Linear Correlations in Bamboo Coral δ13C and δ18O Sampled by SIMS and Micromill: Evaluating Paleoceanographic Potential and Biomineralization Mechanisms Using δ11B and ∆47 Composition
deep-sea corals; paleoclimate; oxygen isotope; clumped isotope; boron isotope; SIMS; vital effect
Recent work demonstrates that bamboo coral growth temperature, averaged over its entire lifespan, can be derived from linear correlations in its carbon and oxygen isotope composition (δ13C, δ18O) when the apparent equilibrium fractionations for a coral's growth rate and calcifying pH are used. Building on this method, this study applies it to coeval coral skeleton to assess the possibility of extracting paleoceanographic timeseries from bamboo coral skeletons.

