Seventy-five samples from the classic sections through the historical type area of the Ashgill Series in the Cautley district and along Pus Gill in the Cross Fell Inlier have been examined for chitinozoans. The results of this study allowed the recognition of five internationally recognized biozones and the definition of two new Avalonian chitinozoan zones. From bottom upwards, these are: the Fungochitina spinifera, the Tanuchitina bergstroemi?, the Conochitina rugata, the Spinachitina fossensis, the Bursachitina umbilicata sp. n., the Ancyrochitina merga and the Belonechitina postrobusta zones. One new species is described: Bursachitina umbilicata sp. n. This biozonation enables a correlation between the Cautley district and the Baltoscand...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The Dob's Linn section has recently been confirmed as the Global Stratotype Section and Point (GSSP)...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The Dob's Linn section has recently been confirmed as the Global Stratotype Section and Point (GSSP)...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
The Arenig Fawr area of North Wales constitutes the type area for the British Lower to Middle Ordovi...
Acritarchs and chitinozoa are wed to date Ordovicinn rocks in England and Wales, but the data-base f...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
Seventy-five samples from the classic sections through the historical type area of the Ashgill Serie...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The Dob's Linn section has recently been confirmed as the Global Stratotype Section and Point (GSSP)...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The Dob's Linn section has recently been confirmed as the Global Stratotype Section and Point (GSSP)...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
To help calibrate the emerging Upper Ordovician chitinozoan biozonation with the graptolite biozonat...
The last decade saw a revival of the debate on the exact stratigraphical position of the Upper Ordov...
The Arenig Fawr area of North Wales constitutes the type area for the British Lower to Middle Ordovi...
Acritarchs and chitinozoa are wed to date Ordovicinn rocks in England and Wales, but the data-base f...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...
The Global Stratotype Section and Point (GSSP) for the Lower Ordovician Floian Stage is defined by t...
New chitinozoan data are presented from the classical section along the Onny River in the type Carad...