Glaciations

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Last updated 3:32 PM on 12/8/25
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71 Terms

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Glaciations

A period when global climate cools significanltly

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What happens in glaciations?

Continental ice sheets expand, sea level drop, ecosystems shift.

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Repeated glaciations in the last ___ million years

2.6 my

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~___ major glaciations in the past million years

~10

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major glaciations in the last _

3, 150,000 years

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Last Glacial Maximum(LGM) was ___ years ago.

~18,000 ya

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Last Glacial Maximum (LGM)

Sheets of ice, sea level drop ~120m

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Causes of Glaciation

Linked to variation in Earths Orbit, Eccentricity, Tilt, Orbital precession

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Linked to variation in Earths Orbit

Cyclic variation Affects solar heating, Milankovitch Cycles

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Eccentricity

Shape of orbit

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Eccentricity happen when ..

Orbits shifts between circular and elliptical

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Eccentricity was ____

~95,000-100,000 years ago

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Eccentricity affects the…

Distance to the sun

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More elliptical:

Cooler summers, ice sheets grow, ice and snow don’t melt

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Obliquely - Tilt

Earth can slightly shift how tilted it is

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Tilt was roughly…

~ 41,000 years ago

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Larger Tilt

Stronger seasons, warmer summers (more melting), cooler winters (more snow, cannot offset melting)

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Smaller tilt

Cooler summers, glaciers grow

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Precision - Wobble

Changes timing of seasons

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Wobble - changing timing of seasons

Determines which hemisphere leans towards or away from the sun

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If cooler summers in northern hemisphere,…

see ice sheets survive and glaciation increases

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Wobble occurred…

~22,000-26,000 years

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Wobble comes from..

gravitational pull from sun and moon

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Cycle Type

Procession, obliquity (tilt), eccentricity

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Procession - Period

~22,000 yrs

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Procession - What it changes

Wobble of Earth’s axis

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Procession - Impact

Alters timing of seasons

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Obliquity (tilt) - Period

~41,000 years

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Obliquity (Tilt) - What it changes

Axial tilt angle

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Obliquity (Tilt) - Impact

Controls seasonal contrast

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Eccentricity - Period

~95,000-100,000 years

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Eccentricity - what it changes

Shape of orbit

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Eccentricity - Impact

Controls distance to Sun

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Why Northern Hemisphere?

Has most of continental land mass

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Has most of continental land mass

Ice grows on land, not ocean. Cool summers = ice age growth. Warm summer = ice age retreat.

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Effects of Last Glaciation - Land

5-7C cooler on average

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Effects of Last Glaciation - Water and air

2-3C cooler on average

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Effects of Last Glaciation - Ice Sheets

Massive ones covered N hemisphere

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Effects of Last Glaciation - Great Lakes

Shaped by glacier movement

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Effects of Last Glaciation - Sea Levels

Drastically lowered, ~430 ft, Water became locked in glacial ice, Exposed large portion of continental shelf

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Effects of Last Glaciation - Land Bridge Formation - Beringia

Allowed humans to migrate into North America and horses to cross into Asia

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Effects of Glaciation - Doggerland

Connected Europe and Britain. English channel was land. Ireland remained isolated. Large costal pains created new habitat (Megafauna)

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How do glaciers change environments?

Glaciers can move seidment

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Glaciers can move sediment

Take from one area, and move it with the glaciers as it moves. Increase erosion. Increase freeze-thawing erosion

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Glaciation: Shifts in Rain Belts

African rain belt shifted south. Congo rainforests became sand dunes. lake Tanganyika 400m shallower.

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LGM

Last Glacial Maximum. 18,000 years

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Lake Tanganyika

Shrunk into three separate basins. Isolated promoted speciation (Why more fish than in any other lakes now)

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Post Glacial Climate - Rain returns

~10,000-7,000. Monsoons strengthen. Lakes became much deeper.

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Post Glacial Climate - Expansion of

Wetlands, Megafauna habitats, Early human population boom

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Post Glacial Climate - 5,000 years ago

Increase moisture in SE North America. Arizona greener, less desert. Indigenous settlements thrived.

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Shifting Biotic Ranges

Climate zones moved during glacial cycles

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Climate zones moved - Changed migration patterns

Wildebeest following the shifting grasslands, Hummingbirds tracked seasonal flowering shifts

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Climate zones moved - Changed where plants could survive

Pushed trees and vegetation towards equator, Shifted organisms to lower elevation

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Shifting Biotic Ranges - What about non mobile organisms?

Local extinctions. Soil microbes/things that don’t move fast enough

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North American Forests

Mountains run north south. Forests could expand south ahead of moving glaciers

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Europe Forests

Mountains run east west. Forests cannot shift south, they get trapped by mountains. Trapped between ice sheets and mountains.

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North America - Mountain Orientation

North-South ranges (Appalachians, Rockies)

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North America - Forest ability to move

Trees migrated south ahead of glaciers

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North America - Glacial survival

Large refuge zones

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North America - Tree diversity today

~600 species

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Europe - Mountain orientation

East-West ranges (Pyrenees, Alps, Carpathians)

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Europe - Forest ability to move

Trees trapped between ice sheets and mountains

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Europe - Glacial survival

Small, fragmented refuges

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Europe - Tree diversity today

~85 species

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How this shapes where organisms live

Climate, Biota, Time, history

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How this shapes where organisms live - Climate

physical factors

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How this shapes where organisms live - Biota

Competition, predation, herbivory, mutualism

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How this shapes where organisms live - Time

Successional stage, disturbance frequency

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How this shapes where organisms live - history

Continental drift, glaciations, extinctions, colonization route

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During glacial maximums, species ranges typically shift where?

Towards the equator

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Why does Europe have fewer species than North America?

During glaciation, Europe trees were trapped by the E-W mountain ranges, so thy couldn’t escape the moving glaciers