Radiocarbon dating of modern peat profiles:: Pre- and post-bomb 14C variations in the construction of age-depth models

被引:71
作者
Goslar, T
van der Knaap, WO
Hicks, S
Andric, M
Czernik, J
Goslar, E
Räsänen, S
Hyötylä, H
机构
[1] Adam Mickiewicz Univ Poznan, Fac Phys, PL-61614 Poznan, Poland
[2] Poznan Radiocarbon Lab, PL-61612 Poznan, Poland
[3] Univ Bern, Inst Plant Sci, CH-3013 Bern, Switzerland
[4] Oulu Univ, Inst Geosci, Oulu 90014, Finland
[5] Slovenian Forestry Inst, Ljubljana 1000, Slovenia
[6] Slovian Acad Sci & Arts, Archaeol Inst, Ljubljana 1001, Slovenia
关键词
D O I
10.1017/S0033822200052243
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present studies of 9 modem (up to 400-yr-old) peat sections from Slovenia, Switzerland, Austria, Italy, and Finland. Precise radiocarbon dating of modem samples is possible due to the large bomb peak of atmospheric C-14 concentration in 1963 and the following rapid decline in the C-14 level. All the analyzed C-14 profiles appeared concordant with the shape of the bomb peak of atmospheric C-14 concentration, integrated over some time interval with a length specific to the peat section. In the peat layers covered by the bomb peak, calendar ages of individual peat samples could be determined almost immediately, with an accuracy of 2-3 yr. In the pre-bomb sections, the calendar ages of individual dated samples are determined in the form of multi-modal probability distributions of about 300 yr wide (about AD 1650-1950). However, simultaneous use of the post-bomb and pre-bomb C-14 dates, and lithological information, enabled the rejection of most modes of probability distributions in the pre-bomb section. In effect, precise age-depth models of the post-bomb sections have been extended back in time, into the "wiggly" part of the C-14 calibration curve. Our study has demonstrated that where annual resolution is concerned, tissues of Sphagnum are the only representative material for C-14 dating, although even samples of pure Sphagnum collected from a very thin slice of the peat section contain tissues grown in different years, so they integrate the atmospheric C-14 signal over a period of time. This time period (0.5-8 yr, depending on the site) seems to correlate with the peat accumulation rate, but it also depends on how the sampled peat sections were handled. When constructing age-depth models, for some peat sections we used the strategy of multi-stage C-14 dating. This led to a drastic reduction in the uncertainty of the age-depth models, by dating only a few additional samples in the profile. Our study is the first in which peat sections from the late pre-bomb time (AD 1900-1960) have been precisely dated at a high temporal resolution. In this time interval, C-14 ages of all the samples dated were younger than those derived from the atmospheric calibration curve, apparently due to the effect of integration. Evidently, the determination of calendar ages based on C-14 dating of single peat samples from that interval may be affected by a serious error if the possibility of integration is ignored.
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页码:115 / 134
页数:20
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