Nitrogen and carbon isotopic dynamics of subarctic soils and plants in southern Yukon Territory and its implications for paleoecological and paleodietary studies

We examine here the carbon and nitrogen isotopic compositions of bulk soils( 8 topsoil and 7 subsoils, including two soil profiles) and five different plant parts of 79 C-3 plants from two main functional groups: herbs and shrubs/subshrubs, from 18 different locations in grass-lands of southern Yukon Territory, Canada( eastern shoreline of Kluane Lake and White-horse area). The Kluane Lake region in particular has been identified previously as an analogue for Late Pleistocene eastern Beringia. All topsoils have higher average total nitrogen delta N-15 and organic carbon delta C-13 than plants from the same sites with a positive shift occurring with depth in two soil profiles analyzed. All plants analyzed have an average whole plant delta C-13 of -27.5 +/- 1.2 parts per thousand and foliar delta C-13 of -28.0 +/- 1.3 parts per thousand, and average whole plant delta N-15 of -0.3 +/- 2.2 parts per thousand and foliar delta N-15 of -0.6 +/- 2.7 parts per thousand. Plants analyzed here showed relatively smaller variability in delta C-13 than delta N-15. Their average delta C-13 after suitable corrections for the Suess effect should be suitable as baseline for interpreting diets of Late Pleistocene herbivores that lived in eastern Beringia. Water availability, nitrogen availability, spacial differences and intra-plant variability are important controls on delta N-15 of herbaceous plants in the study area. The wider range of delta N-15, the more numerous factors that affect nitrogen isotopic composition and their likely differences in the past, however, limit use of the modern N isotopic baseline for vegetation in paleodietary models for such ecosystems. That said, the positive correlation between foliar delta N-15 and N content shown for the modern plants could support use of plant delta(15) N as an index for plant N content and therefore forage quality. The modern N isotopic baseline cannot be applied directly to the past, but it is prerequisite to future efforts to detect shifts in N cycling and forage quality since the Late Pleistocene through comparison with fossil plants from the same region.