Wildlife of
Krasnojarskij kraj

Dominant taiga biome across the central and southern lowlands/plateaus, with extensive larch, pine, spruce, fir and Siberian cedar forests; frequent fire regimes and permafrost-influenced soils in the north/plateau interiors.

Widespread across most of the krai south of the Arctic tundra; roughly ~60-70% of the territory.

Arctic and subarctic tundra on Taymyr Peninsula and high Arctic islands/archipelagos, with moss-lichen carpets, dwarf shrubs, patterned ground, and strong permafrost control; key reindeer and breeding waterbird areas.

Northern third of the krai, strongest on Taymyr and adjacent Arctic lowlands; roughly ~20-30%.

Elevational belts in the Sayan Mountains and other uplands, transitioning from montane conifers to subalpine krummholz, alpine tundra, snowbeds, and rocky highlands; includes glacial and periglacial landforms.

Patchy in southern mountains (Western/Eastern Sayan) and select uplands; roughly ~5-10% (highly localized but important).

Large river systems (Yenisei and major tributaries) and extensive lake districts (notably Putorana Plateau and Taymyr Lake), supporting salmonids/whitefish, riparian forests, floodplains, and migratory bird stopovers.

Linear network throughout the krai; locally dominant along major valleys and lake basins (a few percent by area, but ecologically pervasive).

Peatlands, floodplain marshes, thermokarst wetlands, and permafrost-controlled bog complexes across taiga and tundra; major carbon stores and breeding habitat for waterfowl and cranes.

Scattered statewide, especially in lowlands, river floodplains, and permafrost zones; locally extensive (several percent, with large regional concentrations).

Arctic marine and coastal ecosystems along the Kara Sea and Laptev Sea margins (including island coasts), with seasonal sea ice, polynyas, and productive shelf waters supporting seabirds and marine mammals.

Narrow coastal fringe plus offshore waters within the krai's Arctic frontage; limited land area but significant seascape extent.

Southern transition zones where mixed forests and forest-steppe elements occur (birch/aspen mixed with conifers) under comparatively warmer, more continental conditions than the central plateau taiga.

Small southern portion (notably toward the Minusinsk Basin and Sayan foothills); minor overall (<~5%).

Forest-steppe/steppe-like openings and meadow-steppe patches in the south (especially basins and rain-shadow areas near the Sayan foothills), with grass-forb communities and high seasonal productivity.

Localized in southern basins/valleys; very small share overall (typically <~2%).

Extensive taiga landscapes forming large, often continuous blocks with relatively low fragmentation outside major settlements and industrial corridors.

Core taiga habitat dominated by larch (north/plateau), Scots pine on sandy terraces, and dark conifers (spruce, fir, Siberian cedar) in moister southern/montane zones.

Birch-aspen secondary stands and mixed patches common after fire/logging and along some river terraces in the southern and central taiga.

Open larch woodlands near the taiga-tundra ecotone and on permafrost-affected sites with sparse canopy and lichen-rich ground layers.

Moss-lichen tundra, dwarf-shrub tundra, and polygonal tundra on Taymyr and Arctic islands; important for wild reindeer migration and nesting shorebirds.

Willow/alder shrub belts on riverbanks, deltas, and tundra slopes; expands in sheltered microsites and along floodplains.

Meadow-steppe and forest-steppe clearings in the south (e.g., Minusinsk Basin area), often used for haymaking and grazing where converted.

Subalpine and alpine meadows in the Sayan Mountains, occurring between treeline and rocky summits; rich herb communities and summer pasture for ungulates.

Western/Eastern Sayan mountain systems with strong vertical zonation, steep valleys, and varied microclimates driving high habitat turnover over short distances.

Basalt escarpments and canyon walls (notably in the Putorana Plateau) providing nesting ledges and distinct cliff/ledge plant assemblages.

Large high-latitude and montane lake systems (Taymyr Lake; Putorana's deep, fjord-like lakes) with cold, oligotrophic waters and important fish habitats.

Major free-flowing and regulated reaches of the Yenisei system (including Angara, Lower Tunguska, Podkamennaya Tunguska), with broad floodplains and riparian corridors.

Floodplain wetlands, peatlands, and thermokarst depressions widespread in both taiga and tundra, supporting high seasonal bird abundance.

Shallow, sedge-dominated marshes in deltas, floodplains, and lake margins, especially in the Arctic lowlands during the brief summer.

Peat-accumulating bogs and palsas/peat plateaus in permafrost zones; key long-term carbon stores and wildfire-sensitive areas.

Low Arctic coasts with lagoons, spits, and coastal tundra along the Kara and Laptev seas, strongly shaped by sea ice and storm surges.

Arctic gravel/sand beaches and barrier features, seasonally used by birds; dynamics influenced by ice push and short open-water season.

Rocky island and headland shores (including high Arctic islands) with seabird colonies and wave/ice-scoured intertidal zones.

Nearshore and offshore Arctic waters with seasonal productivity pulses tied to ice melt and polynyas.

Predominantly shelf seabeds (soft sediments and mixed substrates) supporting benthic invertebrate communities important to higher trophic levels.

Localized deeper basins/off-shelf areas beyond the shallow shelf influence in adjacent Arctic seas (less extensive than shelf habitats).

Major urban/industrial nodes (e.g., Krasnoyarsk, Norilsk) with strong local habitat modification and pollution footprints.

Expanding peri-urban zones around major cities and transport corridors, increasing fragmentation in southern portions.

Concentrated mainly in the south (forest-steppe and river valleys) as cropland, hayfields, and pasture; limited compared to the krai's overall area.