Alien Biomes
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Aethelgard Prime
Oceanic World

Aethelgard Prime

Tidally-Locked M-Dwarf Habitable

Life on Aethelgard Prime · 4 species

KeystoneCrustal Slurry-Weaver
Crustal Slurry-WeaverSilicofluxus lithovoraKeystone species
Deep-Strata Moss
Deep-Strata MossLithoflora profundusPrimary Producer

Deep-Strata Moss (*Lithoflora profundus*) thrives within Aethelgard Prime’s perpetual dark-side subterranean fissures. Lacking chlorophyll, it harvests sulfide vent energy via dense, iridescent biofilms clinging to basalt walls. These mats glow faintly azure, pulsing rhythmically with deep geothermal fluctuations. This flora acts as the essential foundational substrate for native Weavers. Larvae embed directly into the moss’s calcified sheath, gaining critical nutrients while reinforcing fragile tunnel structures against constant seismic shifts. Without this vital chemosynthetic carpet, the entire ecosystem collapses, leaving deeper caves barren and cold to crushing planetary pressures.

Cyst Predators
Cyst PredatorsThermovora cystisParasite

On Aethelgard Prime’s perpetual terminator line, Thermovora cystis infiltrates dormant Silicofluxus colonies via microthermal vents. Microscopic faunae penetrate calcified shells during hibernation, digesting latent energy reserves without triggering awakening. Translucent bodies glow faintly against the dim red sun, exploiting metabolic pauses within the protective crust. Though parasitic, this predation regulates Silicofluxus overpopulation in the harsh twilight strip. Exhausted cysts often fail to hatch, preventing resource depletion for emerging flora. Surveys caution that dense swarms sterilize viable habitats if host density drops below sustainable levels, threatening the entire local ecosystem stability.

Mineral Bacteria
Mineral BacteriaFerrumoxidans lithosDecomposer

Ferrumoxidans lithos, or "Mineral Bacteria," thrives in the twilight zones of Aethelgard Prime, specializing in the decomposition of deceased Weavers. These microscopic colonizers secrete potent acids that dissolve the complex silica-gel matrix of their hosts, effectively liquefying rigid structures into a nutrient-rich slurry. This process is vital for planetary stability, preventing organic accumulation while liberating trapped iron and silicon. Once dissolved, the bacteria precipitate these liberated minerals directly back into the crust through rapid biomineralization. The result is a shimmering, rust-colored patina that coats Weaver grave-sites, slowly knitting new geological strata from biological remains. By closing this elemental loop, F. lithos ensures the planet's regenerative cycle continues uninterrupted beneath the eternal gaze of its dim M-dwarf sun.

World Data

star
Red Dwarf (M4V)
gravity
1.2g
atmosphere
Dense CO2/N2, High Pressure
temp
Surface 280K, Crust 400K+
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