The palaeoenvironmental δ13C record in European woolly mammoth tooth enamel

L. Arppe; Kim Aaris-Sørensen; L. Daugnora; L. Lõugas; P. Wojtal; I. Zupiņš

doi:10.1016/j.quaint.2010.10.018

The palaeoenvironmental δ¹³C record in European woolly mammoth tooth enamel

L. Arppe, Kim Aaris-Sørensen, L. Daugnora, L. Lõugas, P. Wojtal, I. Zupiņš

10 Citationer (Scopus)

Abstract

The carbon isotope composition (δ¹³C) of tooth enamel of woolly mammoth molars from Estonia, Latvia, Lithuania, Denmark and southern Poland was analysed and the data were complemented with previously published δ¹³C values from Sweden, Finland and northwestern Russia, Switzerland and Britain. The δ¹³C values display a NE- to SW-trending geographical pattern, with more depleted compositions in the northeast, suggesting differences in the diet consumed by mammoths in the northeastern parts of the study area relative to mammoths in the southwesterly regions. While the pattern is probably a reflection of a number of controlling environmental parameters, with possible additional contribution from physiological factors, statistically significant correlations of the δ¹³C values to δ¹⁸O data from the same specimens and to palaeotemperature estimates imply a strong influence of climate over the δ¹³C values. The δ¹³C data do not provide convincing evidence of any temporal changes in diet.

Originalsprog	Engelsk
Tidsskrift	Quaternary International
Vol/bind	245
Udgave nummer	2
Sider (fra-til)	285-290
Antal sider	6
ISSN	1040-6182
DOI	https://doi.org/10.1016/j.quaint.2010.10.018
Status	Udgivet - 6 dec. 2011

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Adgang til dokumentet

10.1016/j.quaint.2010.10.018

Citationsformater

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title = "The palaeoenvironmental δ13C record in European woolly mammoth tooth enamel",

abstract = "The carbon isotope composition (δ13C) of tooth enamel of woolly mammoth molars from Estonia, Latvia, Lithuania, Denmark and southern Poland was analysed and the data were complemented with previously published δ13C values from Sweden, Finland and northwestern Russia, Switzerland and Britain. The δ13C values display a NE- to SW-trending geographical pattern, with more depleted compositions in the northeast, suggesting differences in the diet consumed by mammoths in the northeastern parts of the study area relative to mammoths in the southwesterly regions. While the pattern is probably a reflection of a number of controlling environmental parameters, with possible additional contribution from physiological factors, statistically significant correlations of the δ13C values to δ18O data from the same specimens and to palaeotemperature estimates imply a strong influence of climate over the δ13C values. The δ13C data do not provide convincing evidence of any temporal changes in diet.",

author = "L. Arppe and Kim Aaris-S{\o}rensen and L. Daugnora and L. L{\~o}ugas and P. Wojtal and I. Zupiņ{\v s}",

year = "2011",

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doi = "10.1016/j.quaint.2010.10.018",

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TY - JOUR

T1 - The palaeoenvironmental δ13C record in European woolly mammoth tooth enamel

AU - Arppe, L.

AU - Aaris-Sørensen, Kim

AU - Daugnora, L.

AU - Lõugas, L.

AU - Wojtal, P.

AU - Zupiņš, I.

PY - 2011/12/6

Y1 - 2011/12/6

N2 - The carbon isotope composition (δ13C) of tooth enamel of woolly mammoth molars from Estonia, Latvia, Lithuania, Denmark and southern Poland was analysed and the data were complemented with previously published δ13C values from Sweden, Finland and northwestern Russia, Switzerland and Britain. The δ13C values display a NE- to SW-trending geographical pattern, with more depleted compositions in the northeast, suggesting differences in the diet consumed by mammoths in the northeastern parts of the study area relative to mammoths in the southwesterly regions. While the pattern is probably a reflection of a number of controlling environmental parameters, with possible additional contribution from physiological factors, statistically significant correlations of the δ13C values to δ18O data from the same specimens and to palaeotemperature estimates imply a strong influence of climate over the δ13C values. The δ13C data do not provide convincing evidence of any temporal changes in diet.

AB - The carbon isotope composition (δ13C) of tooth enamel of woolly mammoth molars from Estonia, Latvia, Lithuania, Denmark and southern Poland was analysed and the data were complemented with previously published δ13C values from Sweden, Finland and northwestern Russia, Switzerland and Britain. The δ13C values display a NE- to SW-trending geographical pattern, with more depleted compositions in the northeast, suggesting differences in the diet consumed by mammoths in the northeastern parts of the study area relative to mammoths in the southwesterly regions. While the pattern is probably a reflection of a number of controlling environmental parameters, with possible additional contribution from physiological factors, statistically significant correlations of the δ13C values to δ18O data from the same specimens and to palaeotemperature estimates imply a strong influence of climate over the δ13C values. The δ13C data do not provide convincing evidence of any temporal changes in diet.

U2 - 10.1016/j.quaint.2010.10.018

DO - 10.1016/j.quaint.2010.10.018

M3 - Journal article

SN - 1040-6182

VL - 245

SP - 285

EP - 290

JO - Quaternary International

JF - Quaternary International

IS - 2