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U–Pb zircon dating from tuffs in the Canning Basin reveals a 1.7-million-year age conflict between palynological zones. The dataset documents an age of 267.04 ± 0.14 Ma for the Microbaculispora villosa Zone, challenging established biostratigraphic correlations. This research by Mory et al. (2017) presents isotopic and palynological evidence from the middle Permian.
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