Calibrating temperature reconstructions from fish otolith oxygen isotope analysis for California's critically endangered Delta smelt (vol 33, pg 1207, 2019)

Rationale Oxygen isotope ratios (delta O-18 values) of fish otoliths (ear bones) are valuable geochemical tracers of water conditions and thermal life history. Delta Smelt (Hypomesus transpacificus) are osmerid forage fish endemic to the San Francisco Estuary, California, USA, that are on the verge of extinction. These fish exhibit a complex life history that allows them to survive in a dynamic estuarine environment; however, a rapidly warming climate threatens this thermally sensitive species. Here we quantify the accuracy and precision of using delta O-18 values in otoliths to reconstruct the thermal life histories of Delta Smelt. Methods Delta Smelt were reared for 360 days using three different water sources with different ambient delta O-18(water) values (-8.75 parts per thousand, -5.28 parts per thousand, and -4.06 parts per thousand) and different water temperatures (16.4 degrees C, 16.7 degrees C, 18.7 degrees C, and 20.5 degrees C). Samples were collected after 170 days (n = 28) and 360 days (n = 14) post-hatch. In situ delta O-18 values were measured from the core of the otolith to the dorsal edge using secondary ion mass spectrometry (SIMS) to reconstruct temporally resolved thermal life histories. Results The delta O-18(otolith) values for Delta Smelt varied as a linear inverse function of water temperature: 1000 ln alpha = 18.39 (+/- 0.43, 1SE)(10(3)TK(-1)) - 34.56 (+/- 1.49, 1SE) and delta O-18(otolith(VPDB)) - delta O-18(water (VPDB)) = 31.34(+/- 0.09, 1SE) - 0.19(+/- 0.01, 1SE) x T degrees C. When the ambient delta O-18(water) value is known, this species-specific temperature-dependent oxygen isotope fractionation model facilitated the accurate (0.25 degrees C) and precise (+/- 0.37 degrees C, 2 sigma) reconstruction of the water temperature experienced by the fish. In contrast, the use of existing general fractionation equations resulted in inaccurate temperature reconstructions. Conclusions The species-specific delta O-18(otolith) fractionation equation allowed for accurate and precise reconstructions of water temperatures experienced by Delta Smelt. Characterization of ambient delta O-18(water) values remains a critical next step for reconstructing thermal life histories of wild Delta Smelt. This tool will provide new insights into habitat utilization, potential thermal refugia, and resilience to future warming for this critically endangered fish.