Modelling the Last Glacial Maximum environments for a refugium of Pleistocene biota in the Russian Altai Mountains, SiberiaPalaeogeography, Palaeoclimatology, Palaeoecology

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00081406" target="_blank" >RIV/00216224:14310/15:00081406 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.sciencedirect.com/science/article/pii/S0031018215004137" target="_blank" >http://www.sciencedirect.com/science/article/pii/S0031018215004137</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.palaeo.2015.07.037" target="_blank" >10.1016/j.palaeo.2015.07.037</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Modelling the Last Glacial Maximum environments for a refugium of Pleistocene biota in the Russian Altai Mountains, SiberiaPalaeogeography, Palaeoclimatology, Palaeoecology

Popis výsledku v původním jazyce

Recent botanical and zoological studies have suggested that the AltaiMountains in southern Siberia are an important refugiumof the last glacial biota that used to bewidespread across northern Eurasia before the Pleistocene? Holocene transition. To obtaininsights into the history of this relict biota,we modelled the spatial distribution of habitats during the Last GlacialMaximum (LGM) in the Russian Altai. We prepared a map of the current vegetation of this area based on the ground-truthed remote sensing data, and modelled the distribution of the current vegetation types using the Random Forest technique with climatic predictors. The models were projected onto the CCSM3 model of the LGMclimate for the Russian Altai and interpreted for 72% of its area because the remaining part is supposed to have been glaciated during the LGM.

Název v anglickém jazyce

Modelling the Last Glacial Maximum environments for a refugium of Pleistocene biota in the Russian Altai Mountains, SiberiaPalaeogeography, Palaeoclimatology, Palaeoecology

Popis výsledku anglicky

Recent botanical and zoological studies have suggested that the AltaiMountains in southern Siberia are an important refugiumof the last glacial biota that used to bewidespread across northern Eurasia before the Pleistocene? Holocene transition. To obtaininsights into the history of this relict biota,we modelled the spatial distribution of habitats during the Last GlacialMaximum (LGM) in the Russian Altai. We prepared a map of the current vegetation of this area based on the ground-truthed remote sensing data, and modelled the distribution of the current vegetation types using the Random Forest technique with climatic predictors. The models were projected onto the CCSM3 model of the LGMclimate for the Russian Altai and interpreted for 72% of its area because the remaining part is supposed to have been glaciated during the LGM.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Palaeogeography, Palaeoclimatology, Palaeoecology

ISSN

0031-0182

e-ISSN

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Svazek periodika

438

Číslo periodika v rámci svazku

NOVEMBER

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

135-145

Kód UT WoS článku

000362613300011

EID výsledku v databázi Scopus

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