In the present paper, the conodont fauna from three detailed sections surveyed in the Lower Triassic sequence of Central Dolpo, Nepal (Tarap-Atali area) is illustrated. Combining faunas from the three sections, it was possible to recognize a succession of faunal events that covers most of the Scythian and the Lower Anisian. In the whole, 11 faunas have been recognized and discussed
The revision of a comprehensive amount of bibliography has made possible the development of a databa...
The present paper is a preliminary contribution to the stratigraphy and conodont biostratigraphy of ...
© 2018 The Author(s). Conchostracans are one of the most common fossil animal groups of continental ...
After initial opening of Neotethys in the Permian, thermal subsidence and deepening continued in the...
A Late Triassic conodont fauna is described and illustrated for the first time from the San Cassiano...
The Guryul Ravine section in Kashmir, northern India is an important reference section for global Lo...
The stratigraphic succession of central Dolpo (Tarap-Atali area) begins with thick calcsilicate marb...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
The taxonomy, diversity, evolutionary lineages, and stratigraphical distributions of Middle and earl...
Stratigraphically important conodonts occurring in the Anisian/Ladinian boundary interval are prelim...
A short history of more than sixty years of conodont researches in the Carnic Alps is outlined. It i...
The base of the Norian Stage (Carnian/Norian boundary, Upper Triassic) is still awaiting a formal de...
Conodonts from the lowermost Triassic Otoceras woodwardi beds and adjacent strata of Spiti are descr...
The controversial biostratigraphy of the well-known Permo-Triassic (P-T) boundary section at Selong,...
The revision of a comprehensive amount of bibliography has made possible the development of a databa...
The present paper is a preliminary contribution to the stratigraphy and conodont biostratigraphy of ...
© 2018 The Author(s). Conchostracans are one of the most common fossil animal groups of continental ...
After initial opening of Neotethys in the Permian, thermal subsidence and deepening continued in the...
A Late Triassic conodont fauna is described and illustrated for the first time from the San Cassiano...
The Guryul Ravine section in Kashmir, northern India is an important reference section for global Lo...
The stratigraphic succession of central Dolpo (Tarap-Atali area) begins with thick calcsilicate marb...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
Extensive tracts of very shallow water carbonates in the valleys of the Yarkhun and Mastuj rivers of...
The taxonomy, diversity, evolutionary lineages, and stratigraphical distributions of Middle and earl...
Stratigraphically important conodonts occurring in the Anisian/Ladinian boundary interval are prelim...
A short history of more than sixty years of conodont researches in the Carnic Alps is outlined. It i...
The base of the Norian Stage (Carnian/Norian boundary, Upper Triassic) is still awaiting a formal de...
Conodonts from the lowermost Triassic Otoceras woodwardi beds and adjacent strata of Spiti are descr...
The controversial biostratigraphy of the well-known Permo-Triassic (P-T) boundary section at Selong,...
The revision of a comprehensive amount of bibliography has made possible the development of a databa...
The present paper is a preliminary contribution to the stratigraphy and conodont biostratigraphy of ...
© 2018 The Author(s). Conchostracans are one of the most common fossil animal groups of continental ...
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