Belonechitina capitata, a typically middle to late Ordovician chitinozoan index taxon was for the first time recovered from the northeastern Kumaon region, a part of Garhwal-Kumaon Tethys basin of the Himalaya, India. This species is of great biostratigraphic importance and has already been reported from Avalonia, Baltica and northern Gondwana. The study area was during Ordovician, part of a low-palaeolatitudinal Gondwana region. The vesicles of recovered forms are black and fragmentary. This is principally attributed to intense tectonic activity during the Himalayan orogenic movement which resulted into high thermal alteration. The chitinozoans are found along with melanosclerites
International audienceThe base of the Darriwilian Stage is defined by the first appearance datum (FA...
International audienceThe QUSAIBA-1 shallow core drilled in NW Saudi Arabia penetrated the Qalibah, ...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
AbstractBelonechitina capitata, a typically middle to late Ordovician chitinozoan index taxon was fo...
Belonechitina capitata, a typically middle to late Ordovician chitinozoan index taxon was for the fi...
The Shiala Formation of the Garhwal-Kumaon subbasin of the Tethyan Himalaya, has been sampled for ch...
International audienceDuring extensive investigations carried out recently on the chitinozoans from ...
Three new chitinozoan species, Conochitina savalaensis, Conochitina viruana and Belonechitina intons...
Chitinozoans from seven cores in the Middle Ordovician upper Goldwyer and Nita for-mations are docum...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
A chitinozoan faunule is reported from a shallow-marineLower Ordovician sequence in the subsurface o...
Isolated chitinozoans from the Scorn Shale Member of the Cedarberg Formation, SW South Africa are de...
The Dawangou section, an auxiliary Global Stratoype Section and Point (GSSP) for the base of the Upp...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
Chitinozoans have a great potential for biostratigraphic correlation of Ordovician through to Devoni...
International audienceThe base of the Darriwilian Stage is defined by the first appearance datum (FA...
International audienceThe QUSAIBA-1 shallow core drilled in NW Saudi Arabia penetrated the Qalibah, ...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
AbstractBelonechitina capitata, a typically middle to late Ordovician chitinozoan index taxon was fo...
Belonechitina capitata, a typically middle to late Ordovician chitinozoan index taxon was for the fi...
The Shiala Formation of the Garhwal-Kumaon subbasin of the Tethyan Himalaya, has been sampled for ch...
International audienceDuring extensive investigations carried out recently on the chitinozoans from ...
Three new chitinozoan species, Conochitina savalaensis, Conochitina viruana and Belonechitina intons...
Chitinozoans from seven cores in the Middle Ordovician upper Goldwyer and Nita for-mations are docum...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
A chitinozoan faunule is reported from a shallow-marineLower Ordovician sequence in the subsurface o...
Isolated chitinozoans from the Scorn Shale Member of the Cedarberg Formation, SW South Africa are de...
The Dawangou section, an auxiliary Global Stratoype Section and Point (GSSP) for the base of the Upp...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
Chitinozoans have a great potential for biostratigraphic correlation of Ordovician through to Devoni...
International audienceThe base of the Darriwilian Stage is defined by the first appearance datum (FA...
International audienceThe QUSAIBA-1 shallow core drilled in NW Saudi Arabia penetrated the Qalibah, ...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...