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Phytate‐iron molar ratio and bioavailability of iron in Bangladesh

OBJECTIVE: Phytate, an important component of plant origin foods, works as a chelator for mineral nutrients such as iron. Estimating the phytate‐iron molar ratio is a traditional method to assess the bioavailability of dietary iron, and a ratio >1 is suggestive of poor absorption of iron through...

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Detalles Bibliográficos
Autores principales: Rahman, Sabuktagin, Shaheen, Nazma
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9322336/
https://www.ncbi.nlm.nih.gov/pubmed/35383403
http://dx.doi.org/10.1111/tmi.13750
Descripción
Sumario:OBJECTIVE: Phytate, an important component of plant origin foods, works as a chelator for mineral nutrients such as iron. Estimating the phytate‐iron molar ratio is a traditional method to assess the bioavailability of dietary iron, and a ratio >1 is suggestive of poor absorption of iron through the intestinal mucosa. In Bangladesh, the ratio is considerably higher; nonetheless, the haemoglobin and ferritin status are satisfactory. Hence, we appraised phytate‐iron molar ratios and concomitant haemoglobin and ferritin status. METHODS: Dietary intake of iron and phytate was estimated in non‐pregnant non‐lactating women and school‐age children from a nationally representative survey. The phytate‐iron molar ratios were estimated. Linear regressions on haemoglobin for the phytate‐iron molar ratios and on molar ratios predicting inflammation‐adjusted ferritin were performed. RESULTS: The median ratios were 6.12 in women and 5.47 in children, with corresponding haemoglobin concentrations of 12.6 and 12.5 g/dl. Hypothetical lowering of the ratios by ~50% revealed a nominal increment of haemoglobin and ferritin. CONCLUSION: The standard cut‐off phytate‐iron molar ratio of >1 is inconsistent with the iron and haemoglobin status of the Bangladeshi population. One plausible explanation for the inconsistency is a non‐dietary environmental factor—groundwater iron. Isotope studies incorporating the iron from dietary and the drinking groundwater sources are needed to establish a ratio which might better explain iron bioavailability.