(Chelicerata: Eurypterida), a Large Sweep-Feeder from the Carboniferous of South Africa C
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Segmentation and Tagmosis in Chelicerata
Arthropod Structure & Development 46 (2017) 395e418 Contents lists available at ScienceDirect Arthropod Structure & Development journal homepage: www.elsevier.com/locate/asd Segmentation and tagmosis in Chelicerata * Jason A. Dunlop a, , James C. Lamsdell b a Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstrasse 43, D-10115 Berlin, Germany b American Museum of Natural History, Division of Paleontology, Central Park West at 79th St, New York, NY 10024, USA article info abstract Article history: Patterns of segmentation and tagmosis are reviewed for Chelicerata. Depending on the outgroup, che- Received 4 April 2016 licerate origins are either among taxa with an anterior tagma of six somites, or taxa in which the ap- Accepted 18 May 2016 pendages of somite I became increasingly raptorial. All Chelicerata have appendage I as a chelate or Available online 21 June 2016 clasp-knife chelicera. The basic trend has obviously been to consolidate food-gathering and walking limbs as a prosoma and respiratory appendages on the opisthosoma. However, the boundary of the Keywords: prosoma is debatable in that some taxa have functionally incorporated somite VII and/or its appendages Arthropoda into the prosoma. Euchelicerata can be defined on having plate-like opisthosomal appendages, further Chelicerata fi Tagmosis modi ed within Arachnida. Total somite counts for Chelicerata range from a maximum of nineteen in Prosoma groups like Scorpiones and the extinct Eurypterida down to seven in modern Pycnogonida. Mites may Opisthosoma also show reduced somite counts, but reconstructing segmentation in these animals remains chal- lenging. Several innovations relating to tagmosis or the appendages borne on particular somites are summarised here as putative apomorphies of individual higher taxa. -
Geological History and Phylogeny of Chelicerata
Arthropod Structure & Development 39 (2010) 124–142 Contents lists available at ScienceDirect Arthropod Structure & Development journal homepage: www.elsevier.com/locate/asd Review Article Geological history and phylogeny of Chelicerata Jason A. Dunlop* Museum fu¨r Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Invalidenstraße 43, D-10115 Berlin, Germany article info abstract Article history: Chelicerata probably appeared during the Cambrian period. Their precise origins remain unclear, but may Received 1 December 2009 lie among the so-called great appendage arthropods. By the late Cambrian there is evidence for both Accepted 13 January 2010 Pycnogonida and Euchelicerata. Relationships between the principal euchelicerate lineages are unre- solved, but Xiphosura, Eurypterida and Chasmataspidida (the last two extinct), are all known as body Keywords: fossils from the Ordovician. The fourth group, Arachnida, was found monophyletic in most recent studies. Arachnida Arachnids are known unequivocally from the Silurian (a putative Ordovician mite remains controversial), Fossil record and the balance of evidence favours a common, terrestrial ancestor. Recent work recognises four prin- Phylogeny Evolutionary tree cipal arachnid clades: Stethostomata, Haplocnemata, Acaromorpha and Pantetrapulmonata, of which the pantetrapulmonates (spiders and their relatives) are probably the most robust grouping. Stethostomata includes Scorpiones (Silurian–Recent) and Opiliones (Devonian–Recent), while -
Bulletin of the Peabody Museum of Natural History Yale Univ
Hallipterus excelsior, a Stylonurid (Chelicerata: Eurypterida) from the Late Devonian Catskill Delta Complex, and Its Phylogenetic Position in the Hardieopteridae O. Erik Tetlie Department of Geology and Geophysics, Yale University, P. O. Box 208109, New Haven CT 06520-8109 USA — email: [email protected] Abstract The priority of the names Stylonurus excelsior and S. lacoanus from the Late Devonian of the east- ern United States has been disputed since they were first recognized as synonyms. The genus Hal- lipterus was later erected for the two known specimens, and they were again separated into distinct species, based on six listed differences, seemingly resolving the priority dispute. However, four of the differences are not present or can be interpreted as ontogenetically or taphonomically induced, and the remaining two are putatively interpreted as sexually dimorphic based on com- parisons with Tarsopterella, a closely related taxon. The two species are therefore synonymized again and the species epithet excelsior is considered to have priority. Advocates of both names also provided different reconstructions, mainly based on other stylonurids. Hallipterus is placed in the Hardieopteridae based on putative synapomorphies with Hardieopterus and particularly Tarsop- terella, the latter also clearly a hardieopterid, and the phylogenetic position of the Hardieopteri- dae is discussed. Although only the original two specimens of H. excelsior are known today, as a century ago, a new reconstruction is provided, supported by phylogenetic evidence, to replace the two earlier versions. Keywords Carapace, Catskill delta, chelicerates, eurypterid, ICZN, North America, synonymy. Introduction Some of the stylonurids (forms without swim- ming legs) were also very large, especially those Eurypterids, commonly referred to as sea scorpi- of Devonian to Permian age, when they chiefly ons, are chelicerate arthropods that lived in mar- occur in deposits of fluvial and lacustrine origin. -
Its Position Within the Adelophthalmidae Tollerton, 1989 by O
bulletin de l'institut royal des sciences naturelles de belgique sciences de la terre, 76: 79-90, 2006 bulletin van het koninklijk belgisch instituut voor natuurwetenschappen aardwetenschappen, 76: 79-90, 2006 A reappraisal of Eurypterus dumonti Stainier, 1917 and its position within the Adelophthalmidae Tollerton, 1989 by O. Erik TETLIE & Peter VAN ROY Tetlie, O.E. & Van Roy, P., 2006 — A reappraisal of Eurypterus prétées ici comme des "dumb-hells" (cfr. Briggs & Wilby 1996), dumonti Stainier, 1917 and its position within the Adelophthalmidae résultant d'action bactérielle avant la fossilisation. Ces structures in¬ Tollerton, 1989. Bulletin de l'Institut royal des Sciences naturelles diquent que le fossile n'est pas une exuvie. L'interprétation d'un de Belgique, Sciences de la Terre 76: 79-90, 6 figs., Brussels, April 15, nombre d'autres caractéristiques diffère aussi de celle de la description 2006-ISSN 0374-6291. originale. Des lignes de descendance possible du clade Adelophthalmus sont identifiées, et la proximité (l'A. dumonti à A. imhofi (République Tchèque) et à A. moyseyi (Royaume-Uni) est suggérée. Abstract Mots-clefs: Eurypterida, appendices, 'dumb-bells', Belgique, terrain houiller. The Carboniferous eurypterid Eurypterus dumonti Stainier, 1917 from Mechelen-aan-de-Maas (Maasmechelen). Belgium is redescribed and assigned to the genus Adelophthalmus. It is diagnosed as having a Introduction raised triangle of unknown function, dorsally on opisthosomal segment 7 and a carapace articulating laterally against the second opisthosomal segment. Earlier assignments ofthis species to the genus Unionopterus, Eurypterids are a diverse group of Palaeozoic, aquatic based on the carapace shape fïgured in the original description chelicerates (Stainier 1917), are incorrect and the existence of a Carboniferous ranging from the Upper Ordovician eurypterid with the characteristics described for Unionopterus must be (Tollerton 2004) to the Upper Permian (Plotnick questioned. -
This Article Appeared in a Journal Published by Elsevier. the Attached Copy Is Furnished to the Author for Internal Non-Commerci
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Gondwana Research 23 (2013) 354–366 Contents lists available at SciVerse ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr A new Ordovician eurypterid (Arthropoda: Chelicerata) from southeast Turkey: Evidence for a cryptic Ordovician record of Eurypterida James C. Lamsdell a,⁎, İzzet Hoşgör b, Paul A. Selden a,c,d a Paleontological Institute and Department of Geology, University of Kansas, Lawrence, Kansas, United States b TransAtlantic Petroleum Ltd.-Viking Int. Ltd. TR-06680, Ankara, Turkey c Natural History Museum, London, United Kingdom d Capital Normal University, Beijing, PR China article info abstract Article history: A new species of eurypterid, Paraeurypterus anatoliensis gen. et sp. nov., is described from the Upper Received 27 January 2012 Ordovician (Katian) Şort Tepe Formation of southeast Turkey. The single specimen, preserving the carapace, Received in revised form 20 April 2012 mesosoma and fragments of appendages, appears morphologically intermediate between the eurypteroid Accepted 20 April 2012 families Dolichopteridae and Eurypteridae. -
A New Eurypterid (Chelicerata) from the Upper Ordovician of Manitoulin Island, Ontario, Canada
J. Paleont., 79(6), 2005, pp. 1166±1174 Copyright q 2005, The Paleontological Society 0022-3360/05/0079-1166$03.00 A NEW EURYPTERID (CHELICERATA) FROM THE UPPER ORDOVICIAN OF MANITOULIN ISLAND, ONTARIO, CANADA CHRISTOPHER A. STOTT,1 O. ERIK TETLIE,2 SIMON J. BRADDY,3 GODFREY S. NOWLAN,4 PAUL M. GLASSER,5 AND MATTHEW G. DEVEREUX6 1Department of Earth Sciences, The University of Western Ontario, London, Ontario N6A 5B7, Canada ,[email protected]., 2Department of Geology and Geophysics, Yale University, PO Box 208109, New Haven, Connecticut 06520-8109, ,[email protected]., 3Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol BS8 1RJ, United Kingdom, 4Geological Survey of Canada, 3303-33rd Street N.W., Calgary, Alberta T2L 2A7, Canada, 5School of Dentistry, Faculty of Medicine & Dentistry, The University of Western Ontario, London, Ontario N6A 5C1, Canada, and 6Faculty of Science, Of®ce of the Dean, The University of Western Ontario, London, Ontario N6A 5B7, Canada ABSTRACTÐA new genus and species of eurypterid (Eurypterida: Chelicerata) is described as Orcanopterus manitoulinensis from the Upper Ordovician Kagawong Submember (Upper Member) of the Georgian Bay Formation, Manitoulin Island, Ontario, Canada. The material comprises several partial specimens in addition to disarticulated carapaces, appendages, metastomas, opisthosomal segments, and telsons. Associated fossils include rare bryozoans, a conularid, ostracodes, and conodonts. A restricted marine lagoon, or very shallow subtidal to intertidal environment is inferred. This assemblage, perhaps representing an accumulation of molted exuviae, was apparently preserved as the result of rapid burial by carbonate muds and silts during a storm event. -
The Early Devonian Eurypterid Grossopterus Overathi (Gross, 1933) from Overath, Germany
Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 5 (2002) 93-104 10.11.2002 The Early Devonian eurypterid Grossopterus overathi (Gross, 1933) from Overath, Germany Jason A. Dunlopl, Simon J. Braddy2 & Erik Tetlie2 With 6 figures Abstract The holotype and only known specimen of the eurypterid (Chelicerata: Eurypterida) Grossopterus overathi (Gross, 1933) from the Early Devonian (Siegennian) of Overath, north-west Germany is redescribed. Based on comparisons with other eurypterid taxa we interpret G. overathi as having a well-preserved type B genital appendage, which exhibits two apomorphic character states: (1) a furca fused into a single, spatulate plate and (2) marginal serrations near the distal end of the appendage. Grossop- terus is assigned to the family Hughmilleriidae, but its carapace resembles that of the larger Slimoniu acuminatu (Salter, 1856) (Slimoniidae). A provisional phylogenetic analysis resolves Grossopterus as the sister group of (Slimonia + Pterygotoidea). The large pterygotids, in particular, have been suggested as significant predators on early vertebrates and hypotheses about eurypterid-fish co-evolution are reviewed, in particular Romer’s proposal that dermal annour in fish evolved in response to eurypterid predation. Key words: Devonian, north-west Germany, Overath, Eurypterida, Grossopterus, Genital appendage, fish, co-evolution. Zusammenfassung Der Holotyp - das einzig bekannte Exemplar - des Eurypteriden (Chelicerata: Eurypterida) Grossopterus overathi (Gross, 1933) aus dem friihen Devon (Siegennian) von Overath im nordwestlichen Deutschland wird wieder beschrieben. Basierend auf Vergleichen mit anderen Eurypteriden-Taxa interpretieren wir G. overathi als Trager eines Typ B-Anhanges, wobei zwei apomorphe Merkmalszustande vorliegen: (1) die Furca ist zu einer einzigen, spatelformigen Platte verschmolzen, und (2) der Seitenrand nahe des distalen Endes des Genitalanhanges ist gezahnt. -
The Evolution of Feeding Within Euchelicerata: Data from the Fossil Groups Eurypterida and Trigonotarbida Illustrate Possible Evolutionary Pathways
The evolution of feeding within Euchelicerata: data from the fossil groups Eurypterida and Trigonotarbida illustrate possible evolutionary pathways Carolin Haug1,2 1 Department of Biology II, Ludwig-Maximilians-Universität München, Planegg-Martinsried, Germany 2 GeoBio-Center, Ludwig-Maximilians-Universität München, Munich, Germany ABSTRACT When the evolution of Euarthropoda is discussed, often the lineage of Chelicerata s. str. is assumed to be the more ‘primitive’ or ‘basal’ part of the tree, especially when compared to the other major lineage, Mandibulata. This claimed primitiveness is (at least partly) based on the assumption that different morphological structures are still in an ancestral state and did not evolve any further. One of these sets of structures is the feeding apparatus, which has been stated to be highly advanced in Mandibulata, but not ‘properly’ developed, or at least not to such a high degree, within Chelicerata s. str. In this study, I reinvestigate the feeding apparatus of different ingroups of Euchelicerata, with a focus on assumed ‘primitive’ groups such as Eurypterida and Trigonotarbida. The basis of this study is a large amount of material from different museum collections, with fossils with the entire feeding apparatuses being exceptionally well preserved. Based on high-resolution micro-photography and three-dimensional imaging, it is possible to resolve fine details of the feeding apparatuses. The results make clear that the feeding apparatuses of different ingroups of Euchelicerata are highly specialised and often possess morphological structures comparable to those of the feeding apparatuses of Submitted 2 October 2019 representatives of Mandibulata, apparently convergently evolved. Though the Accepted 20 July 2020 reconstruction of the evolution of the feeding apparatus within Euchelicerata is to a Published 13 August 2020 certain degree hampered by unclear phylogenetic relationships, there was clearly a Corresponding author shortening of the feeding apparatus from posterior (i.e. -
The Oldest Described Eurypterid: a Giant Middle Ordovician (Darriwilian) Megalograptid from the Winneshiek Lagerstätte of Iowa James C
Lamsdell et al. BMC Evolutionary Biology (2015) 15:169 DOI 10.1186/s12862-015-0443-9 RESEARCH ARTICLE Open Access The oldest described eurypterid: a giant Middle Ordovician (Darriwilian) megalograptid from the Winneshiek Lagerstätte of Iowa James C. Lamsdell1*, Derek E. G. Briggs1,2, Huaibao P. Liu3, Brian J. Witzke4 and Robert M. McKay3 Abstract Background: Eurypterids are a diverse group of chelicerates known from ~250 species with a sparse Ordovician record currently comprising 11 species; the oldest fully documented example is from the Sandbian of Avalonia. The Middle Ordovician (Darriwilian) fauna of the Winneshiek Lagerstätte includes a new eurypterid species represented by more than 150 specimens, including some juveniles, preserved as carbonaceous cuticular remains. This taxon represents the oldest described eurypterid, extending the documented range of the group back some 9 million years. Results: The new eurypterid species is described as Pentecopterus decorahensis gen. et sp. nov.. Phylogenetic analysis places Pentecopterus at the base of the Megalograptidae, united with the two genera previously assigned to this family by the shared possession of two or more pairs of spines per podomere on prosomal appendage IV, a reduction of all spines except the pair on the penultimate podomere of appendage V, and an ornamentation of guttalate scales, including angular scales along the posterior margin of the dorsal tergites and in longitudinal rows along the tergites. The morphology of Pentecopterus reveals that the Megalograptidae are representatives of the derived carcinosomatoid clade and not basal eurypterids as previously interpreted. Conclusions: The relatively derived position of megalograptids within the eurypterids indicates that most eurypterid clades were present by the Middle Ordovician. -
(Eurypterida: Chelicerata) from the Wenlock of Norway
NORWEGIAN JOURNAL OF GEOLOGY A new Baltoeurypterus from the Wenlock of Norway 37 A new Baltoeurypterus (Eurypterida : Chelicerata) from the Wenlock of Norway Odd Erik Tetlie Odd Erik Te tlie, A new Baltoeurypterus (Eurypterida: Chelicerata) from the Wenlock of Norway. Norsk Geologisk Tidsskrift, Vol. 82, pp. 37-44. Tr ondheim 2002. ISSN 029-196X. The genus Baltoeurypteruspreviously had two described species, of which B. tetragonophthalmus, (Fisher,1839), is the best known. A third species, B. henningsmoeni n. sp. is described here, based on two almost complete specimens and several fragments.This species is separated from B. tetra gonophthalmus by a broader paddle {L/W-ratio 1.8), a rounder metastoma (L/W-ratio 1.36) and by the presence of small lateral epimerae on the postabdomen. The distal part of a swimming leg of a pterygotid eurypterid is also described. These fossils constitute the oldest eurypterid remains known fromNorway. Odd Erik Tetlie, Paleontologisk Museum, Universitetet i Oslo, Postboks 1172 Blindern, N0-0318 Oslo, Norway. Present address: Department of Earth Sciences, Universityof Bristol, Wills Memorial Building, Queens Road,Bristol BSB l RJ, U.K. Email: o.e. [email protected]. uk lntroduction fairly complete eurypterids. In an oral statement, pre sented at Nordisk Geologisk Vintermøte, Goteborg in Eurypterids are extinct aquatic arthropods belonging January 1954, he reported the presence of Eurypterus fis to the Chelicerata, and are thus related to the living heri [ = Baltoeurypterus tetragonophthalmus (Fischer marine xiphosurans (horseshoe crabs) and the terres 1839)] and fragmentsof Pterygotus sp. However, notes trial arachnids (e.g., scorpions and spiders). Their habi left by both Henningsmoen and Professor L. -
Geofacts 34: Megalograptus Ohioensis—Ohio's Giant Sea Scorpion
GEOFACTS OHIO GEOLOGICAL SURVEY • DEPARTMENT OF NATURAL RESOURCES Megalograptus ohioensis—Ohio's Giant Sea Scorpion by Mark E. Peter Dorsal View One of Ohio’s most impressive fossil animals is Megalograptus ohioensis, a species of eurypterid (pronounced, “yuh-RIP-tuh-rid”), or “sea scorpion.” At up to 75 centimeters (30 inches) in length, this eurypterid was among the largest marine predators living 445 million years ago, during Late Ordovician time. During this time period, land that is now Ohio was located in a compound eye low latitude, south of Earth’s equator, and was covered by a warm occelli (head) and shallow inland sea. This sea was inhabited by a variety of prosoma (simple eyes) invertebrate animals. Some, such as sea stars, bivalves, and colonial corals, would have closely resembled forms living today. Other carapace groups, such as the extinct eurypterids and trilobites, would have mesosoma (dorsal head shield) been recognizable as relatives of living forms. (middle-body) Discovery The initial discovery of M. ohioensis was made in the summer of metasoma 1938, when Charles D. Cox, a University of Cincinnati student, was (after-body) opisthosoma (abdomen) working for a state highway crew near Manchester in Adams County, Ohio. The crew was excavating Upper Ordovician marine limestones and shales of the Elkhorn Formation. Mr. Cox noticed a large fossil in the bucket of a steam shovel and rescued it from reburial. He brought the fossil to the attention of geology professor Kenneth E. Caster, who later described it as a new species of eurypterid based Ventral View on this specimen and others from the same locality (fig. -
Note on Pterygotus Anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick
A tlantic Geology 95 Note on Pterygotus anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick Randall F. Miller Steinhammer Palaeontology Laboratory, New Brunswick Museum, 277 Douglas Avenue, Saint John, New Brunswick E2K1E5, Canada Date Received June 5, 1995 Date Accepted December 28, 1995 Fragments of the large eurypterid Pterygotus, recently collected from the Devonian Campbellton Formation at Atholville, New Brunswick, are identified as belonging to P. anglicus Agassiz. The only previous Pterygotus specimens from this site, collected in 1881, were assigned to a new species P. atlanticus Clarke and Ruedemann, in 1912. Clarke and Ruedemann’s suggestion that P. atlanticus might turn out to be a small specimen of P. anglicus is supported by this new find. However, possible revision of P. atlanticus awaits the discovery of additional, more complete, material. On a determine que les fragments du grand eurypteride Pterygotus rdcemment recueillis dans la Formation devonienne de Campbellton a Atholville, Nouveau-Brunswick, appartenaient au P. anglicus Agassiz. Les seuls specimens anterieurs de Pterygotus de cet emplacement, preleves en 1881, avaient 6t6 attribues a une nouvelle espece, le P. atlanticus, par Clarke et Ruedemann, en 1912. Cette nouvelle decouverte appuie l’hypothese de Clarke et Ruedemann a l’effet que le P. atlanticus pourrait en realite constituer un petit specimen de P. anglicus. La revision possible de la nature du P. atlanticus necessitera neanmoins la decouverte de materiel supplementaire plus complet. [Traduit par la redaction] I ntroduction L o c a t io n a n d stratigraphy Among reports of rare occurrences of eurypterids in New The specimens described here were recovered from cal Brunswick, two descriptions of Pterygotus exist.