A Predatory Bivalved Euarthropod from the Cambrian
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The Sirius Passet Lagerst‰Tte of North
Durham Research Online Deposited in DRO: 02 January 2019 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Hammarlund, Emma U. and Smith, M. Paul and Rasmussen, Jan A. and Nielsen, Arne T. and Caneld, Donald E. and Harper, David A. T. (2019) 'The Sirius Passet Lagerst¤atteof North Greenlanda geochemical window on early Cambrian lowoxygen environments and ecosystems.', Geobiology., 17 (1). pp. 12-26. Further information on publisher's website: https://doi.org/10.1111/gbi.12315 Publisher's copyright statement: c 2018 The Authors. Geobiology Published by John Wiley Sons Ltd This is an open access article under the terms of the Creative Commons AttributionNonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Received: 14 January 2018 | Revised: 17 August 2018 | Accepted: 22 August 2018 DOI: 10.1111/gbi.12315 ORIGINAL ARTICLE The Sirius Passet Lagerstätte of North Greenland—A geochemical window on early Cambrian low- oxygen environments and ecosystems Emma U. -
Soft−Part Preservation in Two Species of the Arthropod Isoxys from the Middle Cambrian Burgess Shale of British Columbia, Canada
Soft−part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada DIEGO C. GARCÍA−BELLIDO, JEAN VANNIER, and DESMOND COLLINS García−Bellido, D.C., Vannier, J., and Collins, D. 2009. Soft−part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada. Acta Palaeontologica Polonica 54 (4): 699–712. doi:10.4202/app.2009.0024 More than forty specimens from the middle Cambrian Burgess Shale reveal the detailed anatomy of Isoxys, a worldwide distributed bivalved arthropod represented here by two species, namely Isoxys acutangulus and Isoxys longissimus. I. acutangulus had a non−mineralized headshield with lateral pleural folds (= “valves” of previous authors) that covered the animal’s body almost entirely, large frontal spherical eyes and a pair of uniramous prehensile appendages bearing stout spiny outgrowths along their anterior margins. The 13 following appendages had a uniform biramous design—i.e., a short endopod and a paddle−like exopod fringed with marginal setae with a probable natatory function. The trunk ended with a flap−like telson that protruded beyond the posterior margin of the headshield. The gut of I. acutangulus was tube−like, running from mouth to telson, and was flanked with numerous 3D−preserved bulbous, paired features inter− preted as digestive glands. The appendage design of I. acutangulus indicates that the animal was a swimmer and a visual predator living off−bottom. The general anatomy of Isoxys longissimus was similar to that of I. acutangulus although less information is available on the exact shape of its appendages and visual organs. -
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 -
New Cheloniellid Arthropod with Large Raptorial Appendages from the Silurian of Wisconsin, USA
bioRxiv preprint doi: https://doi.org/10.1101/407379; this version posted September 7, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. New cheloniellid arthropod with large raptorial appendages from the Silurian of Wisconsin, USA Andrew J. Wendruff1*, Loren E. Babcock2, Donald G. Mikulic3, Joanne Kluessendorf4 1 Department of Biology and Earth Science, Otterbein University, Westerville, Ohio, United States of America, 2 Department of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America, 3 Illinois Geological Survey, Champaign, Illinois, United States of America, 4 Weis Earth Science Museum, University of Wisconsin-Fox Valley, Menasha, Wisconsin, United States of America *[email protected] Abstract Cheloniellids comprise a small, distinctive group of Paleozoic arthropods of whose phylogenetic relationships within the Arthropoda remain unresolved. A new form, Xus yus, n. gen, n. sp. is reported from the Waukesha Lagerstatte in the Brandon Bridge Formation (Silurian: Telychian), near Waukesha, Wisconsin, USA. Exceptionally preserved specimens show previously poorly known features including biramous appendages; this is the first cheloniellid to show large, anterior raptorial appendages. We emend the diagnosis of Cheloniellida; cephalic appendages are uniramous and may include raptorial appendages; trunk appendages are biramous. bioRxiv preprint doi: https://doi.org/10.1101/407379; this version posted September 7, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. -
The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life
Downloaded from http://jgs.lyellcollection.org/ by guest on October 1, 2021 Review focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2018-042 The Weeks Formation Konservat-Lagerstätte and the evolutionary transition of Cambrian marine life Rudy Lerosey-Aubril1*, Robert R. Gaines2, Thomas A. Hegna3, Javier Ortega-Hernández4,5, Peter Van Roy6, Carlo Kier7 & Enrico Bonino7 1 Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia 2 Geology Department, Pomona College, Claremont, CA 91711, USA 3 Department of Geology, Western Illinois University, 113 Tillman Hall, 1 University Circle, Macomb, IL 61455, USA 4 Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 6 Department of Geology, Ghent University, Krijgslaan 281/S8, B-9000 Ghent, Belgium 7 Back to the Past Museum, Carretera Cancún, Puerto Morelos, Quintana Roo 77580, Mexico R.L.-A., 0000-0003-2256-1872; R.R.G., 0000-0002-3713-5764; T.A.H., 0000-0001-9067-8787; J.O.-H., 0000-0002- 6801-7373 * Correspondence: [email protected] Abstract: The Weeks Formation in Utah is the youngest (c. 499 Ma) and least studied Cambrian Lagerstätte of the western USA. It preserves a diverse, exceptionally preserved fauna that inhabited a relatively deep water environment at the offshore margin of a carbonate platform, resembling the setting of the underlying Wheeler and Marjum formations. However, the Weeks fauna differs significantly in composition from the other remarkable biotas of the Cambrian Series 3 of Utah, suggesting a significant Guzhangian faunal restructuring. -
Soft Anatomy of the Early Cambrian Arthropod Isoxys Curvirostratus from the Chengjiang Biota of South China with a Discussion on the Origination of Great Appendages
Soft anatomy of the Early Cambrian arthropod Isoxys curvirostratus from the Chengjiang biota of South China with a discussion on the origination of great appendages DONG−JING FU, XING−LIANG ZHANG, and DE−GAN SHU Fu, D.−J., Zhang, X.−L., and Shu, D.−G. 2011. Soft anatomy of the Early Cambrian arthropod Isoxys curvirostratus from the Chengjiang biota of South China with a discussion on the origination of great appendages. Acta Palaeontologica Polonica 56 (4): 843–852. An updated reconstruction of the body plan, functional morphology and lifestyle of the arthropod Isoxys curvirostratus is proposed, based on new fossil specimens with preserved soft anatomy found in several localities of the Lower Cambrian Chengjiang Lagerstätte. The animal was 2–4 cm long and mostly encased in a single carapace which is folded dorsally without an articulated hinge. The attachment of the body to the exoskeleton was probably cephalic and apparently lacked any well−developed adductor muscle system. Large stalked eyes with the eye sphere consisting of two layers (as corneal and rhabdomeric structures) protrude beyond the anterior margin of the carapace. This feature, together with a pair of frontal appendages with five podomeres that each bear a stout spiny outgrowth, suggests it was raptorial. The following 14 pairs of limbs are biramous and uniform in shape. The slim endopod is composed of more than 7 podomeres without terminal claw and the paddle shaped exopod is fringed with at least 17 imbricated gill lamellae along its posterior margin. The design of exopod in association with the inner vascular (respiratory) surface of the carapace indicates I. -
Early Cambrian Fuxianhuiids from China Reveal Origin of the Gnathobasic Protopodite in Euarthropods
Early Cambrian fuxianhuiids from China reveal origin of the gnathobasic protopodite in euarthropods The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Yang, Jie, Javier Ortega-Hernández, David A. Legg, Tian Lan, Jin-bo Hou, and Xi-guang Zhang. 2018. “Early Cambrian fuxianhuiids from China reveal origin of the gnathobasic protopodite in euarthropods.” Nature Communications 9 (1): 470. doi:10.1038/s41467-017-02754-z. http://dx.doi.org/10.1038/s41467-017-02754-z. Published Version doi:10.1038/s41467-017-02754-z Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:35015071 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA ARTICLE DOI: 10.1038/s41467-017-02754-z OPEN Early Cambrian fuxianhuiids from China reveal origin of the gnathobasic protopodite in euarthropods Jie Yang1, Javier Ortega-Hernández 2,3, David A. Legg 4, Tian Lan5, Jin-bo Hou1 & Xi-guang Zhang 1 Euarthropods owe their evolutionary and ecological success to the morphological plasticity of their appendages. Although this variability is partly expressed in the specialization of the 1234567890():,; protopodite for a feeding function in the post-deutocerebral limbs, the origin of the former structure among Cambrian representatives remains uncertain. Here, we describe Alacaris mirabilis gen. et sp. nov. from the early Cambrian Xiaoshiba Lagerstätte in China, which reveals the proximal organization of fuxianhuiid appendages in exceptional detail. -
AND MICROFOSSIL RECORD of the CAMBRIAN PRIAPULID OTTOIA by MARTIN R
[Palaeontology, 2015, pp. 1–17] THE MACRO- AND MICROFOSSIL RECORD OF THE CAMBRIAN PRIAPULID OTTOIA by MARTIN R. SMITH1,THOMASH.P.HARVEY2 and NICHOLAS J. BUTTERFIELD1 1Department of Earth Sciences, University of Cambridge, Cambridge, UK; e-mails: [email protected], [email protected] 2Department of Geology, University of Leicester, Leicester, UK ; e-mail: [email protected] Typescript received 11 December 2014; accepted in revised form 31 March 2015 Abstract: The stem-group priapulid Ottoia Walcott, 1911, Ottoiid priapulids represented an important component of is the most abundant worm in the mid-Cambrian Burgess Cambrian ecosystems: they occur in a range of lithologies Shale, but has not been unambiguously demonstrated else- and thrived in shallow water as well as in the deep-water where. High-resolution electron and optical microscopy of setting of the Burgess Shale. A wider survey of Burgess macroscopic Burgess Shale specimens reveals the detailed Shale macrofossils reveals specific characters that diagnose anatomy of its robust hooks, spines and pharyngeal teeth, priapulid sclerites more generally, establishing the affinity establishing the presence of two species: Ottoia prolifica of a wide range of Small Carbonaceous Fossils and demon- Walcott, 1911, and Ottoia tricuspida sp. nov. Direct com- strating the prominent role of priapulids in Cambrian parison of these sclerotized elements with a suite of shale- seas. hosted mid-to-late Cambrian microfossils extends the range of ottoiid priapulids throughout the middle to upper Key words: Burgess Shale, Small Carbonaceous Fossils, pri- Cambrian strata of the Western Canada Sedimentary Basin. apulid diversity, Selkirkia. S TEM-group priapulid worms were a conspicuous compo- in analyses of its ecological and evolutionary significance nent of level-bottom Cambrian faunas (Conway Morris (Wills 1998; Bruton 2001; Vannier 2012; Wills et al. -
The Anatomy, Affinity, and Phylogenetic Significance of Markuelia
EVOLUTION & DEVELOPMENT 7:5, 468–482 (2005) The anatomy, affinity, and phylogenetic significance of Markuelia Xi-ping Dong,a,Ã Philip C. J. Donoghue,b,Ã John A. Cunningham,b,1 Jian-bo Liu,a andHongChengc aDepartment of Earth and Space Sciences, Peking University, Beijing 100871, China bDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK cCollege of Life Sciences, Peking University, Beijing 100871, China ÃAuthors for correspondence (email: [email protected], [email protected]) 1Present address: Department of Earth and Ocean Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, UK. SUMMARY The fossil record provides a paucity of data on analyses have hitherto suggested assignment to stem- the development of extinct organisms, particularly for their Scalidophora (phyla Kinorhyncha, Loricifera, Priapulida). We embryology. The recovery of fossilized embryos heralds new test this assumption with additional data and through the insight into the evolution of development but advances are inclusion of additional taxa. The available evidence supports limited by an almost complete absence of phylogenetic stem-Scalidophora affinity, leading to the conclusion that sca- constraint. Markuelia is an exception to this, known from lidophorans, cyclonerualians, and ecdysozoans are primitive cleavage and pre-hatchling stages as a vermiform and direct developers, and the likelihood that scalidophorans are profusely annulated direct-developing bilaterian with terminal primitively metameric. circumoral and posterior radial arrays of spines. Phylogenetic INTRODUCTION et al. 2004b). Very early cleavage-stage embryos of presumed metazoans and, possibly, bilaterian metazoans, have been re- The fossil record is largely a record of adult life and, thus, covered from the late Neoproterozoic (Xiao et al. -
New Palaeoscolecidan Worms from the Lower Cambrian: Sirius Passet, Latham Shale and Kinzers Shale
New palaeoscolecidan worms from the Lower Cambrian: Sirius Passet, Latham Shale and Kinzers Shale SIMON CONWAY MORRIS and JOHN S. PEEL Conway Morris, S. and Peel, J.S. 2010. New palaeoscolecidan worms from the Lower Cambrian: Sirius Passet, Latham Shale and Kinzers Shale. Acta Palaeontologica Polonica 55 (1): 141–156. Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with notable oc− currences in a number of Burgess Shale−type Fossil−Lagerstätten. In addition to material from the lower Cambrian Kinzers Formation and Latham Shale, we also describe two new palaeoscolecidan taxa from the lower Cambrian Sirius Passet Fossil−Lagerstätte of North Greenland: Chalazoscolex pharkus gen. et sp. nov and Xystoscolex boreogyrus gen. et sp. nov. These palaeoscolecidans appear to be the oldest known (Cambrian Series 2, Stage 3) soft−bodied examples, being somewhat older than the diverse assemblages from the Chengjiang Fossil−Lagerstätte of China. In the Sirius Passet taxa the body is composed of a spinose introvert (or proboscis), trunk with ornamentation that includes regions bearing cuticu− lar ridges and sclerites, and a caudal zone with prominent circles of sclerites. The taxa are evidently quite closely related; generic differentiation is based on degree of trunk ornamentation, details of introvert structure and nature of the caudal re− gion. The worms were probably infaunal or semi−epifaunal; gut contents suggest that at least X. boreogyrus may have preyed on the arthropod Isoxys. Comparison with other palaeoscolecidans is relatively straightforward in terms of compa− rable examples in other Burgess Shale−type occurrences, but is much more tenuous with respect to the important record of isolated sclerites. -
The Endemic Radiodonts of the Cambrian Stage 4 Guanshan Biota of South China
Editors' choice The endemic radiodonts of the Cambrian Stage 4 Guanshan Biota of South China DE-GUANG JIAO, STEPHEN PATES, RUDY LEROSEY-AUBRIL, JAVIER ORTEGA-HERNÁNDEZ, JIE YANG, TIAN LAN, and XI-GUANG ZHANG Jiao, D.-G., Pates, S., Lerosey-Aubril, R., Ortega-Hernández, J., Yang, J., Lan, T., and Zhang, X.-G. 2021. The endemic radiodionts of the Cambrian Stage 4 Guanshan Biota of South China. Acta Palaeontologica Polonica 66 (2): 255–274. The Guanshan Biota (South China, Cambrian, Stage 4) contains a diverse assemblage of biomineralizing and non-biomin- eralizing animals. Sitting temporally between the Stage 3 Chengjiang and Wuliuan Kaili Biotas, the Guanshan Biota con- tains numerous fossil organisms that are exclusive to this exceptional deposit. The Guanshan Konservat-Lagerstätte is also unusual amongst Cambrian strata that preserve non-biomineralized material, as it was deposited in a relatively shallow water setting. In this contribution we double the diversity of radiodonts known from the Guanshan Biota from two to four, and describe the second species of Paranomalocaris. In addition, we report the first tamisiocaridid from South China, and confirm the presence of a tetraradial oral cone bearing small and large plates in “Anomalocaris” kunmingensis, the most abundant radiodont from the deposit. All four radiodont species, and three genera, are apparently endemic to the Guanshan Biota. When considered in the wider context of geographically and temporally comparable radiodont faunas, endemism in Guanshan radiodonts is most likely a consequence of the shallower and more proximal environment in which they lived. The strong coupling of free-swimming radiodonts and benthic communities underlines the complex relationship between the palaeobiogeographic and environmental distributions of prey and predators. -
Annual Meeting 2000
PALAEONTOLOGICAL ASSOCIATION 44th Annual Meeting University of Edinburgh 17-20 December 1999 ABSTRACTS and PROGRAMME Notes: search for keywords or authors using your browser’s "Find" command. For booking details, see the "meetings" section of this site. Oral Presentations BLUE POOL BAY ? A CORAL-REEF OF THE LOWER CARBONIFEROUS OF SOUTH WALES Markus Aretz and Hans-Georg Herbig Institut of Geology, University of Cologne Köln, Zuelpicher Str. 49a, 50674 Cologne, Germany <[email protected]> <[email protected]> Buildups with a rigid coral framework are generally rare in Lower Carboniferous time. An exception was found in the Hunts Bay Oolite-Formation at Blue Pool Bay (Gower Peninsula). This bioherm is intercalated in well-bedded oolitic limestones. It is about 25 meters in width and rises up to 10 meters in thickness. The coral association indicates an Asbian age of the bioherm. The core of the structure consists of large massive colonies of Lithostrotion and a small number of dendroid colonies (Siphonodendron and Syringopora). Most of the corals are preserved in living position. The density of the colonies is high, in many cases they grow upon eachother. Dendroid corals become more common in the outer core. An increase of colonies, which are upside-down orientated, together with broken colonies and coarse debris describe the facies of the flanks. The general decrease of the amount of corals and the gradual increase of fragments of colonies in bioclastic rudstones to wackestones at the top of the structure characterize the end of the biohermal development. Due to the appearance of a coral framework and its thickness, the bioherm is wave resistant.