Biogeography exam 2- Ashton Sanchez

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124 Terms

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small scale dispersal

A small-scale ecological
process that is part of the life
history of every species

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large scale dispersal

Some dispersal is large-scale:
changes a species’ geographical
distribution

To change a species’ geographical distribution, the species must be able to:
Travel to a new area
Withstand unfavorable conditions during the move

survive after arrival (viable population)

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Jump Dispersal

Long-distance dispersal accomplished by movement of individuals within a relatively short period

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Diffusion

Much slower than jump dispersal
Typically occurs over generations by populations gradually spreading out from the
margins of a species’ previous range
May follow one another

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Secular Migration

Expansion occurring over timescales of many generations, providing
opportunities for evolutionary change

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active dispersal

mowing under own power- example monarch butterfly

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passive dispersal

carried by physical agent such as wind water or another organism- common in plants such as diaspores (dandelion)

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phoresy

small animals are transported long distance by other animals

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barrier to dispersal one

physiological

temperature

salinity

change in elevation tends to be a greater barrier to dispersal in tropics compared to higher latitudes

aquatic organisms cannot regulate water and salt balance when facing other environment from normal

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barriers to dispersal two

ecological/physical

habitat selection- ability to recognize and respond appropriately to favorable enviornments

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corridor

A dispersal route that permits the movement of many or most species of a
particular taxon between one region and another

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tethyan seaway

knowt flashcard image
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Filter

A dispersal route that is more restrictive than a corridor. It selectively blocks
the passage of certain forms while allowing those able to tolerate the
conditions of the barrier to migrate freely

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Sweepstakes

Barriers only crossed by rare, chance interchanges

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Active vs passive dispersal curves

knowt flashcard image
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How can habitat selection influence the ability of a species to establish itself after dispersal?

It determines if a disperser finds resources for survival and reproduction. Poor selection leads to death, while good selection allows a population to grow.

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Propagule

It is the group of individuals that disperses to found a new population. Its size and genetic diversity influence establishment success.

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How can the type of reproduction influence the ability to establish a population?

Species with asexual reproduction can establish from a single individual. Sexual species require mates, making establishment harder in low-density areas.

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Evolutionary Species Concept

A lineage with its own evolutionary history and fate. It emphasizes a single, continuous lineage through time.

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Morphological Species Concept

Groups of individuals that are morphologically similar to one
another and are morphologically distinct from other such groups

<p><span style="color: rgb(255, 255, 255);">Groups of individuals that are morphologically similar to one</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">another and are morphologically distinct from other such groups</span></p>
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Biological Species Concept

Species are groups of actually or potentially interbreeding
populations that are reproductively isolated from other such groups

<p><span style="color: rgb(255, 255, 255);">Species are groups of actually or potentially interbreeding</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">populations that are reproductively isolated from other such groups</span></p>
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Phylogenetic Species Concept

Smallest possible group descending from a common ancestor and
recognizable by unique, derived traits (smallest monophyletic groups)

<p><span style="color: rgb(255, 255, 255);">Smallest possible group descending from a common ancestor and</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">recognizable by unique, derived traits (smallest monophyletic groups)</span></p>
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What is a subspecies?

A subspecies is an
aggregate of phenotypically
similar populations of a
species inhabiting a
geographic subdivision of
the range of that species and
differing taxonomically from
other populations of that
species."
Peromyscus (deer mouse) – found in different
ecological conditions

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What is the difference between microevolution and macroevolution?

micro-within species

macro-speciation

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Cladogenesis

a branching process in which new kinds of organisms
originate from a single ancestral species

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Reticulate speciation

new species can also arise through hybridization

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Anagenesis (phyletic speciation)

the transformation of an ancestral
species into a single descendant species by accumulation of changes
over many generations

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What are the 4 main forces of evolution?

mutation

gene flow

genetic drift

natural selection

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Understand how geographic variation in organisms is generated by differences in gene flow and local adaptation

A geographic component to genetic divergence
Both genetic drift and natural selection are facilitated, and gene flow is
impeded, by geographic isolation

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What is a ring species?

Substantial interbreeding among adjacent
populations along the contiguous ring
Apparent reproductive isolation between
the terminal subspecies in the complex

<p><span style="color: rgb(255, 255, 255);">Substantial interbreeding among adjacent</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">populations along the contiguous ring</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">Apparent reproductive isolation between</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">the terminal subspecies in the complex</span><span style="color: rgb(255, 255, 255);"><br></span></p>
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Be able to describe allopatric speciation (modes I and II)
o Understand the Galapagos tortoise and Darwin’s Finches examples

Allopatric speciation:
Requires geographic isolation
Sympatric speciation:
Does NOT require geographic
isolation

Allopatric speciation mode I: Vicariance
An ancestral species (a) widely distributed throughout a geographic area
Original species distribution subdivided by the formation of a
geographic barrier (vicariance)
With gene flow prevented, populations diverge from one another over time and
eventually can be rec-ognized as separate species, b and c.

allopatric speciation mode 2: peripheral isolates (founder events)


Random dispersal of members of the geographically wide-spread species a to
peripheral areas initiates new, geographically isolated populations
Over time, the new peripherally isolated populations diverge to form new species b, c,
and d

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In the context of allopatric speciation, what is reinforcement?

he increase of reproductive isolation between
populations through selection against hybrid offspring

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sympatric speciation and cause

If the geographic overlap of populations of the ancestral species is extensive

Speciation without geographic isolation, often driven by ecological specialization or polyploidy. It can occur within a single population's range.

<p><span>If the geographic overlap of populations of the ancestral species is extensive</span></p><p><span>Speciation without geographic isolation, often driven by ecological specialization or polyploidy. It can occur within a single population's range.</span></p>
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parapatric speciation and cause

If the populations are largely allopatric but overlap in a narrow zone where
depressed fitness of the offspring of interpopulation matings leads to
selection for isolating mechanisms

Speciation between adjacent populations with limited gene flow. Divergence happens along an environmental gradient without a full physical barrier.

<p><span style="color: rgb(255, 255, 255);">I</span><span style="color: rgb(255, 255, 255);">f the populations are largely allopatric but overlap in a narrow zone where</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">depressed fitness of the offspring of interpopulation matings leads to</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">selection for isolating mechanisms</span></p><p><span>Speciation between adjacent populations with limited gene flow. Divergence happens along an environmental gradient without a full physical barrier.</span></p>
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aneuploidy

A single chromosome breaks or fuses with another to change the total number by
plus or minus one

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polyploidy (autopolyploidy and allopolyploidy)

An entire additional set of chromosomes is passed on, changing the number by some multiple (e.g., a doubling or tripling

autopolyploidy-within a population

allopolyploidy-result of hybridization between different but closely related populations or species

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What is an adaptive radiation?

cichlid and pupfish examples

The rapid evolution of many diverse species from a common ancestor, filling various ecological niches. It is often triggered by new habitats, key innovations, or freed-up resources.

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forces that causes diversification and lead to adaptive radiations

competitive exclusion

character displacement

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competitive exclusion

Two or more resource-limited species cannot persist in a stable
environment without segregation of their realized niches
In biogeographic terms:
Species that are extremely similar in their niches tend to have non-
overlapping geographic distributions
Species that coexist in the same area and habitat tend to differ
substantially in their resource use

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character displacement

Character Displacement
Species tend to be more different from one another where they occur together, presumably reflecting
adaptive divergence that reduces competition

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adaptive radiation examples

darwins finches

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Red queen hypothesis

A species must continually evolve to keep pace with an ever-changing environment
Abiotic conditions are shifting
All the other species are evolving, altering the availability of resources and the
patterns and processes of biotic interactions
The probability of extinction is constant over time

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background extinction

he normal rate of extinction for a taxon or biota

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mass extinction

statistically significant increase above background
extinction rate

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number of mass extinctions

five

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general causes of mass extinction

Massive volcanism, asteroid impacts, and dramatic changes in sea level or climate.

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primary cause of permian mass extinction

Massive volcanic eruptions in the Siberian Traps, leading to extreme global warming and ocean anoxia.

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primary cause of end-cretateous mass extinction

A large asteroid impact at Chicxulub, Mexico, causing a "impact winter.”

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bradytelic

very slow speciation

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horotelic

standard rate of speciation

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tachytelic

very fast speciation

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gradualism and punctuate equilibrium

knowt flashcard image
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How does species selection influence the probability of a species going extinct?

Species must have emergent and heritable traits beyond those molded by
microevolutionary processes acting on individuals within a species

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How did the rise of mammals differ from the rise of angiosperms?

explosive radiation of placental mammals vs gradual radiation of angiosperms

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Chronological order of eons

phanerozoic

Precambrian

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chronological order of eras

cenozoic

mesozoic

paleozoic

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order of periods

quaternary

tertiary

cretaceous

jurrassic

triassic

permian

pennslyvanian

mississippian 

devonian

silurian

ordovician

cambrian

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order of cenozoic epochs

quarternary

neogene

paleogene

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Stratigraphy

Each layer of sedimentary origin (and at least some of metamorphic origin) in a stratigraphic column
contains a unique assemblage of fossils characteristic of a particular time span
Layers of rock: strata (singular: stratum)

oldest straa will lie at bottom (law of superposition)

<p><span style="color: rgb(255, 255, 255);">Each layer of sedimentary origin (and at least some of metamorphic origin) in a stratigraphic column</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">contains a unique assemblage of fossils characteristic of a particular time span</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">Layers of rock: strata (singular: stratum)</span></p><p><span style="color: rgb(255, 255, 255);">oldest straa will lie at bottom (law of superposition)</span></p>
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The use of index fossils

Fossil assemblages used to correlate ages of rock strata in one region with
those in distant localities

<p><span style="color: rgb(255, 255, 255);">Fossil assemblages used to correlate ages of rock strata in one region with</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">those in distant localities</span></p>
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Dendrochronology

knowt flashcard image
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absolute dating

How are radioactive isotopes used?

The decay of unstable parent isotopes into stable daughter isotopes at a constant rate is measured.

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absolute dating

What is a half-life?

The time it takes for half of the parent isotope in a sample to decay into the daughter product.

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Who was Alfred Wegener?

A meteorologist who proposed the theory of continental drift.

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evidence for continental drift

coastlines fit together like puzzle pieces

geologic similarities between south america africa and india

flood basalts split across continents

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what is importance of sea floor spreading

Close to ridge = young
Age increases with distance

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importance of paleomegnetism

provides physical evidence for spreading of seafloor

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different layers of earth

crust

mantle

outer core

inner core

lithosphere is crust and upper solid part of mantle

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types of plate movement

ridge push-pushes up through mantle and forms new parts of plate

mantle drag-friction between mantle and plate create drag force

subduction-plates are pulled into magma

<p>ridge push-pushes up through mantle and forms new parts of plate</p><p>mantle drag-friction between mantle and plate create drag force</p><p>subduction-plates are pulled into magma </p>
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ways in which plate boundaries interact

subduction

spreading

slip strike-plates moving against eachother laterally (left right)

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<p>assembly/dissasembly of pangea</p>

assembly/dissasembly of pangea

begins to assemble in devonian, assembled in permian

begins to break in jurassic, dissasembled in cretaceous

<p>begins to assemble in devonian, assembled in permian</p><p>begins to break in jurassic, dissasembled in cretaceous</p>
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origin of laurasia

jurassic

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modern continents of laurasia

Northern landmass that became North America, Europe, and Asia.

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origin of gondawana

jurassic

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modern contintents of gondwana

Southern landmass that became South America, Africa, Antarctica, Australia, and India.

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<p><span style="color: rgb(255, 255, 255);">Understand the sequence of events that led to the breakup of Gondwana and the fates of the</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">separate continents</span></p>

Understand the sequence of events that led to the breakup of Gondwana and the fates of the
separate continents

early jurassic splits into east and west

then splits into north south quadrants

<p>early jurassic splits into east and west </p><p>then splits into north south quadrants</p>
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Understand how movements of plates influenced the development of islands in the Pacific Basin

Which plates were involved?

pacific and australian plates

subduction formed island arcs and volcanoes

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Understand how movements of plates influenced the Indo-Australian region and Wallacea
Which plates were involved?

eurasian, pacific, indian

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What is Wallacea?

A biogeographical region of islands between the Asian and Australian continental shelves. It is a mixing zone with unique species from both regions.

<p><span>A biogeographical region of islands between the Asian and Australian continental shelves. It is a mixing zone with unique species from both regions.</span></p>
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Understand the formation of Central America and the Caribbean

landmass covered by shallow sea, volcanoe formation created islands

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What are epeiric (epicontinental) seas?

Shallow seas that cover continental interiors.

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How did the direction of the Amazon River change and what was the cause?

It originally flowed west, but the rise of the Andes reversed its flow to the east.

<p><span>It originally flowed west, but the rise of the Andes reversed its flow to the east.</span></p>
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origin of Mediterranean sea

tethyan seaway was cut off by retreat of oceans

<p>tethyan seaway was cut off by retreat of oceans</p>
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origin of red sea

great rift valley was cutoff by rising landmasses

<p>great rift valley was cutoff by rising landmasses</p>
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how do hotspots form oceanic islands

Stationary mantle plumes (hotspots) form volcanic island chains as plates move over them.

<p><span>Stationary mantle plumes (hotspots) form volcanic island chains as plates move over them.</span></p>
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how do triple junctions form oceanic islands

Triple junctions are where three plates meet, creating complex geological features.

<p> Triple junctions are where three plates meet, creating complex geological features.</p>
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what was the effect of isolation on Antarctica

The separation of Australia and South America from Antarctica established the cold Antarctic Circumpolar Current as
deep water flowed through the Drake Passage (DP) between Antarctica and South America and over South Tasman
Rise (STR) between Australia and Antarctica. Subsequently, reduced mixing of cold Antarctic waters with those of
warmer regions resulted in the onset of global cooling.

<p><span style="color: rgb(255, 255, 255);">The separation of Australia and South America from Antarctica established the cold Antarctic Circumpolar Current as</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">deep water flowed through the Drake Passage (DP) between Antarctica and South America and over South Tasman</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">Rise (STR) between Australia and Antarctica. Subsequently, reduced mixing of cold Antarctic waters with those of</span><span style="color: rgb(255, 255, 255);"><br></span><span style="color: rgb(255, 255, 255);">warmer regions resulted in the onset of global cooling.</span><span style="color: rgb(255, 255, 255);"><br></span></p>
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Consequences of plate techtonics table

physical isolation of antartica

closure of tethyan seaway

collision of australia with southeast asia

uplift of central american land bridge

<p>physical isolation of antartica</p><p>closure of tethyan seaway</p><p>collision of australia with southeast asia</p><p>uplift of central american land bridge</p>
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What time period is the Pleistocene?

From about 2.6 million to 11,700 years ago.

last glacial maximum was 18000 yrs ago

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What is the difference between a glacial and an interglacial?

A glacial is a cold period with extensive ice sheets. An interglacial is a warmer period between glacials, like the present.

glacial-advancement

interglacial-retreat

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proximate cause of glaciation

What is albedo and how does it influence temperature?

The fraction of the incident sunlight that is reflected by a surface

<p><span>The fraction of the incident sunlight that is reflected by a surface</span></p>
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<p>three components of Milankovitch cycles</p><p><span style="color: rgb(255, 255, 255);">o Variation in eccentricity-rotation around sun<br>o Variation in obliquity-turn of earth on axis<br>o Variation in precession-rotation of earth on its own axis</span></p>

three components of Milankovitch cycles

o Variation in eccentricity-rotation around sun
o Variation in obliquity-turn of earth on axis
o Variation in precession-rotation of earth on its own axis

Changes in the characteristics of Earth’s orbit around the sun have been among the key drivers of
global climate change in the Phanerozoic eon, especially during the Pleistocene epoch

  • Eccentricity: Shape of Earth's orbit (100,000-year cycle).

  • Obliquity: Tilt of Earth's axis (41,000-year cycle).

  • Precession: Wobble of the axis (26,000-year cycle).

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how do variables affect isolation and temp in milankovitch cycle

insolation- total solar radiation reaching earth

drives climactic cycles

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more prominent area of pleistocene glaciation

  • More Prominent: Northern North America and Eurasia.

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less prominent area of pleistocene glaciation

  • Less Prominent: The tropics and many deserts.

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<p>evidence for glaciation</p>

evidence for glaciation

• Glacial till Unsorted sediment deposited directly by glacier ice.
• Drumlins
Elongated hills of glacial till, shaped by moving ice.
• Kames
Mounds of sand and gravel deposited by meltwater.
• Eskers
Long, winding ridges of sand and gravel from subglacial streams.
• Kettle Lakes
Lakes formed by melting ice blocks left in glacial deposits.
• Moraines
Ridges of till marking the former edges of a glacier.

<p><span style="color: rgb(255, 255, 255);">• Glacial till </span><span>Unsorted sediment deposited directly by glacier ice.</span><span style="color: rgb(255, 255, 255);"><br>• Drumlins </span><span>Elongated hills of glacial till, shaped by moving ice.</span><span style="color: rgb(255, 255, 255);"><br>• Kames </span><span>Mounds of sand and gravel deposited by meltwater.</span><span style="color: rgb(255, 255, 255);"><br>• Eskers </span>Long, winding ridges of sand and gravel from subglacial streams.<span style="color: rgb(255, 255, 255);"><br>• Kettle Lakes </span>Lakes formed by melting ice blocks left in glacial deposits.<span style="color: rgb(255, 255, 255);"><br>• Moraines </span><span>Ridges of till marking the former edges of a glacier.</span></p><p></p>
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glacial till

• Glacial till Unsorted sediment deposited directly by glacier ice.

<p><span style="color: rgb(255, 255, 255);">• Glacial till </span>Unsorted sediment deposited directly by glacier ice.</p>
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drumlins


• Drumlins
Elongated hills of glacial till, shaped by moving ice.

<p><span style="color: rgb(255, 255, 255);"><br>• Drumlins </span>Elongated hills of glacial till, shaped by moving ice.</p>
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kames

• Kames Mounds of sand and gravel deposited by meltwater.

<p><span style="color: rgb(255, 255, 255);">• Kames </span>Mounds of sand and gravel deposited by meltwater.</p>
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eskers

• Eskers Long, winding ridges of sand and gravel from subglacial streams.

<p><span style="color: rgb(255, 255, 255);">• Eskers </span>Long, winding ridges of sand and gravel from subglacial streams.</p>

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