Stratigraphic constraints on the Lower CretaceousOrallo Formation, southeastern Queensland: U-Pbdating of bentonite and palynostratigraphy ofassociated strata
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Cooling, J J
Crowley, J L
McKellar, John
Esterle, J
Nicoll, Robert
Bianchi, Valeria
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Taylor & Francis
Abstract
This 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 Sandstone
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Australian Journal of Earth Sciences
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2099-12-31
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