Journal
CHEMICAL GEOLOGY
Volume 447, Issue -, Pages 148-160Publisher
ELSEVIER
DOI: 10.1016/j.chemgeo.2016.10.029
Keywords
Desmophyllum dianthus; Deep-sea coral; pH; Boron isotopes; Trace element; Fibrous aragonite
Categories
Funding
- Natural Environment Research Council [NE/J021075/1]
- NERC [NE/J021075/1] Funding Source: UKRI
- Natural Environment Research Council [NE/J021075/1] Funding Source: researchfish
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The isotopic composition of boron (delta B-11) in marine carbonates is well established as a proxy for past ocean pH, however, its robust application to palaeo-environments relies on the generation of species-specific calibrations. Existing calibrations utilising the deep-sea coral (DSC) Desmophyllum dianthus highlight the potential application of this pervasive species to pH reconstructions of intermediate depth waters. Nevertheless, considerable uncertainty remains regarding the estimation of seawater pH from these bulk skeletal delta B-11 measurements, likely resulting from microstructural heterogeneities in delta B-11 of D. dianthus. To circumvent this problem, thus improving the reliability of the D. dianthus delta B-11-pH calibration, we present a new delta B-11 calibration of micro-sampled fibrous aragonite from this species. Modern coral specimens recovered from the Atlantic, Pacific, and Southern Oceans, micro-sampled using microdrilling, micromilling, and laser cutting extraction, were analysed for trace element (B/Ca, Mg/Ca, Sr/Ca, and U/Ca) and boron isotopic composition. We find the best calibration against the delta B-11 of borate in local ambient seawater (a function of pH and taken from hydrographic data sets; pH range 7.57 to 8.05) utilises delta B-11 measurements of fibres with likely slow growth rates and minimal contamination from adjacent microstructures (identified by low Mg/Ca) for each coral specimen. This new calibration exhibits a stronger, and better-defined dependence on ambient seawater pH compared to bulk coral delta B-11; delta B-11(fibre) = (0.93 +/- 0.17) x delta B-11(borate) + (12.02 +/- 2.63). We suggest that the majority of the variability in measured delta B-11 between replicate bands of fibrous aragonite from a D. dianthus specimen can be explained by small incorporation of non-fibrous aragonite and surface impurities during microsampling and growth rate effects. This study confirms the utility of D. dianthus as an archive of precise palaeo-pH (+/- 0.07 pH units), provided that suitable sampling strategies are applied. Published by Elsevier B.V.
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