J 2019

A modern analogue of the Pleistocene steppe-tundra ecosystem in southern Siberia

CHYTRÝ, Milan, Michal HORSÁK, Jiří DANIHELKA, Nikolai ERMAKOV, Dmitry A GERMAN et. al.

Basic information

Original name

A modern analogue of the Pleistocene steppe-tundra ecosystem in southern Siberia

Authors

CHYTRÝ, Milan (203 Czech Republic, guarantor, belonging to the institution), Michal HORSÁK (203 Czech Republic, belonging to the institution), Jiří DANIHELKA (203 Czech Republic, belonging to the institution), Nikolai ERMAKOV (643 Russian Federation), Dmitry A GERMAN (643 Russian Federation), Michal HÁJEK (203 Czech Republic, belonging to the institution), Petra HÁJKOVÁ (203 Czech Republic, belonging to the institution), Martin KOČÍ (203 Czech Republic, belonging to the institution), Svatava KUBEŠOVÁ (203 Czech Republic, belonging to the institution), Pavel LUSTYK (203 Czech Republic, belonging to the institution), Jeffrey Clark NEKOLA (840 United States of America, belonging to the institution), Věra PAVELKOVÁ ŘIČÁNKOVÁ (203 Czech Republic), Zdenka PREISLEROVÁ (203 Czech Republic, belonging to the institution), Philipp RESL (40 Austria) and Milan VALACHOVIČ (703 Slovakia)

Edition

Boreas, Hoboken, Willey, 2019, 0300-9483

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10506 Paleontology

Country of publisher

United States of America

Confidentiality degree

není předmětem státního či obchodního tajemství

References:

Impact factor

Impact factor: 2.477

RIV identification code

RIV/00216224:14310/19:00107236

Organization unit

Faculty of Science

UT WoS

000454203700003

Keywords in English

LAST GLACIAL MAXIMUM; EASTERN-CENTRAL EUROPE; FOREST-STEPPE; VEGETATION RELATIONSHIPS; MAMMOTH STEPPE; CLIMATE-CHANGE; CENTRAL-ASIA; ALTAI; POLLEN; NORTH

Tags

Tags

International impact, Reviewed
Změněno: 13/3/2020 11:11, Mgr. Marie Šípková, DiS.

Abstract

V originále

Steppe-tundra is considered to have been a dominant ecosystem across northern Eurasia during the Last Glacial Maximum. As the fossil record is insufficient for understanding the ecology of this vanished ecosystem, modern analogues have been sought, especially in Beringia. However, Beringian ecosystems are probably not the best analogues for more southern variants of the full-glacial steppe-tundra because they lack many plant and animal species of temperate steppes found in the full-glacial fossil record from various areas of Europe and Siberia. We present new data on flora, land snails and mammals and characterize the ecology of a close modern analogue of the full-glacial steppe-tundra ecosystem in the southeastern Russian Altai Mountains, southern Siberia. The Altaian steppe-tundra is a landscape mosaic of different habitat types including steppe, mesic and wet grasslands, shrubby tundra, riparian scrub, and patches of open woodland at moister sites. Habitat distribution, species diversity, primary productivity and nutrient content in plant biomass reflect precipitation patterns across a broader area and the topography-dependent distribution of soil moisture across smaller landscape sections. Plant and snail species considered as glacial relicts occur in most habitats of the Altaian steppe-tundra, but snails avoid the driest types of steppe. A diverse community of mammals, including many species typical of the full-glacial ecosystems, also occurs there. Insights from the Altaian steppe-tundra suggest that the full-glacial steppe-tundra was a heterogeneous mosaic of different habitats depending on landscape-scale moisture gradients. Primary productivity of this habitat mosaic combined with shallow snow cover that facilitated winter grazing was sufficient to sustain rich communities of large herbivores.

Links

GAP504/11/0454, research and development project
Name: Změny biodiverzity na přechodu pleistocénu a holocénu: současné analogie v reliktních ekosystémech Sibiře
Investor: Czech Science Foundation