The Global Biogeochemical Cycle of Rhenium

Ghazi, L.; Grant, K. E.; Chappaz, A.; Danish, M.; Peucker‐Ehrenbrink, B.; Pett‐Ridge, J. C.

doi:10.1029/2024gb008254

The Global Biogeochemical Cycle of Rhenium

Journal Article · Fri Oct 04 00:00:00 EDT 2024 · Global Biogeochemical Cycles

DOI:https://doi.org/10.1029/2024gb008254· OSTI ID:2497910

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Oregon State Univ., Corvallis, OR (United States)
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States). Center for Accelerator Mass Spectrometry
Central Michigan Univ., Mount Pleasant, MI (United States)
University of Haifa (Israel)
Woods Hole Oceanographic Institution, Woods Hole, MA (United States)

Here, this paper is the first comprehensive synthesis of what is currently known about the different natural and anthropogenic fluxes of rhenium (Re) on Earth's surface. We highlight the significant role of anthropogenic mobilization of Re, which is an important consideration in utilizing Re in the context of a biogeochemical tracer or proxy. The largest natural flux of Re derives from chemical weathering and riverine transport to the ocean (dissolved = 62 × 10⁶ g yr^-1 and particulate = 5 × 10⁶ g yr^-1). This review reports a new global average [Re] of 16 ± 2 pmol L^-1, or 10 ± 1 pmol L^-1 for the inferred pre-anthropogenic concentration without human impact, for rivers draining to the ocean. Human activity via mining (including secondary mobilization), coal combustion, and petroleum combustion mobilize approximately 560 × 10⁶ g yr^-1 Re, which is more than any natural flux of Re. There are several poorly constrained fluxes of Re that merit further research, including: submarine groundwater discharge, precipitation (terrestrial and oceanic), magma degassing, and hydrothermal activity. The mechanisms and the main host phases responsible for releasing (sources) or sequestrating (sinks) these fluxes remain poorly understood. This study also highlights the use of dissolved [Re] concentrations as a tracer of oxidation of petrogenic organic carbon, and stable Re isotopes as proxies for changes in global redox conditions.

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This content will become publicly available on Sat Oct 04 00:00:00 EDT 2025

Research Organization:: Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)

Sponsoring Organization:: USDOE National Nuclear Security Administration (NNSA); USDOE Laboratory Directed Research and Development (LDRD) Program

Grant/Contract Number:: AC52-07NA27344

OSTI ID:: 2497910

Report Number(s):: LLNL-JRNL-868303; 1099478

Journal Information:: Global Biogeochemical Cycles, Vol. 38, Issue 10; ISSN 0886-6236

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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