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Ecosystems & Energy
Introduction to Ecosystems
 Ecosystem-is a combination of all the living (biotic) and non-living (abiotic) elements in a specific
region, regulated by predominate climatic factors.
 Ecosystems are often referred to as biomes and are further broken down into more specific larger scale
ecosystems, and then habitats, communities, finally populations.
 Habitats-are regions within an ecosystem where an organism or population directly lives, feeds,
reproduces, and interacts with other organisms. Ex. Ecosystem: Estuary(Puget Sound) Habitat: Tolmie
Beach
 Communities-are aggregates of different organisms (plants, animals, fungi, bacteria, protists) that all
cohabitate and interact within the same area. Ex: Organisms within Capital Lake
 Populations-is a group of the same species that is capable of interbreeding living in the same
geographical area. Ex. Coyotes in Capital State Forest
Energy in Ecosystems
Plants vs Animals
 All energy on Earth is derived from photosynthetic organisms (plants, algae,
bacteria).
 Plants obtain energy through the process of photosynthesis. These organisms
are referred to as Autotrophs or Producers
 Animals obtain energy by consuming other organisms. They are referred to as
Heterotrophs or Consumers.
Photosynthesis Equation
6CO2 + 6H2O C6H12O6 + 6O2
Carbon Dioxide
from the air 
Used in the
Calvin Cycle
during the Dark
Reactions Water Split during
Photolysis in the
Light Reactions
Glucose Made in
the Calvin Cycle
during the Dark
Reactions
Oxygen Released
during Photolysis
in the Light
Reactions
Light Energy
chlorophyll
Plants can use this glucose molecule for energy during Cellular Respiration. Plants can
also convert this glucose molecule into other organic compounds such as proteins and
fats/lipids or other carbohydrates like starch and cellulose
Cellular Respiration Equation
C6H12O6 + 6O2 6CO2 + 6H2O + energy
Water 
released
from
Electron
Transport
Chain
Oxygen from the
atmosphere
Used in Electron
Transport Chain
Carbon
Dioxide 
waste
product of
the Citric
Acid Cycle
ATP released from
Glycolysis, Citric
Acid Cycle, and
Electron Transport
Chain
Between 34-36 ATP can be made with this process.
This ATP can be used by the cells for cellular metabolism.
Glucose made in
photosynthesis
by plants or
consumed by
animals
Used in
Glycolysis
Metabolism: Cellular Respiration + Glycolysis
 Cellular Respiration: Process by which mitochondria break down
food molecules to produce ATP in plants and animals
Nutrients + oxygen + water  water + ATP + CO2
 Changes organic chemical energy (glucose) into inorganic chemical
energy (ATP)
 There are three stages of Cellular Respiration
 Glycolysis
 Anaerobic  does not require oxygen
 Citric Acid (Krebs) Cycle
 Aerobic  does require oxygen
 Electron Transport Chain
 Aerobic  does require oxygen
Energy Transfer: Trophic Levels
 Energy moves from one organisms to another when it is eaten
 Each step in this transfer of energy is know as a trophic level
 The main trophic levels are producers, consumers, and decomposers
 The total mass of the organic matter at each trophic level is called biomass
(biomass is just another term for potential energy  energy that is to be eaten and
used.)
 The transfer of energy from one level to another is very inefficient (10% Law)
Ecological Pyramid
 An ecological pyramid shows the
relationship between consumers
and producers at different trophic
levels in an ecosystem
 Shows the relative amounts of
energy or matter contained at
each trophic level
 The Pyramid shows which level
has the most energy and the
highest number of organisms
Food Chains & Webs
 A food chain links species by their feeding relationships.
 A food chain follows the connection between one producer and a single chain of
consumers within an ecosystem.
 A food web shows a complex network of feeding relationships.
Food Web Example
Trophic Levels: Consumers
 Consumers are not all alike.
 Herbivores eat only plants.
 Carnivores eat only animals.
 Omnivores eat both plants and animals.
 Detritivores eat dead organic matter.
 Decomposers are detritivores that break down organic matter into simpler
compounds.
Rainforest Ecosystems
Rainforests
 Tropical Rain Forests:
 Almost constant rainfall close to 200 inches per year
 Temperature averages 77属84F with little seasonal variation
 High Biodiversity: home to millions of animal species, including an estimated 530 million still unknown species of insects,
spiders, and other arthropods
 2% of the land but 遜 of worlds species; single tree can have several thousand insect species
 Dominated by broadleaf evergreen plants; their dense tops block out most of the sun
 Ground has little vegetation (those that do have large leaves); or vines grow on trees to reach the sun
 Little wind because of the dense vegetation; plants depend on bats, birds, bees and other species for pollination
 Coastal Coniferous Forest or Temperate Rain Forests: Runs From British Columbia thru Northern California
 Found in scattered coastal temperate areas that have ample rainfall or are moisture from dense ocean fogs 200-350
inches of precipitation per year with average temperatures are 32F-70F
 These are typically small areas with the largest ones running down the PNW coast, other regions include Chile and
New Zealand
 These have the highest biomass out of any terrestrial ecosystem
 Dominated by coniferous trees, mosses, lichens, fungi, epiphytes, a variety of invertebrates, mammals and birds.
Olympic National Park
Desert Ecosystems
 Desert:
 Annual precipitation is low; often scattered unevenly throughout the year
 Heat of day bakes the earth causing evaporation of water from leaves and soil
 Soils have little vegetation and moisture to store the heat so you can roast
during the day and freeze at night
 Tropical Deserts:
 Hot and dry most of the year; few plants and a hard wind blown surface of
rocks and some sand. Ex. Sahara, Iran
 Temperate Deserts:
 Daytime temperatures are high in the summer and low in winter; more
precipitation than in the topical deserts; drought resistance vegetation  cacti
 Ex. Northern Nevada, New Mexico
 Cold Deserts:
 Vegetation is sparse; winters are cold; summers warm or hot and precipitation
is low; plants and animals have adapted to stay cool and get enough water
Shrubsteppe
 Shrubsteppe-is typical of western landscapes dominated with sagebrush, one or more layers of perennial grasses,
rimrocks, tumbleweeds, and a discontinuous layer of various shrubs.
 Many organisms are said to be sagebrush obligates, such as the WA pygmy rabbits, greater sage grouse, sage sparrows,
pronghorn antelope, sagebrush lizard and sage thrashers. Other organisms are very closely tied to the sagebrush too such
as deer, burrowing owls, road runners, hawks and falcons, snakes and several other small mammals.
 Specific species in this area are Keystone species: Sagebrush and sage grouse
 This ecosystem is particularly threatened by too many juniper trees, free roaming cattle, humans and invasive species.
Mountainous Ecosystems
 Mountains:
 Mountains are steep or high lands that cover 村 of the Earths surface; dramatic
changes in altitude, slope, climate, soil and vegetation occur in a very short
distances
 1.2 bil people (18% of the worlds population) live on them or their edges; 4 bil
(59%) depend on mountain systems for all or some of their water (the majority
of groundwater is replenished from these areas)
 Majority of the worlds forests; habitats that maintain biodiversity and endemic
species found only in these regions
 These landforms regulate the Earths climate: snow and ice reflect solar
radiation helping to cool the planet, while air masses that move over them
create rain shadows, and the plants that grow on their slopes participate in
transpiration
 Mountains are formed through geologic activities and can be found on every
continent on Earth
Ecolosystems in PNW.pptx
Forest Ecosystems
 Forests are classified as an undisturbed area with an average precipitation of 30 inches or more a year, consisting of various
species of trees and smaller woody forms of vegetation.
Northern Conifer Forests -Also called boreal forests or taiga
 These are found in regions with a subarctic climate (high elevations/latitudes) where winters are long and dry with only light
snowfall.
 Temperatures range from cool to extremely cold and summers are very brief with mild to warm temperature.
 These forests, which from an almost unbroken belt across North America and Northern Eurasia.
 Plants species diversity is low in the northern forests because few species can survive the winters.
Pine Forests
 Considered as a dis climax or anthropogenic subclimax formation.
 Anthropogenic activities, such as collecting timber for house, cleaning lands for shifting cultivation, accidental or international
setting of fires transformed these forest into open and drier sites.
 The greatest segment of this vegetation cover lies between 900-1,500 meters where a distinct dry season occurs.
 The undergrowth vegetation of pine forest cannot fully development or advance ecologically
Forests
Grasslands (Prairies) Ecosystems
 Grasslands have continental climates characterized by large annual range of temperatures, cool -
cold winters, with most of precipitation as snow, and hot, summers often experiencing droughts, due
to high evapotranspiration rates.
 These can be found in flat or slightly rolling terrains that cannot support large stand of trees.
 They abound in regions where average precipitation ranges from 10-30 inches a year
 This amount of precipitation is sufficient to grow grass yet, rainfall occurrences are so sporadic that
periodic droughts and grassfires prevent the growth of large stands of trees.
 The grassland soils are thin and cannot store enough water because of intense sunlight, high
temperature and evaporation rates.
 Prairies-have a slightly higher biodiversity than typical grasslands, consisting of wildflowers, small
drought resist shrubs and a higher diversity of grasses and animals as a result.
Ecolosystems in PNW.pptx
Aquatic Ecosystems
 Earth is covered with water  hence we are known as the Water Planet
 Saltwater covers 97% of the Earth
 Freshwater ~3%, which 69% of that is frozen, 30% is groundwater, .3% is surface water (87% is lakes, 2% is rivers)
 Aquatic Life Zones: determined by the amount of salinity  amount of salt (NaCl) in the water
 Saltwater: has an average salinity of 33-37%, colder waters are lower and warmer waters are higher
 Marine: brackish which is a combination of salt and freshwater and are considered to be saltwater and include
 5 oceans: Atlantic, Arctic, Indian and Pacific; Antarctic (Pacific is the largest and deepest)
 Oceans and estuaries, bays, seas, shorelines, coral reefs and mangrove forests all have specific parameters
 Freshwater
 Lakes, rivers and streams, ponds, inland wetlands and swamps
 Can have virtually no dissolved substances and be completely clear or many dissolved substances and cloudy
 How Aquatic Ecosystems are Defined:
 They are stratified (layered) into Zones defined by light penetration, temperature, and depth
 The Pelagic Zone:
 Photic Zone has sufficient light for photosynthesis; most animals live here
 This zone often fluctuates with seasonal changes due to vegetation and input of sediment from runoff
 A subtype of zone, more commonly noted in closed bodies of water is called the Littoral Zone (near shore)
 In marine environments it can exceed 300 feet in clear water allowing for giant kelp to grow, typically tropical waters are
clearer
 Aphotic Zone receives little light; and therefore fewer organisms dwell here
 In deep lakes or marine environments you find the Abyssal Zone at depth of 2,000 to 6,000 m
 In closed bodies of water where little light penetrates it is often referred to as the Profundal Zone
 The Benthic Zone:
 Organic and inorganic sediment at the bottom of all aquatic zones (detritus) important food source for bottom dwellers
 Communities of organisms are collectively called the Benthos
Lakes
Lakes: Natural bodies of freshwater formed from precipitation, runoff or groundwater that fill in depressions in the surface
mostly due to geologic activity such as glaciers eg. Lake Crescent in WA or volcanic activity eg. Crater Lake in OR.
 Natural lakes are NOT to be confused with reservoirs however which are manmade and confined by a dam, dike or
levee.
Two Categories of Lakes
Oligotrophic Lakes:
 Nutrient-poor and generally oxygen-rich
 Small supply of plant nutrients
 Generally deep with steep banks; fed by glaciers and mountain streams with little sediment; crystal clear
Eutrophic Lakes:
 Nutrient-rich and often depleted of oxygen if ice covered in winter
 Rooted and floating aquatic plants live in shallow and well-lighted areas close to shore
 Water is too deep to support rooted aquatic plants; small drifting animals called zooplankton graze on the
phytoplankton
 Invertebrates live in the benthic zone; Fish live in all zones with sufficient oxygen
Ecolosystems in PNW.pptx
Ecolosystems in PNW.pptx
Wetlands
Wetland- an area that remains flooded with fresh water all or part of the year and located away from coastal areas, yet can be affected by
tidal changes (bogs, marshes, swamps and salt marshes)
 Are identified based on their water, soil types (hydric soils), and vegetation.
 Water typically floods the areas consecutively for at least 7.5% of the growing season.
 Hydric soil (wetland soils) remains wet long enough to create oxygen poor conditions.
 Plants in wetlands are hydrophilic adapted to growing in wet soil with little oxygen.
 Wetlands are important environmental functions that are needed to help protect our land and water sources.
 Marshes-contain non-woody plants such as cat tails, reeds, rushes, which anchor themselves in the bottom
 Tend to occur on low flat land in areas with little water movement
 Bottom sediment is nutrient rich and provides habitat for many water fowl
 Swamps-dominated by woody plants such as trees and shrubs, such as mangroves
 Occur on poorly drained land often near streams, typically in lower latitudes
 Great habitat for amphibians, birds and reptiles
Ecolosystems in PNW.pptx
Watershed Regions
Watershed, Drainage Basin: land that delivers runoff, sediment and dissolved substances into a stream; small streams form rivers and
rivers flow downhill to the ocean
 Aquatic Life Zones:
 Source Zone:
 Headwaters or mountain highland streams; usually shallow, cold, clear and swift flowing; waterfalls and rapids
 Not productive because of lack of nutrients and producers; food is from decomposition; algae; fishes
 Transition Zone:
 Middle; become wider, deeper and warmer; slower; more turbid (cloudier)
 Producers; both cold and warm water fish (black bass)
 Floodplain Zone:
 Over time, they shape the land including leveling or cutting through mountains forming canyons; streams can join others,
forming wider and deeper rivers
 Large amount of producers and fish; rivers end in a mouth or delta; absorb the floodwaters and add nutrient rich sediments
Streams and Rivers
Streams and Rivers:
 Most prominent physical characteristic of streams and rivers is flow; which is determined by depth and width of
channel
 Headwaters are generally cold, clear, turbulent, swift, and oxygen rich; they are often narrow and rocky
 Downstream waters diverge into multiple tributaries, which widen, slow, warm and become more laden with
sediment. Depending on the channel slope and width it can increase flow.
 May contain phytoplankton or rooted aquatic plants along the banks and stream bottom
 Diversity of fish and invertebrates inhabit unpolluted rivers and streams
 Damming and flood control impair natural functioning of stream and river ecosystems
 Riparian Zones-are classified as the saturated zone next to any river or stream where vegetation is present and is a
vital part of nutrient input, regulating stream temperatures, and reducing bank erosion.
Marine Ecosystems
Estuaries:
 Where rivers meet the sea; partially enclosed bodies of water where sea water mixes with fresh water as well as nutrients
from streams, rivers and runoff from the land
 Seagrass/Eel Grass Beds:
 Species of plants that grow underwater in shallow marine waters and estuaries along the coastline
 Highly productive and support a variety of marine species
 Stabilize shorelines and reduce wave impact
 Filter the water
 Intertidal Zone:
 Area between high and low tides (gravitational pull of the moon and sun)
 These can be sandy, rocky, mudflats or a combination and provide habitat for small invertebrates and vertebrates
 Larger land vertebrate species rely on these areas for a large percent of their diet
 Organisms must adapt to, salinity, pH, temperature, pressure, light and nutrient changes
 Oxygen and nutrient levels are high but are in constant flux
Ecolosystems in PNW.pptx

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Ecolosystems in PNW.pptx

  • 2. Introduction to Ecosystems Ecosystem-is a combination of all the living (biotic) and non-living (abiotic) elements in a specific region, regulated by predominate climatic factors. Ecosystems are often referred to as biomes and are further broken down into more specific larger scale ecosystems, and then habitats, communities, finally populations. Habitats-are regions within an ecosystem where an organism or population directly lives, feeds, reproduces, and interacts with other organisms. Ex. Ecosystem: Estuary(Puget Sound) Habitat: Tolmie Beach Communities-are aggregates of different organisms (plants, animals, fungi, bacteria, protists) that all cohabitate and interact within the same area. Ex: Organisms within Capital Lake Populations-is a group of the same species that is capable of interbreeding living in the same geographical area. Ex. Coyotes in Capital State Forest
  • 4. Plants vs Animals All energy on Earth is derived from photosynthetic organisms (plants, algae, bacteria). Plants obtain energy through the process of photosynthesis. These organisms are referred to as Autotrophs or Producers Animals obtain energy by consuming other organisms. They are referred to as Heterotrophs or Consumers.
  • 5. Photosynthesis Equation 6CO2 + 6H2O C6H12O6 + 6O2 Carbon Dioxide from the air Used in the Calvin Cycle during the Dark Reactions Water Split during Photolysis in the Light Reactions Glucose Made in the Calvin Cycle during the Dark Reactions Oxygen Released during Photolysis in the Light Reactions Light Energy chlorophyll Plants can use this glucose molecule for energy during Cellular Respiration. Plants can also convert this glucose molecule into other organic compounds such as proteins and fats/lipids or other carbohydrates like starch and cellulose
  • 6. Cellular Respiration Equation C6H12O6 + 6O2 6CO2 + 6H2O + energy Water released from Electron Transport Chain Oxygen from the atmosphere Used in Electron Transport Chain Carbon Dioxide waste product of the Citric Acid Cycle ATP released from Glycolysis, Citric Acid Cycle, and Electron Transport Chain Between 34-36 ATP can be made with this process. This ATP can be used by the cells for cellular metabolism. Glucose made in photosynthesis by plants or consumed by animals Used in Glycolysis
  • 7. Metabolism: Cellular Respiration + Glycolysis Cellular Respiration: Process by which mitochondria break down food molecules to produce ATP in plants and animals Nutrients + oxygen + water water + ATP + CO2 Changes organic chemical energy (glucose) into inorganic chemical energy (ATP) There are three stages of Cellular Respiration Glycolysis Anaerobic does not require oxygen Citric Acid (Krebs) Cycle Aerobic does require oxygen Electron Transport Chain Aerobic does require oxygen
  • 8. Energy Transfer: Trophic Levels Energy moves from one organisms to another when it is eaten Each step in this transfer of energy is know as a trophic level The main trophic levels are producers, consumers, and decomposers The total mass of the organic matter at each trophic level is called biomass (biomass is just another term for potential energy energy that is to be eaten and used.) The transfer of energy from one level to another is very inefficient (10% Law)
  • 9. Ecological Pyramid An ecological pyramid shows the relationship between consumers and producers at different trophic levels in an ecosystem Shows the relative amounts of energy or matter contained at each trophic level The Pyramid shows which level has the most energy and the highest number of organisms
  • 10. Food Chains & Webs A food chain links species by their feeding relationships. A food chain follows the connection between one producer and a single chain of consumers within an ecosystem. A food web shows a complex network of feeding relationships.
  • 12. Trophic Levels: Consumers Consumers are not all alike. Herbivores eat only plants. Carnivores eat only animals. Omnivores eat both plants and animals. Detritivores eat dead organic matter. Decomposers are detritivores that break down organic matter into simpler compounds.
  • 13. Rainforest Ecosystems Rainforests Tropical Rain Forests: Almost constant rainfall close to 200 inches per year Temperature averages 77属84F with little seasonal variation High Biodiversity: home to millions of animal species, including an estimated 530 million still unknown species of insects, spiders, and other arthropods 2% of the land but 遜 of worlds species; single tree can have several thousand insect species Dominated by broadleaf evergreen plants; their dense tops block out most of the sun Ground has little vegetation (those that do have large leaves); or vines grow on trees to reach the sun Little wind because of the dense vegetation; plants depend on bats, birds, bees and other species for pollination Coastal Coniferous Forest or Temperate Rain Forests: Runs From British Columbia thru Northern California Found in scattered coastal temperate areas that have ample rainfall or are moisture from dense ocean fogs 200-350 inches of precipitation per year with average temperatures are 32F-70F These are typically small areas with the largest ones running down the PNW coast, other regions include Chile and New Zealand These have the highest biomass out of any terrestrial ecosystem Dominated by coniferous trees, mosses, lichens, fungi, epiphytes, a variety of invertebrates, mammals and birds.
  • 15. Desert Ecosystems Desert: Annual precipitation is low; often scattered unevenly throughout the year Heat of day bakes the earth causing evaporation of water from leaves and soil Soils have little vegetation and moisture to store the heat so you can roast during the day and freeze at night Tropical Deserts: Hot and dry most of the year; few plants and a hard wind blown surface of rocks and some sand. Ex. Sahara, Iran Temperate Deserts: Daytime temperatures are high in the summer and low in winter; more precipitation than in the topical deserts; drought resistance vegetation cacti Ex. Northern Nevada, New Mexico Cold Deserts: Vegetation is sparse; winters are cold; summers warm or hot and precipitation is low; plants and animals have adapted to stay cool and get enough water
  • 16. Shrubsteppe Shrubsteppe-is typical of western landscapes dominated with sagebrush, one or more layers of perennial grasses, rimrocks, tumbleweeds, and a discontinuous layer of various shrubs. Many organisms are said to be sagebrush obligates, such as the WA pygmy rabbits, greater sage grouse, sage sparrows, pronghorn antelope, sagebrush lizard and sage thrashers. Other organisms are very closely tied to the sagebrush too such as deer, burrowing owls, road runners, hawks and falcons, snakes and several other small mammals. Specific species in this area are Keystone species: Sagebrush and sage grouse This ecosystem is particularly threatened by too many juniper trees, free roaming cattle, humans and invasive species.
  • 17. Mountainous Ecosystems Mountains: Mountains are steep or high lands that cover 村 of the Earths surface; dramatic changes in altitude, slope, climate, soil and vegetation occur in a very short distances 1.2 bil people (18% of the worlds population) live on them or their edges; 4 bil (59%) depend on mountain systems for all or some of their water (the majority of groundwater is replenished from these areas) Majority of the worlds forests; habitats that maintain biodiversity and endemic species found only in these regions These landforms regulate the Earths climate: snow and ice reflect solar radiation helping to cool the planet, while air masses that move over them create rain shadows, and the plants that grow on their slopes participate in transpiration Mountains are formed through geologic activities and can be found on every continent on Earth
  • 19. Forest Ecosystems Forests are classified as an undisturbed area with an average precipitation of 30 inches or more a year, consisting of various species of trees and smaller woody forms of vegetation. Northern Conifer Forests -Also called boreal forests or taiga These are found in regions with a subarctic climate (high elevations/latitudes) where winters are long and dry with only light snowfall. Temperatures range from cool to extremely cold and summers are very brief with mild to warm temperature. These forests, which from an almost unbroken belt across North America and Northern Eurasia. Plants species diversity is low in the northern forests because few species can survive the winters. Pine Forests Considered as a dis climax or anthropogenic subclimax formation. Anthropogenic activities, such as collecting timber for house, cleaning lands for shifting cultivation, accidental or international setting of fires transformed these forest into open and drier sites. The greatest segment of this vegetation cover lies between 900-1,500 meters where a distinct dry season occurs. The undergrowth vegetation of pine forest cannot fully development or advance ecologically
  • 21. Grasslands (Prairies) Ecosystems Grasslands have continental climates characterized by large annual range of temperatures, cool - cold winters, with most of precipitation as snow, and hot, summers often experiencing droughts, due to high evapotranspiration rates. These can be found in flat or slightly rolling terrains that cannot support large stand of trees. They abound in regions where average precipitation ranges from 10-30 inches a year This amount of precipitation is sufficient to grow grass yet, rainfall occurrences are so sporadic that periodic droughts and grassfires prevent the growth of large stands of trees. The grassland soils are thin and cannot store enough water because of intense sunlight, high temperature and evaporation rates. Prairies-have a slightly higher biodiversity than typical grasslands, consisting of wildflowers, small drought resist shrubs and a higher diversity of grasses and animals as a result.
  • 23. Aquatic Ecosystems Earth is covered with water hence we are known as the Water Planet Saltwater covers 97% of the Earth Freshwater ~3%, which 69% of that is frozen, 30% is groundwater, .3% is surface water (87% is lakes, 2% is rivers) Aquatic Life Zones: determined by the amount of salinity amount of salt (NaCl) in the water Saltwater: has an average salinity of 33-37%, colder waters are lower and warmer waters are higher Marine: brackish which is a combination of salt and freshwater and are considered to be saltwater and include 5 oceans: Atlantic, Arctic, Indian and Pacific; Antarctic (Pacific is the largest and deepest) Oceans and estuaries, bays, seas, shorelines, coral reefs and mangrove forests all have specific parameters Freshwater Lakes, rivers and streams, ponds, inland wetlands and swamps Can have virtually no dissolved substances and be completely clear or many dissolved substances and cloudy
  • 24. How Aquatic Ecosystems are Defined: They are stratified (layered) into Zones defined by light penetration, temperature, and depth The Pelagic Zone: Photic Zone has sufficient light for photosynthesis; most animals live here This zone often fluctuates with seasonal changes due to vegetation and input of sediment from runoff A subtype of zone, more commonly noted in closed bodies of water is called the Littoral Zone (near shore) In marine environments it can exceed 300 feet in clear water allowing for giant kelp to grow, typically tropical waters are clearer Aphotic Zone receives little light; and therefore fewer organisms dwell here In deep lakes or marine environments you find the Abyssal Zone at depth of 2,000 to 6,000 m In closed bodies of water where little light penetrates it is often referred to as the Profundal Zone The Benthic Zone: Organic and inorganic sediment at the bottom of all aquatic zones (detritus) important food source for bottom dwellers Communities of organisms are collectively called the Benthos
  • 25. Lakes Lakes: Natural bodies of freshwater formed from precipitation, runoff or groundwater that fill in depressions in the surface mostly due to geologic activity such as glaciers eg. Lake Crescent in WA or volcanic activity eg. Crater Lake in OR. Natural lakes are NOT to be confused with reservoirs however which are manmade and confined by a dam, dike or levee. Two Categories of Lakes Oligotrophic Lakes: Nutrient-poor and generally oxygen-rich Small supply of plant nutrients Generally deep with steep banks; fed by glaciers and mountain streams with little sediment; crystal clear Eutrophic Lakes: Nutrient-rich and often depleted of oxygen if ice covered in winter Rooted and floating aquatic plants live in shallow and well-lighted areas close to shore Water is too deep to support rooted aquatic plants; small drifting animals called zooplankton graze on the phytoplankton Invertebrates live in the benthic zone; Fish live in all zones with sufficient oxygen
  • 28. Wetlands Wetland- an area that remains flooded with fresh water all or part of the year and located away from coastal areas, yet can be affected by tidal changes (bogs, marshes, swamps and salt marshes) Are identified based on their water, soil types (hydric soils), and vegetation. Water typically floods the areas consecutively for at least 7.5% of the growing season. Hydric soil (wetland soils) remains wet long enough to create oxygen poor conditions. Plants in wetlands are hydrophilic adapted to growing in wet soil with little oxygen. Wetlands are important environmental functions that are needed to help protect our land and water sources. Marshes-contain non-woody plants such as cat tails, reeds, rushes, which anchor themselves in the bottom Tend to occur on low flat land in areas with little water movement Bottom sediment is nutrient rich and provides habitat for many water fowl Swamps-dominated by woody plants such as trees and shrubs, such as mangroves Occur on poorly drained land often near streams, typically in lower latitudes Great habitat for amphibians, birds and reptiles
  • 30. Watershed Regions Watershed, Drainage Basin: land that delivers runoff, sediment and dissolved substances into a stream; small streams form rivers and rivers flow downhill to the ocean Aquatic Life Zones: Source Zone: Headwaters or mountain highland streams; usually shallow, cold, clear and swift flowing; waterfalls and rapids Not productive because of lack of nutrients and producers; food is from decomposition; algae; fishes Transition Zone: Middle; become wider, deeper and warmer; slower; more turbid (cloudier) Producers; both cold and warm water fish (black bass) Floodplain Zone: Over time, they shape the land including leveling or cutting through mountains forming canyons; streams can join others, forming wider and deeper rivers Large amount of producers and fish; rivers end in a mouth or delta; absorb the floodwaters and add nutrient rich sediments
  • 31. Streams and Rivers Streams and Rivers: Most prominent physical characteristic of streams and rivers is flow; which is determined by depth and width of channel Headwaters are generally cold, clear, turbulent, swift, and oxygen rich; they are often narrow and rocky Downstream waters diverge into multiple tributaries, which widen, slow, warm and become more laden with sediment. Depending on the channel slope and width it can increase flow. May contain phytoplankton or rooted aquatic plants along the banks and stream bottom Diversity of fish and invertebrates inhabit unpolluted rivers and streams Damming and flood control impair natural functioning of stream and river ecosystems Riparian Zones-are classified as the saturated zone next to any river or stream where vegetation is present and is a vital part of nutrient input, regulating stream temperatures, and reducing bank erosion.
  • 32. Marine Ecosystems Estuaries: Where rivers meet the sea; partially enclosed bodies of water where sea water mixes with fresh water as well as nutrients from streams, rivers and runoff from the land Seagrass/Eel Grass Beds: Species of plants that grow underwater in shallow marine waters and estuaries along the coastline Highly productive and support a variety of marine species Stabilize shorelines and reduce wave impact Filter the water Intertidal Zone: Area between high and low tides (gravitational pull of the moon and sun) These can be sandy, rocky, mudflats or a combination and provide habitat for small invertebrates and vertebrates Larger land vertebrate species rely on these areas for a large percent of their diet Organisms must adapt to, salinity, pH, temperature, pressure, light and nutrient changes Oxygen and nutrient levels are high but are in constant flux