Patterns of Succession
Succession is: Non-seasonal, directional change in plant species living in a particular place through time. Involves: Colonization Establishment Ultimate local extinction Initiated by a disturbance that opens up space and resources
Types of Succession Primary: Occurs when new bare rock is generated by geologic activity (no organic material) Mt. St. Helens, Krakatoa, glacial retreat Secondary: vegetation invades areas that have been previously occupied, but has been removed due to disturbance (fire, agriculture, etc)
Primary Succession after glacial retreat Example of primary succession: lichensmoss small forbsshrubstrees
Lichens and moss growing on rock (primary succession)
Secondary Succession
Secondary Succession in YNP after 1988 fires
Classic Study: Billings (1938) Studied succession from old field to oak forest (150 years) Annual plants = pioneer species Biennial plants, grasses Perennial plants, shrubs After about 15 years: softwood trees After about 50 years hardwood trees, primarily oak
“Old-field Succession”
Successional Progression Annuals: Pioneer Species Tolerate low nutrient soils, need high light Good dispersers Grow rapidly, short life span (1 year) Produce many offspring Biennial plants, grasses Share attributes with pioneer species, but longer lived, grow more slowly Perennials and shrubs Slower growing, longer lived Can reproduce asexually as well as sexually Better competitors
Softwood trees (Pines) Slow growing Eventually produce canopy Shade out light-loving shrubs and perennials in understory Also shades out new baby pines Hardwood trees (Oaks and hickory) Longer lived Better competitors Eventually dominated forest as softwood trees died. Oak forest in this case = climax community
Climax Communities Final successional stage: self-replacing, persistant over very long periods of time Idea of climax community controversial these days because of recognition of role of disturbance Shifting mosaic steady state model: Majority of patches in habitat in some stage of recovering from disturbance Landscape is in a steady-state because roughly constant portions of landscape are in each stage of succession Thus there is a dynamic equilibrium across the landscape
Disturbance Specialists: Often Weeds
Mechanisms of Succession Connell and Slayter, 1977 1. Facilitation - Changes in abiotic conditions are caused by the plants currently occupying an area - These changes favor new invaders over the current occupants (current occupants pave the way for future occupants) Examples: Lichens make soil, nitrogen-fixing plants enrich soil, nurse plants support others
2. Tolerance Plants in different stages of succession don’t have much impact on each other Position in the scheme of succession depends on their different life histories Example: Old field Succession
3. Inhibition Members of one stage of succession resist invasion of later stages Succession proceeds when one stage dies Example: Allelopathy
Succession and Chemical Cycling Biomass, production, diversity and chemical cycling change during succession Biomass and diversity peak in mid-succession, increasing at first to a maximum, then declining and varying over time.
K-selection and r-selection Pioneer species generally have particular set of characteristics - all together these are called r-selected traits Climax species generally have different set - represent a different life history strategy
Succession and Plant Diversity
Succession and Diversity
Just focusing on woody plants:
Corresponding changes in animal species
Succession in the Intertidal
Diversity through Succession in Intertidal
Succession in Streams
Points to Consider: Change through time is a natural characteristic of most ecosystems - when thinking about conservation need to incorporate understanding of natural disturbance regimes Mosaic of Patches in different stages of succession maximizes habitat heterogeneity and thus diversity
Ecological Restoration Attempt to return impacted land to natural state What exactly should be returned? Increasingly are trying to replace the original disturbance regime so that succession can occur naturally Need to restore disturbance and succession processes both temporally and spatially What area of land is big enough to encompass these processes?
Stream Restoration What ecosystem functions/services need to be restored? Habitat Conduit Barrier Filter Source Sink
Processes need to be restored, not just individual components Hydrologic functions: How much flow, how deep, timing Geomorphological functions Stream profile, sedimentation patterns, erosion Physical and Chemical Properties of Water Toxins? Nutrients PH Biological Processes (eg large woody debris, habitat structure, heterogeneity in stream) Role of Disturbance/Dynamic Equilibrium