Ground Plan of the Larval Nervous System in Phoronids: Evidence from Larvae of Viviparous Phoronid
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Development, Organization, and Remodeling of Phoronid Muscles from Embryo to Metamorphosis (Lophotrochozoa: Phoronida) Elena N Temereva1,3* and Eugeni B Tsitrin2
Temereva and Tsitrin BMC Developmental Biology 2013, 13:14 http://www.biomedcentral.com/1471-213X/13/14 RESEARCH ARTICLE Open Access Development, organization, and remodeling of phoronid muscles from embryo to metamorphosis (Lophotrochozoa: Phoronida) Elena N Temereva1,3* and Eugeni B Tsitrin2 Abstract Background: The phoronid larva, which is called the actinotrocha, is one of the most remarkable planktotrophic larval types among marine invertebrates. Actinotrochs live in plankton for relatively long periods and undergo catastrophic metamorphosis, in which some parts of the larval body are consumed by the juvenile. The development and organization of the muscular system has never been described in detail for actinotrochs and for other stages in the phoronid life cycle. Results: In Phoronopsis harmeri, muscular elements of the preoral lobe and the collar originate in the mid-gastrula stage from mesodermal cells, which have immigrated from the anterior wall of the archenteron. Muscles of the trunk originate from posterior mesoderm together with the trunk coelom. The organization of the muscular system in phoronid larvae of different species is very complex and consists of 14 groups of muscles. The telotroch constrictor, which holds the telotroch in the larval body during metamorphosis, is described for the first time. This unusual muscle is formed by apical myofilaments of the epidermal cells. Most larval muscles are formed by cells with cross-striated organization of myofibrils. During metamorphosis, most elements of the larval muscular system degenerate, but some of them remain and are integrated into the juvenile musculature. Conclusion: Early steps of phoronid myogenesis reflect the peculiarities of the actinotroch larva: the muscle of the preoral lobe is the first muscle to appear, and it is important for food capture. -
Calcium Carbonate Biomineralisation in Disparate Systems - Common Mechanisms?
England, Jennifer Katherine (2005) Calcium carbonate biomineralisation in disparate systems - common mechanisms? PhD thesis http://theses.gla.ac.uk/4024/ Copyright and moral rights for this thesis are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This thesis cannot be reproduced or quoted extensively from without first obtaining permission in writing from the Author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the Author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Glasgow Theses Service http://theses.gla.ac.uk/ [email protected] Calcium Carbonate Biomineralisation in Disparate Systems - Common Mechanisms? Jennifer Katherine England A thesis submitted for the degree of Doctor of Philosophy Division of Earth Sciences, Centre for Geosciences, University of Glasgow March 2005 © Jennifer England 2005 Abstract Biominerals are composite materials in which orgaruc components control mineral nucleation and structure. Calcium minerals account for over 50% of biominerals, with calcium carbonate being the most common type. This study considers the extent to which four calcium carbonate biomineral systems share common characteristics. Within the sample set, there is a range of ultrastructures and two types of calcium carbonate polymorph (calcite and aragonite). The mini survey includes three invertebrate systems: two members of the Phylum Brachiopoda; the articulated brachiopod Terebratulina retusa (Subphylum Rhynchonelliformea) and the inarticulated brachiopod Novocrania anomala (Subphylum Craniiformea), and a member of the. Mollusca, the bivalve Mytilus edulis. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
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MarLIN Marine Information Network Information on the species and habitats around the coasts and sea of the British Isles Novocrania anomala, Dendrodoa grossularia and Sarcodictyon roseum on variable salinity circalittoral rock MarLIN – Marine Life Information Network Marine Evidence–based Sensitivity Assessment (MarESA) Review John Readman 2016-03-31 A report from: The Marine Life Information Network, Marine Biological Association of the United Kingdom. Please note. This MarESA report is a dated version of the online review. Please refer to the website for the most up-to-date version [https://www.marlin.ac.uk/habitats/detail/264]. All terms and the MarESA methodology are outlined on the website (https://www.marlin.ac.uk) This review can be cited as: Readman, J.A.J., 2016. [Novocrania anomala], [Dendrodoa grossularia] and [Sarcodictyon roseum] on variable salinity circalittoral rock. In Tyler-Walters H. and Hiscock K. (eds) Marine Life Information Network: Biology and Sensitivity Key Information Reviews, [on-line]. Plymouth: Marine Biological Association of the United Kingdom. DOI https://dx.doi.org/10.17031/marlinhab.264.1 The information (TEXT ONLY) provided by the Marine Life Information Network (MarLIN) is licensed under a Creative Commons Attribution-Non-Commercial-Share Alike 2.0 UK: England & Wales License. Note that images and other media featured on this page are each governed by their own terms and conditions and they may or may not be available for reuse. Permissions beyond the scope of this license are available here. Based -
Lithology Could Affect Benthic Communities Living Below Boulders
Journal of the Marine Lithology could affect benthic communities Biological Association of the United Kingdom living below boulders 1 1 2 2 1 cambridge.org/mbi M. Canessa , G. Bavestrello , E. Trainito , A. Navone and R. Cattaneo-Vietti 1Dipartimento di Scienze della Terra dell’Ambiente e della Vita (DISTAV), Università di Genova, Corso Europa, 26 −16132 Genova, Italy and 2Tavolara-Punta Coda Cavallo MPA, Via San Giovanni, 14 – 07026 Olbia, Italy Review Abstract Cite this article: Canessa M, Bavestrello G, Structure and diversity of sessile zoobenthic assemblages seem to be driven not only by chem- Trainito E, Navone A, Cattaneo-Vietti R (2020). ical-physical constraints and biological interactions but also by substrate lithology and its sur- Lithology could affect benthic communities face features. Nevertheless, broadly distributed crustose epilithic corallines could mask the role living below boulders. Journal of the Marine of substrate on animal settling. To evaluate the direct influence of different rocky substrates, Biological Association of the United Kingdom occurrence and coverage of several sessile species, growing on the dark (i.e. coralline-free) face 100, 879–888. https://doi.org/10.1017/ S0025315420000818 of sublittoral limestone and granite boulders were compared in the Tavolara MPA (Mediterranean Sea). The analysis of photographic samples demonstrated significant differ- Received: 9 January 2020 ences in terms of species composition and coverage, according to lithology. Moreover, lime- Revised: 30 July 2020 stone boulders were widely bare, while the cover per cent was almost total on granite. The Accepted: 10 August 2020 First published online: 11 September 2020 leading cause of observed patterns could be the different level of dissolution of the two types of rocks, due to their different mineral composition and textural characteristics. -
Atlantic Area Eunis Habitats Adding New Habitat Types from European Atlantic Coast to the EUNIS Habitat Classification
Atlantic Area Eunis Habitats Adding new habitat types from European Atlantic coast to the EUNIS Habitat Classification MeshAtlantic Technical Report Nº 3/2013 September 2013 Atlantic Area Eunis Habitats Adding new habitat types from European Atlantic coast to the EUNIS Habitat Classification MeshAtlantic Technical Report Nº 3/2013 September 2013 Citation: Monteiro, P., Bentes, L., Oliveira, F., Afonso, C., Rangel, M., Alonso, C., Mentxaka, I., Germán Rodríguez, J., Galparsoro, I., Borja, A., Chacón, D., Sanz Alonso, J.L., Guerra, M.T., Gaudêncio, M.J., Mendes, B., Henriques, V., Bajjouk, T., Bernard, M., Hily, C., Vasquez, M., Populus, J., Gonçalves, J.M.S. (2013). Atlantic Area Eunis Habitats. Adding new habitat types from European Atlantic coast to the EUNIS Habitat Classification. Technical Report No.3/2013 - MeshAtlantic, CCMAR-Universidade do Algarve, Faro, 72 pp.. CONTENTS SUMMARY ............................................................................................................................. 1 INTRODUCTION ..................................................................................................................... 1 OBJECTIVES ................................................................................................................... 1 CASE STUDIES ........................................................................................................................ 2 CASE STUDY 1 Portugal - Algarve ...........................................................................................2 INTRODUCTION -
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. -
2016 North Sea Expedition: PRELIMINARY REPORT
2016 North Sea Expedition: PRELIMINARY REPORT February, 2017 All photos contained in this report are © OCEANA/Juan Cuetos OCEANA ‐ 2016 North Sea Expedition Preliminary Report INDEX 1. INTRODUCTION ..................................................................................................................... 2 1.1 Objective ............................................................................................................................. 3 2. METHODOLOGY .................................................................................................................... 4 3. RESULTS ................................................................................................................................. 6 a. Area 1: Transboundary Area ............................................................................................. 7 b. Area 2: Norwegian trench ............................................................................................... 10 4. ANNEX – PHOTOS ................................................................................................................ 31 1 OCEANA ‐ 2016 North Sea Expedition Preliminary Report 1. INTRODUCTION The North Sea is one of the most productive seas in the world, with a wide range of plankton, fish, seabirds, and organisms that live on the seafloor. It harbours valuable marine ecosystems like cold water reefs and seagrass meadows, and rich marine biodiversity including whales, dolphins, sharks and a wealth of commercial fish species. It is also of high socio‐ -
Embryogenesis and Larval Development of Phoronopsis Harmeri Pixell, 1912 (Phoronida): Dual Origin of the Coelomic Mesoderm
Invertebrate Reproduction and Development, 50:2 (2007) 57–66 57 Balaban, Philadelphia/Rehovot 0168-8170/07/$05.00 © 2007 Balaban Embryogenesis and larval development of Phoronopsis harmeri Pixell, 1912 (Phoronida): dual origin of the coelomic mesoderm ELENA N. TEMEREVA* and VLADIMIR V. MALAKHOV Biological Faculty, Invertebrate Zoology, Moscow State University, Moscow 119992, Russia Tel. and Fax: +8 (495) 939-4495; email: [email protected] Received 12 December 2006; Accepted 26 March 2007 Summary Phoronids are marine invertebrates which great significance from the perspective of comparative anatomy. Phoronids have traditionally been described as deuterostomes because they exhibit developmental and larval traits similar to those traits found in echinoderms and hemichordates. However, molecular phylogenetic evidence has consistently identified the phoronids and brachiopods as a monophyletic group within the lophotrochozoan protostomes. The nature of egg cleavage, gastrulation and the origin of coelomic mesoderm can help to resolve this contradiction. These questions were investigated with Phoronopsis harmeri. Embryos and actinotroch larvae were cultivated in the laboratory, and embryonic and larval development was followed with SEM, light and video microscopy. Egg cleavage is radial, although the furrows of the 4th and succeeding divisions are oblique, which allows for blastula formation by the 16-cell stage. The ciliated blastula hatches 10 h after the onset of cleavage and acquires the apical tuft. Gastrulation proceeds by invagination. Coelomic mesoderm derives from two, the anterior and posterior, precursors. The anterior precursor forms by cell migration from the anterior wall of the archenteron, the posterior one by enterocoelic outpouching of the midgut. The lining of preoral coelom and tentacle coelom is derived from the anterior precursor, whilst the lining of trunk coelom originates from the posterior one. -
Lophotrochozoa, Phoronida): the Evolution of the Phoronid Body Plan and Life Cycle Elena N
Temereva and Malakhov BMC Evolutionary Biology (2015) 15:229 DOI 10.1186/s12862-015-0504-0 RESEARCHARTICLE Open Access Metamorphic remodeling of morphology and the body cavity in Phoronopsis harmeri (Lophotrochozoa, Phoronida): the evolution of the phoronid body plan and life cycle Elena N. Temereva* and Vladimir V. Malakhov Abstract Background: Phoronids undergo a remarkable metamorphosis, in which some parts of the larval body are consumed by the juvenile and the body plan completely changes. According to the only previous hypothesis concerning the evolution of the phoronid body plan, a hypothetical ancestor of phoronids inhabited a U-shaped burrow in soft sediment, where it drew the anterior and posterior parts of the body together and eventually fused them. In the current study, we investigated the metamorphosis of Phoronopsis harmeri with light, electron, and laser confocal microscopy. Results: During metamorphosis, the larval hood is engulfed by the juvenile; the epidermis of the postroral ciliated band is squeezed from the tentacular epidermis and then engulfed; the larval telotroch undergoes cell death and disappears; and the juvenile body forms from the metasomal sack of the larva. The dorsal side of the larva becomes very short, whereas the ventral side becomes very long. The terminal portion of the juvenile body is the ampulla, which can repeatedly increase and decrease in diameter. This flexibility of the ampulla enables the juvenile to dig into the sediment. The large blastocoel of the larval collar gives rise to the lophophoral blood vessels of the juvenile. The dorsal blood vessel of the larva becomes the definitive median blood vessel. -
Phoronis Pallida Class
Phylum: Phoronida Class: Phoronis pallida Order: A lophophorate coelomate Family: Phoronidae Description 1959). Size: one of the smaller phoronids: 15-30 Collar: not present at base of lophophore: ge- mm long (Silen 1954): sp. pallida. Sand cov- nus Phoronis (Zimmer 2007) (figs. 1, 2, 3). ered tube just a little larger (Silen 1952); ex- Lophophore base and trunk demarcation a panded animal can be 25% longer than slight groove; collar, (if present, as in genus tube. Phoronopsis), extends all around trunk. (Do Color: trunk pale, white, posterior end light not confuse anus and nephridiopores on dor- red. Internal organs visible as red (contain sal base of lophophore with a true collar.) hemoglobin (Zimmer and Haderlie 1980). Bulb: (ampulla)-enlarged posterior end (fig. Tentacles white, without pigmented amoebo- 1). cytes: sp. pallida (Silen 1954). Larva opaque Internal Structure: much systematic work yellow, tube yellow to brown-red (from se- based on longitudinal muscle patterns, etc., creted matter) (Silen 1954). not easily studied by casual field worker. P. Trunk: wormlike: unsegmented, smooth and pallida muscles have unusual longitudinal and soft, but faintly annulated (Hyman 1959), no circular patterns, and few bundles of muscles setae - all characteristic of phylum Phoroni- (18-19). Giant nerve fibers found in this phy- da. Can be faintly differentiated into several lum - except in P. ovalis - also vary in size zones: sp. pallida (Silen 1954). Trunk and and number. P. pallida has one giant nerve whole tube curved toward anal side (Silen fiber, on the left side - usual position in phy- 1954) (fig. 6). lum (Emig 1974). Nephridial structure is also Lophophore: a horseshoe-shaped exten- important in systematics. -
Documenting Neotropical Diversity of Phoronids with DNA Barcoding of Planktonic Larvae
Received: 30 April 2018 | Revised: 25 January 2019 | Accepted: 17 February 2019 DOI: 10.1111/ivb.12242 ORIGINAL ARTICLE Documenting neotropical diversity of phoronids with DNA barcoding of planktonic larvae Rachel Collin1 | Dagoberto E. Venera‐Pontón1 | Amy C. Driskell2 | Kenneth S. Macdonald2 | Kit‐Yu Karen Chan3 | Michael J. Boyle4 1Smithsonian Tropical Research Institute, Balboa, Ancon, Panama Abstract 2Laboratories of Analytical Biology, National Phoronid larvae, actinotrochs, are beautiful and complicated organisms which have Museum of Natural History, Smithsonian attracted as much, if not more, attention than their adult forms. We collected acti‐ Institution, Washington, DC 3Division of Life Science, The Hong Kong notrochs from the waters of the Pacific and Caribbean coasts of Panama, and used University of Science and Technology, Clear DNA barcoding of mtCOI, as well as 16S and 18S sequences, to estimate the diversity Water Bay, Hong Kong of phoronids in the region. We discovered three operational taxonomic units (OTUs) 4Smithsonian Marine Station, Fort Pierce, Florida in the Bay of Panama on the Pacific coast and four OTUs in Bocas del Toro on the Caribbean coast. Not only did all OTUs differ from each other by >10% pairwise dis‐ Correspondence Rachel Collin, Smithsonian Tropical tance in COI, but they also differed from all phoronid sequences in GenBank, includ‐ Research, Institute, Unit 9100, Box 0948, ing the four species for which adults have been reported for the Pacific of Panama, DPO AA 34002, USA Email: [email protected] Phoronopsis harmeri, Phoronis psammophila, Phoronis muelleri, and Phoronis hippocre‐ pia. In each ocean region, one common OTU was more abundant and occurred more Present Address Kit‐Yu Karen Chan, Biology frequently than other OTUs in our samples.