prof. dr. yingzhi gao northeast normal university phone:13664319768 email:gaoyz108@nenu
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Prof. Dr. Yingzhi Gao Northeast Normal University Phone:13664319768 Email:[email protected]. Introduction to Ecosystem Ecology. Principles of Terrestrial Ecosystem Ecology by F. Stuart Chapin III Pamela A. Matson Harold A. Mooney. Textbook:. Course Goals. - PowerPoint PPT PresentationTRANSCRIPT
Prof. Dr. Yingzhi Gao
Northeast Normal University
Phone:13664319768
Email:[email protected]
Introduction to Ecosystem Ecology
Textbook:
• Principles of Terrestrial Ecosystem Ecology
by F. Stuart Chapin III
Pamela A. Matson
Harold A. Mooney
Course Goals
•Understand basic principles Interaction, scale, process, pools and fluxes, trophic,Integration , regulation and management•Get you involved
–Participate!!!
Why should we care about ecosystem ecology?
• Ecosystem ecology provides a mechanistic basis for understanding the Earth System
• Ecosystems provide goods and services to society
• Human activities are changing ecosystems (and therefore the Earth System)
Complex: human activity influence
• Study of interactions among organisms and their physical environment as an integrated system
What is Ecosystem Ecology?
What is an ecosystem?
• bounded ecological system consisting of all the organisms in an area and the physical environment with which they interact– Biotic and abiotic processes– Pools and fluxes
Living aboveground phytomass
Living belowground phytomass
Mineral nutrients in soil solution
Uptake
ExudationWashout
Uptake for shoot production
Retranslocation
Humus
Humification
Immobilization
Standing dead
Litter
Mineralization
Decomposition
Animals
Excreta (Urine)
Degistation
Excreta
(Dung)
Mineralization
Dead belowground phytomass
Decompo-
sition
internal internal nutrient cyclingnutrient cycling
System input:
- wet and dry deposition- N2-fixation- fertilization- water inflow
System definition nutrient cycling
System output:
- water outflow- wind erosion - losses to air (denitrification)- fire (burning dung)- haymaking - animal products (meat, wool,...)
Nitrogen fluxes and pools 2004 and 2005 (g/m²)
Living roots
Dead roots
Living shoot
Plant available
N
Soil Humus N (0-20 cm)
Decomposition
Standing dead and litter
Export
N-uptake
Sheep uptake
Root N-uptake
TO
0.05T79
0.6
T79
5 - 9TO
3 - 5
Living roots
Dead roots
Living shoot
Standing dead and litter
N-uptake
TO
0.23 - 0.26 T79
2.8 - 2.9
TO
1.4 - 2.3T79
2.2 - 3.1
TO
16.7T79
25.4
TO
4.5T79
8.3
TO
1.4 - 2.3T79
2.2 - 3.1
TO
0.6
TO
0.1
TO
0.4TO
1,0
TO
5T79
7
TO
330T79
400
Sheep
Decomposition
Ecosystem Structure: Trophic relations
• Trophic relationships determine an ecosystem’s routes of energy flow and chemical cycling
• Trophic structure refers to the feeding relations among organisms in an ecosystem
• Trophic level refers to how organisms fit in based on their main source of nutrition, including
Trophic levels• Primary producers: autotrophs (plants, algae, man
y bacteria, phytoplankton),• Primary consumers: heterotrophs that feed on auto
trophs (herbivores, zooplankton);• Secondary consumers heterotrophs that feed on pri
mary consumers;• Tertiary consumers (quatenary consumers);• Detritivores (organisms that feed on decaying orga
nic matter, bacteria, fungi, and soil fauna)• Omnivores (feed on everything), frugivore, fungiv
ore…….
Other Definitions
• An ecosystem is a bounded ecological system that includes all the organisms and abiotic pools with which they interact.
• An ecosystems is the sum of all of the biological and nonbiological parts that interact to cause plants grow and decay, soil or sediments to form, and the chemistry of water to change.
Ecosystem Ecology
• The study of the movement of energy and materials, including water, chemicals, nutrients, and pollutants, into, out of, and within ecosystems.
• The study of the interactions among organisms and their environment as an integrated systems.
Example 1
• Small scale: e.g., soil core, appropriate for studying microbial interactions with the soil environment, microbial nutrient transformations, trace gas fluxes,…
Example 2
• Stand: an area of sufficient homogeneity with regard to vegetation, soils, topography, microclimate, and past disturbance history to be treated as a single unit.
Appropriate for studying whole-ecosystem gas exchange, net primary productivity, plant-soil-microbial nutrient and carbon fluxes
Example 3
• Natural boundaries: sometimes, ecosystems are bounded by naturally-delineated borders (lawn, crop field, lake).
Appropriate questions include whole-lake trophic dynamics and energy fluxes (e.g. Lindeman)
Example 4
• Watershed: a stream and all the terrestrial surface that drains into it.
Watershed studies use stream as “sample device”, recording surface exports of water, nutrients, carbon, pollutants, etc., from the watershed.
Temporal Scale
• Instantaneous
Temporal Scale
• Instantaneous
• Seasonal
Temporal Scale
• Instantaneous
• Seasonal
• Succession
Temporal Scale
• Instantaneous
• Seasonal
• Succession
• Species migration
Temporal Scale
• Instantaneous
• Seasonal
• Succession
• Species migration
• Evolutionary history
Temporal Scale
• Instantaneous
• Seasonal
• Succession
• Species migration
• Evolutionary history
• Geologic history
General approaches
• Systems approach– Top-down approach
General approaches
• Systems approach– Top-down approach
• Comparative approach– Bottom-up approach– Based on processes
Historical roots
• Community ecology– Elton – Clements
• Geography– Warming, Schimper, Walter
• Soils– Jenny
Systems Approach
• Lindeman: Trophic dynamics
• Odum: Energy and nutrient flows
• Margalef: Information transfer
• O’Neill: Hierarchy theory
• Holling: Resistance and resilience
Process Approach
• Jenny: State factors
• Billings, Mooney: Ecophysiology
Tansley, British plant ecoslogist
• The use and abuse of vegetational concepts and terms. Ecology 16: 284-307
• First to coin term, “ecosystem”
• Emphasized interactions between biotic and abiotic factors
• Argued against exclusive focus on organisms
Hans Jenny, Soil scientist
• Factors of soil formation, 5 state factors that constrain soil and ecosystem development
• Soil = function of Climate, organisms, parent material, relief (topography) and time, or s=f(clorpt)
• Many patterns of soil and ecosystem properties correlate with state factors (climate and vegetation structure and function)
Ramond Lindeman
• Qualified pools and fluxes of energy in a lake ecosystem emphasizing biotic and abiotic components and exchange
• Fluxes of energy, critical “currency” in ecosystem ecology, basis for comparison among ecosystems
• Synthesized with mathematical model• Coupling of energy flow with nutrient cycling
J. D. Ovington, English forester
• Central question, how much water and nutrients are needed to produce a given amount of wood?
• Constructed ecosystem budgets for nutrients, water, and biomass
• Also included inputs and outputs: exports of logs involves exports of nutrients (thus inputs of nutrients required to maintain productivity
• One of the first to state the need for more basic understanding of ecosystem function for managing natural resources
H. T. Odum and E. P. Odum
• Used radioactive tracers to study movement of energy and materials through a coral reef, documenting patterns of whole system metabolism
• System analysis- ecosystem as a life-support system concept
Earth System and Global Change
• Making history in ecosystem ecology• Impact of human activities on Earth has led to the
need to understand how ecosystem processes affect the atmosphere and oceans
• Large spatial scale, requiring new tools in ecosystem ecology (fluxes tower measurements of gas exchange over large regions, remote sensing from satellites,global networks of atmospheric sampling, global models of ecosystem metabolism).
Frontiers in ecosystem ecology
• Integrating systems analysis, process understanding, and global analysis
• How do changes in the environment alter the controls over ecosystem processes? What are the integrated consequences of these changes? How do these changes in ecosystem properties influence the Earth system?
• Rapid human-induced changes occurring in ecosystems have blurred any previous distinction between basic research and management application
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