Iranognathus sosioensis n.sp., a Changxingian (latest Permian) conodont species of western Sicily, is the youngest Iranognathus species occurring immediately below the Permian-Triassic boundary.The Middle Permian and part of the Late Permian pelagic conodontfaunas of western Sicily are cold bottom-watter faunas, very dif ferentfrom the contemporaneous pelagic warm water faunas . The facial pretensions of I. sosioensis are not yet known. </div
The Permian limestone boulders reworked in the Triassic Lercara Formation (NW Sicily) contain carbon...
A rich, diverse Permian ostracod fauna has been recovered from the red and grey, laminated shales an...
The most lethal mass-extinction of the history of life occurred at the Permian-Triassic boundary (PT...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) c...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) p...
The correlation between the fusulinid-based Tethyan and the conodont-based international timescales ...
The controversial biostratigraphy of the well-known Permo-Triassic (P-T) boundary section at Selong,...
The Bellerophon (Late Permian) and Werfen (Lower Triassic) Formations were investigated on the basis...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
The taxonomy and phylomorphogenesis of conodont pectiniform elements around the Carnian/Norian bound...
Permian strata from the Tieqiao section (Jiangnan Basin, South China) contain several distinctive co...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
Four new species of the conodont genus Hindeodus, Hindeodus eurypyge sp. nov., Hindeodus inflatus sp...
The recovery of conodonts associated with ash beds and magnetostratigraphy in the key Zhongzhai Sect...
The marine conodont fossil species, Hindeodus changxingensis Wang, that has a distinctive morphology...
The Permian limestone boulders reworked in the Triassic Lercara Formation (NW Sicily) contain carbon...
A rich, diverse Permian ostracod fauna has been recovered from the red and grey, laminated shales an...
The most lethal mass-extinction of the history of life occurred at the Permian-Triassic boundary (PT...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) c...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) p...
The correlation between the fusulinid-based Tethyan and the conodont-based international timescales ...
The controversial biostratigraphy of the well-known Permo-Triassic (P-T) boundary section at Selong,...
The Bellerophon (Late Permian) and Werfen (Lower Triassic) Formations were investigated on the basis...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
The taxonomy and phylomorphogenesis of conodont pectiniform elements around the Carnian/Norian bound...
Permian strata from the Tieqiao section (Jiangnan Basin, South China) contain several distinctive co...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
Four new species of the conodont genus Hindeodus, Hindeodus eurypyge sp. nov., Hindeodus inflatus sp...
The recovery of conodonts associated with ash beds and magnetostratigraphy in the key Zhongzhai Sect...
The marine conodont fossil species, Hindeodus changxingensis Wang, that has a distinctive morphology...
The Permian limestone boulders reworked in the Triassic Lercara Formation (NW Sicily) contain carbon...
A rich, diverse Permian ostracod fauna has been recovered from the red and grey, laminated shales an...
The most lethal mass-extinction of the history of life occurred at the Permian-Triassic boundary (PT...