File:Isotopic stages hg.png

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Description Stable oxygen isotope record of the last 300,000 years. The curve shows the last three glacial/interglacial cycles of the Quaternary. Blue is colder climate (glacial), red is warmer climate (interglacial); numbers are isotopic stages used in the dating (chronostratigraphy) of ocean sediments. The short term climatic changes of the Quaternary are induced by the Milankovitch cycles of the earth orbit.
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Source grafic is own work; reference: Martinson et al., 1987 doi:10.1016/0033-5894(87)90046-9 (redrawn after Fig. 18), digital version of data set doi:10.1594/PANGAEA.51706
Author Hannes Grobe/AWI
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current19:16, 12 September 2006Thumbnail for version as of 19:16, 12 September 20061,149 × 799 (109 KB)Hgrobe (talk | contribs){{Information |Description=Stable oxygen isotope record from sediments of the last 300 000 years |Source=own work |Date=2006-09-12 |Author=~~~~ |Permission=Own work, share alike, attribution required (Creative Commons CC-BY-SA-2.5) |other_versions= }} {{

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