Biology Environment: Canonical Domain Analysis
Status: Canonical reference. Full 12-step analysis of the biology environment — the context domain (independent root) of the biology arrangement. The Cx primitive of the SSA when the SSA is instantiated for biology.
Domain kind (R1): Context (constraint) domain. Environment primitives describe STATES that constrain the biology arrangement from outside. They are determined by physics, chemistry, geology, and astronomy — forces independent of biology (mostly; the natural/cultural entanglement applies, see §11.2).
Position in the topology: Independent root. Connects to biology substrate via constraint edges (environment shapes which lattice positions are achievable). Connects to ecosystem via context-mediation edges (environment constrains the ecosystem; ecosystem feeds back to environment via niche construction).
Parallel to: Digital context {Cm, Pl, Lb, Co, Sd, Pr} (entity arrangement, 6 primitives). Cognitive context {Rb, Gs, Po, If, Ks, Th} (cognitive arrangement, 6 primitives). The structural template is shared across information-substrate arrangements: context root with ~6 primitives, feedback loops with surface activity, partly natural and partly accumulated.
Reference (not basis for copying): v1_revision/v1_biology_domain_analysis/bio_v1/exploration-environment-and-ecosystem.md §1-2 contains the v1-era analysis (paired with ecosystem analysis, which is deferred to a separate canonical doc).
Step 1 — Information Gathering
1.1 What we're analyzing
The abiotic physical-chemical-geological-temporal context within which biological life exists. What's GIVEN by physics, chemistry, geology, and astronomy. What organisms ADAPT to but do not (usually) choose.
In scope:
- Energy availability (solar, geothermal, chemical)
- Climate (temperature, precipitation, their patterns)
- Chemistry (atmospheric, aquatic, soil composition)
- Physical structure (terrain, substrate, spatial arrangement)
- Temporal patterns (cycles at multiple scales)
- Disturbance regimes (fire, flood, storm, geologic events)
Not in scope: the biotic community itself (ecosystem domain — separate analysis); organism-level adaptations (organism architecture); metabolism (biology substrate).
1.2 Sources
- Ecology — Begon, Townsend & Harper, Ecology: From Individuals to Ecosystems; Odum, Fundamentals of Ecology
- Climatology — Hartmann, Global Physical Climatology; Trenberth, Climate System Modeling
- Geology / Earth science — Press & Siever, Understanding Earth
- Biogeochemistry — Schlesinger & Bernhardt, Biogeochemistry: An Analysis of Global Change
- Disturbance ecology — Pickett & White, The Ecology of Natural Disturbance and Patch Dynamics
- Astrobiology / planetary science — Kasting & Catling, Astrobiology: A Very Short Introduction
- Niche construction theory — Odling-Smee, Laland & Feldman, Niche Construction: The Neglected Process in Evolution
1.3 The landscape (instances we will position)
| Environment | Character |
|---|---|
| Deep ocean floor | Stable, low-energy, low-disturbance |
| Hydrothermal vent | Chemosynthetic, extreme chemistry, geological disturbance |
| Tropical reef | High-energy, stable climate, complex 3D structure |
| Tropical rainforest | High-energy, low seasonality, complex canopy |
| Temperate forest | Moderate-energy, seasonal, periodic disturbance |
| Savanna | High-energy, seasonal, fire-driven |
| Desert | High-energy, water-limited, simple structure |
| Arctic tundra | Low-energy, extreme cold, permafrost dynamics |
| Estuary | Variable salinity, tidal dynamics |
| Fire-prone shrubland (chaparral, fynbos) | Fire-defined community structure |
Step 2 — Landscape Analysis
2.1 What recurs across all environments
Every biological environment exhibits:
- Energy input — solar, geothermal, chemical
- Climate regime — temperature and precipitation patterns
- Chemical composition — what's available in atmosphere, water, soil
- Physical structure — terrain, substrate, spatial arrangement
- Temporal patterns — cycles at multiple time scales
- Disturbance regime — frequency and intensity of disruptive events
These recur across all habitats from abyssal vents to alpine peaks.
2.2 Why environment is a context domain
Environments are states, not products. Energy input, climate, chemistry, structure, temporal patterns, and disturbance regimes describe the conditions under which life operates. They are the independent inputs to the biology arrangement — biology adapts to them, not the other way around (with the exception of niche construction, where the biotic community partially modifies its abiotic context; see §11.2).
This contrasts with substrate domains (where primitives describe what the substrate IS) and surface domains (where primitives describe what the substrate produces). Context primitives describe what surrounds the substrate-surface chain.
Step 1b — Domain Type Declaration
Context (constraint) domain — independent root. Predicted properties from R11:
- ~6 primitives — confirmed at 6
- Filter: tight, similar to substrate range (12-20%) — confirmed at 17%
- Independent root: not produced by the biology arrangement — confirmed
- Some primitives natural (En, Cl, Ch, St, Tm); some can accumulate from prior biotic activity (atmospheric oxygen content, soil organic matter, modified disturbance regimes from human activity) — natural/cultural entanglement applies
SSA mapping: Cx primitive of the biology arrangement. The biology arrangement's full SSA is: En = biology substrate {G, T, R, P, Reg, Mem}; Vr = ribosome (R within En); Mc = developmental mechanisms (biology-to-organism bridge); Sf = organism architecture; Cm = ecosystem; Cx = environment (this domain); Se = natural selection (within ecosystem analysis).
Step 3/3b — Primitives and Partial Levels
3.1 Six primitives
| # | Primitive | Definition | What it constrains for life |
|---|---|---|---|
| 1 | Energy (En) | Available energy flux: solar, geothermal, chemical | Primary productivity ceiling; metabolic strategy choice |
| 2 | Climate (Cl) | Temperature and precipitation regimes | Biochemical operating conditions; water availability |
| 3 | Chemistry (Ch) | Ambient chemical composition (atmospheric, aquatic, soil) | Metabolic substrate availability; nutrient limitation |
| 4 | Structure (St) | Physical substrate, spatial arrangement, 3D habitat geometry | Habitat availability; niche space; physical support |
| 5 | Temporal (Tm) | Time-varying patterns at multiple scales | Activity timing; life history timing |
| 6 | Disturbance (Db) | Abiotic disruption events: fire, flood, storm, geologic events | Community reset frequency; selection regime |
Note on primitive symbol collision: Both chemistry and the environment have a primitive abbreviated St. They are distinct (chemistry St = molecular structure; environment St = physical/topographic structure). In schema-encoded data they are scoped by their domain, so no actual collision. In prose, qualify as St (chemistry) or St (environment) when ambiguous.
3.2 Stability under 3/3b iteration
Splitting candidates rejected:
- Gravity as a 7th primitive. Constant for terrestrial life (1g). Matters for aquatic life (buoyancy) but subsumed by St (physical substrate). Would need to be separate for cross-planetary analysis.
- Radiation (UV, ionizing) as a 7th primitive. Subsumed by En (energy flux includes radiation spectrum). Surface UV is a function of atmospheric composition (Ch) and latitude (En).
- Pressure as a 7th primitive. Subsumed by St + Ch (atmospheric pressure = f(altitude); hydrostatic = f(depth)).
- Photoperiod as a 7th primitive. Subsumed by Tm — day length IS a temporal regime parameter.
Collapsing candidates rejected:
- Tm and Db merged into "Dynamics." Rejected — temporal patterns are predictable cycles; disturbance is stochastic events. Different statistical character, different selective consequences. Different evolutionary responses (anticipation for Tm; resistance/resilience for Db).
- Cl and Ch merged into "Conditions." Rejected — climate (temperature + water) and chemistry (composition) are independently variable. Same temperature can have different chemistry (deserts vs rainforests at similar temperature have different soil chemistry); same chemistry can have different temperature (warm vs cold ocean).
Verdict: 6 primitives stable.
3.3 Partial levels
Energy (En):
| Level | Description | Example |
|---|---|---|
| En0 | No energy input | Theoretical (interstellar space) |
| En1 | Chemical energy only | Deep subsurface, hydrothermal vents (chemosynthetic), caves |
| En2 | Low solar + chemical | Deep ocean floor (organic rain), polar winter, dense forest understory |
| En3 | Moderate solar | Temperate regions, mid-depth aquatic, cloud forests |
| En4 | High solar | Tropics, shallow aquatic, grasslands, deserts |
| Full En | Abundant multi-source | Tropical shallow marine (solar + tidal + wave + chemical), estuaries |
Phase transition: En1 → En2 (solar energy availability). Below: only chemosynthesis (limited to specific chemical gradients). Above: photosynthesis possible — solar → biomass → entire food web. On Earth, this transition happened ~3.5 Gya when photosynthetic organisms colonized sunlit environments.
Climate (Cl):
| Level | Description | Example |
|---|---|---|
| Cl0 | No climate | Vacuum/space |
| Cl1 | Extreme stable | Deep ocean (~2-4°C), deep caves |
| Cl2 | Moderate stable | Tropical marine, tropical lowland forest |
| Cl3 | Moderate variable | Temperate regions (seasonal) |
| Cl4 | Extreme variable | Continental interiors, deserts |
| Full Cl | Extreme + unpredictable | Arctic/subarctic, high alpine |
Phase transition: Cl2 → Cl3 (seasonality). Below: relatively constant year-round. Above: organisms must sense seasons, adjust metabolism, time reproduction. Where biology's Reg and developmental timing become ecologically critical.
Chemistry (Ch):
| Level | Description | Example |
|---|---|---|
| Ch0 | No chemistry accessible | Vacuum, pure water |
| Ch1 | Minimal nutrients | Oligotrophic ocean, nutrient-poor soils |
| Ch2 | Moderate balanced | Temperate soils, mesotrophic lakes |
| Ch3 | Nutrient-rich | Eutrophic lakes, river deltas, volcanic soils |
| Ch4 | Chemically extreme | Hypersaline, hyperacidic, hypoxic |
| Full Ch | Complex multi-gradient | Estuaries, hot springs, hydrothermal vents |
Phase transition: Ch1 → Ch2 (nutrient sufficiency). Below: growth is nutrient-limited (Liebig's law). Above: nutrients sufficient; energy or competition become limiting.
Structure (St) — physical/topographic:
| Level | Description | Example |
|---|---|---|
| St0 | No physical structure | Open water column (pelagic), open atmosphere |
| St1 | Simple substrate | Flat seabed, sand desert, grassland (effectively 2D) |
| St2 | Heterogeneous substrate | Rocky shore (tide pools, crevices), forest floor |
| St3 | Three-dimensional structure | Coral reef, forest canopy, cave systems, kelp forest |
| St4 | Complex 3D with microhabitats | Old-growth forest, mangrove |
| Full St | Dynamic 3D structure | River systems (meandering, flood-driven), glacial landscapes, active volcanic |
Phase transition: St2 → St3 (three-dimensional structure). Below: effectively 2D habitat. Above: vertical extension multiplies niche space (arboreal vs terrestrial vs fossorial).
Temporal (Tm):
| Level | Description | Example |
|---|---|---|
| Tm0 | No temporal variation | Deep ocean floor, deep cave |
| Tm1 | Diurnal only | Tropical equatorial (no seasons) |
| Tm2 | Tidal + diurnal | Intertidal zones |
| Tm3 | Seasonal + diurnal | Temperate regions |
| Tm4 | Multi-scale temporal | Mediterranean (seasonal + multi-year drought + fire cycles) |
| Full Tm | Geological-scale dynamics | Glacial-interglacial cycles, volcanic archipelago formation |
Phase transition: Tm1 → Tm3 (seasonality). Same threshold as Cl2 → Cl3 from the temporal side. Organisms must track time scales longer than diurnal.
Disturbance (Db):
| Level | Description | Example |
|---|---|---|
| Db0 | No disturbance | Stable deep ocean, stable deep cave |
| Db1 | Rare, low intensity | Stable temperate forest |
| Db2 | Periodic, moderate | Savanna (seasonal fire), flood plain (annual flood), tidal |
| Db3 | Frequent, intense | Fire-prone shrubland (fynbos, chaparral), typhoon coast |
| Db4 | Catastrophic | Volcanic zones, earthquake-prone |
| Full Db | Regime-defining | Yellowstone-type (fire defines ecosystem structure), barrier island |
Phase transition: Db1 → Db2 (periodic disturbance). Below: disturbance rare, climax community develops. Above: disturbance recurs on ecological time scales — community structure includes disturbance adaptation. Disturbance becomes a selective force.
3.4 Phase transition summary
| Primitive | Levels | Phase transition | Significance |
|---|---|---|---|
| En | 6 | En1 → En2 | Photosynthesis becomes possible |
| Cl | 6 | Cl2 → Cl3 | Seasonality begins |
| Ch | 6 | Ch1 → Ch2 | Nutrient sufficiency |
| St | 6 | St2 → St3 | 3D habitat extension |
| Tm | 6 | Tm1 → Tm3 | Multi-scale temporal tracking required |
| Db | 6 | Db1 → Db2 | Disturbance as selective force |
Steps 4–6 — Dependencies, Pairs, Load Classification
4.1 Primitive-presence dependencies
Cl → En climate regime depends on energy input (solar drives temperature/precipitation)
Ch → Cl chemistry depends on climate (temperature affects solubility, weathering, gas exchange)
St → Ch physical structure depends on chemistry (soil formation, mineral substrate, reef building)
Tm → En temporal patterns driven by energy input cycles (solar day, seasons, tides)
Db → Cl disturbance regime depends on climate (drought drives fire; storms drive flood)
Db → St disturbance regime depends on structure (fuel structure determines fire behavior; topography channels floods)
DAG:
En
│
┌───┴───┐
▼ ▼
Cl Tm
│
▼
Ch
│
▼
St
│
┌───┴───────┐
▼ ▼
{Cl, St} ← Db (depends on both)
En is the hub — no dependencies; everything traces back to energy input. Mostly linear chain En → Cl → Ch → St with Db requiring both Cl and St (the disturbance regime requires both climate driving and topographic channeling), and Tm branching from En only.
4.2 Conditional partial-level dependencies
| Constraint | Reasoning |
|---|---|
| Dep(Cl ≥ 3, En ≥ 3) | Seasonal climate requires moderate-to-high solar input |
| Dep(Ch ≥ 3, Cl ≥ 2) | Nutrient-rich chemistry requires liquid water (climate sufficient) |
| Dep(St ≥ 3, Ch ≥ 2) | 3D habitat structure (reefs, forests) requires nutrient sufficiency for the structure builders |
| Dep(St ≥ 4, St ≥ 3 prior, Tm ≥ 3) | Microhabitat complexity requires both prior 3D structure and temporal differentiation |
| Dep(Db ≥ 3, En ≥ 4) | Frequent intense disturbance (fire-prone) requires high energy (fuel productivity) |
| Dep(Db ≥ 4, Tm ≥ 3) | Catastrophic disturbance regimes require long-time-scale dynamics |
5.1 Pair enumeration
C(6, 2) = 15 pairs.
6.1 Load classification
Heavy (6):
| Pair | Name | Content |
|---|---|---|
| En-Cl | Energy → climate | Solar input determines temperature and precipitation patterns. The primary physical driver. |
| Cl-Ch | Climate → chemistry | Temperature drives weathering rates, gas solubility, nutrient cycling. |
| Ch-St | Chemistry → structure | Soil formation from mineral weathering. Reef building from CaCO₃ chemistry. Geochemistry → substrate. |
| Cl-Db | Climate → disturbance | Drought → fire. Storm → flood. Freeze-thaw → rockfall. Climate regime → disturbance regime. |
| En-Tm | Energy → temporal | Solar cycles drive diurnal, seasonal, tidal patterns. Orbital mechanics → Milankovitch cycles. |
| St-Db | Structure → disturbance | Topography channels floods. Fuel structure determines fire behavior. Slope determines landslide risk. |
Medium (5):
| Pair | Name | Content |
|---|---|---|
| En-Ch | Energy → chemistry | Photochemistry. Ozone formation. UV-driven reactions. |
| Cl-Tm | Climate-temporal | Climate has temporal dimensions (variability, seasonality regimes). Closely linked to En-Tm. |
| Ch-Tm | Chemistry-temporal | Geochemical cycles operate at multiple time scales (carbon cycle, nutrient cycling). |
| St-Tm | Structure-temporal | Geomorphological time scales. Erosion, deposition, landform evolution. |
| Tm-Db | Temporal-disturbance | Disturbance frequency IS a temporal pattern. |
Light (4):
| Pair | Name | Content |
|---|---|---|
| En-St | Energy-structure | Solar gradient creates topographic differentiation (slope aspect → microclimate). |
| En-Db | Energy-disturbance | Energy budget affects disturbance intensity (e.g., hurricane energy from sea surface temperature). |
| Ch-Db | Chemistry-disturbance | Chemical disturbance (acid rain, volcanic gas). Mostly mediated by Cl-Db. |
| Tm-Db is already medium (above) |
Wait — recounting. C(6,2) = 15. Heavy 6 + Medium 5 + Light 4 = 15. ✓
Negligible: none.
Distribution: 6/5/4/0 (40% heavy). At the typical level for 6-primitive domains.
6.2 Anchor analysis
- En (Energy): in 3 of 6 heavy pairs (En-Cl, En-Tm; plus En-Ch medium, En-St light). Primary anchor.
- Cl (Climate): in 3 of 6 heavy pairs (En-Cl, Cl-Ch, Cl-Db). Secondary co-anchor.
En and Cl are co-primary anchors. En is the upstream input; Cl is the proximate driver of the rest. Together they exercise the primary heavy structure.
Cross-domain comparison:
| Context domain | Primary anchor | What it concentrates |
|---|---|---|
| Biology environment | En + Cl | Energy and climate as physical drivers |
| Digital context | Cm + Pl | Compute and platform as digital drivers |
| Cognitive context | Rb + Gs | Resources and geography as material drivers |
Across context domains, the primary anchor is the upstream physical/material driver that the rest of the context derives from.
Steps 7–8 — Lattice and Hasse Walks
7.1 Coherent sub-lattice
Valid subsets (En has no deps; Cl needs En; Ch needs Cl; St needs Ch; Tm needs En; Db needs Cl AND St):
| # | Subset | Environmental identity |
|---|---|---|
| 1 | {} | No environment (vacuum) |
| 2 | {En} | Energy only — pure radiative environment |
| 3 | {En, Tm} | Energy with temporal cycles — bare planet with rotation |
| 4 | {En, Cl} | Energy and climate — atmosphere develops |
| 5 | {En, Cl, Tm} | Energy + climate + cycles |
| 6 | {En, Cl, Ch} | Adds chemistry — water, nutrients available |
| 7 | {En, Cl, Ch, Tm} | Above + temporal cycles |
| 8 | {En, Cl, Ch, St} | Adds structure — landforms develop |
| 9 | {En, Cl, Ch, St, Tm} | All non-disturbance primitives |
| 10 | {En, Cl, Ch, St, Db} | All except temporal cycles (theoretical) |
| 11 | {En, Cl, Ch, St, Db, Tm} | Full environment |
11 / 64 = 17.2% coherent. Tight — comparable to biology substrate (12.5%) and chemistry (20%). Sequential chain En → Cl → Ch → St with Db requiring both Cl and St creates the tight filter.
Comparison with other context domains:
| Context | Filter |
|---|---|
| Biology environment | 17% |
| Digital context | ~20% (per analysis-digital-context.md) |
| Cognitive context | similar |
Context domains cluster at substrate-like filter stringency (~12-20%) — consistent with R11's prediction that context resembles substrate in tightness.
7.2 Hasse walks
The mostly-linear dependency structure produces a small number of paths. Two main paths from {} to Full:
- Path α (chain-then-branch): En → En,Cl → En,Cl,Ch → En,Cl,Ch,St → En,Cl,Ch,St,Tm → Full. Linear chain through the substrate-like primitives, then add Db.
- Path β (early-temporal): En → En,Tm → En,Cl,Tm → ... → Full. Tm activated early, parallel to the rest.
The chain part (En → Cl → Ch → St) is invariant — these primitives must come in this order. Tm and Db can interleave.
Step 9 — Load-Bearing Compositions
9.1 Triangles
| Triangle | Name | Emergent property |
|---|---|---|
| En-Cl-Ch | Physical-chemical environment | Determines biochemistry possibilities. Where life CAN happen. |
| Cl-Ch-St | Habitat formation | Soils, reefs, weathered substrates. Where life FINDS a home. |
| En-Cl-Tm | Energy-climate-time | Seasonality, diurnal cycles. The temporal-physical envelope. |
| Cl-St-Db | Disturbance regime | Climate × structure determine disturbance type and frequency. |
9.2 Core triad
{En, Cl, Ch} — energy + climate + chemistry. "What is the physical-chemical context for biochemistry?"
Energy drives climate; climate drives chemistry. These three determine what biochemistry is possible. Without any one vertex, the context for life collapses — energy alone with no climate or chemistry is sterile (lunar surface); climate alone with no chemistry is uninhabitable (atmosphere without substrates); chemistry alone with no climate is frozen.
Step 10 — Emergent Property Map
| Property | Required composition | Required regime | Prediction |
|---|---|---|---|
| Habitable zone | En + Cl | En ≥ 2, Cl ≥ 1 | Energy + non-extreme climate enables liquid water |
| Photosynthetic productivity | En-Cl-Ch | En ≥ 2, Cl ≥ 2, Ch ≥ 2 | Solar + non-extreme + nutrients = primary productivity |
| Niche differentiation | St ≥ 3 | St ≥ 3 | 3D structure multiplies niche space |
| Seasonal life history | Cl-Tm | Cl ≥ 3, Tm ≥ 3 | Seasonal climate drives seasonal organism behavior |
| Fire-adapted communities | Cl-St-Db | Cl ≥ 3, St ≥ 1, Db ≥ 2 | Periodic fire selects fire-adapted species |
| Niche construction effects | All present | Full set, with bidirectional Cm feedback | Ecosystem activity modifies environment (oxygen, soil, hydrology) |
Steps 11–12 — Structural Patterns and Literature Alignment
11.1 Cross-domain patterns
Context as constraint root. Replicates across analyzed arrangements: biology (environment), entity system (digital context), cognition (cognitive context). All three have ~6 primitives, all three are independent roots not produced by their substrate chains.
Filter stringency at substrate range. Biology environment 17%, digital context ~20%, cognitive context similar. R11's prediction that context resembles substrate in tightness holds.
Anchor at upstream driver. Each context domain's anchor is its upstream physical/material primitive. Biology environment anchors on En + Cl (physical drivers); digital context anchors on Cm + Pl (compute infrastructure); cognitive context anchors on Rb + Gs (material resources + geography).
Core triad type. Per R11, context core triads handle "external constraint flow." Biology environment {En, Cl, Ch} captures the physical-chemical chain that constrains biochemistry. Replicates as analogous chains in other context domains.
11.2 The natural/cultural entanglement
Some context primitives are partly natural and partly modified by accumulated biotic activity:
| Primitive | Natural component | Accumulated component |
|---|---|---|
| En | Solar input (planetary) | Energy harvesting infrastructure (no — biology doesn't modify solar input) |
| Cl | Climate from physics | Anthropogenic climate change (modern, post-Holocene) |
| Ch | Initial atmosphere/oceans | Atmospheric oxygen (from photosynthesis); soil organic matter (from decomposers); ocean acidification (modern) |
| St | Geology, erosion | Coral reefs (constructed by biota); soil structure (modified by life); urban structure (modern) |
| Tm | Orbital mechanics | (none significant) |
| Db | Geological events, weather | Anthropogenic fire regimes; flood regulation by dams; storm intensity from climate change |
Niche construction (Odling-Smee et al.) is the formal recognition that biology partially modifies its own context. The methodology accommodates this through feedback edges from ecosystem (Cm) to environment (Cx), creating bidirectional context-community coupling that the original SSA topology represents as the niche-construction cycle.
The natural/cultural entanglement is the structural signature of context evolution: at any moment, the context primitives are STATES that constrain biology, regardless of whether those states arose naturally or were modified by prior biotic activity.
12.1 Literature alignment
- Geographical ecology / biogeography (Cox, Moore). Confirmed: environment determines biome, biome determines what biology is possible. The methodology's En-Cl-Ch triad maps to the Köppen-Geiger climate-vegetation correspondence.
- Disturbance ecology (Pickett, White). Confirmed: disturbance is a structural primitive, not a perturbation. The methodology classifies it as Db and tracks its partial levels (Db0 through Full Db) — matches the disturbance ecology literature on regime-defining disturbance types.
- Niche construction theory (Odling-Smee, Laland, Feldman). The natural/cultural entanglement section captures niche construction as the bidirectional Cx ↔ Cm feedback edge in the SSA. Methodology and theory agree.
- Astrobiology / habitable zone (Kasting, Catling). The lattice position {En ≥ 2, Cl ≥ 1, Ch ≥ 1} corresponds to the classical habitable zone. The methodology generalizes — habitability depends on the full environment lattice position, not just liquid water.
Manifestation Landscape — Earth environments
| Environment | En | Cl | Ch | St | Tm | Db |
|---|---|---|---|---|---|---|
| Deep ocean floor | 1 | 1 | 2 | 1 | 0 | 0 |
| Hydrothermal vent | 1 | 1 | F | 2 | 0 | 2 |
| Tropical reef | 4 | 2 | 3 | 3 | 2 | 2 |
| Tropical rainforest | 4 | 2 | 3 | 4 | 1 | 1 |
| Temperate forest | 3 | 3 | 2 | 3 | 3 | 1 |
| Savanna | 4 | 3 | 2 | 1 | 3 | 2 |
| Desert | 4 | 4 | 1 | 1 | 3 | 1 |
| Arctic tundra | 2 | F | 1 | 1 | 3 | 2 |
| Estuary | 3 | 3 | F | 2 | 2-3 | 2 |
| Fire-prone shrubland | 4 | 3 | 2 | 2 | 3 | 3-F |
(F = Full)
Attractor positions
Real environments cluster at:
- Stable deep / cave (En1, Cl1, Ch2, St1, Tm0, Db0) — low-energy stable.
- Tropical productive (En4, Cl2, Ch3, St3-4, Tm1, Db1-2) — high-energy productive.
- Temperate seasonal (En3, Cl3, Ch2, St3, Tm3, Db1) — moderate, seasonal.
- Disturbance-defined (En4, Cl3, Ch2, St2, Tm3, Db3-F) — communities defined by disturbance regime.
These attractors correspond to Earth's major biome classifications.
Summary
Domain: Biology environment (Cx primitive of biology arrangement).
Domain kind: Context (constraint) domain — independent root.
Primitive set: {En, Cl, Ch, St, Tm, Db}. Note St (environment, physical/topographic) is distinct from St (chemistry, molecular).
Filter stringency: 11/64 = 17.2%. Tight — substrate-range, consistent with R11.
Pair distribution: 6 heavy / 5 medium / 4 light / 0 negligible. 40% heavy (typical).
Core triad: {En, Cl, Ch} — energy + climate + chemistry. Determines biochemistry possibilities.
Primary anchors: En (Energy) and Cl (Climate) — the upstream physical drivers.
Phase transitions: En1 → En2 (photosynthesis); Cl2 → Cl3 (seasonality); Ch1 → Ch2 (nutrient sufficiency); St2 → St3 (3D habitat); Tm1 → Tm3 (multi-scale time); Db1 → Db2 (disturbance as selective force).
Cross-domain parallel: Same structural template as digital context (entity arrangement) and cognitive context (cognitive arrangement). All three have ~6 primitives, all are independent roots, all have feedback loops with their respective ecosystems (niche construction analog).
Open work:
- Ecosystem domain analysis (separate canonical doc, deferred)
- Environment-to-ecosystem bridge analysis
- Context evolution dynamics — how primitives accumulate over time (anthropogenic Db, atmospheric oxygen)
- Cross-arrangement context sharing — does shared physics (Sc4 in current methodology) imply cross-context coupling?
Referenced by the model
Cited as a source by 1 model record (browse the model census):
- environment-context —
domainbiology/sc1