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Interpretation of the Miocene Carl Creek limestone, northwestern Queensland

Bibliographic Data

ID19427277
AuthorsDirk Megirian (corresponding author)
Year1992
Volume9
Issue1
Pages219-248
Publication date1992-12-01
Open AccessYes
TypeARTICLE
VenueThe Beagle Records of the Museums and Art Galleries of the Northern Territory (JOURNAL)
Journal identifiersISSN: 0811-3653
PublisherSmithsonian Institution (PUBLISHER • US)
DOI10.5962/p.263126
OpenAlexW2771509584
LanguageEN
Citations received3
References cited1

The Miocene Carl Creek Limestone of Riversleigh, northwestern Queensland, is a clastic deposit composed of sediments characteristic of humid alluvial fans and tufas (sensu Pedley 1990).Factors influencing clastic-carbonate yield and processes of carbonate deposition indicate that the calciclastic alluvial oulwash comprising the Carl Creek Limestone could only have accumulated under relatively dry, perhaps semi-arid, conditions.This palaeoclimatic interpretation for northern Australia during the Miocene is consistent with interpretations from other data-sets.Other limestone formations of similar age, widely distributed across northern Australia in various sedimentary basins represent different depositional environments, but are here related to the Carl Creek Limestone through a hypothetical hydraulic flow system.Archer et al (1989) postulated the former presence of rainforest at Riversleigh on the basis of an exceptionally diverse mammal fauna, interpreted by them as being a sympatric assemblage.Under climatic conditions postulated here for the region during the Miocene, any rainforest was probably restricted to the proximity of perennial, springfed streams within the Carl Creek Limestone depositional basin.The high mammal .speciesdiversity in the Carl Creek Limestone might result from a combination of a rainforest-adapted proximal community, and mesically-adapted distant communities whose members travelled to permanent water sources during dry periods.Thus, radiation of Australia's marsupial faunas into drier habitats was already well advanced by earliest Carl Creek Limestone times, and Miocene rainforest at Riversleigh represented a refugium for rainforest-adapted taxa

Alluvial fan · Clastic rock · Evaporite · Paleoecology · Rainforest · Sedimentary depositional environment · Sedimentary rock · Siliciclastic · Structural basin · Evolution and Paleontology Studies · Paleontology and Evolutionary Biology · Pleistocene-Era Hominins and Archaeology · Ecology · Geology · Paleontology

  • Late Holocene Fluvial Change in a Tufa-depositing Stream

    KAREN D CARTHEW, Russell N Drysdale•Australian Geographer•2003

  • Two New Genera and Three New Species of Thylacinidae (Marsupialia) from the Miocene of the Northern Territory, Australia

    Open Access•Peter Murray, Dirk Megirian•The Beagle Records of the Museums…•2000

  • Interpretation of the Miocene Carl Creek limestone, northwestern Queensland

    Open Access•Dirk Megirian•The Beagle Records of the Museums…•1992

  • Interpretation of the Miocene Carl Creek limestone, northwestern Queensland

    Open Access•Dirk Megirian•The Beagle Records of the Museums…•1992

Citations per year0.09
Citation span1992 - 2003 (12)
Highly citedNo

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