δ15N

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In geochemistry, paleoclimatology and paleoceanography δ15N or delta-N-15 is a measure of the ratio of stable isotopes 15N:14N.[1]

References[edit]

  1. ^ Katzenberg, MA (2008). "Chapter 13: Stable Isotope Analysis: A Tool for Studying Past Diet, Demography, and Life History". Biological Anthropology of the Human Skeleton (2nd ed.). ISBN 978-0-471-79372-4. 

See also[edit]