TL;DR: A true interreef crinoid fauna lacking components of reefal facies is reported from the Ludlovian of the Mississinewa Shale Member of the Wabash Formation in northern Indiana.
Abstract: A true interreef crinoid fauna lacking components of reefal facies is reported from the Ludlovian of the Mississinewa Shale Member of the Wabash Formation in northern Indiana. The Mississinewa facies that contains this fauna is a dolomitic siltstone or a silty dolomite. The crinoid association reported is composed entirely of new species and is different from other reef and reef-associated, interreef, and non-reef crinoid associations. New species described, herein, include the following: Dimerocrinites (Eucrinus) ankylos n. sp., Periechocrinus shaveri n. sp., Bohemicocrinus? occidens n. sp., Macrostylocrinus styo n. sp., M. homalos n. sp., Gissocrinus hypselos n. sp., and Dendrocrinus diaphoros n. sp. This may be the first occurrence of Bohemicocrinus from outside Bohemia.
TL;DR: In this paper, two new species, Dimerocrinites aragonensis n.sp. and D. sartensisn.sp., are described, and the vertical distribution of the Devonian species established in the Armorican sections shows that D. lanveocensis, which originates close to the Silurian/Devonian boundary, may be used for the characterization of the Lower Lochkovian in the Ibero-Armorican domain.
Abstract: The data set accumulated during the last decade on dimerocrinitid crinoids from the northern margin of Gondwana ranging from Wenlockian lo Pragian has been worked out. Two new species, Dimerocrinites aragonensis n.sp. and D. sartensis n.sp., are described. The following evolutionary trends of the theta are evidenced: significant increase of dorsal cup size and piale thickness, smoothening and loss of plate ornamentation, columnal articular development, and related epifacet reduction. The vertical distribution of the Devonian species established in the Armorican sections shows that D. lanveocensis, which originates close to the Silurian/Devonian boundary, may be used for the characterization of the Lower Lochkovian in the Ibero-Armorican domain. The wide geographical distribution of the dimerocrinitids from South Algeria to the Armorican massif in addition to the robustness of their morphological features, clearly distinct from those of the South Laurussian species, make them paleobiogeographical indicators for the North Gondwanan province. The abundance of dissociated plates and columnals in Lower Lochkovian fine to coarse terrigenous sediments are indicative of proximal paleoenvironments in contrast with the distal open shelf scyphocrinitid biofacies.
TL;DR: The first monographic study devoted to the British Silurian crinoids was by John Phillips as discussed by the authors who described 14 species (eleven new), all from the Wenlock Series of the area around Dudley.
Abstract: SUMMARY John Samuel Miller’s A Natural History of the Crinoidea or Lily-Shaped Animals … (1821), the first monograph of the fossil crinoids, included only three species from what we would now call the British Silurian. The first monographic study devoted to the British Silurian crinoids was by John Phillips ( in Murchison’s The Silurian System , 1839), who described 14 species (eleven new), all from the Wenlock Series of the area around Dudley. These were conservatively placed in five genera, Cyathocrinites Miller, Marsupiocrinites Phillips, Hypanthocrinites Phillips, Actinocrinites Miller and Dimerocrinites Phillips; the same species are now divided between eleven genera. Eight of these taxa are type species, but none is now classified as either Cyathocrinites or Actinocrinites. Hypanthocrinites is a junior synonym of Eucalyptocrinites Goldfuss. The illustrations in Phillips, drawn by J. de C. Sowerby, were much superior to Miller’s plates, but lacked his innovative ‘exploded’ diagrams.