“…‘Primary’ was used for lateral, and ‘secondary’ for medial cover plates in previous work on the Cambrian basal pentaradiate Stromatocystites (Paul and Smith, 1984). ‘Inner’ and ‘outer’ were used by Brower (2006) for two-tiered Late Ordovician crinoids. The term ‘lappets’ was applied to camerate crinoids with a single biserial tier (Kolata, 1982) and, in some cases, to extant crinoid cover plates (Clark and Clark, 1915).…”
Section: Methodsmentioning
confidence: 99%
“…Changes included: (1) extraxial lateral field size reduction or disappearance, (2) floor plates nestling into the adoral channel, but later not expressed as skeletal elements, and (3) medial cover plates consisting of a single biseries or entirely absent. (Brower, 2006, fig. 1), suggesting paedomophosis as a mechanism for the reduction of tier numbers in other taxa.…”
Section: Journal Of Paleontology 94(2):311-333mentioning
confidence: 99%
“…two-tiered Table 2. Characteristic arm types and cover plates among diverse Late Ordovician crinoids (primarily from Brower, 2006 andSprinkle, 1982a, b (Brower, 1966) disparid non-pinnulate, ramulose 1 Ectenocrinus simplex (Hall, 1847) disparid pinnulate 1 Peltacrinus sculptatus Warn, 1982 disparid non-pinnulate 2…”
Section: Independent Origins Of Crinoids and Blastozoans Among Early mentioning
confidence: 99%
“…sp., paratype PE 52753; ( 4 ) rhodocrinitid camerate Archaeocrinus snyderi Guensburg, 1984, unnumbered brachial on same slab with UI X-5738; ( 5, 6 ) disparid Doliocrinus pustulatus Warn, 1982, brachial outline from 1113TX51 and 1279TX177, showing transition from secondary groove to nearly fully enclosed foramen within brachial, cover plates added from Doliocrinus monilicaulis Guensburg, 1984, UI X-5716; ( 7 ) Columbicrinus crassus Ulrich, 1925, UI X-5711, brachial outline from Guensburg (1992); ( 8 ) hybocrinid cladid Hybocrinus bilateralis Guensburg, 1984, UI X-5867 and 5868, and ( 9 ) cladid Cupulocrinus crossmani Brower, 1992, SUI 62895A and 62895C, secondary groove based on unnumbered specimens of Cupulocrinus gracilis in Field Museum collections.…”
Intermediate morphologies of a new fossil crinoid shed light on the pathway by which crinoids acquired their distinctive arms. Apomorphies originating deep in echinoderm history among early nonblastozoan pentaradiate echinoderms distinguish Tremadocian (earliest Ordovician) crinoid arms from later taxa. The brachial series is separated from the ambulacra, part of the axial skeleton, by lateral plate fields. Cover plates are arrayed in two tiers, and floor plates expressed podial basins and pores. Later during the Early Ordovician, floor plates contacted and nestled into brachials, then were unexpressed as stereom elements entirely and cover plates were reduced to a single tier. Incorporation of these events into a parsimony analysis supports crinoid origin deep in echinoderm history separate from blastozoans (eocrinoids, ‘cystoids’). Arm morphology is exceptionally well-preserved in the late Tremadocian to early Floian Athenacrinus broweri new genus new species. Character analysis supports a hypothesis that this taxon originated early within in the disparid clade. Athenacrinus n. gen. (in Athenacrinidae new family) is the earliest-known crinoid to express what is commonly referred to as ‘compound’ or ‘biradial’ morphology. This terminology is misleading in that no evidence for implied fusion or fission of radials exists, rather it is suggested that this condition arose through disproportionate growth.UUID: http://zoobank.org/b383e039-3298-4472-a7e3-e81684f87cfe
“…‘Primary’ was used for lateral, and ‘secondary’ for medial cover plates in previous work on the Cambrian basal pentaradiate Stromatocystites (Paul and Smith, 1984). ‘Inner’ and ‘outer’ were used by Brower (2006) for two-tiered Late Ordovician crinoids. The term ‘lappets’ was applied to camerate crinoids with a single biserial tier (Kolata, 1982) and, in some cases, to extant crinoid cover plates (Clark and Clark, 1915).…”
Section: Methodsmentioning
confidence: 99%
“…Changes included: (1) extraxial lateral field size reduction or disappearance, (2) floor plates nestling into the adoral channel, but later not expressed as skeletal elements, and (3) medial cover plates consisting of a single biseries or entirely absent. (Brower, 2006, fig. 1), suggesting paedomophosis as a mechanism for the reduction of tier numbers in other taxa.…”
Section: Journal Of Paleontology 94(2):311-333mentioning
confidence: 99%
“…two-tiered Table 2. Characteristic arm types and cover plates among diverse Late Ordovician crinoids (primarily from Brower, 2006 andSprinkle, 1982a, b (Brower, 1966) disparid non-pinnulate, ramulose 1 Ectenocrinus simplex (Hall, 1847) disparid pinnulate 1 Peltacrinus sculptatus Warn, 1982 disparid non-pinnulate 2…”
Section: Independent Origins Of Crinoids and Blastozoans Among Early mentioning
confidence: 99%
“…sp., paratype PE 52753; ( 4 ) rhodocrinitid camerate Archaeocrinus snyderi Guensburg, 1984, unnumbered brachial on same slab with UI X-5738; ( 5, 6 ) disparid Doliocrinus pustulatus Warn, 1982, brachial outline from 1113TX51 and 1279TX177, showing transition from secondary groove to nearly fully enclosed foramen within brachial, cover plates added from Doliocrinus monilicaulis Guensburg, 1984, UI X-5716; ( 7 ) Columbicrinus crassus Ulrich, 1925, UI X-5711, brachial outline from Guensburg (1992); ( 8 ) hybocrinid cladid Hybocrinus bilateralis Guensburg, 1984, UI X-5867 and 5868, and ( 9 ) cladid Cupulocrinus crossmani Brower, 1992, SUI 62895A and 62895C, secondary groove based on unnumbered specimens of Cupulocrinus gracilis in Field Museum collections.…”
Intermediate morphologies of a new fossil crinoid shed light on the pathway by which crinoids acquired their distinctive arms. Apomorphies originating deep in echinoderm history among early nonblastozoan pentaradiate echinoderms distinguish Tremadocian (earliest Ordovician) crinoid arms from later taxa. The brachial series is separated from the ambulacra, part of the axial skeleton, by lateral plate fields. Cover plates are arrayed in two tiers, and floor plates expressed podial basins and pores. Later during the Early Ordovician, floor plates contacted and nestled into brachials, then were unexpressed as stereom elements entirely and cover plates were reduced to a single tier. Incorporation of these events into a parsimony analysis supports crinoid origin deep in echinoderm history separate from blastozoans (eocrinoids, ‘cystoids’). Arm morphology is exceptionally well-preserved in the late Tremadocian to early Floian Athenacrinus broweri new genus new species. Character analysis supports a hypothesis that this taxon originated early within in the disparid clade. Athenacrinus n. gen. (in Athenacrinidae new family) is the earliest-known crinoid to express what is commonly referred to as ‘compound’ or ‘biradial’ morphology. This terminology is misleading in that no evidence for implied fusion or fission of radials exists, rather it is suggested that this condition arose through disproportionate growth.UUID: http://zoobank.org/b383e039-3298-4472-a7e3-e81684f87cfe
“…Although there is not a direct correlation of calyx or crown size to column height, it is reasonable to assume that a crinoid with a one or more order of magnitude smaller body would simply be a smaller crinoid with a shorter column, thus closer to the sea floor in lower tiers (Ausich 1980;Ausich and Bottjer 1982;Bottjer and Ausich 1987). Brower (2006) demonstrated that calyx size is positively correlated to the length of the ambulacral tracts, thus the area of the filtration fan would also be smaller. Thus, a smaller crinoid would presumably have lower fecundity and a diminished feeding capacity relative to its larger ancestor.…”
Coincident with the end-Ordovician (end-Katian for crinoids) biodiversity crash, crinoids from Anticosti Island, Quebec, experienced a statistically significant reduction in body size, an evolutionary trend termed the ''Lilliput Effect''. This decrease in body size occurred for the fauna as a whole, and data indicate that neither dominant Ordovician nor dominant Silurian clades experienced preferential size decrease. Because the post-extinction fauna with a diminished size is composed of largely new taxa, this example of the Lilliput Effect is regarded as the miniaturization mode. The miniaturization occurred very rapidly; however, the recovery on Anticosti Island did not occur for as many as 7 Ma. This macroevolutionary asymmetry, as demonstrated in many other studies, highlights the need to preserve the biodiversity present on Earth today.
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