In a serial paper documenting the tabulate coral fauna of the Omi Limestone, Niigata Prefecture, central Japan, this installment focuses favositid and auloporid species from the Eostaffella-Millerella Zone (late Visean to Bashkirian, Carboniferous). They include Pseudofavosites hinaensis Niko, 1999, Michelinia japonica Niko, 2002, Donetzites sp. cf. D. kibiensis Niko, 1999, and Cladochonus ozawai Niko and Haikawa, 2007. The new specimen of P. hinaensis permits a more detailed description than the holotype, and provides emendations of the specific concept. Apparent faunal similarity between tabulate corals of the Omi Limestone and those of the reef complexes in southwest Japan is recognizable
The Middle and Late Triassic was a time of important reef development. This evolution, which is prim...
This paper treats of the Carboniferous fusulinacean zones of the Koyama Limestone in the so-called K...
A new rugose coral species, Lithostrotion (Siphonodendron) hinensis is described in this paper. It w...
A Moscovian (Late Carboniferous) favositid tabulate coral, Sutherlandia was discovered from the Omi ...
Four species of tabulate corals were found from impure limestone, which characteristically contains ...
Three species of tabulate corals were recovered from a float block of limestone collected in the Kot...
A new species of cleistoporid tabulate coral, Donetzites miyakei, is described from the Endothyra Zo...
A new tabulate coral species, Syringopora konishii, is established on the basis of material from flo...
As the second fascicle, this paper describes five species of Devonian alveolitine tabulate corals fr...
This paper gives the results of investigations on corals, obtained from the Carboniferoes rocks of t...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
As the third fascicle, this paper describes two species of heliolitid tabulate corals, namely Heliol...
In this paper the Carboniferous primitive fusulinacean zones of the Hina Limestone are established, ...
From Carboniferous deposits exposed on the southern slope of the Cantabric mountain chain, 58 rugose...
The pre-Moscovian series of Akiyoshi Limestone (Japan), from late Visean to Bashkirian, is divided i...
The Middle and Late Triassic was a time of important reef development. This evolution, which is prim...
This paper treats of the Carboniferous fusulinacean zones of the Koyama Limestone in the so-called K...
A new rugose coral species, Lithostrotion (Siphonodendron) hinensis is described in this paper. It w...
A Moscovian (Late Carboniferous) favositid tabulate coral, Sutherlandia was discovered from the Omi ...
Four species of tabulate corals were found from impure limestone, which characteristically contains ...
Three species of tabulate corals were recovered from a float block of limestone collected in the Kot...
A new species of cleistoporid tabulate coral, Donetzites miyakei, is described from the Endothyra Zo...
A new tabulate coral species, Syringopora konishii, is established on the basis of material from flo...
As the second fascicle, this paper describes five species of Devonian alveolitine tabulate corals fr...
This paper gives the results of investigations on corals, obtained from the Carboniferoes rocks of t...
Coral fossils were recovered from the Renge area, Itoigawa, Niigata Prefecture, central Japan. They ...
As the third fascicle, this paper describes two species of heliolitid tabulate corals, namely Heliol...
In this paper the Carboniferous primitive fusulinacean zones of the Hina Limestone are established, ...
From Carboniferous deposits exposed on the southern slope of the Cantabric mountain chain, 58 rugose...
The pre-Moscovian series of Akiyoshi Limestone (Japan), from late Visean to Bashkirian, is divided i...
The Middle and Late Triassic was a time of important reef development. This evolution, which is prim...
This paper treats of the Carboniferous fusulinacean zones of the Koyama Limestone in the so-called K...
A new rugose coral species, Lithostrotion (Siphonodendron) hinensis is described in this paper. It w...