Oxygen isotope variability in conodonts: implications for reconstructing Palaeozoic palaeoclimates and palaeoceanography

Abstract

Conodonts have the potential to elucidate the intricacies of Palaeozoic climates, especially if δ 18 O values of single apatitic tooth-like ‘elements’ can be used to map evolving sea surface temperatures and differentiate oceanic water masses. Their ecological distribution as pelagic and nektobenthic organisms, high-resolution biostratigraphy, and abundance in Cambrian–Triassic rocks qualifies them as potentially robust climate archives. Previous ion microprobe conodont δ 18 O studies have proceeded directly to palaeotemperature interpretation without appreciation of inter- and intra-element variability or post-mortem artefacts. Here, ion microprobe analyses of Ordovician and Silurian conodonts establishes that: intra-element crown tissue δ 18 O typically varies by ≤1‰ (53% of conodonts analysed), is normally ≤2‰ (92% of analyses), and rarely varies by 2–4‰; δ 18 O can vary across elements, suggesting a microstructural and/or diagenetic control; δ 18 O can vary between species representatives by c . 3‰; δ 18 O of pelagic and nektobenthic taxa can be offset by 2–3‰; elements processed with formic acid have highly variable δ 18 O; and thermal alteration does affect δ 18 O. Conodont ion microprobe δ 18 O values are comparable with those of bulk methods, but utilization of material with no consideration of geological context or processing history may introduce significant artefacts. A protocol for future conodont oxygen isotope ion microprobe studies is proposed. Supplementary material: Full results of oxygen isotope analyses reported in this paper are available at www.geolsoc.org.uk/SUP18516 .