An Exceptionally Preserved Arthropod Cardiovascular System from the Early Cambrian
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Evolutionary and Historical Biogeography of Animal Diversity Learning Objectives
Evolutionary and historical biogeography of animal diversity Learning objectives • The students can explain the common ancestor of animal kingdom. • The students can explain the historical biogeography of animal. • The students can explain the invasion of animal from aquatic to terrestrial habitat. • The students can explain the basic mechanism of speciation, allopatric and non-allopatric. The Common Ancestor of Animal Kingdom Characteristics of Animals • Animals or “metazoans” are typically heterotrophic, multicellular organisms with diploid, eukaryotic cells. • Trichoplax adhaerens is defined as an animal by the presence of different somatic (i.e., non-reproductive) cell types and by impermeable cell–cell connections. Trichoplax adhaerens Blackstone, 2009 Two Hypotheses for the Branching Order of Groups at the Root of the Metazoan Tree 1 2 The choanoflagellates serve as an outgroup in the Bilaterians are the sister group to the placozoan + analysis, and sponges are the sister group to the sponge + ctenophore + cnidarian clade, while placozoans placozoan + cnidarian + ctenophore + bilaterian are the sister group to the sponge + ctenophore + clade. cnidarian clade. Blackstone, 2009 Ancestry and evolution of animal–bacterial interactions • Choanoflagellates as the last common ancestor of animal kingdom. • Urmetazoan is the group of animal with multicellular and produce differentiated cell types (ex. Egg & sperm) R.A. Alegado & N. King, 2014 Conserved morphology and ultrastructure of Choanoflagellates and Sponge choanocytes The collar complex is conserved in choanoflagellates (A. S. rosetta) and sponge collar cells (B. Sycon coactum) flagellum (fL), microvilli (mv), a nucleus (nu), and a food vacuole (fv) Brunet & King, 2017 The Historical Biogeography of Animal Zoogeographic regions Old New Cox, 2001 Plate tectonic regulation of global marine animal diversity A. -
Arachnida, Solifugae) with Special Focus on Functional Analyses and Phylogenetic Interpretations
HISTOLOGY AND ULTRASTRUCTURE OF SOLIFUGES Comparative studies of organ systems of solifuges (Arachnida, Solifugae) with special focus on functional analyses and phylogenetic interpretations HISTOLOGIE UND ULTRASTRUKTUR DER SOLIFUGEN Vergleichende Studien an Organsystemen der Solifugen (Arachnida, Solifugae) mit Schwerpunkt auf funktionellen Analysen und phylogenetischen Interpretationen I N A U G U R A L D I S S E R T A T I O N zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) an der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Anja Elisabeth Klann geboren am 28.November 1976 in Bremen Greifswald, den 04.06.2009 Dekan ........................................................................................................Prof. Dr. Klaus Fesser Prof. Dr. Dr. h.c. Gerd Alberti Erster Gutachter .......................................................................................... Zweiter Gutachter ........................................................................................Prof. Dr. Romano Dallai Tag der Promotion ........................................................................................15.09.2009 Content Summary ..........................................................................................1 Zusammenfassung ..........................................................................5 Acknowledgments ..........................................................................9 1. Introduction ............................................................................ -
(LINNAEUS, 1758) in the SOUTH of WESTERN SIBERIA, RUSSIA (CHILOPODA: SCUTIGEROMORPHA: SCUTIGERIDAE) 1Altai State University, Lenina Avenue, 61, Barnaul 656049, Russia
428 Бiологiчний вiсник UDC 595.624 Nefediev P.S.1, Tuf I.H.2, Dyachkov Yu.V.1, Efimov D.A.3 FIRST RECORD OF SCUTIGERA COLEOPTRATA (LINNAEUS, 1758) IN THE SOUTH OF WESTERN SIBERIA, RUSSIA (CHILOPODA: SCUTIGEROMORPHA: SCUTIGERIDAE) 1Altai State University, Lenina Avenue, 61, Barnaul 656049, Russia. E-mail: [email protected] 2Palacký University, Šlechtitelů 27, Olomouc 77900, Czech Republic. E-mail: [email protected] 3Kemerovo State University, Krasnaya Street, 6, Kemerovo 650043, Russia. E-mail: [email protected] The order, family, genus and species of the house centipede are new to Asian Russia’s list: Scutigeromorpha, Scutigeridae, Scutigera Lamark, 1801, and Scutigera coleoptrata (Linnaeus, 1758). All records of the species in the south of western Siberia appear to be associated with synanthropic habitats. Distributional remarks are provided, all currently reported findings being mapped as well. Key words: house centipede, Scutigera coleoptrata, Scutigeridae, Scutigeromorpha, anthropochore, faunistics, introduction, Siberia. INTRODUCTION The centipede fauna of Siberia is very poorly-studied. All former research has been devoted to Lithobiomorpha and Geophilomorpha in natural habitats. Investigating anthropogenic habitats in the south of western Siberia, we have currently found the house centipede Scutigera coleoptrata (Linnaeus, 1758). Both the order Scutigeromorpha, and the family Scutigeridae it belongs to, are almost worldwide, distributed in all continents, on all major islands and many oceanic islands with the exception of Antarctica, and many records refer to introduced populations of Scutigera coleoptrata (Bonato & Zapparoli, 2011). The samples treated below have been deposited in the collection of the Altai State University, Barnaul, Russia (ASU). RESULTS SCUTIGEROMORPHA Pocock, 1895 SCUTIGERIDAE Gervais, 1837 Scutigera coleoptrata (Linnaeus, 1758) ISSN 2225-5486 (Print), ISSN 2226-9010 (Online). -
Morphology and Function in the Cambrian Burgess Shale
Haug et al. BMC Evolutionary Biology 2012, 12:162 http://www.biomedcentral.com/1471-2148/12/162 RESEARCH ARTICLE Open Access Morphology and function in the Cambrian Burgess Shale megacheiran arthropod Leanchoilia superlata and the application of a descriptive matrix Joachim T Haug1*, Derek EG Briggs2,3 and Carolin Haug1 Abstract Background: Leanchoilia superlata is one of the best known arthropods from the middle Cambrian Burgess Shale of British Columbia. Here we re-describe the morphology of L. superlata and discuss its possible autecology. The re-description follows a standardized scheme, the descriptive matrix approach, designed to provide a template for descriptions of other megacheiran species. Results: Our findings differ in several respects from previous interpretations. Examples include a more slender body; a possible hypostome; a small specialised second appendage, bringing the number of pairs of head appendages to four; a further sub-division of the great appendage, making it more similar to that of other megacheirans; and a complex joint of the exopod reflecting the arthropod’s swimming capabilities. Conclusions: Different aspects of the morphology, for example, the morphology of the great appendage and the presence of a basipod with strong median armature on the biramous appendages indicate that L. superlata was an active and agile necto-benthic predator (not a scavenger or deposit feeder as previously interpreted). Keywords: Megacheira, Great-appendage arthropods, Chelicerata sensu lato, Descriptive matrix, Active predator Background shared with other species. As a consequence, morpho- The description of species is fundamental to the science logical details in many phylogenetic matrices have to be of zoology, including taxonomy, phylogenetic systema- (re-)interpreted, often without the benefit of a compre- tics, functional morphology and ultimately evolutionary hensive description. -
MYRIAPODS 767 Volume 2 (M-Z), Pp
In: R. Singer, (ed.), 1999. Encyclopedia of Paleontology, MYRIAPODS 767 volume 2 (M-Z), pp. 767-775. Fitzroy Dearborn, London. MYRIAPODS JVlyriapods are many-legged, terrestrial arthropods whose bodies groups, the Trilobita, Chelicerata, Crustacea, and the Uniramia, the are divided into two major parts, a head and a trunk. The head last consisting of the Myriapoda, Hexapoda, and Onychophora (vel- bears a single pair of antennae, highly differentiated mandibles (or vet worms). However, subsequent structural and molecular evidence jaws), and at least one pair of maxillary mouthparts; the trunk indicates that there are several characters uniting major arthropod region consists of similar "metameres," each of which is a func- taxa. Moreover, paleobiologic, embryologie, and other evidence tional segment that bears one or two pairs of appendages. Gas demonstrates that myriapods and hexapods are fiindamentally exchange is accomplished by tracheae•a branching network of polyramous, having two major articulating appendages per embry- specialized tubules•although small forms respire through the ological body segment, like other arthropods. body wall. Malpighian organs are used for excretion, and eyes con- A fourth proposal (Figure ID) suggests that myriapods are sist of clusters of simple, unintegrated, light-sensitive elements an ancient, basal arthropod lineage, and that the Hexapoda that are termed ommatidia. These major features collectively char- emerged as an independent, relatively recent clade from a rather acterize the five major myriapod clades: Diplopoda (millipeds), terminal crustacean lineage, perhaps the Malacostraca, which con- Chilopoda (centipeds), Pauropoda (pauropods), Symphyla (sym- tains lobsters and crabs (Ballard et al. 1992). Because few crusta- phylans), and Arthropleurida (arthropleurids). Other features cean taxa were examined in this analysis, and due to the Cambrian indicate differences among these clades. -
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. -
On the Presence of Scutigera Coleoptrata (Linnaeus, 1758) (Chilopoda: Scutigeromorpha: Scutigeridae) in the Metropolitan Region, Chile
MASUMOTO, K., G. DELLACASA & M. KIUCHI 1990. On the Aphodius de Storia naturale, Milano, 114: 51-70. ● REITTER, E. 1895. Einige species of Japan. Entomological Review of Japan, 45: 145-156. ● neue Coleopteren aus Korea und China. Wiener entomologische MÜLLER, G. 1941. Nuovi Coleotteri dell’Africa Orientale. Atti del Zeitung, 14: 208-210. ● SCHMIDT, A. 1907. Zusammentellung der Museo civico di Storia naturale di Trieste, 14: 319-352. ● NEAVE, bis 1906 beschriebenen Aphodiinen. Deutsche entomologische S.A. 1939. Nomenclator Zoologicus. A List of the Names of Genera Zeitschrift, Beilage, 1907-1908: 1-141. ● SCHMIDT, A. 1910a. Col- and Subgenera in Zoology from the Tenth Edition of Linnaeus 1758 eoptera Lamellicornia, Fam. Aphodiidae. 110me Fascicule. In: P. to the End of 1935. Vol. 1, A-C. The Zoological Society of London, Wytsman (ed.), Genera Insectorum. Tervueren, 155 pp, 3 pls. ● London, xiv + 957 pp. ● PAULIAN, R. 1942. Exploration du Parc SCHMIDT, A. 1910b. Aphodiinae. Pars 20, Vol. 19(4). In: S. Schenk- National Albert. Mission G. F. de Witte (1933-35). Fasc. 35. Aphodi- ling (ed.), Coleopterorum Catalogus. W. Junk, Berlin, 111 pp. ● inae (Coleoptera Lamellicornia) Fam. Scarabaeidae. Institut des SCHMIDT, A. 1913. Erster Versuch einer Einteilung der exotischen Parcs Nationaux du Congo Belge, 143 pp., 23 pls. ● PETROVITZ, R. Aphodien in Subgenera und als Anhang einige Neubeschreibungen. 1958. Neue afrikanischen Aphodiusarten (Col. Scarab.). Entomolo- Archiv für Naturgeschichte. Abtheilung A, Original-Arbeiten, 79: 117- gische Arbeiten aus dem Museum G. Frey, 9: 140-159. ● 178. ● SCHMIDT, A. 1922. Coleoptera, Aphodiinae. In: C. Apstein PETROVITZ, R. 1962. Neue und verkannte Aphodiinae aus allen (ed.), Das Tierreich. -
A NEW METAZOAN from the MIDDLE CAMBRIAN of UTAH and the NATURE of the VETULICOLIA by DEREK E
[Palaeontology, Vol. 48, Part 4, 2005, pp. 681–686] RAPID COMMUNICATION A NEW METAZOAN FROM THE MIDDLE CAMBRIAN OF UTAH AND THE NATURE OF THE VETULICOLIA by DEREK E. G. BRIGGS*, BRUCES.LIEBERMAN , SUSAN L. HALGEDAHLà and RICHARD D. JARRARDà *Department of Geology and Geophysics, Yale University, PO Box 208109, New Haven, CT 06520-8109, USA; e-mail: [email protected] Department of Geology, University of Kansas, 1475 Jayhawk Boulevard, 120 Lindley Hall, Lawrence, KS 66045, USA àDepartment of Geology and Geophysics, University of Utah, 135 S. 1460 East, Salt Lake City, UT 84112, USA Typescript received 22 November 2004; accepted in revised form 24 March 2005 Abstract: A new metazoan, Skeemella clavula gen. et sp. arthropodan in character. The similarity of this fossil nov., is described from the Middle Cambrian Pierson Cove to vetulicolians throws hypotheses of their deuterostome Formation of the Drum Mountains, Utah, USA. Skeemella affinity into question and highlights their problematic sta- is similar to vetulicolians, but differs from other examples tus. of this group in the relative proportions of the anterior and posterior sections, the large number of divisions, and Key words: vetulicolian, Cambrian, deuterostome, arthro- the elongate bifid termination. The posterior section is pod. The very name vetulicolian conjures up creatures from species Banffia confusa, to erect a new class of stem-group another planet. These extraordinary fossils, with a head arthropods, the Vetulicolida. They argued that Banffia shield-like anterior and narrow segmented trunk-like pos- constricta from the Burgess Shale belongs to the same terior, are the latest Cambrian group to be accorded phy- class, extending its range to North America. -
The Origin and Evolution of Arthropods Graham E
INSIGHT REVIEW NATURE|Vol 457|12 February 2009|doi:10.1038/nature07890 The origin and evolution of arthropods Graham E. Budd1 & Maximilian J. Telford2 The past two decades have witnessed profound changes in our understanding of the evolution of arthropods. Many of these insights derive from the adoption of molecular methods by systematists and developmental biologists, prompting a radical reordering of the relationships among extant arthropod classes and their closest non-arthropod relatives, and shedding light on the developmental basis for the origins of key characteristics. A complementary source of data is the discovery of fossils from several spectacular Cambrian faunas. These fossils form well-characterized groupings, making the broad pattern of Cambrian arthropod systematics increasingly consensual. The arthropods are one of the most familiar and ubiquitous of all ani- Arthropods are monophyletic mal groups. They have far more species than any other phylum, yet Arthropods encompass a great diversity of animal taxa known from the living species are merely the surviving branches of a much greater the Cambrian to the present day. The four living groups — myriapods, diversity of extinct forms. One group of crustacean arthropods, the chelicerates, insects and crustaceans — are known collectively as the barnacles, was studied extensively by Charles Darwin. But the origins Euarthropoda. They are united by a set of distinctive features, most and the evolution of arthropods in general, embedded in what is now notably the clear segmentation of their bodies, a sclerotized cuticle and known as the Cambrian explosion, were a source of considerable con- jointed appendages. Even so, their great diversity has led to consider- cern to him, and he devoted a substantial and anxious section of On able debate over whether they had single (monophyletic) or multiple the Origin of Species1 to discussing this subject: “For instance, I cannot (polyphyletic) origins from a soft-bodied, legless ancestor. -
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 -
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. -
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.