مقایسهٔ روش‌ها

	نظریه متابولیک اکولوژی	مدل ترکیبی SIAR
حوزه	بوم‌شناسی	بوم‌شناسی
خانواده	Process / pipeline	Process / pipeline
سال پیدایش	2004	2010
پدیدآور	James Brown	Andrew Parnell
نوع	metabolic scaling theory	diet and source apportionment analysis
منبع بنیادین	Brown, J. H., Gillooly, J. F., Allen, A. P., Savage, V. M., & West, G. B. (2004). Toward a metabolic basis of ecology. Ecology, 85(7), 1771-1789.	Parnell, A. C., Inger, R., Bearhop, S., & Jackson, A. L. (2010). Source partitioning using stable isotopes: coping with too much variation. PLoS ONE, 5(3), e9672.
نام‌های دیگر	MTE, metabolic scaling, temperature-size rule, energy allocation	isotope mixing model, Bayesian mixing model, source apportionment, diet analysis
مرتبط	4	4
خلاصه	The Metabolic Theory of Ecology (MTE), developed by Brown and colleagues (2004), provides a unifying framework linking individual metabolic rate to ecological patterns across levels of organization (organisms, populations, ecosystems). MTE predicts how metabolic rate scales with body size (allometry) and temperature, and uses these scaling relationships to explain patterns in life history, population growth, community structure, and ecosystem dynamics. The theory is grounded in physics: metabolic rate is constrained by supply of resources (energy and nutrients) and demand determined by biochemical kinetics.	The Stable Isotope Analysis in R (SIAR) mixing model is a Bayesian framework for estimating the proportional contributions of dietary sources to a consumer, using stable isotope ratios. Developed by Parnell and colleagues (2010) and implemented in the R package siar (and its successor MixSIAR), this method integrates isotopic data from potential food sources and consumers to infer diets. It accounts for uncertainty in isotope fractionation (the shift in isotope ratios between diet and tissue) and natural variation among source populations, producing probability distributions rather than point estimates of diet composition.