Cooling, J JCrowley, J LMcKellar, JohnEsterle, JNicoll, RobertBianchi, Valeria2022-02-020812-0099http://hdl.handle.net/1885/259036This study presents two chemical abrasion-thermal ionisation mass spectrometry (CA-TIMS) U–Pb zircon ages from tuffs as well as palynostratigraphic results from the embracing sedimentary succession of the Orallo Formation, Surat Basin, Queensland. Samples were taken from two Geological Survey of Queensland (GSQ) stratigraphic holes, GSQ DRD 26 and GSQ Roma 2. Palynological results assign the upper part of the Orallo Formation to the lower part of the Ruffordiaspora australiensis Interval Zone rather than the upper part of this zone as previously indicated. A late Valanginian isotopic date of 134.38 ± 0.04 Ma from GSQ DRD 26 and an early Hauterivian date of 132.46 ± 0.36 Ma from GSQ Roma 2 give the Orallo Formation a Berriasian?/ Valanginian–Hautevarian age, rather than the previously inferred Berriasian–Valanginian age determined without any geochronological control. Additionally, when combined with previously published geochronological dates from the Westbourne Formation, these ages suggest that, in the Surat Basin succession, the Jurassic–Cretaceous boundary most likely lies within the Gubberamunda Sandstoneapplication/pdfen-AU© 2020 Geological Society of AustraliaCA-IDTIMSgeochronologypalynologySurat BasinstratigraphyOrallo FormationJ–K boundary202010.1080/08120099.2020.17816902020-12-13