4.7 Article

Boric acid and borate incorporation in inorganic calcite inferred from B/Ca, boron isotopes and surface kinetic modeling

Journal

GEOCHIMICA ET COSMOCHIMICA ACTA
Volume 244, Issue -, Pages 229-247

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2018.10.008

Keywords

Boron; Inorganic calcite; Boron isotopes; B/Ca; Surface kinetic modeling; Precipitation rate; Paleo-pH

Funding

  1. US National Science Foundation [OCE-13-33357, OCE-15-36743, OCE 10-41133]

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The boron concentration (B/Ca ratio) and isotopic composition (delta B-11) iogenic calcite are widely applied to reconstruct past changes in seawater carbonate chemistry. Knowledge of B incorporation pathways into calcite is critical for these applications and for improving the theoretical basis of B proxies. While the canonical interpretation of delta B-11 holds that B in calcite predominantly derives from dissolved borate anion in seawater, recent studies of the B content, coordination, and isotopic composition in calcite suggest more complex B incorporation pathways. To provide new insights into these pathways, here we present delta B-11 of inorganic calcite precipitated from saline solutions of varying pH, calcium and dissolved inorganic carbon (DIC) concentration for which B/Ca data were previously reported by Uchikawa et al. (2015). Results showthat calcite delta B-11 significantly increases with increasing pH and decreases with increasing [Ca2+] and [DIC]. In combination, these experiments show that the difference in delta B-11 between solid calcite and aqueous borate linearly decreases with increasing calcite precipitation rate. To interpret these data, we present the first application of surface kinetic modeling (SKM) to boron incorporation. The SKM can simultaneously explain ratedependentB/Ca and delta B-11 patterns observed in our and previously published inorganic calcite precipitation experiments when both aqueous borate and boric acid contribute to boron in inorganic calcite. If the B incorporation mechanismshown here for inorganic calcite is applicable to biogenic calcite, precipitation rate variations could modify delta B-11 patterns by changing the contributions of aqueous boric acid and borate to boron in calcite. However, better knowledge of biogenic calcite precipitation mechanisms and rates is needed to assess the importance of this effect for applications of B proxies in biogenic carbonates. (C) 2018 Elsevier Ltd. All rights reserved.

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