Abstract

Dairy products occupy a special place among foods in contributing to a major part of our nutritional requirements, while also being prone to fraud. Hence, the verification of the authenticity of dairy products is of prime importance. Multiple stable isotopic studies have been undertaken that demonstrate the efficacy of this approach for the authentication of foodstuffs. However, the authentication of dairy products for geographic origin has been a challenge due to the complex interactions of geological and climatic drivers. This study applies stable isotope measurements of δ2H, δ18O, δ13C and δ15N values from casein to investigate the inherent geo-climatic variation across dairy farms from the South and North Islands of New Zealand. The stable isotopic ratios were measured for casein samples which had been separated from freeze-dried whole milk samples. As uniform feeding and fertilizer practices were applied throughout the sampling period, the subtropical (North Island) and temperate (South Island) climates were reflected in the variation of δ13C and δ15N. However, highly correlated δ2H and δ18O (r = 0.62, p = 6.64 × 10−10, α = 0.05) values did not differentiate climatic variation between Islands, but rather topographical locations. The highlight was the strong influence of δ15N towards explaining climatic variability, which could be important for further discussion.

Highlights

  • Milk is a significant part of the global diet and demand across the international food market is continually increasing [1]

  • Of note is the study by Crittenden et al [7], which demonstrated the possibility of identifying the geographical origin of milk in Australasia using multi-element stable isotope ratio analysis

  • The charts show the variability of casein isotope measurements (δ2 H, δ15 N, δ18 O and δ13 C) between

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Summary

Introduction

Milk is a significant part of the global diet and demand across the international food market is continually increasing [1]. As a result, determining the authenticity and origin of dairy products is vital for ensuring food safety in export markets and the global food trade. Several studies have discussed defining the origin of milk products using stable isotopic ratio analyses [4,5,6,7,8,9,10,11,12,13]. Of note is the study by Crittenden et al [7], which demonstrated the possibility of identifying the geographical origin of milk in Australasia using multi-element stable isotope ratio analysis

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