Denisova Cave Siberia Stratigraphy & Lineage

Altai Mountains, Siberia • 300 ka to 20 ka Pleistocene Hominin Co-Occupation

Chronological Depth: 76,000 BP (76 ka)
MIS 4 (Early Glacial / Steppe-Tundra)
300 ka (Middle Pleistocene) 200 ka 100 ka (MIS 5e Interglacial) 50 ka (Initial Upper Paleolithic) 20 ka (LGM)
Stratigraphic Profile & Occupation Horizon
Paleotemperature Proxy: ~ -4.5°C anomaly (Subarctic Cold Steppe) Active: Denisovan
Click any sedimentary stratum to inspect physical deposit & tool industry East Chamber: Layer 11
Fossil Discoveries & Cultural Material 5 Key Specimens

Denisova 3 (Pinky Bone)

Denisovan Female
Layer 11 (East) ~76 - 52 ka Middle Paleolithic Levallois

The right fifth distal finger phalanx of a juvenile female Denisovan. Yielded the world's first high-coverage archaic genome (~30x) at the Max Planck Institute in Leipzig, proving Denisovans represent a distinct lineage sister to Neanderthals.

Genomic Significance: Preserved extraordinary endogenous DNA due to constant year-round sub-zero cave temperature (~0°C).

Ancient Admixture: Shared Alleles in Modern Populations

Melanesians & Indigenous Australians 4.0 - 6.0% Denisovan
Mainland East Asians & Tibetans 0.1 - 0.5% (EPAS1 Altitude Gene)
Non-African Global Populations (Neanderthal) 1.8 - 2.4% Neanderthal

Genetic Admixture Flow & Interbreeding Events

Denisova 11 ('Denny') Evidence: Direct F1 offspring born to an Altai Neanderthal mother and a Denisovan father carrying distant Neanderthal admixture.
Adaptive Introgression: High-altitude adaptation gene EPAS1 in Tibetans and lipid metabolism alleles in Inuits derived directly from Denisovan pulses.
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