A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature05239.pdf
Reference30 articles.
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3. Knauth, L. P. & Lowe, D. R. Oxygen isotope geochemistry of cherts from the Onverwacht Group (3.4 billion years) Transvaal, South Africa, with implications for secular variations in the isotopic composition of cherts. Earth Planet. Sci. Lett. 41, 209–222 (1978)
4. Knauth, L. P. & Lowe, D. R. High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa. Geol. Soc. Am. Bull. 115, 566–580 (2003)
5. Knauth, L. P. Temperature and salinity history of the Precambrian ocean: implications for the course of microbial evolution. Palaeogeogr. Palaeoclimatol. Palaeoecol. 219, 53–69 (2005)
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