Using Mg Isotopes to Estimate Natural Calcite Compositions and Precipitation Rates During the 2010 Eyjafjallajökull Eruption

Publisher's version (útgefin grein) Chemical weathering of silicate rocks is a key control on the long-term climate, via drawdown of atmospheric CO 2 . Magnesium isotopes are increasingly being used to trace weathering, but are often complicated by several coincident fractionating processes. He...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Pogge von Strandmann, Philip A. E., Olsson, Jonas, Luu, Tu-Han, Gíslason, Sigurður Reynir, Burton, Kevin W.
Other Authors: Institute of Earth Sciences (UI), Jarðvísindastofnun (HÍ), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media SA 2019
Subjects:
Basalt
Carbonate
Magnesium isotopes
Travertine
Weathering
Magnesín (málmar)
Kalksteinn
Veðrun
Eyjafjallajökull
Online Access:https://hdl.handle.net/20.500.11815/1842
https://doi.org/10.3389/feart.2019.00006
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Summary:Publisher's version (útgefin grein) Chemical weathering of silicate rocks is a key control on the long-term climate, via drawdown of atmospheric CO 2 . Magnesium isotopes are increasingly being used to trace weathering, but are often complicated by several coincident fractionating processes. Here we examine Mg isotope ratios of waters stemming from beneath lava flows from the 2010 Eyjafjallajökull eruption. Travertine calcite was observed directly precipitating from these high-TDS (total dissolved solids) waters, and were also sampled. This system therefore provides the opportunity to study natural Mg isotope fractionation by calcite. Riverine δ 26 Mg increase from −2.37 to +0.43% with flow distance, as isotopically light travertine precipitates (δ 26 Mg = −3.38 to −3.94%). The solution Mg isotope ratios also co-vary with pH, calcite saturation indices and Sr/Ca ratios, strongly indicating that they are dominantly controlled by carbonate precipitation. Using experimental isotopic fractionation factors and the measured δ 26 Mg values, we can predict the compositions of the precipitated travertines that are within uncertainty of the directly measured travertines. Hence, in some systems, Mg isotopes can be used to quantify carbonate precipitation. Analyses and PPvS were funded by ERC Consolidator grant 682760 CONTROLPASTCO2. Peer Reviewed

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