<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>16</volume><submitter>Liu R</submitter><pubmed_abstract>&lt;h4>Introduction&lt;/h4>Ammonium (NH&lt;sub>4&lt;/sub> &lt;sup>+&lt;/sup>) and nitrate (NO&lt;sub>3&lt;/sub> &lt;sup>-&lt;/sup>) are the two main forms of inorganic nitrogen (N) that exist in soil and both can be absorbed and utilized by plants. As a vast and crucial biome, soil microorganisms are responsible for mediating the inorganic N assimilation process and enhancing nitrogen use efficiency. Understanding how these microorganisms assimilate different forms of inorganic nitrogen is crucial. There are a handful of microorganisms that play a dominant role in the process of soil inorganic nitrogen assimilation and have a significant advantage in abundance. However, microbial preferences for ammonium or nitrate, as well as differences in their metabolic pathways under co-existing ammonium and nitrate conditions, re</pubmed_abstract><journal>Frontiers in microbiology</journal><pagination>1559884</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12010642</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Transcriptome analysis of nitrogen assimilation preferences in &amp;lt;i&amp;gt;Burkholderia&amp;lt;/i&amp;gt; sp. M6-3 and &amp;lt;i&amp;gt;Arthrobacter&amp;lt;/i&amp;gt; sp. M7-15.</pubmed_title><pmcid>PMC12010642</pmcid><pubmed_authors>Jiang Y</pubmed_authors><pubmed_authors>Chu C</pubmed_authors><pubmed_authors>Wang Q</pubmed_authors><pubmed_authors>Qin H</pubmed_authors><pubmed_authors>Zhong W</pubmed_authors><pubmed_authors>Liu R</pubmed_authors><pubmed_authors>Han C</pubmed_authors><pubmed_authors>Deng H</pubmed_authors></additional><is_claimable>false</is_claimable><name>Transcriptome analysis of nitrogen assimilation preferences in &amp;lt;i&amp;gt;Burkholderia&amp;lt;/i&amp;gt; sp. M6-3 and &amp;lt;i&amp;gt;Arthrobacter&amp;lt;/i&amp;gt; sp. M7-15.</name><description>&lt;h4>Introduction&lt;/h4>Ammonium (NH&lt;sub>4&lt;/sub> &lt;sup>+&lt;/sup>) and nitrate (NO&lt;sub>3&lt;/sub> &lt;sup>-&lt;/sup>) are the two main forms of inorganic nitrogen (N) that exist in soil and both can be absorbed and utilized by plants. As a vast and crucial biome, soil microorganisms are responsible for mediating the inorganic N assimilation process and enhancing nitrogen use efficiency. Understanding how these microorganisms assimilate different forms of inorganic nitrogen is crucial. There are a handful of microorganisms that play a dominant role in the process of soil inorganic nitrogen assimilation and have a significant advantage in abundance. However, microbial preferences for ammonium or nitrate, as well as differences in their metabolic pathways under co-existing ammonium and nitrate conditions, re</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025</publication><modification>2026-06-01T21:07:47.339Z</modification><creation>2025-07-03T03:05:12.999Z</creation></dates><accession>S-EPMC12010642</accession><cross_references><pubmed>40260088</pubmed><doi>10.3389/fmicb.2025.1559884</doi></cross_references></HashMap>