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Artículos de revistas sobre el tema "Biologically-Controlled biomineralization"

Autor: Grafiati

Publicado: 25 de mayo de 2024

Última modificación: 31 de julio de 2025

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1

Ehrlich, Hermann, Elizabeth Bailey, Marcin Wysokowski, and Teofil Jesionowski. "Forced Biomineralization: A Review." Biomimetics 6, no. 3 (2021): 46. http://dx.doi.org/10.3390/biomimetics6030046.

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Biologically induced and controlled mineralization of metals promotes the development of protective structures to shield cells from thermal, chemical, and ultraviolet stresses. Metal biomineralization is widely considered to have been relevant for the survival of life in the environmental conditions of ancient terrestrial oceans. Similar behavior is seen among extremophilic biomineralizers today, which have evolved to inhabit a variety of industrial aqueous environments with elevated metal concentrations. As an example of extreme biomineralization, we introduce the category of “forced biominer

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2

Pamirsky, Igor E., and Kirill S. Golokhvast. "Origin and Status of Homologous Proteins of Biomineralization (Biosilicification) in the Taxonomy of Phylogenetic Domains." BioMed Research International 2013 (2013): 1–7. http://dx.doi.org/10.1155/2013/397278.

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The taxonomic affiliation (in the systematisation of viruses, and biological domains) of known peptides and proteins of biomineralization (silicateins, silaffins, silacidins and silicase) and their primary structure homologues were analyzed (methodsin silico; using Uniprot database). The total number of known peptides and proteins of biosilicification was counted. The data of the quantitative distribution of the detected homologues found in nature are presented. The similarity of the primary structures of silaffins, silacidins, silicateins, silicase, and their homologues was 21–94%, 45–98%, 39

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3

Okada, Satoshi, Chong Chen, Tomo-o. Watsuji, et al. "The making of natural iron sulfide nanoparticles in a hot vent snail." Proceedings of the National Academy of Sciences 116, no. 41 (2019): 20376–81. http://dx.doi.org/10.1073/pnas.1908533116.

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Biomineralization in animals exclusively features oxygen-based minerals with a single exception of the scaly-foot gastropod Chrysomallon squamiferum, the only metazoan with an iron sulfide skeleton. This unique snail inhabits deep-sea hot vents and possesses scales infused with iron sulfide nanoparticles, including pyrite, giving it a characteristic metallic black sheen. Since the scaly-foot is capable of making iron sulfide nanoparticles in its natural habitat at a relatively low temperature (∼15 °C) and in a chemically dynamic vent environment, elucidating its biomineralization pathways is e

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4

SAKURAI, S., R. ASAKAWA, F. HIROTA, T. SATO, K. SERA, and J. ITOH. "QUANTITATIVE AND QUALITATIVE ANALYSIS OF FLUORIDE AND MULTI ELEMENTS OF SHARK TEETH BY PIXE." International Journal of PIXE 18, no. 03n04 (2008): 123–29. http://dx.doi.org/10.1142/s0129083508001466.

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Biomineralization has two types, biologically induced mineralization (BIM) and biologically controlled mineralization (BCM). Shark teeth is a typical representative of BCM. We have measured concentrations of fluorine and multi elements in shark teeth collected in the south of Japan. As a result, it was confirmed that the sample preparation method, which was established for the biological samples, is applicable to the shark teeth samples and the elemental concentration was obtained in good accuracy and reproducibility. Moreover, we clarified that the shark teeth is composed of Fluorapatite by t

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5

Cuéllar-Cruz, Mayra, Karina Sandra Pérez, María Eugenia Mendoza, and Abel Moreno. "Biocrystals in Plants: A Short Review on Biomineralization Processes and the Role of Phototropins into the Uptake of Calcium." Crystals 10, no. 7 (2020): 591. http://dx.doi.org/10.3390/cryst10070591.

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The biomineralization process is a mechanism inherent to all organisms of the Earth. Throughout the decades, diverse works have reported that the origin of life is tied to crystals, specifically to biominerals of silica that catalyzed RNA, and had some influence in the homochirality. Although the mechanism by which crystals surfaces (minerals) gave origin to life has not yet been proven, the truth is that, up to the present, biominerals are being synthetized by the organisms of different kingdoms in two basic ways: biologically induced and biologically controlled biomineralization. Paradoxical

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6

Hafizyar, and Abdulrahimzai. "A Review on Biological Process for Improvement of Soil Properties in Geotechnical Engineering." Kardan Journal of Engineering and Technology 1, no. 1 (2019): 82–98. https://doi.org/10.31841/KJET.2021.8.

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The biological processing of soil, also termed as the bio-mediated soil improvement method, is known to improve the engineering properties of soil and other construcation materials in terms of their environmental sustainability and performance. This paper reviews the soil microorganism process and other environmental factors that affect their metabolic activities and their geometric compatibility with the soil particle sizes. Two approaches are practiced in geotechnical engineering; biologically-induced and biologically-controlled mineralization. Environmental and other factors that may be enc

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7

Hoffmann, René, Benjamin J. Linzmeier, Kouki Kitajima, et al. "Complex Biomineralization Pathways of the Belemnite Rostrum Cause Biased Paleotemperature Estimates." Minerals 11, no. 12 (2021): 1406. http://dx.doi.org/10.3390/min11121406.

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Paleotemperatures based on δ18O values derived from belemnites are usually “too cold” compared to other archives and paleoclimate models. This temperature bias represents a significant obstacle in paleoceanographic research. Here we show geochemical evidence that belemnite calcite fibers are composed of two distinct low-Mg calcite phases (CP1, CP2). Phase-specific in situ measurement of δ18O values revealed a systematic offset of up to 2‰ (~8 °C), showing a lead–lag signal between both phases in analyses spaced less than 25 µm apart and a total fluctuation of 3.9‰ (~16 °C) within a 2 cm × 2 cm

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8

Giordani, Paolo, Paolo Modenesi, and Mauro Tretiach. "Determinant factors for the formation of the calcium oxalate minerals, weddellite and whewellite, on the surface of foliose lichens." Lichenologist 35, no. 3 (2003): 255–70. http://dx.doi.org/10.1016/s0024-2829(03)00028-8.

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AbstractThe factors influencing the predominance of one of the two mineral forms of calcium oxalate (CO), the monohydrated whewellite (COM) and the di-hydrated weddellite (COD), forming the pruina of the upper cortex of lichens, have been investigated through a simple, sensitive histochemical assay: toluidine blue O (TBO), a metachromatic staining test. The differential reactivity of 43 thalli of 17 pruinose foliose species, supplemented by X-ray diffraction analysis and observations with polarizing and scanning electron microscopy, suggests that the histochemical reactivity of hyphal walls an

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9

Al-Battashi, Huda, Sanket J. Joshi, Bernhard Pracejus, and Aliya Al-Ansari. "The Geomicrobiology of Chromium (VI) Pollution: Microbial Diversity and its Bioremediation Potential." Open Biotechnology Journal 10, no. 1 (2016): 379–89. http://dx.doi.org/10.2174/1874070701610010379.

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The role and significance of microorganisms in environmental recycling activities marks geomicrobiology one of the essential branches within the environmental biotechnology field. Naturally occurring microbes also play geo-active roles in rocks, leading to biomineralization or biomobilization of minerals and metals. Heavy metals, such as chromium (Cr), are essential micronutrients at very low concentrations, but are very toxic at higher concentrations. Generally, heavy metals are leached to the environment through natural processes or anthropogenic activities such as industrial processes, lead

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10

Gorzelak, Przemysław, Luis Torres Jr., Dorota Kołbuk, Tobias B. Grun, and Michał Kowalewski. "Geochemical signatures and nanomechanical properties of echinoid tests from nearshore habitats of Florida: environmental and physiological controls on echinoid biomineralization." PeerJ 13 (January 24, 2025): e18688. https://doi.org/10.7717/peerj.18688.

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The mechanisms that regulate minor and trace element biomineralization in the echinoid skeleton can be primarily controlled biologically (i.e., by the organism and its vital effects) or by extrinsic environmental factors. Assessing the relative role of those controls is essential for understanding echinoid biomineralization, taphonomy, diagenesis, and their potential as geochemical archives. In this study, we (1) contrast geochemical signatures of specimens collected across multiple taxa and environmental settings to assess in situ the effects of environmental and physiological factors on skel

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11

Lykoshin, D. D., V. V. Zaitsev, M. A. Kostromina, and R. S. Esipov. "New-generation osteoplastic materials based on biological and synthetic matrices." Fine Chemical Technologies 16, no. 1 (2021): 36–54. http://dx.doi.org/10.32362/2410-6593-2021-16-1-36-54.

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Objectives. The purpose of this analytical review is to evaluate the market for osteoplastic materials and surgical implants, as well as study the features of new-generation materials and the results of clinical applications.Methods. This review summarizes the volumes of research articles presented in the electronic database PubMed and eLIBRARY. A total of 129 scientific articles related to biological systems, calcium phosphate, polymer, and biocomposite matrices as carriers of pharmaceutical substances, primary recombinant protein osteoinductors, antibiotics, and biologically active chemical

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12

Bouabdellah, Mohammed, Wissale Boukirou, Adriana Potra, et al. "Origin of the Moroccan Touissit-Bou Beker and Jbel Bou Dahar Supergene Non-Sulfide Biomineralization and Its Relevance to Microbiological Activity, Late Miocene Uplift and Climate Changes." Minerals 11, no. 4 (2021): 401. http://dx.doi.org/10.3390/min11040401.

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Through integration of Pb-Zn ± Cu non-sulfide mineralogy, texture, and stable isotope (C, O, S) geochemistry, the world-class Touissit- Bou Beker and Jbel Bou Dahar Mississippi Valley-type districts of the Moroccan Atlasic system have been investigated in order to gain insights into the origin and processes that contributed to the formation of the base metal non-sulfide mineralization. In both districts, direct replacement (“red calamine”) and wallrock replacement (“white calamine”) ores are observed. Based on the mineral assemblages, ore textures, and crosscutting relations, three distinct mi

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13

Walton, Derek, and Gordon B. Curry. "Biogeochemistry of brachiopod intracrystalline proteins and amino acids." Paleontological Society Special Publications 6 (1992): 304. http://dx.doi.org/10.1017/s2475262200008649.

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Brachiopods contain several classes of intracrystalline molecules, secreted during the growth of the organism, and subsequently incorporated in the shell during biomineralization. The function of these molecules is not clear, although in the Mollusca, molecules in similar sites are thought to be involved with biologically controlled mineralization. The order of amino acids, and hence the quantity of each amino acid in proteins is determined by the genome of the organism, and study of such molecules should reveal information regarding the genomes of the fossil organisms.Previous studies of foss

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14

Päßler, Jan-Filip, Emilia Jarochowska, Michel Bestmann, and Axel Munnecke. "Distinguishing Biologically Controlled Calcareous Biomineralization in Fossil Organisms Using Electron Backscatter Diffraction (EBSD)." Frontiers in Earth Science 6 (February 28, 2018). http://dx.doi.org/10.3389/feart.2018.00016.

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15

Zhang, Yuchen, Shaoyang Ma, Jiaming Nie, et al. "Journey of Mineral Precursors in Bone Mineralization: Evolution and Inspiration for Biomimetic Design." Small, August 24, 2023. http://dx.doi.org/10.1002/smll.202207951.

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AbstractBone mineralization is a ubiquitous process among vertebrates that involves a dynamic physical/chemical interplay between the organic and inorganic components of bone tissues. It is now well documented that carbonated apatite, an inorganic component of bone, is proceeded through transient amorphous mineral precursors that transforms into the crystalline mineral phase. Here, the evolution on mineral precursors from their sources to the terminus in the bone mineralization process is reviewed. How organisms tightly control each step of mineralization to drive the formation, stabilization,

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16

Dubicka, Zofia, Jarosław Tyszka, Agnieszka Pałczyńska, et al. "Biocalcification in porcelaneous foraminifera." eLife 13 (August 16, 2024). http://dx.doi.org/10.7554/elife.91568.3.

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Living organisms control the formation of mineral skeletons and other structures through biomineralization. Major phylogenetic groups usually consistently follow a single biomineralization pathway. Foraminifera, which are very efficient marine calcifiers, making a substantial contribution to global carbonate production and global carbon sequestration, are regarded as an exception. This phylum has been commonly thought to follow two contrasting models of either in situ ‘mineralization of extracellular matrix’ attributed to hyaline rotaliid shells, or ‘mineralization within intracellular vesicle

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17

Zhang, Zhiliang, Zhifei Zhang, Lars Holmer, Timothy P. Topper, Bing Pan, and Guoxiang Li. "Evolution and diversity of biomineralized columnar architecture in early Cambrian phosphatic-shelled brachiopods." eLife 12 (April 10, 2024). http://dx.doi.org/10.7554/elife.88855.4.

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Biologically-controlled mineralization producing organic-inorganic composites (hard skeletons) by metazoan biomineralizers has been an evolutionary innovation since the earliest Cambrian. Among them, linguliform brachiopods are one of the key invertebrates that secrete calcium phosphate minerals to build their shells. One of the most distinct shell structures is the organo-phosphatic cylindrical column exclusive to phosphatic-shelled brachiopods, including both crown and stem groups. However, the complexity, diversity, and biomineralization processes of these microscopic columns are far from c

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18

Stolarski, Jarosław, Ismael Coronado, Marta Potocka, et al. "Post-mortem recrystallization of biogenic amorphous calcium carbonate guided by the inherited macromolecular framework." Scientific Reports 14, no. 1 (2024). http://dx.doi.org/10.1038/s41598-024-68037-y.

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AbstractIn contrast to abiotically formed carbonates, biogenetic carbonates have been observed to be nanocomposite, organo-mineral structures, the basic build-blocks of which are particles of quasi-uniform size (10–100 nm) organized into complex higher-order hierarchical structures, typically with highly controlled crystal-axis alignments. Some of these characteristics serve as criteria for inferring a biological origin and the state of preservation of fossil carbonate materials, and to determine whether the biomineralization process was biologically induced or controlled. Here we show that a

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19

Chen, Xuefei, Wenfeng Deng, Hangfang Xiao, Yangrui Guo, and Gangjian Wei. "A Perspective on Probing Coral Resilience to Climate and Environmental Changes Using Stable Isotopes of Bio‐Utilized Metal Elements." Journal of Geophysical Research: Biogeosciences 129, no. 1 (2024). http://dx.doi.org/10.1029/2023jg007656.

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AbstractIn the face of diverse challenges like global warming, ocean acidification, and human activities, the world's coral reefs are confronting a severe ecological crisis. Understanding the historical coevolution of corals with their environment and their resilience to current climate change is crucial for protecting these ecosystems and predicting their future. In this context, metal stable isotopes in corals present a novel and alternative methodology. Their significant fractionation during coral biological processes, persistent presence in coral skeletons, and relatively straightforward s

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20

Liu, Xinyi, Yu Li, Jianrui Zha, Xiangna Han, and Hao Wang. "Biofouling and biomineralization of tubular concretions attached to Longquan celadon from Shengbeiyu shipwreck, China (14th Century CE): a multi-analytical case study." Heritage Science 12, no. 1 (2024). http://dx.doi.org/10.1186/s40494-024-01352-9.

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AbstractA comprehensive multi-analytical investigation was conducted on a piece of Longquan celadon excavated from the Shengbeiyu shipwreck site in the East China Sea. This study focused on a representative type of tubular bio-concretions attached to the submerged celadon, believed to have been formed through the construction activities of a marine tubeworm belonging to the benthic phylum of Polychaeta Annelids. The research examined the microstructure, composition and adhesion form of these tubular bio-concretions, aiming to elucidate their developmental and attachment patterns from a biomine

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21

Li, Luoyang, Timothy P. Topper, Marissa J. Betts, et al. "Calcitic shells in the aragonite sea of the earliest Cambrian." Geology, November 2, 2022. http://dx.doi.org/10.1130/g50533.1.

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The initial acquisition of calcium carbonate polymorphs (aragonite and calcite) at the onset of skeletal biomineralization by disparate metazoans across the Ediacaran-Cambrian transition is thought to be directly influenced by Earth’s seawater chemistry. It has been presumed that animal clades that first acquired mineralized skeletons during the so-called “aragonite sea” of the latest Ediacaran and earliest Cambrian (Terreneuvian) possessed aragonite or high-Mg calcite skeletons, while clades that arose in the subsequent “calcite sea” of Cambrian Series 2 acquired low-Mg calcite skeletons. Her

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