<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Saw JJ</submitter><funding>National Aeronautics and Space Administration Astrobiology Institute</funding><funding>Mayo Nephrology/Urology Summer Undergraduate Research Fellowship</funding><funding>Mayo Clinic &amp;amp; Illinois Alliance for Technology-Based Healthcare</funding><funding>O’Brien Urology Research Center</funding><pagination>298-311</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8740987</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>2(2)</volume><pubmed_abstract>&lt;h4>Background&lt;/h4>Human kidney stones form &lt;i>via&lt;/i> repeated events of mineral precipitation, partial dissolution, and reprecipitation, which are directly analogous to similar processes in other natural and manmade environments, where resident microbiomes strongly influence biomineralization. High-resolution microscopy and high-fidelity metagenomic (microscopy-to-omics) analyses, applicable to all forms of biomineralization, have been applied to assemble definitive evidence of &lt;i>in vivo&lt;/i> microbiome entombment during urolithiasis.&lt;h4>Methods&lt;/h4>Stone fragments were collected from a randomly chosen cohort of 20 patients using standard percutaneous nephrolithotomy (PCNL). Fourier transform infrared (FTIR) spectroscopy indicated that 18 of these patients were calcium oxalate (CaOx) sto</pubmed_abstract><journal>Kidney360</journal><pubmed_title>&lt;i>In Vivo&lt;/i> Entombment of Bacteria and Fungi during Calcium Oxalate, Brushite, and Struvite Urolithiasis.</pubmed_title><pmcid>PMC8740987</pmcid><funding_grant_id>DK101405</funding_grant_id><funding_grant_id>DK100227</funding_grant_id><funding_grant_id>NNA13AA91A</funding_grant_id><pubmed_authors>Cregger MA</pubmed_authors><pubmed_authors>Merkel AC</pubmed_authors><pubmed_authors>Dong Y</pubmed_authors><pubmed_authors>Lieske JC</pubmed_authors><pubmed_authors>Krambeck AE</pubmed_authors><pubmed_authors>Lange D</pubmed_authors><pubmed_authors>Fields CJ</pubmed_authors><pubmed_authors>Sanford RA</pubmed_authors><pubmed_authors>Sivaguru M</pubmed_authors><pubmed_authors>Romero MF</pubmed_authors><pubmed_authors>Bruce WJ</pubmed_authors><pubmed_authors>Fouke BW</pubmed_authors><pubmed_authors>Rivera ME</pubmed_authors><pubmed_authors>Chia N</pubmed_authors><pubmed_authors>Saw JJ</pubmed_authors><pubmed_authors>Large T</pubmed_authors><pubmed_authors>Wilson EM</pubmed_authors><pubmed_authors>Bhattacharjee AS</pubmed_authors><pubmed_authors>Weber JR</pubmed_authors></additional><is_claimable>false</is_claimable><name>&lt;i>In Vivo&lt;/i> Entombment of Bacteria and Fungi during Calcium Oxalate, Brushite, and Struvite Urolithiasis.</name><description>&lt;h4>Background&lt;/h4>Human kidney stones form &lt;i>via&lt;/i> repeated events of mineral precipitation, partial dissolution, and reprecipitation, which are directly analogous to similar processes in other natural and manmade environments, where resident microbiomes strongly influence biomineralization. High-resolution microscopy and high-fidelity metagenomic (microscopy-to-omics) analyses, applicable to all forms of biomineralization, have been applied to assemble definitive evidence of &lt;i>in vivo&lt;/i> microbiome entombment during urolithiasis.&lt;h4>Methods&lt;/h4>Stone fragments were collected from a randomly chosen cohort of 20 patients using standard percutaneous nephrolithotomy (PCNL). Fourier transform infrared (FTIR) spectroscopy indicated that 18 of these patients were calcium oxalate (CaOx) sto</description><dates><release>2021-01-01T00:00:00Z</release><publication>2021 Feb</publication><modification>2025-04-22T09:14:19.558Z</modification><creation>2025-04-05T22:58:59.501Z</creation></dates><accession>S-EPMC8740987</accession><cross_references><pubmed>35373025</pubmed><doi>10.34067/KID.0006942020</doi><doi>10.34067/kid.0006942020</doi></cross_references></HashMap>