<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>14</volume><submitter>Rempfert KR</submitter><pubmed_abstract>Nitrogen (N) is an essential element for life. N compounds such as ammonium ( NH4+ ) may act as electron donors, while nitrate ( NO3- ) and nitrite ( NO2- ) may serve as electron acceptors to support energy metabolism. However, little is known regarding the availability and forms of N in subsurface ecosystems, particularly in serpentinite-hosted settings where hydrogen (H&lt;sub>2&lt;/sub>) generated through water-rock reactions promotes habitable conditions for microbial life. Here, we analyzed N and oxygen (O) isotope composition to investigate the source, abundance, and cycling of N species within the Samail Ophiolite of Oman. The dominant dissolved N species was dependent on the fluid type, with Mg&lt;sup>2+&lt;/sup>- HCO3- type fluids comprised mostly of NO3- , and Ca&lt;sup>2+&lt;/sup>-OH&lt;sup>-&lt;/sup> </pubmed_abstract><journal>Frontiers in microbiology</journal><pagination>1139633</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC10160414</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Subsurface biogeochemical cycling of nitrogen in the actively serpentinizing Samail Ophiolite, Oman.</pubmed_title><pmcid>PMC10160414</pmcid><pubmed_authors>Asamoto CK</pubmed_authors><pubmed_authors>Nothaft DB</pubmed_authors><pubmed_authors>Rempfert KR</pubmed_authors><pubmed_authors>Templeton AS</pubmed_authors><pubmed_authors>Evans RD</pubmed_authors><pubmed_authors>Matter JM</pubmed_authors><pubmed_authors>Kopf SH</pubmed_authors><pubmed_authors>Kraus EA</pubmed_authors><pubmed_authors>Spear JR</pubmed_authors></additional><is_claimable>false</is_claimable><name>Subsurface biogeochemical cycling of nitrogen in the actively serpentinizing Samail Ophiolite, Oman.</name><description>Nitrogen (N) is an essential element for life. N compounds such as ammonium ( NH4+ ) may act as electron donors, while nitrate ( NO3- ) and nitrite ( NO2- ) may serve as electron acceptors to support energy metabolism. However, little is known regarding the availability and forms of N in subsurface ecosystems, particularly in serpentinite-hosted settings where hydrogen (H&lt;sub>2&lt;/sub>) generated through water-rock reactions promotes habitable conditions for microbial life. Here, we analyzed N and oxygen (O) isotope composition to investigate the source, abundance, and cycling of N species within the Samail Ophiolite of Oman. The dominant dissolved N species was dependent on the fluid type, with Mg&lt;sup>2+&lt;/sup>- HCO3- type fluids comprised mostly of NO3- , and Ca&lt;sup>2+&lt;/sup>-OH&lt;sup>-&lt;/sup> </description><dates><release>2023-01-01T00:00:00Z</release><publication>2023</publication><modification>2025-04-22T05:13:18.715Z</modification><creation>2025-04-05T21:14:08.456Z</creation></dates><accession>S-EPMC10160414</accession><cross_references><pubmed>37152731</pubmed><doi>10.3389/fmicb.2023.1139633</doi></cross_references></HashMap>