Nicoll et al. (1999, Brigham Young University Geology Studies 44, 27-101) published the taxonomy of species of the ramiform conodont Iapetognathus Landing in Fortey et al. (1982, The Cambrian-Ordovician boundary: sections, fossil distributions, and correlations, National Museum of Wales, Geological Series No. 3, Cardiff, 95-129) and its ancestor Iapetonudus Nicoll et al., 1999. Cooper et al. (2001, Episodes 24, 19-28) used the First Appearance Datum of Iapetognathus fluctivagus Nicoll et al., 1999 to mark the base of the Ordovician System at Green Point, Newfoundland. Terfelt et al. (2012, Lethaia 45, 227-237) re-evaluated Iapetognathus at Green Point and made several taxonomic and stratigraphic conclusions, nearly all of which we refute he...
The conodont fauna of the reference succession of the British regional Llandeilian Stage of the Llan...
Although Katian conodont faunas from high-latitude Gondwanan to peri-Gondwanan regions are widely re...
Olistostromes with calcareous olistoliths are rare components in the Ordovician successions inNWEur...
In 2000, the International Union of Geological Sciences (IUGS) ratified the decision from the Intern...
The GSSP (Global Boundary Stratotype Section and Point) of the Cambrian-Ordovician boundary was form...
Ordovician System and base of the lowest Ordovician stage (Tremadocian) is exposed in the coastal pl...
Middle and upper Katian conodonts were previously known in the British Isles from relatively small c...
Middle and Upper Katian conodonts are previously known in the British Isles from relatively small co...
Abstract: Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western...
Thirty species (representing 19 genera) of Early Ordovician conodonts are described and iIlustrated ...
Lower Ordovician conodonts are reported from continental slope deposits of yhe Cow Head Group from s...
Contribución al IGCP 653Although Katian conodont faunas from high-latitude Gondwanan to peri-Gondwan...
This paper presents taxonomical description of latest Tremadocian to Middle Arenigian conodonts reco...
Conodonts from fine clastics of the Road River Formation in the Richardson Mountains range from Midd...
The strata exposed along Lord Lindsay River on southern Boothia Peninsula were previously named the ...
The conodont fauna of the reference succession of the British regional Llandeilian Stage of the Llan...
Although Katian conodont faunas from high-latitude Gondwanan to peri-Gondwanan regions are widely re...
Olistostromes with calcareous olistoliths are rare components in the Ordovician successions inNWEur...
In 2000, the International Union of Geological Sciences (IUGS) ratified the decision from the Intern...
The GSSP (Global Boundary Stratotype Section and Point) of the Cambrian-Ordovician boundary was form...
Ordovician System and base of the lowest Ordovician stage (Tremadocian) is exposed in the coastal pl...
Middle and upper Katian conodonts were previously known in the British Isles from relatively small c...
Middle and Upper Katian conodonts are previously known in the British Isles from relatively small co...
Abstract: Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western...
Thirty species (representing 19 genera) of Early Ordovician conodonts are described and iIlustrated ...
Lower Ordovician conodonts are reported from continental slope deposits of yhe Cow Head Group from s...
Contribución al IGCP 653Although Katian conodont faunas from high-latitude Gondwanan to peri-Gondwan...
This paper presents taxonomical description of latest Tremadocian to Middle Arenigian conodonts reco...
Conodonts from fine clastics of the Road River Formation in the Richardson Mountains range from Midd...
The strata exposed along Lord Lindsay River on southern Boothia Peninsula were previously named the ...
The conodont fauna of the reference succession of the British regional Llandeilian Stage of the Llan...
Although Katian conodont faunas from high-latitude Gondwanan to peri-Gondwanan regions are widely re...
Olistostromes with calcareous olistoliths are rare components in the Ordovician successions inNWEur...