Stable isotope (δ18O, δ13C, and δD) signatures of recent terrestrial communities from a low-latitude, oceanic setting: Endemic land snails, plants, rain, and carbonate sediments from the eastern Canary Islands

Abstract Stable isotopes of oxygen and carbon extracted from fossil land snail shells have been used increasingly to interpret past environments. To evaluate the utility of this approach for low-latitude oceanic islands, populations of the modern helicid land snail Theba geminata – a species also abundant in the Quaternary fossil record of the region – were sampled at ten low altitude ( δ D and − 2‰ (V-SMOW) for δ 18 O, ranging from − 11‰ to + 2‰ (V-SMOW) and from − 2.6‰ to − 0.7‰ (V-SMOW), respectively. The local vegetation is heterogeneous, including C 3 , C 4 , and CAM plants. δ 13 C values vary from − 13.0‰ to − 29.0‰ (V-PDB) across plant species. Of the 24 species, five are C 4 , 15 are C 3 , and four are CAM plants. The δ 18 O values for shells represent a narrow range of values (from − 0.3‰ to + 2.5‰ [V-PDB]), which is consistent with the low climate seasonality typifying low-latitude oceanic settings. Hypothetical model of the expected δ 18 O value for shell aragonite precipitated in equilibrium suggests that the most negative δ 18 O shell represent the closest estimate for δ 18 O rain water . The δ 13 C values of shells range from − 9.4‰ to + 1.7‰ (V-PDB). The most positive δ 13 C values are attributed to a diet based on C 4 plants. The comparison of δ 13 C values of soft tissues and shells suggests that snails ingested notable amounts (from ~ 20% up to ~ 40%) of foreign carbonates. Consequently, fossil shells with the most negative δ 13 C values should be selected for radiocarbon dating in future geochronological studies of the region. The δ 13 C values of body tissues vary from − 12.0‰ to − 27.2‰ (V-PDB), indicating that land snails consumed C 3 and C 4 plants indiscriminately. The mean carbon isotopic composition, averaged across multiple fossil specimens, may thus provide a useful tool for reconstructing paleoclimates and paleoenvironments throughout the Quaternary history of the Canary Islands and other comparable low-latitude oceanic settings.