Palaeotemperature trend for Precambrian life inferred from resurrected proteins
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature06510.pdf
Reference30 articles.
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2. Hofmann, H. J., Grey, K., Hickman, A. H. & Thorpe, R. I. Origin of 3.45 Ga coniform stromatolites in Warrawoona Group, Western Australia. Geol. Soc. Am. Bull. 111, 1256–1262 (1999)
3. Knauth, L. P. & Lowe, D. R. Oxygen Isotope Geochemistry of Cherts from Onverwacht Group (3.4 billion years), Transvaal, South Africa, with implications for secular variations in 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. Robert, F. & Chaussidon, M. A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts. Nature 443, 969–972 (2006)
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