AGE OF THE YOUNGER LAXÁ LAVA AND LAKE MÝVATN, NORTHERN ICELAND, DETERMINED BY AMS RADIOCARBON DATING

Lake Mývatn and several smaller lakes in northern Iceland were formed by the large Holocene lava flow of the Younger Laxa Lava (YLL). The age of the YLL was estimated by tephrochronology at 1800–2300 BP (Thorarinsson 1951). Conventional radiocarbon dating of charred vegetation beneath the YLL (Thorarinsson 1964) yielded uncalibrated ages of 1940 ± 270 14 C yr BP (Yale), 2110 ± 140 14 C yr BP (Copenhagen), and 1990 ± 50 14 C yr BP (Winnipeg). Ongoing paleolimnological research at Lake Mývatn requires a more precise age estimation of the YLL. Charcoal samples from beneath the YLL was collected at Presthvammur in 2007 and analyzed by accelerator mass spectrometry (AMS) 14 C measurements. The reliability of the conventional 14 C ages of the samples Yale, Copenhagen, and Winnipeg was re-evaluated, applying criteria from Pettit et al. (2003) and Graf (2009). The result of AMS 14 C measurement (2170 ± 38 cal yr BP) underpins the local tephrochronology and provides a reliable age of the YLL and Lake Mývatn. DOI:  10.2458/azu_js_rc.v54i2.15970