The Transbaikal conifer forests ecoregion (WWF ID: PA0609) covers a 1,000 km by 1,000 km region of mountainous southern taiga stretching east and south from the shores of Lake Baikal in the Southern Siberia region of Russia, and including part of northern Mongolia.[1] Historically, the area has been called "Dauria", or Transbaikal ("the land beyond Lake Baikal"). It is in the Palearctic realm, and mostly in the boreal forests/taiga biome with a subarctic, humid climate. It covers 200,465 km2 (77,400 sq mi).[2][3]
| Transbaikal conifer forests | |
|---|---|
 Buryatia landscape | |
 Transbaikal conifer forests ecoregion (in purple) | |
| Ecology | |
| Realm | Palearctic |
| Biome | Boreal forests/taiga |
| Geography | |
| Area | 200,465 km2 (77,400 sq mi) |
| Countries | Russia, Mongolia |
| Coordinates | 51°N 110°E / 51°N 110°E |
| Climate type | Subarctic, dry winters (Koppen Dwc) |
Location and description
editThe ecoregion is centered on the Yablonoi Mountains, a range that reaches heights of 1,600 m (5,200 ft), and runs southwest to northeast, parallel to Lake Baikal. The western edge of the region is the eastern shore of Lake Baikal and the Barguzin mountain range. The city of Chita is at the northeast of the region, and the city of Ulaanbaatar, Mongolia, is just outside the southern point of the region. To the south are the Khentii Mountains in Mongolia. To the east are the temperate grasslands of the Daurian forest steppe ecoregion. To the north is the Vitim tableland.[4][5]
The parallel ridges of the mountains in the region form the continental divide between rivers flowing to the Arctic Ocean (by way of Lake Baikal and the Lena River), and the Pacific Ocean (by way of the Amur River).
Climate
editThe climate of the ecoregion is dry-winter subarctic (Köppen Dwc). This climate is characterized by long, very cold winters, and cool summers, but with little snow in the winter. The Siberian High (also called the Siberian Anticyclone) keeps the area particularly dry in winter. During the summer, the Asiatic Low brings hot air from the deserts of China and Mongolia, raising the temperature in the Transbaikal.[5] To the east of the region, the climate grades into a dry winter humid continental climate (Dwb), with longer summers. To the south of the ecoregion in Mongolia, the climate grades into a cold semi-arid climate (Köppen BSk), with less precipitation than the Transbaikal. Precipitation in the Transbaikal ranges from 400 to 500 millimetres (16 to 20 in)/year in the uplands, to 200 millimetres (8 in)/year in the lower and more southerly areas.[5]
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Flora
editThe region is mostly forested below the 1,400 meter level. The characteristic trees on the warmer, wetter west side of the Yablonovsky Ridge are Dahurian larch (Larix gmelinii) and Siberian pine (Pinus sibirica). On the warmer and drier east of the ridge the larch is mixed with Scots pine (Pinus sylvestris).[5] The trees are draped with moss and lichen.
The flora of the Transbaikal exhibits altitude zoning. At the lowest levels in the river valleys and lowlands (0–600 meters), the characteristic vegetation is that of the steppes: bunchgrass (Stipa capillata), fescue, junegrass (Koeleria gracilis), and Filifolium (Tanacetum sibiricum). The next level (600-1,100 meters) is a forest-steppe level, and from 1,100 to 1800 meters a forest level featuring Larix gemilii and Pinus sylvestris. Above 1,800 meters is shrub land of Siberian dwarf pine (Pinus pumila, dwarf birch (Betula exilis), and Juniperus pseudosibirica. Unlike the Sayan and Altai mountains to the west, the climate of the Transbaikal is too extreme to support alpine meadows; the vegetation proceeds from forest directly to higher-altitude shrubs.[5]
Fauna
editThe extensive tree cover provides good habitat for deer, bighorn sheep, bear, wild boar, and other large mammals.[7]
Freshwater ecosystems
editThe Transbaikal terrestrial ecoregion covers the "Lake Baikal" Freshwater Ecoregion (WWF ID:606). This freshwater ecoregion supports a "large lakes" habitat for aquatic life, the primary focus of scientific study being on Lake Baikal itself and fish that spawn in the rivers that feed into it (such as the Barguzin River in the Transbaikal).[8]
Protections
editThe Lake Baikal area on the western edge of the ecoregion is a UNESCO Man and Biosphere (MAB) Biosphere Reserve. It is also a UNESCO World Heritage Site
Three large protected areas of the Russian Federation in the Transbaikal ecoregion are:
- Baikal Nature Reserve. An IUCN class Ia "strict ecological reserve" (a Zapovednik) on the southeast shore of Lake Baikal. (Area: 1,657 km2)
- Barguzin Nature Reserve. An IUCN class Ia strict ecological reserve (a Zapovednik) on the eastern shore of Lake Baikal. (Area: 2,482 km2)
- Sokhondo Nature Reserve. An IUCN class Ia strict ecological reserve (a Zapovednik) centered on the Sokhondo Mountain massif in Chita Oblast in the south east of the ecoregion. (Area: 2,110 km2)
Two large protected areas of the Transbaikal are in Mongolia:
- Khan Khentii Strictly Protected Area. An IUCN class Ib "wilderness area", in the Khentii Mountains, and containing the sacred Burkhan Khaldun mountain. (Area: 12,270 km2)
- Onon-Balj National Park. A national park created in 2000 that protects the source of the Onon River, which is ultimately the source of the Amur River. (Area: 4,158 km2)
Threats
editForest fires are always a threat to wooded, dry areas; drought in recent years has increased the threat of wildfire. The area also suffers from pest outbreaks and uncontrolled logging. There is also gold mining in the area, which is a threat to the streams and bogs.[9]
Urban areas and settlements
editThe major cities of the ecoregion are Ulan-Ude and Petrovsk-Zaybaykalsky in Republic of Buryatia, and Chita and Khilok in Zabaykalsky Krai. Otherwise, the region is sparsely populated. The Trans-Siberian Railroad bisects the region from west to east.
See also
editReferences
edit- ^ "Trans-Baikal conifer forests". Global Species. Myers Enterprises II. Retrieved 17 April 2016.
- ^ "Trans-Baikal conifer forests". Wild World Ecoregion Profile. National Geographic / Internet Archive Wayback. Archived from the original on March 8, 2010. Retrieved 17 April 2016.
{{cite web}}: CS1 maint: unfit URL (link) - ^ Olson, David M; Dinerstein, Eric (Spring 2002). "The Global 200: Priority Ecoregions for Global Conservation" (PDF). Annals of the Missouri Botanical Garden. 89 (2): 199–224. doi:10.2307/3298564. JSTOR 3298564.
- ^ "Trans-Baikal coniferous forests". Amur Information Center. Amur Information Center. Retrieved 17 April 2016.
- ^ a b c d e "Mountains of the Baikal Region and Transbaikalia". Russian Nature. Rusnature. Retrieved 17 April 2016.
- ^ "Khilok Monthly Climate Averages". WorldWeatherOnline.com.
- ^ "Trans-Baikal coniferous forests". Ecoregions of the World. World Wildlife Federation. Retrieved 17 April 2016.
- ^ "Lake Baikal Freshwater Ecoregion". Freshwater Ecoregions of the World. FEOW. Retrieved 17 April 2016.
- ^ Kharuk, Vyacheslav (2011). "Drought-Caused Forest Decline In The Trans-Baikal Lake Area". AGU Fall Meeting. 2011. Bibcode:2011AGUFMGC31A1012R. Retrieved 17 April 2016.