File:Glacial effect hg.png
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| Description | Glacial effect (after Shackleton): The ratio of stable oxygen isotopes 16O/18O in the oceans is changed by the build up of ice sheets on the continents during glacials due to fractionated evaporation and precipitation in high latitudes. A global change in sea level of about 100 m between glacials and interglacials generates a difference of 1 per mil. The variations in the isotope ratio are archived in carbonaceous plankton shells and can be used to date quaternary sediments and reconstruct paleoclimate. |
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| Source | Own work |
| Author | Hannes Grobe, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany |
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| current | 20:49, 25 June 2006 | | 2,000 × 1,373 (1.64 MB) | Hgrobe (talk | contribs) | {{Information |Description = '''Glacial effect''': The ratio of stable oxygen isotopes 16O/18O in the oceans is changed by the build up of ice sheets on the continents during glacials due to fractionated evaporation and precipitation in high latitudes. A |
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