Grasslands and Shrublands of Mongolia

Research output: Contribution to book/Conference proceedings/Anthology/ReportChapter in book/Anthology/ReportContributedpeer-review

Contributors

  • Martin Pfeiffer - , University of Bayreuth, National University of Mongolia (Author)
  • Choimaa Dulamsuren - , University of Freiburg (Author)
  • Karsten Wesche - , International Institute Zittau, Chair of Biodiversity of Higher Plants, Senckenberg Gesellschaft für Naturforschung, German Centre for Integrative Biodiversity Research (iDiv) Halle—Jena—Leipzig (Author)

Abstract

Mongolian grasslands and arid rangelands cover 80% of the country’s area at an estimated 1.2 million km2. They are still relatively intact, with largely natural environmental conditions and natural structure, and the country has declared >17% of its territory as conservation area. The region has an extremely continental climate with absolute temperatures fluctuating between −50°C and +45°C, and <350mm rainfall per year. Botanically, Mongolia is located at the intersection between three different subkingdoms (i.e., the Boreal, Tethyan, and East Asian subkingdoms) of the Holarctic realm. Nomadic herders use these pastures since the Bronze Age and livestock grazing has been the dominant human impact in Mongolian grasslands until now, with the national herd comprising >65Mio. animals in 2018. Overgrazing has become a major problem in parts of the steppe ecosystem, impacting fauna and flora and leading to a higher vulnerability of herds to mass mortality in harsh winters. Global warming is another major global change impact in Mongolia.

Details

Original languageEnglish
Title of host publicationEncyclopedia of the World's Biomes
PublisherElsevier
PagesV3-759-V3-772
Volume1-5
ISBN (electronic)9780128160961
Publication statusPublished - 1 Jan 2020
Peer-reviewedYes

Keywords

ASJC Scopus subject areas

Keywords

  • Biodiversity, Climate change, Flora regions, Gobi, Human impact, Mobile pastoral livestock husbandry, Nature conservation, Overgrazing, Palaearctic steppe biome, Permafrost