文摘
δ11B of deep sea coral is potentially a powerful tool to reconstruct intermediate depth seawater pH. Microstructural heterogeneities result in uncertainty in pH derived from bulk skeletal δ11B. We present δ11B and trace element composition of micro-sampled fibrous aragonite from D. dianthus. δ11B of fibres lowest in Mg for each coral reveal a stronger, and better-defined dependence on ambient seawater pH. D. dianthus is an archive of precise palaeo-pH (< 0.1 pH units), providing that suitable sampling strategies are applied.