1991
DOI: 10.1016/0305-4403(91)90063-u
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Natural variations in the carbon isotope values of plants: Implications for archaeology, ecology, and paleoecology

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Cited by 538 publications
(400 citation statements)
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“…Apart from evaporation, other properties such as soil depth, water holding capacity, salinity, soil resistance and nitrogen content can either limit the water available to crops or affect photosynthesis rates in other ways (see Masle and Farquhar, 1988;Farquhar et al, 1989;Condon et al, 1992;Shangguan et al, 2000; Shaheen and Hood-Nowotny, 2005;Cabrera-Bosquet et al, 2007). The variable nature of soil properties means that they can change considerably within a relatively small area, affecting noticeable intra-and interspecies differences in plant stable isotope composition within the same habitat (Tieszen, 1991;Heaton, 1999).…”
Section: Evapotranspiration and Local Growing Conditionsmentioning
confidence: 99%
“…Apart from evaporation, other properties such as soil depth, water holding capacity, salinity, soil resistance and nitrogen content can either limit the water available to crops or affect photosynthesis rates in other ways (see Masle and Farquhar, 1988;Farquhar et al, 1989;Condon et al, 1992;Shangguan et al, 2000; Shaheen and Hood-Nowotny, 2005;Cabrera-Bosquet et al, 2007). The variable nature of soil properties means that they can change considerably within a relatively small area, affecting noticeable intra-and interspecies differences in plant stable isotope composition within the same habitat (Tieszen, 1991;Heaton, 1999).…”
Section: Evapotranspiration and Local Growing Conditionsmentioning
confidence: 99%
“…e.g. 7 The 18 O/ 16 O ratio in the phosphate and carbonate components of fossil bioapatite in individuals reflects the isotopic composition of the total ingested water in food and drink 8,9 and, in turn, climate variability via the effects of temperature and Rayleigh distillation on the isotopic composition of precipitation environmental water. Sequential intra-tooth measurements of 18 O/ 16 O and 13 C/ 12 C along the direction of growth are useful to assess the compositional variations of these parameters along a tooth mineralisation trajectory, as they reflect seasonal environmental variations during this period.…”
mentioning
confidence: 99%
“…Elemental composition (particularly %C) of each foodstuff/macronutrient group was based on formulae provided in Morrison et al (2000). Isotopic offsets between measured bulk food isotope values and the isotopic values of specific dietary macronutrients were derived from Tieszen (1981). Digestibility was determined following Hopkins et al (1981).…”
Section: Methodsmentioning
confidence: 99%