Ecological Succession Notes

Chapter VII. Ecological Succession

A. Types of Succession (based on Origin)

  • Primary Succession:
    • The process of creating life in an area where no life previously existed.
    • A step-by-step invasion of animals and plants in a bare area until it becomes a climax community.
    • Begins in a place without any soil, such as:
      • Sides of volcanoes
      • Landslides
      • Flooded areas
    • Starts with the arrival of pioneer species that do not need soil to survive (e.g., lichens).
    • Overview of Primary Succession:
      • Bare rock is colonized by pioneer species (e.g., moss).
      • Decomposition creates a layer of topsoil.
      • Grasses grow and displace the pioneer species.
      • More nutrients in the soil allow for shrub growth.
      • Increase in soil depth allows for the growth of trees.
    • When lichens die, they decompose, adding a small amount of organic matter to the rock or soil, allowing mosses and ferns to grow on the new soil.
    • When mosses and ferns die, they add more organic material to the soil, thickening the soil layer, which allows grasses and other plants to take over.
    • When grasses and other annuals die, they add more nutrients to the soil, enabling shrubs and trees to survive.
    • Insects, small birds, and mammals begin to move in.
    • Types of Primary Succession (based on substrate):
      • Hydrarch: Starts on a wet substrate.
        • Hydrosere: Stages of Hydrarch Succession
          • (1) Newly formed water body
          • (2) Phytoplankton Stage
          • (3) Rooted Submerged Stage
          • (4) Rooted Floating Stage
          • (5) Reed-Swamp Stage
          • (6) Sedge Marsh or Meadow Stage
          • (7) Woodland Stage
          • (8) Forest Stage
      • Xerarch: Starts on a dry surface, like an exposed rock.
        • Stages of Xerarch Succession:
          • Bare rock
          • Lichens
          • Small annuals
          • Perennial plants, lichens, herbs, grasses
          • Grasses, shrubs, shade-intolerant trees
          • Shade-tolerant trees
          • Intermediate stages
          • Climax community
    • Example: During primary succession on lava in Maui, Hawaii, succulent plants are pioneer species.
  • Secondary Succession:
    • The process of re-stabilization that follows a disturbance in an area where life has previously existed.
    • Occurs in an area or gap disturbed (by fire, typhoon, flood, and other natural or human disturbances) and previously vegetated.
    • Stages of Secondary Succession:
      • Pioneer Species: Annual plants (0 years)
      • Intermediate Species: Grasses and perennials (1-2 years), Grasses, shrubs, pines, young oak and hickory (3-4 years)
      • Climax Community: Mature oak and hickory forest (150+ years)

B. Other Types of Succession

  • Cyclic:
    • When climax plant communities absorb random occurrences of gaps triggered by the fall of dead old trees, landslips, lightning strikes, etc.
    • The situation recruits light-demanding plant species that would again close the gap.
    • Never attains climax.
  • Directional:
    • Linear, step-by-step invasion of plant species until a climax community is reached.
    • Sere.
  • Autogenic:
    • Refers to the influence of resident plant communities (indigenous) on the limiting factors (light regime, litter, temperature oscillations, increased humidity, change in soil substrate, etc.).
    • Resident plants define the set of recruits for the next seral plant community that would emerge.
  • Allogenic:
    • Succession caused by major environmental changes beyond the control of the indigenous organisms.
    • Examples include climate change, changes in sea level or topography, and bioinvasive alien species.
  • Progressive:
    • Succession often leads to communities with greater complexity and progressively becoming more mesic (moist).
    • Example: Sierra Madre Mountain Ranges and other Tropical Rainforests (TRFs)
    • Pioneer trees -> secondary forest -> climax forest
  • Retrogressive:
    • Opposite direction toward simpler, more depauperate communities and toward a more hydric (wet) or a more xeric (dry) habitat.
    • Some retrogressive successions are allogenic (e.g., logging, introduction of cattle, weedy annuals, and fire).

Ecological Succession

  • Ecological succession is the change in species composition of an ecosystem.
  • It is a series of progressive changes in the species that make up a community over time.
  • Plant succession is a directional, cumulative change in the species that occupy a given area.
  • Time involved: 1-500 years.

Seral Community

  • A step-by-step invasion of animals and plants in a bare area until it becomes a climax community.
  • Types of Seres:
    • Hydrosere: Succession in an aquatic habitat.
    • Xerosere: Succession in a dry habitat.
    • Lithosere: Succession on a bare rock surface.
    • Psammosere: Succession initiating on sandy areas.
    • Halosere: Succession starting in saline soil or water.
    • Senile: Succession of microorganisms on dead matter.
    • Eosere: Development of vegetation in an era.
  • A seral community is an intermediate stage of ecological succession advancing towards the climax community.
  • It is replaced by the subsequent community.
  • It consists of simple food webs and food chains.
  • It exhibits a very low degree of diversity.
  • The individuals are less in number, and the nutrients are also less.

Climax Community

  • Remains the same throughout time if not disturbed.
  • Vegetation has fully developed.
  • Received the maximum number of species.
  • Has filled all available niches.
  • State of equilibrium.
  • A climax community is not limited to a tree community but can be cacti in deserts or grasses in fields.

Disclimax

  • When succession is not allowed to develop due to many destabilizing factors.
  • Naturally driven by external perturbations:
    • Recurrent landslides, unpredictable dry conditions, fire.
  • Anthropogenic factors:
    • Farming (e.g., savanna grassland of Carranglan, Nueva Ecija).

Formation of Gaps in the Forest

  • Chablis:
    • Creation of opening or gap mainly by the fall of trees.
    • Small but the most largely occurring creator of forest gaps.
    • Domino effect (fungal attack, then soon die and fall).
    • From medieval French, means fallen tree, its rests and caused light gap; vertical and horizontal projection.
  • Windthrow: Hastened due to typhoon.
  • Faults and Landslips:
    • Geologically unstable areas (slopes) + earthquake + rain.
    • Example: Digdig, Carranglan, Nueva Ecija, after the 1990 Earthquake; Landslide caused by typhoon Pablo in 2012.
  • Volcanic Eruption: Large gaps.
    • Krakatau island in Indonesia in 1883 (completely burned to ashes) ~ recovered 34 years later.
    • Mount Pinatubo eruption (start another cycle of succession).
  • Fire:
    • Regular and highly seasonal (i.e., savanna and steppes).
    • Lightning ignites dry grass and then spreads.
    • Kalimantan, Indonesia (El Nino phenomenon burned a considerable extent of TRF in Borneo).
  • Anthropogenic Gaps: Worst cause of gaps!
    • Logging
    • Kaingin (slash-and-burn farming)
    • Road construction
    • Accidental fires (El Nino + accidental spread of fire).

Succession Process

  1. Nudation: The exposure of a new surface in a primary succession or the clearing away of previous vegetation in secondary succession.
  2. Migration: Of seeds, spores, or vegetative propagules from adjacent areas, though in secondary succession, many of these are already present in the soil (also animals).
  3. Ecesis: The germination, early growth, and establishment of plants.
  4. Competition: Among the established plants.
  5. Reaction: The autogenic effects of plants on the habitat.
  6. Stabilization: The climax.

Threats to Succession

  • The grasses that move in as pioneer species are often thought of as weeds.
  • The subsequent growth of shrubs is considered undesirable “brush”.

Does Ecological Succession Ever Stop?

  • Over a long period, the climate conditions of an ecosystem are bound to change.
  • No ecosystem has existed or will remain unchanged over a Geological Time Scale.

Schrödinger Ratio and Succession

  • CO<em>2O</em>2<1\frac{CO<em>2}{O</em>2} < 1 or CO<em>2O</em>2>1\frac{CO<em>2}{O</em>2} > 1
  • CO<em>2O</em>2=1\frac{CO<em>2}{O</em>2} = 1 and O<em>2>CO</em>2O<em>2 > CO</em>2
  • O2 emission: measures the rate of photosynthesis: GPP
  • CO2 emission: measure of CRs or (Rs)
  • 1st law of Thermodynamics: GPP=CSB+CRsGPP = CSB + CRs
  • 2nd law of Thermodynamics: CSB=GPPCRsCSB = GPP – CRs
  • THEREFORE,
    • If O<em>2>CO</em>2O<em>2 > CO</em>2, Biomass accumulates (E is > 1)
    • If O<em>2=CO</em>2O<em>2 = CO</em>2, New biomass is just enough to replace dead biomass (E is = 1)

Virgin Forest – Gaps, Building and Mature Phases Succession Cycle

GAPBUILDING-UPMATURE
Ecological succession at the local levelPioneer speciesClimax species
Chablis, lightning, landslips
CO<em>2O</em>2=1\frac{CO<em>2}{O</em>2} = 1 Because O<em>2=CO</em>2O<em>2 = CO</em>2\frac{CO2}{O2} < 1 Because O<em>2>CO</em>2O<em>2 > CO</em>2\frac{CO2}{O2} < 1 O2O_2 (Production) denotes community biomass buildup
CO<em>2O</em>2=1\frac{CO<em>2}{O</em>2} = 1CO2(Decomposition) denotes community biomass biodegration
  • Respiration increases with increasing age of ecosystem development. More CO2CO_2 is interpreted as a means to pump out disorder (or Entropy) and maintain ecosystem integrity/stability while there is no more growth. Production is for maintenance.

Summary

FeaturePrimary SuccessionSecondary Succession
Starting PointBegins with no lifeFollows removal of existing biota
Soil ConditionNo soil presentSoil already present
Initial EnvironmentNew area (e.g., volcanic island)Old area (e.g., following a bush fire)
Pioneer SpeciesLichen and moss come firstSeeds and roots already present
BiomassBiomass is lowBiomass is higher