Encyclopedia of Geobiology

2011 Edition
| Editors: Joachim Reitner, Volker Thiel

Soda Ocean Hypothesis

  • Stephan Kempe
  • Jozef Kazmierczak
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-9212-1_192

Definition

The “soda ocean hypothesis” (SOH) stands for the concept of an early (i.e., in essence Precambrian) alkaline or even highly “alkaline ocean,” in analogy to the chemistry of the present-day “soda lakes.”

Soda ocean hypothesis (SOH)

The SOH has been advanced in biology (e.g., Snyder and Fox, 1975) for biochemical reasons before it was developed in earth sciences for geochemical reasons (Kempe and Degens, 1985; Kempe et al., 1989; Kempe and Kazmierczak, 1994).

In biology, the SOH rests on the observations that certain reactions considered essential for biogenesis would be favored by alkaline conditions (e.g., Abelson, 1966). One of those is the experimental observation that peptide bonds are more stable in alkaline than in acidic environments (e.g., Dose and Rauchfuss, 1972).

In earth sciences, the SOH rests on elemental mass balances, thermodynamic and kinetic arguments, and the analogy to modern soda lakes. These arguments are in short:
  1. 1.

    A CO2-rich atmosphere in the...

Keywords

Saturation Index Soda Lake Early Ocean PCO2 Atmosphere Divalent Earth Alkaline 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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Copyright information

© Springer Science+Business Media B.V. 2011

Authors and Affiliations

  • Stephan Kempe
    • 1
  • Jozef Kazmierczak
    • 2
  1. 1.Department of Physical Geology and Global Cycles Institute for Applied GeosciencesUniversity of TechnologyDarmstadtGermany
  2. 2.Institute of PaleobiologyPolish Academy of SciencesWarszawaPoland