ORDER REDLICHIIDAIntroduction: Primitive trilobites with numerous thoracic segments with spinose tips.
last revised 30 September 2010 by S. M. Gon III
Cephalon: large and typically semicircular; glabella typically long, well-segmented, parallel, tapering, or expanding forwards; genal spines typically present, strong, usually continued from a narrow, tubular cephalic border; eyes typically large, crescentic, with large, inflated palpebral lobe ridges running toward front of glabella (anterior of S3); eye ridge may be subdivided; hypostome natant or conterminant, usually very wide rostral plate present.
Thorax: with numerous segments (up to 90+), pleurae usually with spinose tips; may be subdivided into prothorax and opisthothorax.
Pygidium: typically tiny (micropygous), one or very few segments.
Occurrence: L. Cambrian to M. Cambrian.
Suborders: Olenellina and Redlichiina.
Cephalon: lacking facial sutures; glabella typically
with rather deep lateral furrows; in some species the front
glabellar lobe is an almost circular boss; natant or
conterminant hypostome, very wide rostral
plate extending between genal angles, with perrostral suture (no
Holmiidae: Andalusiana, Baltobergstroemia, Callavia (=Cephalacanthus/Callavalonia; =Cobboldus), Cambropallas, Elliptocephala (/Georgiellus, /Ebenezeria), Holmia (=Esmeraldina), Holmiella, Iyouella, Kjerulfia, Palmettaspis, Postfallotaspis, Schmidtiellus (/Schmidtia).
Fallotaspididae: Choubertella, Daguinaspis (=Eodaguinaspis; =Epidaguinaspis), Eofallotaspis, Fallotaspis, Lenallina, Parafallotaspis, Pelmanaspis, Wolynaspis.
Judomiidae: Judomia, Judomiella, Paranevadella, Sinskia.
Neltneriidae: Bondonella, Neltneria.
Nevadiidae: Buenellus, Cambroinyoella, Cirquella, Limniphacos, Nevadella, Nevadia, Plesionevadia, Pseudojudomia, Sdzuyomia.
Cephalon: with opisthoparian facial sutures; early forms
tend to have tapering, conical glabella with furrows extending
far backwards; later forms with glabella expanding forwards to
inflated frontal lobe; hypostome conterminant (e.g.,
Redlichia) or natant (e.g., Dolerolenus), rostral
plate narrower than in Olenellina, bound by rostral and
Chengkouaspidae: Aragotus, Bathynotus (=Pagura), Bathynotellus, Belliceps, Chengkouaspis, Elegestina, Inella, Pseudoresserops, Terechtaspis (=Nellina).
Dolerolenidae: Dolerolenus (/Olenopsis; =Malungia), Giordanella, Granolenus, Paramalungia.
Gigantopygidae: Bornemannaspis, Gigantopygus, Parayiliangella, Pseudoyiliangella, Yilliangella (=Palaeoaspis), Yilliangellina, Zhangshania.
Kueichowiidae: Kueichowia, Shatania.
Mayiellidae: Mayiella, Qiaodiella, Qiaotingaspis
Metadoxididae: Churkinia, Conomicmacca, Enantiaspis, Fuminaspis, Hongshiyanaspis, Metadoxides (=Anadoxides), Minusinella, Onaraspis, Pratungusella.
Redlichiidae: Breviredlichia, Chaoaspis, Chengjiangaspis, Conoredlichia, Elganellus, Eoredlichia (=Archaeops; = Saukiandops; =Galloredlichia; = Pararedlichia), Hesa, Iglesiella, Irgitkhemia, Jingyangia, Kepingaspis, Kuanyangia, Latiredlichia, Lemdadella, Leptoredlichia (=Paraleptoredlichia), Maopingaspis, Metaredlichia, Mianxianella, Nebidella, Neoredlichia, Ningqiangaspis, Olgaspis, Pachyredlichia, Parawutingaspis, Parazhenbaspis, Pseudoredlichia, Pseudowutingaspis, Pteroredlichia (=Spinoredlichia), Redlichia (/Hoeferia; =Mesodema; =Dongshania), Redlichops, Sapushania, Sarassina, Sardaspis, Sardoredlichia, Syndianella, Tolbinella, Ushbaspis (=Metaredlichioides), Wengangaspis, Wutingaspis, Xela, Xenoredlichia, Yorkella, Zhanglouia.
Redlichinidae: Asthenaspis, Kolbaspis, Parasajanaspis, Redlichina, Sajanaspis, Sekwiaspis, Tungusella.
Saukiandidae: Australaspis, Clariondia, Despujolsia, Dolerolichia, Eops, Ezhimia, Longianda, Pareops, Perrector (=Rawops), Planocephalus, Pseudosaukianda, Realaspis, Resserops, Richterops (=Marsaisia), Saukianda.
Yinitidae: Drepanopyge, Drepanuroides (=Xishuiella), Hongjunshaoia, Longduia, Meitanella, Paokannia, Parapaokannia, Parayinites, Pseudopaokannia, Qingkouia (=Paradrepanuroides), Yinites, Yunnanaspidella, Yunnanaspis.
Akbashichia, Fandianaspis, Iolgia, Micangshania, Xingzishania.
Centropleuridae: Anopolenus, Beishanella, Centropleura, Clarella, Luhops.
Xystriduridae: Galahetes, Inosacotes, Polydinotes, Xystridura (/Milesia).
|ADDITIONAL CLASSIFICATION NOTES FOR
As one of the most primitive order of trilobites (along with Ptychopariida), the two suborders, Redlichiina and Olenellina, each pose some taxonomic problems. The Redlichiina may be considered the most basal group of non-olenellid trilobites, alongside the ellipsocephaloid Ptychopariida. Much of the historical taxonomy of Redlichiida has been developed stratigraphically. Both ptychopariid and corynexochid trilobites have sister taxa that could currently be classified as Redlichiida, making the order paraphyletic. For example, the Ellipsocephaloidea, once considered part of the Redlichiida, is now considered a primitive "bridge" between the Redlichiida and Ptychopariida. As sister taxa for other orders are defined in the Redlichiina, an evolutionarily meaningful classification may emerge.
Geyer (1996) in his review of Moroccan fallotaspidids questioned the importance of lack of facial sutures uniting the Fallotaspidoidea with Olenelloidea in the suborder Olenellina, pointing out that Fallotaspis and Lemdadella are difficult to distinguish if facial sutures are disregarded, and that although olenelloids follow fallotaspidoids stratigraphically, there is no clear transition between any fallotaspidoids and olenelloids, whereas holmiid olenelloids resemble redlichioids such as Gigantopygus. Geyer suggested that at least some olenelloids may have arrived at their lack of facial sutures secondarily from redlichioids.
Jell (2003) examines the earliest lineages of trilobites and has some controversial proposals. He notes that the earliest trilobites were probably natant (vs Fortey's assertion that an attached hypostome is the primitive state). This means that some lineages went from natant to attached, and others may have remained natant (leading to the Librostoma). Another assertion is that facial sutures may have arisen from fallotaspidoids more than once, and that one lineage (from Profallotaspis to Archaeaspis to Judomiidae and Holmiidae to Olenellidae) retained the primitively sutureless condition to give rise to the Olenelloidea. If Jell's lineages are valid, then both suborder Redlichiina and order Ptychopariida are polyphyletic! Indeed, recent research on the oldest trilobites in the fossil record indicate that in portions of Gondwanaland (now parts of Spain and Morocco), the first trilobites are ellipsocephaloids. This further points to the very close relationship between the Ellipsocephaloidea and Redlichiida.
With a primitive lack of facial sutures, and a
stratigraphically early range, the Olenellida have been
recognized as distinct sister
taxon to "typical" trilobites, and arguments have been made to
them from the Trilobita. Fortey (1990) argued effectively for
the Olenellina as trilobites, but the relationship between
the Olenellina and Redlichiina and other suture-bearing
trilobites is by no means clear. They seem united
by shared primitive characters (e.g., micropygy, numerous
segments with spinose tips, long, cresentic eyes, etc.). Without
clarified relationship, the Order Redlichiida as now defined
both Redlichiina and Olenellina, and excluding
Ellisocephaloidea) may not be justified. Jell (2003) suggests
that Eofallotaspis gives rise to Lemdadella, and
to Eoredlichia and the Redlichiidae.
The ontogeny of olenelloids shows an interesting detachment of
the hypostome from the rostral plate in mid-ontogeny, with a
redocking of the hypostome by maturity. This may be relevant to
evolution of the natant orders (Ptychopariida, etc.), but is
consistent with Jell's (2003) suggestion that the natant state
The family Bathynotidae was included in the order Redlichiida in the 1959 Treatise, but is listed as "order uncertain" in the 1997 Treatise. Its dorsal features are easily placed in the Redlichioidea, but its ventral features (particularly rostral plate lacking/greatly reduced) defy the typical pattern. Jell & Adrain (2003) nonetheless place Bathynotus in the redlichioid family Chengkouaspidae, with which it shares many dorsal characters. More recently, in 2013 Elicki and Geyer placed new species of the redlichioid genus Myopsolenites in the family Bathynotidae. They argued that Myopsolenites and the entire Onaraspis clade belongs in the Bathynotidae. This would suggest that the family would not merit a subordinal placement, but instead sit among the primitive redlichioid families discussed above, closest, perhaps, to the Metadoxididae. The placement of fallotaspidoid genera in the families Archaeaspididae and Fallotaspididae in Jell & Adrain is not universally accepted, with arguments for placement of Profallotaspis and Repinaella in Archaeaspididae by Geyer (1996) and Hollingsworth (2008). Fritzaspis Hollingsworth, is placed in Archaeaspididae.
Paterson & Edgecombe removed Holyoakia from the Emuellidae (and in fact, removed it from Order Redlichiida, arguing that it is a member of Dorypygidae, Order Corynexochida). Paterson & Jago 2006 described Megapharanaspis, a new genus of emuelloid.
Elicki, O. & G. Geyer. 2013. The Cambrian trilobites of Jordan--taxonomy, systematic and stratigraphic significance. Acta Geol. Polonica 63(1):1-56.
Fortey, R. A. Trilobite systematics: the last 75 years. J. of Paleontology. 75(6):1141-51.
Fortey, R. A. 1990. Ontogeny, hypostome attachment, and trilobite classification. J. of Paleontology. 33:529-76.
Geyer, G. 1996. The Moroccan fallotaspidid trilobites revisited. Beringeria 18:89-199.
Hollingsworth, J.S., 2008. The first trilobites in Laurentia and elsewhere. In: I.Rábano, R. Gozalo and D. García-Bellido (Eds.), Advances in trilobite research. Cuadernos del Museo Geominero, nº 9. Instituto Geológico y
Jell, P.A. & J.M. Adrain. 2003 Available generic names for trilobites. Memoirs of the Queensland Museum 48(2):331-553
Paterson, J.R. & G.D., Edgecombe. 2006. The Early Cambrian trilobite family Emuellidae Pocock, 1970: Systematic position and
revision of Australian species. Journal of Paleontology 80(3): 496-513.
Paterson, J.R. & J.B. Jago. 2006. New trilobites from the Lower Cambrian Emu Bay Shale Lagerstätte at Big Gully, Kangaroo Island,
South Australia. Memoirs of the Association of Australasian Palaeontologists 32:43-57.
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