Abstract

ABSTRACT 185 pairs of δ 13C and δ 15N values for aurochs, cattle and sheep bones from the northern Netherlands were studied to establish the influence of salt marsh grazing on bone δ 13C and δ 15N values. The observed values proved significantly increased compared to livestock that grazed inland. The δ 13C and δ 15N values of animals grazing former salt marshes were significantly less increased than those grazing the unembanked salt marsh. Absent regular salt marsh flooding may explain the reduced δ 13C increase in bones of animals grazing there. The δ 15N values of ruminants grazing the embanked salt marshes continued to be increased, presumably due to persisting saline water at shallow depths. The δ 13C values of the salt marsh grazing ruminants correspond with a δ 13C increase of 5‰ compared to eleven modern salt marsh plants from Schiermonnikoog studied in this paper. The δ 15N values of the eleven Schiermonnikoog salt marsh plants proved variable, on average too low to explain the observed 3.5‰ increase in δ 15N values. This suggests that vegetation δ 15N values cannot be the only cause of the high δ 15N values observed in salt marsh ruminants. Other processes may be responsible for the high δ 15N values of salt marsh grazing ruminants as well.

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