• DOI:10.1046/j.1440-0952.2003.00984.x
• Corpus ID: 128739024

First known Cretaceous glaciation: Livingston Tillite Member of the Cadna‐owie Formation, South Australia

@article{Alley2003FirstKC,
  title={First known Cretaceous glaciation: Livingston Tillite Member of the Cadna‐owie Formation, South Australia},
  author={Neville F. Alley and Lawrence A. Frakes},
  journal={Australian Journal of Earth Sciences},
  year={2003},
  volume={50},
  pages={139 - 144}
}

• N. Alley, L. Frakes
• Published 1 April 2003
• Geology, Environmental Science
• Australian Journal of Earth Sciences

A 2 m‐thick diamictite occurs near the base of the Cretaceous Eromanga Basin succession at Trinity Well, at the northern extremity of the Flinders Ranges in South Australia. The diamictite consists of a matrix of silt‐ and clay‐size particles and a framework of sand and coarser materials up to small boulder size. Scanning electron microscope study reveals the presence of numerous quartz grains displaying extreme angularity and surface textures attributed to glacial crushing. Sandy sediments considered as fluvioglacial in origin and a locally developed facies displaying flow structures attributed to solifluction processes constitute the basal 3–5 m of the sequence. In places these directly underlie the diamictite and rest with angularity on Neoproterozoic Adelaidean strata. Conformably above the diamictite at the type locality ‘Recorder Hill’ is a sequence approximately 15 m thick of fine sand and silt units containing lonestones up to ∼70 cm diameter and hummocky cross‐stratification. These sediments have been assigned to the Cadna‐owie Formation and are dated on palynology as Berriasian to Valanginian. The occurrence of diamictite containing glacially affected quartz grains contributes to our interpretation that the southern margin of the Eromanga Basin, and at least the adjacent part of the northern Flinders Ranges, were affected by glaciation in the Early Cretaceous. The associated dropstone and solifluction facies and nearby glendonite pseudomorphs after ikaite are further evidence of at least intermittent cold climates at this time.