Biology subjects

Scoppola, E.

Publications and source records attributed to Scoppola, E..

5 recordsLinked to original sources

bioRxiv2026

Magnetic organelle gene clusters enable bacterial growth and ATP homeostasis under oxidizing conditions

Biological organisms can produce magnetic nanoparticles made of magnetite to detect the Earth's magnetic field for orientation. The evolutionary mechanisms that led to the acquisition of this capacity remain unknown. The most ancient organisms known to perform magnetic orientation are magnetotactic bacteria. Under tight genetic control, they produce chains of magnetite nanoparticles in dedicated organelles to allow efficient navigation in aquatic environments containing molecular oxygen. Yet, these bacteria have been proposed to emerge before molecular oxygen became abundant on Earth, at a time when this navigation system could not have served its current function. Here, we show that gene clusters responsible of magnetite formation and organization enable resistance against hydrogen peroxide, a toxic oxygen-derived compound that was produced during the early stages of Earth's oxygenation when iron oxidation consumed molecular oxygen. Characterization of the nanoparticle's oxidation state supported the involvement of magnetite in resistance to hydrogen peroxide-induced oxidative stress. These findings are compatible with an early emergence of magnetotactic bacteria, before natural waters became oxygenated. We propose a conceptual framework to explain the origin of magnetic orientation in bacteria, and offer tools to identify the initiation of Earth's oxygenation in a time-resolved manner.

microbiology↗

bioRxiv2026

Crystallization of magnesium calcite otoconia in the inner ear of the developing quail

Otolith organs are specialized structures of the vertebrate inner ear that provide the inertial mass required for maintaining equilibrium. Mammals possess two otolithic organs, the utricle and the saccule, whereas birds and other non-mammalian vertebrates also retain a third one, the lagena, whose development remains poorly understood and whose function is still debated. In birds, the lagena contains thousands of calcium carbonate biomineral particles, termed otoconia. Here, we reconstruct the developmental crystallization of lagena otoconia in the Japanese quail (Coturnix japonica) throughout embryogenesis. We combine multiscale imaging with structural, compositional, and crystallographic analyses across length scales. We show that lagena mineralization precedes cranial bone formation and proceeds predominantly through the growth of existing otoconia rather than continued nucleation. Otoconia develop through progressive particle growth, alignment, and fusion within a pre-existing organic compartment while maintaining a persistent central core, ultimately forming magnesium calcite biominerals. This maturation is accompanied by progressive nanoscale densification, transforming early mineral deposits into mature hierarchical crystals. This work establishes a developmental model of avian otoconia formation and provides new insights into how hierarchical calcium carbonate crystals are assembled during vertebrate development. Statement of significanceOtoliths are the only calcite based biomineral in our body that has a physiological function, yet their developmental assembly remain incompletely understood. While the utricle and saccule have been extensively investigated across vertebrates, the lagena, a third otolithic organ lost during mammalian evolution, has received comparatively little attention. Here, we combine multiscale imaging and materials characterization to reconstruct the developmental crystallization of lagena otoconia in the Japanese quail. We establish how hierarchical magnesium calcite biominerals emerge through coordinated mineral growth, structural maturation, and crystallization, providing a developmental framework for avian otoconia formation and new insights into the assembly of vertebrate calcium carbonate crystals.

developmental biology↗

bioRxiv2022

Induced mineralization in Escherichia coli biofilms: the key role of bacterial alkaline phosphatase

Biofilms appear when bacteria colonize a surface and synthesize and assemble extracellular matrix components. In addition to the organic matrix, some biofilms precipitate mineral particles such as calcium phosphate. While calcified biofilms induce diseases like periodontitis in physiological environments, they also inspire the engineering of living composites. Understanding mineralization mechanisms in biofilms will thus provide key knowledge for either inhibiting or promoting mineralization in these research fields. The enzyme alkaline phosphatase (ALP) plays a key role in calcium phosphate precipitation in mammalian bone tissue. Produced by eukaryotic cells, ALP catalyzes the hydrolysis of monophosphates starting from different precursors (e.g., alkaloids, proteins) and makes phosphate ions readily available for the precipitation with calcium. Bacterial ALPs are expressed by the well-characterized gram-negative and gram-positive bacteria E. coli and S. aureus as well as a large number of marine and soil bacteria. While it was recently proposed that bacterial ALPs induce mineral precipitation, their role in biofilm mineralization is not fully understood. In this work, we address this question using the biofilm-forming E. coli K-12 strain W3110, which expresses periplasmic ALP from the phoA gene. We first identify the mineralization conditions of biofilms grown on nutritive agar substrates supplemented with calcium ions and {beta}-glycerophosphate. We then localize the mineral phase at different scales, using light and scanning electron microscopy as well as X-ray microtomography. Wide-angle X-ray scattering enables us to further identify the mineral as being hydroxyapatite. Finally, growing E. coli cells on mineralizing medium supplemented with an ALP inhibitor demonstrates that ALP is essential for biofilm mineralization. This is confirmed with a bacteria-free model, where the deposition of a drop of bacterial ALP solution on calcium and {beta}-glycerophosphate containing agar substrate is sufficient to induce mineralization. Overall, these results will benefit the development of strategies against diseases involving calcified biofilms as well as the engineering of biofilm-based living composites.

microbiology↗

bioRxiv2022

Gradients of orientation, composition and hydration of proteins for efficient light collection by the cornea of the horseshoe crab

The lateral eyes of the horseshoe crab, Limulus polyphemus, are the largest compound eyes within recent Arthropoda. While this visual system has been extensively described before, the precise mechanism allowing vision has remained controversial. Correlating quantitative refractive index (RI) mapping and detailed structural analysis, we demonstrate how gradients of RI in the cornea result from the hierarchical organization of chitin-protein fibers, heterogeneity in protein composition and bromine doping, as well as spatial variation in water content. Combining the realistic cornea structure and measured RI gradients with full-wave optical modelling and ray-tracing approaches, we show that the light collection mechanism depends on both refraction-based graded index (GRIN) optics and total internal reflection. The optical properties of the cornea are governed by different mechanisms at different hierarchical levels, demonstrating the remarkable versatility of arthropod cuticle. One-sentence summaryStructural hierarchy and protein hydration determine the optical performance of the cornea of L. polyphemus.

biophysics↗

bioRxiv2021

Spores and extracellular matrix components impart molecular order in Bacillus subtilis biofilms.

Biofilms are multicellular microbial communities that encase themselves in an extracellular matrix (ECM) of secreted biopolymers and attach to surfaces and interfaces. Bacterial biofilms are detrimental in hospital and industrial settings, but they can be beneficial in agricultural contexts. An essential property of biofilms that grants them with increased survival relative to planktonic cells is phenotypic heterogeneity; the division of the biofilm population into functionally distinct subgroups of cells. Phenotypic heterogeneity in biofilms can be traced to the cellular level, however, the molecular structures and elemental distribution across whole biofilms as well as possible linkages between them remain unexplored. Mapping X-ray diffraction (XRD) across intact biofilms in time and space, we revealed the dominant structural features in Bacillus subtilis biofilms, stemming from matrix components, spores and water. By simultaneously following the X-ray fluorescence (XRF) signal of biofilms and isolated matrix components, we discovered that the ECM preferentially binds calcium ions over other metal ions, specifically, zinc, manganese and iron. These ions, remaining free to flow below macroscopic wrinkles that act as water channels, eventually accumulate and lead to sporulation. The possible link between ECM properties, regulation of metal ion distribution and sporulation across whole intact biofilms unravels the importance of molecular-level heterogeneity in shaping biofilm physiology and development. Significance StatementBiofilms are multicellular soft microbial communities that are able to colonize synthetic surfaces as well as living organisms. To survive sudden environmental changes and efficiently share their common resources, cells in a biofilm divide into subgroups with distinct functions, leading to phenotypic heterogeneity. Here, by studying intact biofilms by synchrotron X-ray diffraction and fluorescence, we revealed correlations between biofilm macroscopic architectural heterogeneity and the spatio-temporal distribution of extracellular matrix, spores, water and metal ions. Our findings demonstrate that biofilm heterogeneity is not only affected by local genetic expression and cellular differentiation, but also by passive effects resulting from the physicochemical properties of the molecules secreted by the cells, leading to differential distribution of nutrients that propagates through macroscopic length scales.

microbiology↗