CH 3: Ecosystem Ecology and Biomes
Ecosystem: a particular location on Earth distinguished by its particular mix of interacting biotic (living) and abiotic (non-living) components
Photosynthesis and Respiration
Producers: organisms that use the energy of the sun to produce usable forms of energy; also known as autotrophs
Consumers: organisms that obtain energy by feeding on other organisms, including both herbivores and carnivores; also known as heterotroph
Photosynthesis: producers use solar energy to convert carbon dioxide and water into glucose
Cellular Respiration: the process by which organisms convert glucose and oxygen into carbon dioxide, water, and energy in the form of ATP.
Trophic Levels, Food Chains, and Food Webs
Trophic levels: successive levels of organisms consuming one another
Food chain: sequence of consumption from producers through tertiary consumers
Food web: a complex network of interrelated food chains that illustrates how energy and nutrients flow through different organisms in an ecosystem.
Producers
Primary consumers (herbivores): plant and algae eating animals (e.g. zebras, grasshoppers, and tadpoles)
Secondary consumers (carnivores): heterotrophs that obtain energy by eating other consumers (e.g. lions, hawks, and rattlesnakes)
Tertiary consumers: carnivores that eat secondary consumers (e.g. bald eagles)
Scavengers: carnivores that consume dead animals
Detritivores: organisms that specialize in breaking down dead tissue and waste products into smaller particles
Ecosystem Productivity
Gross Primary productivity (GPP): the total amount of energy captured by producers through photosynthesis over a specific time period.
Net Primary Productivity (NPP): energy captured (GPP) minus the energy respired by producers
GPP is revenue while NPP is profit
Energy Transfer Efficiency and Trophic Pyramids
Energy in an ecosystem is measured in terms of biomass
Biomass: total mass of all living matter in a specific area; represented using a trophic pyramid
Standing Crop: amount of biomass present in an ecosystem at a given time
Ecological efficiency: the proportion f consumed energy that can be passed from one trophic level to another
Trophic Pyramid: representation of distribution of biomass among trophic levels
Matter Cycles
Biosphere: the global sum of all ecosystems, encompassing both terrestrial and aquatic environments.
Earth can be divided into four compartments: earth (soil and rock), water, and atmosphere, and living things
All matter cycles involve the movement of materials from one compartment to other compartments
Biogeochemical Cycles: the cycling of matter through the biosphere
Bio: life
Geo: earth
Chemical: matter
Hydrologic Cycle: The movement of water through the biosphere
Nitrogen Cycle: The process by which nitrogen is converted between its various chemical forms as it circulates among the atmosphere, terrestrial, and marine ecosystems.
Carbon Cycle: The process involving the movement of carbon among the atmosphere, terrestrial organisms, and oceans, which plays a crucial role in regulating climate and supporting life.
Ecosystem and Disturbance
Disturbance: an event caused by physical, chemical , or biological agents that results in changes in population size or community composition
Natural ecosystem disturbances include hurricanes, ice storms, tsunamis, volcanic eruptions, and forest fires
Anthropogenic ecosystem disturbances include human settlements, agriculture, air and water pollution, and clear-cutting of forests, as well as strip mining
Resistance vs. Resilience
Resistance: a measure of how much disturbance an ecosystem can tolerate without significantly changing the flows of energy and matter
Resilience: the rate at which an ecosystem returns to its original state after a disturbance
Watershed Studies
Watershed: all of the land in a given landscape that drains into a particular stream, river, lake, or wetland
Weather: the short term, local conditions of the atmosphere (e.g. temperature, humidity, clouds, precipitation, wind speed, and atmospheric pressure)
Climate: average weather that occurs in a given region over a long period (typically several decades)
Earth’s Atmosphere
Troposphere: layer closest to Earth’s surface extending roughly 10 miles above Earth
Stratosphere: above the troposphere extending roughly 10-31 miles
Atmospheric Convection Currents
Density: less-dense air rises, denser air sinks
Water vapor capacity: warm air has a higher capacity for water vapor than cold air
Adiabatic Heating or Cooling
As air rises, it expands and cools adiabatically, leading to cloud formation and precipitation, while descending air compresses and warms, inhibiting cloud development.
Latent Heat Release: This process occurs when water vapor condenses into liquid water, releasing heat into the surrounding environment, which can further influence weather patterns and climate dynamics.
Earth’s Rotation and the Coriolis Effect
Coriolis Effect: the deflection of an object’s path due to Earth’s rotation
Prevailing winds are produced by a combo of atmospheric convection currents and the Coriolis effect
Ocean Currents
Driven by a combo of temp, gravity, prevailing winds, the Coriolis effect, and the locations of continents
Warm water expands and rises
Gyres: Large-scale circular ocean currents that are influenced by the Earth's wind patterns and rotation, resulting in the movement of water in a clockwise direction in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.
Upwelling: The process where cold, nutrient-rich water rises to the surface, primarily driven by the action of winds and ocean currents, significantly enhances productivity in marine ecosystems.
Thermohaline Circulation: A large-scale ocean circulation pattern driven by differences in water temperature and salinity, which plays a crucial role in regulating global climate and transporting nutrients across the world's oceans.
El Nino
Southern Oscillation ENSO
Every 3-7 years, Earth’s atmosphere and ocean surface currents interact in the tropical Pacific Ocean to reverse direction
La Nina
Opposite weather patterns compared to El Niño, such as increased rainfall in the western Pacific and drought conditions in the eastern regions.
Robert Harding Whittaker (1920-1980)
American Ecologist
Cornell University
Biomes: Large geographic regions on Earth with a unique climate, plants (flora), and animals (fauna) that are adapted to those specific conditions
Tundra
Cold, treeless biome with low-growing vegetation
Soil is completely frozen in winter
Short, four month growing season
Permafrost: underlying subsoil is permanently frozen
Boreal Forest
Sometimes called Taiga
Mostly coniferous (cone-bearing) evergreen trees
Found between about 50 and 60 degrees North in Europe, Russia, and N. America
Plant growth more constrained by low temp than precipitation
Soil id nutrient-poor due to slow decomposition
Temperate Rainforest
Moderate temps and high precipitation
Coastal biome ocean currents moderate temp fluctuations and provide water vapor
12 month growing season where winters are rainy and summers are foggy
Mild temps and high precipitation supports growth of huge trees
Temperate Seasonal Forest
Receive over 1 meter (39 inches) of precipitation annually
Found in the Eastern U.S., Japan, China, Europe, Chile, and Eastern Australia
Dominated by broadleaf deciduous trees such as beech, male, oak, and hickory
Warmer temps = more decomposition so soils generally contain more nutrients than those of boreal forests
Woodland/Shrubland
Mediterranean Climate
Hot, dry summers and mild, rainy winters
12 month growing season but plant growth constrained by low summer precipitation cool winter temperatures
Plants of this biome are well adapted to both fire and drought
Temperate Grassland/Cold Desert
Great plains of N. America, S. America, Central Asia, and Eastern Europe
Cold, harsh, winters and hot, dry, summers
Dominated by grasses and non-woody flowering adapted to wildfires and frequent grazing
Tropical Rainforest
Located between 20 degrees north and south of the equator
Central and S. America, Africa, SE Asia, and NE Australia
Frequent rainfall, warm and wet with steady temps
More biodiversity than any other terrestrial biome (2/3rds of Earth’s terrestrial species)
Tropical Seasonal Forest/Savanna
Warm temps and distinct wet and dry seasons
Central America, Atlantic coast of S. America, southern Asia, in NW Australia, sub-Saharan Africa
Fairly fertile soil but low precipitation constraints plant growth
Grasses and scattered deciduous trees are common
Subtropical Desert
30 degrees N and S with hot temps and extremely dry conditions
Mojave Desert in SW U.S., Sahara, Middle East, Great Victoria Desert of Australia
Cacti, euphroes, and succulent plants
Aquatic Biomes
Categorized by salinity, depth, and water flow
Lakes and Ponds
Littoral Zone: the shallow area of soil and water near the shore where algae and emergent plants grow
Limnetic Zone: open water, where rooted plants can no longer survive. Phytoplankton are the only photosynthetic organisms. This zone extends to as deep as sunlight can penetrate
Profundal Zone: the zone where sunlight cannot penetrate and therefore producers cannot survive
Benthic Zone: muddy bottom of a lake or pond beneath the limnetic and profundal zone
Salt Marshes: one of the world’s most productive biomes
Mangrove Swamps
Found along tropical and subtropical coasts and contain trees whose roots are submerged in water
Mangrove trees are salt tolerant and help protect the coastlines from erosion and storm damage
Intertidal Zone
Narrow band of coastline that exists between the levels of high ride and low tide
Waves that crash onto the shore in this biome can make it a challenge for organisms to hold on and not get washed away
Coral Reefs
Found in warm, shallow water beyond the shoreline
Earth’s most diverse marine biome
Found in water that is relatively poor in nutrients and food; depends on coral-algae mutualism
Coral bleaching: when the algae inside the coral dies due to combo of disease and environmental change
The Open Ocean
The depth that light can penetrate in the open ocean is dependent on the amount of sediment and algae suspended in the water
Photic Zone: the zone that receives enough light to allow photosynthesis to occur
Aphotic Zone: the deeper water that lacks sufficient light for photosynthesis
Chemosynthesis: the process that occurs in the aphotic zone when some species of bacteria use methane and hydrogen sulfide to generate energy