Unveiling the Role of Rhizaria in the Silicon Cycle Natalia Llopis Monferrer
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Sodium Silicate Crops
Sodium Silicate Crops 1 Identification of Petitioned Substance 2 3 Chemical Names: CAS Numbers: 4 Sodium Silicate 1344-09-8 5 6 Other Name: Other Codes: 7 Sodium metasilicate; Sodium silicate glass; EPA PC code: 072603 (NLM, 2011a); European 8 Sodium water glass; Silicic acid, sodium salt; Inventory of Existing Commercial Chemical 9 tetrasodium orthosilicate (IPCS, 2004) Substances (EINECS) Number: 215-687-4 (IPCS, 10 2004) 11 Trade Names: 12 Waterglass, Britesil, Sikalon, Silican, Carsil, 13 Dryseq, Sodium siloconate, Star, Soluble glass, 14 Sodium polysilicate (NLM, 2011a), N® - PQ 15 Corporation (OMRI, 2011) 16 Characterization of Petitioned Substance 17 18 Composition of the Substance: 19 The basic formula of sodium silicate is Na2O· nO2Si, which represents the components of silicon dioxide (SiO2) 20 and sodium oxide (Na2O) and the varying ratios of the two in the various formulations. This ratio is commonly 21 called the molar ratio (MR), which can range from 0.5 to 4.0 for sodium silicates and varies depending on the 22 composition of the specific sodium silicate. The structural formulas of these silicates are also variable and can be 23 complex, depending on the formulation, but generally do not have distinct molecular structures (IPCS, 2004). 24 The basic structure of soluble silicates, including sodium and potassium silicates, is a trigonal planar 25 arrangement of oxygen atoms around a central silicon atom, as depicted in Figure 1 below. Physical and 26 chemical properties of sodium silicate are summarized in Table 1, on page 2. 27 28 29 30 31 32 33 34 35 Figure 1: Chemical Structure of Sodium Silicate (NLM, 2011a) 36 37 Specific Uses of the Substance: 38 39 Sodium silicate and other soluble silicates have been used in many industries since the early 19th century. -
Molecular Phylogenetic Position of Hexacontium Pachydermum Jørgensen (Radiolaria)
Marine Micropaleontology 73 (2009) 129–134 Contents lists available at ScienceDirect Marine Micropaleontology journal homepage: www.elsevier.com/locate/marmicro Molecular phylogenetic position of Hexacontium pachydermum Jørgensen (Radiolaria) Tomoko Yuasa a,⁎, Jane K. Dolven b, Kjell R. Bjørklund b, Shigeki Mayama c, Osamu Takahashi a a Department of Astronomy and Earth Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan b Natural History Museum, University of Oslo, P.O. Box 1172, Blindern, 0318 Oslo, Norway c Department of Biology, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan article info abstract Article history: The taxonomic affiliation of Hexacontium pachydermum Jørgensen, specifically whether it belongs to the Received 9 April 2009 order Spumellarida or the order Entactinarida, is a subject of ongoing debate. In this study, we sequenced the Received in revised form 3 August 2009 18S rRNA gene of H. pachydermum and of three spherical spumellarians of Cladococcus viminalis Haeckel, Accepted 7 August 2009 Arachnosphaera myriacantha Haeckel, and Astrosphaera hexagonalis Haeckel. Our molecular phylogenetic analysis revealed that the spumellarian species of C. viminalis, A. myriacantha, and A. hexagonalis form a Keywords: monophyletic group. Moreover, this clade occupies a sister position to the clade comprising the spongodiscid Radiolaria fi Entactinarida spumellarians, coccodiscid spumellarians, and H. pachydermum. This nding is contrary to the results of Spumellarida morphological studies based on internal spicular morphology, placing H. pachydermum in the order Nassellarida Entactinarida, which had been considered to have a common ancestor shared with the nassellarians. 18S rRNA gene © 2009 Elsevier B.V. All rights reserved. Molecular phylogeny. 1. Introduction the order Entactinarida has an inner spicular system homologenous with that of the order Nassellarida. -
Sediment Activity Answer Key
Sediment Activity Answer Key 1. Were your predictions close to where calcareous and siliceous oozes actually occur? Answers vary. 2. How does your map compare with the sediment distribution map? Answers vary. 3. Which type of ooze dominates the ocean sediments, calcareous or siliceous? Why? Calcareous sediments are formed from the remains of organisms like plankton with calcium-based skeletons1, such as foraminifera, while siliceous ooze is formed from the remains of organisms with silica-based skeletons like diatoms or radiolarians. Calcareous ooze dominates ocean sediments. Organisms with calcium-based shells such as foraminifera are abundant and widely distributed throughout the world’s ocean basins –more so than silica-based organisms. Silica-based phytoplankton such as diatoms are more limited in distribution by their (higher) nutrient requirements and temperature ranges. 4. What parts of the ocean do not have calcareous ooze? What might be some reasons for this? Remember that ooze forms when remains of organisms compose more than 30% of the sediment. The edges of ocean basins bordering land tend to have a greater abundance of lithogenous sediment –sediment that is brought into the ocean by water and wind. The proportion of lithogenous sediment decreases however as you move away from the continental shelf. In nutrient rich areas such as upwelling zones in the polar and equatorial regions, silica-based organisms such as diatoms or radiolarians will dominate, making the sediments more likely to be a siliceous-based ooze. Further, factors such as depth, temperature, and pressure can affect the ability of calcium carbonate to dissolve. Areas of the ocean that lie beneath the carbonate compensation depth (CCD), below which calcium carbonate dissolves, typically beneath 4-5 km, will be dominated by siliceous ooze because calcium-carbonate-based material would dissolve in these regions. -
Four Hundred Million Years of Silica Biomineralization in Land Plants
Four hundred million years of silica biomineralization in land plants Elizabeth Trembath-Reicherta,1, Jonathan Paul Wilsonb, Shawn E. McGlynna,c, and Woodward W. Fischera aDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125; bDepartment of Biology, Haverford College, Haverford, PA 19041; and cGraduate School of Science and Engineering, Tokyo Metropolitan University, Hachioji-shi, Tokyo 192-0397, Japan Edited by Thure E. Cerling, University of Utah, Salt Lake City, UT, and approved February 20, 2015 (received for review January 7, 2015) Biomineralization plays a fundamental role in the global silicon Silica is widely used within plants for structural support and cycle. Grasses are known to mobilize significant quantities of Si in pathogen defense (19–21), but it remains a poorly understood the form of silica biominerals and dominate the terrestrial realm aspect of plant biology. Recent work on the angiosperm Oryza today, but they have relatively recent origins and only rose to sativa demonstrated that silica accumulation is facilitated by taxonomic and ecological prominence within the Cenozoic Era. transmembrane proteins expressed in root cells (21–24). Phy- This raises questions regarding when and how the biological silica logenetic analysis revealed that these silicon transport proteins cycle evolved. To address these questions, we examined silica were derived from a diverse family of modified aquaporins that abundances of extant members of early-diverging land plant include arsenite and glycerol transporters (19, 21, 25, 26). A clades, which show that silica biomineralization is widespread different member of this aquaporin family was recently identi- across terrestrial plant linages. Particularly high silica abundances fied that enables silica uptake in the horsetail Equisetum,an are observed in lycophytes and early-diverging ferns. -
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. -
The Planktonic Protist Interactome: Where Do We Stand After a Century of Research?
bioRxiv preprint doi: https://doi.org/10.1101/587352; this version posted May 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Bjorbækmo et al., 23.03.2019 – preprint copy - BioRxiv The planktonic protist interactome: where do we stand after a century of research? Marit F. Markussen Bjorbækmo1*, Andreas Evenstad1* and Line Lieblein Røsæg1*, Anders K. Krabberød1**, and Ramiro Logares2,1** 1 University of Oslo, Department of Biosciences, Section for Genetics and Evolutionary Biology (Evogene), Blindernv. 31, N- 0316 Oslo, Norway 2 Institut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta, 37-49, ES-08003, Barcelona, Catalonia, Spain * The three authors contributed equally ** Corresponding authors: Ramiro Logares: Institute of Marine Sciences (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003, Barcelona, Catalonia, Spain. Phone: 34-93-2309500; Fax: 34-93-2309555. [email protected] Anders K. Krabberød: University of Oslo, Department of Biosciences, Section for Genetics and Evolutionary Biology (Evogene), Blindernv. 31, N-0316 Oslo, Norway. Phone +47 22845986, Fax: +47 22854726. [email protected] Abstract Microbial interactions are crucial for Earth ecosystem function, yet our knowledge about them is limited and has so far mainly existed as scattered records. Here, we have surveyed the literature involving planktonic protist interactions and gathered the information in a manually curated Protist Interaction DAtabase (PIDA). In total, we have registered ~2,500 ecological interactions from ~500 publications, spanning the last 150 years. -
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. -
Rhizaria, Cercozoa)
Protist, Vol. 166, 363–373, July 2015 http://www.elsevier.de/protis Published online date 28 May 2015 ORIGINAL PAPER Molecular Phylogeny of the Widely Distributed Marine Protists, Phaeodaria (Rhizaria, Cercozoa) a,1 a a b Yasuhide Nakamura , Ichiro Imai , Atsushi Yamaguchi , Akihiro Tuji , c d Fabrice Not , and Noritoshi Suzuki a Plankton Laboratory, Graduate School of Fisheries Sciences, Hokkaido University, Hakodate, Hokkaido 041–8611, Japan b Department of Botany, National Museum of Nature and Science, Tsukuba 305–0005, Japan c CNRS, UMR 7144 & Université Pierre et Marie Curie, Station Biologique de Roscoff, Equipe EPPO - Evolution du Plancton et PaléoOcéans, Place Georges Teissier, 29682 Roscoff, France d Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Sendai 980–8578, Japan Submitted January 1, 2015; Accepted May 19, 2015 Monitoring Editor: David Moreira Phaeodarians are a group of widely distributed marine cercozoans. These plankton organisms can exhibit a large biomass in the environment and are supposed to play an important role in marine ecosystems and in material cycles in the ocean. Accurate knowledge of phaeodarian classification is thus necessary to better understand marine biology, however, phylogenetic information on Phaeodaria is limited. The present study analyzed 18S rDNA sequences encompassing all existing phaeodarian orders, to clarify their phylogenetic relationships and improve their taxonomic classification. The mono- phyly of Phaeodaria was confirmed and strongly supported by phylogenetic analysis with a larger data set than in previous studies. The phaeodarian clade contained 11 subclades which generally did not correspond to the families and orders of the current classification system. Two families (Challengeri- idae and Aulosphaeridae) and two orders (Phaeogromida and Phaeocalpida) are possibly polyphyletic or paraphyletic, and consequently the classification needs to be revised at both the family and order levels by integrative taxonomy approaches. -
Dive Into Oceanography with Trusted Content and Innovative Media
Dive into Oceanography with Trusted Content and Innovative Media The best-selling brief book in the oceanography market combines dynamic visuals and a student-friendly narrative to bring oceanography to life and inspire students to engage and learn more about the oceans and environments around them. The 13th edition creates an interactive learning experience, providing tightly integrated text and digital offerings that make oceanography approachable and digestible for students. An emphasis on the process of science throughout the text provides students with an understanding of how scientists think and work. It also helps students develop the scientific skills of devising experiments and interpreting data. A01_TRUJ1521_13_SE_WALK.indd 1 28/11/2018 13:12 Dive into the Process of Science GraphIt! Activities are a great way to help your students develop their understanding of graphs and data. These activities use real data to help students build science literacy skills and their understanding of how to analyze and interpret graphs. 4.5 What Are the Characteristics of Cosmogenous Sediment? 125 PROCESS OF SCIENCE 4.1: extinction, large outpourings of basaltic did not reveal any K–T deposits. Evidently, When The Dinosaurs Died: volcanic rock in India (called the Deccan the impact and resulting huge waves had Traps) and other locations had occurred. stripped the ocean floor of its sediment. The Cretaceous–Tertiary Also, if there was a catastrophic meteor However, at 1600 kilometers (1000 miles) (K–T) Event impact, where was the crater? from the impact site, the telltale sediments In the early 1990s, the 190-kilometer from the catastrophe, such as the iridium- BACKGROUND (120-mile)-wide Chicxulub (pronounced rich clay layer, were preserved in sea floor The extinction of the dinosaurs—and about “SCHICK-sue-lube”) Crater off the Yu- sediments. -
Checklist, Assemblage Composition, and Biogeographic Assessment of Recent Benthic Foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes
Zootaxa 4731 (2): 151–192 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2020 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4731.2.1 http://zoobank.org/urn:lsid:zoobank.org:pub:560FF002-DB8B-405A-8767-09628AEDBF04 Checklist, assemblage composition, and biogeographic assessment of Recent benthic foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes JOACHIM SCHÖNFELD1,3 & JULIA LÜBBERS2 1GEOMAR Helmholtz-Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany 2Institute of Geosciences, Christian-Albrechts-University, Ludewig-Meyn-Straße 14, 24118 Kiel, Germany 3Corresponding author. E-mail: [email protected] Abstract We describe for the first time subtropical intertidal foraminiferal assemblages from beach sands on São Vincente, Cape Verdes. Sixty-five benthic foraminiferal species were recognised, representing 47 genera, 31 families, and 8 superfamilies. Endemic species were not recognised. The new checklist largely extends an earlier record of nine benthic foraminiferal species from fossil carbonate sands on the island. Bolivina striatula, Rosalina vilardeboana and Millettiana milletti dominated the living (rose Bengal stained) fauna, while Elphidium crispum, Amphistegina gibbosa, Quinqueloculina seminulum, Ammonia tepida, Triloculina rotunda and Glabratella patelliformis dominated the dead assemblages. The living fauna lacks species typical for coarse-grained substrates. Instead, there were species that had a planktonic stage in their life cycle. The living fauna therefore received a substantial contribution of floating species and propagules that may have endured a long transport by surface ocean currents. The dead assemblages largely differed from the living fauna and contained redeposited tests deriving from a rhodolith-mollusc carbonate facies at <20 m water depth. -
Predatory Flagellates – the New Recently Discovered Deep Branches of the Eukaryotic Tree and Their Evolutionary and Ecological Significance
Protistology 14 (1), 15–22 (2020) Protistology Predatory flagellates – the new recently discovered deep branches of the eukaryotic tree and their evolutionary and ecological significance Denis V. Tikhonenkov Papanin Institute for Biology of Inland Waters, Russian Academy of Sciences, Borok, 152742, Russia | Submitted March 20, 2020 | Accepted April 6, 2020 | Summary Predatory protists are poorly studied, although they are often representing important deep-branching evolutionary lineages and new eukaryotic supergroups. This short review/opinion paper is inspired by the recent discoveries of various predatory flagellates, which form sister groups of the giant eukaryotic clusters on phylogenetic trees, and illustrate an ancestral state of one or another supergroup of eukaryotes. Here we discuss their evolutionary and ecological relevance and show that the study of such protists may be essential in addressing previously puzzling evolutionary problems, such as the origin of multicellular animals, the plastid spread trajectory, origins of photosynthesis and parasitism, evolution of mitochondrial genomes. Key words: evolution of eukaryotes, heterotrophic flagellates, mitochondrial genome, origin of animals, photosynthesis, predatory protists, tree of life Predatory flagellates and diversity of eu- of the hidden diversity of protists (Moon-van der karyotes Staay et al., 2000; López-García et al., 2001; Edg- comb et al., 2002; Massana et al., 2004; Richards The well-studied multicellular animals, plants and Bass, 2005; Tarbe et al., 2011; de Vargas et al., and fungi immediately come to mind when we hear 2015). In particular, several prevailing and very abun- the term “eukaryotes”. However, these groups of dant ribogroups such as MALV, MAST, MAOP, organisms represent a minority in the real diversity MAFO (marine alveolates, stramenopiles, opistho- of evolutionary lineages of eukaryotes. -
Guidance for Identification and Naming of Substance Under REACH
Guidance for identification and naming of substances under 3 REACH and CLP Version 2.1 - May 2017 GUIDANCE Guidance for identification and naming of substances under REACH and CLP May 2017 Version 2.1 2 Guidance for identification and naming of substances under REACH and CLP Version 2.1 - May 2017 LEGAL NOTICE This document aims to assist users in complying with their obligations under the REACH and CLP regulations. However, users are reminded that the text of the REACH and CLP Regulations is the only authentic legal reference and that the information in this document does not constitute legal advice. Usage of the information remains under the sole responsibility of the user. The European Chemicals Agency does not accept any liability with regard to the use that may be made of the information contained in this document. Guidance for identification and naming of substances under REACH and CLP Reference: ECHA-16-B-37.1-EN Cat. Number: ED-07-18-147-EN-N ISBN: 978-92-9495-711-5 DOI: 10.2823/538683 Publ.date: May 2017 Language: EN © European Chemicals Agency, 2017 If you have any comments in relation to this document please send them (indicating the document reference, issue date, chapter and/or page of the document to which your comment refers) using the Guidance feedback form. The feedback form can be accessed via the EVHA Guidance website or directly via the following link: https://comments.echa.europa.eu/comments_cms/FeedbackGuidance.aspx European Chemicals Agency Mailing address: P.O. Box 400, FI-00121 Helsinki, Finland Visiting address: Annankatu 18, Helsinki, Finland Guidance for identification and naming of substances under 3 REACH and CLP Version 2.1 - May 2017 PREFACE This document describes how to name and identify a substance under REACH and CLP.