Orbital Forcing of the Marine Isotope Stage 9 Interglacial

Milankovitch orbital forcing theory has been used to assign time scales to many paleoclimate records. However, the validity of this theory remains uncertain, and independent sea-level chronologies used to test its applicability have been restricted largely to the past ∼135,000 years. Here, we report...

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Veröffentlicht in:	Science (American Association for the Advancement of Science) 2001-01, Vol.291 (5502), p.290-293
Hauptverfasser:	Stirling, C. H., Esat, T. M., Lambeck, K., McCulloch, M. T., Blake, S. G., D.-C. Lee, Halliday, A. N.
Format:	Artikel
Sprache:	eng
Schlagworte:	Age Ancestry Animals Climate Climate change Climatic changes Cnidaria - chemistry Cnidaria - growth & development Coral reefs Corals Diagenetic processes Earth sciences Earth, ocean, space Exact sciences and technology Geological time Glacial climates Humans Insolation Isotopes Marine Marine and continental quaternary Marine isotope stages Mass Spectrometry Pacific Islands Radioisotopes - analysis Reefs Sea level Seawater Selection Criteria Surficial geology Theory Thorium - analysis Time Uranium - analysis
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