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The expansion and migration of small mammals in the Makalu Barun region induced by changes of the Himalayan environment during the Quaternary

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F75010330%3A_____%2F22%3A00014131" target="_blank" >RIV/75010330:_____/22:00014131 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216208:11310/22:10457172

  • Výsledek na webu

    <a href="https://karolinum.cz/casopis/auc-geographica/rocnik-57/cislo-2/clanek-10901" target="_blank" >https://karolinum.cz/casopis/auc-geographica/rocnik-57/cislo-2/clanek-10901</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.14712/23361980.2022.13" target="_blank" >10.14712/23361980.2022.13</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    The expansion and migration of small mammals in the Makalu Barun region induced by changes of the Himalayan environment during the Quaternary

  • Popis výsledku v původním jazyce

    This paper describes the course of migration and expansion of small mammals in the Makalu Barun region influenced by the oroge-netic uplift of the East Nepal Himalaya and climatically conditioned changes in the extent of morphogenetic zones from the Upper Pleistocene up to the present. The results of zoological and parasitological research are compounded with the knowledge of the dynamic development of landforms, which testifies to significant changes in the high-mountain environment during the Quaternary. The migration of Palearctic species of small mammals across the gradually emerging orographical barrier during the orogenesis of the High Himalaya was completely interrupted by the glaciation in the Upper Pleistocene. This extensive glaciation also excluded occurrence and survival of small mammals in the high-mountain valleys of the Makalu Barun region. Migration routes and the exten-sion of the territory of small mammals remained open only in the periglacial zone of the Arun and Barun Khola valleys. Following the interstadial period of warmer and humid climate conditions were changed by the Late Glacial Maximum when small mammals were again pushed away from heavily glaciated valleys to the lower altitude periglacial zone. During the Holocene interglacial, the occurrence of fauna and flora in the high-mountain valleys depended on repeated spatial changes of periglacial and glacial morpho-climatic zones. Current biogeographical hazards are accentuated due to the rapid retreat of glaciers, the expansion of the periglacial morphoclimatic zone and the increased human impact in the High Himalaya.

  • Název v anglickém jazyce

    The expansion and migration of small mammals in the Makalu Barun region induced by changes of the Himalayan environment during the Quaternary

  • Popis výsledku anglicky

    This paper describes the course of migration and expansion of small mammals in the Makalu Barun region influenced by the oroge-netic uplift of the East Nepal Himalaya and climatically conditioned changes in the extent of morphogenetic zones from the Upper Pleistocene up to the present. The results of zoological and parasitological research are compounded with the knowledge of the dynamic development of landforms, which testifies to significant changes in the high-mountain environment during the Quaternary. The migration of Palearctic species of small mammals across the gradually emerging orographical barrier during the orogenesis of the High Himalaya was completely interrupted by the glaciation in the Upper Pleistocene. This extensive glaciation also excluded occurrence and survival of small mammals in the high-mountain valleys of the Makalu Barun region. Migration routes and the exten-sion of the territory of small mammals remained open only in the periglacial zone of the Arun and Barun Khola valleys. Following the interstadial period of warmer and humid climate conditions were changed by the Late Glacial Maximum when small mammals were again pushed away from heavily glaciated valleys to the lower altitude periglacial zone. During the Holocene interglacial, the occurrence of fauna and flora in the high-mountain valleys depended on repeated spatial changes of periglacial and glacial morpho-climatic zones. Current biogeographical hazards are accentuated due to the rapid retreat of glaciers, the expansion of the periglacial morphoclimatic zone and the increased human impact in the High Himalaya.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10508 - Physical geography

Návaznosti výsledku

  • Projekt

  • Návaznosti

    V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Ostatní

  • Rok uplatnění

    2022

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    AUC Geographica

  • ISSN

    0300-5402

  • e-ISSN

    2336-1980

  • Svazek periodika

    57

  • Číslo periodika v rámci svazku

    2

  • Stát vydavatele periodika

    CZ - Česká republika

  • Počet stran výsledku

    23

  • Strana od-do

    158-180

  • Kód UT WoS článku

    000905275400007

  • EID výsledku v databázi Scopus

    2-s2.0-85146219523