Scientists at IOCB Prague are uncovering new details of gene transcription. They have identified a previously unknown molecular mechanism by which the transcription of genetic information from deoxyribonucleic acid (DNA) into ribonucleic acid (RNA) can be initiated. The researchers focused on a specific class of molecules known as alarmones, which are found in cells across a wide range of organisms and whose levels often increase under conditions of cellular stress. The results were published in the prestigious scientific journal Nature Chemical Biology.<img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_bc2bfffa6c.jpg" alt="IOCB Prague/Tomáš Belloň: Research from IOCB Prague reveals a previously unknown mechanism of genetic transcription: Dr. Hana Cahová, head of the Chemical Biology of Nucleic Acids research group." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_bc2bfffa6c.jpg 234w," sizes="100vw" width="2000" height="1335"><div>Molecules of ribonucleic acid can carry a variety of chemical modifications at one end, known as caps. In eukaryotic organisms, including human cells, the best-known cap plays an important role in RNA stability and in regulating its subsequent fate. In recent years, however, it has become clear that alternative, non-canonical RNA caps also exist, although their formation and the mechanisms by which they are attached to RNA remain only partially understood. These include alarmone caps, formed by dinucleoside polyphosphate molecules, that protect cellular RNA at moments when the cell is under threat.In their study, <a target="_blank" rel="noopener noreferrer" href="https://cahova.group.uochb.cz/en">Dr. Hana Cahová</a> and colleagues examined bacterial RNA polymerase and investigated how this enzyme can initiate transcription using dinucleoside polyphosphates (NpNs) instead of the standard RNA building blocks. For the first time, the scientists described, at the atomic level, how RNA bearing an alarmone cap can be generated directly at the initiation of gene transcription. They also observed that NpNs bind through a different type of base pairing than is typically observed.The work was significantly shaped by Valentina Serianni from Hana Cahová’s team, who demonstrated the ability of dinucleoside polyphosphates to initiate gene transcription, and by Jana Škerlová, who focused on the structural analysis of RNA polymerase. Using cryogenic electron microscopy data, she showed how dinucleoside polyphosphate molecules bind within the active site of RNA polymerase – that is, the core of the enzyme where genetic information is transcribed. Together, their findings help to elucidate the processes that accompany the transcription of genetic information from DNA to RNA.Hana Cahová adds: “We’re describing something that truly occurs in cells and that we’re now able to observe directly at the level of individual molecules. This allows us to answer fundamental questions about cellular processes, such as how cells adapt to stress. RNA plays a central role in this, as it carries the cascade of information underlying any cellular response – for example, to threatening conditions caused by nutrient deprivation or temperature shock.”<img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_2_0fe88ff9e9.jpg" alt="IOCB Prague/Tomáš Belloň: Research from IOCB Prague reveals a previously unknown mechanism of genetic transcription: Dr. Tomáš Kouba, head of the Cryogenic Electron Microscopy core facility." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_2_0fe88ff9e9.jpg 234w," sizes="100vw" width="2000" height="1335"><div>Cryogenic electron microscopy (cryo-EM) was central to the project. This part of the work was led by Dr. Tomáš Kouba, one of the authors of the study. “Cryogenic electron microscopy allows us to freeze biological molecules in a state very close to their natural form and then determine their three-dimensional structure. This makes it possible to look directly into the active centers of enzymes and observe their function down to the atomic level,” he explains.Last year, IOCB Prague opened a new <a target="_blank" rel="noopener noreferrer" href="https://cryoem.group.uochb.cz/en">cryo-EM center</a> that is unique within the Czech research environment. State-of-the-art cryogenic electron microscopes are housed in a specially designed building and enable the study of biological processes with exceptional structural precision.<img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_3_4d881e7a58.jpg" alt="IOCB Prague: Research from IOCB Prague reveals a previously unknown mechanism of genetic transcription: This work shows how NpnNs initiate bacterial transcription. Cryo-EM reveals how nucleobases pair with the template: one in canonical and one in reverse Watson–Crick mode, providing a structural basis for their function as non-canonical RNA caps." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_UOCHB_Vyzkum_z_UOCHB_odhaluje_dosud_nepoznany_zpusob_prepisu_geneticke_informace_3_4d881e7a58.jpg 245w," sizes="100vw" width="2000" height="1077"><blockquote><h4>The Original article</h4><h4><a target="_blank" rel="noopener noreferrer" href="https://www.nature.com/articles/s41589-025-02134-5">Molecular insight into 5′ RNA capping with NpnNs by bacterial RNA polymerase</a></h4>Valentina M. Serianni, Jana Škerlová, Anna Knopp Dubánková, Anton Škríba, Hana Šváchová, Tereza Vučková, Anatolij Filimoněnko, Milan Fábry, Pavlína Řezáčová, Tomáš Kouba &amp; Hana Cahova&nbsp;Nat. Chem. Biol. 21 (2026)<a target="_blank" rel="noopener noreferrer" href="https://doi.org/10.1038/s41589-025-02134-5">https://doi.org/10.1038/s41589-025-02134-5</a><h6>licensed under <a target="_blank" rel="noopener noreferrer" href="https://creativecommons.org/licenses/by/4.0/">CC-BY 4.0</a></h6></blockquote><h4>Abstract</h4>RNA capped with dinucleoside polyphosphates has been discovered in bacteria and eukaryotes only recently. The likely mechanism of this specific capping involves direct incorporation of dinucleoside polyphosphates by RNA polymerase as noncanonical initiating nucleotides. However, how these compounds bind into the active site of RNA polymerase during transcription initiation is unknown. Here, we explored transcription initiation in vitro, using a series of DNA templates in combination with dinucleoside polyphosphates and model RNA polymerase from Thermus thermophilus. We observed that the transcription start site can vary on the basis of the compatibility of the specific template and dinucleoside polyphosphate. Cryo-electron microscopy structures of transcription initiation complexes with dinucleoside polyphosphates revealed that both nucleobase moieties can pair with the DNA template. The first encoded nucleotide pairs in a canonical Watson–Crick manner, whereas the second nucleobase pairs noncanonically in a reverse Watson–Crick manner. Our work provides a structural explanation of how dinucleoside polyphosphates initiate RNA transcription.</div></div>

Research from IOCB Prague reveals a previously unknown mechanism of genetic transcription

In the week from February 9, the following webinars await you in the field of atomic and molecular spectroscopy and spectrometry<blockquote><h4><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinars">👉 DETAILS AND REGISTRATION IN THE WEBINARS SECTION</a></h4>👉 Search and filter in the largest global database with over 5 000 GC, LC, MS and spectroscopy webinars.</blockquote><h5>1. Thermo Fisher Scientific: Process Raman – A Reliable and Versatile Tool for Downstream Process Monitoring and Control for mAb Production</h5><ul><li>Tu, 10.2.2026 16:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/5808">Registration</a></li></ul>The presentation highlights how process Raman spectroscopy offers several advantages over traditional in-line UV-Vis analysis for process monitoring and metabolite production control.<h5>2. Bruker: Meet Compact-Q DEER Spectrometer – Your Gateway to Quantum Innovation</h5><ul><li>Tu, 10.2.2026 17:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/5757">Registration</a></li></ul>Discover how the Compact-Q DEER spectrometer enables high-fidelity qubit characterization and control, combining advanced microwave architecture, AWGs, and cryogen-free operation.<h5>3. Agilent Technologies: Novel Advancements in Trace Level Determination and Long-Term Stability of Metals in TMAH and UPW Matrices</h5><ul><li>Tu, 10.2.2026 21:30 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/3733">Registration</a></li></ul>Explore novel approaches for trace-level metal determination and long-term stability assessment in TMAH and ultrapure water matrices.<h5>4. AZoM: From First to Best – Introducing the Litesizer DIF Series</h5><ul><li>We, 11.2.2026 15:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/5765">Registration</a></li></ul>Join this live webinar introducing the new Litesizer DIF series of laser diffraction particle size analyzers.<h5>5. Anton Paar: Polymer Rheology – Rotational and Transient Measurements on a Polymer Melt</h5><ul><li>We, 11.2.2026 18:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/5786">Registration</a></li></ul>Learn how rotational and transient viscosity measurements on rotational rheometers reveal polymer melt flow behavior, from method setup and accessories to data interpretation.<h5>6. Milestone: Practical Guidance to Improve the Journey from Sample to Heavy Metals Analysis for Environmental Labs</h5><ul><li>Th, 12.2.2026 16:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/5803">Registration</a></li></ul>Improve heavy metals analysis in environmental laboratories with practical tips on reagents, filtration, cleaning, and workflow optimization to enhance data quality and efficiency.<h5>7. Agilent Technologies: Moving from R&amp;D and Limited QC on a UV-Vis-NIR Instrument to Large-Scale QC Using an Autosampler</h5><ul><li>Th, 12.2.2026 20:00 CET</li><li><a target="_blank" rel="noopener noreferrer" href="https://icpms.labrulez.com/webinar/2104">Registration</a></li></ul>This presentation covers key aspects of adding and using an autosampler to maximize UV-Vis-NIR QC workflows when scaling from R&amp;D to routine quality control.

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LA-ICP-MS imaging, particularly in TOF mode, provides rapid, high-resolution elemental maps of complex geological materials, but quantitative accuracy is often limited by heterogeneous mineralogy. This study introduces a workflow using UMAP for unsupervised dimensionality reduction combined with k-means clustering to segment mineral phases directly from per-pixel elemental data.Cluster compositions are matched to known minerals based on stoichiometry, allowing phase-specific normalization and reducing quantification errors by up to 60%. Validated on dawsonite-bearing sandstones, the approach enables consistent phase-resolved geochemical comparisons across depth profiles and establishes UMAP as a practical tool for accurate, interpretable multielement imaging.<blockquote><h4>The original article</h4><h4><a target="_blank" rel="noopener noreferrer" href="https://pubs.acs.org/doi/10.1021/acs.analchem.5c05398">Mineral Phase-Resolved Quantification in LA-ICP-MS Imaging</a></h4>Barbara Umfahrer, Jakub Buday, Pavel Pořízka, Jozef Kaiser, Paolo S. Garofalo*, and Detlef Günther*Anal. Chem. 2026, 98, 1, 581–589<a target="_blank" rel="noopener noreferrer" href="https://doi.org/10.1021/acs.analchem.5c05398">https://doi.org/10.1021/acs.analchem.5c05398</a><h6>licensed under <a target="_blank" rel="noopener noreferrer" href="https://creativecommons.org/licenses/by/4.0/">CC-BY 4.0</a></h6></blockquote>Selected sections from the article follow. Formats and hyperlinks were adapted from the original.Since its introduction in 1985, <a href="javascript:void(0);">(1)</a> Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS) has matured into a routine technique for both qualitative and quantitative elemental analysis, finding use in diverse fields such as geology, <a href="javascript:void(0);">(2−4)</a> biology, <a href="javascript:void(0);">(5,6)</a> materials science, <a href="javascript:void(0);">(7)</a> and cultural heritage. <a href="javascript:void(0);">(8,9)</a> Especially in comparison to liquid analysis techniques, the method excels through minimal sample preparation, negligible sample destruction, and low limits of detection, which enable trace element analysis. However, besides the availability of standard reference materials, a longstanding challenge of quantitative LA-ICP-MS is the need for a suitable internal standard to account for variations in ablation rate and transport efficiency, as well as instrumental drift. <a href="javascript:void(0);">(10)</a> Developed for applications in geological matrices, this requirement was elegantly circumvented by Liu et al. <a href="javascript:void(0);">(11)</a> through 100 wt % normalization, which assumes that all detected elements form oxides summing up to 100 wt %. This approach was conceptually inspired by the summed-spectrum normalization calibration procedure introduced by Leach and Hieftje in 2000, which emphasized the use of total signal intensities for robust internal standardization. <a href="javascript:void(0);">(12)</a> The 100 wt % normalization strategy was subsequently extended to the bulk analysis of carbonates. <a href="javascript:void(0);">(13)</a>Concurrently, the advent of time-of-flight (TOF) mass analyzers and the development of fast-washout laser ablation cells <a href="javascript:void(0);">(14−16)</a> have transformed LA-ICP-MS into a powerful imaging tool, capable of generating spatial maps across a variety of sample matrices at high data acquisition rates. <a href="javascript:void(0);">(17−19)</a> Furthermore, in comparison to, e.g., X-ray fluorescence spectroscopy (XRF) or Scanning Electron Microscopy with Energy-Dispersive X-ray Spectroscopy (SEM-EDS), LA-ICP-MS offers a high depth resolution of approximately 0.2 μm on glass, enabling precise measurement of fine-scale structures not only laterally but also in depth. <a href="javascript:void(0);">(18)</a> However, as the volume and complexity of these elemental images have grown according to the progressive advancement of the method itself, now consisting of gigabytes of data produced within minutes, manual data interpretation has become increasingly impractical. To uncover meaningful details and patterns, researchers have applied multivariate methods such as Principal Component Analysis (PCA) and k-means clustering to reduce dimensionality and delineate distinct regions within the images. <a href="javascript:void(0);">(20−23)</a> The nonlinear dimensionality reduction technique Uniform Manifold Approximation and Projection (UMAP), <a href="javascript:void(0);">(24)</a> which supports data interpretation with its capability to capture and separate subtle local structures, has first been employed to LA-ICP-MS bulk analysis data in 2024, where it was used to classify pyrite samples and discriminate between Pb and Zn deposit types. <a href="javascript:void(0);">(25,26)</a> In combination with elemental imaging, UMAP has recently been applied to biological tissue data sets as an exploratory analysis tool, <a href="javascript:void(0);">(27)</a> further enhancing the ability to visualize and interpret complex elemental distributions.Despite these advances, no existing approach combines the unsupervised segmentation of mineral phases by UMAP with phase-specific normalization. In this study, we introduce a UMAP-driven workflow that (1) automatically segments distinct mineralogical phases within fine-grained geological matrices and (2) applies phase-specific 100 wt % normalization (e.g., oxide <a href="javascript:void(0);">(11)</a> or carbonate <a href="javascript:void(0);">(13)</a>), thereby improving quantification accuracy and enabling phase-specific quantitative interpretation of mineral distributions in complex matrices.<h4>Materials and Methods</h4><h5>LA-ICP-TOFMS Imaging</h5>LA-ICP-TOFMS analyses were performed using a 193 nm ArF excimer laser (GeoLas C, Lambda Physik, Göttingen, Germany) coupled to an ICP-TOFMS instrument (icpTOF 2R, TOFWERK AG, Thun, Switzerland). Ablation was conducted in the modified parallel flow ablation cell (MPFAC) <a href="javascript:void(0);">(16,34)</a> under a He atmosphere (99.999%, Linde Gas Schweiz AG, Dagmersellen, Switzerland) with Ar (99.996%, Linde Gas Schweiz AG) used as the carrier gas. A piezoelectrically driven xyz translational stage (1 nm resolution, SmarAct GmbH, Oldenburg, Germany) enabled precise sample positioning. Laser, stage movement, and ICP-TOFMS data acquisition were synchronized using a custom-built imaging control system. <a href="javascript:void(0);">(19)</a> The system was optimized each day based on maximum sensitivity while ensuring a 238U+/232Th+ intensity ratio of 1.0 to 1.1 on NIST SRM 610 and a 232Th16O+/232Th+ rate of below 0.5%.<h5>LIBS Imaging</h5>The LIBS analyses were performed on a Firefly system (Lightigo, Czech Republic). The laser (1064 nm, 5 mJ, pulse duration ∼10 ns, diameter 6 mm, operating at 50 Hz) was focused on the sample with a singlet lens (focal length 50 mm) to a 30 μm spot. The spatial resolution of the acquired elemental maps, with a size of about 16 mm × 26 mm, was 20 μm. Plasma radiation is collected by a multifiber configuration with a collimator and an optical fiber (400 μm core diameter), which delivered the light to several Czerny–Turner spectrometers (resolution 0.25–0.4 nm). The spectral range of the spectrometers is 180–850 nm. The radiation is collected 1.5 μs after ablation, with a gate width of 15 μs.Data processing was done with Python 3.11.8 in the Spyder environment and included background correction and per-pixel z-score normalization.<h4>Results and Discussion</h4><h5>LIBS and XRD Measurements</h5>To assess whether carbonate-based normalization <a href="javascript:void(0);">(13)</a> is warranted, first, large-scale LIBS elemental intensity maps of the samples across about a third of the thin sections were acquired. <a target="_blank" rel="noopener noreferrer" href="https://pubs.acs.org/doi/10.1021/acs.analchem.5c05398#fig1">Figure 1</a> reveals the results for “Layer 2” of the Poggio del Gatto sandstone for selected elements. A complete mapping of all four thin sections can be found in <a target="_blank" rel="noopener noreferrer" href="https://pubs.acs.org/doi/suppl/10.1021/acs.analchem.5c05398/suppl_file/ac5c05398_si_001.pdf">Figures S3 and S6</a> in the Supporting Information. The maps reveal that C is strongly enriched in fracture veins as well as in finer-grained domains within the matrix and correlates with Ca, indicating carbonate minerals rather than oxides. Bulk XRD analysis identifies calcite alongside quartz, plagioclase, white mica, and kaolinite. These complementary observations confirm calcite as a major phase and thus justify the need for performing the 100 wt % normalization on a carbonate basis for pixels representing calcite.<img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Anal_Chem_2026_98_1_581_589_Figure_1_LIBS_elemental_intensity_maps_of_the_data_set_from_Layer_2_of_the_Poggio_del_Gatto_sandstone_mounted_on_a_microscope_slide_73ada1b7b8.jpg" alt="Anal. Chem. 2026, 98, 1, 581–589: Figure 1. LIBS elemental intensity maps of the data set from “Layer 2” of the Poggio del Gatto sandstone mounted on a microscope slide, depicting calcite veins and fine-grained structures within the matrix, underlining the need for carbonate-based normalization for specific pixels. Emission lines for evaluation are shown in the corresponding subfigure title. The epoxy used to fix the thin section on the slide is visible along the margin." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Anal_Chem_2026_98_1_581_589_Figure_1_LIBS_elemental_intensity_maps_of_the_data_set_from_Layer_2_of_the_Poggio_del_Gatto_sandstone_mounted_on_a_microscope_slide_73ada1b7b8.jpg 245w," sizes="100vw" width="2088" height="414"><h5>Renormalization Based on Carbonates</h5>Applying an oxide-based normalization to carbonate samples will introduce composition-dependent biases that cannot immediately be generalized as a singular numerical value. The difference between the molecular masses of carbonate CO32– and its oxide equivalent O2– yields an intrinsic bias on the order of a factor of about two, depending on the stoichiometry. Once this data is renormalized to a total of 100 wt %, the magnitude of the error becomes highly dependent on the specific elemental composition of the sample. An exemplary calculation illustrating this effect for a representative calcite pixel is provided in <a target="_blank" rel="noopener noreferrer" href="https://pubs.acs.org/doi/suppl/10.1021/acs.analchem.5c05398/suppl_file/ac5c05398_si_001.pdf">Table S2</a>, yielding a relative error of 79%. In practice, this error varies across the image according to the local phase composition. <a target="_blank" rel="noopener noreferrer" href="https://pubs.acs.org/doi/10.1021/acs.analchem.5c05398#fig6">Figure 6</a> illustrates the impact of normalization approaches for layer 2 of the samples as well as the spatial distribution of the resulting relative error. The figure presents Ca and Si elemental maps in two rows, while the first three columns compare different normalization strategies: normalization based on all oxides, normalization based on all carbonates, and a pixel-wise normalization guided by mineral phase identification, as outlined in the workflow proposed in this study. The final column displays the relative error between the bulk oxide- or carbonate-based normalization and the pixel-wise, phase-informed normalization.<img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Anal_Chem_2026_98_1_581_589_Figure_6_Comparison_of_normalization_strategies_for_Ca_and_Si_LA_ICP_TOFMS_elemental_maps_in_Layer_2_ce3a0c1a5c.jpg" alt="Anal. Chem. 2026, 98, 1, 581–589: Figure 6. Comparison of normalization strategies for Ca and Si LA-ICP-TOFMS elemental maps in “Layer 2” of the Poggio del Gatto sandstone. Rows show Ca (top) and Si (bottom); columns compare (1) oxide-based normalization, (2) carbonate-based normalization, (3) pixel-wise, phase-informed normalization (this study), and (4) relative error between the first two and the phase-informed approach." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Anal_Chem_2026_98_1_581_589_Figure_6_Comparison_of_normalization_strategies_for_Ca_and_Si_LA_ICP_TOFMS_elemental_maps_in_Layer_2_ce3a0c1a5c.jpg 202w," sizes="100vw" width="2088" height="1622">For Ca (in this matrix primarily associated with calcite, a dominant carbonate phase in our samples), the relative error depicted quantifies the effect of applying oxide-based normalization across the entire image. This results in a systematic overestimation of the Ca concentration by approximately 60%. Conversely, for Si─in this matrix found mainly in quartz and various plagioclase phases─the error is shown for applying carbonate-based normalization across an oxidic matrix. In such cases, the Si concentrations are underestimated by roughly 10% to 40%, depending on the mineral phase.These findings highlight that using a single normalization scheme across heterogeneous samples introduces substantial quantification errors. To mitigate this, the pixel-wise phase segmentation enabled by the proposed UMAP-based workflow offers a significant advantage, especially in fine-grained matrices. In short, phase-aware, pixel-wise normalization combines the strengths of both normalization approaches and proves to be highly beneficial.<h4>Conclusion</h4>This study demonstrates that phase-specific normalization, guided by unsupervised phase segmentation of LA-ICP-MS images, can substantially improve the accuracy of elemental quantification in fine-grained geological matrices. Rather than relying on a single global assumption (e.g., all oxides or all carbonates), the workflow adapts normalization to the actual mineralogy, minimizing systematic errors and enabling phase-resolved geochemical interpretation.The segmentation step, based on UMAP embedding and k-means clustering, is fully unsupervised. However, the subsequent matching of clusters to specific minerals still relies on a limited set of preidentified stoichiometries and is therefore not yet fully unsupervised. Expansion to larger stoichiometric databases could help overcome this limitation and move toward automated mineral classification. A key challenge remains the similarity of cation ratios in certain mineral groups, which may still require complementary data to ensure robust assignments.Overall, beyond the specific case of the Poggio del Gatto sandstone presented in this study, this work provides a framework for quantitative elemental imaging of complex geological samples and is readily transferable to other contexts that require spatially resolved composition-aware normalization. This contribution adds a practical implementation to a growing literature that already uses multivariate statistics to unlock the immense information depth of LA-ICP-TOFMS.

Mineral Phase-Resolved Quantification in LA-ICP-MS Imaging

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The Institute of Organic Chemistry and Biochemistry of the Czech Academy of Sciences (IOCB Prague) is a leading scientific institution in the Czech Republic, recognized internationally. Its primary mission is basic research in the fields of chemical biology and medicinal chemistry, organic and material oriented chemistry, chemistry of natural compounds, biochemistry and molecular biology, physical chemistry, theoretical chemistry, and analytical chemistry. 

Institute of Organic Chemistry and Biochemistry of the Czech Academy of Sciences

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Thermo Scientific IonicX Portable XRF Analyzer

Thermo Scientific™ IonicX enables fast and accurate salt analysis in raw materials using portable XRF without complex preparation or destructive testing.

<div><div>Identify ionic salts in seconds with minimal sample preparation. The Thermo Scientific™ IonicX™ Portable XRF Analyzer provides:<ul><li>Fast and accurate verification of ionic salt raw materials</li><li>High sample throughput for pharmaceutical and biopharmaceutical manufacturers</li></ul>Cut testing time and costs by replacing:<ul><li>time-consuming</li><li>resource-intensive</li><li>wet chemistry and benchtop methods</li></ul>with a ✅ non-destructive, ✅ non-contact, ✅ portable XRF analyzer for ionic salts.<h3>⚙️ Key Features</h3><ul><li>Portable verification of a wide range of ionic salts in seconds</li><li>Compliant with 21 CFR Part 11:<ul><li>electronic signatures</li><li>user access control</li><li>audit trails</li></ul></li><li>Non-destructive testing of raw materials</li><li>Minimal sample preparation</li><li>Simple operation, no extensive operator training required</li><li>Lightweight and compact design for easy portability</li><li>Wi-Fi enabled</li><li>Hot Swap Battery</li><li>IP54 Certified – splash and dust proof</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_Ionic_X_Portable_XRF_Analyzer_2_aa24221e46.jpg" alt="Thermo Scientific™ IonicX Portable XRF Analyzer " srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_Ionic_X_Portable_XRF_Analyzer_2_aa24221e46.jpg 156w," sizes="100vw" width="650" height="650"><h3>📏&nbsp;Specifications</h3><ul><li>Bluetooth: Supports print functionality and barcode reader</li><li>Camera:<ul><li>Macro Camera: Integrated CCD macro camera for capturing overview images of parts and tagging measurement locations</li><li>Micro Camera: Integrated CCD micro camera for locating and recording measurement positions</li></ul></li><li>Certifications/Compliance:&nbsp;<ul><li>EN 55011:2010</li><li>EN 61326:2013</li><li>FCC 47 CFR Part 15</li><li>Safety EN 61010; 2010 (3rd Ed) with national deviations for US and Canada</li><li>RoHS EN 50581; 2012</li></ul></li><li>Data Entry:&nbsp;<ul><li>Touchscreen keyboard</li><li>User customizable data entry</li><li>Optional wireless remote barcode reader</li></ul></li><li>Data Storage:&nbsp;<ul><li>512 MB internal system memory/16 GB industrial grade storage</li><li>Stores approximately 130,000 readings with spectra (fewer if macro and micro images are saved)</li></ul></li><li>Data Transfer: Wi-Fi, USB</li><li>Dimensions: 12 × 12 × 8 in. (30.48 × 30.48 × 20.32 cm)</li><li>Display Type: Tilting, color, resistive touchscreen display</li><li>IP Rating: IP54 (splash and dust proof)</li><li>Languages: English</li><li>Licensing: Varies by region; Contact your local distributor</li><li>Operating Environment:&nbsp;<ul><li>Temperature: 0°C to 50°C (external fan recommended when ambient temperature is greater than 33°C)</li><li>Humidity: 10% to 90% relative humidity non-condensing</li></ul></li><li>Operating System: Linux</li><li>Optional Accessories:&nbsp;<ul><li>Thermo Scientific portable test stand</li><li>Thermo Scientific mini test stand</li></ul></li><li>Power Consumption: 12V lithium-ion battery, or 12V DC, 3A, 3.6W power supply</li><li>Security Features: Password-protected user security</li><li>Software: IonicX PC software</li><li>Spot Size: Standard: 8 mm collimation</li><li>Standard Accessories:&nbsp;<ul><li>Locking shielded carrying case</li><li>Two (2) lithium-ion battery packs</li><li>One (1) 110/220 VAC battery charger/AC adaptor</li><li>Check samples</li><li>Safety lanyard</li><li>PC connection cable (USB)</li></ul></li><li>System Details: Built-in standardization via automatic system check</li><li>Weight (English): 5.8 lbs. with battery and test stand</li><li>Weight (Metric): 2.6 kg with battery and test stand</li><li>X-Ray Source Type:&nbsp;<ul><li>X-Ray Tube: Ag anode (6–50 kV, 0–500 μA, 5W max)</li><li>Dynamically adjustable current for optimal sensitivity on every analysis</li></ul></li><li>Applications: Raw Material Testing</li><li>Detector Type: Proprietary Large Area Drift Detector</li><li>Tube Voltage: 6 to 50 kV</li><li>Unit Size: Each</li></ul></div></div>

Thermo Scientific ARL EQUINOX 100 X-ray Diffractometer

The ARL EQUINOX 100 is a compact benchtop XRD for QC, research, and routine use. It captures full diffraction patterns in real time with a CPS detector — no moving parts or scanning needed.

<h4>Compact, powerful, and flexible benchtop XRD system for routine and advanced applications</h4>The ARL EQUINOX 100 is a compact benchtop X-ray diffractometer (XRD) designed for quality control, academic research, and routine analysis. It features a unique curved position-sensitive (CPS) detector that enables real-time acquisition of the entire diffraction pattern — with no moving parts and no scanning required.<h3>Key Features</h3><ul><li>Real-time acquisition: entire diffraction pattern captured in seconds</li><li>Wide angular range: up to 110° 2θ without moving components</li><li>No external water cooling: no chiller required</li><li>Standard power outlet: plug-and-play with no special electrical setup</li><li>Low-power microfocus X-ray source: high intensity and efficient optics</li><li>Versatile measurement: reflection and transmission modes</li><li>Easy installation: suitable for labs, mobile labs, and field vans</li></ul><h3>Sample Handling &amp; Accessories</h3><ul><li>Fixed non-spinning sample stage</li><li>Spinning stages for powders, bulks, filters, and pressed pellets</li><li>Capillary sample stage for transmission mode</li><li>Controlled atmosphere sample stage</li><li>6-position automatic sample changer</li><li>Dedicated stage for thin film analysis (GIXRD, XRR)</li><li>Temperature-controlled stages (–10 °C to 500 °C)</li></ul><h3>Typical Applications</h3><ul><li>Phase identification and quantification</li><li>Degree of crystallinity, crystallite size, and lattice parameters</li><li>Crystal structure solutions and Rietveld refinement</li><li>Thin film characterization (GIXRD, XRR)</li><li>In-situ and dynamic studies (e.g., phase transitions)</li><li>Fields: materials science, geology, nanomaterials, chemistry, pharmaceuticals, metallurgy, teaching</li></ul><h3>Software &amp; Compliance</h3><ul><li>SolstiX™ XRD Software with 21 CFR Part 11 compliance</li><li>Electronic signatures, audit trails, secured data handling — ideal for pharmaceutical QA/QC environments</li></ul><h3>Why Choose ARL EQUINOX 100?</h3><ul><li>Simultaneous, real-time data acquisition</li><li>Compact, rugged, and mobile-ready design</li><li>High performance at low operating cost</li><li>Flexible platform for a broad range of samples and applications</li></ul>

Thermo Scientific ARL EQUINOX 1000 Benchtop X-Ray Diffractometer

The Thermo Scientific™ ARL™ EQUINOX 1000 enables ultra-fast XRD with a unique curved detector capturing all diffraction peaks at once, delivering complete analysis in just minutes.

The Thermo Scientific™ ARL™ EQUINOX 1000 offers very fast measurements compared to other diffractometers due to our unique EQUINOX curved detector that can measure all diffraction peaks simultaneously across a wide angular range. It will take you just a few minutes on most samples to get a complete analysis regardless of your resolution requirements.<ul><li>Research</li><li>Environment</li><li>Geology, Cement, Mining</li><li>Metallurgy</li><li>Pharmaceuticals</li><li>Education</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_ec89ff8753.jpg" alt="Thermo Scientific ARL EQUINOX 1000 Benchtop X-Ray Diffractometer: No scanning required. Measures the whole 2 theta range simultaneously and in real time." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_ec89ff8753.jpg 245w," sizes="100vw" width="800" height="361">The ARL EQUINOX 1000 is a rugged multi-purpose benchtop style instrument designed for QA/QC, academic and routine X-ray diffraction applications. The ARL EQUINOX 1000 is the perfect instrument when space becomes a priority. With its truly excellent performance it is the perfect match for laboratories that are looking for a simple and powerful benchtop X-ray diffractometer. Several sample holders are available on this instrument such as a 6 or 30 positions sample holder, powder transmission mode sample holders, small thin film sample attachment.<ul><li>Real time acquisition</li><li>Easy to use</li><li>No alignment needed</li><li>Very reliable</li><li>Superb resolution</li><li>No maintenance &nbsp;</li><li>You want to perform transmission analysis? Choose either the Sample Spinner for reflection and transmission analysis on powder samples or the capillary sample holder for Transmission mode analysis depending on your needs.</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_2_2d447eb239.jpg" alt="Thermo Scientific ARL EQUINOX 1000 Benchtop X-Ray Diffractometer" srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_2_2d447eb239.jpg 245w," sizes="100vw" width="1074" height="286"><ul><li>You need to analyze several powder samples a day? Optimize your throughput with the 6 or 30 position sample changer. &nbsp;</li><li>You need to perform grazing incidence measurement on small samples? Try our Small Thin Layer analysis attachment.</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_3_7b095f3848.jpg" alt="Thermo Scientific ARL EQUINOX 1000 Benchtop X-Ray Diffractometer: Silver Behenate powder sample recorded on EQUINOX 1000 in reflection mode." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_3_7b095f3848.jpg 245w," sizes="100vw" width="871" height="450"><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_4_4ef24412ee.jpg" alt="Thermo Scientific ARL EQUINOX 1000 Benchtop X-Ray Diffractometer: Si powder sample recorded on ARL EQUINOX 1000 in reflection mode." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_1000_Benchtop_X_Ray_Diffractometer_4_4ef24412ee.jpg 245w," sizes="100vw" width="871" height="452"><h3>Specification</h3><ul><li>X-ray source: Generator: 3500 W (60kV / 60mA - Option 30kV limitation) Cu, Co - Standard sealed X-ray tube</li><li>Detector: Curved Position Sensitive X-ray Detector, CPS 180 Curvature radius: 180mm Acquisition in real time over 110° 2Theta</li><li>Goniometric table: No moving parts: acquisition in asymmetric mode</li><li>Sample holders:&nbsp;<ul><li>Fixed, with or without sample rotation&nbsp;</li><li>Reflection or transmission mode&nbsp;</li><li>Zero background sample cup&nbsp;</li><li>Sample changer: 6 or 30 positions&nbsp;</li><li>Thin layer attachment</li></ul></li><li>Optic: Monochromatic (Germanium, Graphite)</li><li>Computer: Windows© 8, 7 Vista, XP</li><li>Software:&nbsp;<ul><li>Real time diffractogram display&nbsp;</li><li>Multiple and automatic recording&nbsp;</li><li>Peak search&nbsp;</li><li>Deconvolution with several shapes&nbsp;</li><li>Phase indentification and quantification&nbsp;</li><li>Degree of crystallinity determination&nbsp;</li><li>Cell parameters, crystallite size, lattice strain&nbsp;</li><li>Crystal structure analysis&nbsp;</li><li>Rietveld analysis&nbsp;</li><li>Free open database for search match&nbsp;</li><li>Option: ICDD PDF2 or PDF4 databases</li></ul></li><li>Power: 30-32A / 208-230V / 50-60Hz</li><li>Weight: ~90 kg</li><li>Cooling water:&nbsp;<ul><li>Flow: ~3,5l/min&nbsp;</li><li>T°C: ~18 / 25°C</li></ul></li><li>Dimensions: 996 mm H x 715 mm D x 750 mm W</li></ul>

Thermo Scientific ARL EQUINOX 3000 Benchtop X-Ray Diffractometer

Thermo Scientific ARL EQUINOX 3000 XRD: real-time acquisition, no scanning, superb resolution, versatile sample handling, reliable and easy to use for research and industry.

The Thermo Scientific™ ARL™ EQUINOX 3000 measurements are very fast compared with other diffractometers in that the unique Inel curved detector can measure all diffraction peaks simultaneously. Due to this acquisition in real time, all kinetic studies are facilitated.The Thermo Scientific™ ARL™ EQUINOX 3500 is an evolution of ARL EQUINOX 3000 model. It is exactly the same configuration except that it works with a bigger radius of curvature detector. So, obtained data have a better resolution.<ul><li>Research</li><li>Environment</li><li>Geology, Cement, Mining</li><li>Metallurgy</li><li>Pharmaceuticals</li><li>Education</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_3_9768c30fd3.jpg" alt="Thermo Scientific ARL EQUINOX 3000 Benchtop X-Ray Diffractometer: No scanning required. Measures the whole 2 theta range simultaneously and in real time." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_3_9768c30fd3.jpg 222w," sizes="100vw" width="790" height="556">The ARL EQUINOX 3000 is a a research-grade diffractometer with a very high resolution diffraction system providing the user a choice of features including higher resolution detectors, a larger sample area and choice of X-ray sources.The free space in the sample compartment is very large and will accommodate practically any sample and any sample handling device including furnaces, auto samplers, large assemblies, etc.<ul><li>Real time acquisition</li><li>Extremely accurate</li><li>Easy to use</li><li>No alignment needed</li><li>Very reliable</li><li>Superb resolution</li><li>No maintenance &nbsp;</li><li>You want to perform transmission analysis? Choose either the Sample Spinner for reflection and transmission analysis on powder samples or the capillary sample holder for Transmission mode analysis depending on your needs. &nbsp;</li><li>You need to analyze several powder samples a day? Optimize your throughput with the 6 or 30 position sample changer. &nbsp;</li><li>You need to perform grazing incidence measurement? Try our Thin Layer analysis attachment.</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_9649c7af2e.jpg" alt="Thermo Scientific ARL EQUINOX 3000 Benchtop X-Ray Diffractometer: HTK1200N, TTK450." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_9649c7af2e.jpg 245w," sizes="100vw" width="1228" height="336"><ul><li>This system allows you to work with controlled temperature or atmosphere chamber. Anton Paar and other suppliers chambers can be availabledepending on your needs.</li></ul><img src="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_2_94015af651.jpg" alt="Thermo Scientific ARL EQUINOX 3000 Benchtop X-Ray Diffractometer: LaB6 powder sample recorded on ARL EQUINOX 3000 in reflection mode." srcset="https://storage.googleapis.com/labrulez-bucket-strapi-h3hsga3/thumbnail_Thermo_Scientific_ARL_EQUINOX_3000_Benchtop_X_Ray_Diffractometer_2_94015af651.jpg 245w," sizes="100vw" width="850" height="334"><h3>Specification</h3><ul><li>X-ray source: Generator: 3500 W (60kV / 60mA - Option 30kV limitation) Standard sealed X-ray tube: Cu, Co, Mo, ... radiation</li><li>Detector:&nbsp;<ul><li>Curved Position Sensitive X-ray Detector, CPS120&nbsp;</li><li>Curvature radius: 250mm&nbsp;</li><li>Acquisition in real time over 120° 2Theta&nbsp;</li><li>Option: CPS590 (500mm, 90° 2Theta – EQUINOX 3500)</li></ul></li><li>Goniometric table:&nbsp;<ul><li>No moving parts&nbsp;</li><li>Acquisition in asymmetric mode</li></ul></li><li>Sample holders:&nbsp;<ul><li>Fixed, with or without sample rotation&nbsp;</li><li>Reflection or transmission mode&nbsp;</li><li>Sample changer: 6 or 30 positions&nbsp;</li><li>Thin layer attachment</li></ul></li><li>Special camera:&nbsp;<ul><li>Heating camera: low and high temperature&nbsp;</li><li>Humidity chamber, Electrochemistry cell</li></ul></li><li>Optic: Monochromatic</li><li>Computer: Windows© 8, 7 Vista, XP</li><li>Software:&nbsp;<ul><li>Real time diffractogram display&nbsp;</li><li>Multiple and automatic recording&nbsp;</li><li>Peak search&nbsp;</li><li>Deconvolution with several shapes&nbsp;</li><li>Phase identification and quantification&nbsp;</li><li>Degree of crystallinity determination&nbsp;</li><li>Cell parameters, crystallite size, lattice strain&nbsp;</li><li>Crystal structure analysis&nbsp;</li><li>Transition phase&nbsp;</li><li>Thin film (reflectometry, etc.)&nbsp;</li><li>Rietveld analysis&nbsp;</li><li>Free open database for search match&nbsp;</li><li>Option: ICDD PDF2 or PDF4 databases</li></ul></li><li>Power: 30-32A / 208-230V / 50-60 Hz</li><li>Cooling water: Flow: ≈ 3,5 L/min - T°C: ≈18 to 25 °C</li><li>Dimensions:&nbsp;<ul><li>1565 mm H x 750 mm D x 1040 mm W EQUINOX 3000&nbsp;</li><li>1815 mm H x 744 mm D x 1206 mm W EQUINOX 3500</li></ul></li></ul>

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