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Devon B. Cole

Researcher at Georgia Institute of Technology

Publications -  30
Citations -  1394

Devon B. Cole is an academic researcher from Georgia Institute of Technology. The author has contributed to research in topics: Authigenic & Geology. The author has an hindex of 13, co-authored 27 publications receiving 847 citations. Previous affiliations of Devon B. Cole include Colorado College & Indian Council of Agricultural Research.

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Evolution of the global phosphorus cycle

TL;DR: A compilation of phosphorus abundances in marine sedimentary rocks spanning the past 3.5 billion years is presented and it is found that a combination of enhanced phosphorus scavenging in anoxic, iron-rich oceans and a nutrient-based bistability in atmospheric oxygen levels could have resulted in a stable low-oxygen world.
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A shale-hosted Cr isotope record of low atmospheric oxygen during the Proterozoic

TL;DR: Evidence for a delayed rise of atmospheric oxygen strongly suggests that environmental factors have played a fundamental role in controlling the emergence and expansion of complex life on Earth.
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A new estimate of detrital redox-sensitive metal concentrations and variability in fluxes to marine sediments

TL;DR: In this article, an extensive study of soils across the continental United States and their elemental concentrations was conducted, and the authors found large deviations from accepted crustal averages in redox-sensitive metals (Fe, Cr, U, V) compared to typical detrital tracers (Al, Ti, Sc, Th).
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On the co-evolution of surface oxygen levels and animals.

TL;DR: Views from across this interpretive spectrum are presented—in a point–counterpoint format—regarding crucial aspects of the potential links between animals and surface oxygen levels to disentangle the relationships between oxygen availability and emergence and diversification of animal life.
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Persistent global marine euxinia in the early Silurian.

TL;DR: The authors use a metal isotope mass balance model and find the marine anoxia event lasted over 3 million years, notably longer than the anoxic event associated with the Permian-Triassic extinction and Cretaceous ocean anoxic events.