Biomineralization of Three Calcium Silicate-Based Cements After Implantation in Rat Subcutaneous Tissue

Total Page:16

File Type:pdf, Size:1020Kb

Biomineralization of Three Calcium Silicate-Based Cements After Implantation in Rat Subcutaneous Tissue Restor Dent Endod. 2021 Feb;46(1):e1 https://doi.org/10.5395/rde.2021.46.e1 pISSN 2234-7658·eISSN 2234-7666 Research Article Biomineralization of three calcium silicate-based cements after implantation in rat subcutaneous tissue Ranjdar Mahmood Talabani ,1* Balkees Taha Garib ,2 Reza Masaeli ,3 Kavosh Zandsalimi ,4 Farinaz Ketabat 5 1Department of Conservative Dentistry, University of Sulaimani, Sulaimani, Iraq 2Department of Oral Diagnosis, University of Sulaimani, Sulaimani, Iraq 3Department of Dental Biomaterial, Tehran University of Medical Sciences, Tehran, Iran 4Department of Life Sciences Engineering, Faculty of New Sciences and Technologies, University of Tehran, Tehran, Iran Received: Jan 24, 2020 5Division of Biomedical Engineering, University of Saskatchewan, Saskatoon, Canada Revised: Jul 22, 2020 Accepted: Aug 7, 2020 Talabani RM, Garib BT, Masaeli R, ABSTRACT Zandsalimi K, Ketabat F Objectives: The aim of this study was to evaluate the dystrophic mineralization deposits *Correspondence to from 3 calcium silicate-based cements (Micro-Mega mineral trioxide aggregate [MM-MTA], Ranjdar Mahmood Talabani, BDS, MSc Biodentine [BD], and EndoSequence Root Repair Material [ESRRM] putty) over time after Lecturer, Department of Conservative Dentistry, University of Sulaimani, subcutaneous implantation into rats. Sulaymaniyah - Dream Land B-25, Materials and Methods: Forty-five silicon tubes containing the tested materials and 15 empty Sulaymaniyah 46001, Kurdistan Region, Iraq. tubes (serving as a control group) were subcutaneously implanted into the backs of 15 Wistar E-mail: [email protected] rats. At 1, 4, and 8 weeks after implantation, the animals were euthanized n( = 5 animals/ Copyright © 2021. The Korean Academy of group), and the silicon tubes were removed with the surrounding tissues. Histopathological Conservative Dentistry tissue sections were stained with von Kossa stain to assess mineralization. Scanning electron This is an Open Access article distributed microscopy and energy-dispersive X-ray spectroscopy (SEM/EDX) were also used to assess under the terms of the Creative Commons the chemical components of the surface precipitates deposited on the implant and the Attribution Non-Commercial License (https:// pattern of calcium and phosphorus distribution at the material-tissue interface. The calcium- creativecommons.org/licenses/by-nc/4.0/) which permits unrestricted non-commercial to-phosphorus ratios were compared using the non-parametric Kruskal-Wallis test at a use, distribution, and reproduction in any significance level of 5%. medium, provided the original work is properly Results: The von Kossa staining showed that both BD and ESRRM putty induced cited. mineralization starting at week 1; this mineralization increased further until the end of the study. In contrast, MM-MTA induced dystrophic calcification later, from 4 weeks onward. Conflict of Interest No potential conflict of interest relevant to this SEM/EDX showed no statistically significant differences in the calcium- and phosphorus-rich article was reported. areas among the 3 materials at any time point (p > 0.05). Conclusions: After subcutaneous implantation, biomineralization of the 3-calcium silicate- Author Contributions based cements started early and increased over time, and all 3 tested cements generated Conceptualization: Talabani RM, Garib BT, Masaeli R. Data curation: Talabani RM. Formal calcium- and phosphorus-containing surface precipitates. analysis: Talabani RM. Investigation: Talabani Keywords: RM, Zandsalimi K, Ketabat F. Methodology: Biodentine; Biomineralization; EndoSequence Garib BT, Masaeli RM. Project administration: Talabani RM. Software: Ketabat F. Supervision: Garib BT, Masaeli R. Validation: Zandsalimi K. Visualization: Garib BT. Writing - original INTRODUCTION draft: Talabani RM. Writing - review & editing: Garib BT. Calcium silicate-based cements are biocompatible ceramic compounds. They are neither harmful nor shrinkable and largely remain in a fixed chemical state within biological https://rde.ac 1/13 Biomineralization of calcium silicate-based cements ORCID iDs media [1]. In the 1990s, calcium silicate-based materials were introduced to endodontics Ranjdar Mahmood Talabani as retrograde filling materials [2]. These new calcium silicate cements were composed of https://orcid.org/0000-0002-9833-1013 tricalcium and dicalcium silicates, calcium phosphates, and calcium hydroxide, as well as Balkees Taha Garib https://orcid.org/0000-0003-3607-6907 zirconium oxide as a radiopacifier [3]. Reza Masaeli https://orcid.org/0000-0002-3003-889X The excellent biocompatibility of these cements is attributed to their analogous relationship Kavosh Zandsalimi with biological hydroxyapatite. During the hydration process, bioceramics generate various https://orcid.org/0000-0002-8877-0565 material compounds (such as hydroxyapatites) that can trigger a regenerative response in the Farinaz Ketabat human body [4]. https://orcid.org/0000-0001-7357-8100 Calcium silicate bioactive cements upregulate the differentiation of osteoblasts, fibroblasts, cementoblasts, odontoblasts, and many stem cells. When inserted in biological liquid media, they can induce the chemical formation of a calcium phosphate/apatite coating. Their capacity to enhance calcium phosphate deposits is the basis of their use for dentin remineralization and tissue regeneration [5]. In vitro studies by Gandolfi et al. [6], in vivo animal tests by Reyes-Carmona et al. [7], and clinical studies [8] have postulated that calcium phosphate deposits could nucleate apatite and promote remineralization to trigger the formation of new mineralized tissues. Micro-Mega mineral trioxide aggregate (MM-MTA; Micro-Mega SA, Besançon, France) is pre-dosed and supplied in a capsule of tricalcium silicate-based cement. Its newer formulations were designed to minimize the disadvantages of original MTA products, with improved setting and handling. Their composition includes calcium carbonate, which not only decreases the setting time [9] but also is osteoconductive, osteoinductive, and biocompatible. The biological integration of MM-MTA is due to calcium ions, which form hydroxyapatite upon contact with phosphate ions in the body [10]. Biodentine (BD; Septodont, Saint Maur des Fosses, France) was developed as a novel tricalcium silicate-based cement in 2010 [11] that can also serve as a dentin substitute [12]. In addition to its superiority to MTA in terms of manipulation, compatibility, and hardening, it releases significantly more calcium ions with deeper integration into human root canal dentin than MTA [13]. Along with calcium and silicon, the intertubular diffusion of carbonate into the dentin leads to the establishment of a mineral infiltration zone [14]. EndoSequence Root Repair Material putty (ESRRM putty) is another premixed, ready-to-use calcium silicate-based cement. It is manufactured by Brasseler USA (Savannah, GA, USA) for use as an alternative to MTA. Favorable characteristics of ESRRM putty include a shorter setting time and superior handling features [15]. This putty possesses better color stability and handling while exhibiting physiochemical properties comparable to MTA. The essential characteristic is that this material can release calcium and phosphate ions, which are necessary for hydroxyapatite deposition [16]. A number of available in vivo laboratory studies have been conducted to assess the bioactivity and biomineralization capacities of various calcium silicate-based materials. The biomineralization of MM-MTA and ESRRM putty has not been studied in a rat tissue model, and few studies have assessed the capacity of BD to form an area that stains positive with von Kossa stain, which is suggestive of mineralization, after implantation in an animal model [17,18]. Thus, the aim of the present study was to assess and compare the timing and capacity of calcification associated with MM-MTA, BD, and ESRRM putty using von Kossa https://rde.ac https://doi.org/10.5395/rde.2021.46.e1 2/13 Biomineralization of calcium silicate-based cements stain. Additionally, this study analyzed the scattering of calcium and phosphorus at the material-tissue interface via scanning electron microscopy (SEM) and energy-dispersive X-ray spectroscopy (EDX) after subcutaneous implantation in rat tissue. MATERIALS AND METHODS The principles of laboratory animal care were applied in this study (National Institutes of Health publication 85–23, 1985). The current study also adhered to national regulations on animal care as approved by the Ethical Committee for Animal Research of University of Sulaimani (No. 9; 6/2/2017). In this study, 15 male Wistar albino rats aged 4–5 months and weighing 250–350 g were used. The animals were bred at controlled room temperature and were provided with water and food ad libitum. Animal care was based on guidance from the Farabi Comprehensive Center of Excellence in Ophthalmology at Tehran University of Medical Sciences. Three commercially available calcium silicate-based cement materials were used (Table 1): BD (Septodont), ESRRM putty (Brasseler USA), and MM-MTA capsules (MicroMega). Implantation in subcutaneous tissue In this study, 60 sterile silicon tubes (length, 7 mm; inner diameter, 2 mm; outer diameter, 4 mm; both ends open) were used, 45 of which were filled with the 3 tested cements (15 tubes for each cement), while the remaining 15 tubes were used as negative controls without the insertion of any materials. Thus, each rat received 3 tested materials and
Recommended publications
  • 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.
    [Show full text]
  • Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
    sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean.
    [Show full text]
  • Silicate Weathering in Anoxic Marine Sediment As a Requirement for Authigenic Carbonate Burial T
    Earth-Science Reviews 200 (2020) 102960 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Silicate weathering in anoxic marine sediment as a requirement for authigenic carbonate burial T Marta E. Torresa,*, Wei-Li Hongb, Evan A. Solomonc, Kitty Millikend, Ji-Hoon Kime, James C. Samplef, Barbara M.A. Teichertg, Klaus Wallmannh a College of Earth, Ocean and Atmospheric Science, Oregon State University, Corvallis OR 97331, USA b Geological Survey of Norway, Trondheim, Norway c School of Oceanography, University of Washington, Seattle, WA 98195, USA d Bureau of Economic Geology, University of Texas at Austin, Austin, TX 78713, USA e Petroleum and Marine Research Division, Korea Institute of Geoscience and Mineral Resources, Daejeon, South Korea f School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA g Geologisch-Paläontologisches Institut, Wilhelms-Universität Münster, Corrensstr. 24, 48149 Münster, Germany h IFM-GEOMAR Leibniz Institute of Marine Sciences, Wischhofstrasse 1-3, 24148 Kiel, Germany ARTICLE INFO ABSTRACT Keywords: We emphasize the importance of marine silicate weathering (MSiW) reactions in anoxic sediment as funda- Silicate weathering mental in generating alkalinity and cations needed for carbonate precipitation and preservation along con- Authigenic carbonate tinental margins. We use a model that couples thermodynamics with aqueous geochemistry to show that the CO2 Organogenic dolomite released during methanogenesis results in a drop in pH to 6.0; unless these protons are buffered by MSiW, Alkalinity carbonate minerals will dissolve. We present data from two regions: the India passive margin and the active Carbon cycling subduction zone off Japan, where ash and/or rivers supply the reactive silicate phase, as reflected in strontium isotope data.
    [Show full text]
  • The Silicate Structure Analysis of Hydrated Portland Cement Paste
    The Silicate Structure Analysis of Hydrated Portland Cement Paste CHARLES W. LENTZ, Research Department, Dow Corning Corporation, Midland, Michigan A new technique for recovering silicate structures as trimeth- ylsilyl derivatives has been used to study the hydration of port- land cement. By this method only the changes iii the silicate portion of the structure can be determined as a function of hydration time. Cement pastes ranging in age from one day to 14. 7 years were analyzedfor the study. The hydration reaction is shown to be similar to a condensation type polymerization. The orthosilicate content of cement paste (which probably rep- resents the original calcium silicates in the portland cement) gradually decreases as the paste ages. Concurrentiy a disilicate structure is formed which reaches a maximum quantity in about four weeks and then it too diminishes as the paste ages. Minor quantities of a trisiicate and a cyclic tetrasiicate are shown to be present in hydrated cement paste. An unidentified polysilicate structure is produced by the hydration reaction which not only increases in quantity throughout the age period studied, but also increases in molecular weight as the paste ages. THE SILICON atoms in silicate minerals are always in fourfold coordination with oxygen. These silicon-oxygen tetrahedra can be completely separated from each other, as in the orthosilicates, they can be paired, as in the pyrosilicates, or they can be in other combinations with each other to give a variety of silicate structures. If the min- eral is composed only of Si and 0, then there is a three-dimensional network of silicate tetrahedra.
    [Show full text]
  • Biomineralization and Global Biogeochemical Cycles Philippe Van Cappellen Faculty of Geosciences, Utrecht University P.O
    1122 Biomineralization and Global Biogeochemical Cycles Philippe Van Cappellen Faculty of Geosciences, Utrecht University P.O. Box 80021 3508 TA Utrecht, The Netherlands INTRODUCTION Biological activity is a dominant force shaping the chemical structure and evolution of the earth surface environment. The presence of an oxygenated atmosphere- hydrosphere surrounding an otherwise highly reducing solid earth is the most striking consequence of the rise of life on earth. Biological evolution and the functioning of ecosystems, in turn, are to a large degree conditioned by geophysical and geological processes. Understanding the interactions between organisms and their abiotic environment, and the resulting coupled evolution of the biosphere and geosphere is a central theme of research in biogeology. Biogeochemists contribute to this understanding by studying the transformations and transport of chemical substrates and products of biological activity in the environment. Biogeochemical cycles provide a general framework in which geochemists organize their knowledge and interpret their data. The cycle of a given element or substance maps out the rates of transformation in, and transport fluxes between, adjoining environmental reservoirs. The temporal and spatial scales of interest dictate the selection of reservoirs and processes included in the cycle. Typically, the need for a detailed representation of biological process rates and ecosystem structure decreases as the spatial and temporal time scales considered increase. Much progress has been made in the development of global-scale models of biogeochemical cycles. Although these models are based on fairly simple representations of the biosphere and hydrosphere, they account for the large-scale changes in the composition, redox state and biological productivity of the earth surface environment that have occurred over geological time.
    [Show full text]
  • University of Nevada Reno SILICATE and CARBONATE SEDIMENT
    University of Nevada Reno /SILICATE AND CARBONATE SEDIMENT-WATER RELATIONSHIPS IN WALKER LAKE, NEVADA A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Geochemistry by Ronald J. Spencer MINES 2 - UBKAKY %?: The thesis of Ronald James Spencer is approved: University of Nevada Reno May 1977 ACKNOWLEDGMENTS The author gratefully acknowledges the contributions of Dr. L. V. Benson, who directed the thesis, and Drs. L. C. Hsu and R. D. Burkhart, who served on the thesis ccmnittee. A special note of thanks is given to Pat Harris of the Desert Research Institute, who supervised the wet chemical analyses on the lake water and pore fluids. I also would like to thank John Sims and Mike Rymer of the U. S. Geological Survey, Menlo Park, for their effort in obtaining the piston core; and Blair Jones of the U. S. Geological Survey, Reston, for the use of equipment and many very helpful suggestions. Much of the work herein was done as a part of the study of the "Dynamic Ecological Relationships in Walker Lake, Nevada", and was supported by the Office of Water Research and Technology through grant number C-6158 to the Desert Research Institute. I thank the other members involved in the study; Drs. Dave Koch and Roger Jacobson, and Joe Mahoney, Jim Cooper, and Jim Hainiine; for advice in their fields of expertise and help in sample collection. Special thanks are extended to my wife, Laurie, without whose help and support this thesis could not have been completed. A final note of thanks to Tina Nesler, who advised Laurie in the typing of the manuscript.
    [Show full text]
  • A Perspective on Underlying Crystal Growth Mechanisms in Biomineralization: Solution Mediated Growth Versus Nanosphere Particle Accretion
    CrystEngComm A perspective on underlying crystal growth mechanisms in biomineralization: solution mediated growth versus nanosphere particle accretion Journal: CrystEngComm Manuscript ID: CE-HIG-07-2014-001474.R1 Article Type: Highlight Date Submitted by the Author: 01-Dec-2014 Complete List of Authors: Gal, Assaf; Weizmann Institute of Science, Structural Biology Weiner, Steve; Weizmann Institute of Science, Structural Biology Addadi, Lia; Weizmann Institute of Science, Structural Biology Page 1 of 23 CrystEngComm A perspective on underlying crystal growth mechanisms in biomineralization: solution mediated growth versus nanosphere particle accretion Assaf Gal, Steve Weiner, and Lia Addadi Department of Structural Biology, Weizmann Institute of Science, Rehovot, Israel 76100 Abstract Many organisms form crystals from transient amorphous precursor phases. In the cases where the precursor phases were imaged, they consist of nanosphere particles. Interestingly, some mature biogenic crystals also have nanosphere particle morphology, but some are characterized by crystallographic faces that are smooth at the nanometer level. There are also biogenic crystals that have both crystallographic faces and nanosphere particle morphology. This highlight presents a working hypothesis, stating that some biomineralization processes involve growth by nanosphere particle accretion, where amorphous nanoparticles are incorporated as such into growing crystals and preserve their morphology upon crystallization. This process produces biogenic crystals with a nanosphere particle morphology. Other biomineralization processes proceed by ion-by-ion growth, and some cases of biological crystal growth involve both processes. We also identify several biomineralization processes which do not seem to fit this working hypothesis. It is our hope that this highlight will inspire studies that will shed more light on the underlying crystallization mechanisms in biology.
    [Show full text]
  • An Overview of Biomineralization Processes and the Problem of The
    11 An Overview of Biomineralization Processes and the Problem of the Vital Effect Steve Weiner Department of Structural Biology Weizmann Institute of Science 76100 Rehovot Israel Patricia M. Dove Department of GeoSciences Virginia Tech Blacksburg, Virginia 24061 U.S.A. “Biomineralization links soft organic tissues, which are compositionally akin to the atmosphere and oceans, with the hard materials of the solid Earth. It provides organisms with skeletons and shells while they are alive, and when they die these are deposited as sediment in environments from river plains to the deep ocean floor. It is also these hard, resistant products of life which are mainly responsible for the Earth’s fossil record. Consequently, biomineralization involves biologists, chemists, and geologists in interdisciplinary studies at one of the interfaces between Earth and life.” (Leadbeater and Riding 1986) INTRODUCTION Biomineralization refers to the processes by which organisms form minerals. The control exerted by many organisms over mineral formation distinguishes these processes from abiotic mineralization. The latter was the primary focus of earth scientists over the last century, but the emergence of biogeochemistry and the urgency of understanding the past and future evolution of the Earth are moving biological mineralization to the forefront of various fields of science, including the earth sciences. The growth in biogeochemistry has led to a number of new exciting research areas where the distinctions between the biological, chemical, and earth sciences disciplines melt away. Of the wonderful topics that are receiving renewed attention, the study of biomineral formation is perhaps the most fascinating. Truly at the interface of earth and life, biomineralization is a discipline that is certain to see major advancements as a new generation of scientists brings cross-disciplinary training and new experimental and computational methods to the most daunting problems.
    [Show full text]
  • Effect of Ph Change on Exoskeletons of Selected Saltwater Organisms Which Rely on Calcium Fixation Derya Z
    Journal of Emerging Investigators Effect of pH change on exoskeletons of selected saltwater organisms which rely on calcium fixation Derya Z. Tansel1, Ariadna Arreaza2, Berrin Tansel2 1 Coral Gables Senior High, Coral Gables, FL 2 Florida International University, Miami, FL Summary increase in H+ concentration in the last 200 years (1,2,3). The projections for rising atmospheric carbon dioxide According to atmospheric CO2 projections, ocean surface concentrations indicate that the pH levels of the ocean pH levels are estimated to decrease by 0.3-0.4 units by surface could decrease by 0.3-0.4 units by the end of the end of the 21st century. This decrease corresponds the 21st century. The objective of this research was to to an increase in the hydrogen ion concentration of about evaluate the effect of pH on the exoskeletons of six aquatic organisms commonly found in South Florida 100-150% above the levels in the late 1800s (4,5). The coastal waters. The exoskeleton samples studied were impacts of ocean acidification can be 10–50% higher from the common nutmeg (Cancellaria reticulate), near coastal areas due to proximity to anthropogenic lettered olive (Oliva sayana), stiff pen shell (Atrina rigida), sources (6). kitten’s paw (Plicatulidae), fan coral (Gorgonia ventalina), Although some species can tolerate pH changes, and common slipper shell (Crepidula fornicate). The many marine organisms and processes can be impacted, exoskeleton samples were exposed to saltwater (34% including the composition of communities and food webs salinity) at pH levels ranging from 8.3 to 6.0 for 5 days.
    [Show full text]
  • 1 Supplementary Materials and Methods 1 S1 Expanded
    1 Supplementary Materials and Methods 2 S1 Expanded Geologic and Paleogeographic Information 3 The carbonate nodules from Montañez et al., (2007) utilized in this study were collected from well-developed and 4 drained paleosols from: 1) the Eastern Shelf of the Midland Basin (N.C. Texas), 2) Paradox Basin (S.E. Utah), 3) Pedregosa 5 Basin (S.C. New Mexico), 4) Anadarko Basin (S.C. Oklahoma), and 5) the Grand Canyon Embayment (N.C. Arizona) (Fig. 6 1a; Richey et al., (2020)). The plant cuticle fossils come from localities in: 1) N.C. Texas (Lower Pease River [LPR], Lake 7 Kemp Dam [LKD], Parkey’s Oil Patch [POP], and Mitchell Creek [MC]; all representing localities that also provided 8 carbonate nodules or plant organic matter [POM] for Montañez et al., (2007), 2) N.C. New Mexico (Kinney Brick Quarry 9 [KB]), 3) S.E. Kansas (Hamilton Quarry [HQ]), 4) S.E. Illinois (Lake Sara Limestone [LSL]), and 5) S.W. Indiana (sub- 10 Minshall [SM]) (Fig. 1a, S2–4; Richey et al., (2020)). These localities span a wide portion of the western equatorial portion 11 of Euramerica during the latest Pennsylvanian through middle Permian (Fig. 1b). 12 13 S2 Biostratigraphic Correlations and Age Model 14 N.C. Texas stratigraphy and the position of pedogenic carbonate samples from Montañez et al., (2007) and cuticle were 15 inferred from N.C. Texas conodont biostratigraphy and its relation to Permian global conodont biostratigraphy (Tabor and 16 Montañez, 2004; Wardlaw, 2005; Henderson, 2018). The specific correlations used are (C. Henderson, personal 17 communication, August 2019): (1) The Stockwether Limestone Member of the Pueblo Formation contains Idiognathodus 18 isolatus, indicating that the Carboniferous-Permian boundary (298.9 Ma) and base of the Asselian resides in the Stockwether 19 Limestone (Wardlaw, 2005).
    [Show full text]
  • Biomineralization and Evolutionary History Andrew H
    1 111 Biomineralization and Evolutionary History Andrew H. Knoll Department of Organismic and Evolutionary Biology Harvard University Cambridge, Massachusetts, 02138 U.S.A. INTRODUCTION The Dutch ethologist Niko Tinbergen famously distinguished between proximal and ultimate explanations in biology. Proximally, biologists seek a mechanistic understanding of how organisms function; most of this volume addresses the molecular and physiological bases of biomineralization. But while much of biology might be viewed as a particularly interesting form of chemistry, it is more than that. Biology is chemistry with a history, requiring that proximal explanations be grounded in ultimate, or evolutionary, understanding. The physiological pathways by which organisms precipitate skeletal minerals and the forms and functions of the skeletons they fashion have been shaped by natural selection through geologic time, and all have constrained continuing evolution in skeleton-forming clades. In this chapter, I outline some major patterns of skeletal evolution inferred from phylogeny and fossils (Figure 1), highlighting ways that our improving mechanistic knowledge of biomineralization can help us to understand this evolutionary record (see Leadbetter and Riding 1986; Lowenstam and Weiner 1989; Carter 1990; and Simkiss and Wilbur 1989 for earlier reviews). Figure 1. A geologic time scale for the past 1000 million years, showing the principal time divisions used in Earth science and the timing of major evolutionary events discussed in this chapter. Earlier intervals of time—the Mesoproterozoic (1600–1000 million years ago) and Paleoproterozoic (2500– 1600 million years ago) eras of the Proterozoic Eon and the Archean Eon (> 2500 million years ago)— are not shown. Time scale after Remane (2000).
    [Show full text]
  • Biomineralization & Biominerals “It's a Hard Life”
    Maria Isabel López Fierro Biomineralization Literature Review & Biominerals Chair: Marc A. Meyers “It’s a hard life” Joanna McKittrick Jan Talbot Image credit: Out Of The Blue Aquaculture Ltd 1 Outline Sponge Spicule Introduction & History Basic Biomineralization Principles Saturation, Nucleation, Growth, & Organic Matrix Image credit: http://www.choijinhyuk.com Bleached Coral Biominerals & Biomineralization Models Calcium Carbonate Shells: Nacre Silica Image credit: jroy.abenaza.com2 Sponge Spicule Hydroxyapatite Bone Why do we need to understand biomineralization? Summary & Conclusions Introduction & History of Biomineralization 3 Introduction: The Process Biomineralization is the process by which living form and influence the precipitation of minerals. 5µm No single or ‘grand’ •Crystals from the inner shell layer of the Eastern mechanism. oyster onto a metal implant. •sheets converge forming a“rosette” structure. Combination of efforts •Organic matrix appears like “glue.” from cells, producing Image credit: http://www.scienceasart.org organic and inorganic Skinner and Jahren (2003)4 molecules that combine in various structural ways to form an unique material. Introduction: Why mineralize? Evolution of Biomineralization has provided organisms with a strong building material. o Minerals are stiff and brittle (& cheap energy wise) o Organic materials are soft and pliable Functions include: v Strength & Integrity v Protection. v Mobility v Storage - Biominerals are ion reservoir for cellular functions. v Cutting and grinding v Buoyancy v Optical, magnetic and gravity sensing 5 History of biominerals First biomineralization evidence from microbial stromatolites - 3500M years ago Not controlled deposition of inorganic solids 560M years ago - organisms from different phyla evolved the ability Runnegar and Bengtson (1992) to form different minerals. To date there are 64+ 6 biominerals identified.
    [Show full text]