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- W1909741232 abstract "Abstract The boron isotope ratio (δ 11 B) of marine biogenic carbonates can reconstruct pH and p CO 2 of seawater, and potentially CO 2 concentration in the atmosphere. To date, δ 11 B‐pH SW calibration has been proposed via culturing experiments, where calcifying organisms are cultured under artificially acidified seawater. However, in scleractinian corals, reconstructed pH values using culture‐based calibrations do not agree well with actual observations of seawater CO 2 chemistry. Thus, another approach is needed to establish a more reliable calibration method. In this study, we established field‐based calibrations for Chichijima and Tahiti, both located in subtropical gyres where surface seawater is close to CO 2 equilibrium. We suggest a new approach to calibration of δ 11 B‐pH in which the long‐term δ 11 B variation of massive Porites corals is compared with the decreasing pH trend (i.e., ocean acidification) that has occurred since the Industrial Revolution. This calibration will offer a new avenue for studying seawater CO 2 chemistry using coral δ 11 B in diverse settings, such as upwelling regions, coral reefs, and coastal areas." @default.
- W1909741232 created "2016-06-24" @default.
- W1909741232 creator A5053354632 @default.
- W1909741232 creator A5064811681 @default.
- W1909741232 creator A5065774676 @default.
- W1909741232 creator A5068579805 @default.
- W1909741232 date "2015-09-01" @default.
- W1909741232 modified "2023-10-14" @default.
- W1909741232 title "A new method for calibrating a boron isotope paleo-pH proxy using massive<i>P</i><i>orites</i>corals" @default.
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- W1909741232 doi "https://doi.org/10.1002/2015gc005975" @default.
- W1909741232 hasPublicationYear "2015" @default.
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