nerc.ac.uk

Multiple Palaeoproterozoic carbon burial episodes and excursions

Martin, A.P.; Prave, A.R.; Condon, D.J.; Lepland, A.; Fallick, A.E.; Romanshkin, A.E.; Medvedev, P.V.; Rychanchik, D.V.. 2015 Multiple Palaeoproterozoic carbon burial episodes and excursions. Earth and Planetary Science Letters, 424. 226-236. 10.1016/j.epsl.2015.05.023

Before downloading, please read NORA policies.
[thumbnail of aMartin_etal_MultipleCBEs_accepted.pdf]
Preview
Text
aMartin_etal_MultipleCBEs_accepted.pdf - Accepted Version

Download (1MB) | Preview

Abstract/Summary

Organic-rich rocks (averaging 2–5% total organic carbon) and positive carbonate-carbon isotope excursions (View the MathML source and locally much higher, i.e. the Lomagundi-Jatuli Event) are hallmark features of Palaeoproterozoic successions and are assumed to archive a global event of unique environmental conditions following the c. 2.3 Ga Great Oxidation Event. Here we combine new and published geochronology that shows that the main Palaeoproterozoic carbon burial episodes (CBEs) preserved in Russia, Gabon and Australia were temporally discrete depositional events between c. 2.10 and 1.85 Ga. In northwest Russia we can also show that timing of the termination of the Lomagundi-Jatuli Event may have differed by up to 50 Ma between localities, and that Ni mineralisation occurred at c. 1920 Ma. Further, CBEs have traits in common with Mesozoic Oceanic Anoxic Events (OAEs); both are exceptionally organic-rich relative to encasing strata, associated with contemporaneous igneous activity and marked by organic carbon isotope profiles that exhibit a stepped decrease followed by a stabilisation period and recovery. Although CBE strata are thicker and of greater duration than OAEs (100 s of metres versus metres, ∼106 years versus ∼105 years), their shared characteristics hint at a commonality of cause(s) and feedbacks. This suggests that CBEs represent processes that can be either basin-specific or global in nature and a combination of circumstances that are not unique to the Palaeoproterozoic. Our findings urge circumspection and re-consideration of models that assume CBEs are a Deep Time singularity.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1016/j.epsl.2015.05.023
ISSN: 0012-821X
NORA Subject Terms: Earth Sciences
Date made live: 09 Jun 2015 13:12 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/510813

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...