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Summary Of: 100,000-year problem

Encyclodia Page On: 100,000-year problem

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An average of several samples of δ18O, a proxy for temperature, for the last 600,000 years | | past temperatures | insolation | variations in the Earth's orbit | climate | ice ages | A δ18O record for the past 120,000 years | | temperature | readily inferred | oxygen isotopes | δ18O | Vostok | sediments | Nicholas Shackleton | Dole effect | The effect of obliquity variations may, in concert with precession, be amplified by orbital inclination. | | resonance frequency | continental drift | sea floor spreading | Precessional cycles may produce a 100,000 effect. | | Orbital inclination | eccentricity | 3He | produced | solar rays | Precession cycles | An algal bloom. The relative importance of land- and sea-based photosynthesis may fluctuate on a 100,000 year timescale. | | algal bloom | Dole effect | photosynthesisers | resolution | ice cores | EPICA | correlation | Milankovitch cycles | Paleoclimatology | Isotope geochemistry | Oxygen-18 | Shackleton, N.J. | doi | 2007 | 05-09 | 2001 | 04-27 | doi | 2007 | 09-14 | dead link | doi | 2007 | 05-09 | doi | ISSN | doi | doi | 2008 | 06-25 | 2007 | 05-09 | doi | doi | 2007 | 05-09 | doi | 2007 | 05-09 | 1998 | 05-08 | doi | 2007 | 05-09 | dead link | 2007 | 05-09 | 1976 | 12-10 | doi | 2007 | 05-09 | 1980 | 02-29 | doi | 2007 | 05-09 | doi | 2007 | 10-17 | ISSN | 2007 | 05-09 | 2007 | 05-09 | doi | Categories | Ice ages | Climatology | Climate change | All articles with dead external links | Articles with dead external links since June 2008 | Pages with DOIs broken since 2008 |
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