Nitrogen isotope analyses of reindeer (Rangifer tarandus), 45,000 BP to 9,000 BP: Palaeoenvironmental reconstructions. (2008) (original) (raw)

Pleistocene faunal δ 15N variations are thought to reflect changes in climatic and environmental conditions. Researchers are still unclear, however, which climatic/environmental parameter is the primary control on Pleistocene faunal δ 15N values. Through extensive nitrogen isotope analysis of Late Pleistocene reindeer (Rangifer tarandus) collagen we investigated whether permafrost development during the Late Pleistocene coincided with changes in δ 15N values. After 45 ka BP reindeer δ 15N declined, with lowest δ 15N values observed after the Last Glacial Maximum (LGM), between 15 and 11 ka BP. The decline in δ 15N appears to be of a greater magnitude in more northern regions than in the South of France, a pattern similar to that previously observed for horse. On a global scale, ecosystem δ 15N is controlled by the relative openness of the nitrogen cycle, which in turn is controlled by climate. Low soil and plant δ 15N are observed in cold and/or wet regions and high δ 15N are seen in hot and/or arid areas. The regional pattern in reindeer δ 15N decline mimics the pattern of climatic deterioration in Europe culminating at the LGM, with climate cooling being more intense in northern Europe than in southern Europe. However, the lowest reindeer δ 15N values are observed after temperatures started to rise. This may have been due to a lag in the response of the nitrogen cycle to increasing temperatures. Alternatively it may have been linked to the influence of permafrost degradation on soil and plant δ 15N and thus faunal δ 15N. The renewed climatic cooling during the Younger Dryas did not see a fall in reindeer δ 15N. Limited data does, however, suggest a post Younger Dryas depletion in reindeer δ 15N values.