Taxa axis (4 levels): Methanobrevibacter ruminantium (hydrogenotrophic), Methanobacterium spp. (H2-flexible; observed as transient colonizer before Methanobrevibacter dominance ), Methanosphaera stadtmanae (methylotrophic; can persist when Methanobrevibacter is suppressed ), and Methanoculleus/Methanofollis-type hydrogenotrophs (landfill-dominant, 92% of clones hydrogenotrophic where pH and total phosphorus shaped community structure ). Monoxenic + all pairwise co-cultures.
Mineral axis (4 levels): basalt powder, serpentine/olivine, Fe-sulfate (jarosite-like), and phyllosilicate clay — autoclaved, sterile, characterized by XRD/BET. Nutrient baseline buffered to the observed alkaline-alkaline (pH 8–9.4) range where hydrogenotrophs thrive.
Atmosphere axis (3 levels): Mars-analog (95% CO2, 2% N2, trace H2, ~50–100 mbar), Mars-analog at 1 atm, and Earth-analog negative control. Temperature +2°C (Mars-analog) and 37°C (physiological control). n = 4 biological replicates × 4 taxa × 4 minerals × 3 atmospheres = 192 microcosms; use a fractional factorial screen (resolution V) before full deployment.
Sources: reported values from a 10-cow Holstein trial (small n, 5/group, SF6 tracer has known uncertainties — a stated limitation).
Blindspots: no supplied source directly tests Mars-like pressure or gas composition; Mars-analog threshold values (mbar, H2 partial pressure) must be set from planetary-science literature not present here. Composition–causation links in supplied data are correlative; causal tests require the monoxenic arms.
Assumptions: exponential decay to low-pressure steady state; uncertainty spans ±30–50% based on variance seen in animal trial CH4 data (e.g., 221.9–336.8 g/head/day control range). Values are modeled expectations only.
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