Ecosystems and Biomes Review
Ecosystems
1.1 Ecosystems Overview
Definition of an ecosystem: A system composed of living organisms interacting with each other and their physical environment (e.g., soil, air, water).
1.2 Learning Objectives/EK/Skills
Learning Objective
ERT-1.A: Explain how the availability of resources influences species interactions.
Suggested Skill
1.A: Concept Explanation: Describe environmental concepts and processes.
Essential Knowledge
ERT-1.A.1: In a predator-prey relationship, the predator consumes the prey, affecting the population dynamics and behavior of both species.
ERT-1.A.2: Symbiosis refers to long-term interactions between two species. Types include:
Mutualism: Both species benefit (e.g., bees and flowers).
Commensalism: One species benefits, the other is not significantly affected (e.g., birds nesting in trees).
Parasitism: One species benefits at the expense of the other (e.g., tapeworms in mammals).
ERT-1.A.3: Competition arises when species vie for limited resources, which may occur intra-specifically (within a species) or inter-specifically (between species). Resource partitioning, wherein species utilize the same resource differently (e.g., in time, place, or manner), can help mitigate competition.
1.3 Ecosystem Basics
Individual: A single organism (e.g., one elk).
Population: A group of individuals of the same species (e.g., an elk herd).
Community: All living organisms in a specific area.
Ecosystem: The sum of living and nonliving components in an area (including flora, fauna, rocks, soil, water, air).
Biome: A larger ecosystem type characterized by specific climate conditions influencing seed and animal species (e.g., tropical rainforest).
1.4 Organism Interactions
Types of Organism Interactions:
Mutualism: Both organisms benefit (e.g., coral reefs).
Competition: Organisms compete for resources, limiting the population size.
Predation: One organism consumes another for energy (e.g., leopards preying on giraffes).
Commensalism: One organism benefits without impacting the other (e.g., birds nesting in trees).
1.5 Predation
Predation Relationship: Identified as (+/-). Examples:
True Predators: Carnivores that kill prey for energy (e.g., leopard and giraffe).
Herbivores: Consume plants for energy (e.g., giraffe and trees).
Parasites: Derive energy from a host, often without killing the host (e.g., mosquitoes).
Parasitoids: Lay eggs in a host; larvae consume host from inside (e.g., parasitic wasps).
1.6 Symbiosis Explained
Symbiosis: Derived from the roots "sym" (together) and "bio" (life), indicating close living arrangements.
Types of symbiotic relationships:
Mutualism (+/+)
Commensalism (+/0)
Parasitism (+/-)
Example of mutualism: Coral providing structure for algae; algae providing sugars for coral energy.
Example of lichen: A mutualistic relationship between fungi and algae, where each organism benefits nutritionally.
1.7 Competition and Resource Partitioning
Resource partitioning aids in minimizing competition by utilizing resources differently, which can include:
Temporal partitioning: Different times of resource use (e.g., wolves vs. coyotes).
Spatial partitioning: Different habitat use (e.g., plants with different root depths).
Morphological partitioning: Differentiation based on evolved body features affecting resource use.
1.8 Practice Question FRQ 1.1
Identify two organisms competing for a shared resource.
Explain how resource partitioning could help reduce competition among them.
1.2 Terrestrial Biomes
1.9 Learning Objective
ERT-1.B: Describe the global distribution and principal environmental aspects of terrestrial biomes.
Suggested Skill
1.B: Concept Explanation: Explain environmental concepts and processes.
Essential Knowledge
ERT-1.B.1: A biome is defined by characteristic plant and animal communities, adapted to its specific climate.
ERT-1.B.2: Major terrestrial biomes include:
Taiga
Temperate rainforests
Temperate seasonal forests
Tropical rainforests
Shrublands
Temperate grasslands
Savanna
Desert
Tundra
ERT-1.B.3: The distribution of nonmineral terrestrial natural resources, including water and lumber, varies based on climate, geography, latitude, altitude, nutrient availability, and soil quality.
ERT-1.B.4: Biome distribution is dynamic, subject to change from climate shifts.
1.10 Biome Characteristics
Biomes are influenced by average annual temperature and precipitation, affecting vegetation and animal life (for example: desert and tundra).
Latitude affects temperature and precipitation, leading to predictable biome patterns on Earth.
Higher latitudes (60°+) typically host tundra and boreal biomes.
Mid-latitudes (30°-60°) are home to temperate biomes.
Tropic areas by the equator are warmer.
1.11 Nutrient Availability in Biomes
Nutrient-poor soils are typical in:
Tropical Rainforests: High competition due to various plant species.
Boreal Forests: Low decomposition rates lead to nutrient-poor conditions.
Nutrient-rich soils often seen in temperate forests due to abundant organic matter decomposition.
1.12 Shifting Biomes
Climate change leads to biome shift, for instance, boreal forests shifting northward as permafrost melts.
1.13 Practice Question FRQ 1.2
Describe how a specific characteristic of a biome determines its organism community.
1.3 Aquatic Biomes
1.14 Learning Objectives
ERT-1.C: Describe the global distribution and principal environmental aspects of aquatic biomes.
Suggested Skill
1.B: Concept Explanation: Explain environmental concepts and processes.
Essential Knowledge
ERT-1.C.1: Freshwater biomes encompass streams, rivers, ponds, and lakes, significant for drinking water.
ERT-1.C.2: Marine biomes include oceans, coral reefs, marshlands, and estuaries; algae in marine environments contribute to much of Earth’s oxygen.
ERT-1.C.3: The global distribution of marine resources, like various fish, is influenced by salinity, depth, turbidity, nutrient availability, and temperature.
1.15 Characteristics of Aquatic Biomes
Depth: Affects sunlight penetration for photosynthesis.
Temperature: Warmer waters hold less dissolved oxygen.
Salinity: Determines species survivability (e.g., freshwater vs. marine).
Flow: Influences oxygen availability and aquatic life behaviors.
1.16 Freshwater: Rivers & Lakes
Rivers: High oxygenation due to flow, carry nutrients to delta and floodplain regions.
Lakes: Defined zones based on depth:
Littoral: Shallow water with plants.
Limnetic: Well-lit area supporting phytoplankton.
Profundal: Deep section lacking light.
Benthic: Bottom layer where decomposers inhabit.
1.17 Freshwater: Wetlands
Wetland Definition: Area with soil that is submerged or saturated in water for part of the year, supporting emergent plants.
Benefits of Wetlands:
Reduces flood impact.
Recharges groundwater.
Filters contaminants in water.
Supports diverse plant growth.
1.18 Estuaries
Areas where rivers meet oceans, creating high productivity zones due to nutrient deposits.
Salt Marsh: Coastal estuary in temperate areas, breeding grounds for fish.
Mangrove Swamps: Found in tropics, provide stabilization and habitat.
1.19 Coral Reefs
Located in warm, shallow waters, coral reefs are the most diverse marine ecosystems.
Demonstrate mutualism between corals and algae, vital for the reef’s health.
1.20 Intertidal Zones
Areas along the coastline, home to organisms adapted to varying conditions (e.g., barnacles).
1.21 Open Ocean
Generally non-productive; algae and phytoplankton are restricted to the photic zone.
The ocean's vast space contributes significantly to oxygen production.
1.4 Carbon Cycle
1.22 Learning Objectives/EK/Skill
ERT-1.D: Explain the steps and reservoir interactions in the carbon cycle.
Suggested Skill
2.B: Explain relationships between characteristics of environmental concepts visually.
Essential Knowledge
ERT-1.D.1: The carbon cycle refers to carbon's movement between sources and sinks, involving various chemical transformations like (CO2) and glucose (C6H{12}O6).
ERT-1.D.2: Reservoirs vary in carbon retention periods; some are short-term, while others like sedimentary rocks are long-term.
ERT-1.D.3: Carbon cycling involves crucial processes like photosynthesis and respiration.
ERT-1.D.4: Decomposition reinforces carbon storage, while fossil fuel combustion rapidly releases carbon back into the atmosphere.
1.23 Carbon Cycle Overview
Flash processes (like combustion) occur quickly while sedimentation and burial are slow.
Key reservoirs include:
Carbon Sink: Reservoir storing more carbon than it releases (e.g., oceans, plants).
Carbon Source: Processes that add carbon to the atmosphere (e.g., combustion of fossil fuels).
1.24 Photosynthesis and Cellular Respiration
Photosynthesis: Converts (CO_2) into glucose, utilizing sunlight.
Cellular Respiration: Organisms break down glucose, releasing (CO_2).
Counteract emissions from human activities and maintain atmospheric balance.
1.25 Ocean and Atmosphere Exchange
Carbon exchange occurs between the ocean and atmosphere via direct diffusion.
Ocean acidification results from increasing atmospheric carbon influencing marine ecosystems.
1.26 Burial, Extraction & Combustion
Process of burial takes a long time, while extraction and combustion are significantly faster, leading to increased atmospheric carbon.
1.27 Feedback Mechanisms in Carbon Cycle
Increased atmospheric (CO_2) contributes to climate change and potential ecological impacts over time.
1.28 Practice Question FRQ 1.4
Identify a quick and a slow process in the carbon cycle while addressing the fossil fuel impact over the last 250 years.
1.5 Nitrogen Cycle
1.29 Learning Objectives/EK/Skill
ERT-1.E: Explain the steps and reservoir interactions in the nitrogen cycle.
Suggested Skill
2.B: Explain relationships visually.
Essential Knowledge
ERT-1.E.1: The nitrogen cycle details nitrogen in various forms moving between sources and sinks.
ERT-1.E.2: Nitrogen reservoirs are generally short-term holdings.
ERT-1.E.3: Nitrogen fixation converts atmospheric nitrogen (N_2) into forms usable by plants.
ERT-1.E.4: The atmosphere signifies the major nitrogen reservoir.
1.30 Nitrogen Cycle Overview
Nitrogen is crucial for DNA and proteins. However, atmospheric nitrogen's (N_2) form is unusable by most organisms.
1.31 Nitrogen Fixation
Includes two processes:
Synthetic Fixation: Combustion of fossil fuels converts (N2) into nitrate (NO3^−).
Bacterial Fixation: Specific bacteria fix (N2) into ammonia (NH3).
1.32 Steps in Nitrogen Cycle
Include nitrification, ammonification, assimilation, and denitrification.
Human Impacts on the Nitrogen Cycle
Excessive nitrogen fertilizer usage leads to leaching, eutrophication, climate implications, and pollutes water sources.
1.33 Practice Question 1.5
Describe a vital nitrogen cycle transformation and its significance to ecosystems.
1.6 Phosphorus Cycle
1.34 Learning Objectives/EK/Skill
ERT-1.F: Explain the steps and reservoir interactions in the phosphorus cycle.
Suggested Skill
2.B: Visual representation relationships.
Essential Knowledge
ERT-1.F.1: Phosphorus cycle involves movement between sources and sinks without atmospheric presence.
ERT-1.F.2: Major phosphorus reservoirs are found in rocks and sediments.
ERT-1.F.3: Phosphorus is limiting in ecosystems, often scarce.
1.35 Phosphorus Cycle Basics
Very slow compared to nitrogen and carbon cycles; weathering leads to longer processes.
1.36 Phosphorus Sources and Assimilation
Natural phosphorus sources arise from weathered rocks, while synthetic sources result from mining.
1.37 Eutrophication
Occurs when excess nutrients from fertilizers stimulate drastic algae growth, depleting oxygen and resulting in ecosystem failures.
1.38 Practice Question 1.6
Choose two phosphorus reservoirs and describe their interaction.
1.7 Hydrologic (Water) Cycle
1.39 Learning Objectives/EK/Skill
ERT-1.G: Explain the water cycle's steps and reservoir interactions.
Suggested Skill
2.B: Visual representations of relationships.
Essential Knowledge
ERT-1.G.1: The hydrologic cycle, powered by energy from the sun, is the movement of water among its various forms.
ERT-1.G.2: Oceans serve as Earth's primary water reservoir, with ice caps and groundwater being smaller reservoirs.
1.40 Water Cycle Overview
Movement of water (solid, liquid, gas) varies extensively across the environment, chiefly through evaporation and transpiration.
1.41 Key Processes in Water Cycle
Evaporation and transpiration return water vapor into the atmosphere, driven by solar energy.
1.42 Runoff and Infiltration
Precipitation can either flow over surfaces (runoff) or saturate the ground (infiltration), both crucial for maintaining freshwater supplies.
1.43 Practice Question FRQ 1.7
Describe a water cycle process and its effect on water movement.
1.8 Primary Productivity
1.44 Learning Objectives/EK/Skill
ENG-1.A: Explain solar energy acquisition and transfer among organisms.
Suggested Skill
1.A: Concept Explanation: Describe environmental concepts and processes.
Essential Knowledge
ENG-1.A.1: Primary productivity rate measures solar energy conversion into organic compounds through photosynthesis.
ENG-1.A.2: Gross primary productivity (GPP) represents total photosynthesis rate in an area.
ENG-1.A.3: Net primary productivity (NPP) accounts for energy loss through respiration.
ENG-1.A.4: Productivity measured in energy units (e.g., kcal/m^2/yr).
ENG-1.A.5: Light absorption in water impacts aquatic photosynthesis.
1.45 Calculating NPP
Formula for NPP: NPP = GPP - RL,
where RL is respiration loss by plants, representing energy utilizational costs.
1.46 Ecological Efficiency of Biomes
Efficiency reflected in the rate of energy transfer, which is estimated at 10% from one level to the next in a trophic structure.
1.47 Trends in Productivity
Productivity in ecosystems depends on water, temperature, and nutrient availability, affecting biodiversity levels.
1.48 Practice Question FRQ 1.8
Discuss NPP and its relationship to biodiversity.
1.9 Trophic Levels & The 10% Rule
1.49 Learning Objectives/EK/Skill
ENG-1.B: Explain energy flow and matter cycling through trophic levels.
1.50 10% Rule in Energy Transfer
States that approximately 10% of energy is maintained when moving between trophic levels, while the rest is dissipated as heat.
1.51 Conservation of Matter and Energy
Energy is conserved but can change forms, and trophic dynamics illustrate energy availability across ecosystems.
1.52 Trophic Levels Defined
Producers: Convert sunlight into energy.
Primary Consumers: Herbivores feeding on producers.
Secondary and Tertiary Consumers: Carnivores feeding on other consumers.
1.53 Practice Questions FRQs 1.9 & 1.10
Assess energy availability in a food chain context.
1.10 Food Chains and Food Webs
1.54 Learning Objectives/EK/Skill
ENG-1.D: Describe food chains and webs, including their components by trophic level.
1.55 Understanding Food Webs
A food web connects multiple food chains, illustrating the flow of matter and energy.
1.56 Feedback Loops in Ecosystems
Organisms' additions or removals affect ecosystem dynamics.
1.57 Practice Question FRQ 1.11
Illustrate the effects of population changes in ecosystems on food webs.