Bibliografías temáticas / Biologically-Controlled biomineralization

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

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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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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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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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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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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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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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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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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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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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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Tesis sobre el tema "Biologically-Controlled biomineralization"

Wallace, Adam Folger. "Biologically Controlled Mineralization and Demineralization of Amorphous Silica." Diss., Virginia Tech, 2008. http://hdl.handle.net/10919/27424.

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Living systems possess seemingly bottomless complexity. Attempts to parse the details of one cellular process from all other concurrent processes are challenging, if not daunting undertakings. The apparent depth of this problem, as it pertains to biomineralization, is related to the small number of existing studies focused on the development of a mechanism-based understanding of intracellular mineralization processes. Molecular biologists and geneticists have only begun to turn their attention towards identification and characterization of molecules involved in regulating and controlling biomi

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Park, Yeseul. "Metal sulfide biomineralization by magnetotactic bacteria." Electronic Thesis or Diss., Aix-Marseille, 2022. http://www.theses.fr/2022AIXM0262.

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La biominéralisation de sulfures métalliques est observée tant dans des cultures microbiennes que dans la nature. Cependant, seulement quelques cas ont été définis comme étant des processus biologiquement contrôlés comme cela est le cas pour la greigite produite par les bactéries magnétotactiques. Pendant ma thèse, j'ai découvert un nouveau type de biominéralisation intracellulaire de sulfure métallique en étudiant l'impact du cuivre sur la biominéralisation de la greigite par la bactérie Desulfamplus magnetovallimortis BW-1.Le biominéral que j'ai identifié a une structure et une organisation

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Capítulos de libros sobre el tema "Biologically-Controlled biomineralization"

Bazylinski, Dennis A., and Richard B. Frankel. "8. Biologically Controlled Mineralization in Prokaryotes." In Biomineralization, edited by Patricia M. Dove, James J. De Yoreo, and Steve Weiner. De Gruyter, 2003. http://dx.doi.org/10.1515/9781501509346-013.

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Mann, Stephen. "Chemical control of biomineralization." In Biomineralization Principles and Concepts in Bioinorganic Materials Chemistry. Oxford University PressOxford, 2001. http://dx.doi.org/10.1093/oso/9780198508823.003.0004.

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Abstract The high level of regulation associated with biologically controlled mineralization is fundamentally dependent on the chemical control of inorganic precipitation and crystallization. In this chapter, we review the key principles of precipitation—usually from the standpoint of ‘crystallization’ —and illustrate their relevance to biomineralization. The aim is to introduce the fundamental chemical concepts that are pivotal to the specific biological control mechanisms described in Chapters 5 to 8.

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Lowenstam, Heinz A., and Stephen Weiner. "Protoctista." In On Biomineralization. Oxford University Press, 1989. http://dx.doi.org/10.1093/oso/9780195049770.003.0006.

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This kingdom is denned by exclusion, in that its members are neither animals, plants, fungi, nor prokaryotes. They comprise eukaryotic microorganisms and their immediate descendants (Margulis and Schwartz 1988). Of the 27 phyla that make up this kingdom, no less than 17 contain members that form mineralized hard parts. Although the vast majority of Protoctista are microorganisms, their smallness does not in any way imply an inability to control their biomineralization processes. On the contrary, many of the mineralizing Protoctista form very elaborate and complex structures. D’Arcy Thompson wa

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