A board is a persistent structured configuration of matter or energy that operates under a dominant constraint regime and possesses internal thresholds governing its state transitions.
A board requires:
Bounded structure
Operational stability
Defined state-change thresholds
Persistence relative to surrounding fluctuations
Boards begin when stable bound states emerge.
No bound state, no board.
An atom is a board.
A rock is a board.
A flame is a board.
A river basin is a board.
A planet is a board.
Boards are stable for now.
Disciplines: physics, materials science, thermodynamics, geology
Boards are nested hierarchically.
Lower boards operate within the allowances of higher boards.
Atomic boards operate within nuclear constraints.
Mineral boards operate within atomic bonding rules.
River boards operate within climatic and tectonic constraints.
Planetary boards operate within stellar and radioactive constraints.
Dominance flows downward.
Internal failure occurs when thresholds are exceeded under unchanged dominant constraints.
External override occurs when a higher board shifts the regime.
These must be distinguished.
Disciplines: systems theory, geophysics, planetary science
Boards differ by configuration of interlinked variables:
1. Budget — total energy flux available.
2. Transport capacity — how matter and energy move.
3. Scale — spatial extent.
4. Sparsity — dispersion relative to scale and budget.
5. Disturbance regime — frequency and amplitude of shocks.
6. Turnover rate — renewal relative to structural lifespan.
These variables are coupled:
Budget and scale influence sparsity.
Transport modifies effective sparsity.
Disturbance shapes turnover.
Turnover governs memory retention.
Boards are constraint labs defined by these parameters.
Disciplines: ecology, fluid dynamics, statistical mechanics
Variance and Mobility
Sparse boards amplify intake variance.
Low encounter probability increases fluctuation in resource acquisition.
High variance selects for:
Mobility (reduces spatial variance)
Longevity (averages temporal variance)
Storage (buffers amplitude)
Reproductive insurance
Search cost must remain below expected intake.
Search cost < expected intake.
Large sparse boards — deserts, deep sea — select for efficient movement and long survival windows.
Dense boards reduce variance and allow reduced mobility.
Variance drives architecture.
Disciplines: population ecology, evolutionary biology, statistical physics
When Renewal Is Slower Than Residue Accumulation
Archive boards exist when:
Structural renewal rate < residue accumulation rate.
Examples:
Atacama Desert:
Minimal rainfall
Low mechanical erosion
Long surface persistence
Meromictic lakes:
Stable stratification
Minimal vertical mixing
Long sediment retention
Archive status depends on low disturbance and low turnover.
Stable for now.
Disciplines: sedimentology, limnology, paleoclimatology
Narrowing Configuration Space
Board hardening is progressive narrowing of allowable configuration space.
Deep sea hardening involved:
Cooling
Oxygenation
Circulation stabilization
Constraints intensified:
Lower temperature
Higher pressure
Thin energy flux
Configuration space narrowed, selecting specialized architectures.
Hardening increases time constants and reduces allowable variation.
Disciplines: oceanography, evolutionary biology, thermodynamics
Under aridification, river persistence depends on:
Headwater security
Elevation gradient
Basin integration
The Orange River persisted because:
Upstream rainfall remained sufficient.
Incision maintained channel function.
Basin scale buffered climate variability.
Failure occurs when active transport ceases under unchanged constraints.
Dry paleochannels represent deletion of flow memory.
Disciplines: geomorphology, hydrology, climate science
Maintenance-to-Intake Ratio
Scaling is governed by:
Maintenance cost / intake flux.
If this ratio decreases, scaling up is viable.
If it increases, scaling down is enforced.
Gigantism appears where:
Insulation reduces heat loss (polar boards)
Buoyancy reduces maintenance cost (deep sea)
Intake predictable (open oceans, savannas)
Bulk functions as insulation plus reserve.
Dwarfism emerges when intake cannot sustain maintenance demands.
Resizing aligns architecture with budget.
Disciplines: physiology, metabolic ecology, island biogeography
When Persistence Requires Departure or State Change
Exit boards arise when local persistence cannot be maintained indefinitely because constraint escalation will exceed repair capacity.
Repair time constant < disturbance escalation → persistence possible.
Repair time constant > disturbance escalation → exit required.
There are two distinct exit regimes.
Variance-Driven Escape
Erratic exit boards are dominated by high-amplitude, unpredictable disturbance.
Characteristics:
Disturbance timing uncertain.
Spatial patchiness variable.
Amplitude fluctuating.
Repair window narrow.
Examples:
Fire-prone savannas
Flash-flood deserts
Cyclone coasts
Volcanic zones
Even seasonal fire regimes remain erratic because:
Ignition timing varies.
Intensity varies.
Spatial extent varies.
Architecture under erratic exit boards favors:
Elasticity
Rapid mobility
Reproductive staging
Investment flexibility
Kangaroos demonstrate reproductive elasticity in forage-variable landscapes.
Flight in birds is an erratic exit architecture.
In open savanna boards, ostriches demonstrate architectural shift:
Horizontal speed became cheaper than aerial escape.
The board stopped paying for wings.
Erratic exit boards select for flexible, reactive escape.
Disciplines: disturbance ecology, behavioral ecology, evolutionary biology
Predictable Cyclical Transition
Planned exit boards are dominated by predictable, periodic constraint shifts.
Characteristics:
Disturbance timing regular.
Resource windows cyclical.
Transition window known.
Examples:
Migratory flyways
Arctic seasonal systems
Monsoon-dependent ecosystems
Anadromous salmon runs
Architecture under planned exit boards favors:
Energy staging before departure
Timing precision
Corridor memory
Long-range navigation
Migration is anticipatory.
Systems move before local collapse.
If periodicity destabilizes, planned exit boards degrade into erratic boards.
Disciplines: migration ecology, chronobiology, population dynamics
Material Possibility and Radioactive Time
Heavy element production enabled:
Rocky planet formation
Mineral diversity
Surface chemistry complexity
Radioactive isotopes function as timed boards:
Decay defines internal heat persistence
Heat drives tectonics
Tectonics reshapes surface boards
Half-life sets internal energy time constant.
Cosmic boards define material possibility before biological boards emerge.
Disciplines: astrophysics, nuclear physics, planetary geology
Atomic board:
Bound electron structure
Ionization thresholds
Excitation states
Rock board:
Mineral lattice
Fracture thresholds
Melting thresholds
Porosity constraints
A flame is a reactive board.
A cloud is a transient board.
A radioactive isotope is a timed board.
Boards begin at bound-state formation.
Disciplines: atomic physics, crystallography, combustion chemistry
Boards remain stable while dominant constraints remain continuous.
Internal failure occurs when persistence thresholds are exceeded under unchanged constraints.
External override occurs when higher-level constraint regimes shift.
Failure deletes active structural persistence.
Residue may remain.
Stable for now.
Disciplines: resilience science, systems theory, evolutionary dynamics
Boards are persistent structured configurations under constraint.
They differ by:
Budget
Transport
Scale
Sparsity
Disturbance
Turnover
Sparse boards amplify variance.
Archive boards preserve memory.
Hardening boards narrow configuration space.
Resizing boards align scale with budget.
Exit boards require mobility or timing discipline.
Cosmic boards define material possibility.
Nothing permanent.
Only structures that remain affordable under current constraints.
Stable for now.