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Optics-Based Surveys of Large Unicellular Zooplankton: a Case Study on Radiolarians and Phaeodarians
Plankton Benthos Res 12(2): 95–103, 2017 Plankton & Benthos Research © The Plankton Society of Japan Optics-based surveys of large unicellular zooplankton: a case study on radiolarians and phaeodarians 1, 2 3 4,5 YASUHIDE NAKAMURA *, REI SOMIYA , NORITOSHI SUZUKI , MITSUKO HIDAKA-UMETSU , 6 4,5 ATSUSHI YAMAGUCHI & DHUGAL J. LINDSAY 1 Department of Botany, National Museum of Nature and Science, Tsukuba 305–0005, Japan 2 Graduate School of Fisheries and Environmental Sciences, Nagasaki University, Nagasaki 852–8521, Japan 3 Department of Earth Science, Graduate School of Science, Tohoku University, Sendai 980–8578, Japan 4 Research and Development (R&D) Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237–0061, Japan 5 School of Marine Biosciences, Kitasato University, Sagamihara 252–0373, Japan 6 Graduate School of Fisheries Sciences, Hokkaido University, Hakodate 041–8611, Japan Received 24 May 2016; Accepted 6 February 2017 Responsible Editor: Akihiro Tuji Abstract: Optics-based surveys for large unicellular zooplankton were carried out in five different oceanic areas. New identification criteria, in which “radiolarian-like plankton” are categorized into nine different groups, are proposed for future optics-based surveys. The autonomous visual plankton recorder (A-VPR) captured 65 images of radiolarians (three orders: Acantharia, Spumellaria and Collodaria) and 117 phaeodarians (four taxa: Aulacanthidae, Phaeosphaeri- da, Tuscaroridae and Coelodendridae). Colonies were observed for one radiolarian order (Collodaria) and three phae- odarian taxa (Phaeosphaerida, Tuscaroridae and Coelodendridae). The rest of the radiolarian orders (Taxopodia and Nassellaria) and the other phaeodarian taxa were not detected because of their small cell size (< ca. -
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. -
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. -
Distribution Patterns of the Radiolarian Nuclei and Symbionts Using DAPI-Fluorescence
Bull. Natl. Mus. Nat. Sci., Ser. B, 35(4), pp. 169–182, December 22, 2009 Distribution Patterns of the Radiolarian Nuclei and Symbionts Using DAPI-Fluorescence Noritoshi Suzuki1*, Kaoru Ogane1,9, Yoshiaki Aita2, Mariko Kato3, Saburo Sakai4, Toshiyuki Kurihara5, Atsushi Matsuoka6, Susumu Ohtsuka7, Akio Go8, Kazumitsu Nakaguchi8, Shuhei Yamaguchi8, Takashi Takahashi7 and Akihiro Tuji9 1 Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aoba 6–3, Aramaki, Aoba-ku, Sendai, 980–8578 Japan 2 Department of Geology, Faculty of Agriculture, Utsunomiya University, Mine-machi 350, Utsunomiya, 321–8505 Japan 3 Plant Science, Graduate School of Agricultural Science, Utsunomiya University, Mine-machi 350, Utsunomiya, 321–8505 Japan 4 Institute of Biogeoscience, JAMSTEC, Natsushima-cho 2–15, Yokosuka, 237–0061 Japan 5 Graduate School of Science and Technology, Niigata University, Niigata, 950–2181 Japan 6 Department of Geology, Faculty of Science, Niigata University, Niigata, 950–2181 Japan 7 Takehara Marine Science Station, Setouchi Field Science Center, Graduate School of Biosphere Science, Hiroshima University, Minato-machi 5–8–1, Takehara, Hiroshima, 725–0024 Japan 8 Faculty of Applied Biological Science, Hiroshima University, Kagamiyama 1–4–4, Higashi-Hiroshima, 739–8528 Japan 9 Department of Botany, National Museum of Nature and Science, Amakubo 4–1–1, Tsukuba, 305–0005 Japan * E-mail: [email protected] Abstract This study is the first report on the successful application of the DAPI (4Ј,6-diamidino- 2-phenylindole) staining technique to 22 families of five of the six radiolarian orders (Acantharia, Collodaria, Nassellaria, Spumellaria, and Taxopodia, excluding Entactinaria). A total of six Acan- tharian species, three Collodarian species, three Spumellarian species, 18 Nassellarian species, and one Taxopod species emitted blue light under epifluorescence microscopy after DAPI staining. -
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. -
Articles and Minimizes the Loss of Material
Clim. Past, 16, 2415–2429, 2020 https://doi.org/10.5194/cp-16-2415-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Technical note: A new automated radiolarian image acquisition, stacking, processing, segmentation and identification workflow Martin Tetard1, Ross Marchant1,a, Giuseppe Cortese2, Yves Gally1, Thibault de Garidel-Thoron1, and Luc Beaufort1 1Aix Marseille Univ, CNRS, IRD, Coll France, INRAE, CEREGE, Aix-en-Provence, France 2GNS Science, Lower Hutt, New Zealand apresent address: School of Electrical Engineering and Robotics, Queensland University of Technology, Brisbane, Australia Correspondence: Martin Tetard ([email protected]) Received: 3 June 2020 – Discussion started: 9 July 2020 Revised: 22 September 2020 – Accepted: 5 October 2020 – Published: 2 December 2020 Abstract. Identification of microfossils is usually done ing, processing, segmentation and recognition, is entirely by expert taxonomists and requires time and a significant automated via a LabVIEW interface, and it takes approx- amount of systematic knowledge developed over many years. imately 1 h per sample. Census data count and classi- These studies require manual identification of numerous fied radiolarian images are then automatically exported and specimens in many samples under a microscope, which is saved. This new workflow paves the way for the analysis very tedious and time-consuming. Furthermore, identifica- of long-term, radiolarian-based palaeoclimatic records from tion may differ between operators, biasing reproducibility. siliceous-remnant-bearing samples. Recent technological advances in image acquisition, pro- cessing and recognition now enable automated procedures for this process, from microscope image acquisition to taxo- nomic identification. 1 Introduction A new workflow has been developed for automated radio- larian image acquisition, stacking, processing, segmentation The term radiolarians currently refers to the polycystine ra- and identification. -
Unveiling the Role of Rhizaria in the Silicon Cycle Natalia Llopis Monferrer
Unveiling the role of Rhizaria in the silicon cycle Natalia Llopis Monferrer To cite this version: Natalia Llopis Monferrer. Unveiling the role of Rhizaria in the silicon cycle. Other. Université de Bretagne occidentale - Brest, 2020. English. NNT : 2020BRES0041. tel-03259625 HAL Id: tel-03259625 https://tel.archives-ouvertes.fr/tel-03259625 Submitted on 14 Jun 2021 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. THESE DE DOCTORAT DE L'UNIVERSITE DE BRETAGNE OCCIDENTALE ECOLE DOCTORALE N° 598 Sciences de la Mer et du littoral Spécialité : Chimie Marine Par Natalia LLOPIS MONFERRER Unveiling the role of Rhizaria in the silicon cycle (Rôle des Rhizaria dans le cycle du silicium) Thèse présentée et soutenue à PLouzané, le 18 septembre 2020 Unité de recherche : Laboratoire de Sciences de l’Environnement Marin Rapporteurs avant soutenance : Diana VARELA Professor, Université de Victoria, Canada Giuseppe CORTESE Senior Scientist, GNS Science, Nouvelle Zélande Composition du Jury : Président : Géraldine SARTHOU Directrice de recherche, CNRS, LEMAR, Brest, France Examinateurs : Diana VARELA Professor, Université de Victoria, Canada Giuseppe CORTESE Senior Scientist, GNS Science, Nouvelle Zélande Colleen DURKIN Research Faculty, Moss Landing Marine Laboratories, Etats Unis Tristan BIARD Maître de Conférences, Université du Littoral Côte d’Opale, France Dir. -
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INDEX* With the exception of Allee el al. (1949) and Sverdrup et at. (1942 or 1946), indexed as such, junior authors are indexed to the page on which the senior author is cited although their names may appear only in the list of references to the chapter concerned; all authors in the annotated bibliographies are indexed directly. Certain variants and equivalents in specific and generic names are indicated without reference to their standing in nomenclature. Ship and expedition names are in small capitals. Attention is called to these subindexes: Intertidal ecology, p. 540; geographical summary of bottom communities, pp. 520-521; marine borers (systematic groups and substances attacked), pp. 1033-1034. Inasmuch as final assembly and collation of the index was done without assistance, errors of omis- sion and commission are those of the editor, for which he prays forgiveness. Abbott, D. P., 1197 Acipenser, 421 Abbs, Cooper, 988 gUldenstUdti, 905 Abe, N.r 1016, 1089, 1120, 1149 ruthenus, 394, 904 Abel, O., 10, 281, 942, 946, 960, 967, 980, 1016 stellatus, 905 Aberystwyth, algae, 1043 Acmaea, 1150 Abestopluma pennatula, 654 limatola, 551, 700, 1148 Abra (= Syndosmya) mitra, 551 alba community, 789 persona, 419 ovata, 846 scabra, 700 Abramis, 867, 868 Acnidosporidia, 418 brama, 795, 904, 905 Acoela, 420 Abundance (Abundanz), 474 Acrhella horrescens, 1096 of vertebrate remains, 968 Acrockordus granulatus, 1215 Abyssal (defined), 21 javanicus, 1215 animals (fig.), 662 Acropora, 437, 615, 618, 622, 627, 1096 clay, 645 acuminata, 619, 622; facing -
6. Neogene and Quaternary Radiolarians from Leg 1251
Fryer, P., Pearce, J. A., Stokking, L. B., et al., 1992 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 125 6. NEOGENE AND QUATERNARY RADIOLARIANS FROM LEG 1251 Yu-jing Wang2 and Qun Yang2 ABSTRACT Radiolarians were recovered from three of the five holes investigated during Leg 125. Relative abundances are estimated at Holes 782A and 784A, where preservation is poor to good. Rare, poorly preserved radiolarians are present in Hole 786A. Seven radiolarian zones are recognized in the latest early- middle Miocene to early Pleistocene of Holes 7 82A and 784A. These zones are approximately correlated to the zones of Sanfilippo and others published in 1985. INTRODUCTION as Dorcadospyris cf. dentata, Lychnocanoma elongata, and Sticho- corys delmontensis. Radiolarians were recovered from three of the five holes inves- tigated during Leg 125. The localities of these Holes are: (Fig. 1): Dorcadospyris alata Zone, Riedel and Sanfilippo, 1970; emend. 1971. The base of this zone is defined by the first appearance of Dor- Hole782A: 30° 51.60^, 141° 18.84'E, cadospyris alata and by the top of the Diartus petterssoni Zone. Hole 784A: 30°54.40'N, 140°44.27'E, and Hole 786A: 31 ° 55X 141 Diartus petterssoni Zone, Riedel and Sanfilippo, 1970; emend. 1978. The base is defined by the earliest morphotypic presence of All holes were drilled at the abyssal depths in the Izu-Bonin Diartus petterssoni and the top by the base of the Didymocyrtis Forearc in the western Pacific Ocean. A total of 97 samples were antepenultima Zone. examined for this study, among which the following listed intervals are barren of radiolarians: Didymocyrtis antepenultima Zone, Riedel and Sanfilippo, 1970; emend. -
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. -
Radiolarian Distribution in Equatorial Pacifie Plankton East
OCEANOLOGICA ACTA 1985 -VOL. 8 - N• 1 ~---- Tropical Pacifie Zooplankton distribution Living radiolaria distribution Radiolarian distribution In East Radiolaria Pacifique tropical Distribution du zooplancton equatorial Pacifie plankton Distribution des radiolaires vivants Radiolaria Demetrio Boltovskoy, Silvia S. Jankilevich Consejo Nacional de Investigaciones Cientificas y Técnicas, Departamento de Ciencias Biol6gicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, 1428 Buenos Aires, Argentina. Received 2/1/84, in revised form 10/5/84, accepted 22/6/84. ABSTRACT On the basis of radiolarian data, four major areas can be recognized in the Eastern equatorial Pacifie Ocean (transected from approximately 9°N, 80°W to 2°N, 140°W to l7°N, 155°W): 1) Between 5°N, 80°W and 2°N, 95°W, with high overall productivity and low radiolarian abundance and diversity; Spongodiscus sp. A, and to a lesser extent D. tetrathalamus, are the dominating taxa in this assemblage. 2) Along the equator, between approximately 95°W and 140°W. The productivity and planktonic standing stock of this area decrease to the west, while its radiolarian diversity and abundance increa.se, as well as the diversity of sorne other zooplankters. This area can be further subdivided into two sections at 124°W, the western one being conspicuously richer both quanti- and qualitatively than the eastern section. 0. stenozona + T. octacantha are characteristic of this area. 3) From approximately 6°N, 138°W to 10°N, 142°W; radiolarian abundance and diversity drop sharply, as weil as overall planktonic productivity and standing stock. 4) From approximately 10°N, 142°W to 17°N, 153°W; there is a further decrease in radiolarian abundance and diversity.