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GeoRef Categories
Era and Period
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Echidnina
Figure 3 —A distance of 6 mm on these photographs is equivalent to the len...
EARLIEST ORDOVICIAN (EARLY TO MIDDLE TREMADOCIAN) RADIOLARIAN FAUNAS OF THE COW HEAD GROUP, WESTERN NEWFOUNDLAND
Figure 4 —A distance of 6 mm on these photographs is equivalent to the len...
LATE CAMBRIAN RADIOLARIAN FAUNAS AND BIOSTRATIGRAPHY OF THE COW HEAD GROUP, WESTERN NEWFOUNDLAND
Middle Ordovician (middle Darriwilian) Archaeospicularia and Entactinaria (radiolarians) from the Table Cove Formation, Piccadilly Quarry, Newfoundland, Canada
Figure 5 —A distance of 6 mm on these photographs is equivalent to a lengt...
Figure 11. Scale bar equals 50 µm. 1, 2, Antygopora ordovicica Maletz and...
Earliest Arenig Radiolarians from the Cow Head Group, Western Newfoundland
Scanning electron micrographs of radiolarians extracted from limestones fro...
Figure 12 —A distance of 6 mm on these photographs is equivalent to a leng...
Figure 9 —A distance of 6 mm on these photographs is equivalent to the len...
Figure 7 —A distance of 6 mm on these photographs is equivalent to a lengt...
List of archaeospicularians, entactinarians, and other radiolarians of unce...
The Beothuka terranova (Radiolaria) assemblage and its importance for the understanding of early Ordovician radiolarian evolution
Palaeogeographical distribution of Ordovician Radiolarian occurrences: patterns, significance and limitations
Abstract Over the past 15 years, significant progress has been achieved in our understanding of Lower Palaeozoic radiolarian faunas. However, description of biogeographical patterns of Ordovician Radiolaria is hampered by the paucity of known occurrences as well as possible taphonomic influences. The distribution of all known assemblages is analysed in time and space. Lower Ordovician (especially Tremadocian) Radiolaria are known from two distinct tropical localities of Laurentia. Geographical coverage is much better for the Middle Ordovician (Darriwilian). However, data are concentrated in tropical palaeolatitudes (between 30°N and 30°S). The absence of data from mid/high-latitude localities limits any biogeographical insights. In addition to this there are taphonomic and taxonomic biases. Data are also sparse for the Upper Ordovician. However, comparison between Australian and Nevadan material of Katian age shows strong similarities, suggesting the presence of a coherent tropical radiolarian bioprovince, as in the modern ocean.