A diverse Upper Ordovician (Eastonian) graptoloid fauna of some 20 taxa has been obtained from ‘black shales’ of\ud the uppermost Foxlow Beds near Ryrie Hill south of Michelago. Eighteen of these are figured and described. The\ud age indication is Eastonian 2 and 3, possibly about the caudatus/morrisi Biozone boundary in global graptolite\ud terms. Some specimens exhibit a peculiar preservation, possibly of associated soft parts, though not necessarily\ud graptolite soft parts
Graptolites and conodonts are frequent fossils in Sandbian (Late Ordovician) outcrops of the Argenti...
The Shelve Rlller exposes a sequence of beds from Arenig to Caradoc with a mixed fauna of brachiopod...
Eleven graptolite zones are recognized in New Zealand and are considered to represent most of the Or...
Darriwilian (Ordovician) graptolite faunas and provincialism in the Töyen Shale of th
Graptolite fossils provide a means for separating Late Ordovician autochthonous Martinsburg foreland...
Paleontological collections, including many new graptolite discoveries from northern New Jersey, eas...
an age of latest Arenig (upper D. hirundo biozone). Comparison with graptolites of the same age from...
Ashgill age graptolites have been collected from seven sections of the Cape Phillips Formation acros...
Early Ordovician (late Arenig) graptolites are identified from strata near the Northwest Gander Rive...
Graptolites are one of the significant groups of stratigraphic index fossils in the Early Palaeozoic...
Two new graptolite assemblages are identified from discrete intervals within the Phu Ngu Formation, ...
An Ordovician–Silurian boundary section marked by an uninterrupted, relatively high rate of black sh...
Cj T h e Cow H e a d G r o u p is an al lochthonous sequence of Middle Cambr ian to late Arenig sedi...
Marine shales directly overlying lower Hirnantian (uppermost Ordovician) glacially related sediments...
Graptolites occur very sparingly in the Upper Ordovician strata of the Cincinnati region. Among the ...
Graptolites and conodonts are frequent fossils in Sandbian (Late Ordovician) outcrops of the Argenti...
The Shelve Rlller exposes a sequence of beds from Arenig to Caradoc with a mixed fauna of brachiopod...
Eleven graptolite zones are recognized in New Zealand and are considered to represent most of the Or...
Darriwilian (Ordovician) graptolite faunas and provincialism in the Töyen Shale of th
Graptolite fossils provide a means for separating Late Ordovician autochthonous Martinsburg foreland...
Paleontological collections, including many new graptolite discoveries from northern New Jersey, eas...
an age of latest Arenig (upper D. hirundo biozone). Comparison with graptolites of the same age from...
Ashgill age graptolites have been collected from seven sections of the Cape Phillips Formation acros...
Early Ordovician (late Arenig) graptolites are identified from strata near the Northwest Gander Rive...
Graptolites are one of the significant groups of stratigraphic index fossils in the Early Palaeozoic...
Two new graptolite assemblages are identified from discrete intervals within the Phu Ngu Formation, ...
An Ordovician–Silurian boundary section marked by an uninterrupted, relatively high rate of black sh...
Cj T h e Cow H e a d G r o u p is an al lochthonous sequence of Middle Cambr ian to late Arenig sedi...
Marine shales directly overlying lower Hirnantian (uppermost Ordovician) glacially related sediments...
Graptolites occur very sparingly in the Upper Ordovician strata of the Cincinnati region. Among the ...
Graptolites and conodonts are frequent fossils in Sandbian (Late Ordovician) outcrops of the Argenti...
The Shelve Rlller exposes a sequence of beds from Arenig to Caradoc with a mixed fauna of brachiopod...
Eleven graptolite zones are recognized in New Zealand and are considered to represent most of the Or...