Enamel-Like Apatite Crown Covering Amorphous Mineral in a Crayfish Mandible

Total Page:16

File Type:pdf, Size:1020Kb

Enamel-Like Apatite Crown Covering Amorphous Mineral in a Crayfish Mandible ARTICLE Received 11 Nov 2011 | Accepted 11 Apr 2012 | Published 15 May 2012 DOI: 10.1038/ncomms1839 Enamel-like apatite crown covering amorphous mineral in a crayfish mandible Shmuel Bentov1,2, Paul Zaslansky3,†, Ali Al-Sawalmih3, Admir Masic3, Peter Fratzl3, Amir Sagi2,4, Amir Berman1,4,5 & Barbara Aichmayer3 Carbonated hydroxyapatite is the mineral found in vertebrate bones and teeth, whereas invertebrates utilize calcium carbonate in their mineralized organs. In particular, stable amorphous calcium carbonate is found in many crustaceans. Here we report on an unusual, crystalline enamel-like apatite layer found in the mandibles of the arthropod Cherax quadricarinatus (freshwater crayfish). Despite their very different thermodynamic stabilities, amorphous calcium carbonate, amorphous calcium phosphate, calcite and fluorapatite coexist in well-defined functional layers in close proximity within the mandible. The softer amorphous minerals are found primarily in the bulk of the mandible whereas apatite, the harder and less soluble mineral, forms a wear-resistant, enamel-like coating of the molar tooth. Our findings suggest a unique case of convergent evolution, where similar functional challenges of mastication led to independent developments of structurally and mechanically similar, apatite-based layers in the teeth of genetically remote phyla: vertebrates and crustaceans. 1 Department of Biotechnological Engineering, Ben-Gurion University, 84105 Beer-Sheva, Israel. 2 Department of Life Sciences, Ben-Gurion University, 84105 Beer-Sheva, Israel. 3 Max Planck Institute of Colloids and Interfaces, Department of Biomaterials, Research Campus Golm, 14424 Potsdam, Germany. 4 National Institute for Biotechnology in the Negev, Ben-Gurion University, 84105 Beer-Sheva, Israel. 5 Ilse Katz Institute for Nanoscale Science and Technology, Ben-Gurion University, 84105 Beer-Sheva, Israel. †Present address: Julius Wolff Institute and Centre for Musculoskeletal Surgery, Charité - Universitätsmedizin Berlin, 13353 Berlin, Germany. Correspondence and requests for materials should be addressed to A.B. (e-mail: [email protected]) or to B.A. (e-mail: [email protected]). NATURE COMMUNICATIONS | 3:839 | DOI: 10.1038/ncomms1839 | www.nature.com/naturecommunications © 2012 Macmillan Publishers Limited. All rights reserved. ARTICLE NatUre cOMMUNicatiONS | DOI: 10.1038/ncomms1839 eeth are exposed to considerable abrasion and mechanical a d stresses. The structure, mineralogy and composition of these PO3− CO2− Tmastication tools are intimately linked to feeding habits and 4 3 are subject to evolutionary selective pressures. As a result, teeth are usually the hardest parts of the body, with superior wear-resistance and biomechanical toughness. Typically, a tooth can be divided into b three structurally important components: a hard and wear-resist- Intensity (a.u.) 1 3 ant working part, a softer supporting ‘cushion’ that can withstand 2 the impacting, compressive or tensile stresses and a hard–soft inter- 3 2 face that is usually mechanically graded to minimize interfacial 200 400 600 800 1,000 1,200 1 stresses1–3. Diverse examples for the formation of this tri-element Raman shift (cm−1) tooth structural approach are known. Among the mollusks, chitons e (Polyplacophora) use iron oxide (magnetite)4,5 along with calcium phosphate mineral6 in their teeth while limpets (Gastropoda) form c iron oxide (goethite) and silica-laden teeth7. The better-known cal- 1 cium phosphate (hydroxyapatite)-based mammalian teeth, where 2 a hard enamel layer covers a softer bulk of dentin to form highly 1 2 efficient cutting and grinding tools3 are of course a benchmark ref- erence for teeth structure. Another interesting example are the self- 3 3 sharpening sea urchin (Echinoidea) teeth with grinding tips that are made of calcite reinforced with high content of magnesium ions, Figure 1 | Distribution of different minerals in the mandible. (a) Schematic 8,9 to a level close to dolomite . Common to all these teeth types is representation of the crayfish C.( quadricarinatus), red arrow indicating the the choice, or compositional modification of minerals for increased position of the oral opening. (b) Ventral view of the mandible and the oral 8 hardness of the working surface and the exquisite control of their opening showing the basal segment (1), the anterior molar (2) and the location and ultrastructural organization. The latter is often char- outer incisor (3). Scale bar, 5 mm. (c) Detailed view of an isolated mandible. acterized by fibrillar or elongated needle structures oriented per- The coloured points indicate positions where Raman spectra (shown in d) pendicular to the load bearing direction. Various designs are also were measured. Scale bar, 2 mm. (d) Chemical analysis of the mandible by found in the interfaces between the hard cover and the underlying Raman spectroscopy reveals the coexistence of amorphous carbonate and softer support layer. A well-known example is the mammalian den- phosphate in the basal segment (blue, broadened peaks), apatite in the molar tin–enamel junction, a distinct layer that prevents crack propaga- (red) and calcite in the incisor (green). The calcite is located beneath the 10,11 tion from enamel into dentin . An interesting alternative to all brown chitinous cover of the incisor whereas the molar apatite is exposed. these highly mineralized teeth are the sclerotized teeth of Polychaete The main mode (ν ) of carbonate and phosphate are indicated. (e) Micro- 12,13 1 worms, where the use of mineral (copper biominerals) is sparse CT image of the mandible showing higher density of the molar tooth due and non-mineralized zinc and copper serve to crosslink and harden to increased attenuation (brighter regions) of the molar with respect to the 13,14 a proteinaceous matrix rich in histidine . basal segment and anterior incisor. The scale bar corresponds to 1 mm. In the current study, we investigate the mandible of the arthropod Cherax quadricarinatus (freshwater crayfish). In crustaceans, the mandibles are part of the exoskeleton and are periodically removed which serves for grabbing and holding food20 (Fig. 1b). The and regenerated during each molting cycle that may occur every anterior molar ridge of C. quadricarinatus contains a large tooth few days in early growth stages15. In contrast to mammalian bone that is distinct from the rest of the mandible in both colour and and dentin, which are collagen-based tissues with embedded car- form (Fig. 1c). Raman spectroscopy (Fig. 1d) revealed that the bonated hydroxyapatite crystals, the exoskeletons of crustaceans are mandible contains four different minerals: ACC and amorphous chitin-based and commonly reinforced with calcium carbonate16. calcium phosphate (ACP) in the base of the mandible, calcite in the The cuticle of C. quadricarinatus is known to contain amorphous incisor and, most surprisingly, FAP in the anterior molar. Figure calcium carbonate (ACC)15,17, which can be easily dissolved before 1e shows an X-ray tomography reconstruction of such a mandible. the molting as compared with its crystalline polymorphs15,18. We The significantly higher density of the molar (due to higher X-ray found that the mandibles of the freshwater crayfish contain more attenuation) corresponds to the bright appearance of the tissues than only ACC mineral. They are in part covered by a layer of flu- observed in Fig. 1c. orapatite (FAP) crystals, reminiscent of the hydroxyapatite-based enamel found in vertebrate teeth. We studied the crayfish mandibles The microstructure of the molar tooth. Phase contrast-enhanced on various length-scales and discovered that the complex functional synchrotron-based X-ray microtomography revealed the 3D inter- tooth structure is quickly grown by carefully combining amorphous nal microstructure of the molar (Fig. 2a), combining the effects of and crystalline minerals. The appearance of an enamel-like apatite density variations with contrast arising because of the diffraction of layer and similarities in the investigated mechanical properties of X-rays at interfaces within the specimen21. A virtual slice through the molar crayfish tooth and mammalian teeth suggest a unique the tomogram of a water-immersed typical tooth (Fig. 2a) highlights case of convergent evolution. Similar functional challenges of need- two different zones, namely the apatite high-density mineral layer ing to grind food, led to remarkably similar solutions that appeared (light grey, to the right) and the base of the mandible (medium grey, independently in genetically remote phyla: the vertebrates and this centre), consisting of lower-density chitin and amorphous mineral. ancient group of arthropods19. The outermost grinding surface is found on the right hand side of the image (delineated by the white–black line caused by X-ray Results interference effect). The apatite layer contains an array of parallel Four different minerals found in the mandible. In crayfish, the channels arranged normal to the outer surface, in a radial direc- mandibles form the anterior mouthparts, located directly in front tion. These channels are similar and analogous to the crustacean of the oral opening (Fig. 1a). The mandibles consist of a large base, cuticular pore canal system that is formed by cellular extensions of capped with two protuberances: the molar ridge, which serves as a the epithelial cells22. The channels cross the cuticular ‘basal layer’, massive grinding surface for mastication, and the incisor process, running
Recommended publications
  • Download PDF About Minerals Sorted by Mineral Name
    MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky.
    [Show full text]
  • MINERALIZATION in the GOLD HILL MINING DISTRICT, TOOELE COUNTY, UTAH by H
    MINERALIZATION IN THE GOLD HILL MINING DISTRICT, TOOELE COUNTY, UTAH by H. M. EI-Shatoury and J. A. Whelan UTAH GEOLOGICAL AND MINERALOGIC~4L SURVEY affiliated with THE COLLEGE OF MINES AND MINERAL INDUSTRIES University of Utah~ Salt Lake City~ Utah Bulletin 83 Price $2.25 March 1970 CONTENTS Page ABSTRACT. • • . • . • . • . • • . • . • . • • • . • • . • . • .. 5 INTRODUCTION 5 GENERAL GEOLOGY. .. 7 ECONOMIC GEOLOGY. 7 Contact Metasomatic Deposits. 11 Veins. • . 11 Quartz-Carbonate-Adularia Veins 11 Quartz Veins . 15 Calcite Veins. 15 Replacement Deposits . 15 Replacement Deposits in the Ochre Mountain Limestone 15 Replacement Deposits in the Quartz Monzonite 17 HYDROTHERMAL ALTERATION. 17 Alteration of Quartz Monzonite. • 17 Alteration of Limestones. 22 Alteration of the Manning Canyon Formation 23 Alteration of the Quartzite. 23 Alteration of Volcanic Rocks. 23 Alteration of Dike Rocks. 23 Alteration of Quartz-Carbonate Veins . 23 OXIDATION OF ORES. 23 Oxidation of the Copper-Lead-Arsenic-Zinc Replacement Deposits 24 Oxidation of Tungsten and Molybdenum Deposits. 24 Oxidation of the Lead-Zinc Deposits 25 MINERALOGY. 25 CONTROLS OF MINERAL LOCALIZATION 25 ZONAL ARRANGEMENT OF ORE DEPOSITS. 25 GENESIS OF ORE DEPOSITS. 29 DESCRIPTION OF PROPERTIES. 29 The Alvarado Mine. 29 The Cane Spring Mine 30 The Bonnemort Mine 32 The Rube Gold Mine . 32 The Frankie Mine 32 The Yellow Hammer Mine 33 The Rube Lead Mine . 34 FUTURE OF THE DISTRICT AND RECOMMENDATIONS. .. 34 ACKNOWLEDGMENTS. .. 36 REFERENCES. • . .. 36 2 ILLUSTRATIONS Page Frontis piece Figure I. Index map showing location and accessibility to the Gold Hill mining district, Utah . 4 2. Geologic map of Rodenhouse Wash area, showing occurrence of berylliferous quartz-carbonate-adularia veins and sample locations.
    [Show full text]
  • ADA Fluoridation Facts 2018
    Fluoridation Facts Dedication This 2018 edition of Fluoridation Facts is dedicated to Dr. Ernest Newbrun, respected researcher, esteemed educator, inspiring mentor and tireless advocate for community water fluoridation. About Fluoridation Facts Fluoridation Facts contains answers to frequently asked questions regarding community water fluoridation. A number of these questions are responses to myths and misconceptions advanced by a small faction opposed to water fluoridation. The answers to the questions that appear in Fluoridation Facts are based on generally accepted, peer-reviewed, scientific evidence. They are offered to assist policy makers and the general public in making informed decisions. The answers are supported by over 400 credible scientific articles, as referenced within the document. It is hoped that decision makers will make sound choices based on this body of generally accepted, peer-reviewed science. Acknowledgments This publication was developed by the National Fluoridation Advisory Committee (NFAC) of the American Dental Association (ADA) Council on Advocacy for Access and Prevention (CAAP). NFAC members participating in the development of the publication included Valerie Peckosh, DMD, chair; Robert Crawford, DDS; Jay Kumar, DDS, MPH; Steven Levy, DDS, MPH; E. Angeles Martinez Mier, DDS, MSD, PhD; Howard Pollick, BDS, MPH; Brittany Seymour, DDS, MPH and Leon Stanislav, DDS. Principal CAAP staff contributions to this edition of Fluoridation Facts were made by: Jane S. McGinley, RDH, MBA, Manager, Fluoridation and Preventive Health Activities; Sharon (Sharee) R. Clough, RDH, MS Ed Manager, Preventive Health Activities and Carlos Jones, Coordinator, Action for Dental Health. Other significant staff contributors included Paul O’Connor, Senior Legislative Liaison, Department of State Government Affairs.
    [Show full text]
  • Tungsten Minerals and Deposits
    DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 652 4"^ TUNGSTEN MINERALS AND DEPOSITS BY FRANK L. HESS WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Page. Introduction.............................................................. , 7 Inquiries concerning tungsten......................................... 7 Survey publications on tungsten........................................ 7 Scope of this report.................................................... 9 Technical terms...................................................... 9 Tungsten................................................................. H Characteristics and properties........................................... n Uses................................................................. 15 Forms in which tungsten is found...................................... 18 Tungsten minerals........................................................ 19 Chemical and physical features......................................... 19 The wolframites...................................................... 21 Composition...................................................... 21 Ferberite......................................................... 22 Physical features.............................................. 22 Minerals of similar appearance.................................
    [Show full text]
  • Preparation and Solubility of Hydroxyapatite
    JOURNAL O F RESEARC H of the National Bureau of Standards - A. Ph ys ics a nd Chemistry Vol. 72A, No. 6, N ovember- December 1968 Preparation and Solubility of Hydroxyapatite E. C. Moreno,* T. M. Gregory,* and W. E. Brown* Institute for Basic Standards, National Bureau of Standards, Washington, D.C. 20234 (August 2, 1968) Two portions of a syntheti c hydroxyapatite (HA), Ca" OH(PO'}J, full y characterized by x-ray, infrared, petrographi c, and chemi cal anal yses, were heated at 1,000 °C in air and steam atmospheres, respectively. Solubility isotherms for these two samples in the syste m Ca(OH}2 -H3PO,-H20 were determined in the pH range 5 to 7 by equilibrating the solids with dilute H3 PO. solutions. Both sam­ ples of HA disso lved stoichiometrically. The activity products (Ca + +)'( OH - ) (pO~f' and their standard errors-obtained by a least squares adjustment of the measurements (Ca and P concentrations and pH of the saturated solutions) subject to the conditions of electroneutralit y, constancy of the activity product, and stoichiometric dissolution - were 3.73 ± 0.5 x 10- 58 for the steam-h eated HA and 2_5, ± 0.4 x 10- 55 for the air-heated HA. Allowance was made in the calculations for the presence of the ion pairs [CaHPO. lo and [CaH2P04 1+ The hi gher solubility product for the air-heated HA is as­ cribed either to a change in the heat of formation brought about by partial dehydration or to a state of fine subdivision resulting from a disproportionation reacti on_ The solubility product constant s were used to cal culate the points of intersection (i.e_, sin gular points) of the two HA solubility isot herms with the isotherms of CaHPO.
    [Show full text]
  • Minerals Found in Michigan Listed by County
    Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee,
    [Show full text]
  • Scheelite Cawo4 C 2001-2005 Mineral Data Publishing, Version 1
    Scheelite CaWO4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m. Crystals are typically pseudo-octahedral {011} or {112}, with modifying forms {001}, {013}, {121}, several others, to 32 cm; commonly granular, massive. Twinning: {110}, common, penetration and contact twins, composition plane {110} or {001}. Physical Properties: Cleavage: On {101}, distinct; on {112}, interrupted; on {001}, indistinct. Hardness = 4.5–5 D(meas.) = 6.10(2) D(calc.) = 6.09 Bright bluish white cathodoluminescence and fluorescence under SW UV and X-rays. Optical Properties: Transparent to opaque; transparent in transmitted light. Color: Colorless, white, gray, brown, pale yellow, yellow-orange, pale shades of orange, red, green; may be compositionally color zoned. Streak: White. Luster: Vitreous to adamantine. Optical Class: Uniaxial (+). = 1.935–1.938 ω = 1.918–1.921 Cell Data: Space Group: I41/a (synthetic). a = 5.2429(3) c = 11.3737(6) Z = 4 X-ray Powder Pattern: Kernville, California, USA. 3.10 (100), 4.76 (55), 3.072 (30), 1.928 (30), 1.592 (30), 2.622 (25), 2.296 (20) Chemistry: (1) (2) WO3 80.17 80.52 MoO3 0.07 MgO trace CaO 19.49 19.48 Total 99.73 100.00 (1) Schwarzenberg, Germany. (2) CaWO4. Polymorphism & Series: Forms a series with powellite. Occurrence: Typically a component of contact-metamorphic tactite; in high-temperature hydrothermal veins and greisen; less common in granite pegmatites and medium-temperature hydrothermal veins; alluvial. Association: Cassiterite, wolframite, topaz, fluorite, apatite, tourmaline, quartz (greisen); grossular–andradite, diopside, vesuvianite, tremolite (tactite). Distribution: An important ore of tungsten, with many localities.
    [Show full text]
  • Development of a New Approach to Diagnosis of the Early Fluorosis
    www.nature.com/scientificreports OPEN Development of a new approach to diagnosis of the early fuorosis forms by means of FTIR and Raman microspectroscopy Pavel Seredin1,2*, Dmitry Goloshchapov1, Yuri Ippolitov3 & Jitraporn Vongsvivut4 This study is aimed at investigating the features of mineralization of the enamel apatite at initial stages of fuorosis development. Samples of teeth with intact and fuorotic enamel in an early stage of the disease development (Thylstrup–Fejerskov Index = 1–3) were studied by Raman scattering and FTIR using Infrared Microspectroscopy beamline at Australian Synchrotron equipment. Based on the data obtained by optical microspectroscopy and calculation of the coefcient R [A-type/B-type], 2− which represents the ratio of carbonation fraction of CO3 , replacing phosphate or hydroxyl radicals in the enamel apatite lattice, the features of mineralization of enamel apatite in the initial stages of development of the pathology caused by an increased content of fuorine in the oral cavity were established. Statistical analysis of the data showed signifcant diferences in the mean values of R [A-type/B-type] ratio between the control and experimental groups for surface layers (p < 0.01). The data obtained are potentially signifcant as benchmarks in the development of a new approach to preventive diagnostics of the development of initial and clinically unregistered stages of human teeth fuorosis, as well as personalized control of the use of fuoride-containing caries-preventive agents. It has been established that caries prevalence is associated with the intake of fuorine compounds 1,2, that is, the less fuoride, the higher is caries frequency3,4.
    [Show full text]
  • Preparation of Fluoride Substituted Apatite Cements As the Building
    G Model APSUSC-21728; No. of Pages 6 ARTICLE IN PRESS Applied Surface Science xxx (2011) xxx–xxx Contents lists available at ScienceDirect Applied Surface Science journal homepage: www.elsevier.com/locate/apsusc Preparation of fluoride substituted apatite cements as the building blocks for tooth enamel restoration Jie Wei a,b, Jiecheng Wang a, Xiaochen Liu a, Jian Ma c, Changsheng Liu b, Jing Fang a,∗, Shicheng Wei a,d,∗∗ a Center for Biomedical Materials and Tissue Engineering, Academy for Advanced Inter-disciplinary Studies, Peking University, Beijing 100871, PR China b Key Laboratory for Ultrafine Materials of Ministry of Education, East China University of Science and Technology, Shanghai 200237, PR China c Hospital of Stomatology, Tongji University, Shanghai 200072, PR China d School and Hospital of Stomatology, Peking University, Beijing 100081, PR China article info abstract Article history: Fluoride substituted apatite cement (fs-AC) was synthesized by using the cement powders of tetracal- Received 31 January 2011 cium phosphate (TTCP) and sodium fluoride (NaF), and the cement powders were mixed with diluted Received in revised form 12 April 2011 phosphoric acid (H3PO4) as cement liquid to form fs-AC paste. The fs-AC paste could be directly filled Accepted 12 April 2011 into the carious cavities to repair damaged dental enamel. The results indicated that the fs-AC paste Available online xxx was changed into fluorapatite crystals with the atom molar ratio for calcium to phosphorus of 1.66 and the F ion amount of 3 wt% after self-hardening for 2 days. The solubility of fs-AC in Tris–HCl solution Keywords: (pH 6) was slightly lower than hydroxyapatite cement (HAC) that was similar to the apatite in enamel, Dental enamel Carious cavities indicating the fs-AC was much insensitive to the weakly acidic solution than the apatite in enamel.
    [Show full text]
  • A Mineralogical Perspective on the Apatite in Bone
    Materials Science and Engineering C 25 (2005) 131–143 www.elsevier.com/locate/msec A mineralogical perspective on the apatite in bone Brigitte WopenkaT, Jill D. Pasteris Department of Earth and Planetary Sciences, One Brookings Drive, Campus Box 1169, Washington University, St. Louis, MO 63130, USA Available online 19 March 2005 Abstract A crystalline solid that is a special form of the mineral apatite dominates the composite material bone. A mineral represents the intimate linkage of a three-dimensional atomic structure with a chemical composition, each of which can vary slightly, but not independently. The specific compositional–structural linkage of a mineral influences its chemical and physical properties, such as solubility, density, hardness, and growth morphology. In this paper, we show how a mineralogic approach to bone can provide insights into the resorption–precipitation processes of bone development, the exceedingly small size of bone crystallites, and the body’s ability to (bio)chemically control the properties of bone. We also discuss why the apatite phase in bone should not be called hydroxylapatite, as well as the limitations to the use of the stoichiometric mineral hydroxylapatite as a mineral model for the inorganic phase in bone. This mineralogic approach can aid in the development of functionally specific biomaterials. D 2005 Elsevier B.V. All rights reserved. Keywords: Calcium phosphates; Bioapatite; Biominerals; Mineralogy; Crystalline structure; Raman spectroscopy 1. Introduction chemical substitutions. Such substitutions slightly change the structure of a mineral and often have critical effects on The major constituent of bone is a calcium phosphate mineral properties, such as solubility, hardness, brittleness, mineral that is similar in composition and structure to strain, thermal stability, and optical properties like bire- minerals within the apatite group, which form naturally in fringence [1,2].
    [Show full text]
  • Geochemistry and Origin of Scheelites from the Xiaoyao Tungsten Skarn Deposit in the Jiangnan Tungsten Belt, SE China
    minerals Article Geochemistry and Origin of Scheelites from the Xiaoyao Tungsten Skarn Deposit in the Jiangnan Tungsten Belt, SE China Qiangwei Su 1,*, Jingwen Mao 1, Jia Sun 1, Linghao Zhao 2 and Shengfa Xu 3 1 MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; [email protected] (J.M.); [email protected] (J.S.) 2 National Research Centre for Geoanalysis, Beijing 100037, China; [email protected] 3 332 Geological Team of Anhui Bureau of Geology and Mineral Resources, Huangshan 245000, China; [email protected] * Correspondence: [email protected] Received: 13 January 2020; Accepted: 11 March 2020; Published: 18 March 2020 Abstract: The type, association, variations, and valence states of several metal elements of scheelite can trace the source and evolution of the ore-forming fluids. There are four types of scheelite from the Xiaoyao deposit: (1) scheelite intergrown with garnet in the proximal zone (Sch1a) and with pyroxene in the distal zone (Sch1b), (2) scheelite replaced Sch1a (Sch2a) and crystallized as rims around Sch1b (Sch2b), (3) quartz vein scheelite with oscillatory zoning (Sch3), and 4) scheelite (Sch4) within micro-fractures of Sch3. Substitutions involving Mo and Cd are of particular relevance, and both elements are redox-sensitive and oxidized Sch1a, Sch2b, Sch3 are Mo and Cd enriched, relatively reduced Sch1b, Sch2a, Sch4 are depleted Mo and Cd. Sch1a, Sch2a, Sch3, and Sch4 are characterized by a typical right-inclined rare earth element (REE) pattern, inherited from ore-related granodiorite and modified by the precipitation of skarn minerals.
    [Show full text]
  • Petrography and Origin of Xenotime and Monazite Concentrations Central City District Colorado
    Petrography and Origin of Xenotime and Monazite Concentrations Central City District Colorado GEOLOGICAL SURVEY BULLETIN 1032-F Prepared in part on behalf of the U.S. Atomic Energy Commission and pub­ lished with the permission of the Com­ mission Petrography and Origin of Xenotime and Monazite Concentrations Central City District Colorado By E. J. YOUNG and P. K. SIMS GEOLOGY AND ORE DEPOSITS, CLEAR CREEK, GILPIN, AND LARIMER COUNTIES, COLORADO GEOLOGICAL SURVEY BULLETIN 1032-F Prepared in part on behalf of the U.S. Atomic Energy Commission and pub­ lished with the permission of the Com­ mission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1961 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price 20 cents (paper cover) CONTENTS Page Abstract___ --------_-__-_--__--___-__-______-_-_______--_-______ 273 Introduction. _____________________________________________________ 273 Laboratory methods.______________________________________________ 275 Geologic setting.__________________________________________________ 275 Jasper Cuts area._________________________________________________ 277 Fourmile Gulch area.______________________________________________ 287 Illinois Gulch area_________________________________________________ 293 Origin of xenotime and monazite concentrations.______________________ 294 References cited___________________________________________________ 296
    [Show full text]