Definition
The Lomagundi carbon isotope excursion (LCIE), sensu stricto (s.s.), refers to highly positive carbon isotope values (on the average +8 ‰, but values as high as +16 ‰ are not uncommon with the highest values observed at +28 ‰) in Paleoproterozoic sedimentary carbonates deposited between ~2.22 and 2.06 Ga (Karhu and Holland 1996; Bekker et al. 2003), likely reflecting seawater composition. The beginning and the end of the excursion have not so far been recognized in the sedimentary record, and there is also uncertainty about the exact age of these transitions. Positive (at ~2.32 Ga and between ~2.45 and ~2.32 Ga; Bekker et al. 2001; Rasmussen et al. 2013) and negative (between ~2.45 and 2.32 Ga; Bekker et al. 2005) carbon isotope excursions have been found leading to the LCIE s.s. The older positive carbon isotope excursions, in particular the ~2.32 Ga one, are considered to be an...
References and Further Reading
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Bekker, A. (2014). Lomagundi Carbon Isotope Excursion. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5127-1
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Lomagundi Carbon Isotope Excursion- Published:
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DOI: https://doi.org/10.1007/978-3-642-27833-4_5127-1