1/70
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No analytics yet
Send a link to your students to track their progress
Glaciations
A period when global climate cools significanltly
What happens in glaciations?
Continental ice sheets expand, sea level drop, ecosystems shift.
Repeated glaciations in the last ___ million years
2.6 my
~___ major glaciations in the past million years
~10
major glaciations in the last _
3, 150,000 years
Last Glacial Maximum(LGM) was ___ years ago.
~18,000 ya
Last Glacial Maximum (LGM)
Sheets of ice, sea level drop ~120m
Causes of Glaciation
Linked to variation in Earths Orbit, Eccentricity, Tilt, Orbital precession
Linked to variation in Earths Orbit
Cyclic variation Affects solar heating, Milankovitch Cycles
Eccentricity
Shape of orbit
Eccentricity happen when ..
Orbits shifts between circular and elliptical
Eccentricity was ____
~95,000-100,000 years ago
Eccentricity affects the…
Distance to the sun
More elliptical:
Cooler summers, ice sheets grow, ice and snow don’t melt
Obliquely - Tilt
Earth can slightly shift how tilted it is
Tilt was roughly…
~ 41,000 years ago
Larger Tilt
Stronger seasons, warmer summers (more melting), cooler winters (more snow, cannot offset melting)
Smaller tilt
Cooler summers, glaciers grow
Precision - Wobble
Changes timing of seasons
Wobble - changing timing of seasons
Determines which hemisphere leans towards or away from the sun
If cooler summers in northern hemisphere,…
see ice sheets survive and glaciation increases
Wobble occurred…
~22,000-26,000 years
Wobble comes from..
gravitational pull from sun and moon
Cycle Type
Procession, obliquity (tilt), eccentricity
Procession - Period
~22,000 yrs
Procession - What it changes
Wobble of Earth’s axis
Procession - Impact
Alters timing of seasons
Obliquity (tilt) - Period
~41,000 years
Obliquity (Tilt) - What it changes
Axial tilt angle
Obliquity (Tilt) - Impact
Controls seasonal contrast
Eccentricity - Period
~95,000-100,000 years
Eccentricity - what it changes
Shape of orbit
Eccentricity - Impact
Controls distance to Sun
Why Northern Hemisphere?
Has most of continental land mass
Has most of continental land mass
Ice grows on land, not ocean. Cool summers = ice age growth. Warm summer = ice age retreat.
Effects of Last Glaciation - Land
5-7C cooler on average
Effects of Last Glaciation - Water and air
2-3C cooler on average
Effects of Last Glaciation - Ice Sheets
Massive ones covered N hemisphere
Effects of Last Glaciation - Great Lakes
Shaped by glacier movement
Effects of Last Glaciation - Sea Levels
Drastically lowered, ~430 ft, Water became locked in glacial ice, Exposed large portion of continental shelf
Effects of Last Glaciation - Land Bridge Formation - Beringia
Allowed humans to migrate into North America and horses to cross into Asia
Effects of Glaciation - Doggerland
Connected Europe and Britain. English channel was land. Ireland remained isolated. Large costal pains created new habitat (Megafauna)
How do glaciers change environments?
Glaciers can move seidment
Glaciers can move sediment
Take from one area, and move it with the glaciers as it moves. Increase erosion. Increase freeze-thawing erosion
Glaciation: Shifts in Rain Belts
African rain belt shifted south. Congo rainforests became sand dunes. lake Tanganyika 400m shallower.
LGM
Last Glacial Maximum. 18,000 years
Lake Tanganyika
Shrunk into three separate basins. Isolated promoted speciation (Why more fish than in any other lakes now)
Post Glacial Climate - Rain returns
~10,000-7,000. Monsoons strengthen. Lakes became much deeper.
Post Glacial Climate - Expansion of
Wetlands, Megafauna habitats, Early human population boom
Post Glacial Climate - 5,000 years ago
Increase moisture in SE North America. Arizona greener, less desert. Indigenous settlements thrived.
Shifting Biotic Ranges
Climate zones moved during glacial cycles
Climate zones moved - Changed migration patterns
Wildebeest following the shifting grasslands, Hummingbirds tracked seasonal flowering shifts
Climate zones moved - Changed where plants could survive
Pushed trees and vegetation towards equator, Shifted organisms to lower elevation
Shifting Biotic Ranges - What about non mobile organisms?
Local extinctions. Soil microbes/things that don’t move fast enough
North American Forests
Mountains run north south. Forests could expand south ahead of moving glaciers
Europe Forests
Mountains run east west. Forests cannot shift south, they get trapped by mountains. Trapped between ice sheets and mountains.
North America - Mountain Orientation
North-South ranges (Appalachians, Rockies)
North America - Forest ability to move
Trees migrated south ahead of glaciers
North America - Glacial survival
Large refuge zones
North America - Tree diversity today
~600 species
Europe - Mountain orientation
East-West ranges (Pyrenees, Alps, Carpathians)
Europe - Forest ability to move
Trees trapped between ice sheets and mountains
Europe - Glacial survival
Small, fragmented refuges
Europe - Tree diversity today
~85 species
How this shapes where organisms live
Climate, Biota, Time, history
How this shapes where organisms live - Climate
physical factors
How this shapes where organisms live - Biota
Competition, predation, herbivory, mutualism
How this shapes where organisms live - Time
Successional stage, disturbance frequency
How this shapes where organisms live - history
Continental drift, glaciations, extinctions, colonization route
During glacial maximums, species ranges typically shift where?
Towards the equator
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