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[

] 81

Mankind on the shores of the Baikal:

the transboundary ecosystem of

Russia and Mongolia

E. I. Lishtovannii and A. N. Matveev, Irkutsk State University, Russia; B. Bayartogtokh,

Mongolian State University; and T. Villemin, University of Savoie, France

L

ake Baikal, located in South-Eastern Siberia, is one of

the most unique lakes in the world. It was formed 25-30

million years ago and corresponds to a rift valley that is

almost subsiding today. The lake contains about 20 per cent of

the world’s surface freshwater supply and its transparency is

striking up to 40 metres deep. It is a place of biological water

flora and fauna diversity on a global scale. At present, more than

2,630 species and varieties of plants and animals are known

to science, two thirds of which are endemic.

1

The number of

known Baikal organisms is continuously growing, as revealed

by research done by Russian and other scientists.

Lake Baikal was inscribed on the United Nations Educational,

Scientific and Cultural Organization’s (UNESCO) World Heritage

List in 1996. In 2008, the Russian Government announced that the

lake is one of the seven wonders of Russia.

The largest tributary of Lake Baikal is the Selenga

river, which springs in Mongolia and brings more

than 60 per cent of the water influx to the lake. The

Selenga river basin is a transnational mega-ecosystem,

the largest water basin of Mongolia and the Republic of

Buryatia region of the Russian Federation. The Selenga

basin comprises more than 80 per cent of the Baikal

basin, indicating the significant role of Mongolia in the

long-term ecological health of the lake.

The Selenga, flowing into Lake Baikal, forms the

world’s largest freshwater delta occupying an area of 680

km². This delta was included in the Ramsar Convention

list of Wetlands of International Importance in 1996 –

a decision explained by the river’s abundance of flora

and fauna, as well as its considerable role in the purifi-

cation of polluted Selenga waters coming into the lake.

The drainage basin of the Selenga river is 447,060 km

2

,

with a length of 1,024 km (including the headwaters of

the Ider River which are 1,476 km long). The length of

the river in Russia is 409 km. The river basin is directly

affected by industrial and agricultural sites located in

Mongolia and in the Republic of Buryatia, and indirectly

affected through the air by industrial sites of the Irkutsk

region. Surface pollution, caused by precipitation and

anthropogenic sources, directly influences all elements of

the Selenga ecosystem and gradually percolates through

underground layers. There is a more intense migration

of toxic components through these structures. Linearly

elongated centres of underground toxic water pollution

are formed in the area and might enter the Selenga as well

as the Baikal water system. In such a situation, the delta

plays a significant role in Selenga river self-purification

processes. The delta is a massive wetland area, which

undergoes intensive processes of binding and sedimenta-

tion of river-driven organic matter and pollutants.

In the Selenga delta area, the most apparent changes

in the lake water level result from the natural and

anthropogenic processes connected with the Irkutsk

Hydroelectric Power Station. The dam was constructed

in the late 1950s on the Baikal’s outlet, the Angara

River, 60 km from the place where the Angara flows

out of the lake. Seismic, tectonic and other endogenous

T

ransboundary

W

ater

M

anagement

Lake Baikal contains about 20 per cent of the world’s surface freshwater supply and

2,630 plant and animal varieties

Image: Evgeni Kozyrev