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106 Cards in this Set

  • Front
  • Back

What is community structure?

Interactions among separate populations within the same space and time


Consists of many species interacting in many ways (competition, predation, mutualism, parasitism, transfer of energy, nutrients)


What are major physical features that determine species diversity?


latitude, depth, pollution


What non-physical explanations are there for species diversity?



Abundance,


Dominance,

Evenness,

Richness

What types of communities have high species diversity?

Mid latitude, abundance of rain, warm temperature, and even weather

species equilibrium model for islands

immigration, low diversity, endemic animals


What factors influence the number of species on an island?


Distance from mainland, density and evenness of endemic species


native species?

Species that occur naturally in a community

nonnative species

Migrate, introduced purposely or accidentally into a community


Can be invasive, alien, or exotic


Many drastically changed native communities

indicator species?

Serve as early warnings of damage to a community

keystone species?

species that have a more important role in a community than suggested by their abundance


What properties does species richness convey to a community?


?


What is stability of species diversity?


?

What is ecological succession?

The gradual change in species composition of a given area.


What is primary succession?


•The gradual establishment of biotic communities on nearly lifeless ground



•Begins in area where there is no soil or sediment (aquatic)


What is secondary succession?


• Reestablishment of biotic communities in an area where some type of biotic community is already present



• Followed by return to climax community following disturbance




• Occurs in an area where natural community disturbed, removed, destroyed – soil or bottom sediment remain



What are pioneer species?


• arrive at newly formed habitat



– Lichens, mosses



– Start soil formation – may take hundreds of years for soil to form



What is a climax community?


End species of succession. Maples, Oaks, etc.


How does succession apply to animals?


Food, shelter, habitat



– Early successional species: rabbit, quail, dove, pheasant



– Midsuccessional: elk, moose, deer, grouse




– Late successional: turkey, squirrel, owl, bear



How does a community change during succession besides the types of species present?


Species diversity



Trophic structure



Niches



Energy flow and efficiency




Nutrient cycling




What is facilitation in relation to succession?

• One set of species makes an area suitable for species with different niche requirements




• Lichens & mosses build up soil – habitat suitable for herbs & grasses


What is inhibition in relation to succession?

• Early species hinder establishment and growth of other species



• Plants may release toxins that reduce competition from other plants




• Succession proceeds after another disturbance


What is tolerance in relation to succession?

later species out compete???????


What is the intermediate disturbance hypothesis and how does it relate to succession?


?


How does the equilibrium theory of community

How does the non equilibrium theory of community structure relate to succession?

??


What is a landscape?



heterogeneous area consisting of distinctive patches organized into a mosaic pattern


What is landscape ecology

a subdiscipline of ecology that studies relationships between spatial patterns and ecological processes over a range of scales




Why has landscape ecology blossomed as a field of ecology over the past several decades? What facets are included in the study of landscape ecology?



1. Interdisciplinary links
2. Humans and human influences
3. Ecological consequences of spatial patterns


– Extent, origin and effects across multiple spatial scales


What components make up the structure of a landscape? What are landscape elements?


Matrix


Patches


Corridors


Fragmentation


Edge Effects


What is a patch?


– Relatively homogenous area that differs from its surroundings



– Patches vary in size, shape, number and composition and are distributed within a landscape within a variety of spatial patterns


What is the matrix of a landscape?

backgrounds of mosaic upon which patches are formed

fragmentation


Process that often occurs as a result of human activity ???

corridors

link patches within matrix


important for dispersal

edge effects

– High species diversity at edges & species unique to edge habitat




– Alternately – edge habitat lower quality than interior habitat



What is an ecotone?



Edges of habitat patches are often not sharp boundaries, but instead are physical and biological transitions from one ecosystem type to another



Explain how the structure of a landscape influences the inhabitants of that landscape.


???

ecotype


Edges may have species common in both patches as well as species unique to the edge habitat and therefore edges of patches are often high diversity habitats



How do different species explore a patchy ocean environment?


???

Succession

Seen relationship between disturbance and community dynamics

Flooding

results in higher export of phosphorous and loss from the ecosystem

Eutrophication

increased productivity and decreased biodiversity




seasonal algal blooms, increased oxygen, kills fish

Water cycle

Powered by energy from the sun and gravity, winds and air




Humidity(amount of H2Ovapor in air)


Winds& air masses




Evaporation, Transpiration, Condensation, Precipitation, Infiltration, Percolation, Runoff

Flooding

results in higher export of phosphorous and loss from the ecosystem



Loss phosphorous=less photosynthesis and production

Transpiration

evaporated from plant leaves

Condensation

H2O vapor to liquid H2O

Precipitation

rain, sleet, snow, hail

Infiltration

H2O in soil

Percolation

downward flow into groundwater aquifers

Runoff

downward slope movement to the sea




Increased runoff


Less infiltration to soil &aquifers•Increased flooding•Increased erosion

Absolute humidity

H2O vapor/unit air

Relative humidity

-H2O vapor % maximum air could hold at ToC

Dew point

temperature at which condensation occurs

Condensationnuclei

Water cycle




Particles for H2O vapor to collect precipitation




Volcanic ash, Soil dust, Smoke


Sea salt, Particulate matter (pollution)

purification

Condensation/evaporation distillary


Filtration in rivers, streams, soil, rockto aquifers

Erosion

Moves soil, materials


Sculpssurface of earth

Carbon Cycle

Cycling of carbon in ecosystems between organisms through photosynthesis and cellular respiration, between the ocean and atmosphere which act as major carbon resevoirs, in geological processes through geologic cycles or burning fossil fuels,

Carbon

central element in biological molecules

CO2

key part of biosphere thermostat


–Too much CO2 removed = atm cools


–Too much CO2 generated = atm warms (greenhouse

Carbon cycle amongst organisms

Producers remove CO2 from atm and convert to glucose through consumers and convert it back to CO2 through photosynthesis and cellular respiration

Ocean and Atmosphere for Carbon

Major carbon reservoir


Regulates amount of CO2 inatmosphere


CO2 isreadily soluble in water, some remains dissolved in ocean, some removed by photosynthesis, some reacts with water to form HCO3


Lost through evaporation


Some removed in CaCO3(coral, coralinealgae, mollusks)

Geological Processes for Carbon

CaCO3sediments deposited as limestone, dolomite and fossil fuels



Returnedin long-term geologic cycles or burning fossil fuels

Nitrogen Cycle

NitrogenFixation


Nitrification


Assimilation


Ammonification


Denitrification

NitrogenFixation

N from the atmosphere




Bacteriaconverts gaseous N2 to NH3 (ammonia)




Blue-greenalgae in soil & water–Bacteriain root nodules

Nitrification

Conversion of ammonia to nitrate (NO3-)




NH3 insoil converted in two-step process by aerobic bacteria


–Tonitrite (NO2-)toxic to plants


–Thento nitrate (NO3-)taken up by plants as nutrient

Assimilation

Assimilation of nitrate by plants & conversion to organic-N




Plantroots absorb NH3,NH4 &NO3-




MakeN-containing organic molecules (DNA, AA’s, proteins)

Ammonification

Recycling of organic-N by decomposers




Decomposerbacteria convert N-rich wastes to inorganic:


NH3,NH4

Denitrification

Conversion of ammonia to N2




Byother specialized bacteria (mostly anaerobic)




Water-loggedsoil, sediments in lakes, oceans, swamps


ConvertNH3,NH4 to: Nitrite (NO2-) andnitrate (NO3-)


Theninto N2 gas –released into atmosphere to begin cycle

The Phosphorous Cycle

Essentialelement: DNA, RNA, cell membranes, energy (ATP), bones, teeth




Circulatesthrough water, earth, organisms




Phosphorus often limits productivity




Transformations

Transformations in Phosphorous Cycle

Plants assimilate (PO43-)& incorporate into organic compounds


Animals/bacteria break down organicphosphorus


released as phosphate salts/ions

Phosphorous limits productivity

Aquatic systems: phosphate only slightlysoluble in water


Soils: only readily available between pHof 6-7

Circulatesthrough water, earth, organisms

Very little in atm


Bacteria not very important (as in Ncycle)

HumanPerturbations Phosphorous Cycle

Mining phosphate rock, removing trees, adding excess P to water

The Sulfur Cycle

–Much stored in rocks, minerals, sedimentas sulfate SO42-


–Enters atmosphere


Transformations

How sulfur enters the atmosphere

Hydrogen sulfide (H2S) from Volcanoes, decaying organic matter (swamps, bogs)


Sulfur dioxide (SO2)from volcanoes


Sulfate (SO42-) insea spray


Dimethylsulfide from marine algae

How Sulfur is transformed

–Sulfate assimilated to organic sulfur


–Excess S excreted & decomposersoxidize to sulfate

•HumanPerturbations with the Sulfur Cycle



- Acid Rain •


Often associated with iron (FeS) – released when coal/oil burned •


SO2 combines with O2 & H2O forming H2SO4

chemoautotrophs

not photosynthetic




–Reduce inorganic carbon (from CO2)using energy obtained from oxidation of inorganic substrates:


•methane (CH4)


•hydrogen


•ammonia (NH3)


-nitrifying bacteria


•nitrite (NO2-)


-nitrifying bacteria


•hydrogen sulfide (H2S),sulfate (SO42-),sulfur•ferrous iron salts



riffles

•Fast flowwater with high primary productivity•Diatoms,moss, blue-green algae



Pools

site of respiration and decomposition


CO2 production supplies carbon for photosynthesis for organisms to other parts of the stream or river.

Headwaters

shallow, cold, swift


low productivity: 90% from surrounding vegetation



Nertic province

Water over continental and island shelves




Shallow – sunlight for photosynthesis




Input of nutrients from land – forphotosynthesis




Very productive waters – 8% of oceansurface but >80% of harvest from ocean

Oceanic Province

Open ocean away from continents


photosynthesis only on upper few 100 meters


most ocean below photic zone: no photosynthesis


in open waters plenty of sunlight but nutrients are limiting


large amount of photosynthesis by plankton but low biomass


energy diversity of open water lower than intertidal

Pelagic

on the water column photic

Benthic

on bottom

Epipelagic

me

Abyssal

deep sea

photic

light

aphotic

nonlight

Intertidal

low and high tides


main challenge: being outside of the water

standard answer for biodiversity

all nature is in between and removing pieces affects the whole

Human benefits from biodiversity

food, medicine, industrial products

Communities provide essential services

maintenance of atmosphere composition


maintenance of soil composition


Reservoir of natural economics



Biodiversity maintains optimal community functions

communities function best when they have full compliment of species

Factors responsible for for Extinction

Habitat reduction and modification


Fragmentation


Edges


Isolated Islands



Small population sizes

Random extinctions

Introduction of Exotic Species

Decreases in habitat quality frequently result from introduced predators

Overexploitation

many species have succumbed to effect of direct exploitation by humans

Island Extinction

DoDo Bird


80 years to go extinct


destroyed forest habitat and introduced pigs dogs and rats

ICUN

International Union for the conservation of Nature




Red list

Biome

climate, geological features, and soil continue to shape the physical environment

Climate Zones

terrestrial biomes delineated based on annual patterns of water and temperature




conditions of moisture and temp inflience plant forms present in different terrestrial regions

Characteristic Vegetation

physical environment establishes limits of plant distribution




RAINFALL

Biome boundaries

boundaries correspond to climate zones (temp and rainfall)


tropical


temperate


polar

Tropical Climate Zones

close to equator


temperature flux more annually


warm climate and plants adapted to warm




trop rainforest


trop seasonal forest/savanah


subtrop

Temperate Climates

moderate climates


limited growing season


vegetation dominated by deciduous trees and no small trees or shrubs




temp rainforest


temp seasonal forest


woodland/shrubery


temp grassland

High Lattitude

average temp below 5 C


boreal forest develops between temps of 5 and -5


tundra develops