The palaeoenvironment and conditions of deposition at Mulbring Quarry have been the subject of academic research. Vanderlaan (2007) concluded that
the deposition of the specimens took place in a quiet shallow marine, low
energy environment. This is evidenced by low levels of fragmentation in the bryozoans and most of the bivalves and brachiopods are articulated meaning that the segments are found still attached together. The position of the site on the continent can also be inferred by the high levels of lithic material and the presence of wood fragments (Vanderlaan, 2007) indicating that the original site of deposition was mid-continental shelf below the normal wave base and at a high latitude. Vanderlaan (2007) notes that the presence of drop stones is an indicator of a cold water environment with seasonal ice cover. The drop stones and wood fragments however are quite small and are not common but still occur.
References
Excursion Handout. 2012. Permian Fossils and Palaeoenvironments of the Hunter Valley.Percival, I.G. 1979. The geological heritage of New South Wales, volume 1. Geological Society of Australia, Sydney.
Vanderlaan, T. 2007. Middle Permian palaeoecology and depositional environment of the Fenestella Shale Member, Branxton Formation, lower Hunter Valley. Unpub. Hons Thesis, Macquarie University.
Hi, I know this a long shot but would you be able to help me locate the name and contacts for the owners of the Mulbring Quarry as I would like to take my grandthere in the holidays, small group of around 20. Regards
ReplyDeleteLeanda