<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Song N</submitter><funding>National Natural Science Foundation of China</funding><pagination>12885-12892</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8697359</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>11(21)</volume><pubmed_abstract>Besides geography and climate, biological factors play an important role in shaping travertine landforms, but the biochemical mechanisms of microbial processes in travertine formation have been rarely studied. Two psychrophilic bacterial strains, A20-18 and B21-3 of &lt;i>Pseudomonas psychrophila&lt;/i>, isolated from travertine pools of Huanglong, a typical alpine travertine landform, were investigated for their roles in calcium carbonate mineralization, including the deposition process and products. X-ray diffraction, Fourier-transform infrared spectroscopy, and scanning electron microscopy were used to characterize the crystal phase and morphology of CaCO&lt;sub>3&lt;/sub> precipitation. The results showed that there were no significant differences between the two strains in CaCO&lt;sub>3&lt;/sub> deposi</pubmed_abstract><journal>RSC advances</journal><pubmed_title>Carbonate biomineralization differentially induced by two psychrophilic &lt;i>Pseudomonas psychrophila&lt;/i> strains isolated from an alpine travertine landform.</pubmed_title><pmcid>PMC8697359</pmcid><funding_grant_id>41572035</funding_grant_id><funding_grant_id>41472309</funding_grant_id><funding_grant_id>41877288</funding_grant_id><pubmed_authors>Song N</pubmed_authors><pubmed_authors>Yang L</pubmed_authors><pubmed_authors>Huang Y</pubmed_authors><pubmed_authors>Li Q</pubmed_authors><pubmed_authors>Sun G</pubmed_authors><pubmed_authors>Zhou Y</pubmed_authors><pubmed_authors>Pan L</pubmed_authors><pubmed_authors>Dong P</pubmed_authors><pubmed_authors>Zhao Y</pubmed_authors><pubmed_authors>Zhao X</pubmed_authors></additional><is_claimable>false</is_claimable><name>Carbonate biomineralization differentially induced by two psychrophilic &lt;i>Pseudomonas psychrophila&lt;/i> strains isolated from an alpine travertine landform.</name><description>Besides geography and climate, biological factors play an important role in shaping travertine landforms, but the biochemical mechanisms of microbial processes in travertine formation have been rarely studied. Two psychrophilic bacterial strains, A20-18 and B21-3 of &lt;i>Pseudomonas psychrophila&lt;/i>, isolated from travertine pools of Huanglong, a typical alpine travertine landform, were investigated for their roles in calcium carbonate mineralization, including the deposition process and products. X-ray diffraction, Fourier-transform infrared spectroscopy, and scanning electron microscopy were used to characterize the crystal phase and morphology of CaCO&lt;sub>3&lt;/sub> precipitation. The results showed that there were no significant differences between the two strains in CaCO&lt;sub>3&lt;/sub> deposi</description><dates><release>2021-01-01T00:00:00Z</release><publication>2021 Mar</publication><modification>2026-05-31T06:59:56.283Z</modification><creation>2025-02-19T01:55:16.447Z</creation></dates><accession>S-EPMC8697359</accession><cross_references><pubmed>35423815</pubmed><doi>10.1039/d1ra00578b</doi></cross_references></HashMap>