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Summary Of: 100,000-year problem
Encyclodia Page On: 100,000-year problem
These Are Links To Other Documents
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past temperatures
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insolation
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variations in the Earth's orbit
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climate
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ice ages
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temperature
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readily inferred
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oxygen isotopes
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δ
18
O
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Vostok
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sediments
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Nicholas Shackleton
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Dole effect
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resonance frequency
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continental drift
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sea floor spreading
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Orbital inclination
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eccentricity
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3
He
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produced
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solar rays
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Precession cycles
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algal bloom
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Dole effect
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photosynthesisers
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resolution
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ice cores
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EPICA
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correlation
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Milankovitch cycles
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Paleoclimatology
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Isotope geochemistry
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Oxygen-18
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Shackleton, N.J.
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doi
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doi
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ISSN
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doi
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doi
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doi
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doi
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doi
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1998
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05-08
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doi
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1976
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12-10
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doi
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1980
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02-29
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doi
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doi
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ISSN
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doi
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Categories
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Ice ages
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Climatology
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Climate change
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This article is licensed under the
GNU Free Documentation License
. It uses material from the
Wikipedia article "100,000-year problem"
.
