In Myanmar, Middle Devonian coral bearing carbonate deposits arelimited in Pyinoolwin Township, i.e. Padaukpin area and Pwepon area. At the generic level, most rugose corals from the "Maymyo Formation" including Padaukpin Limestone and Pwepon Limestone are widely distributed especially in the Old World Realm. Detailed palaeoecological study indicates that the abundant rugose coral fauna from the .Middle Devonian "Maymyo Formation" may have lived in a warm, shallow, well-oxygenated seas having moderate to high wave energy probably situated near the margin of the carbonate platform adjacent to the basinal deposits in tropical to temperate zone. After death they had been transported and quickly deposited in a calm water environment on the con...
Limestone and chert sections from the Loei fold belt in Loei Province, northeastern Thailand, have y...
Rugosa and Tabulata from the Late Devonian of central Dolpo (Nepal) belong to the genera Kuangxiastr...
Metazoan reef builders receded globally during the Carboniferous resulting from the Late Devonian ex...
The occurence of approximately 100 rugose coral genera has been confirmed in the Devonian carbonate ...
Rich coral faunas occur within a major transgressional-regressional cycle of latest Eifelian to Give...
The most earliest Mississippian rugose corals are post-disaster taxa occurring in a biosphere strong...
Eight provinces of coral distribution were established in the Early Devonian of Eurasia and Australi...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
The distribution of Rugose Corals between the end of the Frasnian and the early Tournaisian is revie...
The Karakorum Block is regarded as a microplate of "Gondwanan" origin and was part of the Cimmerian ...
The Fanning River Group is among the best exposed marine-dominated Devonian sequences in eastern Aus...
Normal marine salinity is the main limiting factor for the Subclass Rugosa. Water depth and temperat...
The Bitlis-Pörtürge Massif of SE Turkey is a metamorphic belt separating the Arabian Plate from the ...
The Jack Formation forms part of the Silurian Graveyard Creek Group within the Graveyard Creek Subpr...
A middle Viséan (Mississippian) coral biostrome is reported for the first time from the Shangsi Form...
Limestone and chert sections from the Loei fold belt in Loei Province, northeastern Thailand, have y...
Rugosa and Tabulata from the Late Devonian of central Dolpo (Nepal) belong to the genera Kuangxiastr...
Metazoan reef builders receded globally during the Carboniferous resulting from the Late Devonian ex...
The occurence of approximately 100 rugose coral genera has been confirmed in the Devonian carbonate ...
Rich coral faunas occur within a major transgressional-regressional cycle of latest Eifelian to Give...
The most earliest Mississippian rugose corals are post-disaster taxa occurring in a biosphere strong...
Eight provinces of coral distribution were established in the Early Devonian of Eurasia and Australi...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
The distribution of Rugose Corals between the end of the Frasnian and the early Tournaisian is revie...
The Karakorum Block is regarded as a microplate of "Gondwanan" origin and was part of the Cimmerian ...
The Fanning River Group is among the best exposed marine-dominated Devonian sequences in eastern Aus...
Normal marine salinity is the main limiting factor for the Subclass Rugosa. Water depth and temperat...
The Bitlis-Pörtürge Massif of SE Turkey is a metamorphic belt separating the Arabian Plate from the ...
The Jack Formation forms part of the Silurian Graveyard Creek Group within the Graveyard Creek Subpr...
A middle Viséan (Mississippian) coral biostrome is reported for the first time from the Shangsi Form...
Limestone and chert sections from the Loei fold belt in Loei Province, northeastern Thailand, have y...
Rugosa and Tabulata from the Late Devonian of central Dolpo (Nepal) belong to the genera Kuangxiastr...
Metazoan reef builders receded globally during the Carboniferous resulting from the Late Devonian ex...