
Rapid 14C excursion at 3372-3371 BCE not observed at two different locations
Excursions in the carbon-14 (14C) record measured in tree rings are attributed to various high energy but short-lived cosmic effects. Wang et al. proposed a new event at 3372–3371 BCE based on a single set of annual 14C data measured on a floating tree rings from a buried specimen of Chinese wingnut (Pterocarya stenoptera).
Eredeti fellelhetőség: mtmt.hu

