Arthropod Origins
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Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction
Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction by Curtis R. Congreve B.S., University of Rochester, 2006 M.S., University of Kansas, 2008 Submitted to the Department of Geology and the Faculty of the Graduate School of The University of Kansas in partial fulfillment on the requirements for the degree of Doctor of Philosophy 2012 Advisory Committee: ______________________________ Bruce Lieberman, Chair ______________________________ Paul Selden ______________________________ David Fowle ______________________________ Ed Wiley ______________________________ Xingong Li Defense Date: December 12, 2012 ii The Dissertation Committee for Curtis R. Congreve certifies that this is the approved Version of the following thesis: Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction Advisory Committee: ______________________________ Bruce Lieberman, Chair ______________________________ Paul Selden ______________________________ David Fowle ______________________________ Ed Wiley ______________________________ Xingong Li Accepted: April 18, 2013 iii Abstract: The end Ordovician mass extinction is the second largest extinction event in the history or life and it is classically interpreted as being caused by a sudden and unstable icehouse during otherwise greenhouse conditions. The extinction occurred in two pulses, with a brief rise of a recovery fauna (Hirnantia fauna) between pulses. The extinction patterns of trilobites are studied in this thesis in order to better understand selectivity of the -
Hox Gene Duplications Correlate with Posterior Heteronomy in Scorpions
Downloaded from http://rspb.royalsocietypublishing.org/ on February 17, 2015 Hox gene duplications correlate with posterior heteronomy in scorpions Prashant P. Sharma1, Evelyn E. Schwager2, Cassandra G. Extavour2 and Ward C. Wheeler1 rspb.royalsocietypublishing.org 1Division of Invertebrate Zoology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA 2Department of Organismic and Evolutionary Biology, Harvard University, 16 Divinity Avenue, Cambridge, MA 02138, USA Research The evolutionary success of the largest animal phylum, Arthropoda, has been attributed to tagmatization, the coordinated evolution of adjacent metameres Cite this article: Sharma PP, Schwager EE, to form morphologically and functionally distinct segmental regions called Extavour CG, Wheeler WC. 2014 Hox gene tagmata. Specification of regional identity is regulated by the Hox genes, of duplications correlate with posterior which 10 are inferred to be present in the ancestor of arthropods. With six heteronomy in scorpions. Proc. R. Soc. B 281: different posterior segmental identities divided into two tagmata, the bauplan of scorpions is the most heteronomous within Chelicerata. Expression 20140661. domains of the anterior eight Hox genes are conserved in previously surveyed http://dx.doi.org/10.1098/rspb.2014.0661 chelicerates, but it is unknown how Hox genes regionalize the three tagmata of scorpions. Here, we show that the scorpion Centruroides sculpturatus has two paralogues of all Hox genes except Hox3, suggesting cluster and/or whole genome duplication in this arachnid order. Embryonic anterior expression Received: 19 March 2014 domain boundaries of each of the last four pairs of Hox genes (two paralogues Accepted: 22 July 2014 each of Antp, Ubx, abd-A and Abd-B) are unique and distinguish segmental groups, such as pectines, book lungs and the characteristic tail, while main- taining spatial collinearity. -
Online Dictionary of Invertebrate Zoology Parasitology, Harold W
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Armand R. Maggenti Online Dictionary of Invertebrate Zoology Parasitology, Harold W. Manter Laboratory of September 2005 Online Dictionary of Invertebrate Zoology: S Mary Ann Basinger Maggenti University of California-Davis Armand R. Maggenti University of California, Davis Scott Gardner University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/onlinedictinvertzoology Part of the Zoology Commons Maggenti, Mary Ann Basinger; Maggenti, Armand R.; and Gardner, Scott, "Online Dictionary of Invertebrate Zoology: S" (2005). Armand R. Maggenti Online Dictionary of Invertebrate Zoology. 6. https://digitalcommons.unl.edu/onlinedictinvertzoology/6 This Article is brought to you for free and open access by the Parasitology, Harold W. Manter Laboratory of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Armand R. Maggenti Online Dictionary of Invertebrate Zoology by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Online Dictionary of Invertebrate Zoology 800 sagittal triact (PORIF) A three-rayed megasclere spicule hav- S ing one ray very unlike others, generally T-shaped. sagittal triradiates (PORIF) Tetraxon spicules with two equal angles and one dissimilar angle. see triradiate(s). sagittate a. [L. sagitta, arrow] Having the shape of an arrow- sabulous, sabulose a. [L. sabulum, sand] Sandy, gritty. head; sagittiform. sac n. [L. saccus, bag] A bladder, pouch or bag-like structure. sagittocysts n. [L. sagitta, arrow; Gr. kystis, bladder] (PLATY: saccate a. [L. saccus, bag] Sac-shaped; gibbous or inflated at Turbellaria) Pointed vesicles with a protrusible rod or nee- one end. dle. saccharobiose n. -
Discussion Acta Palaeontologica Polonica 63 (1): 105– 110, 2018
Discussion Acta Palaeontologica Polonica 63 (1): 105– 110, 2018 Reply to Comment on “Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris” with the formal description of Stanleycaris STEPHEN PATES, ALLISON C. DALEY, and JAVIER ORTEGA-HERNÁNDEZ As part of a comprehensive examination of all radiodontans extend beyond the fossil margins into the rock matrix, demon- from Cambrian localities in the USA, Pates et al. (2017a, b) strating that they are not part of the fossil specimen. and Pates and Daley (2017) revised the taxonomic affinities of several described specimens. This included the reinter- Antenniform frontal appendage.—There are no features that distinguish the structure regarded by Gámez Vintaned et al. pretation of two putative lobopodians, one from the Wheeler (2011) as an antenniform limb, and the interpretation of this Formation (Utah, USA) and one from the Valdemiedes For- feature as a small burrow is more compelling as it extends into mation (Spain), as frontal appendages of the radiodontan the surrounding matrix. Structures identified as “pores” are like- genera Stanleycaris and Caryosyntrips respectively. In their ly plucked mineral grains approximately aligned in this region, comment, Gámez Vintaned and Zhuravlev (2018) disagree and other unaligned voids can be seen elsewhere in the SEM with these conclusions and raise three topics for discussion: images (Gámez Vintaned et al. 2011: fig. 12.5h, k). (i) anatomical features they suggest support a lobopodian affinity for “Mureropodia”; (ii) the identity of Caryosyntrips Proboscis with retractor-protractor muscle system.—The as a radiodontan, and the assignment of certain specimens to presence of a fleshy proboscis among lobopodians has only been this genus; and (iii) the nomenclatural status of Stanleycaris reliably documented in the Chengjiang Onychodictyon ferox (Ou hirpex as an invalid taxon. -
Available Generic Names for Trilobites
AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites. -
Copertina Guida Ai TRILOBITI V3 Esterno
Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di Scienze della Terra dell'Università di Genova. Attualmente risiede in Belgio dove svolge attività come specialista nel settore dei Sistemi di Informazione Geografica e analisi di immagini digitali. Curatore scientifico del Museo Back to the Past, ha pubblicato numerosi volumi di paleontologia in lingua italiana e inglese, collaborando inoltre all’elaborazione di testi e pubblicazioni scientifiche a livello nazonale e internazionale. Oltre alla passione per questa classe di artropodi, i suoi interessi sono orientati alle forme di vita vissute nel Precambriano, stromatoliti, e fossilizzazioni tipo konservat-lagerstätte. Carlo Kier nato a Milano nel 1961, Carlo si è laureato in Legge, ed è attualmente presidente della catena di alberghi Azul Hotel. Risiede a Cancun, Messico, dove si dedica ad attività legate all'ambiente marino. All'età di 16 anni, ha iniziato una lunga collaborazione con il Museo di Storia Naturale di Milano, ed è a partire dal 1970 che prese inizio la vera passione per i trilobiti, dando avvio a quella che oggi è diventata una delle collezioni paleontologiche più importanti al mondo. La sua instancabile attività di ricerca sul terreno in varie parti del globo e la collaborazione con professionisti del settore, ha permesso la descrizione di nuove specie di trilobiti ed artropodi. Una forte determinazione e la costruzione di un nuovo complesso alberghiero (AZUL Sensatori) hanno infine concretizzzato la realizzazione -
2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS
2nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS. Characters and Parsimony. Jonathan M. Adrain, Department of Palaeontology, The Natural History Museum, London SW7 5BD, United King- dom; Gregory D. Edgecombe, Centre for Evolutionary Research, Australian Museum, 6 College Street, Sydney South, New South Wales 2000, Australia Character analysis is the single most important element of any phylogenetic study. Characters are simply criteria for comparing homologous organismic parts between taxa. Homology of organismic parts in any phylogenetic study is an a priori assumption, founded upon topological similarity through some or all stages of ontogeny. Once homolo- gies have been suggested, characters are invented by specifying bases of comparison of organismic parts from taxon to taxon within the study group. Ideally, all variation in a single homology occurring within the study group should be accounted for. Comparisons are between attributes of homologous parts, (e.g., simple presence, size of some- thing, number of something), and these attributes are referred to as character states. Study taxa are assigned member- ship in one (or more, in the case of polymorphisms) character-state for each character in the analysis. A single char- acter now implies discrete groupings of taxa, but this in itself does not constitute a phylogeny. In order to suggest or convey phylogenetic information, the historical status of each character-state, and of the the group of taxa it sug- gests, must be evaluated. That is, in the case of any two states belonging to the same character, we need to discover whether one state is primitive (broadly speaking, ancestral) or derived (representative of an evolutionary innovation) relative to the other. -
Fossils from South China Redefine the Ancestral Euarthropod Body Plan Cédric Aria1 , Fangchen Zhao1, Han Zeng1, Jin Guo2 and Maoyan Zhu1,3*
Aria et al. BMC Evolutionary Biology (2020) 20:4 https://doi.org/10.1186/s12862-019-1560-7 RESEARCH ARTICLE Open Access Fossils from South China redefine the ancestral euarthropod body plan Cédric Aria1 , Fangchen Zhao1, Han Zeng1, Jin Guo2 and Maoyan Zhu1,3* Abstract Background: Early Cambrian Lagerstätten from China have greatly enriched our perspective on the early evolution of animals, particularly arthropods. However, recent studies have shown that many of these early fossil arthropods were more derived than previously thought, casting uncertainty on the ancestral euarthropod body plan. In addition, evidence from fossilized neural tissues conflicts with external morphology, in particular regarding the homology of the frontalmost appendage. Results: Here we redescribe the multisegmented megacheirans Fortiforceps and Jianfengia and describe Sklerolibyon maomima gen. et sp. nov., which we place in Jianfengiidae, fam. nov. (in Megacheira, emended). We find that jianfengiids show high morphological diversity among megacheirans, both in trunk ornamentation and head anatomy, which encompasses from 2 to 4 post-frontal appendage pairs. These taxa are also characterized by elongate podomeres likely forming seven-segmented endopods, which were misinterpreted in their original descriptions. Plesiomorphic traits also clarify their connection with more ancestral taxa. The structure and position of the “great appendages” relative to likely sensory antero-medial protrusions, as well as the presence of optic peduncles and sclerites, point to an overall -
Evidence for Gill Slits and a Pharynx in Cambrian Vetulicolians: Implications for the Early Evolution of Deuterostomes Ou Et Al
Evidence for gill slits and a pharynx in Cambrian vetulicolians: implications for the early evolution of deuterostomes Ou et al. Ou et al. BMC Biology 2012, 10:81 http://www.biomedcentral.com/1741-7007/10/81 (2 October 2012) Ou et al. BMC Biology 2012, 10:81 http://www.biomedcentral.com/1741-7007/10/81 RESEARCHARTICLE Open Access Evidence for gill slits and a pharynx in Cambrian vetulicolians: implications for the early evolution of deuterostomes Qiang Ou1, Simon Conway Morris2*, Jian Han3, Zhifei Zhang3, Jianni Liu3, Ailin Chen4, Xingliang Zhang3 and Degan Shu1,3* Abstract Background: Vetulicolians are a group of Cambrian metazoans whose distinctive bodyplan continues to present a major phylogenetic challenge. Thus, we see vetulicolians assigned to groups as disparate as deuterostomes and ecdysozoans. This divergence of opinions revolves around a strikingly arthropod-like body, but one that also bears complex lateral structures on its anterior section interpreted as pharyngeal openings. Establishing the homology of these structures is central to resolving where vetulicolians sit in metazoan phylogeny. Results: New material from the Chengjiang Lagerstätte helps to resolve this issue. Here, we demonstrate that these controversial structures comprise grooves with a series of openings. The latter are oval in shape and associated with a complex anatomy consistent with control of their opening and closure. Remains of what we interpret to be a musculature, combined with the capacity for the grooves to contract, indicate vetulicolians possessed a pumping mechanism that could process considerable volumes of seawater. Our observations suggest that food captured in the anterior cavity was transported to dorsal and ventral gutters, which then channeled material to the intestine. -
The Evolution of Trilobite Body Patterning
ANRV309-EA35-14 ARI 20 March 2007 15:54 The Evolution of Trilobite Body Patterning Nigel C. Hughes Department of Earth Sciences, University of California, Riverside, California 92521; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:401–34 Key Words First published online as a Review in Advance on Trilobita, trilobitomorph, segmentation, Cambrian, Ordovician, January 29, 2007 diversification, body plan The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The good fossil record of trilobite exoskeletal anatomy and on- 10.1146/annurev.earth.35.031306.140258 togeny, coupled with information on their nonbiomineralized tis- Copyright c 2007 by Annual Reviews. sues, permits analysis of how the trilobite body was organized and All rights reserved developed, and the various evolutionary modifications of such pat- 0084-6597/07/0530-0401$20.00 terning within the group. In several respects trilobite development and form appears comparable with that which may have charac- terized the ancestor of most or all euarthropods, giving studies of trilobite body organization special relevance in the light of recent advances in the understanding of arthropod evolution and devel- opment. The Cambrian diversification of trilobites displayed mod- Annu. Rev. Earth Planet. Sci. 2007.35:401-434. Downloaded from arjournals.annualreviews.org ifications in the patterning of the trunk region comparable with by UNIVERSITY OF CALIFORNIA - RIVERSIDE LIBRARY on 05/02/07. For personal use only. those seen among the closest relatives of Trilobita. In contrast, the Ordovician diversification of trilobites, although contributing greatly to the overall diversity within the clade, did so within a nar- rower range of trunk conditions. -
The Extent of the Sirius Passet Lagerstätte (Early Cambrian) of North Greenland
The extent of the Sirius Passet Lagerstätte (early Cambrian) of North Greenland JOHN S. PEEL & JON R. INESON Ancillary localities for the Sirius Passet biota (early Cambrian; Cambrian Series 2, Stage 3) are described from the im- mediate vicinity of the main locality on the southern side of Sirius Passet, north-western Peary Land, central North Greenland, where slope mudstones of the Transitional Buen Formation abut against the margin of the Portfjeld Forma- tion carbonate platform. Whilst this geological relationship may extend over more than 500 km east–west across North Greenland, known exposures of the sediments yielding the lagerstätte are restricted to a 1 km long window at the south-western end of Sirius Passet. • Keywords: Early Cambrian, Greenland, lagerstätte. PEEL, J.S. & INESON, J.R. The extent of the Sirius Passet Lagerstätte (early Cambrian) of North Greenland. Bulletin of Geosciences 86(3), 535–543 (4 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received March 24, 2011; accepted in revised form July 8, 2011; published online July 28, 2011; issued September 30, 2011. John S. Peel, Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE-75 236 Uppsala, Sweden; [email protected] • Jon R. Ineson, Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; [email protected] Almost all of the fossils described from the early Cambrian The first fragmentary fossils from the Sirius Passet Sirius Passet Lagerstätte of northern Peary Land, North Lagerstätte (GGU collection 313035) were collected by Greenland, were collected from a single, west-facing talus A.K. -
Palaeoecology of the Early Cambrian Sinsk Biota from the Siberian Platform
Palaeogeography, Palaeoclimatology, Palaeoecology 220 (2005) 69–88 www.elsevier.com/locate/palaeo Palaeoecology of the Early Cambrian Sinsk biota from the Siberian Platform Andrey Yu. Ivantsova, Andrey Yu. Zhuravlevb,T, Anton V. Legutaa, Valentin A. Krassilova, Lyudmila M. Melnikovaa, Galina T. Ushatinskayaa aPalaeontological Institute, Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow 117997, Russia bA´rea y Museo de Paleontologı´a, faculdad de Ciences, Universidad de Zaragoza, C/ Pedro Cerbuna, 12, E-50009, Zaragoza, Spain Received 1 February 2002; accepted 15 January 2004 Abstract The Sinsk biota (Early Cambrian, Botoman Stage, Siberian Platform) inhabited an open-marine basin within the photic zone, but in oxygen-depleted bottom waters. Its rapid burial in a fine-grained sediment under anoxic conditions led to the formation of one of the earliest Cambrian Lagerst7tte. All the organisms of the biota were adapted to a life under dysaerobic conditions. It seems possible that the adaptations of many Cambrian organisms, which composed the trophic nucleus of the Sinsk Algal Lens palaeocommunity to low oxygen tensions allowed them to diversify in the earliest Palaeozoic, especially during the Cambrian. Nowadays these groups comprise only a negligible part of communities and usually survive in settings with low levels of competition. Nonetheless, the organization of the Algal Lens palaeocommunity was not simple, it consisted of diverse trophic guilds. The tiering among sessile filter-feeders was well developed with the upper tier at the 50 cm level. In terms of individuals, the community was dominated by sessile filter-feeders, vagrant detritophages, and diverse carnivores/scavengers. The same groups, but in slightly different order, comprised the bulk of the biovolume: vagrant epifaunal and nektobenthic carnivores/ scavengers, sessile filter-feeders, and vagrant detritophages.