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27 mars 2017
Oxygen isotope fractionation between bird eggshell calcite and body water: application to fossil eggs from Lanzarote (Canary Islands)

Fig. δ18O of fossil bird eggshells from Puffinus sp abd an indeterminate giant bird.

  Oxygen and carbon isotope compositions of fossil bird eggshell calcite (δ18Ocalc and δ13Ccalc) are regularly used to reconstruct paleoenvironmental conditions. The δ18Ocalc values mainly reflect the oxygen isotope composition of the waters ingested by birds (δ18Ow), which in turn are controlled by local climatic parameters (air temperature, local humidity), whereas the δ13Ccalc value provides information on birds foraging environment as well as local relative humidity. However, the interpretation of δ18Ocalc values of fossil eggshells is limited to qualitative variations in local climatic conditions as oxygen isotope fractionations between calcite, body fluids and drinking water have not been determined yet. For this purpose, eggshells, albumen and drinking water of extant birds have been sampled and analyzed for their oxygen and carbon isotope compositions. Enrichments in 18O relative to 16O between body fluids and drinking water of +2.2±0.4 ‰ for semi-aquatic birds and of +4.1 ±0.5‰ for terrestrial birds are observed. Using our dataset and published values, two empirical equations relating the δ18Ocalc value of eggshell calcite to the δ18Ow value of ingested water have been established for terrestrial and semi-aquatic birds. These equations have been applied to two cases of fossil eggshells from Lanzarote, Canary Islands, in order to infer the ecologies of the Pleistocene marine bird Puffinus sp. and of the enigmatic giant birds from the Pliocene of Valle Grande. Both δ18Ocalc and δ13Ccalc of Puffinus eggshells point to a semi-aquatic marine bird ingesting mostly seawater with a δ18Ow value -0.6±0.3‰. In the case of the Pliocene giant bird, low δ13Ccalc values of eggshells point to a terrestrial lifestyle and the δ18Ocalc values allowed us to calculate an ingested local freshwater δ18Ow value of -2.8±0.3‰.  This set of equations can help to quantitatively estimate the origin of waters ingested by extinct birds as well as to infer either local environmental (marine or freshwater) or climatic (local air temperatures, precipitations) conditions.

Authors : N. Lazzerini , C. Lécuyer, R. Amiot, D. Angst, E. Buffetaut, F.  Fourel , V. Daux  et al.

Ref. :  Sci. Nature 103:81

 

 

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