Wildlife of
Habarovskij kraj

Dominant taiga landscapes of larch, spruce, fir, and pine with understories of mosses and ericaceous shrubs; shaped by cold winters, fire, and permafrost-influenced soils in places.

Largest share of the interior and northern parts; extensive across lowlands and foothills away from the southernmost Amur-Ussuri influence.

Southern mixed forests with Korean pine and broadleaf species (oak, elm, linden, maple), providing key habitat structure for Amur tiger and rich ungulate prey bases.

Concentrated in the south and southeast (lower Amur and Sikhote-Alin-related areas), mainly at lower elevations and warmer valleys.

Treeless or sparsely shrubby tundra-like communities in the far north and most exposed coastal/headland or high-latitude settings, with lichens, sedges, and dwarf shrubs; often associated with cold maritime winds and permafrost.

Patchy and limited-primarily northern coastal fringes and some high, windswept areas.

Above-treeline belts in mountain ranges with alpine meadows, rocky slopes, and dwarf shrub/lichen communities; important for cold-adapted plants and as summer range for some wildlife.

Scattered across higher elevations of major ranges (e.g., Dzhugdzhur and other interior/coastal mountains).

Large river corridors (especially the Amur and tributaries) with side channels, oxbows, floodplain lakes, and cold headwater streams supporting salmonid spawning and rearing.

Widespread throughout; strongest expression along the Amur basin and major tributary systems.

Amur floodplain marshes, swamps, peatlands, and seasonally inundated meadows; critical for waterfowl migration, amphibians, and nutrient cycling.

Extensive in lowlands and broad valley bottoms, especially along the middle/lower Amur and deltaic/coastal lowlands.

Cold, nutrient-rich seas of the Sea of Okhotsk and adjacent coastal waters (including the Tatar Strait), with productive shelf ecosystems, sea ice seasonality, and strong links to anadromous fish runs.

Along the entire eastern shoreline and island/coastal complexes (e.g., Shantar area) and south toward the Tatar Strait.

Continuous forest matrix across most of the krai, ranging from taiga to mixed forests; large intact tracts remain compared with many temperate regions.

Taiga stands dominated by larch and spruce-fir on colder sites; frequent post-fire succession mosaics and extensive moss/lichen ground layers.

Broadleaf and mixed deciduous elements in warmer southern valleys and lower slopes (oak, birch, aspen), often intergrading with Korean pine-broadleaf forests.

Open, patchier tree cover in fire-influenced areas, river terraces, and transition zones between dense taiga and wet meadows.

Willow/alder shrublands on floodplains and along streams, plus dwarf-shrub heaths in colder, wind-exposed sites.

Rugged ranges and dissected uplands (including coastal mountains) creating strong elevation-driven habitat zonation and refugia.

Rock faces and river bluffs used by nesting raptors and seabirds; also support specialized cliff and scree vegetation.

Major trunk rivers (Amur) and extensive tributary networks with spawning migrations of salmonids and strong flood-pulse dynamics.

Floodplain lakes and oxbow lakes in the Amur system; important for fish nurseries and waterbirds.

Large floodplain wetland complexes with seasonally inundated habitats and high productivity; important stopover for migratory birds.

Forested and shrub swamps in low-lying floodplains and poorly drained basins, often with alder and willow.

Sedge- and reed-dominated marshes in floodplains and coastal lowlands; key breeding habitat for waterfowl.

Peat-forming bogs and mire systems in cold, poorly drained areas; locally extensive in flat lowlands and permafrost-influenced terrain.

Brackish mixing zones near river mouths along the Sea of Okhotsk and Tatar Strait coasts; important for juvenile fish and migratory birds.

Sea of Okhotsk shoreline with strong seasonality (sea ice, storms) and coastal wetlands, lagoons, and rocky headlands.

Sandy and gravel beaches along parts of the coast, influenced by ice push and storm reshaping.

Rocky capes and island shorelines (notably around the Shantar region) supporting seabird rookeries and intertidal communities.

Nearshore kelp and macroalgal beds in cold, clear waters that provide shelter and feeding grounds for fish and invertebrates.

Pelagic waters offshore in the Sea of Okhotsk and adjacent straits supporting wide-ranging seabirds and marine mammals.

Deeper offshore zones beyond the shelf break where present, supporting cold-water benthic and midwater communities.

Broad continental shelf seabeds (mud/sand/gravel) that underpin productive fisheries and benthic food webs.

Urban habitats around major settlements such as Khabarovsk and Komsomolsk-on-Amur, with strong river-coastal transport corridors.

Agricultural mosaics mainly in the southern Amur lowlands and accessible river valleys, interspersed with remnant forest and wetlands.