Development of biota within the Seliverstov Glacier deglaciation zone after the Little Ice Age maximum (Mongun-Taiga mountain range, Southeastern Altai)

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Development of biota within the Seliverstov Glacier deglaciation zone after the Little Ice Age maximum (Mongun-Taiga mountain range, Southeastern Altai). / Ганюшкин, Дмитрий Анатольевич ; Деркач, Екатерина Сергеевна ; Курочкин, Юрий Николаевич.

в: Acta Biologica Sibirica, Том 11, 2025, стр. 907-929.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{28ea47b941ac4c1583d934d80aa83464,

title = "Development of biota within the Seliverstov Glacier deglaciation zone after the Little Ice Age maximum (Mongun-Taiga mountain range, Southeastern Altai)",

abstract = "Recognized as part of the so-called Third Pole, the highlands of the Tuvan Altai represent the most arid part of the Russian Altai with a sharply continental climate, despite these features being a large glaciation node. Deglaciation caused by global climate change creates conditions for the initiation of postglacial vegetation successions. However, if the newest dynamics of glaciers of the high mountain massif of Mongun-Taiga, located at the junction of the mountain structures of the south-east of the Russian Altai and the mountain systems of the Sayan and Mongolian Altai, is well studied from a glaciological point of view, the issues of postglacial successions of biota in this region remain practically unstudied. This article is an attempt to give the first characteristics of the biota in the deglaciation zones of the Seliverstov Glacier in relation to deglaciation zones of different ages and typologies.",

keywords = "Mongun-Taiga, Russian Altai, biota, deglaciation zones, glaciers, species composition",

author = "Ганюшкин, {Дмитрий Анатольевич} and Деркач, {Екатерина Сергеевна} and Курочкин, {Юрий Николаевич}",

year = "2025",

doi = "10.5281/zenodo.16886561",

language = "English",

volume = "11",

pages = "907--929",

journal = "Acta Biologica Sibirica",

issn = "2412-1908",

publisher = "Издательство Алтайского государственного университета",

}

RIS

TY - JOUR

T1 - Development of biota within the Seliverstov Glacier deglaciation zone after the Little Ice Age maximum (Mongun-Taiga mountain range, Southeastern Altai)

AU - Ганюшкин, Дмитрий Анатольевич

AU - Деркач, Екатерина Сергеевна

AU - Курочкин, Юрий Николаевич

PY - 2025

Y1 - 2025

N2 - Recognized as part of the so-called Third Pole, the highlands of the Tuvan Altai represent the most arid part of the Russian Altai with a sharply continental climate, despite these features being a large glaciation node. Deglaciation caused by global climate change creates conditions for the initiation of postglacial vegetation successions. However, if the newest dynamics of glaciers of the high mountain massif of Mongun-Taiga, located at the junction of the mountain structures of the south-east of the Russian Altai and the mountain systems of the Sayan and Mongolian Altai, is well studied from a glaciological point of view, the issues of postglacial successions of biota in this region remain practically unstudied. This article is an attempt to give the first characteristics of the biota in the deglaciation zones of the Seliverstov Glacier in relation to deglaciation zones of different ages and typologies.

AB - Recognized as part of the so-called Third Pole, the highlands of the Tuvan Altai represent the most arid part of the Russian Altai with a sharply continental climate, despite these features being a large glaciation node. Deglaciation caused by global climate change creates conditions for the initiation of postglacial vegetation successions. However, if the newest dynamics of glaciers of the high mountain massif of Mongun-Taiga, located at the junction of the mountain structures of the south-east of the Russian Altai and the mountain systems of the Sayan and Mongolian Altai, is well studied from a glaciological point of view, the issues of postglacial successions of biota in this region remain practically unstudied. This article is an attempt to give the first characteristics of the biota in the deglaciation zones of the Seliverstov Glacier in relation to deglaciation zones of different ages and typologies.

KW - Mongun-Taiga

KW - Russian Altai

KW - biota

KW - deglaciation zones

KW - glaciers

KW - species composition

UR - https://www.mendeley.com/catalogue/05562e1a-a0f3-30ee-8db9-579a8b93b32d/

U2 - 10.5281/zenodo.16886561

DO - 10.5281/zenodo.16886561

M3 - Article

VL - 11

SP - 907

EP - 929

JO - Acta Biologica Sibirica

JF - Acta Biologica Sibirica

SN - 2412-1908

ER -

ID: 139802590