Understanding variations in the routes by which wild animals gain and lose water is challenging, and common methods require longitudinal sampling, which can be prohibitive. However, a new approach uses 'O ('O of animal body water), calculated from measurements of 'O and 'O in a single sample, as a natural tracer of water flux. 'O is promising, but its relationship to organismal variables such as metabolic rate and water intake have not been validated.
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