The Wollaston Medal is a scientific award for geology, the highest award granted by the Geological Society of London.
Ceraurinella is an extinct genus of trilobite in the family Cheiruridae. There are about 19 described species in Ceraurinella.
Inoceramus is an extinct genus of fossil marine pteriomorphian bivalves that superficially resembled the related winged pearly oysters of the extant genus Pteria. They lived from the Early Jurassic to latest Cretaceous.
Ronald Pearson Tripp FRSE was a British palaeontologist specializing in trilobites. He was self-taught in palaeontology and became an authority on the taxonomy of the trilobite order Lichida and the trilobite family Encrinuridae.
Eulimidae is a family of very small parasitic sea snails, marine gastropod mollusks in the superfamily Vanikoroidea.
Deacybele is a genus of trilobites in the order Phacopida, that existed during the upper Ordovician in what is now Ireland. It was described by Whittington in 1965, and the type species is Deacybele arenosa, which was originally described under the genus Calymene by McCoy in 1846. The type locality was the Avoca Formation.
Heliomeroides is a trilobite in the order Phacopida, that existed during the upper Ordovician in what is now the United States. It was described by Evitt in 1951, and the type species is Heliomeroides teres. The type locality was the Lincolnshire Formation in Virginia.
Struszia is a genus of fossil trilobites from the Silurian period, erected in 1993 and named after paleontologist Desmond L. Strusz.
The Florida Open is the Florida state open golf tournament, open to both amateur and professional golfers. It is now organized by the Florida State Golf Association (FSGA). It has been played annually since 1942 at a variety of courses around the state. There were earlier "Florida Open"s played in the 1920s and 1930s, not associated with the current version, that are considered official PGA Tour events.
Raphiophoridae is a family of small to average-sized trilobites that first occurred at the start of the Ordovician and became extinct at the end of the Middle Silurian.
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