Rich coral faunas occur within a major transgressional-regressional cycle of latest Eifelian to Givetian age at the base of the Burdekin Basin, north Queensland. This sequence is represented by the tripartite Fanning River Group, with the initial Big Bend Arkose comprising non-marine to near-shore siliciclastic deposits, followed by the predominantly carbonate Burdekin Formation developed in shallow shelf environments, and at the top, the Cultivation Gully Formation of sandstones and shales representing the concluding regressive phase. Thirty-three species and subspecies of rugose corals are described from the Fanning River Group including the following 11 new taxa: Lekanophyllum fultum zonophylloides subsp. nov., L. hillae sp. nov., Centri...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
With 7 figures Abstract: A rugose coral fauna from Givetian and Lower Frasnian strata of the Khoshye...
The Bitlis-Pörtürge Massif of SE Turkey is a metamorphic belt separating the Arabian Plate from the ...
The Fanning River Group is among the best exposed marine-dominated Devonian sequences in eastern Aus...
The occurence of approximately 100 rugose coral genera has been confirmed in the Devonian carbonate ...
The Laroona Formation and Mount Podge Limestone are defined for the lower conglomerates and micaceou...
The Jack Formation forms part of the Silurian Graveyard Creek Group within the Graveyard Creek Subpr...
In Myanmar, Middle Devonian coral bearing carbonate deposits arelimited in Pyinoolwin Township, i.e....
Of the fourteen species (six new) assigned to eight rugosan and five tabulatan genera, identified ...
The most earliest Mississippian rugose corals are post-disaster taxa occurring in a biosphere strong...
The Karakorum Block is regarded as a microplate of "Gondwanan" origin and was part of the Cimmerian ...
Palaeozoic coral communities were dominated by two extinct coral groups: Tabulata and Rugosa. Whilst...
Preliminary to the descriptions of genera and species is a very brief discussion of coral terminolog...
The distribution of Rugose Corals between the end of the Frasnian and the early Tournaisian is revie...
The small solitary coral dominated, Grypophgllum-Ctnstophgllum association, a pioneer coral communit...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
With 7 figures Abstract: A rugose coral fauna from Givetian and Lower Frasnian strata of the Khoshye...
The Bitlis-Pörtürge Massif of SE Turkey is a metamorphic belt separating the Arabian Plate from the ...
The Fanning River Group is among the best exposed marine-dominated Devonian sequences in eastern Aus...
The occurence of approximately 100 rugose coral genera has been confirmed in the Devonian carbonate ...
The Laroona Formation and Mount Podge Limestone are defined for the lower conglomerates and micaceou...
The Jack Formation forms part of the Silurian Graveyard Creek Group within the Graveyard Creek Subpr...
In Myanmar, Middle Devonian coral bearing carbonate deposits arelimited in Pyinoolwin Township, i.e....
Of the fourteen species (six new) assigned to eight rugosan and five tabulatan genera, identified ...
The most earliest Mississippian rugose corals are post-disaster taxa occurring in a biosphere strong...
The Karakorum Block is regarded as a microplate of "Gondwanan" origin and was part of the Cimmerian ...
Palaeozoic coral communities were dominated by two extinct coral groups: Tabulata and Rugosa. Whilst...
Preliminary to the descriptions of genera and species is a very brief discussion of coral terminolog...
The distribution of Rugose Corals between the end of the Frasnian and the early Tournaisian is revie...
The small solitary coral dominated, Grypophgllum-Ctnstophgllum association, a pioneer coral communit...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
With 7 figures Abstract: A rugose coral fauna from Givetian and Lower Frasnian strata of the Khoshye...
The Bitlis-Pörtürge Massif of SE Turkey is a metamorphic belt separating the Arabian Plate from the ...