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The Biosphere

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Earth rotates faster under the air at the equator than it does at the poles ... Openings in ocean floor that spew mineral-rich, superheated water ... – PowerPoint PPT presentation

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Title: The Biosphere


1
The Biosphere
  • Biology 1030
  • Principles of Biology

2
Climate
  • Average weather condition in a region
  • Affected by
  • amount of incoming solar radiation
  • prevailing winds
  • elevation

3
The Atmosphere
  • Three layers
  • Outer mesosphere
  • Middle stratosphere (includes ozone layer)
  • Inner troposphere (where air is warmed by the
    greenhouse effect)

4
Warming the Atmosphere
  • Solar energy warms the atmosphere and sets global
    air circulation patterns in motion

5
Rotation and Wind Direction
  • Earth rotates faster under the air at the equator
    than it does at the poles
  • Deflection east and west

6
Seasonal Variation
  • Northern end of Earths axis tilts toward sun in
    June and away in December
  • Difference in tilt causes differences in sunlight
    intensity and day length
  • The greater the distance from the equator, the
    more pronounced the seasonal changes

7
Varying Temperatures
8
Pollutants
  • Substances with which an ecosystem has had no
    prior evolutionary experience
  • No adaptive mechanisms are in place to deal with
    them

9
Ozone Thinning
  • In early spring and summer ozone layer over
    Antarctica thins
  • Seasonal loss of ozone is at highest level ever
    recorded

10
Effect of Ozone Thinning
  • Increased amount of UV radiation reaches Earths
    surface
  • UV damages DNA and negatively affects human
    health
  • UV also affects plants, lowers primary
    productivity

11
Air Pollutants
  • Carbon oxides
  • Sulfur oxides
  • Nitrogen oxides
  • Volatile organic compounds
  • Photochemical oxidants
  • Suspended particles

12
Protecting the Ozone Layer
  • CFC production has been halted in developed
    countries, will be phased out in developing
    countries
  • Methyl bromide will be phased out
  • Even with bans it will take more than 50 years
    for ozone levels to recover

13
Thermal Inversion
  • Weather pattern in which a layer of cool, dense
    air is trapped beneath a layer of warm air

cooler air
normal circulation
cool air
warm air
cool air
warm inversion air
cool air
14
Industrial Smog
  • Gray-air smog
  • Forms over cities that burn large amounts of coal
    and heavy fuel oils mainly in developing
    countries
  • Main components are sulfur oxides and suspended
    particles

15
Photochemical Smog
  • Brown-air smog
  • Forms when sunlight interacts with components
    from automobile exhaust
  • Nitrogen oxides are the main culprits
  • Hot days contribute to formation

16
Acid Deposition
  • Caused by the release of sulfur and nitrogen
    oxides
  • Coal-burning power plants and motor vehicles are
    major sources

17
Ocean Currents
  • Upper waters move in currents that distribute
    nutrients and affect regional climates

18
Rain Shadow
  • Air rises on the windward side, loses moisture
    before passing over the mountain

19
Coastal Breezes
  • Breeze blows in direction of warmer region
  • Direction varies with time of day

20
Biogeographic Realms
  • Six areas in which plants and animals are
    somewhat similar
  • Maintain their identity because of climate and
    physical barriers that tend to maintain isolation
    between species

21
Biomes
  • Regions of land characterized by habitat
    conditions and community structure
  • Distinctive biomes prevail at certain latitudes
    and elevations

22
nearctic
neotropical
23
Hot Spots
  • Portions of biomes that show the greatest
    biodiversity
  • Conservationists are working to inventory and
    protect these regions
  • 24 hot spots hold more than half of all
    terrestrial species

24
Deserts
  • Less than 10 centimeters annual rainfall, high
    level of evaporation
  • Tend to occur at 30 degrees north and south and
    in rain shadows
  • One third of land surface is arid or semiarid

25
Dry Shrublands and Woodlands
  • Semiarid regions with cooler, wet winters and
    hot, dry summers
  • Tend to occur in western or southern coastal
    regions between latitudes of 30 and 40 degrees

26
Forest Biomes
  • Tall trees form a continuous canopy
  • Evergreen broadleaves in tropical latitudes
  • Deciduous broadleaves in most temperate latitudes
  • Evergreen conifers at high temperate elevations
    and at high latitudes

27
Arctic Tundra
  • Occurs at high latitudes between polar ice cap
    and boreal forests
  • Summers are short and snow-free
  • Permafrost lies beneath surface, causes
    waterlogging in summer
  • Nutrient cycling is very slow

28
Alpine Tundra
  • Occurs at high elevations throughout the world
  • No underlying permafrost
  • Plants are low, cushions or mats as in arctic
    tundra

29
Lakes
  • Bodies of standing freshwater
  • Eutrophic lake is shallow, nutrient-rich, has
    high primary productivity
  • Oligotrophic lake is deep, nutrient-poor, has low
    primary productivity

30
Lake Zonation
LITTORAL
LITTORAL
LIMNETIC
limit of effective light penetration
PROFUNDAL
31
Thermal Layering
  • In temperate-zone lakes, water can form distinct
    layers during summer

wind
THERMOCLINE
32
Seasonal Overturn
  • In spring and fall, temperatures in the lake
    become more uniform
  • Oxygen-rich surface waters mix with deeper
    oxygen-poor layers
  • Nutrients that accumulated at bottom are brought
    to the surface

33
Eutrophication
  • Enrichment of a body of water with nutrients
  • Can occur naturally over long time span
  • Can be triggered by pollutants

34
Estuary
  • Partially enclosed area where saltwater and
    freshwater mix
  • Dominated by salt-tolerant plants
  • Examples are Chesapeake Bay, San Francisco Bay,
    salt marshes of New England

35
Mangrove Wetlands
  • Tropical saltwater ecosystem
  • Form in nutrient-rich tidal flats
  • Dominant plants are salt-tolerant mangroves
  • Florida, Southeast Asia

36
Coral Reefs
  • Develop in clear, warm waters near coasts or
    around volcanic islands, mainly between latitudes
    25 north and south
  • Coral bleaching is on the rise occurs when
    sea temperatures rise

37
The Open Ocean
38
Phytoplankton
  • Floating or weakly swimming photoautotrophs form
    the base for most oceanic food webs
  • Ultraplankton are photosynthetic bacteria

39
Deep Ocean Food Webs
  • Regions too dark for photosynthesis
  • Marine snow supports a detrital food web
  • Organic matter drifts down from shallower water
  • Diverse species migrate up and down in water
    column daily

40
Hydrothermal Vents
  • Openings in ocean floor that spew mineral-rich,
    superheated water
  • Primary producers are chemoautotrophic bacteria
    use sulfides as energy source
  • Life may have originated in similar conditions on
    early Earth

41
Upwelling
  • Upward movement of water along a coast replaces
    surface waters that move away from shore

42
Cholera Connection
  • Cholera outbreaks are correlated with rises in
    sea temperature
  • Dormant stage of causative organism lives in
    copepods
  • Copepod population increases when phytoplankton
    increase in warming seas
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