Marine and Freshwater Micropearls: Biomineralization Producing
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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. -
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. -
Improved Protocol for the Preparation of Tetraselmis Suecica Axenic
36 The Open Biotechnology Journal, 2010, 4, 36-46 Open Access Improved Protocol for the Preparation of Tetraselmis suecica Axenic Culture and Adaptation to Heterotrophic Cultivation Mojtaba Azma1, Rosfarizan Mohamad1, Raha Abdul Rahim2 and Arbakariya B. Ariff*,1 1Department of Bioprocess Technology, Faculty of Biotechnology and Biomolecular Sciences, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia 2Department of Cell and Molecular Biology, Faculty of Biotechnology and Biomolecular Sciences, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia Abstract: The effectiveness of various physical and chemical methods for the removal of contaminants from the microal- gae, Tetraselmis suecica, culture was investigated. The information obtained was used as the basis for the development of improved protocol for the preparation of axenic culture to be adapted to heterotrophic cultivation. Repeated centrifugation and rinsing effectively removed the free bacterial contaminants from the microalgae culture while sonication helped to loosen up the tightly attached bacterial contaminants on the microalgae cells. Removal of bacterial spores was accom- plished using a mixture of two antibiotics, 5 mg/mL vancomycine and 10 mg/mL neomycine. Walne medium formulation with natural seawater was preferred for the enhancement of growth of T. suecica. Adaptation of growth from photoautot- rophic to heterotrophic conditions was achieved by the repeated cultivation of photoautotrophic culture with sequential reduction in illumination time, and finally the culture was inoculated into the medium containing 10 g/L glucose, incu- bated in total darkness to obtain heterotrophic cells. Changes in the morphology and composition of T. suecica cells dur- ing the adaptation from photoautotrophic to heterotrophic condition, as examined under Transmission Electron Micro- scope, were also reported. -
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. -
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. -
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. -
Gc – Ms) Analysis
Academic Sciences International Journal of Pharmacy and Pharmaceutical Sciences ISSN- 0975-1491 Vol 5, Issue 3, 2013 Research Article EVALUATION OF ANTIMICROBIAL METABOLITES FROM MARINE MICROALGAE TETRASELMIS SUECICA USING GAS CHROMATOGRAPHY – MASS SPECTROMETRY (GC – MS) ANALYSIS V. DOOSLIN MERCY BAI1 AND S. KRISHNAKUMAR2* 1Department of Biomedical Engineering Rajiv Gandhi College of Enginnering and Technology.Puducherry 607402, India, 2Department of Biomedical Engineering, Sathyabama University, Chennai 600119, Tamil Nadu, India. Email: [email protected] Received: 15 Mar 2013, Revised and Accepted: 23 Apr 2013 ABSTRACT Objective: Marine natural products have been considered as one of the most promising sources of antimicrobial compounds in recent years. Marine microalgae Tetraselmis suecica (Kylin) was selected for the present antimicrobial investigation. Methods: The effects of pH, temperature and salinity were tested for the growth of microalgae. The antibacterial effect of different solvent extracts of marine microalgae Tetraselmis suecica against selected human pathogens such as Vibrio cholerae, Klebsiella pneumoniae, Escherichia coli, Pseudomonas aeruginosa, Salmonella sp, Proteus sp., Streptococcus pyogens, Staphylococcus aureus, Bacillus megaterium and Bacillus subtilis were investigated. The GC-MS analysis was done with standard specification to identify the active principle of bioactive compound. Results: The highest cell density was observed when the medium adjusted with 40ppt of salinity in pH of 9.0 at 250C during 9th day of incubation period. Methanol + chloroform (1:1) crude extract of Tetraselmis suecica was confirmed considerable activity against gram negative bacteria than gram positive human pathogen. GC-MS analysis revealed the presence of unique chemical compounds like 1-ethyl butyl 3-hexyl hydroperoxide (MW: 100) and methyl heptanate (MW: 186) respectively for the crude extract of Tetraselmis suecica. -
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). -
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. -
An Introduction to Biomineralization
MATERIAL SCIENCE MEETS MEDICINE – PRESENTATION ABSTRACTS BIOMINERALIZATION An Introduction to Biomineralization John Dunlop Department of Biomaterials, Max Planck Institute of Colloids and Interfaces, Potsdam-Golm Many living organisms, ranging from bacteria to plants to animals, can control the formation of mineral both within and around their cells. These bio-minerals play important functional roles in organisms. The most obvious function is structural, with nano-sized mineral particles reinforcing our bones being a well- known example. Biominerals are also used in living systems in many other ways. To name just a few examples; they are used as transparent lenses as well as magnetic sensors and they also store important ions such as calcium used in the metabolism. All of these different functions arise through the exquisite control of the biomineralization process. Nature forms these minerals in incredibly complex shapes, with well-defined sizes and in addition can control what phase of mineral is formed (crystalline or amorphous for example). As such much research has been done to understand the process of biomineralization particularly with its application in the bioinspired design of novel materials. In medicine, and especially in the field of bone biology knowledge of how bone mineral forms is fundamental in the understanding, treatment and control of degenerative diseases such as osteoporosis. This presentation will give a general overview of the concept of biomineralization, and its application to medicine. The idea is to firstly present the evolutionary background of minerals in biology, showing a variety of examples from all domains of life. The presentation will then focus on giving a short summary of how mineralized tissues form, and then give an overview on how minerals organisation controls the tissue mechanical properties. -
"Phycology". In: Encyclopedia of Life Science
Phycology Introductory article Ralph A Lewin, University of California, La Jolla, California, USA Article Contents Michael A Borowitzka, Murdoch University, Perth, Australia . General Features . Uses The study of algae is generally called ‘phycology’, from the Greek word phykos meaning . Noxious Algae ‘seaweed’. Just what algae are is difficult to define, because they belong to many different . Classification and unrelated classes including both prokaryotic and eukaryotic representatives. Broadly . Evolution speaking, the algae comprise all, mainly aquatic, plants that can use light energy to fix carbon from atmospheric CO2 and evolve oxygen, but which are not specialized land doi: 10.1038/npg.els.0004234 plants like mosses, ferns, coniferous trees and flowering plants. This is a negative definition, but it serves its purpose. General Features Algae range in size from microscopic unicells less than 1 mm several species are also of economic importance. Some in diameter to kelps as long as 60 m. They can be found in kinds are consumed as food by humans. These include almost all aqueous or moist habitats; in marine and fresh- the red alga Porphyra (also known as nori or laver), an water environments they are the main photosynthetic or- important ingredient of Japanese foods such as sushi. ganisms. They are also common in soils, salt lakes and hot Other algae commonly eaten in the Orient are the brown springs, and some can grow in snow and on rocks and the algae Laminaria and Undaria and the green algae Caulerpa bark of trees. Most algae normally require light, but some and Monostroma. The new science of molecular biology species can also grow in the dark if a suitable organic carbon has depended largely on the use of algal polysaccharides, source is available for nutrition. -
Remineralization of Demineralized Dentin Using a Dual-Analog System
Remineralization of demineralized dentin using a dual-analog system N Saxena1 S Habelitz2 GW Marshall2 LB Gower1 1 – Materials Science and Engineering, University of Florida, Gainesville, FL, USA 2 – Preventative and Restorative Dental Sciences, University of California San Francisco, San Francisco, CA, USA Correspondence to: Laurie Gower Materials Science and Engineering University of Florida 549 Gale Lemerand Dr. Gainesville, FL 32611 [email protected] 1 Abstract Objectives Improved methods are needed to remineralize dentin caries in order to promote conservation of dentin tissued and minimize the surgical interventions that are currently required for clinical treatment. Here we test the hypothesis that bulk substrates can be effectively mineralized via a dual- analog system proposed by others, using a tripolyphosphate “templating analog” and a poly(acrylic acid) or poly(aspartic acid) “sequestration analog”, the latter of which generates the polymer-induced liquid-precursor (PILP) mineralization process studied in our lab. Material & Methods – Demineralized human dentin slices were remineralized with and without pre-treatment with tripolyphosphate. Both poly(acrylic) acid and poly(aspartic acid) were used as PILP process-directing agents or “sequestration analogs”. A control experiment with no polymer present was also conducted. Results – No mineralization was observed in any of the poly(acrylic acid) groups. In both the poly(aspartic acid) and no polymer groups, tripolyphosphate inhibited mineralization on the surfaces of the specimens and promoted mineralization within the interiors of the specimens. Pre- treatment with tripolyphosphate enhanced overall mineralization of the poly(aspartic acid) group. However, when analyzed via TEM, regions with little mineral were still present. Conclusion – Poly(acrylic acid) was unable to remineralize demineralized dentin slices, even when pre-treated with tripolyphosphate.