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We present precipitation isotope data (δ2H and δ18O values) from 19 stations across the tropics collected from 2012 to 2017 under the Coordinated Research Project F31004 sponsored by the International Atomic Energy Agency. Rainfall samples were collected daily and analysed for stable isotopic ratios of oxygen and hydrogen by participating laboratories following a common analytical framework. We also calculated daily mean stratiform rainfall area fractions around each station over an area of 5° x 5° longitude/latitude based on TRMM/GPM satellite data. Isotope time series, along with information on rainfall amount and stratiform/convective proportions provide a valuable tool for rainfall characterisation and to improve the ability of isotope-enabled Global Circulation Models to predict variability and availability of inputs to fresh water resources across the tropics.

We present stable isotopic data obtained in order to elucidate the diet of current domestic camelids and their feeding areas, as a necessary step for the interpretation of archaelogical assemblages, and to answer questions regarding past diet, herd structure, foraging zones and interaction with human populations. Seventeen new d 13C collagen isotope values from Lama glama bones were measured in order to start a systematic study of the isotopic ecology of herbivory in the Puna ecosystem of Jujuy province, Argentina. These values were compared with those previously available, and a reliable correlation between altitude and variation in isotopic values was found: of the order of À2% depletion for each 500 m increase in altitude. These results were interpreted as related to variation in vegetal assemblage due to altitude. We consider that the outcomes of this research exceed the scope of our study area, being important to the Argentine Puna as a whole, and will also contribute to the development of current animal population ecological models applied to the interpretation of archaeological remains.

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