ASKiIMAN™ ARCHIVE / ENVIRONMENTAL ECOLOGY
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WORLD A — ECOLOGY FOUNDATIONS · REALM 11

Ecological Succession

30 Ontological Micro-Realms · Primary/Secondary, Autogenic/Allogenic & Xerarch/Hydrarch Pathways

PRIMARY (PRISERE) ↔ SECONDARY (SUBSERE) → AUTOGENIC VS ALLOGENIC → PROGRESSIVE VS RETROGRESSIVE → XERARCH & HYDRARCH → MESIC CLIMAX

The 30 Ontological Nodes of Realm 11

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NODE 11.01

Ecological Succession

  • Ragnar Hult 1885-term
  • Directional community replacement
  • Cowles and Clements-theory
  • Predictable temporal development
NODE 11.02

Sere & Seral Communities

PIONEER→SERAL→CLIMAX
  • Sere: entire developmental-sequence
  • Pioneer initial colonizers
  • Seral transitional communities
  • Climax terminal equilibrium
NODE 11.03

Primary Succession (Prisere)

  • Starts on sterile-substrate
  • Zero pre-existing soil
  • Zero organic seed-bank
  • Requires centuries-to-millennia
NODE 11.04

Primary Bare Substrates

  • Cooled volcanic lava-basalt
  • Surtsey Krakatoa islands
  • Retreating glacial moraines
  • Newly formed sand-dunes
NODE 11.05

Secondary Succession (Subsere)

  • Follows community disturbance
  • Intact mature soil-profile
  • Surviving seed-spore bank
  • Rapid 50–200-year recovery
NODE 11.06

Post-Fire & Old-Field Subsere

  • Abandoned agricultural farmland
  • Post-wildfire forest regrowth
  • Windthrow storm gaps
  • Root-crown resprouting acceleration
NODE 11.07

Primary vs Secondary

1000 YRSVS100 YRS
  • Nudation complete vs-partial
  • Lichen pioneers vs-annual-weeds
  • Pedogenesis required vs-humus-present
  • Slow versus fast-velocity
NODE 11.08

Autogenic Succession

  • Self-driven biotic replacement
  • Organisms alter own-habitat
  • Litter humus accumulation
  • Canopy shading self-replacement
NODE 11.09

Allogenic Succession

  • Externally driven abiotic-shift
  • Geophysical climate forcing
  • River siltation deposition
  • Sea-level coastal changes
NODE 11.10

Autogenic vs Allogenic

INTERNAL⇄EXTERNAL
  • Arthur Tansley 1935-distinction
  • Biotic reaction vs-abiotic-forcing
  • Predictable vs episodic-shifts
  • Coupled real-world interplay
NODE 11.11

Progressive Succession

  • Forward complexity ascent
  • Increasing total biomass
  • Taller canopy stratification
  • Rising species diversity
NODE 11.12

Retrogressive Succession

  • Backward degenerative reversal
  • Forest-to-scrub-to-barren
  • Driven by chronic-overgrazing
  • Acid rain soil-exhaustion
NODE 11.13

Deflected Succession

  • Arrested by recurring-disturbance
  • Maintained plagioclimax state
  • Mowing grazing burning-regimes
  • Managed anthropogenic grasslands
NODE 11.14

Autotrophic Succession

P / R > 1 → 1
  • Dominated by green-plants
  • Starts in inorganic-environment
  • Gross Production exceeds-Respiration
  • Organic matter accumulates
NODE 11.15

Heterotrophic Succession

R > P · DECAY
  • Dominated by fungi-bacteria-detritivores
  • Starts on organic-detritus
  • Respiration exceeds Production
  • Depletes substrate to-zero
NODE 11.16

Microsere (Serule)

  • Miniature microhabitat succession
  • Dead fallen tree-trunks
  • Animal carrion decomposition-waves
  • Dung-pat coprophilous fungi
NODE 11.17

Cyclic Succession

↺ LOOP
  • Alex Watt 1947-model
  • Pioneer-building-mature-degenerate
  • Heather Calluna moorland-cycle
  • Non-directional internal regeneration
NODE 11.18

Induced Succession

  • Human-engineered crop communities
  • Agricultural weed inhibition
  • Reverts upon abandonment
  • Managed silvicultural plantations
NODE 11.19

Xerarch Succession (Xerosere)

XERIC DRY→MESIC
  • Initiated in dry-habitats
  • Extreme water deficiency
  • Progressive moisture retention
  • Subdivided by substrate-type
NODE 11.20

Lithosere: 6 Rock Stages

  • Crustose-foliose lichen stages
  • Moss bryophyte mat-stage
  • Annual-perennial herb stage
  • Shrub to climax-forest
NODE 11.21

Lichen Rock Weathering

  • Rhizocarpon Parmelia pioneers
  • Carbonic lichenic acid-secretion
  • Chelation mineral dissolution
  • Traps wind-blown dust-humus
NODE 11.22

Psammosere: Sand Dunes

  • Shifting quartz sand-substrate
  • Ammophila marram-grass binding
  • Embryo fore-yellow-grey dunes
  • Cowles Lake Michigan-dunes
NODE 11.23

Halosere: Salt Marshes

  • Saline intertidal mudflats
  • Salicornia glasswort pioneers
  • Spartina cordgrass sediment-trapping
  • Elevates land desalinates-soil
NODE 11.24

Oxylosere & Epilithic Seres

SPHAGNUM pH<4
  • Oxylosere acidic peat-bogs
  • Sphagnum cation-exchange acidification
  • Chasmosere rock-crevice succession
  • Gypsosere gypsum-crust succession
NODE 11.25

Hydrarch Succession (Hydrosere)

AQUATIC→MESIC
  • Initiated in freshwater-ponds
  • Progressive siltation shallowing
  • Organic peat-muck buildup
  • Aquatic-to-terrestrial conversion
NODE 11.26

Early Hydrosere Stages (1–3)

  • 1. Phytoplankton pioneer-stage
  • 2. Rooted submerged (Hydrilla-Vallisneria)
  • 3. Rooted floating (Nymphaea-Nelumbo)
  • Free-floating Azolla Lemna-mats
NODE 11.27

Late Hydrosere Stages (4–7)

  • 4. Reed-swamp emergent (Typha-Phragmites)
  • 5. Sedge-meadow marsh (Carex-Juncus)
  • 6. Woodland shrub-stage (Salix-Alnus)
  • 7. Mesophytic climax-forest
NODE 11.28

Mesarch Climax Convergence

XERO →MESIC← HYDRO
  • Dry becomes wetter
  • Wet becomes drier
  • Both converge on-mesic
  • Equifinality climatic convergence
NODE 11.29

Odum's Bioenergetic Trends

P/R→1 · B/P↑
  • E.P. Odum 1969-table
  • Linear-grazing to detritus-webs
  • Open to closed-nutrient-cycles
  • r-strategists to K-strategists
NODE 11.30

Chronosequence Method

  • Space-for-time substitution
  • Glacier Bay Alaska-moraines
  • Hawaii lava-flow ages
  • Palynological sediment cores

Core Ontological Distinctions

1. Primary Succession (Prisere) vs. Secondary Succession (Subsere)

Primary Succession starts on a completely sterile, lifeless substrate with zero soil and zero seeds (cooled lava, bare rock, glacial retreat), requiring hundreds to thousands of years to build soil via pioneer lichens/mosses. Secondary Succession starts after a disturbance (fire, logging, abandoned farmland) where well-developed soil, humus, and a subterranean seed bank already exist, reaching climax much faster (50–200 years).

2. Autogenic vs. Allogenic Succession

Autogenic Succession is driven from within by the living organisms themselves modifying their own environment (adding humus, altering soil pH, casting shade). Allogenic Succession is driven from outside by external geophysical or climatic forces (siltation from a river catchment, volcanic ash, climate shifts).

3. Xerarch vs. Hydrarch Convergence

Xerarch Succession (Xerosere) begins in extremely dry conditions (bare rock Lithosere or sand Psammosere) and progressively retains more moisture. Hydrarch Succession (Hydrosere) begins in open water and progressively fills in with sediment and peat. Remarkably, both opposite pathways converge toward the exact same medium-moisture Mesic (Mesarch) Climax Forest.

Archival Progression · [011 / 266]

Realm 11 Complete

All 30 nodes of **Realm 11: Ecological Succession** (`11.01` to `11.30`) are forged. Next is the final realm of **World A**: **Realm 12: Succession Process & Climax** (`[012 / 266]`).