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Excellent and Exciting Ecology
Chapter 52 ~ An Introduction to Ecology and the Biosphere I am the Lorax. I speak for the trees. I speak for the trees, for the trees have no tongues.
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Vocabulary Ecology: the study of interactions between organisms and their environments
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Global Climate Climate is the long term prevailing weather in an area
Temperature, precipitation, sunlight and wind Macroclimate – global, regional patterns Microclimate – very fine, localized pattern (i.e. conditions beneath a fallen log
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Intensity and angle of sunlight affect climate
Sunlight strikes tropics most directly More heat and light per unit of Surface area (SA) Poles (higher latititude) – strikes at oblique angle What are some differences in the ecology of tropics vs. poles? 5
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Air Circulation and Wind Patterns affect climate
Solar radiation near equator sets up patterns of air circulation and precipitation Remember – high temp = evaporation – warm air rises and loses water (rain) Dry Air mass falls at 30° - (desert here) Air flows toward poles (60 °) and release water again Dry air flows at poles leaving cold, dry conditions 6
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Ocean currents influence climate along coasts
Ocean currents heat or cool air masses coasts – generally wetter than inland at same latitude High specific heat of water helps moderate climate
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Mountains affect sunlight, temperature and rainfall
Windward side - air rises and releases moisture – causes leeward side – drier South facing slopes in N. hemisphere get more sunlight – warmer and drier 9
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Summarize how air circulation, sunlight, and ocean currents can affect the global climate.
Predict what might happen if there were a change in the precipitation level in a certain area. (long lasting)
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American Beech case study
Seeds do not have wings and have not moved rapidly Northward since the last ice age (only .2 km per year). As Earth temps increase, the distribution will have to shift north in order for the trees to survive (7-9 km per year) What might happen to the tree population if human’s do not assist in the movement to new habitat
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Biomes Major terrestrial or aquatic life zones
Characterized by vegetation type and physical environment
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Tropical Forest Found near equator
Rainfall constant ( cm annually) Air Temperature high year-round (25-29˚ C) Vertical layering with canopy
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Desert 30 ˚ North and south latitude
Precipitation low and variable (less than 30 cm per year Temp varies by season and daily (not always hot in the desert) Adaptations include water conservation/storage
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Savanna Found near equator Rainfall averages 30-50 cm per year
Dry season can be 8-9 months Temp warm year round Scattered trees, many grasses (Think Lion King )
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Chaparral Mid-latitude coastal regions Seasonal Precipitation
Rainy winters, long dry summers Shrubs, small trees Adaptations to drought and fire
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Temperate Grassland Seasonal precipitation Dry winters, wet summers
Periodic drought is common Cold winters, hot summers Grasses Large grazing mammals (bison)
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Coniferous Forest (Taiga)
Northern North America and Eurasia Cold, long winters, hot summers Cone bearing trees Migratory birds, moose, brown bears
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Temperate Broadleaf Forest
Mid-latitudes in Northern hemisphere cm of rain annually Cold winters, hot humid summers Closed canopy Deciduous trees (lose leaves in winter)
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Tundra Arctic regions High winds, low temperatures
20-60 cm of precipitation Long, cold winters, short summers with low temperatures Permafrost – permanently frozen layer of soil
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Aquatic Biomes Marine (salt water) – averages 3% salt concentration
Fresh Water – less that 0.1% salt concentration
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Vertical Stratification
Photic zone – light for photosynthesis Aphotic zone – little light available Benthic Zone – bottom of all aquatic zones Benthos – community of organisms in benthic zone Detritus – dead organic matter that falls down from upper zone – gives food to benthos Thermocline – narrow layer of abrupt temperature change – cyles oxygen and nutrients
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Standing Bodies of Water
Lake Classification Oligotrophic – nutrient poor and oxygen rich Eutrophic – nutrient rich and oxygen poor in deepest areas
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Wetlands Habitat that is inundated with water at least some of the time •Plants adapted to water saturated soil Low oxygen levels
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Moving Bodies of Water Rivers and streams
Nutrient content depends on overhanging vegetation – usually high oxygen content because of turbulence Headwater – cold, clear, turbulent Downstream – warmer, more turbid (cloudy)
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Estuary Transition area between river and sea
Seawater enters during rising tide and returns to sea when tide falls Organisms must be able tolerate both salt/fresh water
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Intertidal Zone Happens twice daily on marine shores
Variation in temperature, salinity and air exposure
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Ocean Pelagic Open blue water constantly mixed by wind driven oceanic currents 70% of Earth’s surface
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Coral Reefs Formed from calcium carbonate skeletons of corals
Found mainly in tropical marine areas Need high oxygen levels
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Marine Benthic Zone Seafloor below the surface waters of the coastal zone and pelagic zone Receives no sunlight Water temperature declines with depth Chemoautotrophic prokaryotes are producers in deep sea hydrothermal vents
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Interactions Between Organisms and Environment
Biotic – living components of the environment (other species) that can affect microclimate Predation Parasitism Competition Disease
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Interactions Between Organisms and Environment
Abiotic: non-living components that can affect microclimate Temperature Light Water Nutrients Salinity Rocks/Soil
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Dispersal Movement of individuals away from their area of origin
Contributes to global distribution of organisms
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Urchin case study Question – does feeding by sea urchins limit seaweed distribution? Experiment – Tested %seaweed cover in an area under different conditions: Both limpets and urchins present Only removing limpits Only removing urchins Removing both limpits and urchins
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Which scenario cause the greatest increase in %seaweed cover?
Which organism (limpit or urchin) affected the % seaweed cover the most? Write two sentences using the graph to explain your answer.
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