APES Unit 9
Unit 9.1: The Stratospheric Ozone Depletion
Troposphere VS Stratosphere
These are the two locations for ozone in our atmosphere
Troposphere- produces ozone from photochemical smogs, greenhouse gas effect (can be harmful)
Stratosphere - naturally occurring ozone that provides protection from UVB-UVC rays
Using that radiation to transform ozone (O3) to atmospheric oxygen (O2)
Antarctic Spring
Antarctic winters can create stratospheric clouds full of ice crystals
Crystals melt in the beginning of the spring
Chemical reactions convert less reactive chlorine into a more reactive form
Chlorine degrades ozone into atmospheric oxygen (O2)
The ozone layer thins
Chlorofluorocarbons (CFCs)
Refrigerant/coolant
Propellant
Some types of plastics
CFCs can escape and enter the stratosphere
UV light removes chlorine from CFCs
Free chlorine catalyzes the conversion of O3 to O2
Effects of Ozone Depletion
Thinning of ozone layers, especially at poles
Disrupts photosynthesis, both terrestrial and in phytoplankton
Disrupts food chains and food webs
Impacts populations of some organisms like amphibians
Impacts human health: skin cancer, cataracts
Unit 9.2: Reducing Ozone Depletion
Montreal Protocol - an international treaty that phased out the use of CFCs and their manufacture in 1987
They did this upon recognizing CFCs were thinning the ozone layers and harming the environment
However CFCs are persistent, so it will take decades for CFCs currently in the stratosphere to completely dissipate, allowing the ozone layer to fully repairable
HFCs (hydrofluorocarbons) replace CFCs
No chlorine to catalyze transformation of ozone into atmospheric oxygen
Powerful greenhouse gas
Unit 9.3: The Greenhouse Effect
The greenhouse effect occurs in the troposphere
The sun’s solar radiation warms the earth
Some energy is reflected, some energy is re-radiated as heat back into space
Some re-radiated heat is absorbed by greenhouse gasses in the troposphere, then emitted again toward the surface of the Earth as heat
The “greenhouse effect” helps to keep the Earth at a temperature that can support life
The greenhouse effect and the ozone layer are in two separate layers of the atmosphere
Greenhouse gasses
Carbon dioxide - CO2
Vast majority come from combustion, either from transportation or fossil fuels
Methane - CH4
Comes from enteric fermentation, natural gas and petroleum systems, and several other sources
Water vapor - H2O
Condenses and produces precipitation, does not spend much time in the atmosphere
Does not play a large role in the greenhouse effect
Nitrous Oxide - N2O
It is an agricultural source management issue
Chlorofluorocarbons (CFCs) - example: CF2Cl2
Both CFCs and HFCs are man made
Hydrofluorocarbons (HFCs)
Substitution for CFCs
Tropospheric Ozone - O3
Comes from photochemical smog
Carbon dioxide is a reference molecule for the greenhouse effect, so has a global warming potential (GWP) of 1
GWPs or various greenhouse gasses: CFCs/HFCs > ozone > nitrous oxide > methane > carbon dioxide
Carbon dioxide has the greatest overall impact on the greenhouse effect because of its concentration in the atmosphere
Human activities influence the concentration of various greenhouse gasses in the atmosphere
Unit 9.4: Increases in the Greenhouse Gasses
Greenhouse gasses that produce the greenhouse effect include carbon dioxide, methane, nitrous oxide, ozone, CFCs, HFCs, and water vapor
Concentrations of many greenhouse gasses have steadily increased in the atmosphere as a result of human activity
Increased greenhouse gasses have led to climate change
Sea Levels Rise
Land ice (example: continental glaciers, ice sheets) melts, adding to the volume of water in the ocean
Thermal expansion of the ocean, due to warming from climate change, increases the volume of the ocean
Disease vectors expand their range
Climate change impacts Ecological Populations
Habitat destruction
Loss of food source
Timing of food source availability changes
New temperatures beyond range of tolerance
New salinity beyond range of tolerance
Increased storm intensity
Increased possibility of fire
Impacted annual group behaviors timing of migration, hibernation
Climate Change Impacts Human Populations
Low-income populations
Occupational groups
People in certain locations
Pregnant women
People with pre-existing medical conditions
Children
Older adults
People with disabilities
Indigenous people
Climate Change Has Global Impact
Environmental Impacts
Changes in ocean salinity and temperature affect marine organisms at every trophic level in many ways
Changes in temperature affect terrestrial organisms at every trophic level in many ways
Impacts on Humans
Impacts include responses to temperature changes, access to food, access to fresh water, and changing land availability
Anthropogenic activities produce the additional greenhouse gasses that drive climate change
Many activities - individual actions, agriculture, industry - produce greenhouse gasses
Unit 9.5: Global Climate Change
Historical records about climate change
We have records over the past 800,000 years that tell us about regular periods of warming, cooling, and carbon dioxide increase and decrease
We get this information from ice cores in arctic areas
We can measure how much carbon dioxide is the ice and how melted it is can tell us about warming or cooling
Change in temperature could also cause a change in air circulation, global wind patterns, and soil quality
Current data shows that the Earth is warming, which is correlated with an increase in the concentration of greenhouse gasses in the atmosphere
Effects of climate change include rising temperatures, rising seas levels, and displacement of coastal populations
Rising Temperatures Melt Global Ice
Melting polar ice reveals darker soil and water (lower albedo than ice), which drives a positive feedback warming loop
Melting permafrost releases methane gas, which drives a positive feedback warming loop
Melting sea ice affects species that depend on the ice for habitat and food, such as polar bears and seals
Climate Change Leads to Changes in the World Ocean
Climate change leads to sea level rise
Benefit - new marine habitat created
Drawback - increasing depth of ocean impacts organisms that will no longer be in the photic zone
Climate change can alter ocean currents
Salinity and temperature changes impact water density, which can impact the ocean conveyor belt
Altered ocean currents can impacts terrestrial climate, especially in coastal areas
Unit 9.6: Ocean Warming
Ocean Warming - the global increase in ocean water temperatures
The amount of warming isn’t uniform across the globe - some ocean areas have warmed more quickly than others
Effects of Ocean Warming
Increase in greenhouse gasses can lead to a variety of environment problems
Rising sea levels from melting ice sheets and ocean water expansions
Thermal expansion of the ocean due to ocean warming causes rising sea levels and displacement of coastal populations due to flooding
Ocean warming affects marine species in a variety of ways
Loss of habitat
Negatively impacts hunting and feeding patterns
Can impact predator and prey interactions
Affects coastlines that impact species using both land and water resources
Can push communities out of the photonics
Impacts primary productivity of phytoplankton, the basis for marine food webs
Metabolic Changes
Marine species will not be able to escape to cooler areas
This could weaken organisms and cause them to die
Reduction of biodiversity and disruption of trophic structures
Reproductive Changes
Organisms weakened by thermal stress do not reproduce well
Many marine reproductive patterns are timed based on specific ocean temperatures - disruption of these temperature patterns leads to reproductive harm
Coral Bleaching
Warming temperatures stress the corals, they expel that algae that gives them color, giving them a bleached color
Can recover, but if conditions persist they will die
They are the foundation of highly biodiverse reef ecosystems, their loss will disrupt the trophic structure and has a negative impact on the marine ecosystem
Unit 9.7: Ocean Acidification
Ocean Acidification - the decrease of pH of ocean waters
The pH scale is logarithmic- each jump of one on the scale is a tenfold increase, so about a 30% increase
Like ocean warming, ocean acidification is due primarily to greenhouse gas concentrations in the atmosphere, specifically carbon dioxide
The more CO2 is released into the atmosphere, the more the oceans absorb, lowering their pH through specific chemical reactions
Anthropogenic activities that contribute to ocean acidification are those that lead to increased CO2, including
Burning/combustion of fossil fuels
Vehicle emissions
Deforestation
When CO2 is absorbed by seawater a series of chemical reactions occur which result in an increase in hydrogen ions
The water combines with the carbon dioxide to create carbonic acid, which is a weak acid. The carbonic acid then dissociates into hydrogen ions and bicarbonate ions
The greater the concentration of hydrogen ions, the lower the pH of the water (more acidic)
Effects of Ocean Acidification
Increased concentration of hydrogen ions bond with available carbonate ions in seawater, a bicarbonate ion is formed
Marine organism can’t extract this carbonate, making it difficult for them to build shells and exoskeletons
Corals need free carbonate ions to form skeletons as well
This loss of calcium carbonate is very harmful for these organisms
Oceans absorb carbon dioxide, the more carbon dioxide present, the more they absorb, which warms the ocean
Unit 9.8: Invasive Species
Invasive Species - an alien species whose introduction does or is likely to cause economic or environmental harm or harm to human health
Invasive species can be beneficial sometimes, but they are considered invasive when they threaten native species in some manner
Non-native species may be introduced into ecosystems accidentally or purposefully
They tend to be niche, generalist, r-selected species
They can withstand a wide variety of abiotic conditions
Can survive on a lot of food
Can produce a lot of offspring in a short time, but there is little parental care
Exponential growth, mature very quickly
Not every species that is introduced to an ecosystem becomes invasive
Insavises have a competitive advantage over natives
How are invasive species spread?
Transport of lumber and firepower
Ballast water in ships, movement of boats and boat trailers, international travel as well
Movement of wind and water
On the fur of other animals
How to Control the Spread
Clean boats and boat trailers
Prevent dumping of aquariums and release of exotic pets
Clean hiking gear before going into a new hiking area
Keep firewood wear it was cut to prevent spread of wood-borne pathogens
How can we Control the Spread?
Introduce a competitor species
Introduce a predator species
Introduce a virus
Physically remove them
Release a pesticide to control their spread
Unit 9.9: Endangered Species
Factors that Lead to Extinction
As habitats are lost or altered globally, many species are threatened with extinction
Extensive Hunting
Poaching is illegal hunting, killing or capturing of animals for sale of profit
Animals are hunted for food, prized body parts, traditional medicinal uses
Medical research purposes
Sport
Limited Diet & Habitat
Species who are niche specialists are generally at greater risk of extinction
These species typically need specific materials for their diet and habitat to survive, and do not reproduce quickly
Outcompeted by Invasive Species
Invasive species have little diet and habitat requirements, so they can out-adapt and out-compete some native species that have a limited lifestyle
The biological and behavioral traits of a species will determine their risk of extinction when exposed to environmental change
Species that can adapt to these changes better have less of a chance of becoming extinct
Adaptation requires genetic diversity
Species can migrate to a more favorable environment to avoid extinction, but this could also raise competition in the new environment
Selective Pressure - any external factor that changes the behavior and fitness of organisms within an environment
Examples include
Resource Availability
Food
Water
Habitat
Mates
Abiotic Environmental Condition
Temperature
Humidity
Tree cover
Salinity
Biological Factors
Pathogens (viruses, bacteria, and fungi)
Diseases
Selective pressure determine which genetic and behavioral traits are favorably adapted to the environment and which aren’t
Pressures will change in changing environments, so traits that were once advantageous in an environment may not continue to be so
Competition can occur within or between species in an ecosystem where there are limited resources
Species seek to limit competition because it’s biologically costly
Competition consumes important metabolic resources, so competitive strategies generally evolve to a limit resource conflicts through resource partitioning
Organisms may compete within their own species resources, such as
Territory
Food
Mates
Habitat
Competition can become intense enough to eat to a species’ endangerment or extinction when:
Trophic relationships are disrupted
There is increased competition invasive species
Resources have become increasingly scarce due to habitat loss or climate change
Strategies to Protect Species
Legislation - (with enforcement) is one primary way to help protect endangered species
Criminalizing poaching and instituting steep fines and/or punishment for poachers can help curb this practice
Laws prohibiting the harming of endangered species and their habitats, or trade in endangered species
The Lacey Act
The Endangered Species Act
The Marine Mammal Protection Act
CITES (the Convention on International Trade in Endangered of Wild Fauna and Flora)
The establishment of protected areas for species, such as wildlife refuges or national parks
Enforcement of conversation practices help as well
Unit 9.10: Human Impacts on Biodiversity
HIPPCO - an acronym regarding the main factors leading to decreases in biodiversity
Habitat destruction
Invasive species
Population growth
Pollution
Climate change
Over exploitation
Habitat Fragmentation
Occurs when large habitats are broken up into smaller, isolated area
Caused by construction of roads and pipelines, clearing of land for agriculture, and logging
Not all species are equally impacted by this
Generalists who thrive in abiotic conditions, or species that thrive in areas where two habitats meet can adapt to fragmentation
Specialists with specific habitat requirements suffer more
Generally decreases biodiversity despite some generalist species having an increase in population
Climate Change and Habitat Loss
Global climate change plays a large role in habitat loss
As average global temperature rises, habitats may be lost due to
Coastal inundation from melting ice and permafrost
Rising sea levels due to thermal expansion
Changes in precipitation patterns due to changing atmospheric and oceanic circulation patterns
Climate change has been most intense in northern latitudes; as warming trends continue, these areas will be at most risk for habitat loss and loss of biodiversity
Domestication and Loss of Biodiversity
Humans have been domesticating organisms for thousands of years
Domestication - involves artificial selection, in which organisms with the most desirable traits for humans are crossbred to enhance the occurrence of that in the species
Many domesticated species are managed for economic returns, and provide humans with
Food
Medicine
Labor
Pollination Services
When humans assume responsibility for the reproduction and selection of traits in another species, genetic diversity will be reduced
Domestication for economic return leads to a loss of biodiversity
Examples of this can be seen in domestic livestock (cattle, sheep, goats, pigs), honeybees, and the agricultural practice of monocropping
Strategies to Mitigate Biodiversity Loss
As global climate change intensifies, it is important that we address current and future losses of biodiversity. Strategies include:
The creation of protected areas, such as wildlife refuges and parks
The creation of habitat corridors to reduce the negative effects of habitat fragmentation
Restoration of lost habitats
Sustainable land use practices
Unit 9.1: The Stratospheric Ozone Depletion
Troposphere VS Stratosphere
These are the two locations for ozone in our atmosphere
Troposphere- produces ozone from photochemical smogs, greenhouse gas effect (can be harmful)
Stratosphere - naturally occurring ozone that provides protection from UVB-UVC rays
Using that radiation to transform ozone (O3) to atmospheric oxygen (O2)
Antarctic Spring
Antarctic winters can create stratospheric clouds full of ice crystals
Crystals melt in the beginning of the spring
Chemical reactions convert less reactive chlorine into a more reactive form
Chlorine degrades ozone into atmospheric oxygen (O2)
The ozone layer thins
Chlorofluorocarbons (CFCs)
Refrigerant/coolant
Propellant
Some types of plastics
CFCs can escape and enter the stratosphere
UV light removes chlorine from CFCs
Free chlorine catalyzes the conversion of O3 to O2
Effects of Ozone Depletion
Thinning of ozone layers, especially at poles
Disrupts photosynthesis, both terrestrial and in phytoplankton
Disrupts food chains and food webs
Impacts populations of some organisms like amphibians
Impacts human health: skin cancer, cataracts
Unit 9.2: Reducing Ozone Depletion
Montreal Protocol - an international treaty that phased out the use of CFCs and their manufacture in 1987
They did this upon recognizing CFCs were thinning the ozone layers and harming the environment
However CFCs are persistent, so it will take decades for CFCs currently in the stratosphere to completely dissipate, allowing the ozone layer to fully repairable
HFCs (hydrofluorocarbons) replace CFCs
No chlorine to catalyze transformation of ozone into atmospheric oxygen
Powerful greenhouse gas
Unit 9.3: The Greenhouse Effect
The greenhouse effect occurs in the troposphere
The sun’s solar radiation warms the earth
Some energy is reflected, some energy is re-radiated as heat back into space
Some re-radiated heat is absorbed by greenhouse gasses in the troposphere, then emitted again toward the surface of the Earth as heat
The “greenhouse effect” helps to keep the Earth at a temperature that can support life
The greenhouse effect and the ozone layer are in two separate layers of the atmosphere
Greenhouse gasses
Carbon dioxide - CO2
Vast majority come from combustion, either from transportation or fossil fuels
Methane - CH4
Comes from enteric fermentation, natural gas and petroleum systems, and several other sources
Water vapor - H2O
Condenses and produces precipitation, does not spend much time in the atmosphere
Does not play a large role in the greenhouse effect
Nitrous Oxide - N2O
It is an agricultural source management issue
Chlorofluorocarbons (CFCs) - example: CF2Cl2
Both CFCs and HFCs are man made
Hydrofluorocarbons (HFCs)
Substitution for CFCs
Tropospheric Ozone - O3
Comes from photochemical smog
Carbon dioxide is a reference molecule for the greenhouse effect, so has a global warming potential (GWP) of 1
GWPs or various greenhouse gasses: CFCs/HFCs > ozone > nitrous oxide > methane > carbon dioxide
Carbon dioxide has the greatest overall impact on the greenhouse effect because of its concentration in the atmosphere
Human activities influence the concentration of various greenhouse gasses in the atmosphere
Unit 9.4: Increases in the Greenhouse Gasses
Greenhouse gasses that produce the greenhouse effect include carbon dioxide, methane, nitrous oxide, ozone, CFCs, HFCs, and water vapor
Concentrations of many greenhouse gasses have steadily increased in the atmosphere as a result of human activity
Increased greenhouse gasses have led to climate change
Sea Levels Rise
Land ice (example: continental glaciers, ice sheets) melts, adding to the volume of water in the ocean
Thermal expansion of the ocean, due to warming from climate change, increases the volume of the ocean
Disease vectors expand their range
Climate change impacts Ecological Populations
Habitat destruction
Loss of food source
Timing of food source availability changes
New temperatures beyond range of tolerance
New salinity beyond range of tolerance
Increased storm intensity
Increased possibility of fire
Impacted annual group behaviors timing of migration, hibernation
Climate Change Impacts Human Populations
Low-income populations
Occupational groups
People in certain locations
Pregnant women
People with pre-existing medical conditions
Children
Older adults
People with disabilities
Indigenous people
Climate Change Has Global Impact
Environmental Impacts
Changes in ocean salinity and temperature affect marine organisms at every trophic level in many ways
Changes in temperature affect terrestrial organisms at every trophic level in many ways
Impacts on Humans
Impacts include responses to temperature changes, access to food, access to fresh water, and changing land availability
Anthropogenic activities produce the additional greenhouse gasses that drive climate change
Many activities - individual actions, agriculture, industry - produce greenhouse gasses
Unit 9.5: Global Climate Change
Historical records about climate change
We have records over the past 800,000 years that tell us about regular periods of warming, cooling, and carbon dioxide increase and decrease
We get this information from ice cores in arctic areas
We can measure how much carbon dioxide is the ice and how melted it is can tell us about warming or cooling
Change in temperature could also cause a change in air circulation, global wind patterns, and soil quality
Current data shows that the Earth is warming, which is correlated with an increase in the concentration of greenhouse gasses in the atmosphere
Effects of climate change include rising temperatures, rising seas levels, and displacement of coastal populations
Rising Temperatures Melt Global Ice
Melting polar ice reveals darker soil and water (lower albedo than ice), which drives a positive feedback warming loop
Melting permafrost releases methane gas, which drives a positive feedback warming loop
Melting sea ice affects species that depend on the ice for habitat and food, such as polar bears and seals
Climate Change Leads to Changes in the World Ocean
Climate change leads to sea level rise
Benefit - new marine habitat created
Drawback - increasing depth of ocean impacts organisms that will no longer be in the photic zone
Climate change can alter ocean currents
Salinity and temperature changes impact water density, which can impact the ocean conveyor belt
Altered ocean currents can impacts terrestrial climate, especially in coastal areas
Unit 9.6: Ocean Warming
Ocean Warming - the global increase in ocean water temperatures
The amount of warming isn’t uniform across the globe - some ocean areas have warmed more quickly than others
Effects of Ocean Warming
Increase in greenhouse gasses can lead to a variety of environment problems
Rising sea levels from melting ice sheets and ocean water expansions
Thermal expansion of the ocean due to ocean warming causes rising sea levels and displacement of coastal populations due to flooding
Ocean warming affects marine species in a variety of ways
Loss of habitat
Negatively impacts hunting and feeding patterns
Can impact predator and prey interactions
Affects coastlines that impact species using both land and water resources
Can push communities out of the photonics
Impacts primary productivity of phytoplankton, the basis for marine food webs
Metabolic Changes
Marine species will not be able to escape to cooler areas
This could weaken organisms and cause them to die
Reduction of biodiversity and disruption of trophic structures
Reproductive Changes
Organisms weakened by thermal stress do not reproduce well
Many marine reproductive patterns are timed based on specific ocean temperatures - disruption of these temperature patterns leads to reproductive harm
Coral Bleaching
Warming temperatures stress the corals, they expel that algae that gives them color, giving them a bleached color
Can recover, but if conditions persist they will die
They are the foundation of highly biodiverse reef ecosystems, their loss will disrupt the trophic structure and has a negative impact on the marine ecosystem
Unit 9.7: Ocean Acidification
Ocean Acidification - the decrease of pH of ocean waters
The pH scale is logarithmic- each jump of one on the scale is a tenfold increase, so about a 30% increase
Like ocean warming, ocean acidification is due primarily to greenhouse gas concentrations in the atmosphere, specifically carbon dioxide
The more CO2 is released into the atmosphere, the more the oceans absorb, lowering their pH through specific chemical reactions
Anthropogenic activities that contribute to ocean acidification are those that lead to increased CO2, including
Burning/combustion of fossil fuels
Vehicle emissions
Deforestation
When CO2 is absorbed by seawater a series of chemical reactions occur which result in an increase in hydrogen ions
The water combines with the carbon dioxide to create carbonic acid, which is a weak acid. The carbonic acid then dissociates into hydrogen ions and bicarbonate ions
The greater the concentration of hydrogen ions, the lower the pH of the water (more acidic)
Effects of Ocean Acidification
Increased concentration of hydrogen ions bond with available carbonate ions in seawater, a bicarbonate ion is formed
Marine organism can’t extract this carbonate, making it difficult for them to build shells and exoskeletons
Corals need free carbonate ions to form skeletons as well
This loss of calcium carbonate is very harmful for these organisms
Oceans absorb carbon dioxide, the more carbon dioxide present, the more they absorb, which warms the ocean
Unit 9.8: Invasive Species
Invasive Species - an alien species whose introduction does or is likely to cause economic or environmental harm or harm to human health
Invasive species can be beneficial sometimes, but they are considered invasive when they threaten native species in some manner
Non-native species may be introduced into ecosystems accidentally or purposefully
They tend to be niche, generalist, r-selected species
They can withstand a wide variety of abiotic conditions
Can survive on a lot of food
Can produce a lot of offspring in a short time, but there is little parental care
Exponential growth, mature very quickly
Not every species that is introduced to an ecosystem becomes invasive
Insavises have a competitive advantage over natives
How are invasive species spread?
Transport of lumber and firepower
Ballast water in ships, movement of boats and boat trailers, international travel as well
Movement of wind and water
On the fur of other animals
How to Control the Spread
Clean boats and boat trailers
Prevent dumping of aquariums and release of exotic pets
Clean hiking gear before going into a new hiking area
Keep firewood wear it was cut to prevent spread of wood-borne pathogens
How can we Control the Spread?
Introduce a competitor species
Introduce a predator species
Introduce a virus
Physically remove them
Release a pesticide to control their spread
Unit 9.9: Endangered Species
Factors that Lead to Extinction
As habitats are lost or altered globally, many species are threatened with extinction
Extensive Hunting
Poaching is illegal hunting, killing or capturing of animals for sale of profit
Animals are hunted for food, prized body parts, traditional medicinal uses
Medical research purposes
Sport
Limited Diet & Habitat
Species who are niche specialists are generally at greater risk of extinction
These species typically need specific materials for their diet and habitat to survive, and do not reproduce quickly
Outcompeted by Invasive Species
Invasive species have little diet and habitat requirements, so they can out-adapt and out-compete some native species that have a limited lifestyle
The biological and behavioral traits of a species will determine their risk of extinction when exposed to environmental change
Species that can adapt to these changes better have less of a chance of becoming extinct
Adaptation requires genetic diversity
Species can migrate to a more favorable environment to avoid extinction, but this could also raise competition in the new environment
Selective Pressure - any external factor that changes the behavior and fitness of organisms within an environment
Examples include
Resource Availability
Food
Water
Habitat
Mates
Abiotic Environmental Condition
Temperature
Humidity
Tree cover
Salinity
Biological Factors
Pathogens (viruses, bacteria, and fungi)
Diseases
Selective pressure determine which genetic and behavioral traits are favorably adapted to the environment and which aren’t
Pressures will change in changing environments, so traits that were once advantageous in an environment may not continue to be so
Competition can occur within or between species in an ecosystem where there are limited resources
Species seek to limit competition because it’s biologically costly
Competition consumes important metabolic resources, so competitive strategies generally evolve to a limit resource conflicts through resource partitioning
Organisms may compete within their own species resources, such as
Territory
Food
Mates
Habitat
Competition can become intense enough to eat to a species’ endangerment or extinction when:
Trophic relationships are disrupted
There is increased competition invasive species
Resources have become increasingly scarce due to habitat loss or climate change
Strategies to Protect Species
Legislation - (with enforcement) is one primary way to help protect endangered species
Criminalizing poaching and instituting steep fines and/or punishment for poachers can help curb this practice
Laws prohibiting the harming of endangered species and their habitats, or trade in endangered species
The Lacey Act
The Endangered Species Act
The Marine Mammal Protection Act
CITES (the Convention on International Trade in Endangered of Wild Fauna and Flora)
The establishment of protected areas for species, such as wildlife refuges or national parks
Enforcement of conversation practices help as well
Unit 9.10: Human Impacts on Biodiversity
HIPPCO - an acronym regarding the main factors leading to decreases in biodiversity
Habitat destruction
Invasive species
Population growth
Pollution
Climate change
Over exploitation
Habitat Fragmentation
Occurs when large habitats are broken up into smaller, isolated area
Caused by construction of roads and pipelines, clearing of land for agriculture, and logging
Not all species are equally impacted by this
Generalists who thrive in abiotic conditions, or species that thrive in areas where two habitats meet can adapt to fragmentation
Specialists with specific habitat requirements suffer more
Generally decreases biodiversity despite some generalist species having an increase in population
Climate Change and Habitat Loss
Global climate change plays a large role in habitat loss
As average global temperature rises, habitats may be lost due to
Coastal inundation from melting ice and permafrost
Rising sea levels due to thermal expansion
Changes in precipitation patterns due to changing atmospheric and oceanic circulation patterns
Climate change has been most intense in northern latitudes; as warming trends continue, these areas will be at most risk for habitat loss and loss of biodiversity
Domestication and Loss of Biodiversity
Humans have been domesticating organisms for thousands of years
Domestication - involves artificial selection, in which organisms with the most desirable traits for humans are crossbred to enhance the occurrence of that in the species
Many domesticated species are managed for economic returns, and provide humans with
Food
Medicine
Labor
Pollination Services
When humans assume responsibility for the reproduction and selection of traits in another species, genetic diversity will be reduced
Domestication for economic return leads to a loss of biodiversity
Examples of this can be seen in domestic livestock (cattle, sheep, goats, pigs), honeybees, and the agricultural practice of monocropping
Strategies to Mitigate Biodiversity Loss
As global climate change intensifies, it is important that we address current and future losses of biodiversity. Strategies include:
The creation of protected areas, such as wildlife refuges and parks
The creation of habitat corridors to reduce the negative effects of habitat fragmentation
Restoration of lost habitats
Sustainable land use practices