2012
DOI: 10.2478/s13386-012-0015-3
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Dating of the Reo site (Island of Saaremaa, Estonia) with silicate and iron microspherules points to an exact age of the fall of the Kaali meteorite

Abstract: Pollen analyses and radiocarbon dates from the bottom sediments in the Kaali main crater suggested that the crater group is at least 4000-5000 years old. Investigations of silicate impact microspherules in surrounding mires (Raukas et al. 1995) put the age about 7500-7600 yr BP. Recently we found both silicate and iron microspherules from organic sediments below well-dated beach ridge in Reo site what supports the conclusions that the most realistic age of the Kaali craters is 7600±50 14 C BP (8335-8537 cal BP… Show more

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Cited by 4 publications
(14 citation statements)
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“…) and the Reo gravel pit (Moora et al. ), and considerably older than proposed ages (800–400 BCE) of the Kaali based on detecting a meteoritic signal within the Piila bog (Rasmussen et al. ; Veski et al.…”
Section: Discussionmentioning
confidence: 95%
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“…) and the Reo gravel pit (Moora et al. ), and considerably older than proposed ages (800–400 BCE) of the Kaali based on detecting a meteoritic signal within the Piila bog (Rasmussen et al. ; Veski et al.…”
Section: Discussionmentioning
confidence: 95%
“…) or iron‐nickel spherules (Moora et al. ) and Kaali has not been established. An association between them and the crater is based on geographical proximity of the impact site with the Piila bog (~10 km) and Reo gravel pit (~7.5 km).…”
Section: Discussionmentioning
confidence: 99%
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