ECOLOGY Exam 1
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- Ecosystem
-
The biotic community & its abiotic enviro functioning as a system
{2 components=
1)living--biotic
2)physical--abiotic} - Earth's Interception of Solar Radiation
-
Earth intercepts solar energy in *shortway radiation* (from hot masses=sun).
energy passes through atmosphere, then hits surface and is emitted back as *longwave radiation* (from cooler masses=earth).
Longer wavelengths can't pass through atmosphere as easily so some is returned to Earth.
==The Greenhouse Effect==
...crucial to maintaining surface temp of earth... - Temp Gradiant from Equator to Poles
-
the amount of solar radiation intercepted decreased with latitude away from equator.
*due to earth's tilt*
at higher latitudes radiation hits surface at steeper angle and has to travel through a deeper layer of air
&Reason for the Seasons = Earth's Tilt
(causes parts of earth to receive seasonal differences in solar radiation) - Adiabatic Cooling
-
Decrease in air temperature through expansion---not heat loss
*responsible for decrease in temp w/altitude*
*ALSO moist air cools slower than dry air - Atmospheric Circulation
-
air=constant state of movement
due to vertical movements of air patterns & earth's rotation
air/H20 currents deflected rt in N Hemisphere
&
currents deflected lft in S Hemisphere
*3 Cells in each hemisphere -
Vertical movements of air
(imaginary non-rotating earth) -
-Equatorial region receives most solar radiation
-warm air rises bc its less dense than cooler air
-warm air from equator rises
=low pressure at surface
=air rising beneath it forces air mass to spread N & S
=as move toward poles air cools & sinks
==raises surface pressure
====that heavier air then moves back toward equator - Patterns in Ocean Currents
-
caused by
1)global pattern of wind
2)Coriolis Effet
*act like wind until hit continents
(Gyres go west (due2wind) til hit continents then split to N & S then cool, move east(due2wind), hit continents, then flow back to equator) - Gyres
-
the 2 circular water motions that dominate each ocean
-N Hemisphere = clockwise
-S Hemisphere = counter clockwise - Saturation Vapor Pressure
- Max amt of moisture the air can hold at a given temp
- Precipitation patterns determined by
-
Wind,
Temp,
Ocean Currents - Latent Heat
-
Amount of energy released or absorbed during change in state (of matter)
-more ordered (liquid) to less ordered (gas) state =energy is absorbed
-less ordered to more ordered =energy is released -
Evaporation
v
Condensation -
Evaporation= liquid to gas state
Condensation= water vapor to liquid state -
Rate of Evaporation = Rate of Condensation
Means: -
The air is saturated
(when air & liquid h20 meet = molecules freely exchanged) - Pattern
-
Non-random Spatial Distribution
*due to limits in distribution of organisms (no limits = no patterns) - Population
- group of individuals of the same species in an area--Interbreeding
- Community
- all populations of different species living and interacting within an ecosystem
-
Ecosystem
(in community terms) -
Communities + Physical Enviro = Ecosystems
*exchanges of materials & flow of energy
(abiotic + biotic)
-adjacent ecosystems interact - Landscape
-
a "Patchwork" pattern of adjacent ecosystems
(ecosystems linked by H20 flow & movement of organisms) - Basic Unit of Ecology?
-
The INDIVIDUAL
-responds to enviro
-B & D = pop dynamics
-interactions = communities
-passes genes to next generations = nat. sel. - Why are there limits to distribution?
-
bc limits to information, genectic know-how
(Life Organized with Information) - Autecology
-
Ecology of Single Species Population
(like studying certain aspects of gerbils)
("species one at a time")
*population ecology, psysiological ecology, life histories* - Synecology
-
Ecology of plural species considered together
*wildlife ecology, communtiy ecology, landscape ecology, life zone ecology..* - Population Distribution described by 2 basic laws:
-
1) Lieberg's Law of the Minimum
-how much will a bucket hold?
2)Shelford's Law of Tolerance
-thought lieberg's was too simple--you can have too much of a good thing.
(middle--optimum is better than min and max) -
Shelford's laws of distribution
(law of tolerance) -
1)the range of a species is limited by changes in limiting factors (factors beyond limit tolerated by the species)
2)the distribution area (where species can live) is determined by the power of migration & their tolerance
**they live there bc they can stand it & they can get there - Gradiant Analysis
-
plot of
Species Distribution against a Spatial Vaiable
(elevation, temp, moisture, nutrients)
AKA: relative abundance of individuals of a species along enviro gradiants
---QUANTIFIED LIMITS---
**WHITTAKER**
{shows communities are generalizations...not absolute} - Zonation v Succesion
-
Zonation=spatial
-changes in community structure across landscape
Succesion=Temporal(time)
-changes in community structure through time - Primary Succession
-
on Newly Exposed Surface (NO SOIL)
ex. st helens, glacier bay - Secondary Succession
-
vegetation has been removed but SOIL REMAINS
(after disturbances)
ex. post fire - Changes over succession?
- Species presence & Relative abundance
- 150 year study of succesion?
-
identify differences in space
which represent
differences in time
(old field succession- when was the field abandoned?) -
Trends in Ecological Succesion
(from Early to Late) -
-food webs->more complex
-biodiversity->increases
-specialization->narrows
-nutrient cycling->tighter
-stability->higher
-photosynthetic/respiration (P/R Ratio)->lowers from >1 to ~1 -
Ecological Succesion
definition -
change in composition of biotic community over "ecological time" (10-1000 yrs)
ex. abandoned field= weeds->herbs->shrubs
*can be cyclical (fire-prone ecosystems) - Community Evolution
-
development of regional biota over "evolutionary time" (1000-1000000 yrs)
ex. savannas replaced by grassland as rockies rise & rainshadow forms -
Physiological time
v
Ecological time
v
Evolutionary time -
SHORTEST TO LONGEST:
physiological
ecological
evolutionary -
Why does ecological Succession occur?
2 competing (prob both right) theories -
1)FACILITATION MODEL
-early species (pioneers) change the conditions of a site to make it more habitable for later invading species
2)INHIBITION MODEL
-early species resist invasion & remain until they're replaced by:
Competition, Predation, Disturbance -
FACILITATION MODEL
theory of ecological succession - early species (pioneers) change the conditions of a site to make it more habitable for later invading species
-
INHIBITION MODEL
theory of ecological succession -
early species resist invasion & remain until they're replaced by:
Competition, Predation, Disturbance - Natural Selection Requires (2)
-
1)Variation among individuals
2)differences in survival and reproduction (fitness) - Fitness
- contribution individual makes to future generations
-
Directional
Stabilizing
Disruptive
SELECTION -
DIRECTIONAL:
trait shifted to one extreme or the other
DISRUPTIVE:
Favors both extremes simultaniously
STABILIZING:
favors individuals near mean population - MENDEL
-
1)alternate units control heritable traits
2)for each characteristic organism has 2 units
3)when 2 units are different the dominant is expressed & recessive is not
(unit = gene/allele)-later - DNA's contained in
-
Chromosomes
(which are oganized into subunits--GENES) - alternate forms of genes =
- alleles
- water cycle
-
solar radiation provides energy for evaporation of water
1-Precipitation
2-interception (some water doesn't infiltrate into ground and evaporates back into air
3-filtration (leads to groundwater)
4-Evapotranspiration (sum of evaporating water from surface and from transpiration {the evaporation of water from leaves/plants} - Water's physical Properties
-
1)polar
*H+ O- bonding*
CAUSES
a)hydrogen bonding
b)high specific heat
c)cohesion & surface tension
d)buoyancy
e)high solubility - Specific Heat of Water
-
large quantities of heat energy required to change state of matter
bc of lattice arrangement of H & O water becomes denser til 4* C then decreases in density
*Ice floats bc lattice structure has holes=not dense
-insulates water below - Cohesion & Surface Tension
-
Cohesion:
water molecules stick to eachother resisting breaking
Surface Tension-
water hits air=weaker attraction than water to water below - Viscosity of water
-
due to cohesion (attraction of water molecules = harder to seperate)
viscosity of water is much greater than air
-also due to fact that its more dense than air
----causes buoyancy - Buoyancy
-
caused by viscosity
if body's weight in water is is less than water it displaces = upward force = buoyancy
*since most aquatic animals have nuetral buoyancy they don't require structural material (skeletons) to hold themselves erect in water
*ps. higher density of water means greater changes in pressure than in air - Water as a Solvent
-
boundery between air and H20 experiences DIFFUSION (molecules move from high concentration to low concentration)
= net transfer of Oxygen &Carbon Dioxide - Solubility in water depends on
-
1)temperature
-solubility decreases at temperature increases (solubility greater at lower temps)
2)pressure
(solubility increases as pressure increases)
3)salinity
(solubility decreases as salinity increases)
*greater density and viscocity of water limit diffusion from air - Solubility of O2 and CO2 (carbon dioxide)
-
-solubility of O2= low
-solubility of CO2= high
-CO2 reacts w/H20 and produces carbonic acid
--->result in more H+
--->more acidity (more H+ = more acidic)
*alkaline = more OH- less H+ - Light & Water
-
lower angle light hits = more reflected
light in water reduced by:
-reflection
-particles
-water itself absorbs light - Water & Temperature
-
*high heat capacity *resists change in temp
*high heat of vaporization
*high heat of fusion (energy taken out to freeze
-surface temperatures = reflect incoming/outgoing radiation
-decline in solar radiation w/depth
-most rapid decline = thermocline
*thermocline seperates warm upper "epilimnion" and deeper colder denser "hypolimnion"
--->ESTABLISHING PATTERNS OF ZONATION - Standing bodies of water Circulation in spring/fall
-
temp & sunlight low
-surface water cools
-becomes denser & sinks
-warmer water goes to surface
-it cools and sinks
=vertical circulation
ps. in winter warmest part is at bottom -
Water as a Solvent (in general)
*solution w/H20 as solvent = acqueous solution -
-can dissolve more substances than any liquid
-nutrients and waste are dissolved and transported
-solubility due to H-bonding (attract molecules carrying a charge)
--->ex. sodium chloride (Na+) & (Cl-) are more attracted to water molecules than eachother.... so they dissasociate and dissolve
(solubility of sodium chloride =HIGH)
*when concentration reaches solute max excess amts are deposited as sediments - water distribution
-
Oceans
Ice
Goundwater
Surfacewater
Atmosphere
Biosphere
*highest to lowest*
**Hydrosphere crucial to biosphere but biosphere trivial to hydrosphere - first law of ecology
-
water flows downhill
--integrates ecosystems (connects landscapes) -
Simplest measure of Community Structure
=
Species Richness - number of species w/i a community
- Spatial Patterns
-
-species distributions/limits
-productivity (primary & secondary)
-Biotic Communities - Time Patterns
-
-individual position/movement
-population dynamics
-ecological succession
-community development
(community evolution) - Mosaic
-
patchwork or different types of land
(all in an ecological community)
*product of boundaries defined by changes in structure of distinct patches - Patches
-
-distinct LOCAL communities
-realatively homogeneous
-differ from surroundings in structure and species comp
-embedded in matrix
-produced by variations in geology(rocks), topography(physical structure), soil, climate, human activity, natural events (fire, grazing)
*crop fields, forests, ponds* - Landscape Ecology
-
study of causes of formation of patches and boundaries (and the consequences of these spatial patterns--concerned w/size/shape of patches)
[the interactions depend on size and spatial arrangement]
(think of ecosphere as hierarchy)
*landscapes dynamic in space and time (change occurs)
*complexity is key - Matrix
- group of many different patches
-
Patches'
area, shape, & orientation
determine -
-their suitability as habitats
-influence ecological processes (wind flow, seed dispersal, animal movement) - topography
- physical structure of a landscape
- Edges
- the perimeter of a patch
- Inherent Edges
-
-abrupt change in physical conditions (topography, substrate, soil type, microclimate)BETWEEN COMMUNITIES (patches)
-long term natural features (like rock outcrops)
-usually stable & Permanent - Induced Edges
-
-resulting from natural disturbances (fires storms floods) & human activity (housing, farms)
-edges that are subject to successional changes over time - Borders
-
where edge of one patch meets edge of another
(area of contact, seperation, transition between patches) - Wide Borders form transition zone called
- ECOTONE
- Edge Species
- species restricted exclusively to edge environments
- Edge Effect
-
high species richness bc they can support species of adjoining communities & opportunistic species adapt to edges
influenced by
-border area available
-greater contrast between patches= greater diversity - Corridors
-
strips of similar habitat
-connect seperate patches
-usually of human origin
-provide habitat
-can act as filters/barriers
-permit travel ways - Filter effect
-
gaps in corridors allow some organisms to cross and restrict others
-can spread diseases between patches
(can be roads) - Disturbance
-
event that disrupts community structure & function
-create patterns & are influenced by patterns
*Intensity= measured by proportion of total pop that disturbance kills
*Scale= the spatial extent of impact relative to size of affected landscape
*Frequency= mean # of disturbances in a time interval -
Small Scale
Large Scale
Severe
DISTURBANCES -
SMALL SCALE:
-make gaps
-creating patches of different comp. and stage
LARGE SCALE:
-favor opportunistic species
-species like original pop eventually replace early species
SEVERE disturbances:
can replace a community altogether
*too frequent disturbances can eliminate a species - "Shifting Mosaic"
-
the patches of communities that define a landscape is always changing
-landscape is composed of patches each in different stages of development - Landscapes
- patchwork mosaics
-
Biological Molecules
Polymers
and their monomers -
*Carbohydrates-->Glucose
*Fats-->Fatty Acids & Glycerol
*Proteins-->Amino Acids
*Nucleic Acids-->Nucleotides - Dominant Species
-
species predominating community
-based on # and size of individuals - Keystone SPecies
-
have influence on community disproportionate to their #s
-removal causes changes in structure and significant loss of diversity - Basal Species
- feed on no other species but are fed upon by others
- Intermediate species
- feed on other species and are also prey of other species
- Top Predators
-
prey on intermediate and basal species
and aren't fed on by other species - Zonation
- spatial change in community structure
- Guilds
-
groups of species that exploit a common resource in a similar fashion
(ex. hummingbirds & other nectar feeding birds exploit flowering plants) - Functional Type
- group of species based on common response to environment, life history, or role in community
- 2 views of community
-
1)Organismic Concept of Communities
(clements)
-community as unit - each species component of the whole
-whenever a habitat repeats the same species occurs
-species in association have similar distributional limits
-common evolutionary history & similar tolerances
2)Individualistic/Continuum Concept
(gleason)
-relationship among species in a community are a result of their tolerances --NOT strong interactions or common evolutionary history -
Ecology v
Environmental Management v
Environmentalism -
ECOLOGY:
science of understanding our surroundings
ENVIRO MANAGEMENT:
how CAN we work the world
ENVIRONMENTALISM:
how SHOULD we work the world (lifestyle choices) -
Modes of Evolution
(different time scales) -
Cultural
Organic
Geophysical
Cosmic
Shortest to Longest -
Origin of Life
Extraterrestrial Hypo - "seeds" from space arrived on meteorites
-
Origin of Life
Chemoautotrophic Hypo -
life from the deep
-from deep sea hydrothermal vents - Mechanism of Organic Evolution
- Natural Selection
- Darwin Observed (3)
-
1)Variation
2)Overpopulation
(more offspring produced than survive to reproduce)
3)Competition
(struggle for resources in finite enviros)
CONCLUSION: natural selection
(2/3 ecology[overpop & competition], 1/3 genetics [variation]) - Darwin didn't understand
-
-mutation
-mechanisms of genetics - Fundamental Forces of Nature:
-
1)Gravitational
2)Weak
3)Electromagnetic*
*fundamental force of life
4)Nuclear
-Weakest to Strongest- - Fragmentation can occur on what scale
-
any spatial scale
-from roads to continental drift - Biomes
-
-bigger than states, smaller than continents
-distinguished by vegetation & climate
-emphasize evolutionary convergence & -paralled evolution (dissimilar organisms come to look similar *placental & marsupial animals*
*biomes regional community, life zones local community* -
2 types of environmental change
(succession) -
1)autogenic - result of organisms in community
2) allogenic - of physical enviro (temp) - Riparian Corridors
- woodland along bank of river
-
The most abundant elements in earth's crust are:
(3) -
Oxygen
Silicon
Aluminum - Fathers of Ecology:
- Hunters/Gatherers
- Leeward side of mountain =
- rain shadow
- Life zones driven by
-
*temperature
*precipitation
*soils
(life zones more useful in steep gradiants bc H20 flows downhill) - standing water zoned by :
-
1)temperature
2)production/respiration (P/R Ratio) - 6 Major Elements in Organic Molecules
-
H -hydrogen
O -oxygen
C -carbon
N -nitrogen
P -phosphorous
S -sulfur
(CHNOPS)---HOCNPS - Land : H20 =
- 1 : 3
-
Atmospheric
Gas Content -
1/4 Oxygen
3/4 Nitrogen - Efficiency of Energy Transfers
-
10%
(100- plant =
10- 1* consumer =
1- 2* consumer)
*=degree - Humans are expensive for biosphere to maintain bc
-
-large
-warm (endothermic)
-consumers (herbivores, carnivores, omnivores) - ecosystem ecology
- study of whole living systems
- phsiological ecology
-
responses of individuals to environmental conditions
(temp, moisture, light) -
The Grants'
(people) - documented natural selection (& the different types) on galapagos islands after darwin
-
Chromosomes
Genes
Alleles
Locus
Homozygous
Heterozygous
Genotype
Phenotype
Gene Pool -
Chromosomes(contain DNA)
Genes(subunit on chrom that carries DNA)
Alleles(alternate forms of a gene)
Locus(where allele occupies chrom)
Homozygous(allels on locus are the same)
Heterozygous(alleles are different)
Genotype(sum of hereditary info)
Phenotype(external expression of genotype)
Gene Pool(total collection of genes in all individuals of a pop) - Hardy-Weinberg Principle
-
gene frequencies will remain the same over time IF
1)mating is random
2)mutations don't occur
3)pop is large
4)natural selection doesn't occur
5)migrations don't occur - Biological Species
- a group of populations whose individuals have the potential to interbreed
- isolating mechanisms
-
allow a species to remain distinct
-reproductive barriers --don't allow exchange of genes between populations
--premating (habitat, isolation, behavior, mechanical)
OR
--postmating (reduce reproductive success of offspring that arise from mating of ind of diff species) - Hybrids
- offspring resulting from mating of 2 diff species
- Sympatric species
- occupy the same area at the same time -- opportunity to interbreed
- Allopatric Species
- occupy areas seperated by time or space (don't come into physical contact with eachother)
- high temps lethal to most organisms bc
- they denature proteins
- life zones
-
NOT the same as biomes
*are influenced by temperature - international biological program in the US (US-IBP)
- efforts organized by biomes
- MERRIAM
- life zones
- conservation ecology & population ecology...
- go hand in hand
- ODUM
- brought engeneering perspective to ecological energetics
- science is:
-
-a search for patterns of cause and effect in the universe
-common sense--natural way of working the human mind
-an evolution tested process - an african plant is similar in appearance to a mexican plant
-
convergent evolution
(development of similar characteristics of species in different areas but under similar enviro conditions) - organic evolution
-
*change in gene frequency over time
[central concept in ecology] -
based on lecture
scientific study of ecology in colorado began with - paleolithic people ~15,000 yrs ago
- biological magnification
-
accumulation of fat-soluble chemicals thru food chain
(pesticides etc) - communication necessarily involves
-
1)sending individual (or cell)
2)receiving individual (or cell)
3) irritability (biological sense of word) -
larger edge per area
advantage of who? -
-small!
(in support of several small argument) - people involved in laying foundations for conservation ecology
-
-macarthur
(mathematical ecologist)
-e.o. wilson
(sociobiologist)
-darwin
(pioneer evolutionist)
-elton
(community ecologist)