ME

Community Change & Stability

Succession: Change in Species Composition

  • Succession refers to the change in the species composition of communities over ecological time, typically ranging from 1 to 500 years.
  • Examples of species involved in succession include lichens, mosses, grasses, herbs, shrubs, tree seedlings, aspen, black spruce, jack pine, paper birch, balsam fir, and white spruce.
  • The process starts with a pioneer community and progresses toward a climax community over time.

Two Types of Succession

  • Primary Succession: Succession that occurs on land not previously occupied by vegetation. Example: recent volcanic deposits.
  • Secondary Succession: Succession that occurs following a disturbance of vegetated land. Example: regrowth of a forest after logging.

Stages of Succession

  • Sere: A recognized successional sequence.
  • Seral Stage: A particular phase (community) within a sere.
  • Pioneer Stage (Community): The earliest seral stage.
  • Climax: The final seral stage, representing the endpoint of succession.
  • Disclimax: A successional endpoint maintained by disturbance, such as fire-maintained pine forests.
  • Ecesis: Establishment phase.

Clementsian View of Succession

  • Nudation: The disturbance process that sets the stage for succession, including consideration of residuals (what remains after the disturbance).
  • Migration: The dispersal process involving initial colonists with significant dispersal capabilities. Early succession often involves wind-dispersed seeds, while later stages involve animal-dispersed seeds.
  • Ecesis: The establishment phase, where recruits must grow and reproduce under harsh and extreme initial conditions.
  • Reaction: Facilitation by organisms that change the environment, favoring different suites of migrants and residuals.
  • Competition: Includes all biotic interactions. Plant density increases, leading to greater resource competition and increased importance of other biotic interactions like herbivory and seed predation.
  • Stabilization: The climax stage is reached.

Traditional View of Succession

  • The traditional view of succession is linear, progressive, and predictable, with a single endpoint.
  • Succession starts with new land (primary succession) and progresses through pioneer and seral stages to a climax stage.
  • Disturbances at any stage can set back succession and initiate secondary succession.
  • Micro-cyclic succession involves small, non-cumulative changes.

Disturbance: The Starting Point

  • Disturbance is defined as an event that disrupts community structure and changes resource availability.
    • Disturbances can be natural or anthropogenic.
    • Disturbances vary in intensity, extent, and frequency, significantly influencing the speed and direction of succession.
  • Examples of disturbances include:
    • Blast damage to conifer forests around Mt. St. Helens.
    • Fire damage in lodgepole pine forests in Yellowstone National Park.
    • Hurricane Katrina.
    • Modern agriculture as human-managed succession.

Studying Succession

  • Plant ecologists study succession through:
    • Repeated sampling of the same site over time using permanent plots or repeat photographs, which is usually a very long process.
    • Analysis of chronosequences, studying communities of different ages and inferring successional changes.
  • Example: Primary Succession at Glacier Bay, Alaska
    • Demonstrates the progression from a pioneer stage with fireweed to a Dryas stage, an Alder stage, and finally a Spruce stage over time (1760-1941).

Secondary Succession Example

  • Forest Cleared in Southern Poland
    • Shows stages of regrowth after 7, 15, 30, 95, and 150 years.

Predictability of Succession

  • Succession on Lake Michigan Sand Dunes:
    • Henry C. Cowles (1901) studied diagrammatic profiles across Indiana sand dunes.
    • Stages include:
      • Pioneer Stage: Dune grasses stabilize the nutrient-poor, sandy substrate.
      • Early Successional Tree Stage: Fast-growing, short-lived trees such as cottonwoods.
      • Mid-Successional Pine Forest.
      • Late-Successional Hardwood Forest: Oaks transition to Beech-Maple (climax).

Dependence on Initial Conditions

  • The outcome of succession may depend on initial conditions.
  • Initial conditions include:
    • Damp depressions, upper beach, eroding surfaces, depositing crests, and steep lee slopes.
  • Physiographic processes include:
    • Foredune initiation and marram blowout initiation.
  • Pioneer vegetation includes:
    • Rush meadow, cottonwood, sand reed grasses, and shrubs.
  • Conifers (mostly temporary):
    • Jack and white pines, arbor vitae, and balsam fir.
  • Climax dominants:
    • Tallgrass prairie, red maple swamp, black oak, white oak, red and white maples, sugar and red beech hemlock, and birches (paper and yellow).

Secondary Succession in North Carolina Piedmont

  • Years after abandonment:
    • 0: Cropland.
    • 1: Crabgrass, horseweed.
    • 2: White aster, ragweed.
    • 5: Broomsedge.
    • 10: Broomsedge, pine seedlings.
    • 20: Young pines, Broomsedge.
    • 30: Shortleaf pine (drier sites) or Loblolly pine (moister sites).
    • 40: Shortleaf pine, hardwood understory or Loblolly pine, hardwood understory.
    • 60: White oak, post oak, hickory, dogwood, etc. or White oak, many hickories, dogwood, sourwood, etc.

Species Replacement

  • Species and communities replace one another due to:
    • Changes in resource availability and abiotic environment during succession.

Resource and Abiotic Environment Changes

  • Examples:
    • Percentage of soil moisture changes with dune age, r^2 = 0.943
    • Total soil C (Mg/ha) changes with dune age, r^2 = 0.921
    • Proportion of full sunlight decreases with dune age.
    • Total soil N (Mg/ha) changes with dune age, r^2 = 0.906

Adaptations

  • Early and late successional plants are adapted to different light and soil environments.
  • Differences in tolerances, resource requirements, and life-history strategies lead to species replacement.

Ecosystem Trends During Succession

TraitEarly StagesLate Stages
BiomassSmallLarge
PhysiognomySimpleComplex
Leaf orientationMonolayeredMultilayered
Major site of nutrient storageSoilBiomass
Role of detritusMinorImportant
Mineral cyclesOpen (leaky), rapid transferClosed (tight), slow transfer
Net primary production (NPP)HighLow
Site qualityExtremeMesic
Importance of the macroenvironmentGreatModerated and dampened; less
StabilityLowHigh
Plant species diversityLowHigh
Species life-history characterrK
Propagule dispersal vectorWindAnimals
Propagule longevityLongShort

Community Stability

  • Stability refers to whether some communities are more stable than others when facing disturbance or stress.
  • Stability can mean:
    • Resistance: The ability of a community to remain unchanged during stress.
    • Resilience: The ability of a community to return to normal following disturbance.

Vegetation Change in Southern Texas

  • Pre-settlement (ca. 150 years ago): Open grassland/savanna.
  • Today: Dense, thorn woodland dominated by Mesquite and shrubs due to overgrazing and lack of fire.

Development of Woody Plant Clusters

  • Shows the development of woody plant clusters in southern Texas grasslands over time (10-15 years, 30-40 years, 50-60 years).
  • Dominant species include Prosopis, Zanthoxylum, Celtis, Condalia, Opuntia, Diospyros, Ziziphus, and Schaefferia.

Succession Pattern

  • Hypothesized pattern of succession from grassland to savanna to woodland involving cluster expansion and coalescence.

Conceptual Model

  • Conceptual model of changes in community structure as a function of grazing pressure and fire.

Multiple Stable States

  • Multiple stable states are possible, represented by gravitational potential.

Diversity and Stability

  • The relationship of whether diverse communities are more stable and better able to resist disturbance.
  • Plant biomass in prairie plots experiencing drought is related to plant species diversity (Dave Tilman, 1996).