This thesis presents new graptoloid biostratigraphic range charts for the Ordovician and Silurian of Britain. The Ordovician graptoloid succession is represented by two separate biostratigraphic frameworks; one for England and Wales, another for Scotland, due to significant stratigraphic disparity between the graptoloid faunal assemblages of the two regions. The British Silurian sequence is represented by a single graptoloid biostratigraphic scheme reflecting more uniform graptoloid assemblages.;The reliability of the taxonomic foundation upon which the range charts are based is tested using the dominant Ludlow Series (Silurian) graptoloid subfamily Saetograptinae Urbanek. The results suggest that intraspecific variation has led to over...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
Siurian graptolite zones are of markedly shorter duration than those of the Ordovician, averaging 0....
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
697 taxa of planktonic graptolites are recorded, and their stratigraphical ranges are given, through...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
with that of the Siurian and is in need of relhement, especially by detailed collecting from suitabl...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
Continuously fossiliferous sections in south Wales and Shropshire spanning the base of the Upper Ord...
Continuously fossiliferous sections in south Wales and Shropshire spanning the base of the Upper Ord...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
Siurian graptolite zones are of markedly shorter duration than those of the Ordovician, averaging 0....
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
697 taxa of planktonic graptolites are recorded, and their stratigraphical ranges are given, through...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
with that of the Siurian and is in need of relhement, especially by detailed collecting from suitabl...
Graptolites, extinct macrozooplankton of the phylum Hemichordata were a major element of the Early P...
Continuously fossiliferous sections in south Wales and Shropshire spanning the base of the Upper Ord...
Continuously fossiliferous sections in south Wales and Shropshire spanning the base of the Upper Ord...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
The global standard for the Llandovery Series (early Silurian) in centralWales is re-assessed in the...
Siurian graptolite zones are of markedly shorter duration than those of the Ordovician, averaging 0....