Diversity and Evolution of TIR-Domain-Containing Proteins in Bivalves and Metazoa: New Insights from Comparative Genomics
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New Record of a Primitive Brachiopod Benthic Fauna from the North- East Coast of India
ISSN: 2347-3215 Volume 2 Number 3 (March-2014) pp. 70-73 www.ijcrar.com New record of a primitive brachiopod benthic fauna from the North- East coast of India S.Samanta1*, A.Choudhury2 and S.K.Chakraborty3 1Department of Zoology,Vidyasagar University Midnapore-721102, West Bengal, India 2S.D.Marine Biological Research Institute, Sagar Island, Sundarban, 24 Parganas(S)- 743373.West Bengal, India 3Faculty of Science, Department of Zoology, Vidyasagar University, Midnapore-721102, West Bengal, India *Corresponding author KEYWORDS A B S T R A C T The intertidal belt at the confluence of Subarnarekha estuary, a transboundary Brachiopoda; with Bay of Bengal is an example of physically stressed heterogeneous Lingula anatina; habitats possessing a number of mudflats and sand flats that support the lives Living fossil; of an assemblage of diversified macrobenthic fauna. The Brachiopods West Bengal; (Lampshells) make up a major macrobenthic faunal group in this area which Subarnarekha estuary. includes several morphotypes of Lingula anatina distributed in some restricted areas of the world. The morpho-anatomic study of Lingula anatina- a Precambrian living fossil as a new record from the eastern part of West Bengal has been undertaken in the present study. Introduction The intertidal belt of Midnapore coast, shelled marine animal. About 30000 especially the studied area supports species and 120 genera under the phylum diversified forms of macrobenthic fauna of brachiopoda have been described in a which include good number of fossil record which extends into the lower brachiopodans which has not been reported Cambrian period of which 300 or so earlier from West Bengal coast-Talsari species of brachiopods remain. -
Biogeographical Homogeneity in the Eastern Mediterranean Sea. II
Vol. 19: 75–84, 2013 AQUATIC BIOLOGY Published online September 4 doi: 10.3354/ab00521 Aquat Biol Biogeographical homogeneity in the eastern Mediterranean Sea. II. Temporal variation in Lebanese bivalve biota Fabio Crocetta1,*, Ghazi Bitar2, Helmut Zibrowius3, Marco Oliverio4 1Stazione Zoologica Anton Dohrn, Villa Comunale, 80121, Napoli, Italy 2Department of Natural Sciences, Faculty of Sciences, Lebanese University, Hadath, Lebanon 3Le Corbusier 644, 280 Boulevard Michelet, 13008 Marseille, France 4Dipartimento di Biologia e Biotecnologie ‘Charles Darwin’, University of Rome ‘La Sapienza’, Viale dell’Università 32, 00185 Roma, Italy ABSTRACT: Lebanon (eastern Mediterranean Sea) is an area of particular biogeographic signifi- cance for studying the structure of eastern Mediterranean marine biodiversity and its recent changes. Based on literature records and original samples, we review here the knowledge of the Lebanese marine bivalve biota, tracing its changes during the last 170 yr. The updated checklist of bivalves of Lebanon yielded a total of 114 species (96 native and 18 alien taxa), accounting for ca. 26.5% of the known Mediterranean Bivalvia and thus representing a particularly poor fauna. Analysis of the 21 taxa historically described on Lebanese material only yielded 2 available names. Records of 24 species are new for the Lebanese fauna, and Lioberus ligneus is also a new record for the Mediterranean Sea. Comparisons between molluscan records by past (before 1950) and modern (after 1950) authors revealed temporal variations and qualitative modifications of the Lebanese bivalve fauna, mostly affected by the introduction of Erythraean species. The rate of recording of new alien species (evaluated in decades) revealed later first local arrivals (after 1900) than those observed for other eastern Mediterranean shores, while the peak in records in conjunc- tion with our samplings (1991 to 2010) emphasizes the need for increased field work to monitor their arrival and establishment. -
On the History of the Names Lingula, Anatina, and on the Confusion of the Forms Assigned Them Among the Brachiopoda Christian Emig
On the history of the names Lingula, anatina, and on the confusion of the forms assigned them among the Brachiopoda Christian Emig To cite this version: Christian Emig. On the history of the names Lingula, anatina, and on the confusion of the forms assigned them among the Brachiopoda. Carnets de Geologie, Carnets de Geologie, 2008, CG2008 (A08), pp.1-13. <hal-00346356> HAL Id: hal-00346356 https://hal.archives-ouvertes.fr/hal-00346356 Submitted on 11 Dec 2008 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Carnets de Géologie / Notebooks on Geology - Article 2008/08 (CG2008_A08) On the history of the names Lingula, anatina, and on the confusion of the forms assigned them among the Brachiopoda 1 Christian C. EMIG Abstract: The first descriptions of Lingula were made from then extant specimens by three famous French scientists: BRUGUIÈRE, CUVIER, and LAMARCK. The genus Lingula was created in 1791 (not 1797) by BRUGUIÈRE and in 1801 LAMARCK named the first species L. anatina, which was then studied by CUVIER (1802). In 1812 the first fossil lingulids were discovered in the Mesozoic and Palaeozoic strata of the U.K. -
Palaeoecology of the Arda Biota
Chapter 3 Palaeoecology of the Arda biota Fossil specimens collected in the Arda marine succession are identified and illustrated in this chapter (Crippa & Raineri submitted). Their ecology and palaeoecology is here discussed, focusing the attention on Glycymeris, Aequipecten and Arctica , as they represent the genera whose species have been used for the isotopic analyses; an in depth palaeoecological investigation is in fact important for interpreting the data resulting from the geochemical study. A discussion on the palaeoecological significance of the overall Arda fauna is also reported (Crippa et al., in prep.). 3.1 Faunal composition The fauna is composed by 159 taxa (Table 3.1; Pl. 1-11 at the end of this chapter) coming from 218 fossil beds, of which bivalves are dominant with 105 taxa, followed by gastropods (44 taxa) and a few corals (3 taxa) and serpulids (2 taxa); brachiopods, echinoids, barnacles, bryozoans and scaphopods do also occur in the fauna but they are left in open nomenclature due to their poor state of preservation. Bivalve taxonomy is a complicated topic in constant evolution; as Bieler & Mikkelsen (2006) observed “much of the taxonomic instability in bivalve research is not a result of conflicting hypotheses of relationships, but one of an overabundance of available names” and this is the main problem I dealt with the bivalve identification of the Arda assemblages. According to Jimenez et al. (2009) the status of many genera is still uncertain and species are assigned to different genera depending on the authors; nonetheless, there is certain stability in the species concept that allows adequate classification at the species levels. -
Name-Bearing Fossil Type Specimens and Taxa Named from National Park Service Areas
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 73. 277 NAME-BEARING FOSSIL TYPE SPECIMENS AND TAXA NAMED FROM NATIONAL PARK SERVICE AREAS JUSTIN S. TWEET1, VINCENT L. SANTUCCI2 and H. GREGORY MCDONALD3 1Tweet Paleo-Consulting, 9149 79th Street S., Cottage Grove, MN 55016, -email: [email protected]; 2National Park Service, Geologic Resources Division, 1201 Eye Street, NW, Washington, D.C. 20005, -email: [email protected]; 3Bureau of Land Management, Utah State Office, 440 West 200 South, Suite 500, Salt Lake City, UT 84101: -email: [email protected] Abstract—More than 4850 species, subspecies, and varieties of fossil organisms have been named from specimens found within or potentially within National Park System area boundaries as of the date of this publication. These plants, invertebrates, vertebrates, ichnotaxa, and microfossils represent a diverse collection of organisms in terms of taxonomy, geologic time, and geographic distribution. In terms of the history of American paleontology, the type specimens found within NPS-managed lands, both historically and contemporary, reflect the birth and growth of the science of paleontology in the United States, with many eminent paleontologists among the contributors. Name-bearing type specimens, whether recovered before or after the establishment of a given park, are a notable component of paleontological resources and their documentation is a critical part of the NPS strategy for their management. In this article, name-bearing type specimens of fossil taxa are documented in association with at least 71 NPS administered areas and one former monument, now abolished. -
Paleogeography and History of the Geological Development of the Amazonas Basin 449-502 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1963 Band/Volume: 106 Autor(en)/Author(s): Loczy Louis Artikel/Article: Paleogeography and History of the Geological Development of the Amazonas Basin 449-502 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at 449 Jb. Geol. B. A. Bd. 106 S. 449—502 Wien, Dezember 1963 Paleogeography and History of the Geological Development of the Amazonas Basin By Louis LOCZY (With 3 Tables) Contents *) Page Abstract 449 Introduction 451 I. Sedimentary Evolution of the Lower-, Middle- and Upper Amazonas Trough in Brazil 452 II. Sedimentary Evolution of the Upper Amazonas Subandean Zone 457 1. Territory of Acre (Brazil) 457 2. Northeastern Bolivia, Rio Beni and Caupolican Region 459 3. Eastern Peru—Montana Region 461 4. Eastern Ecuador—El Oriente 464 5. Southeastern Colombia—Putomayo and Caqueta Regions 467 III. Chronology of Geological Events and Paleogeography 469 IV. Tectonic Evolution 489 1. The Amazonas Trough in Brazil 489 2. Tectonic Events in the Subandean Amazonas Area 493 References 494 Abstract The huge Amazonas Basin, a sparsely inhabited and badly accessible jungle area, covering approximately 2,100.000 sq. km., stirs up the common interest at the present time. The petroleum explorations become chiefly conspicuous. The Amazonas Basin can be subdivided into two principal morpho- structural units, which differ clearly by their stratigraphical and structural conditions. There are: I—The Lower, Middle and Upper Amazonas Trough in Brazil, and II—The Subandean Zone of Upper Amazonas. *) Note: The redaction ventures to point out, that editing the above work of Prof. -
Description of the Niagara Quadrangle
DESCRIPTION OF THE NIAGARA QUADRANGLE. By E. M. Kindle and F. B. Taylor.a INTRODUCTION. different altitudes, but as a whole it is distinctly higher than by broad valleys opening northwestward. Across northwestern GENERAL RELATIONS. the surrounding areas and is in general bounded by well-marked Pennsylvania and southwestern New York it is abrupt and escarpments. i nearly straight and its crest is about 1000 feet higher than, and The Niagara quadrangle lies between parallels 43° and 43° In the region of the lower Great Lakes the Glaciated Plains 4 or 5 miles back from the narrow plain bordering Lake Erie. 30' and meridians 78° 30' and 79° and includes the Wilson, province is divided into the Erie, Huron, and Ontario plains From Cattaraugus Creek eastward the scarp is rather less Olcott, Tonawanda, and Lockport 15-minute quadrangles. It and the Laurentian Plateau. (See fig. 2.) The Erie plain abrupt, though higher, and is broken by deep, narrow valleys thus covers one-fourth of a square degree of the earth's sur extending well back into the plateau, so that it appears as a line face, an area, in that latitude, of 870.9 square miles, of which of northward-facing steep-sided promontories jutting out into approximately the northern third, or about 293 square miles, the Erie plain. East of Auburn it merges into the Onondaga lies in Lake Ontario. The map of the Niagara quadrangle shows escarpment. also along its west side a strip from 3 to 6 miles wide comprising The Erie plain extends along the base of the Portage escarp Niagara River and a small area in Canada. -
Mesa Verde National Park Paleontological Resource Inventory (Non-Sensitive Version)
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Mesa Verde National Park Paleontological Resource Inventory (Non-Sensitive Version) Natural Resource Report NPS/MEVE/NRR—2017/1550 ON THE COVER An undescribed chimaera (ratfish) egg capsule of the ichnogenus Chimaerotheca found in the Cliff House Sandstone of Mesa Verde National Park during the work that led to the production of this report. Photograph by: G. William M. Harrison/NPS Photo (Geoscientists-in-the-Parks Intern) Mesa Verde National Park Paleontological Resources Inventory (Non-Sensitive Version) Natural Resource Report NPS/MEVE/NRR—2017/1550 G. William M. Harrison,1 Justin S. Tweet,2 Vincent L. Santucci,3 and George L. San Miguel4 1National Park Service Geoscientists-in-the-Park Program 2788 Ault Park Avenue Cincinnati, Ohio 45208 2National Park Service 9149 79th St. S. Cottage Grove, Minnesota 55016 3National Park Service Geologic Resources Division 1849 “C” Street, NW Washington, D.C. 20240 4National Park Service Mesa Verde National Park PO Box 8 Mesa Verde CO 81330 November 2017 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. -
The Cambrian System in Northwestern Argentina: Stratigraphical and Palaeontological Framework Geologica Acta: an International Earth Science Journal, Vol
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Aceñolaza, G. F. The Cambrian System in Northwestern Argentina: stratigraphical and palaeontological framework Geologica Acta: an international earth science journal, vol. 1, núm. 1, 2003, pp. 23-39 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50510104 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.1, Nº1, 2003, 23-39 Available online at www.geologica-acta.com The Cambrian System in Northwestern Argentina: stratigraphical and palaeontological framework G. F. ACEÑOLAZA INSUGEO – CONICET. Facultad de Ciencias Naturales e I.M.L., Universidad Nacional de Tucumán Miguel Lillo 205, 4000 Tucumán, Argentina. E-mail: [email protected] ABSTRACT Cambrian sequences are widespread in the early Paleozoic of the Central Andean Basin. Siliciclastic sediments dominate these sequences although several minor occurrences of carbonates and volcanic rocks have been observed. The rocks assigned to the Cambrian System in NW Argentina are recognized in the Puna, Eas- tern Cordillera, Subandean Ranges and the Famatina System. This paper gives a general overview of the Cam- brian formations outcropping in the northern provinces of Jujuy, Salta, Tucumán, Catamarca and La Rioja. Spe- cial emphasis has been given to the stratigraphical and biostratigraphical framework of the sequences. Late Precambrian-Early Cambrian thick sedimentary wackes dominate the basal Puncoviscana Formation (s.l.), cha- racterized by a varied ichnofauna that includes the Precambrian-Cambrian transitional levels. -
New Record of a Primitive Brachiopod, Lingula Sp. in Lubuk Damar, Indonesia
BIODIVERSITAS ISSN: 1412-033X Volume 18, Number 4, October 2017 E-ISSN: 2085-4722 Pages: 1438-1444 DOI: 10.13057/biodiv/d180420 Short Communication: New record of a primitive brachiopod, Lingula sp. in Lubuk Damar, Indonesia ANANINGTYAS S. DARMARINI1,♥, YUSLI WARDIATNO2,♥♥, TRI PRARTONO3, KADARWAN SOEWARDI2 1Doctoral Program in Aquatic Resources Management, Graduate School, Institut Pertanian Bogor. Jl. Raya Darmaga, Kampus IPB Darmaga, Bogor 16680, West Java, Indonesia. ♥email: [email protected] 2Department of Aquatic Resources Management, Faculty of Fisheries and Marine Science, Institut Pertanian Bogor. Jl. Raya Darmaga, Kampus IPB Darmaga, Bogor 16680, West Java, Indonesia. Tel./fax.: +62-251-8622932, ♥♥email: [email protected] 3Department of Marine Sciences and Technology, Faculty of Fisheries and Marine Sciences, Institut Pertanian Bogor. Jalan Raya Darmaga, Kampus IPB Darmaga, Bogor 16680, West Java, Indonesia. Manuscript received: 3 May 2017. Revision accepted: 10 September 2017. Abstract. Darmarini AS, Wardiatno Y, Prartono T, Soewardi K. 2017. Short Communication: New record of primitive brachiopod, Lingula sp. in mangrove ecosystem of Lubuk Damar, Aceh Tamiang, Indonesia. Biodiversitas 18: 1438-1444.. This study reports the occurrence of the primitive brachiopod, Lingula in mangrove ecosystem as a new record in Indonesia. Specimens were collected from the mangrove sediment at a depth of between the sediment surface and 20 cm beneath. Lingula has a glossy shell and oval-ovate shell shape. The color of shell is brownish or greenish. In posterior a point where pedicle occurs is found. The pedicle is a prolongation of the body like an anchor, with varying length, rough, hard and striped texture. Pedicle has soft transparent layer and the edges are covered by the substrate. -
Abstract Book
La Troisième Conférence Méditerranéenne de la Biodiversité 2019 Hammamet – Tunisie 1-3 Novembre 2019 SOMMAIRE COMMUNICATIONS ORALES Communication orale N° : 1 .............................................................................................................................. 1 Ecrevisse de Louisiane (Procambarus clarkii Girard, 1852) au Maroc Yahya Ben Yahcoub, Mohammed Fekhaoui, Abdallah El Abidi, Fatima Wariaghli, Ahmed Yahyaoui, . Communication orale N° : 2 .............................................................................................................................. 2 Etude de l’écobiologie en vue de la confirmation de l’installation de Stephanolepis diaspros (Fraser-Brünner, 1940) dans la lagune de Bizerte SAMI MILI, Rym ENNOURI, Basma HABBACHI, Raouia GHANEM, Moez SHAEIK, Dakher TROUDI, . Communication orale N° : 3 .............................................................................................................................. 3 Etude de la diversité du peuplement des coléoptères coprophages dans la région de Rédjas -Mila -Algérie- Mehdi El Aichar, . Communication orale N° : 4 .............................................................................................................................. 4 Expansion du crabe bleu Callinectes sapidus (Rathbun, 1896) dans la région nord de la Tunisie et son premier signalement dans la lagune de Ghar El Melh et la lagune de Bizerte MAROUENE BDIOUI, OLFA BEN ABDALLAH-BEN HADJ HAMIDA, NADER BEN HADJ HAMIDA, HECHMI MISSAOUI, . Communication orale N° : -
Shedding Light: a Phylotranscriptomic Perspective Illuminates the Origin of Photosymbiosis in Marine Bivalves
Shedding light: A phylotranscriptomic perspective illuminates the origin of photosymbiosis in marine bivalves Jingchun Li ( [email protected] ) University of Colorado Boulder https://orcid.org/0000-0001-7947-0950 Sarah Lemer University of Guam Marine Laboratory Lisa Kirkendale Western Australian museum Rüdiger Bieler the Field Museum Colleen Cavanaugh Harvard University Gonzalo Giribet Harvard University Research article Keywords: Photosymbiosis, Tridacinae, Fraginae, Symbiodiniaceae, Reef habitat Posted Date: February 7th, 2020 DOI: https://doi.org/10.21203/rs.2.16100/v2 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published at BMC Evolutionary Biology on May 1st, 2020. See the published version at https://doi.org/10.1186/s12862-020-01614-7. Page 1/34 Abstract Background Photosymbiotic associations between metazoan hosts and photosynthetic dinoagellates are crucial to the trophic and structural integrity of many marine ecosystems, including coral reefs. Although extensive efforts have been devoted to study the short-term ecological interactions between coral hosts and their symbionts, long-term evolutionary dynamics of photosymbiosis in many marine animals are not well understood. Within Bivalvia, the second largest class of mollusks, obligate photosymbiosis is found in two marine lineages: the giant clams (subfamily Tridacninae) and the heart cockles (subfamily Fraginae), both in the family Cardiidae. Morphologically, giant clams show relatively conservative shell forms whereas photosymbiotic fragines exhibit a diverse suite of anatomical adaptations including attened shells, leafy mantle extensions, and lens-like microstructural structures. To date, the phylogenetic relationships between these two subfamilies remain poorly resolved, and it is unclear whether photosymbiosis in cardiids originated once or twice.