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Limited oxygen production in the Mesoarchean ocean
Frantz Ossa Ossa1,2, Axel Hofmann2, Jorge E Spangenberg3
1Department of Geosciences, University of Tuebingen, 72074 Tuebingen, Germany; frantz.ossaossa@gmail.com.
Summary
Mesoarchean oceans show evidence of localized oxygen oases, but lacked a widespread aerobic nitrogen cycle. Nutrient limitations, not nitrogen, likely restricted oxygen-producing life during this early Earth period.
Area of Science:
- Geochemistry
- Paleoceanography
- Early Earth conditions
Background:
- Archean Eon characterized by anoxic surface conditions and anaerobic bioessential element cycling.
- Mesoarchean (3.2-2.8 Ga) ocean oxygenation is debated, contrasting with Neoarchean 'oxygen oases'.
Purpose of the Study:
- Investigate Mesoarchean ocean oxygenation and nitrogen cycling.
- Determine the extent and causes of potential oxygen oases during the Mesoarchean.
Main Methods:
- Analysis of nitrogen (δ15N) and carbon (δ13C) isotope values in Mesoarchean shales.
- Assessment of local seawater redox conditions and manganese precipitation.
- Evaluation of iron and manganese redox systematics.
Main Results:
- Evidence for localized oxygen oases in the Mesoarchean ocean, indicated by iron and manganese redox data.
- Nitrogen isotope data suggest a molybdenum-dependent diazotrophic biosphere, with no significant aerobic nitrogen cycle.
- Dissolved O2 levels were likely too low or spatially limited to form a substantial nitrate reservoir.
Conclusions:
- Mesoarchean oxygen oases existed but did not support a widespread aerobic nitrogen cycle.
- Nutrient limitations, possibly phosphorus, suppressed oxygen-producing organisms and limited oxygenation expansion.
- Contrasts with Neoarchean oxygenation, highlighting different environmental controls on early Earth life.
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