The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks, supplement to: Eagle, R A; Eiler, J M; Tripati, Aradhna K; Ries, Justin B; Freitas, P S; Hiebenthal, Claas; Wanamaker, Alan D; Taviani, Marco; Elliot, Mary; Marenssi, Sergio; Nakamura, K; Ramirez, P; Roy, K (2013): The influence of temperature and seawater carbonate saturation state on 13C–18O bond ordering in bivalve mollusks. Biogeosciences, 10(7), 4591-4606

• Main Authors: Eagle, R A, Eiler, J M, Tripati, Aradhna K, Ries, Justin B, Freitas, P S, Hiebenthal, Claas, Wanamaker, Alan D, Taviani, Marco, Elliot, Mary, Marenssi, Sergio, Nakamura, K, Ramirez, P, Roy, K
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2013
• Subjects: Animalia; Argopecten irradians; Benthic animals; Benthos; Biomass/Abundance/Elemental composition; Coast and continental shelf; Containers and aquaria 20-1000 L or < 1 m**2; Laboratory experiment; Mollusca; Mya arenaria; Not applicable; Single species; Temperate; Species; Identification; Salinity; Temperature, water; Partial pressure of carbon dioxide water at sea surface temperature wet air; Alkalinity, total; pH; Aragonite saturation state; Number of measurements; δ13C; δ18O; Δ47 Carbon dioxide; Δ47 Carbon dioxide, standard error; Carbonate system computation flag; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Carbonate ion; Carbon, inorganic, dissolved; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Elliot; Ramirez; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.831770; https://doi.pangaea.de/10.1594/PANGAEA.831770

The shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk delta 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C-18O bond abundance, denoted by the measured parameter Delta 47, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 °C, and field collected specimens spanning a range of -1 to 29 °C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between Delta 47 and growth temperature. We also find that the slope of a linear regression through all the Delta 47 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the Delta 47 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between Delta 47-temperature relationships between calcitic and aragonitic taxa. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2014-04-15.