Ecological Succession

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Core Idea

Ecological succession is the directional, predictable change in community composition over time following a disturbance or the colonization of a new substrate. Primary succession begins on bare substrate (e.g., after glacial retreat or volcanic eruption), starting with pioneer species that modify the abiotic environment. Secondary succession occurs where soil and seeds remain after disturbance (e.g., after fire or agricultural abandonment). The intermediate disturbance hypothesis predicts that moderate disturbance frequency maximizes species diversity by preventing competitive exclusion.

How It's Best Learned

Follow a successional chronosequence — compare sites of different ages after a known disturbance and track community composition changes. Distinguish facilitation, tolerance, and inhibition models of succession. Study Glacier Bay (primary) and old-field succession (secondary) as classical cases.

Common Misconceptions

Explainer

From community ecology, you know that species don't just coexist — they compete, facilitate each other, and shift in relative abundance over time. Ecological succession is what happens when you zoom out and watch that process unfold over years, decades, or centuries following a disturbance or the creation of new habitat. It is the directional, somewhat predictable turnover of species assemblages through time.

The most important first distinction is between primary and secondary succession. Primary succession starts on bare substrate where no life previously existed and no soil is present — think of the rock left behind as a glacier retreats, or the fresh lava field after an eruption. There is nothing to start with except rock and atmosphere. Pioneer species — typically hardy lichens, mosses, and nitrogen-fixing bacteria — are the first colonizers. They can tolerate the harsh abiotic conditions (extreme temperature swings, no water retention, no nutrients) and, crucially, they begin to modify those conditions: lichens chemically weather rock, organic matter accumulates, soil begins to form. This is facilitation — early species make the environment more hospitable for later arrivals. Secondary succession is faster because soil and a seed bank already exist after the disturbance; a burned forest or abandoned agricultural field is not starting from zero.

It is important to understand that pioneer species are not "trying" to be replaced — they simply engineer conditions that eventually favor competitors they cannot resist. As soil depth increases and nutrients accumulate, shrubs can establish. Shrubs shade out the lichens and mosses that cannot grow in low light. Later, trees shade out the shrubs. Each seral stage is outcompeted by the next — not because the pioneers were weak, but because they transformed the environment to favor different species.

The intermediate disturbance hypothesis adds a crucial wrinkle to this picture. It predicts that species diversity is not highest in undisturbed, "mature" communities — it peaks at intermediate disturbance frequencies. With no disturbance, competitive dominants gradually eliminate subordinate species (succession proceeds to a low-diversity dominant state). With very high disturbance, nothing can establish between events. At intermediate levels — periodic fires, storms, gap formation — the community is repeatedly reset in patches, preventing any single dominant from monopolizing all space and resources. This explains why some of the most diverse ecosystems on Earth (tropical forests, coral reefs, grasslands) are characterized by persistent, moderate disturbance.

Finally, abandon the idea that succession reliably ends at a stable "climax community." This concept was appealing in early ecology but has been revised substantially. Ecosystems exist in dynamic equilibrium, driven by ongoing disturbance. Many communities persist in alternative stable states — different species assemblages that are each self-maintaining under the same climate conditions. Which state a community ends up in depends partly on history: which species arrived first, which disturbances occurred, and what legacy effects persist from previous occupants. Succession describes a trajectory, not a guaranteed destination.

Practice Questions 3 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsTriple Integrals in Cartesian CoordinatesTriple Integrals in Cylindrical and Spherical CoordinatesChange of Variables and the Jacobian DeterminantApplications of Triple Integrals: Volume and MassVector Fields and Their RepresentationsLine Integrals of Vector FieldsGreen's TheoremSurface Integrals and Flux of Vector FieldsSurface Integrals and Flux of Vector FieldsDivergence Theorem: Flux and OutflowDivergence TheoremElectric FluxGauss's LawConductors in Electrostatic EquilibriumCapacitance and CapacitorsDielectricsDielectric Constant and Relative PermittivityElectric Field Inside Dielectric MaterialsDielectric Materials and PolarizationDielectric Susceptibility and PermittivityEnergy Density in Electric FieldsElectric Current and Current DensityElectrical Resistance and ResistivityOhm's Law and Circuit ElementsElectromotive Force (EMF) and BatteriesKirchhoff's Circuit Laws: Voltage and CurrentDC Circuit Network Analysis MethodsTransient Response in RC CircuitsRC CircuitsLC and RLC CircuitsAC Circuits: FundamentalsImpedance and ReactanceAC Power and ResonanceElectromagnetic WavesThe Electromagnetic SpectrumBlackbody Radiation and Planck's LawPhotoelectric EffectThe Photon: Light as QuantaCompton ScatteringWave-Particle Dualityde Broglie WavelengthHeisenberg Uncertainty PrincipleWavefunction and the Born RuleThe Schrödinger EquationState Vectors and WavefunctionsQuantum SuperpositionQuantum EntanglementBell Theorem and Bell InequalitiesPostulates of Quantum MechanicsScattering TheoryIntroduction to Scattering TheoryPartial Wave Analysis in ScatteringSpin Angular MomentumElectron Spin and Intrinsic Magnetic MomentStern-Gerlach Experiment: Spin Quantization and MeasurementElectron Diffraction and Matter Wave PropertiesDavisson-Germer Experiment: Crystal Diffraction of ElectronsElectron Diffraction and Matter Wave InterferenceWavefunctions and Probability Density InterpretationQuantum Superposition and Linear Combinations of StatesQuantum Operators and ObservablesCanonical Commutation Relations and UncertaintyHeisenberg Uncertainty Principle and Measurement LimitsTime-Independent Schrödinger Equation and EigenvaluesHydrogen Atom in Quantum MechanicsSpectral Lines and Energy TransitionsSelection Rules for Atomic TransitionsLS and jj Coupling Schemes in Multi-Electron AtomsPauli Exclusion Principle and Antisymmetric WavefunctionsElectron Configuration and the Aufbau PrincipleThe Periodic Table and Atomic Electronic StructureThe Periodic TableElectron ConfigurationPeriodic TrendsIonization EnergyIonic BondingLewis StructuresResonance Structures and Delocalized ElectronsResonance and Formal ChargeMolecular Polarity and Dipole MomentsIntermolecular ForcesStates of Matter and Phase Changes: Melting, Boiling, and SublimationGas Laws and the Ideal Gas EquationGas Stoichiometry and Volume-Volume CalculationsThermochemistry and EnthalpyHeat Capacity and CalorimetryEntropy and Molecular DisorderSpontaneity and ΔGEntropy and Gibbs Free EnergyChemical EquilibriumChemical KineticsRate Law DeterminationEnzyme KineticsCell Cycle Regulation and CheckpointsMitosisCytokinesisMeiosisChromosomal Theory of InheritanceMendelian GeneticsDominance, Recessiveness, and Allelic InteractionsSex-Linked InheritanceNon-Mendelian Inheritance PatternsPopulation Genetics and Hardy-Weinberg EquilibriumNatural SelectionAdaptation and FitnessLife History Strategies: r- and K-SelectionPredator-Prey Dynamics and the Lotka-Volterra ModelCommunity Ecology: Structure and OrganizationSpecies Interactions: Competition, Predation, Mutualism, and ParasitismEcological Succession

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