Variations in bone collagen N13C and N15N values of fauna from Northwest Europe over the last 40 000 years

We report here a signal in the temporal variation of stable isotopes in protein from surviving animal bone in Northwest Europe over the past glacial cycle. There is a change in the average N13C values of fauna in the Holocene, and there is also a significant reduction in N15N values of herbivore bon...

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Bibliographic Details
Main Authors: M. P. Richards A, R. E. M. Hedges B
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2001
Subjects:
palaeoclimate
stable isotopes
N13C
N15N
palaeoenvironments
archaeology
Europe
ice core
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1248
http://www.eva.mpg.de/evolution/staff/richards/pdf/MR_and_REMH_Palaeo3.pdf
Description
Summary:We report here a signal in the temporal variation of stable isotopes in protein from surviving animal bone in Northwest Europe over the past glacial cycle. There is a change in the average N13C values of fauna in the Holocene, and there is also a significant reduction in N15N values of herbivore bone collagen towards the end of the last glaciation, with a subsequent recovery soon after the start of the Holocene. This change is observed for several species and is restricted to those regions most affected by the glacial advance. Comparison with ice core data shows that there is a strong correlation between the average N13C values of three herbivore species and ice core CO2 concentration. The data presented here show how readily available faunal bone collagen N13C and N15N measurements provide a record of past climate and environmental change on a regional to continental scale.

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