Midterm Flashcards
Ecology
Scientific study of interactions between organisms and their environment
Controlled experiment
Experimental groups are compared with a control group that lacks the factor being tested.
No control= no real experiment
Standard error
Graphs with smaller standard error are more accurate. You can make a standard error smaller by replicating.
Case study: factors affecting amphibian declines
- habitat loss
- pathogens
- climate change
- Ribeiroia trematoe flatworms
Scientific Method
- Make observations and ask questions (pattern)
- Use previous knowledge or intuition to develop hypothesis (process)
- Evaluate hypothesis by experimentation, observational studies, or quantitative models
- Use the results to modify the hypotheses, pose new questions, or draw conclusions about the natural world
Experimental design
- Replicate- perform each treatment more than once on independent units
- Assign treatments at random
- Analyze results using statistical methods
Observational field study
2 groups and you sample them
Ex) one’s healthy and one’s deformed
Controlled experiment
Able to control the variables
Ex) tadpoles and parasite Ribeiroia in the lab
Field experiment
Cages
Ex) ponds with pesticides vs. No pesticides; cages for pesticides
Spatial scales
Small: soil micrrorganisms
Large: atmospheric pollutants
Temporal scales
Short: leaf response to sunlight
Long: how species change over geologic time
Levels of Biological Organization
Individual Population Community (diff species) Ecosystem (abiotic and biotic) Landscape Biosphere
Population
Group of individuals of a species that are living and interacting in a particular area
Community
Association of populations of different species in the same area
Ecosystem
Community of organisms (biotic) plus the physical environment (abiotic)
Landscapes
Heterogenous areas, including multiple ecosystems that are connected
Biosphere
All living organisms on earth plus the environments in which they live
Evolution
- Change in genetic characteristics of a population over time
- Descent with modification- organisms gradually accumulate differences from their ancestors
Adaptation
A characteristic that improves survival or reproduction
Natural selection
Individuals with certain adaptations tend to survive and reproduce at a higher rate than other individuals
If the adaptation is heritable…
The frequency of the characteristic may increase in a population over time.
Ie) superbug evolution
Ecosystem processes
- energy moves through ecosystems in a single direction only- it cannot be recycled
- nutrients are continuously recycled from the physical environment to organisms and back again- that is the nutrient cycle.
Producers
Capture energy from an external source (eg. The sun) and use it to produce food
Net primary productivity (NPP)
(Accumulation of energy)
-energy captured by producers, minus the amount lost as heat in cellular respiration
Consumers
Get energy by eating other organisms or their remains
What is causing changes in salmon catch?
- threats to streams
- changes in the oceans
Threats to streams
Damming, pollution, and overfishing
Changes in the ocean
- climatic variation in the North Pacific
- periods of high salmon production in Alaska= periods of low production in Oregon and Washington
- correlation between salmon production shifts and sea surface temperatures
Pacific Decadal Oscillation (PDO)
Associated with 20 to 30 year cycles of warm and cool temperatures in the North Pacific
Weather
Current conditions- temperature, precipitation, humidity, cloud cover
Climate
Long-term description of weather, based on averages and variation measured over decades
-characterized by average conditions, but extreme conditions are also important
Mediterranean-type climate
Precipitation is concentrated in winter
Grassland precipitation
Spread evenly throughout the year
Conduction
Kinetic energy is transferred by molecules in direct contact with one another
Convection
Energy transfer by movements of air or water currents
Sensible heat flux
Energy transfer from warm air immediately above the surface to the cooler atmosphere by convection and conduction
Greenhouse gasses
Absorb and reradiate the infrared radiation emitted by Earth
- water vapor (H2O)
- carbon dioxide (CO2)
- Methane (CH4)
- Nitrous oxide (N2O)
Consequences of greenhouse gases
-without any greenhouse gasses in the atmosphere it would be 33 degrees colder. They have a pretty strong impact
Solar radiation
- poles the sun’s rays are spread over a larger area and take a longer path through the atmosphere
- near the equator, the sun’s rays strike earth’s surface perpendicularly
Surface heating and uplift
- warm air is less dense than cool air, so the air above the warm surface rises
- as the warm air rises, it expands and cools
- eventually the air cools enough to form clouds
Where do clouds usually form?
Troposphere and stratosphere.
Also near the trophics leading to a low pressure zone
Where do deserts usually occur?
At areas of very low precipitation at high pressures
Atmospheric Circulation
- warmee air moves from the equator north and south
- air from the poles moves back down towards the surface
- ferrell cell fluctuates the most. Is the temperate zone
Polar cell, Ferrell cell, and the Hadley cell result in which 3 major climatic zones?
Occurs in each hemisphere:
- Tropical
- Temperate
- Polar
Prevailing winds
Areas of high and low pressure created by the circulation cells resulting in air movements
The Coriolis Effect
Winds appear to be deflected due to the rotation of the Earth
Global Wind Patterns
- prevailing winds change depending on the time of year
- wind tends to blow from areas of low pressure to areas of high pressure
Ocean Circulation
- ocean currents are largely determined by prevailing winds
- wind produces drag on the surface of the water, and over time creates directions
Polar Downwelling
- Where warm tropical surface currents reach polar areas: the water cools, ice forms, the water becomes more saline and more dense and sinks (downwelling).
- The downwelling water mass moves back towards the equator, carrying cold polar water
Coastal upwelling
- brings nutrients up into the zone with life feeding lots of small organisms
- most zones of water remain pretty much unmixed
Coastal upwelling
- where deep ocean water rises to the surface
- occurs where prevailing winds blow parallel to a coastline
- surface water flows away from the coast and deeper, colder ocean water rises up to replace it
Large-scale atmospheric and oceanic circulation patterns establish global patterns of temperature and precipitation
- average annual temperatures become progressively cooler from the equator toward the poles
- this pattern is altered by ocean currents, continental topography, and the distribution of land and water masses
Do temperatures fluctuate more over land or water?
More over land
Precipitation patterns associated with atmospheric circulation cells are modified by what?
Mountain ranges, semipermanent high- and low-pressure zones
Rain shadow effect
Moist on one mountain side. Arid on the other. Can also see major wind pattern differences on either side.
Evapotranspiration
Water loss through transpiration by plants, plus evaporation from the soil.
-transfers energy (as latent heat) and water into the atmosphere, thereby affecting air temperature and moisture
Albedo
Capacity of a land surface to reflect solar radiation- is influenced by vegetation type, soils, and topography
-rates of evapotransporation greatly decline in deforested areas. Causing the local climate to get dryer and hotter
Seasonality
- temperate and polar zones have pronounced seasonal variation in solar radiation and temperature
- difference in seasonal solar radiation increases from the tropics toward the poles, and results in varying day lengths
- seasonality influences biological activity and distributions of organisms
- aquatic environments also experience seasonal changes in temperature
Aquatic stratification
- affects nutrients and oxygen
- complete mixing (turnover) occurs in spring and fall
- water, depending on its temperature, changes density
El Nino
Are longer-scale climate variations that occur every 3 to 8 years and last about 18 months
La Nina
Events are stronger phases of the normal pattern, with high pressure off the coast of South America and low pressures in the western Pacific
Long-term Considerations
- earth’s climate alternates between warm and cool cycles
- warmer periods are associated with higher concentrations of greenhouse gases
- earth is currently in a cool phase characterized by formation of glaciers, followed by warm periods with glacial melting
- these glacial-interglacial cycles occur at frequencies of about 100, 000 years
Milankovitch Cycles
The glacial-interglacial cycles have been explained by regular changes in the shape of Earth’s orbit and the tilt of its axis
The chemical environment
Key chemical determinants of biological function:
- salinity
- acidity
- oxygen availability
Salnization
Soils in arid regions become saline when water is brought to the surface by plant roots or irrigation, and high rates of evapotranspiration result in salt build-up
Acidity
Ability of a solution to act as an acid: a compound that gives up protons (H+) to a solution
Alkalinity
Ability of a solution to act as a base: a compound that takes up H+ or gives up hydroxide ions (OH-)
What are biomes characterized by?
Leaf decidousness and succulence
Convergent evolution
- plants don’t move around, so they’re forced to adapt and make it work where they are
- so plants can be morphologically similar (function the same), but be taxinomically different
- immobility of plants make them vulnerable to selective pressures
Terrestrail biomes
- characterized by growth forms of the dominant plants, such as leaf decidousness or succulence
- similar biotic assemblages indicate similar responses to climatic forces in different locations
- plants are best for this classification
Tropical rainforest
- high biomass, high diversity: about 50% of Earth’s species
- 11% of Earth’s terrestrial vegetation cover
- no seasonal changes
- best tropical rainforests occur between 10 degrees N and S of the equator
Tropical deforestation
- disappearing due to logging and conversion to pasture and croplands
- about 50% of the tropical rainforest biome had been altered
- soils are nutrient poor
- nutirents are in the living material
- when the huge massive vegetation is removed and converted to farmland it makes it hotter and dryer
Tropical Seasonal Forests and Savannas
- wet and dry seasons
- shorter trees, deciduous in dry seasons, more grasses and shrubs
- less than 50% have been unaltered by human activity
- threats: human population growth, converted to cropland and pasture
Hot Deserts
- sparse vegetation and animal populations
- abundance may be low but species diversity cam be high
- 30 degrees N and S of the equator; exception being those formed by rain shadows
Temperate Grasslands
- maintained by frequent fires and large herbivores such as bison
- grasses grow more roots than stems and leaves, to cope with dry conditions
- most human impacted biome on the planet due to high soil fertility
- grasslands more continental
- shrublands and woodlands more coastal
Temperature Shrublands and Woodlands
- evergreen shrubs and trees
- Mediterranean-type climates: wet winters and hot, dry summers
- fire is common
- converted to crops and vineyards, but the soils are nutrient-poor
- shrublands in continental interiors occur in rain shadows and seasonally cold climates
Temperate Deciduous Forests
- species diversity lower than tropical rainforests, but still high
- more precipitation tends to occur when its warm
- fertile soils and climate make this biome good for agriculture
Temperate evergreen forests
- they receive high rainfall amounts and have mild winters
- lower diversity than tropical and decidous forest
- pine needles tend to be slightly acidic
- high acidity tends to increase leaching
- extensive clearing. Sometimes trees replaced with non-native species
Boreal Forest (Taiga)
- permafrost (soil that remains frozen year round) prevents drainage and results in saturated soils
- cold, wet conditions in boreal soils limit decomposition, so soils have high organic matter
- lakes lost once permafrost is gone because nothing to support the lake
- have not been as impacted by human activities though impacts are accelerating
Tundra
- widespread permafrost
- largest pristine areas on earth
- increased exploration and development of energy resources
- arctic warming at almost double the global average
- further N and S most severe impacts of climate change
Mountains (Elevation)
On mountains, temperature and precipitation change with elevation, resulting in zones similar to biones
Marine Biological Zones
- determined by ocean depth, light availability, and the stability of the bottom substrate
- aphotic: where the light doesn’t penetrate
Coral reefs
- restricted to warm, shallow water
- complex habitat: a huge diversity of marine life
- rates of biomass production are some of the highest in the world
Human impacts on marine biological zones
- polluntants and nutrients via river
- commercial fishing
- greenhouse gas emissions
- increase in UV radiation due to stratospheric ozone loss
- excess nutrients algae growth
- coral bleaching
- acidification
Freshwater systems
Streams and rivers are lotic systems
- smallest streams are first order streams
- these converge to form second order streams
- large streams are 6th order streams or greater
Spatial zonation in streams
- distribuation of organisms reflect the energetic and environmental conditions experienced in progressively larger streams
- vast majority of life occurs where the nutrients are
- lakes are basically wide streams with less currents
Human impacts on freshwater habitats
- sewage and industrial wastes
- fertilizer runoff
- non-native species
- deforestation and erosion
- dams
Cryonics
Preservation of bodies by freezing
Physiological ecology
Study of interactions between organisms and the physical environments that influence their survival and persistence
Two options with environmental change?
Tolerance and avoidance
Climate envelope
Range of condition over which a species occurs
Stress
Environmental change results in decreased rates of physiological processess, lowering the potential for survival, growth, or reproduction
Acclimatization
Adjusting to stress through behavior or physiology (individuals)
Ecotypes
Populations with adaptations to unique environments
-can eventually become separate species as populations diverge and become reproductively isolated
Latent heat transfer
Water absorbs heat as it changes from a liquid to a gas state
Stomata
Can control transpiration rates
Evaporative heat loss
Uncommon in animals
Ex) sweating in humans
Ectotherms
Regulate body temperature through energy exchange with the external environment
Endotherms
Rely primarily on internal heat generation- mostly birds and mammals