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An Icelandic freshwater radiocarbon reservoir effect: Implications for lacustrine 14C chronologies

Ascough, PL; Cook, GT; Hastie, H; Dunbar, E; Church, MJ; Einarsson, Á; McGovern, TH; Dugmore, AJ

An Icelandic freshwater radiocarbon reservoir effect: Implications for lacustrine 14C chronologies Thumbnail


PL Ascough

GT Cook

H Hastie

E Dunbar

Á Einarsson

TH McGovern

AJ Dugmore


A freshwater radiocarbon (14C) reservoir effect (FRE) is a 14C age offset between the atmospheric and freshwater carbon reservoirs. FREs can be on the order of 10 000 14C yr in extreme examples and are a crucial consideration for 14C dating of palaeoenvironmental and archaeological samples. Correction for a FRE may be possible, provided the FRE and the proportion of FRE-affected carbon within a sample can be accurately quantified. However, although such correction is desirable for affected samples, it is essential that such correction is accurate in order to produce useful chronological information. Accuracy of FRE correction can be limited by spatial variation in FRE within a freshwater system, but despite this there is currently a paucity of information to identify and quantify such variability within affected systems. Here we present results of a study that investigates the effects of spatial FRE variation upon dating accuracy within the freshwater system of Lake Mývatn, northern Iceland. A substantial FRE (>10 000 14C yr) has previously been identified in archaeological and modern samples from the region, which shows the potential for considerable spatial variability. The study also assesses the use of δ13C and δ15N in age correction of affected samples. The results show that benthic detritus and organisms at primary trophic levels from locations within the lake are affected by a FRE of at least 3500 14C yr, with clear spatial variation resulting in 14C age differences of up to 7670 14C yr between samples. There is a broad correlation between stable isotope values and FRE within the data set. However, large associated uncertainties currently preclude highly accurate and precise stable isotope-based quantification of the proportion of FRE-affected carbon within archaeological and palaeoenvironmental samples from Mývatn and the surrounding region.


Ascough, P., Cook, G., Hastie, H., Dunbar, E., Church, M., Einarsson, Á., …Dugmore, A. (2011). An Icelandic freshwater radiocarbon reservoir effect: Implications for lacustrine 14C chronologies. Holocene, 21(7), 1073-1080.

Journal Article Type Article
Publication Date Nov 1, 2011
Deposit Date Jul 22, 2011
Publicly Available Date Oct 15, 2014
Journal Holocene
Print ISSN 0959-6836
Electronic ISSN 1477-0911
Publisher SAGE Publications
Peer Reviewed Peer Reviewed
Volume 21
Issue 7
Pages 1073-1080
Keywords Freshwater, Iceland, Radiocarbon, Reservoir effect.


Accepted Journal Article (864 Kb)

Copyright Statement
The final definitive version of this article has been published in the journal The Holocene, 21/7, 2011 © The Author(s) 2011 by SAGE Publications Ltd at The Holocene page: on SAGE Journals Online:

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