Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia

If ancient carbon is incorporated into lakes and rivers, it can be transferred along the foodchain where it can cause radiocarbon dates to appear erroneously old. This effect is known as the 14 C freshwater reservoir effect (FRE), and causes particular problems when dating human remains. Several stu...

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Published in:Radiocarbon
Main Authors: Wood, R E, Higham, T F G, Buzilhova, A, Suvorov, A, Heinemeier, J, Olsen, J
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2013
Subjects:
Online Access:http://dx.doi.org/10.1017/s0033822200047883
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spelling crcambridgeupr:10.1017/s0033822200047883 2024-03-03T08:47:30+00:00 Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia Wood, R E Higham, T F G Buzilhova, A Suvorov, A Heinemeier, J Olsen, J 2013 http://dx.doi.org/10.1017/s0033822200047883 en eng Cambridge University Press (CUP) Radiocarbon volume 55, issue 01, page 163-177 ISSN 0033-8222 1945-5755 General Earth and Planetary Sciences Archeology journal-article 2013 crcambridgeupr https://doi.org/10.1017/s0033822200047883 2024-02-08T08:45:08Z If ancient carbon is incorporated into lakes and rivers, it can be transferred along the foodchain where it can cause radiocarbon dates to appear erroneously old. This effect is known as the 14 C freshwater reservoir effect (FRE), and causes particular problems when dating human remains. Several studies have attempted to use carbon and/or nitrogen stable isotopes to predict the size of the FRE, with mixed success. We have examined whether the FRE at the Mesolithic-Neolithic burial ground of Minino, northwest Russia, is correlated with these stable isotope systems. To assess the size of the FRE, 9 pairs of human bone and burial goods were dated, such as spears and pendants made of herbivore bone. In addition, further human and faunal bones were analyzed for carbon and nitrogen stable isotopes. Although these stable isotopes suggest that freshwater resources dominated the protein intake of those buried at Minino, no relationship between stable isotopes and the FRE was found. Instead, we found that the FRE was relatively consistent at 490 ± 80 14 C yr. With caution, this can be subtracted from burials at Minino to provide a low-resolution chronology for the burial ground. We demonstrate that it is not possible to assume that a relationship exists between stable isotopes and 14 C, and each population thought to be affected by a FRE must be examined individually. Article in Journal/Newspaper Northwest Russia Cambridge University Press Minino ENVELOPE(35.300,35.300,63.783,63.783) Radiocarbon 55 01 163 177
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
Archeology
spellingShingle General Earth and Planetary Sciences
Archeology
Wood, R E
Higham, T F G
Buzilhova, A
Suvorov, A
Heinemeier, J
Olsen, J
Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
topic_facet General Earth and Planetary Sciences
Archeology
description If ancient carbon is incorporated into lakes and rivers, it can be transferred along the foodchain where it can cause radiocarbon dates to appear erroneously old. This effect is known as the 14 C freshwater reservoir effect (FRE), and causes particular problems when dating human remains. Several studies have attempted to use carbon and/or nitrogen stable isotopes to predict the size of the FRE, with mixed success. We have examined whether the FRE at the Mesolithic-Neolithic burial ground of Minino, northwest Russia, is correlated with these stable isotope systems. To assess the size of the FRE, 9 pairs of human bone and burial goods were dated, such as spears and pendants made of herbivore bone. In addition, further human and faunal bones were analyzed for carbon and nitrogen stable isotopes. Although these stable isotopes suggest that freshwater resources dominated the protein intake of those buried at Minino, no relationship between stable isotopes and the FRE was found. Instead, we found that the FRE was relatively consistent at 490 ± 80 14 C yr. With caution, this can be subtracted from burials at Minino to provide a low-resolution chronology for the burial ground. We demonstrate that it is not possible to assume that a relationship exists between stable isotopes and 14 C, and each population thought to be affected by a FRE must be examined individually.
format Article in Journal/Newspaper
author Wood, R E
Higham, T F G
Buzilhova, A
Suvorov, A
Heinemeier, J
Olsen, J
author_facet Wood, R E
Higham, T F G
Buzilhova, A
Suvorov, A
Heinemeier, J
Olsen, J
author_sort Wood, R E
title Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
title_short Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
title_full Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
title_fullStr Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
title_full_unstemmed Freshwater Radiocarbon Reservoir Effects at the Burial Ground of Minino, Northwest Russia
title_sort freshwater radiocarbon reservoir effects at the burial ground of minino, northwest russia
publisher Cambridge University Press (CUP)
publishDate 2013
url http://dx.doi.org/10.1017/s0033822200047883
long_lat ENVELOPE(35.300,35.300,63.783,63.783)
geographic Minino
geographic_facet Minino
genre Northwest Russia
genre_facet Northwest Russia
op_source Radiocarbon
volume 55, issue 01, page 163-177
ISSN 0033-8222 1945-5755
op_doi https://doi.org/10.1017/s0033822200047883
container_title Radiocarbon
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container_issue 01
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