π UNIT 9 NOTES (Biodiversity, Ozone, Climate Change)
π± The 6th Mass Extinction
Scientists believe Earth is currently in a 6th mass extinction
About 1,000 species lost per year
Main cause: human activity (habitat destruction, pollution, etc.)
𧬠Biodiversity & Species Categories
Key Definitions
Extinct species: no individuals left
Threatened species: likely to become endangered soon
Near-threatened species: may become threatened in future
Least concern species: widespread and abundant
Endemic species: found only in one specific area
𧬠Importance of Genetic Diversity
High genetic diversity = better survival
Low diversity β harder to:
adapt to environmental changes
resist diseases
π Value of Biodiversity
Types of Value
Intrinsic value: value just for existing (ethical/moral)
Instrumental value: usefulness to humans
Ecosystem Services
Provisioning: resources we use (food, medicine)
Regulating services: natural processes (climate, water cycles)
Support systems:
pollination (bees, birds, bats)
pest control
β HIPPCO (Causes of Biodiversity Loss)
H: Habitat loss
I: Invasive species
P: Pollution
P: Population growth
C: Climate change
O: Overharvesting
πΏ Invasive Species
Definitions
Exotic species: outside native range
Invasive species: spreads rapidly and harms ecosystem
Examples
Kudzu vine: blocks sunlight, kills plants
Zebra mussel: clogs pipes, outcompetes natives
Buffel grass: steals water from native plants
Silver carp: crowds out native fish
π Environmental Laws & Protection
CITES: controls trade of endangered species
Red List: tracks extinction risk
Lacey Act: bans illegal wildlife trade
Endangered Species Act (ESA): protects species & habitats
Marine Mammal Protection Act (1972): protects marine mammals
NEPA (1970): environmental impact assessments
OSHA (1970): worker safety from hazards
π³ Protected Areas
Biosphere reserve: protected land with zones
Core zone: most protected, highest biodiversity
Buffer zone: limited human activity
Transition zone: human use allowed
β OZONE DEPLETION (from your slides)
π Stratospheric Ozone
Protects Earth from UV radiation
Essential for life
β Causes
CFCs (chlorofluorocarbons):
used in aerosols, refrigerators
break down ozone layer
β Effects
More UV radiation reaches Earth
Causes:
skin cancer & cataracts (humans)
plant damage β reduced photosynthesis
π‘ CLIMATE CHANGE
π¬ Greenhouse Gases
Carbon dioxide (COβ)
Methane (CHβ)
Nitrous oxide (NβO)
Water vapor
CFCs
Key Ideas
COβ = most common
Methane = much stronger than COβ
NβO = long-lasting (100+ years)
CFCs = extremely powerful
π Evidence of Climate Change
Rising COβ levels (Keeling Curve)
Increasing global temperatures
Ice cores show past cooler climates
π Consequences
Rising sea levels (melting ice + expansion)
Changing migration patterns
Altered plant flowering times
More droughts
Spread of diseases
π Ocean Impacts
Ocean Warming
caused by greenhouse gases
leads to:
habitat loss
coral bleaching
Ocean Acidification
COβ absorbed β lowers pH
harms coral (canβt build shells)
π Feedback Loops
Positive feedback: amplifies change (worsens warming)
Negative feedback: reduces change (stabilizes system)
Example:
Ice melts β less reflection β more heat absorbed β more melting
π Climate Policies
Kyoto Protocol:
aimed to reduce emissions
U.S. signed but never ratified
Cap-and-Trade:
companies buy/sell pollution permits
Carbon sequestration:
storing carbon to reduce emissions
π° Economics & Environment
Kuznets Curve:
pollution increases β then decreases as income rises
GDP:
total value of goods/services in a country
π Worldviews
Anthropocentric: human-centered
Biocentric: all living things have value
Ecocentric: ecosystems as a whole matter
π± Sustainability
Stewardship: caring for Earth for future generations
Triple Bottom Line:
Profit
People
Planet
πΎ Sources of Greenhouse Gases
Nitrous Oxide
Human: agriculture
Natural: wet soils
Carbon Dioxide
Human: fossil fuels
Natural: volcanoes, decomposition
Methane
Human: livestock, rice fields
Natural: wetlands
CFCs
Human only: aerosols, foam
Water Vapor
Natural: evaporation
π§ Quick Study Tips
HIPPCO = main causes of biodiversity loss
CFCs = ozone depletion
COβ = climate change driver
Biodiversity = stability
β How Photochemical Smog Forms
1. Start with Primary Pollutants
These are released directly into the air:
Nitrogen oxides (NOβ) β from cars, power plants
Volatile organic compounds (VOCs) β from gasoline, paints, industrial chemicals
2. Sunlight Triggers Reactions
UV radiation from the sun hits these pollutants
This provides energy for chemical reactions
3. Ozone Formation (Secondary Pollutant)
NOβ (nitrogen dioxide) breaks apart in sunlight
This leads to formation of ground-level ozone (Oβ)
4. More Secondary Pollutants Form
Reactions with VOCs create:
Ozone (Oβ)
PANs (peroxyacyl nitrates)
Other oxidants
These together = photochemical smog