Chernoybl
Minamata disease
Silent spring
Millennium Ecosystem Assessment
Tropical rainforest
Poison dart frog
Location: Near equator (tropics of Cancer (23.5°N) and Capricorn (23.5°S))
Temperature: Constant high (21-30°C)
Precipitation: High (2000-10000 mm annually)
Productivity: High
Species Diversity: High
Example: Amazon, South America
Human Impacts:
- 38% of the remaining Amazonian rainforest is suffering from degradation
- 20% of the Amazon rainforest has been destroyed since the 1970s
- 36% of Earth’s tropical rainforests remain intact
Temperate Rainforest
Human Impacts:
- Logging
- Cut and burn trees to generate electricity
- Paper industry
- Pollution (industrial activities, agricultural runoff, & urbanization)
- Lead to the decline of s sensitive species and disrupt ecological interactions.
Boreal Forest
Tundra
Location: Places with high latitudes and low insolation (60°-75° North and South)
Temperature: Extremely low (often snowing, -40 to 18°C)
Precipitation: Low (150 to 250 mL/yr)
Productivity: Low
Example: Iceland, Europe
Reindeer moss, thick shrub absorbs moisture
Human Impacts:
Climate change and global warming, which are causing the permafrost to thaw and the tundra to shrink
Desert
Location: 30 degrees North and South of the equator.
Temperature: Extremely high (45-49 degrees Celcius)
Precipitation: Low (under 250mm annually)
Productivity: Very low
Species Diversity: Low
Example: Sahara, Africa
Scorpion
Tropical Coral Reef
Human Impacts:
- Climate change
- Declining water quality
- Overfishing
- Pollution
- Unsustainable coastal development
- By 2050, 70-90% of coral will die (coral bleaching)
- Corals lose their symbiotic algae (zooxanthellae) which provide nutrients through photosynthesis. When they are released due to environmental stresses, corals lose their color and die.
Hydrothermal Vents
Human Impacts:
- Deep-sea mining
- Climate change
- Pollution
Savannah
Temperate Grasslands
Tri-Cellular Atmospheric Wind Model
Made up of three air masses that influence atmospheric movement and heat energy redistribution
Hadley Cell
- Largest cell (0° to 40° N and S)
- Trade winds travel from the tropical region to the equator
- When trade winds meet, hot air rises, forming thunderstorms
- Air travels higher and becomes cooler (sinks to subtropical region)
- Dry, cloudless air is warmed by the sun (Hot Deserts)
Ferrel Cell
- Middle cell (edge of Hadley cell to 70° N and S)
- Moves in the opposite direction
- Air joins with Hadley and Polar Cell (unsettled weather)
Polar Cell
- smallest/weakest cell (edge of Ferrel cell to 90° N and S)
- Air is cold and sinks = high pressures
- Air is warmed and rises to return to the poles
Primary succession
Surtsey, Iceland
- Formed due to an undersea eruption in 1963
- 30 plant species had been established by 2008
- Forestation on the island may require 300-2000 years
Secondary Succession natrual
Mount St Helen, US
- Volcanic eruption in 1980 caused disturbance in meadows and forests. This destroyed the community
Secondary Succession Due to Human Impact
Heather Moorlands, Northern England
- Logging in the Middle Ages removed deciduous woodland
Zonation
Constructive/Divergent Plate Tectonics
Mid-Atlantic Ridge
1. Convection currents rise & spread outwards when they reach the top of the mantle
2. Plates are dragged apart
3. Magma from the mantle rises up through the opened cracks
4. Ocean ridges and volcanoes are formed
5. Magma cools, forming new ocean crust
Convergent Plate Tectonics
(Continental-Continental crust)
Himalayas
1. Mantle convection currents converge & sink
2. Plates are pushed together
3. Plates crumble up (forms mountains)
Conservative Plate Tectonics
San Andreas fault of California
- No crust is created or destroyed
- Plates move past each other
Convergent Plate Tectonics
(Oceanic-Continental crust)
Andes Mountains/Peru Trench
1. Plates move toward each other
2. Denser plate subducts (oceanic plate)
3. Causes earthquakes & volcanic eruptions
Convergent Plate Tectonics
(Oceanic-Oceanic crust)
Lemnos (Island of Hephaestus)
1. One plate sinks beneath the other
2. Subduction zone forms along the boundary where the denser plate sinks into the mantle
3. Plate is heated
4. Plumes of molten magma rise upward through the top plate
5. Volcanic island is formed
Hot Spot
Hawaiian Ridge
1. A random spot where magma rises from the core boundary
2. magma rises (thinks the plate above it)
3. Shield volcano is formed