The 14 C Content of Modern Vegetation Samples from the Flanks of the Katla Volcano, Southern Iceland

• Published in: Radiocarbon
• Main Authors: Shore, J. S., Cook, G. T., Dugmore, A. J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 1995
• Subjects: General Earth and Planetary Sciences; Archeology; Katla; Mýrdalur; Engimýri; Iceland
• Online Access: http://dx.doi.org/10.1017/s0033822200031015; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200031015

Samples of living terrestrial plants comprising a moss ( Calliergon sp.), Carex spp. and Alchemilla spp. were collected from the surface of the mire at Engimýri in Mýrdalur, southern Iceland, 10 km from the crater rim of the central complex of the Katla volcano. This area is 16 km from the fissures active in ad 1918 and was directly affected by the tephra fall. Although there is no hot-spring or fumerole activity in the area, sufficient volcanic activity during the weeks preceding sample collection produced a strong sulphurous odor in the streams. As part of a large-scale dating program, we analyzed the modern vegetation to determine whether anomalies caused by the uptake of “old” volcanic CO 2 were apparent. The results showed 14 C values for the Calliergon sp., Carex spp. and Alchemilla spp. of 113.2 ± 0.6 pMC, 113.03 ± 0.52 pMC and 113.10 ± 0.6 pMC, respectively. The δ 13 C PDB values were −28.7‰, −28.0‰ and −27.0‰, respectively. Similar vegetation, i.e. , terrestrial plants from a marsh environment in southern Scotland, were also analyzed as a comparison and gave 14 C values of 113.16 ± 0.55 and 112.98 ± 0.59 pMC. The implication is that Icelandic vegetation at Engimýri is not affected by “old” carbon from volcanic emissions and dates obtained for this Icelandic peat are acceptable and directly comparable with Scottish peat.