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An Exceptionally Preserved Arthropod Cardiovascular System from the Early Cambrian
ARTICLE Received 20 Dec 2013 | Accepted 4 Mar 2014 | Published 7 Apr 2014 DOI: 10.1038/ncomms4560 An exceptionally preserved arthropod cardiovascular system from the early Cambrian Xiaoya Ma1,2, Peiyun Cong1, Xianguang Hou1, Gregory D. Edgecombe2 & Nicholas J. Strausfeld3 The assumption that amongst internal organs of early arthropods only the digestive system withstands fossilization is challenged by the identification of brain and ganglia in early Cambrian fuxianhuiids and megacheirans from southwest China. Here we document in the 520-million-year-old Chengjiang arthropod Fuxianhuia protensa an exceptionally preserved bilaterally symmetrical organ system corresponding to the vascular system of extant arthropods. Preserved primarily as carbon, this system includes a broad dorsal vessel extending through the thorax to the brain where anastomosing branches overlap brain seg- ments and supply the eyes and antennae. The dorsal vessel provides segmentally paired branches to lateral vessels, an arthropod ground pattern character, and extends into the anterior part of the abdomen. The addition of its vascular system to documented digestive and nervous systems resolves the internal organization of F. protensa as the most completely understood of any Cambrian arthropod, emphasizing complexity that had evolved by the early Cambrian. 1 Yunnan Key Laboratory for Palaeobiology, Yunnan University, Kunming 650091, China. 2 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK. 3 Department of Neuroscience and Center for Insect Science, University of Arizona, Tucson, Arizona 85721, USA. Correspondence and requests for materials should be addressed to X.H. (email: [email protected]) or to N.J.S. (email: fl[email protected]). -
The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
The Impact of Deep-Tier Burrow Systems in Sediment Mixing and Ecosystem Engineering in Early Cambrian Carbonate Settings
www.nature.com/scientificreports OPEN The impact of deep-tier burrow systems in sediment mixing and ecosystem engineering in early Received: 17 November 2016 Accepted: 02 March 2017 Cambrian carbonate settings Published: 04 April 2017 Li-Jun Zhang1, Yong-An Qi1, Luis A. Buatois2, M. Gabriela Mángano2, Yao Meng1 & Da Li1 Bioturbation plays a substantial role in sediment oxygen concentration, chemical cycling, regeneration of nutrients, microbial activity, and the rate of organic matter decomposition in modern oceans. In addition, bioturbators are ecosystem engineers which promote the presence of some organisms, while precluding others. However, the impact of bioturbation in deep time remains controversial and limited sediment mixing has been indicated for early Paleozoic seas. Our understanding of the actual impact of bioturbation early in the Phanerozoic has been hampered by the lack of detailed analysis of the functional significance of specific burrow architectures. Integration of ichnologic and sedimentologic evidence from North China shows that deep-tier Thalassinoides mazes occur in lower Cambrian nearshore carbonate sediments, leading to intense disruption of the primary fabric. Comparison with modern studies suggest that some of the effects of this style of Cambrian bioturbation may have included promotion of nitrogen and ammonium fluxes across the sediment-water interface, average deepening of the redox discontinuity surface, expansion of aerobic bacteria, and increase in the rate of organic matter decomposition and the regeneration of nutrients. Our study suggests that early Cambrian sediment mixing in carbonate settings may have been more significant than assumed in previous models. Bioturbation, involving both particle and solute transport within burrows, into the surrounding sediment and across the sediment-water interface, is one of the most important factors in affecting oxygen concentration in the sediment, chemical cycling, regeneration of nutrients, microbial activity and the rate of organic matter decom- position in modern oceans1–3. -
This Is a PDF File of the Manuscript That Has Been Accepted for Publication
This is a PDF file of the manuscript that has been accepted for publication. This file will be reviewed by the authors and editors before the paper is published in its final form. Please note that during the production process errors may be discovered which could affect the content. All legal disclaimers that apply to the journal pertain. A new link between "Orsten"-type assemblages and the Burgess Shale—a Marrella-like arthropod from the Cambrian of Australia JOACHIM T. HAUG, CHRISTOPHER CASTELLANI, CAROLIN HAUG, DIETER WALOSZEK, and ANDREAS MAAS Haug, J.T., Castellani, C., Haug, C., Waloszek, D., and Maas, A. 201X. A new link between "Orsten"-type assemblages and the Burgess Shale—a Marrella-like arthropod from the Cambrian of Australia. Acta Palaeontologica Polonica 5X (X): xxx-xxx. http://dx.doi.org/10.4202/app.2011.0120 An isolated exopod in uncompressed three-dimensional "Orsten"-type preservation from the Cambrian of Australia represents a new species of Marrellomorpha, Austromarrella klausmuelleri gen. et sp. nov. The exopod is composed of at least 17 annuli. Each of the proximal annuli carries a pair of lamellae: one lamella on the lateral side and one on the median side. The distal annuli bear stout spines in the corresponding position instead of lamellae, most likely representing early ontogenetic equivalents of the lamellae. The new find extends the geographical range of the taxon Marrellomorpha. Additionally, it offers a partial view into marrellomorph ontogeny. The occurrence of a marrellomorph fragment in "Orsten"-type preservation provides new insight into the possible connections between the "Orsten" biotas and other fossil Lagerstätten. -
A New Phyllopod Bed-Like Assemblage from the Burgess Shale of the Canadian Rockies
ARTICLE Received 30 Dec 2013 | Accepted 7 Jan 2014 | Published 11 Feb 2014 DOI: 10.1038/ncomms4210 A new phyllopod bed-like assemblage from the Burgess Shale of the Canadian Rockies Jean-Bernard Caron1,2,3, Robert R. Gaines4,Ce´dric Aria1,2, M. Gabriela Ma´ngano5 & Michael Streng6 Burgess Shale-type fossil assemblages provide the best evidence of the ‘Cambrian explosion’. Here we report the discovery of an extraordinary new soft-bodied fauna from the Burgess Shale. Despite its proximity (ca. 40 km) to Walcott’s original locality, the Marble Canyon fossil assemblage is distinct, and offers new insights into the initial diversification of metazoans, their early morphological disparity, and the geographic ranges and longevity of many Cambrian taxa. The arthropod-dominated assemblage is remarkable for its high density and diversity of soft-bodied fossils, as well as for its large proportion of new species (22% of total diversity) and for the preservation of hitherto unreported anatomical features, including in the chordate Metaspriggina and the arthropod Mollisonia. The presence of the stem arthropods Misszhouia and Primicaris, previously known only from the early Cambrian of China, suggests that the palaeogeographic ranges and longevity of Burgess Shale taxa may be underestimated. 1 Department of Natural History-Palaeobiology, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario, Canada M5S 2C6. 2 Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, Ontario, Canada M5S 3B2. 3 Department of Earth Sciences, University of Toronto, 25 Russell Street, Toronto, Ontario, Canada M5S 3B1. 4 Geology Department, Pomona College, 185 E. Sixth Street, Claremont, California 91711, USA. -
Paleoecology of the Greater Phyllopod Bed Community, Burgess Shale ⁎ Jean-Bernard Caron , Donald A
Available online at www.sciencedirect.com Palaeogeography, Palaeoclimatology, Palaeoecology 258 (2008) 222–256 www.elsevier.com/locate/palaeo Paleoecology of the Greater Phyllopod Bed community, Burgess Shale ⁎ Jean-Bernard Caron , Donald A. Jackson Department of Ecology and Evolutionary Biology, University of Toronto, Toronto, Ontario, Canada M5S 3G5 Accepted 3 May 2007 Abstract To better understand temporal variations in species diversity and composition, ecological attributes, and environmental influences for the Middle Cambrian Burgess Shale community, we studied 50,900 fossil specimens belonging to 158 genera (mostly monospecific and non-biomineralized) representing 17 major taxonomic groups and 17 ecological categories. Fossils were collected in situ from within 26 massive siliciclastic mudstone beds of the Greater Phyllopod Bed (Walcott Quarry — Fossil Ridge). Previous taphonomic studies have demonstrated that each bed represents a single obrution event capturing a predominantly benthic community represented by census- and time-averaged assemblages, preserved within habitat. The Greater Phyllopod Bed (GPB) corresponds to an estimated depositional interval of 10 to 100 KA and thus potentially preserves community patterns in ecological and short-term evolutionary time. The community is dominated by epibenthic vagile deposit feeders and sessile suspension feeders, represented primarily by arthropods and sponges. Most species are characterized by low abundance and short stratigraphic range and usually do not recur through the section. It is likely that these are stenotopic forms (i.e., tolerant of a narrow range of habitats, or having a narrow geographical distribution). The few recurrent species tend to be numerically abundant and may represent eurytopic organisms (i.e., tolerant of a wide range of habitats, or having a wide geographical distribution). -
A New Marrellomorph Euarthropod from the Early Ordovician of Argentina
Editors' choice A new marrellomorph euarthropod from the Early Ordovician of Argentina MARÍA J. ARIS, JOSE A. CORRONCA, SEBASTIÁN QUINTEROS, and PAOLO L. PARDO Aris, M.J., Corronca, J.A., Quinteros, S., and Pardo, P.L. 2017. A new marrellomorph euarthropod from the Early Ordo- vician of Argentina. Acta Palaeontologica Polonica 62 (X): xxx–xxx. Marrellomorphs (class Marrellomorpha) are a group of Paleozoic arthropods with a very poor fossil record. Here we describe a new marrellomorph arthropod Mimetaster florestaensis sp. nov. from the Tremadocian (earliest Ordovician) of Argentina. The new species is characterized by the shape and direction of the three pairs of principal spines, and the existence of strong secondary spines only in the proximal two-thirds of the anterolateral spines. As a result of phyloge- netic analysis the new species integrates a trichotomy with Mimetaster hexagonalis and a Moroccan unnamed marrellid as sister groups. This discovery increases the known diversity of Marrellomorpha and represents the first occurrence of this group in South America, expanding the spatial distribution of the clade. Key words: Marrellida, Mimetasteridae, Tremadocian, Floresta Formation, Argentina, Salta. María J. Aris [[email protected]], Cátedra de Paleontología, Consejo de Investigación de la Universidad Nacional de Salta (CIUNSa) and Instituto para el Estudio de la Biodiversidad de Invertebrados (IEBI), Facultad de Ciencias Naturales de la Universidad Nacional de Salta, Av. Bolivia 5150, CP 4400 Salta, Argentina. Jose A. Corronca [[email protected]] and Paolo L. Pardo [[email protected]], Instituto para el Estudio de la Biodiversidad de Invertebrados (IEBI) and Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Facultad de Ciencias Naturales de la Universidad Nacional de Salta, Av. -
Parvancorina — an Arthropod from the Late Precambrian (Ediacarian) of South Australia
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Annalen des Naturhistorischen Museums in Wien Jahr/Year: 1980 Band/Volume: 83 Autor(en)/Author(s): Glaessner [Glässner] Martin Fritz Artikel/Article: Parvancorina - an artheopod from the Late Precambrian (Ediacarian) of South Australia. 83-90 ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien 83 83-90 Wien, Dezember 1980 Parvancorina — an arthropod from the Late Precambrian (Ediacarian) of South Australia By MARTIN F. GLAESSNEE *) (With I textfigure and 3 plates) Abstract After consideration of the preservation of the remains of the flexible integuments of some 60 specimens of Parvancorina minchami GLAESSNER, 1958, from Ediacara, available details of their morphology are reviewed and interpreted in terms of growth, feeding and locomotion. Insufficient detail of their limbs is preserved to define unequivocally the systematic position and phylogenetic significance of Parvancorina. Resemblances with other fossils support assignment to the Arthropoda. The genus is believed to be related to Marrellomorpha which appear to be phylogenetically close to ancestral Trilobitomorpha. These are considered to have diversified into divergent lines of descent leading to Crustacea and Chelicerata, but Parvancorina is unlikely to have direct descendants among the living arthropods. Zusammenfassung Etwa 60 Exemplare von Parvancorina minchami GLAESSNER, 1958, von der Fund- stelle Ediacara wurden untersucht. Die Fossilisation ihrer oft deformierten und ursprüng- lich biegsamen Körperhülle wird beschrieben und Wachstum, Nahrungsaufnahme und Bewegung werden dargestellt. Der Bau der Gliedmaßen ist nicht in Einzelheiten erkenn- bar, so daß die systematische und phylogenetische Einordnung der Gattung nicht präzi- siert werden kann. -
Canada Archives Canada Published Heritage Direction Du Branch Patrimoine De I'edition
THE BURGESS SHALE: A CAMBRIAN MIRROR FOR MODERN EVOLUTIONARY BIOLOGY by Keynyn Alexandra Ripley Brysse A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Institute for the History and Philosophy of Science and Technology University of Toronto © Copyright by Keynyn Alexandra Ripley Brysse (2008) Library and Bibliotheque et 1*1 Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-44745-1 Our file Notre reference ISBN: 978-0-494-44745-1 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library permettant a la Bibliotheque et Archives and Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par Plntemet, prefer, telecommunication or on the Internet, distribuer et vendre des theses partout dans loan, distribute and sell theses le monde, a des fins commerciales ou autres, worldwide, for commercial or non sur support microforme, papier, electronique commercial purposes, in microform, et/ou autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in et des droits moraux qui protege cette these. this thesis. Neither the thesis Ni la these ni des extraits substantiels de nor substantial extracts from it celle-ci ne doivent etre imprimes ou autrement may be printed or otherwise reproduits sans son autorisation. -
1532 Legg.Vp
The morphology and affinities of Skania fragilis (Arthropoda) from the middle Cambrian Burgess Shale DAVID A. LEGG The enigmatic arthropod Skania fragilis, from the middle Cambrian (Series 3, Stage 5) Burgess Shale Formation (Yoho National Park, British Columbia, Canada), is redescribed based on 14 new specimens reposited at the Royal Ontario Mu- seum. These specimens provide a clearer picture of the morphology of this taxon and help to resolve conflicting opinions regarding potential homology of particular features. Specifically, the anchor-shaped anterior, which has been compared to a similar structure in the putative Precambrian arthropod Parvancorina, is shown to represent an anterior cephalic doublure with features comparable to the mediolateral spines of marrellids, such as Marrella. Beyond a vaguely cordiform outline, no other features are shown to be shared between Skania and Parvancorina, weakening claims that crown-group arthropods were present in the Neoproterozoic. The removal of these taxa from Arthropoda is in keeping with recent molecular clock analyses, which demonstrate a Cambrian diversification of Euarthropoda. A phylogenetic analysis resolved Skania as the most basal member of Acercostraca, a clade of marrellomorphs including Vachonisia and Xylokorys, united by the presence of a cordiform dorsal shield. Similarities between these taxa and marrellids may indicate that the elongate posterior spines of Marrella and related taxa, and the dorsal shield of acercostracans have a common origin akin to the carapace anlagen of extant crustaceans. • Key words: marrellomorph, carapace formation, Burgess Shale. LEGG, D.A. 2015. The morphology and affinities of Skania fragilis (Arthropoda) from the middle Cambrian Burgess Shale. Bulletin of Geosciences 90(3), 509–518 (5 figures, 2 online appendices). -
Biogeography and the Cambrian Radiation of Arachnomorph Arthropods
San Jose State University SJSU ScholarWorks Faculty Publications Geology January 2007 Biogeography and the Cambrian radiation of arachnomorph arthropods Jonathan R. Hendricks University of Kansas, [email protected] Bruce S. Lieberman University of Kansas Follow this and additional works at: https://scholarworks.sjsu.edu/geol_pub Part of the Geology Commons Recommended Citation Jonathan R. Hendricks and Bruce S. Lieberman. "Biogeography and the Cambrian radiation of arachnomorph arthropods" Memoirs of the Association of Australasian Palaeontologists (2007): 29-39. This Article is brought to you for free and open access by the Geology at SJSU ScholarWorks. It has been accepted for inclusion in Faculty Publications by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. Biogeography and the Cambrian radiation of arachnomorph arthropods JONATHAN R. HENDRICKS & BRUCE S. LIEBERMAN HENDRICKS, J.R. & LIEBERMAN, B.S., 2007:12:21. Biogeography and the Cambrian radiation of arachnomorph arthropods. Memoirs of the Association of Australasian Palaeontologists 34, 461-471. ISSN 0810-8889. Biogeographic patterns in primarily Cambrian arachnomorph taxa are investigated using a recently constructed phylogenetic hypothesis in order to explore the biogeographic context of the Cambrian radiation. A modified version of Brooks Parsimony Analysis is employed to elucidate patterns of vicariance and geodispersal in taxa from six regions (Laurentia, Baltica, Siberia, Australia, Africa and China). Well resolved vicariance and geodispersal trees are very similar and reconstruct Laurentia and China as sister areas. This close area relationship between Laurentia and China provides extensive evidence for congruent vicariance and range expansion in Cambrian arachnomorphs, while data from trilobites do not show this pattern. -
Moulting Arthropod Caught in the Act a Cambrian Fossil Confirms That Early Arthropods Shed Their Coats Just As They Do Today
brief communications Moulting arthropod caught in the act A Cambrian fossil confirms that early arthropods shed their coats just as they do today. ntil now, the existence of ecdysis (moulting) in early arthropods has Ubeen based solely on inference. Here we describe a 505-million-year-old specimen of the Cambrian soft-bodied arthropod Marrella splendens that has been visibly preserved in the middle of the act of moulting. This speci- men confirms that early arthropods moulted during growth, just as they do today. Ecdysis is a fundamental process that is thought to characterize the clade Ecdysozoa, which encompasses all moulting animals, including arthropods, tardigrades, ony- chophorans, nematodes, nematomorphs, kinorhynchs and priapulids1.It may be that creatures in other groups moult2,but evi- dence for this is anecdotal. Although ecdysis seems to have been a common feature of these phyla as far back as the Cambrian period3,evi- dence for moulting during the Cambrian is circumstantial. For example, a few Cambrian trilobite specimens have been recorded as being pre- served in an exuvial configuration4, indicat- ing that they had just moulted. Mineralized hard parts of the trilobite exoskeleton found next to similar, less well mineralized parts Figure 1 The oldest known fossil of an arthropod in the act of moulting: Marrella splendens, from the Middle Cambrian Burgess Shale of British have been interpreted as a new exoskeleton Columbia, Canada. a, Specimen of M. splendens (ROM 56781) emerging and pulling out the flexible lateral spines from the old exoskeleton emerging from the old one, the exuvia. This (exuvia). b, Camera lucida drawing of the same specimen.