Biologically driven isotopic fractionations in bivalves: from palaeoenvironmental problem to palaeophysiological proxy

Abstract

Traditional bulk stable isotope (δ18O and δ13C) and clumped isotope (Δ47) records from bivalve shells provide invaluable histories of Earth's local and global climate change. However, biologically driven isotopic fractionations (BioDIFs) can overprint primary environmental signals in the shell. Here, we explore how conventional measurements of δ18O, δ13C, and Δ47 in bivalve shells can be re‐interpreted to investigate these physiological processes deliberately. Using intrashell Δ47 and δ18O alignment as a proxy for equilibrium state, we separately examine fractionations and/or disequilibrium occurring in the two major stages of the biomineralisation process: the secretion of the extrapallial fluid (EPF) and the precipitation of shell material from the EPF. We measured δ18O, δ13C, and Δ47 in fossil shells representing five genera (Lahillia, Dozyia, Eselaevitrigonia, Nordenskjoldia, and Cucullaea) from the Maastrichtian age [66–69 million years ago (Ma)] López de Bertodano Formation on Seymour Island, Antarctica. Material was sampled from both the outer and inner shell layers (OSL and ISL, respectively), which precipitate from separate EPF reservoirs. We find consistent δ18O values across the five taxa, indicating that the composition of the OSL can be a reliable palaeoclimate proxy. However, relative to the OSL baseline, ISLs of all taxa show BioDIFs in one or more isotopic parameters. We discuss/hypothesise potential origins of these BioDIFs by synthesising isotope systematics with the physiological processes underlying shell biomineralisation. We propose a generalised analytical and interpretive framework that maximises the amount of palaeoenvironmental and palaeobiological information that can be derived from the isotopic composition of fossil shell material, even in the presence of previously confounding ‘vital effects’. Applying this framework in deep time can expand the utility of δ18O, δ13C, and Δ47 measurements from proxies of past environments to proxies for certain biomineralisation strategies across space, time, and phylogeny among Bivalvia and other calcifying organisms.

Frontiers of Carbonate Clumped Isotope Thermometry

“…In some cases, T 47 was immune to these biases [foraminifera (Section 5.1)], whereas in others, biologic effects were seen in 47 as well as δ 18 O and δ 13 C [corals (Saenger et al 2012, Spooner et al 2016]. Increasingly, patterns in δ 18 O, 47 , and 48 can inform the mechanisms behind biologic effects (Curley et al 2023). Such insights can both allow reconstruction of original temperature signals in spite of biologic effects and reveal physiological biomineralization processes going on in different organisms relevant to understanding evolution and organism adaptability.…”