Abstract

Burial of large quantities of magnetite (Fe(II)Fe(III)2O4) in iron formations (IFs) likely contributed to the protracted oxidation of Earth's surface during the Precambrian Eons. Magnetite can form through a diversity of biological and abiotic pathways and its preservation in IFs may thus be variably interpreted as the result of some combination of these processes. Such interpretations give rise to divergent pictures of the Precambrian Earth system and models for its evolution through time. New knowledge on the contribution of specific magnetite formation pathways is, therefore, needed to accurately tether our conceptual and numerical models to the geologic record. To constrain pathways of magnetite formation under ferruginous conditions, we conducted geochemical and multi-method microspectroscopic analyses on particles obtained from the water columns and sediments of ferruginous lakes Matano and Towuti, in Indonesia. We find that biologically reactive Fe(III) mineral phases are reduced in the anoxic waters of both lakes, causing the formation of primary authigenic magnetite, directly in the water column. This water column magnetite often takes conspicuous framboidal forms, which given the link to microbial Fe(III) reduction, may provide a biological signature on early Earth and by extension, other planetary bodies. The consumption of more biologically reactive forms of Fe(III) and the resulting delivery of primary magnetite to underlying sediments promotes the burial of oxidized equivalents and implies that primary magnetite formation could have been a principal pathway of Fe delivery to IFs. Combined, the removal of Fe from Earth's surface through biologically induced magnetite formation and subsequent burial in IFs, suggests that seawater chemistry and the microbially mediated reactions that cause magnetite formation played key roles in Earth system evolution and in setting the pace for planetary oxidation through the Precambrian Eons.

Highlights

  • Biogeochemical cycling of iron (Fe) and carbon (C) plays a key role in setting Earth’s surface redox budgets and climate

  • In Lakes Matano (LM), these three pools together account for 83% and 70% of the total particulate Fe recovered in the shallow and deep traps, respectively, whereas in LT they account for 79% and 77% respectively

  • We find that in ferruginous Lakes Matano (LM) and Towuti (LT) in Indonesia that magnetite forms directly in the water column

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Summary

Introduction

Biogeochemical cycling of iron (Fe) and carbon (C) plays a key role in setting Earth’s surface redox budgets and climate. Fe(III)-bearing minerals, by contrast, is a net sink for atmospheric oxygen (Holland, 1984; Holland, 2002) The magnitudes of these sources and sinks are influenced by dynamics in coupled C and Fe cycling, which can induce secular variation in Earth’s surface chemistry (Catling and Claire, 2005; Holland, 2002, 2006; Kasting, 2013) and over geological timescales this can lead to fundamentally different ocean-atmosphere redox states and climate systems (Holland, 2002; Kasting, 2013). IF mineralogy, notably, is dominated by the mixed-valence oxide magnetite (Fe2+Fe3+2O4) (Klein, 2005), and burial of magnetite in IFs played an important role as a sink for

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