mountain steppe - определение. Что такое mountain steppe
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Что (кто) такое mountain steppe - определение

WIDESPREAD BIOME DURING THE LAST GLACIAL MAXIMUM
Steppe tundra; Tundra-steppe; Steppe-tundra; Tundra steppe; Mammoth steppes
  • date=7 June 2019}}</ref>
  • cave lions]] inhabited the mammoth steppe during the Pleistocene.
  • Vegetation types at the time of [[Last Glacial Maximum]]
  • Climatic suitability for the woolly mammoths in the Late Pleistocene and Holocene. Increasing intensities of red represent increasing suitability of the climate and increasing intensities of green represent decreasing suitability. Black points are the records of mammoth presence for each of the periods. Black lines represent the northern limit of modern humans and black dotted lines indicate uncertainty in the limit of modern humans (D. Nogués-Bravo et al. 2008).<ref name=nogues2008/>
  • [[Ubsunur Hollow Biosphere Reserve]] located on the border of Mongolia and the Republic of Tuva is one of the last remnants of the mammoth steppe<ref name=pavelkova2014/>

Bugeac steppe         
Bugeac steppe; Stepa Bugeacului; Steppe of Bugeac; Steppe of Budjak; Steppe of Budzhak; Budjak Steppe; Budzhak Steppe; Budzhak steppe; Budjak steppe; Bugeac Plain; Bugeac plain; Budjak plain; Budjak Plain; Budzhak Plain; Budzhak plain
The Bugeac steppe (; ) is a steppe located in the south of Ukraine and Moldova from the Dniester to Prut rivers reaching down to the Black Sea.Welcome to Moldova!
Pontic–Caspian steppe         
  • [[Zaporozhian Cossacks]] fighting Tatars from the [[Crimean Khanate]] – late 19th-century painting
  • date=4 April 2017}}</ref>
  • Streltsovskaya Steppe, a preserved area in [[Milove Raion]] in [[Luhansk Oblast]], Ukraine. The steppe is often dominated by plumes of ''[[Stipa]]'' in early summer.
  • Tulipa suaveolens]]'', one of the most typical spring flowers of the Pontic-Caspian steppe
ECOREGION OF GRASSLANDS THAT ENCOMPASS MOST OF THE WESTERN SEGMENT OF THE EURASIAN STEPPE
Pontic steppes; Pontic-Caspian; Pontic steppe; Pontic Steppe; Ponto-Caspian; Ponto-Caspian region; Pontocaspian; Pontocaspian region; Pontocaspian Region; Ponto-Caspian Region; History of the Eurasian steppe; Pontic-Caspian Steppe; Don Steppe; Ponto-Caspian Basin; Ukrainian steppes; Pontic-Caspian steppe; Steppes of Eastern Europe; Ukrainian steppe; Ponto–Caspian steppe; Ponto-Caspian steppe
The Pontic–Caspian steppe, formed by the Caspian steppe and the Pontic steppe, is the steppeland stretching from the northern shores of the Black Sea (the Pontus Euxinus of antiquity) to the northern area around the Caspian Sea. It extends from Dobruja in the northeastern corner of Bulgaria and southeastern Romania, through Moldova and southern and eastern Ukraine, across the Russian Northern Caucasus, the Southern and lower Volga regions to western Kazakhstan, adjacent to the Kazakh steppe to the east, both forming part of the larger Eurasian Steppe.
Kalmyk Steppe         
STEPPE IN ASTRAKHAN OBLAST, RUSSIA
Kalmuck Steppe; Kalmyk steppe; Kalmyk Steppe Kalmuck
Kalmuk Steppe, or Kalmyk Steppe is a steppe with a land area of approximately 100,000 km², bordering the northwest Caspian Sea, bounded by the Volga on the northeast, the Manych on the southwest, and the territory of the Don Cossacks on the northwest. The historic home to the Kalmuck or Kalmyks it is in the Federal subject of Astrakhan Oblast in Russia. Before the appearance of the Kalmyks to this region, the area was long known as the Povoletsk steppe by the Russians.

Википедия

Mammoth steppe

During the Last Glacial Maximum, the mammoth steppe, also known as steppe-tundra, was the Earth's most extensive biome. It spanned from Spain eastward across Eurasia to Canada and from the arctic islands southward to China. The mammoth steppe was cold and dry. The vegetation was dominated by palatable high-productivity grasses, herbs and willow shrubs. The animal biomass was dominated by reindeer, bison, horses, and woolly mammoth. This ecosystem covered wide areas of the northern part of the globe, thrived for approximately 100,000 years without major changes, but then diminished to small regions around 12,000 years ago.