始太古代

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始太古代英语Eoarchean),是太古宙的第一個代,前一個是早雨海代,後一個是古太古代,時間介於40~36之間。

在地质学历史上,始太古代是指地球表面凝固的最早时期。它在古太古代之前、早雨海代之后。这个时期大气压大概是10到100帕。[1][2][3]

参考[编辑]

  1. ^ Mulkidjanian, A. Y. On the origin of life in the zinc world: 1. Photosynthesizing, porous edifices built of hydrothermally precipitated zinc sulfide as cradles of life on Earth.. Biol. Direct. 2009, 4: 26. doi:10.1186/1745-6150-4-26. 
  2. ^ Mulkidjanian, A. Y.; Bychkov, A. Y.; Dibrova, D. V.; Galperin, M. Y.; Koonin, E. V. Origin of first cells at terrestrial, anoxic geothermal fields. Proc. Natl. Acad. Sci. USA. 2012, 109 (14): E821–30. Bibcode:2012PNAS..109E.821M. doi:10.1073/pnas.1117774109. PMC 3325685. PMID 22331915. 
  3. ^ Mulkidjanian, A. Y. Energetics of the First Life. In R. Egel, D.-H. Lankenau, and A. Y. Mulkidjanian (ed.), Origins of Life: The Primal Self-Organization. Springer Verlag, Heidelberg.(book). 2011: 3–33.