Articles and Minimizes the Loss of Material
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
First Application of PDMPO to Examine Silicification in Polycystine Radiolaria
Plankton Benthos Res 4(3): 89–94, 2009 Plankton & Benthos Research © The Plankton Society of Japan First application of PDMPO to examine silicification in polycystine Radiolaria KAORU OGANE1,*, AKIHIRO TUJI2, NORITOSHI SUZUKI1, TOSHIYUKI KURIHARA3 & ATSUSHI MATSUOKA4 1 Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Sendai, 980–8578, Japan 2 Department of Botany, National Museum of Nature and Science, Tsukuba, 305–0005, Japan 3 Graduate School of Science and Technology, Niigata University, Niigata 950–2181, Japan 4 Department of Geology, Faculty of Science, Niigata University, Niigata 950–2181, Japan Received 4 February 2009; Accepted 10 April 2009 Abstract: 2-(4-pyridyl)-5-[(4-(2-dimethylaminoethylaminocarbamoyl)methoxy)-phenyl] oxazole (PDMPO) is a fluo- rescent compound that accumulates in acidic cell compartments. PDMPO is accumulated with silica under acidic con- ditions, and the newly developed silica skeletons show green fluorescent light. This study is the first to use PDMPO in polycystine radiolarians, which are unicellular planktonic protists. We tested Acanthodesmia sp., Rhizosphaera trigo- nacantha, and Spirocyrtis scalaris for emission of green fluorescence. Entire skeletons of Acanthodesmia sp. and Sr. scalaris emitted green fluorescent light, whereas only the outermost shell and radial spines of Rz. trigonacantha showed fluorescence. Two additional species, Spongaster tetras tetras and Rhopalastrum elegans did not show fluorescence. Green fluorescence of the entire skeleton is more like the “skeletal thickening growth” defined by silica deposition throughout the surface of the existing skeleton. The brightness of the fluorescence varied with each cell. This difference in fluorescence may reflect the rate of growth in these cells. Green fluorescence in PDMPO-treated polycystines sug- gests the presence of similar metabolic systems with controlled pH. -
An Evaluated List of Cenozic-Recent Radiolarian Species Names (Polycystinea), Based on Those Used in the DSDP, ODP and IODP Deep-Sea Drilling Programs
Zootaxa 3999 (3): 301–333 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2015 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3999.3.1 http://zoobank.org/urn:lsid:zoobank.org:pub:69B048D3-7189-4DC0-80C0-983565F41C83 An evaluated list of Cenozic-Recent radiolarian species names (Polycystinea), based on those used in the DSDP, ODP and IODP deep-sea drilling programs DAVID LAZARUS1, NORITOSHI SUZUKI2, JEAN-PIERRE CAULET3, CATHERINE NIGRINI4†, IRINA GOLL5, ROBERT GOLL5, JANE K. DOLVEN6, PATRICK DIVER7 & ANNIKA SANFILIPPO8 1Museum für Naturkunde, Invalidenstrasse 43, 10115 Berlin, Germany. E-mail: [email protected] 2Institute of Geology and Paleontology, Tohoku University, Sendai 980-8578 Japan. E-mail: [email protected] 3242 rue de la Fure, Charavines, 38850 France. E-mail: [email protected] 4deceased 5Natural Science Dept, Blinn College, 2423 Blinn Blvd, Bryan, Texas 77805, USA. E-mail: [email protected] 6Minnehallveien 27b, 3290 Stavern, Norway. E-mail: [email protected] 7Divdat Consulting, 1392 Madison 6200, Wesley, Arkansas 72773, USA. E-mail: [email protected] 8Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92093, USA. E-mail: [email protected] Abstract A first reasonably comprehensive evaluated list of radiolarian names in current use is presented, covering Cenozoic fossil to Recent species of the primary fossilising subgroup Polycystinea. It is based on those species names that have appeared in the literature of the Deep Sea Drilling Project and its successor programs, the Ocean Drilling Program and Integrated Ocean Drilling Program, plus additional information from the published literature, and several unpublished taxonomic da- tabase projects. -
Radiozoa (Acantharia, Phaeodaria and Radiolaria) and Heliozoa
MICC16 26/09/2005 12:21 PM Page 188 CHAPTER 16 Radiozoa (Acantharia, Phaeodaria and Radiolaria) and Heliozoa Cavalier-Smith (1987) created the phylum Radiozoa to Radiating outwards from the central capsule are the include the marine zooplankton Acantharia, Phaeodaria pseudopodia, either as thread-like filopodia or as and Radiolaria, united by the presence of a central axopodia, which have a central rod of fibres for rigid- capsule. Only the Radiolaria including the siliceous ity. The ectoplasm typically contains a zone of frothy, Polycystina (which includes the orders Spumellaria gelatinous bubbles, collectively termed the calymma and Nassellaria) and the mixed silica–organic matter and a swarm of yellow symbiotic algae called zooxan- Phaeodaria are preserved in the fossil record. The thellae. The calymma in some spumellarian Radiolaria Acantharia have a skeleton of strontium sulphate can be so extensive as to obscure the skeleton. (i.e. celestine SrSO4). The radiolarians range from the A mineralized skeleton is usually present within the Cambrian and have a virtually global, geographical cell and comprises, in the simplest forms, either radial distribution and a depth range from the photic zone or tangential elements, or both. The radial elements down to the abyssal plains. Radiolarians are most useful consist of loose spicules, external spines or internal for biostratigraphy of Mesozoic and Cenozoic deep sea bars. They may be hollow or solid and serve mainly to sediments and as palaeo-oceanographical indicators. support the axopodia. The tangential elements, where Heliozoa are free-floating protists with roughly present, generally form a porous lattice shell of very spherical shells and thread-like pseudopodia that variable morphology, such as spheres, spindles and extend radially over a delicate silica endoskeleton. -
Order Spumellaria Family Collosphaeridae
Order Spumellaria Family Collosphaeridae Acrosphaera murrayana (Haeckel) (Figure 15.19) [=Polysolenia murrayana]. Large pores, each surrounded by a crown of short spines. Shell diameter: 70-180 µm. Ref: Strelkov and Reshetnjak (1971), Nigrini and Moore (1979). Acrosphaera spinosa (Haeckel) group? (Figure 1D, 15.18) [=Polysolenia spinosa, ?P. lappacea, ?P. flammabunda]. Irregular pores and many irregularly arranged spines scattered about the surface, some of the latter extending from the pore-rims. Spine and pore patterns are variable. Shell diameter: 60-160 µm. Ref: Strelkov and Reshetnjak (1971), Boltovskoy and Riedel (1980). Buccinosphaera invaginata Haeckel (Figure 15.17) [=Collosphaera imvaginata]. The smooth shell produces several pored tubes directed toward the center of the sphere. Rather small, irregular pores. Shell diameter: 100-130 µm. Ref: Strelkov and Reshetnjak (1971), Nigrini (1971). 35 Collosphaera huxleyi Müller (Figure 1E, 15.13). Shells with small to medium-sized pores scattered about the surface only; no spines or tubes. Shell diameter: 80-150 µm. Ref: Strelkov and Reshetnjak (1971), Boltovskoy and Riedel (1980). Collosphaera macropora Popofsky (Figure 15.15). No spines or tubes on shell surface; few very large pores, sometimes angular. Shell diameter: 100-120 µm. Ref: Strelkov and Reshetnjak (1971), Boltovskoy and Riedel (1980). Collosphaera tuberosa Haeckel (Figure 15.14). No spines or tubes on shell surface, but with conspicuous lumps and depressions; many small, irregularly shaped pores. Shell diameter: 50-300 µm. Ref: Strelkov and Reshetnjak (1971), Boltovskoy and Riedel (1980). Siphonosphaera martensi Brandt (Figure 15.20). Each pore bears a short centrifugal tube, tube walls are imperforate. Shell diameter: 90-100 µm. Ref: Strelkov and Reshetnjak (1971). -
Gayana 72(1) 2008.Pmd
Gayana 72(1): 79-93, 2008 ISSN 0717-652X RADIOLARIOS POLYCYSTINA (PROTOZOA: NASSELLARIA Y SPUMELLARIA) SEDIMENTADOS EN LA ZONA CENTRO-SUR DE CHILE (36°- 43° S) POLYCYSTINA RADIOLARIA (PROTOZOA: NASSELLARIA AND SPUMELLARIA) SEDIMENTED IN THE CENTER-SOUTH ZONE OF CHILE (36°- 43° S) Odette Vergara S.1, Margarita Marchant S. M.1 & Susana Giglio2,3 1Departamento de Zoología, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Casilla 160-C, Concepción, Chile, [email protected]. 2Laboratorio de Procesos Oceanográficos y Clima (PROFC), Universidad de Concepción, Casilla 160-C, Concepción, Chile. 3Magíster en Ciencias con mención Oceanografía, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Casilla 160-C, Concepción, Chile. RESUMEN Los radiolarios son protozoos planctónicos marinos, los cuales, a pesar de ser sólo una célula, son sofisticados y complejos organismos. La Subclase Radiolaria está formada por 2 superórdenes: Trypilea y Polycystina, siendo el último el más estudiado, pues su esqueleto de opal es más resistente a la disolución en agua de mar y por ende, más comúnmente preservados en el registro fósil. Los radiolarios han sido usados como una útil herramienta oceanográfica, bioestratigráfica y paleoambiental, gracias a su esqueleto de sílice y a su gran rango geológico. En nuestro país el conocimiento de este grupo es muy escaso, es por esto que el presente trabajo, tiene como principal objetivo, aportar con la identificación y descripción de especies de radiolarios Polycystinos, no antes registrados para esta zona en particular. El material fue recolectado por la Expedición PUCK R/V Sonne Cruise SO-156 Valparaíso-Chiloé-Talcahuano realizada en mayo de 2001. -
Einführung in Das Studium Der Radiolarien
Naturwissenschaftliche Vereinigung Hagen e.V. Mikroskopische Arbeitsgemeinschaft GERHARD GÖKE Einführung in das Studium der Radiolarien Veröffentlichung der NWV-Hagen e.V Sonderheft SH 2 September 1994 Von der MIKRO-HAMBURG mit neuem Layout versehen 2008 2 Gerhard Göke Einführung in das Studium der Radiolarien Präparation und Untersuchungsmethoden Inhaltsverzeichnis Geschichte der Radiolarienforschung 3 Die Radiolarien der Challenger-Expedition 12 Zur Bearbeitung der Barbados-Radiolarien 19 Weichkörper, Fortpflanzung, Ökologie, Bathymetrie 22 Stammesgeschichte, Skelettbau und System 26 Fang und Lebendbeobachtung rezenter Radiolarien 32 Aufbereitung fossiler Radiolarien 33 Die Herstellung von Mikropräparaten: 34 Streupräparate 34 Gelegte Einzelformen 35 Typenplatten und Fundortplatten 35 Auflichtpräparate 36 System der Radiolarien 37 Tafeln 41 3 Geschichte der Radiolarienforschung Bereits in der ersten Hälfte des 19.Jahrhunderts waren Radiolarien bekannt, obgleich man diese Rhizopoden nicht richtig in das zoologische System einord- nen konnte. In der zweiten Hälfte wurden sie dann so intensiv bearbeitet, daß der Umfang der in diesem Zeitabschnitt veröffentlichten Radiolarienliteratur im 20.Jahrhundert nicht mehr erreicht werden konnte. F.MEYEN beobachtete während seiner „Reise um die Erde" (1832 -1834) die ersten lebenden Radiolarien im Meeresplankton (1). Er nannte sie Palmellarien. Seine Beschreibungen von Sphaerozoum fuscum und Physematium atlanticum blieben lange Zeit das Einzige, was man über die Vertreter dieser Tiergruppe wußte. Noch ältere Beobachtungen von Planktonorganismen, die sich mit gro- ßer Wahrscheinlichkeit als Radiolarien deuten lassen, hat CH.G.EHRENBERG in seiner Abhandlung „Über das Leuchten des Meeres“ zitiert (2). Nach seinen Angaben hat der Naturforscher TILESIUS, der KRUSENSTERN in den Jahren 1803 bis 1806 auf seiner Erdumseglung begleitete, in tropischen Meeren bei großer Hitze und anhaltender Windstille „Infusionsthierchen“ beobachtet, die große Ähnlichkeit mit Acanthometren hatten (3). -
The Horizontal Distribution of Siliceous Planktonic Radiolarian Community in the Eastern Indian Ocean
water Article The Horizontal Distribution of Siliceous Planktonic Radiolarian Community in the Eastern Indian Ocean Sonia Munir 1 , John Rogers 2 , Xiaodong Zhang 1,3, Changling Ding 1,4 and Jun Sun 1,5,* 1 Research Centre for Indian Ocean Ecosystem, Tianjin University of Science and Technology, Tianjin 300457, China; [email protected] (S.M.); [email protected] (X.Z.); [email protected] (C.D.) 2 Research School of Earth Sciences, Australian National University, Acton 2601, Australia; [email protected] 3 Department of Ocean Science, Hong Kong University of Science and Technology, Kowloon, Hong Kong 4 College of Biotechnology, Tianjin University of Science and Technology, Tianjin 300457, China 5 College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China * Correspondence: [email protected]; Tel.: +86-606-011-16 Received: 9 October 2020; Accepted: 3 December 2020; Published: 13 December 2020 Abstract: The plankton radiolarian community was investigated in the spring season during the two-month cruise ‘Shiyan1’ (10 April–13 May 2014) in the Eastern Indian Ocean. This is the first comprehensive plankton tow study to be carried out from 44 sampling stations across the entire area (80.00◦–96.10◦ E, 10.08◦ N–6.00◦ S) of the Eastern Indian Ocean. The plankton tow samples were collected from a vertical haul from a depth 200 m to the surface. During the cruise, conductivity–temperature–depth (CTD) measurements were taken of temperature, salinity and chlorophyll a from the surface to 200 m depth. Shannon–Wiener’s diversity index (H’) and the dominance index (Y) were used to analyze community structure. -
First Application of PDMPO to Examine Silicification in Polycystine Radiolaria
Plankton Benthos Res 4(3): 89–94, 2009 Plankton & Benthos Research © The Plankton Society of Japan First application of PDMPO to examine silicification in polycystine Radiolaria KAORU OGANE1,*, AKIHIRO TUJI2, NORITOSHI SUZUKI1, TOSHIYUKI KURIHARA3 & ATSUSHI MATSUOKA4 1 Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Sendai, 980–8578, Japan 2 Department of Botany, National Museum of Nature and Science, Tsukuba, 305–0005, Japan 3 Graduate School of Science and Technology, Niigata University, Niigata 950–2181, Japan 4 Department of Geology, Faculty of Science, Niigata University, Niigata 950–2181, Japan Received 4 February 2009; Accepted 10 April 2009 Abstract: 2-(4-pyridyl)-5-[(4-(2-dimethylaminoethylaminocarbamoyl)methoxy)-phenyl] oxazole (PDMPO) is a fluo- rescent compound that accumulates in acidic cell compartments. PDMPO is accumulated with silica under acidic con- ditions, and the newly developed silica skeletons show green fluorescent light. This study is the first to use PDMPO in polycystine radiolarians, which are unicellular planktonic protists. We tested Acanthodesmia sp., Rhizosphaera trigo- nacantha, and Spirocyrtis scalaris for emission of green fluorescence. Entire skeletons of Acanthodesmia sp. and Sr. scalaris emitted green fluorescent light, whereas only the outermost shell and radial spines of Rz. trigonacantha showed fluorescence. Two additional species, Spongaster tetras tetras and Rhopalastrum elegans did not show fluorescence. Green fluorescence of the entire skeleton is more like the “skeletal thickening growth” defined by silica deposition throughout the surface of the existing skeleton. The brightness of the fluorescence varied with each cell. This difference in fluorescence may reflect the rate of growth in these cells. Green fluorescence in PDMPO-treated polycystines sug- gests the presence of similar metabolic systems with controlled pH. -
1 Flux Variations and Vertical Distributions Of
1 Flux variations and vertical distributions of siliceous Rhizaria (Radiolaria and 2 Phaeodaria) in the western Arctic Ocean: indices of environmental changes 3 4 Takahito Ikenoue a, b, c, *, Kjell R. Bjørklund b, Svetlana B. Kruglikova d, Jonaotaro 5 Onodera c, Katsunori Kimoto c, Naomi Harada c 6 7 a: Department of Earth and Planetary Sciences, Graduate School of Sciences, Kyushu 8 University, 6-10-1 Hakozaki, Higashi-ku, Fukuoka 812-8581, Japan 9 10 b: Natural History Museum, Department of Geology, University of Oslo, P.O. Box 11 1172 Blindern, 0318 Oslo, Norway 12 13 c: Research and Development Center for Global Change, JAMSTEC, Natsushima-cho 14 2-15, Yokosuka, 237-0061, Japan. 15 16 d: P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovsky 17 Prospect 36, 117883 Moscow, Russia 18 19 *Corresponding author; Present address: Central Laboratory, Marine Ecology Research 20 Institute, 300 Iwawada, Onjuku-machi, Isumi-gun, Chiba 299-5105 Japan; E-mail: 21 [email protected] 22 23 Abstract 24 The vertical distribution of radiolarians was investigated using a vertical multiple 25 plankton sampler (100−0, 250−100, 500−250 and 1,000−500 m water depths, 62 µm 26 mesh size) at the Northwind Abyssal Plain and southwestern Canada Basin in 27 September 2013. To investigate seasonal variations in the flux of radiolarians in relation 28 to sea ice and water masses, a time series sediment trap system was moored at Station 29 NAP (75°00'N, 162°00'W, bottom depth 1,975 m) in the western Arctic Ocean during 30 October 2010–September 2012. -
An Evaluated List of Cenozic-Recent Radiolarian Species Names (Polycystinea), Based on Those Used in the DSDP, ODP and IODP Deep-Sea Drilling Programs
Zootaxa 3999 (3): 301–333 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2015 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3999.3.1 http://zoobank.org/urn:lsid:zoobank.org:pub:69B048D3-7189-4DC0-80C0-983565F41C83 An evaluated list of Cenozic-Recent radiolarian species names (Polycystinea), based on those used in the DSDP, ODP and IODP deep-sea drilling programs DAVID LAZARUS1, NORITOSHI SUZUKI2, JEAN-PIERRE CAULET3, CATHERINE NIGRINI4†, IRINA GOLL5, ROBERT GOLL5, JANE K. DOLVEN6, PATRICK DIVER7 & ANNIKA SANFILIPPO8 1Museum für Naturkunde, Invalidenstrasse 43, 10115 Berlin, Germany. E-mail: [email protected] 2Institute of Geology and Paleontology, Tohoku University, Sendai 980-8578 Japan. E-mail: [email protected] 3242 rue de la Fure, Charavines, 38850 France. E-mail: [email protected] 4deceased 5Natural Science Dept, Blinn College, 2423 Blinn Blvd, Bryan, Texas 77805, USA. E-mail: [email protected] 6Minnehallveien 27b, 3290 Stavern, Norway. E-mail: [email protected] 7Divdat Consulting, 1392 Madison 6200, Wesley, Arkansas 72773, USA. E-mail: [email protected] 8Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92093, USA. E-mail: [email protected] Abstract A first reasonably comprehensive evaluated list of radiolarian names in current use is presented, covering Cenozoic fossil to Recent species of the primary fossilising subgroup Polycystinea. It is based on those species names that have appeared in the literature of the Deep Sea Drilling Project and its successor programs, the Ocean Drilling Program and Integrated Ocean Drilling Program, plus additional information from the published literature, and several unpublished taxonomic da- tabase projects. -
Radiolarian Paleontologists
RADI LARIA VOLUME 23 SEPTEMBER 2005 NEWSLETTER OF THE INTERNATIONAL ASSOCIATION OF RADIOLARIAN PALEONTOLOGISTS ISSN: 0297.5270 INTERRAD International Association of Radiolarian Paleontologists A Research Group of the International Paleontological Association Officers of the Association President Past President CHRIS HOLLIS PETER BAUMGARTNER Inst. of Geol. and Nuclear Sciences Lausanne, Switzerland Lower Hutt, New Zealand [email protected] [email protected] Secretary Treasurer GIUSEPPE CORTESE ELSPETH URQUHART Alfred Wegener Institute (AWI) P.O. Box 13697 for Polar and Marine Research Musselburgh – East Lothian P.O.Box 120161 Scotland EH21 8YD 27515 Bremerhaven U.K. Germany Tel: 1-305-361-4668 Tel: (471) 2831 1207 Fax: 1-305-361-4632 Fax: (471) 2831 1149 Email: [email protected] e-mail: [email protected] Working Group Chairmen Paleozoic Cenozoic PATRICIA WHALEN, U.S.A. ANNIKA SANFILIPPO California, U.S.A. [email protected] [email protected] Mesozoic Recent LUIS O’DOGHERTY, Cadiz, SPAIN DEMETRIO BOLTOVSKOY Buenos Aires, ARGENTINA [email protected] [email protected] INTERRAD is an international non-profit organization for researchers interested in all aspects of radiolarian taxonomy, palaeobiology, morphology, biostratigraphy, biology, ecology and paleoecology. INTERRAD is a Research Group of the International Paleontological Association (IPA). Since 1978 members of INTERRAD meet every three years to present papers and exchange ideas and materials. INTERRAD MEMBERSHIP: The international Association of Radiolarian Paleontologists is open to any one interested on receipt of subscription. The actual fee is US $ 15 per year. Membership queries and subscription are sent to the Treasurer. Changes of address can be sent to the Secretary. -
Flux Variations and Vertical Distributions of Siliceous Rhizaria
1 Flux variations and vertical distributions of siliceous Rhizaria (Radiolaria and 2 Phaeodaria) in the western Arctic Ocean: indices of environmental changes 3 4 Takahito Ikenoue a, b, c, *, Kjell R. Bjørklund b, Svetlana B. Kruglikova d, Jonaotaro 5 Onodera c, Katsunori Kimoto c, Naomi Harada c 6 7 a: Department of Earth and Planetary Sciences, Graduate School of Sciences, Kyushu 8 University, 6-10-1 Hakozaki, Higashi-ku, Fukuoka 812-8581, Japan 9 10 b: Natural History Museum, Department of Geology, University of Oslo, P.O. Box 1172 11 Blindern, 0318 Oslo, Norway 12 13 c: Research and Development Center for Global Change, JAMSTEC, Natsushima-cho 14 2-15, Yokosuka, 237-0061, Japan. 15 16 d: P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovsky 17 Prospect 36, 117883 Moscow, Russia 18 19 *Corresponding author; Present address: Central Laboratory, Marine Ecology Research 20 Institute, 300 Iwawada, Onjuku-machi, Isumi-gun, Chiba 299-5105 Japan; E-mail: 21 [email protected] 22 23 Abstract 24 The vertical distribution of radiolarians was investigated using a vertical multiple 25 plankton sampler (100−0, 250−100, 500−250 and 1,000−500 m water depths, 62 µm 26 mesh size) at the Northwind Abyssal Plain and southwestern Canada Basin in 27 September 2013. To investigate seasonal variations in the flux of radiolarians in relation 28 to sea-ice and water masses, a time series sediment trap system was moored at Station 29 NAP (75°00'N, 162°00'W, bottom depth 1,975 m) in the western Arctic Ocean during 30 October 2010–September 2012.