Chapter 52
Ecology is the study of interactions between organisms and the environment
Observations and experimentation are used in modern ecology
Rediscovery of the harlequin toad in Costa Rica raised questions about environmental factors and population size
Ecology can be studied at various levels
Global ecology: examines energy and material influence on organisms throughout the biosphere
Landscape ecology: focuses on connected ecosystems and the interchange of energy and materials
Ecosystem ecology: studies individual ecosystems, including biotic and abiotic components, energy flow, and chemical cycling
Community ecology: analyzes interactions between populations of different species in a specific area
Population ecology: studies factors affecting the size of a specific group of individuals of the same species over time
Organismal ecology: explores how an organism's physical structure, physiology, and behavior deal with environmental challenges
Climate and Global Patterns
Climate refers to long-term prevailing weather conditions
Four major abiotic components influence climate: temperature, precipitation, sunlight, and wind
Macroclimate: patterns on a larger scale (global, regional, landscape)
Microclimate: specific locations with fine-scale patterns
Solar energy and the planet's movement in space determine global climate patterns
Sun's warming effect causes temperature variations and influences evaporation, air, and water circulation
Sunlight hits at different angles, leading to latitudinal variations in climate
Circulation and Precipitation Patterns
Warm, wet air masses flow from the tropics to the poles, releasing water and causing precipitation
Descending dry air creates arid climates around 30 degrees north and south
Air flowing closer to the Earth's surface generates predictable wind patterns
Cooling trade winds blow from east to west in the tropics
Prevailing westerlies blow from west to east in temperate zones
Cycles and Regional Effects on Climate
Climate can be affected by seasons, large bodies of water, and mountains
Seasonality depends on light and temperature, increasing towards the poles
Belts of wet and dry air shift throughout the year based on the changing angle of the sun
Ocean currents and large lakes moderate the climate of nearby terrestrial environments
Mountains influence sunlight and create rain shadows and leeward sides
Every thousand-meter increase in elevation causes a temperature drop of approximately six degrees
Microclimate and Biomes
Microclimates are influenced by abiotic and biotic factors
Terrestrial biomes are identified by climate and disturbance
Biomes are recognized by vegetation type or environment
Climate plays a key role in determining biome distribution
Climatographs plot temperature versus precipitation in a region
Biomes are also affected by annual patterns
Global Climate Change
Global climate change has significant impacts on the biosphere
Past climate changes have affected species distribution and extinction
Predictions for future climate change scenarios show potential range shifts for species
Terrestrial Biomes
Terrestrial biomes can be identified by climate and disturbance
Various types of biomes exist, including tundra, taiga, temperate deciduous forest, tropical rainforest, grassland, desert, and chaparral
Temperature and precipitation patterns help distinguish between biomes
Terrestrial Biomes
Features of Terrestrial Biomes
Named for physical or climatic factors, as well as vegetation
Overlaps between biomes
Vertical layering with different layers providing habitats for animals
Biomes are dynamic and have ranges of patchiness
Similar characteristics in separated biomes arise through convergent evolution
Disturbance in Terrestrial Biomes
Storms, fire, human activity cause changes in the community
Fires can maintain savannah vegetation and create gaps in forests
Fire suppression has changed vegetation in the Great Plains
Tropical Forest
Found in equatorial and sub-equatorial regions
Constant rainfall
Vertically layered with intense competition for light
Home to millions of animal species
Human population growth is destroying tropical forests
Deserts
Occur in bands 30 degrees north and south of the equator, interior of continents
Low and highly variable precipitation
Plants adapted for heat and desiccation tolerance
Common desert animals include snakes, lizards, scorpions, ants, beetles, migratory resident birds, and seed-eating rodents
Urbanization and conversion to agriculture have reduced desert biodiversity
Grass Savannah
Found in equatorial and sub-equatorial regions
Seasonal precipitation
Grasses and forbs make up the majority of ground cover
Dominant plant species are fire-adapted and drought-tolerant
Common species include insects, wildebeests, zebras, lions, and hyenas
Human fires help maintain this biome by minimizing vertical layering
Chaparral
Found in mid-latitude coastal regions on several continents
Highly seasonal precipitation with rainy winters and dry, hot summers
Dominated by shrubs, small trees, grasses, and herbs
Plants adapted to fire and drought
Common species include amphibians, birds, reptiles, insects, mammals, and browsing mammals
Agriculture and urbanization have reduced chaparral areas
Temperate Grasslands
Found on multiple continents
Highly seasonal precipitation with cold winters and hot, wet summers
Dominant plants are grasses and forbs adapted to drought and fire
Native mammals include bison, wild horses, and prairie dogs
Conversion to farmland has reduced grassland areas
Northern Coniferous Forest (Taiga)
Found in northern North America and Eurasia
Largest terrestrial biome
Variable precipitation with cold winters and hot summers
Dominated by conifers
Common species include migratory resident birds, moose, brown bears, and Siberian tigers
Logging is a significant threat to these forests
Temperate Broadleaf Forest
Found in mid-latitudes in the northern hemisphere, also in Chile, South Africa, Australia, and New Zealand
Lots of precipitation throughout the year
Cold winters and hot, humid summers
Vertical layers with deciduous trees in the northern hemisphere and evergreen eucalyptus in Australia
Mammals, birds, and insects utilize all vertical layers
Settlement and agriculture have impacted these forests, but some areas are showing recovery
Tundra
Found in expansive areas of the Arctic and alpine regions
Low precipitation in the Arctic, higher in alpine regions
Cold winters and cool summers
Permafrost prevents water absorption by soil
Vegetation includes herbaceous plants, mosses, grasses, forbs, shrubs, trees, and lichens
Mammals include musk oxen, caribou, reindeer, bears, wolves, and foxes
Sparse settlement, but oil and mineral extraction are threats
Aquatic Biomes
Overview of Aquatic Biomes
Largest part of the biosphere in terms of area
Salt concentrations of about 3% in marine biomes and less than 0.1% in freshwater biomes
Linked to surrounding terrestrial biomes
Zones in Aquatic Biomes
Stratified into zones based on light penetration, temperature, and depth
Upper photic zone has sufficient light for photosynthesis
Lower aphotic zone receives little light
Pelagic zone includes both photic and aphotic zones
Abyssal zone is deep in the aphotic zone with a depth of 2000 to 6000 meters
Benthic zone is the bottom sediment of all aquatic zones
Detritus from surface water provides food for organisms in the lower aphotic zone and benthic zone
Zonation in Aquatic Biomes
Aquatic biomes have zonation similar to terrestrial biomes
Lake zonation is different from ocean zonation
No abyssal zone in lakes
No significant depth variation in lake zonation compared to ocean zonation
Aquatic biomes vary based on depth, light penetration, distance from shore, and position in zones
Thermocline separates warm upper layer from cold deeper layer in aquatic biomes
Lakes undergo semi-annual mixing called turnover to distribute oxygenated and nutrient-rich water
Organisms primarily live in the shallow photic zone, while the aphotic zone has little life
Lakes
Lakes range from small ponds to large lakes
Temperate lakes have seasonal thermocline, while tropical lowland lakes have year-round thermocline
Oligotrophic lakes are nutrient-poor with high oxygen levels
Eutrophic lakes are nutrient-rich and often depleted of oxygen, especially when covered by ice in winter
Rooted floating aquatic plants live in shallow, well-lighted areas
Zooplankton graze on phytoplankton in lakes
Invertebrates live in the benthic zone, fishes live in zones with sufficient oxygen
Human nutrient input can lead to algae blooms, oxygen depletion, and fish kills
Wetlands
Wetlands are inundated by water and support water-adapted plants
High organic production and decomposition, low dissolved oxygen
Wetlands can develop in shallow basins, flooded river banks, or coastal areas
Wetlands are highly productive biomes
Plants found in wetlands include lilies, cattails, sedges, tamarack, and black spruce
Wetlands are home to diverse invertebrates, birds, otters, frogs, and alligators
Wetlands are important for water purification and flood reduction
Human activities have destroyed up to 90% of wetlands
Streams and Rivers
Current is the prominent physical characteristic of streams and rivers
Headwaters are cold, clear, turbulent, and oxygen-rich
Rivers are warmer, more turbid, and more oxygenated
Unpolluted rivers can support diverse fish and invertebrate populations
Pollution can degrade water quality and harm organisms
Damming for flood control disrupts stream and river ecosystems
Estuaries
Estuaries are transition areas between rivers and the sea
Salinity varies with tides, nutrient-rich and productive
Estuaries have tidal channels, islands, natural levees, and mud flats
Salt marsh grasses and algae are major producers in estuaries
Estuaries attract marine invertebrates, fish, waterfowl, and marine mammals
Humans consume oysters, crabs, and fish from estuaries
Human interference upstream has disrupted estuaries worldwide
Intertidal Zones
Intertidal zones are periodically submerged and exposed by tides
Organisms in intertidal zones face temperature and salinity variations and wave forces
Oxygen and nutrient levels are high
Sandy zones support seagrass and algae, rocky zones support attached marine algae
Animals in rocky zones have structural adaptations to attach, while sandy zones bury organisms
Animals in intertidal zones include sponges, sea anemones, echinoderms, and small fishes
Oil pollution has disrupted many intertidal zones
Oceanic Pelagic Zones
Oceanic pelagic zones are constantly mixed by oceanic currents
High oxygen levels, turnover in temperate oceans renews nutrients in the photic zone
Phytoplankton and zooplankton are dominant organisms
Free-swimming animals and marine mammals also inhabit pelagic zones
Overfishing has reduced fish populations, pollution has harmed the zone
Coral Reefs
Coral reefs are formed from coral skeletons in the photic zone
Shallow reef-building corals live in warm, clear water
Deep-sea corals live at greater depths with less light availability
Corals require high oxygen concentrations and a solid substrate to attach
Coral reefs can progress from fringing reefs to barrier reefs to coral atolls
Marine Benthic Zone
Marine benthic zone is below the surface waters of coastal and offshore zones
Deep benthic abyssal zone has cold temperatures and high water pressures
Soft sediments and occasional rocky areas in the benthic zone
Seaweeds and filamentous algae are found in the benthic zone
Deep-sea hydrothermal vents have unique prokaryotes, echinoderms, and arthropods
Neritic benthic communities include invertebrates and some fishes
Overfishing and pollution have depleted populations in the benthic zone
Interactions between Organisms and Environment
Species distribution is influenced by interactions between organisms and their environment
Evolution and ecological interactions both play a role in species distribution
Ecological events can lead to evolutionary changes, such as beak size in Galapagos finches
Factors Influencing Species Distribution
Biotic and abiotic factors can influence species distribution
Climate, interspecific interactions, and other factors impact kangaroos
Ecologists' Approach
Ecologists study species distribution and the factors that allow them to exist in certain areas
Dispersal allows for global distribution of organisms
Natural range expansions and adaptive radiation demonstrate the role of dispersion in species distribution
Cattle egrets expanded their distribution in the Americas since the late 1800s
Greater distances of dispersal can lead to adaptive radiation
Hawaiian silver swords descended from a North American tarweed species
Transplants and Invasive Species
Transplants involve intentional or accidental relocation of organisms
Invasive species can disrupt communities and ecosystems
Successful transplants may indicate a larger potential range for a species
Factors Affecting Species Distribution
Organisms do not occupy all potential range habitats
Predation, herbivory, and competition can affect species distribution
Abiotic factors such as temperature, water, sunlight, wind, rocks, and soil also influence species distribution
Factors vary depending on location and time
Influence of Abiotic Factors
Environmental Temperature
Temperature impacts biological processes
Cells can freeze and rupture below zero degrees Celsius
Proteins can become denatured above certain temperatures
Mammals and birds maintain internal temperature for survival
Water
Water is crucial for survival
Desert organisms have adaptations to conserve water
Oxygen diffusion is slow in water, leading to low oxygen concentrations in deeper oceans and lakes
Salinity affects water and impacts excretory system and water balance in aquatic organisms
Freshwater and saltwater environments are inhabited by different organisms
Sunlight
Intensity and quality of sunlight impact photosynthesis
Water absorbs light in aquatic environments, leading to more photosynthesis near the surface
Available light in deserts provides energy but can also cause stresses on plants and animals
Soil Characteristics
Soil characteristics limit plant growth and