California
State University Long Beach
GEOL 300i; Earth Systems
and Global Change
Lecture 19
Dr.
Rick Behl
Rapid climatic change
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Abrupt or shorter-lived than Milankovitch
band cycles
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Related to switching on/off or changing the
global conveyor belt
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Changes equator-pole heat flow
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Changes CO2 reservoir
-
I.e., Younger Dryas cold episode
Dansgaard-Oeschger interstadials
(warm episodes)
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More than 2 dozen rapid warming events during
last ice age (last 125,000 years)
-
Previously unknown from marine sediment records
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Occur irregularly approximately every 1500-2000
years
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Discovered in the Greenland ice cores, and
shown by:
-
Oxygen isotopes (temperature)
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Up to 8-10°C in a few decades
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Dust (continental aridity and wind)
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Snow (precipitation)
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Higher rates of accumulation
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CO2 and Methane (CH4)
Heinrich events
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Huge iceberg armadas that covered the North
Atlantic
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Recorded by 6 layers of ice-rafted sediment
in deep sea ooze in the past Ice Age
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Occurred after about every 2-4 Dansgaard-Oeschger
events
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During very cold intervals
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Approximately every 6100 years
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Finale of series of increasingly colder episodes
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In between the D-O warm events
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Sedimentation rates in the N. Atlantic are
too low to record the more rapid D-O events
Rapid change in the Pacific Region
Santa Barbara basin
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Ultra-high-resolution sedimentary record
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Very high sedimentation rates (near land)
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Oceanographically & climatically sensitive
location
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Combined record of land and sea environments
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Marine benthic organisms
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Land-derived pollen from plants
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Minimal biological mixing
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Dansgaard-Oeschger interstadials
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Decreased oxygenation of bottom water
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Preservation of laminations
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Low-oxygen tolerant benthic foraminifera
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Surface water warmings
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Also around the Pacific rim
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Japan Sea
-
Offshore Oregon
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Gulf of California (Guaymas basin)
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Pacific circulation and environments influenced
by global change
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Changed sources and character of intermediate
water
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John Francis
Email: jfrancis@csulb.edu
Phone: 562-985-4928
written by R. Behl.
Last changes: 24 Oct. 1997