4.2 Article

Radiocarbon dating distal tephra from the Early Bronze Age Avellino eruption (EU-5) in the coastal basins of southern Lazio (Italy): Uncertainties, results, and implications for dating distal tephra

Journal

QUATERNARY GEOCHRONOLOGY
Volume 63, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.quageo.2021.101154

Keywords

Tephrochronology; Radiocarbon dating; Bayesian analysis; Sampling error; Avellino eruption; Tephra toxicity; Central Italy

Funding

  1. Netherlands Organisation for Scientific Research (NWO), Free Competition grant [360-61-060]

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The study analyzed the age of the major Somma-Vesuvius Avellino (AV) eruption, obtaining more accurate results through an improved methodology and resolving controversies. This highlights the need for a thorough approach in C-14 dating in the Central Mediterranean. The study also points out potential environmental issues caused by toxic fluorine concentrations in volcanic tephra.
Distal tephra from the major Somma-Vesuvius Avellino (AV) eruption is widespread in the coastal basins of Southern Lazio (Central Italy). Dated to 1995 +/- 10 cal yr BC in 2011, later on doubts arose about the reliability of this frequently cited age. This led to a major effort to date AV tephra holding sections, based on a thorough methodological approach. Various aspects were studied to identify sections yielding reliable C-14 ages, including bioturbation, inbuilt age, and variable sediment accumulation rate. Lowered rates upon deposition of tephra, particularly in anoxic marshy environments and attributed to toxic F contents, showed up as sharp increases in pollen density. The 'sampling error' was quantified for specific sedimentary environments and derived from coring data and published data on accum|ulation rates for similar Central Mediterranean sites. Next, two Bayesian analyses were performed, a traditional using the full set of samples and a novel, based on samples that were deemed as suitable (no bioturbation, inbuilt age, etc.) and of which the age was corrected for the sampling error. The age obtained by the novel analysis had the smallest range (1909-1868 cal yr BC), differs about a century, and is virtually identical to the ages published by Passariello et al. (2009) and Alessandri (2019). The earlier found age (2011) is ascribed to a statistical coincidence. The results solve a long debate on the age of the AV eruption, which is the youngest of the three major eruptions in the Central Mediterranean Bronze Age. Ages of the other two, the Agnano Mt Spina (Phlegrean) and FL eruption (Etna), are still uncertain and disputed. This study illustrates the need for a thorough approach in C-14 dating tephra holding sediment archives in the Central Mediterranean, and employed a methodology that can be applied in such approach. Attention is called for potentially toxic fluorine concentrations in Campanian tephra, which may have had a serious impact on the contemporary environment and induced chronological hiatuses, but hitherto were not reported for the early tephra.

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