present climatic conditions
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/geosciences8120439
op_coverage agris
genre taiga
Thermokarst
Yakutia
genre_facet taiga
Thermokarst
Yakutia
op_source Geosciences; Volume 8; Issue 12; Pages: 439
op_relation https://dx.doi.org/10.3390/geosciences8120439
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences8120439
container_title Geosciences
container_volume 8
container_issue 12
container_start_page 439
_version_ 1774724052118667264