The Biosphere and Animal Distribution Chapter 37.
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Transcript of The Biosphere and Animal Distribution Chapter 37.
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The Biosphere and Animal Distribution
Chapter 37
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Earth Environment - OverviewWater has physical properties critical to life on
earth.
The steady supply of sunlight maintains a suitable range of temperatures for life metabolism.
Living matter requires a supply of major and minor elements available on earth.
The earth’s gravity is strong enough to hold an extensive gaseous atmosphere.
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Earth EnvironmentThe environment is modified by organisms.
Organisms are adapted by evolution to the environment.
The earth is an open system with a continuous supply of energy.
Building materials for life come from producers and are cycled through consumers.
Life is part of a cycle of life-death-decay-recycling.
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Earth EnvironmentThe primitive earth of
4.5 billion years ago had a reducing atmosphere of ammonia, methane, and water and was fit for pre-biotic synthesis of early living forms.This early
atmosphere would be fatal to today’s organisms.
The appearance of free oxygen in the atmosphere is an example of the reciprocity of life and the earth.
Living organisms produce changes in their environment and must adapt and evolve.
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BiosphereThe biosphere
is the thin outer layer of the earth capable of supporting life.Includes living
organisms as well as the physical environments.
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Biosphere - SubdivisionsLithosphere – rocky material of the earth’s outer shell.
Source of mineral elements required for life.
Hydrosphere – water on or near the earth’s surface.
Atmosphere – the gaseous component of the biosphere.Atmospheric oxygen is produced by photosynthesis.
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Greenhouse EffectMaterials in the atmosphere, such as CO2 and
water vapor retain heat, raising atmospheric temperature.Greenhouse effectBurning fossil fuels increases CO2 in the
atmosphere.
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Greenhouse EffectThe greenhouse effect provides conditions essential for
life on Earth.Humans are increasing this effect. Increased temperatures could lead to a rise in sea level
as polar ice melts.
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BiomesVarying combinations of both biotic and abiotic factors
determine the nature of Earth’s many biomes.
Biomes are the major types of ecological associations that occupy broad geographic regions of land or water.
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BiomesEach biome grades into the next – without sharp
boundaries.Boundary areas are called ecoclines.
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Terrestrial BiomesClimate is particularly
important in determining why particular terrestrial biomes are found in certain areas.TemperatureRainfallSolar radiation
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Terrestrial Biomes
The sun’s rays strike higher latitudes at a lower angle.Atmospheric
heating is less.
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Terrestrial BiomesAir warmed at the equator rises and moves toward the
poles.
Replaced by cold air moving away from the poles.
Rotation of the earth complicates this pattern.Three latitudinal cells result.
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Terrestrial BiomesHot, moist air rises at
equator, cools, condenses and provides rainfall (tropical forests).
Warm air flows northward, and sinks at 20-30° latitude – dry.
Air heats, absorbs moisture (desert areas), then the air flows toward the equator again.
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The Distribution of Major Terrestrial Biomes
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General Features of Terrestrial Biomes
Vertical stratification is an important feature of terrestrial biomes.CanopyLow-treeShrub understoryGround layerForest floor (litter
layer)
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Temperate Deciduous ForestTemperate deciduous forests receive rain year-
round. Cold winters and hot, humid summers.Animals may migrate, hibernate, or survive on scarce
available food or stored fat through the winter.
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Coniferous ForestConiferous forests, or taiga, are common in the
northern hemisphere. Evergreens dominantColder, less rain than temperate forests.
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Coniferous ForestMammals that
inhabit coniferous forests include deer, moose, elk, snowshoe hares, wolves, foxes, lynxes, weasels, bears.Adapted for long,
snowy winters.
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Tropical ForestTropical rain forests receive lots of rain and are
generally warm year-round.StratifiedDiverse
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Tropical ForestCanopy – insectivorous birds and bats fly
above the canopy.Fruit bats, canopy birds, and mammals live in the
canopy eating leaves & fruit.
Middle zones are home to arboreal mammals (monkeys, sloths), birds, bats, insects, amphibians.Climbing animals move along the tree trunks feeding
at all levels.
Ground level contains larger mammals (capybara, paca, agouti, pigs) as well as a variety of reptiles and amphibians.
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Tropical ForestNutrients in a tropical forest are tied up in living
organisms.Soil is poor.
Slash and burn agriculture involves removing vegetation to grow crops – but the soil is so poor that the fields must be moved often.
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GrasslandTemperate grasslands receive seasonal
precipitation and have cold winters and hot summers.Prairie
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GrasslandGrasses and herds
of large grazing mammals are dominant.Jackrabbits, prairie
dogs, and ground squirrels are common.
Predators include coyotes, cougars, bobcats, raptors, badgers, and ferrets.
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GrasslandSavannas are tropical grasslands with seasonal
rainfall.
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GrasslandChaparral receives highly seasonal rainfall.
Shrubs and small trees are common.Adaptations to fire.
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TundraTundra has a permanently frozen layer of soil
called permafrost that prevents water infiltration.Very cold, short growing season.Little rain
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TundraTundra is often covered with bogs, marshes, or ponds.Grasses, sedges, and lichens may be common.Lemmings, caribou, musk-oxen, arctic foxes, arctic
hares, ptarmigans and other migratory birds.
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DesertDeserts have very low precipitation – less than 30
cm/yr.Variable temperatures.Animals often nocturnal and live in burrows.Reptiles and small mammals are common.
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Aquatic Biomes
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Aquatic BiomesAquatic biomes account for the largest part of the
biosphere in terms of area.Can contain fresh or salt water.
Oceans cover about 75% of Earth’s surface.Have an enormous impact on the biosphere.
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Inland WatersOnly about 2.5% of the earth’s water is fresh.
Much of that is found in polar ice caps or underground aquifers.
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Inland WatersLotic, or running water habitats include streams and
rivers.More oxygen
Lentic, or standing water habitats include lakes and ponds.Less oxygen
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Inland WatersOligotrophic
lakes – nutrient poor & oxygen rich.
Eutrophic lakes – nutrient rich & sometimes oxygen poor.Eutrophication
An oligotrophic lake A eutrophic lake
LAKES
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Inland WatersStreams and
rivers have a current.
STREAMS AND RIVERS
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Inland WatersAnimals living in vegetation or debris of the bottom
(benthos) are called benthic.Snails, mussels, crustaceans, insects.
Animals up in the water column are pelagic.Swimming animals are called nekton.Floating or weak swimmers are called plankton.
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WetlandsWetlands
include areas that are able to support aquatic plants.
May be freshwater or marine.
WETLANDS
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EstuariesEstuaries are transition
areas between river and sea.Salinity varies from
nearly fresh to the salinity of seawater.
ESTUARIES
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Aquatic BiomesMany aquatic biomes are stratified into zones
or layers defined by light penetration, temperature, and depth.The photic zone is the most productive.
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Rocky Intertidal ZoneThe rocky intertidal zone is alternately
submerged and exposed by the tides.Upper zones are exposed to air longer.Physical stress (desiccation, waves, temp,
salinity), predation, and competition produce distinct bands.
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Rocky Subtidal ZoneKelp forests
dominated by brown seaweeds occupy shallow subtidal waters.Grazing urchins
and molluscs are common.
Predators include sea stars, fishes, and otters.
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Rocky Subtidal ZoneCoral reefs are
limited to the photic zone in tropical marine environments with high water clarity.Highly diverse
CORAL REEFS
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Nearshore Soft SedimentsIntertidal and subtidal environments with soft sediments
include beaches, mudflats, salt marshes, sea-grass beds, and mangrove communities.
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Nearshore Soft SedimentsSalt marsh habitat
includes grasses, mussels, crabs, shrimp, and polychaetes.Burrowing organisms.Deposit or filter
feeders.Small fishes and birds
that feed on them are common.
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Nearshore Soft SedimentsCalm, tropical, coastal
areas support mangrove communities.Mangrove trees grow
submerged in soft sediments.
Rich community of detritus feeders (oysters, crabs, shrimp).
Many fishes – often used as a nursery ground.
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Deep-Sea SedimentsThe deep sea includes the continental slope,
continental rise, and abyssal plain.Sand where there are currents, fine mud where currents
are weak.Suspension feeding invertebrates are common.Deposit feeders found in muddy areas.
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Hydrothermal VentsHydrothermal vents occur on the abyssal plain in
areas of submarine volcanic activity.Archaebacteria that derive energy by oxidizing sulfides
form the basis of the food chain.Grazed by bivalves, limpets, and crabs.Other organisms, like tube worms, have symbiotic
archaebacteria.
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Pelagic RealmThe pelagic realm includes the open ocean area.
High oxygen, low nutrient levels.Areas of upwelling bring nutrients up from the sea floor.
OCEANIC PELAGIC BIOME
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Pelagic RealmEpipelagic – surface
waters
Mesopelagic – twilight zone, supports a varied community of animals.
Deep sea forms depend on a rain of organic debris from above.
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ZoogeographyZoogeography describes patterns of animal
distribution and species diversity.Why species and species diversity are distributed as they
are.
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ZoogeographyThe history of an animal species must be
documented before we can understand why it lives where it does.Camels originated in North America and spread to
Eurasia, Africa, and South America.Camels went extinct in North America 10,000 years
ago.Today, we see true camels in Eurasia & Africa and
camel descendents (llamas, alpacas etc) in South America.
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ZoogeographyGeologic change is responsible for much of the
alteration in animal distribution.
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ZoogeographyPhylogenetic systematics allows us to reconstruct
histories of animal distributions.Geographical distributions of closely related species are
mapped onto a cladogram to generate hypotheses of the geographic history.
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ZoogeographyDisjunct distributions are closely related species that
live in widely separated areas.Dispersal – a population moves to a new location.Vicariance – environmental changes break up a once
continuous population into small pockets.
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Distribution by DispersalDispersal involves emigration from one region and
immigration into another.One way outward movement.
Different from a periodic movement back & forth.
Active or passiveCenter of originExplains movement of animal populations into favorable
habitats adjacent to the place of origin.
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Distribution by VicarianceAreas once joined may become separated by barriers.
Population becomes fragmented into smaller, isolated populations.
Lava flowsContinental driftEmergence of mountain ranges
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Distribution by VicarianceVicariance by continental
drift helps to explain the disjunct distribution of ratite birds.Ancestral species
widespread throughout Southern Hemisphere.
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Distribution by VicarianceAs the continents
moved apart, the ancestral species was fragmented into disjunct populations that evolved independently producing the diversity seen today.
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Continental DriftThe concept of continental drift was proposed by
Alfred Wegener in 1912.Not fully accepted until the mechanism was found.
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Continental DriftPlate tectonics is the mechanism of continental drift.
The earth’s surface is composed of 6-10 rocky plates which shift position on a more malleable underlying layer.
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Continental DriftPangaea – the single great landmass – broke up 200
million years ago.Two supercontinents resulted:
Laurasia – North America, Eurasia, GreenlandGondwana – South America, Africa, Madagascar, Arabia,
India, Australia, New Guinea, Antarctica
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Continental DriftContinental drift explains several puzzling distributions
of animals.Similarity between some organisms in South America and
Africa.
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Continental Drift - The Case of Marsupial Evolution
Marsupials appeared about 100 million years ago in South America.
They spread through Antarctica and Australia that were at that time joined together.
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Continental Drift - The Case of Marsupial Evolution
Marsupials encountered placental mammals in North America, could not compete, and became extinct. The modern opossums are recent arrivals from South America.
The placental mammals expanded into South America, but the marsupials were well established there.
About 50 million years ago, Australia drifted apart from Antarctica and remained in isolation with only marsupials to diversify on the continent.
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Wallace’s LineWallace’s line
represents a geographic separation between Asian and Australian faunas.
A collision of tectonic plates brought formerly distant land masses closer together.
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Temporary Land BridgesTemporary land bridges
have been important pathways for dispersal.Land bridge connected
Asia and North America across the Bering Strait.
Today, a land bridge connects North and South America
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Climatic Cycles and Vicariance
Glacial cycles have occurred with durations of 20,000 to 100,000 years within the past three million years.
Taxa sharing the same areas typically differ greatly in evolutionary age and in phylogenetic branching pattern.
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Climatic Cycles and Vicariance
Cycling temperatures interact with the habitat requirements of animals.