1 Ecosystem Ecology Energy Flows and Nutrient Cycles
2 Introduction to Ecosystems Some reflected Some converted to heat Some absorbed PSN Some absorbed by organisms, soils, water
3 Introduction to Ecosystems Plants use solar energy to synthesize sugars Plant growth Storage
4 Introduction to Ecosystems Forest is sunlight transformed Portion consumed by herbivores Consumed by detritivores Soil organic matter
5 Definition Forest can be viewed as a system Absorbs Transforms Stores Physical, chemical and biological structures and processes are inseparable -> Ecosystem = biological community plus all abiotic factors influencing the community
6 Definition Concept 1 st proposed in 1935 though the organism may claim primary interest we cannot separate them from their special environment with which they form on physical system Arthur Tansley ( )
7 Definition Ecosystems process matter and energy Distinctly different approach from individual, population, & community ecology mostly non-evolutionary more non-biological processes (chemistry, physics) Laws of physics determine a lot of what goes on in ecosystems
8 Definition Ecosystem Ecologists study flows of energy and nutrients Areas of interest include Primary Production Energy Flow Nutrient Cycling
9 Definition What Are the Energy Sources in Ecosystems? What Limits Primary Production? What Controls Energy Flow Through Consumers? How Does Energy Flow Structure Ecosystems?
10 Simple laws of physics Conservation of matter -- matter is neither created nor destroyed, only changed in form Conservation of energy -- energy is neither created nor destroyed, only changed in form Entropy -- Any transfer or change of energy cannot be 100% efficient. Some energy is degraded to lower quality, less useful energy (=heat)
11 Energy Ability to do work Kinetic -- energy now doing work Potential -- energy stored (e.g., in chemical bonds within living organisms) Consequence of entropy material moves spontaneously down a concentration gradient the reverse requires expenditure of energy Organisms move matter up concentration gradients by expending energy
12 Energy flows within ecosystems Energy moves one way within ecosystems No cycles Every transfer results in reduction in usable energy (production of some heat) Input is energy from nonliving sources, primarily the sun via photosynthesis
13 A Simple Food Chain: From the Plankton to the Largest Animal on Earth
15 Energy Sources in Ecosystems Autotrophs organisms that obtain energy from inorganic sources, such as by photosynthesis. Autotrophs are the ultimate biological source of energy for ecosystems. Primary production is the energy autotrophs acquire from the inorganic environment. Gross primary production (GPP) the total rate of energy capture by autotrophs. Net primary production (NPP) the total rate of energy capture by autotrophs minus energy lost in their respiration. Heterotrophs are organisms that obtain energy from organic compounds, generally from other organisms, living or dead. Secondary production the acquisition of energy by heterotrophs.
16 The Inorganic Sources of Energy Chemoautotrophs (eubacteria and archaea) derive energy from the oxidation of electron donors in the environment. E.g. hydrogen H 2, hydrogen sulfide (H 2 S), or methane (CH 4 ). Photoautotrophs derive energy from sunlight through photosynthesis.
17 Energy Flow Through Ecosystems
18 Energy Pyramid in Ecosystems
19 Energy Loss Along the Food Chain Affects Which Species Can Be Sustainably Harvested
20 Primary Production Net = Gross Respiration Amount of energy available to consumers in the ecosystem Measured by Rate of carbon uptake Amount of biomass O 2 produced
21 Global Patterns of Primary Production Terrestrial systems: high productivity - green; low productivity - red. Marine systems: high productivity - red, moderate productivity - yellow, low productivity - blue.
22 Primary Production Because rates vary from 1 ecosystem to another study factors that control rates Patterns of natural variation can provide clues to environmental factors that control the process
23 Rosenzweig 1968 estimated influence of moisture and temperature on rates Annual net primary productivity Annual actual evapotranspiration (AET) total amount of water that evaporates and transpires off of landscape during course of year.
24 What does this tell us? AET (temperature and precipitation) accounts for significant proportion of variation in annual net primary productivity But
25 Primary Productivity Rosenzweig attempts to explain variation in primary productivity across terrestrial ecosystems but what about within ecosystems?
26 Primary Productivity O.E. Sala Colorado State University explored factors controlling primary productivity in central grasslands of North America 9498 sites grouped into 100 representative study areas Mississppi/Arkansas New Mexico/Montana
27 Primary Productivity Highest in eastern grasslands lowest in west Corresponds to change from tallgrass to shortgrass prairie
28 Significant relationship with precipitation If temperature added no improvement in fit Why? Warm temperatures occur at all grasslands during the growing season.
29 mm shows production ranging from g/m 2 Why? Differences challenge ecologists for explanation
30 Primary Productivity Can it be explained by differences in soil fertility? N & P Do nutrients explain differences in rates of primary productivity? Experiments conducted to enhance nutrients
31 Primary Productivity Owensby et al. Journal of Range Management 23: Tallgrass prairie fertilization with N & P Large production responses with N 46% Not with P Why?
32 Primary Productivity Lack of response may be due to efficient mutualistic relationship with mycorrhizal fungi and plants Latter studies confirm findings Avg increase with N +68% ANPP, in burned sites but only +9% in burned sites NO3 availability higher in unburned sites
33 Primary Productivity Despite major influence of temperature and moisture on ANPP, variation in nutrient availability can also have measureable affect.
34 Primary Productivity Aquatic Systems Significant positive relationships with nutrient availability and primary productivity 1 st studies P & phytoplankton biomass Japanese lakes (1950 s 60 s) 1 0 Productivity P content
35 Primary Productivity Aquatic Systems Later similar relationship seen with lakes in Northern Hemisphere Slopes in both studies nearly identical! 1 0 Productivity P content Nutrients particularly P, control phytoplankton biomass
36 Primary Productivity Aquatic Systems Whole lake experiments NW Ontario, Canada 1968 Vinyl curtain divided lake into 8 ha basins C & N - C & N & P - Both sides responded to nutrient additions - Phytoplankton biomass reference lakes
38 Primary Productivity Aquatic Systems Freshwater systems P additions have a much larger effect Marine systems N additions have a much larger effect on hard bottom substrates (coral reefs, rocky intertidal, open ocean)
39 Trophic Cascades Chemical controls on 1 0 productivity = bottom up controls But consumers may also influence 1 0 productivity = top down controls
40 Trophic Cascades Carpenter, Kitchell and Hodgosn Bioscience 35: Althoght nutrients determine 1 0 productivity in lakes, piscivorous and planktivorous fish can cause significant deviations 1 0 Productivity Zooplankton size
41 Trophic Cascades Proposed influence of consumers on lake 1 0 productivity propagate through food web 1 0 Productivity Zooplankton size
42 Trophic Cascades Visualized effects of consumers coming from top of food web to base Trophic Cascade Hypothesis Similar to Keystone Species but Trophic Cascade model focused on effects of consumer on ecosystem processes and not on species diversity
43 Trophic Cascades 1. Piscivorous fish (LMB) feed on plankivorous fish & inverts 2. Because of their influence on planktivorous fish, LMB indirectly effect populations of zooplankton By reducing plankivorous fish, LMB reduce feeding pressure on zooplankton
44 Trophic Cascades 3. Large bodied zooplankton dominate zooplankton community 4. Dense population of zooplankton reduces phytoplankton biomass and rate of 1 0 productivity
48 Trophic Cascades Results 1. Reducing planktivorous fish 1 0 productivity - in absence of minnows, predaceous inverts fed heavily on smaller herbivorous zooplankton 2. Increasing plankivorous fish / reduce LMB 1 0 productivity Reproductive rates of LMB increased 50x Trophic activities of few species can have large effects on ecosystem processes
49 Trophic Cascades Majority tests of Trophic Cascades have been done in aquatic systems Strong 1992 Ecology 73: Are Trophic Cascades all Wet? - Most likely to occur in ecosystems with lower species diversity and reduced spatial and temporal complexity - Characteristic of many aquatic ecosystems
50 Trophic Cascades Some terrestrial systems consumers have been found to have significant effects Serengeti Grassland Ecosystem
51 Trophic Cascades Serengeti Mara 25,000 km 2 Grassland ecosystem 1.4 million Wildebeest 600,000 Thompson s Gazelle 200,000 Zebra 52,000 Buffalo 60,000 Topi 20 + additional grazing mammals
52 Trophic Cascades Grazers consume 66% of ANPP Potential for effect on ecosystem Complex interrelations of biotic and abiotic factors
53 Trophic Cascades Soil fertility and rainfall stimulate primary productivity and thus distribution of grazing mammals Grazing mammals affect Water balance Soil fertility Plant productivity
54 Trophic Cascades McNaughton positive relationship primary productivity and precipitation but grazing also increased primary productivity Plant growth rates increased - Compensatory Growth Lower rates of respiration (lower biomass) Reduced self-shading Improved water balance (reduced leaf surface area)
55 Trophic Cascades Serengeti now considered exceptional ecosystem but not always so
56 Trophic Cascades North American Grasslands was likely comparable. 60 million bison grazed grasslands up until middle of 19 th century. Research suggests they may have had similar affects on grasslands.
57 Energy Flow Energy is lost with each transfer between trophic levels Assimilation efficiency Respiration by consumers Heat production
58 Energy Flow Research at Lake Mendota, WI Demonstrated ~ 10% of available energy is transferred to next trophic level Rule of thumb This limits # of trophic levels within ecosystems!
59 Energy Flow Eventually there is insufficient energy to support viable populations
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Primary Production and Energy Flow Chapter 18 Sunlight to photosynthesizer to herbivore to carnivore to decomposer!!! 1 Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or
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