<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>13</volume><submitter>Alcaman-Arias ME</submitter><pubmed_abstract>Marine ammonia oxidizers that oxidize ammonium to nitrite are abundant in polar waters, especially during the winter in the deeper mixed-layer of West Antarctic Peninsula (WAP) waters. However, the activity and abundance of ammonia-oxidizers during the summer in surface coastal Antarctic waters remain unclear. In this study, the ammonia-oxidation rates, abundance and identity of ammonia-oxidizing bacteria (AOB) and archaea (AOA) were evaluated in the marine surface layer (to 30 m depth) in Chile Bay (Greenwich Island, WAP) over three consecutive late-summer periods (2017, 2018, and 2019). Ammonia-oxidation rates of 68.31 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> (2018) and 37.28 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> (2019) were detected from illuminated 2 m seawater incubations. However, high ammonia-oxidation rates between 267.75 and 109.38 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> were obtained under the dark condition at 30 m in 2018 and 2019, respectively. During the late-summer sampling periods both stratifying and mixing events occurring in the water column over short timescales (February-March). Metagenomic analysis of seven nitrogen cycle modules revealed the presence of ammonia-oxidizers, such as the Archaea &lt;i>Nitrosopumilus&lt;/i> and the Bacteria &lt;i>Nitrosomonas&lt;/i> and &lt;i>Nitrosospira&lt;/i>, with AOA often being more abundant than AOB. However, quantification of specific &lt;i>amo&lt;/i>A gene transcripts showed number of AOB being two orders of magnitude higher than AOA, with &lt;i>Nitrosomonas&lt;/i> representing the most transcriptionally active AOB in the surface waters. Additionally, &lt;i>Candidatus&lt;/i> Nitrosopelagicus and &lt;i>Nitrosopumilus&lt;/i>, phylogenetically related to surface members of the NP-ε and NP-γ clades respectively, were the predominant AOA. Our findings expand the known distribution of ammonium-oxidizers to the marine surface layer, exposing their potential ecological role in supporting the marine Antarctic system during the productive summer periods.</pubmed_abstract><journal>Frontiers in microbiology</journal><pagination>821902</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8992545</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Surface Ammonia-Oxidizer Abundance During the Late Summer in the West Antarctic Coastal System.</pubmed_title><pmcid>PMC8992545</pmcid><pubmed_authors>Cifuentes-Anticevic J</pubmed_authors><pubmed_authors>Troncoso M</pubmed_authors><pubmed_authors>Bello E</pubmed_authors><pubmed_authors>Testa G</pubmed_authors><pubmed_authors>Alcaman-Arias ME</pubmed_authors><pubmed_authors>Diez B</pubmed_authors><pubmed_authors>Farias L</pubmed_authors></additional><is_claimable>false</is_claimable><name>Surface Ammonia-Oxidizer Abundance During the Late Summer in the West Antarctic Coastal System.</name><description>Marine ammonia oxidizers that oxidize ammonium to nitrite are abundant in polar waters, especially during the winter in the deeper mixed-layer of West Antarctic Peninsula (WAP) waters. However, the activity and abundance of ammonia-oxidizers during the summer in surface coastal Antarctic waters remain unclear. In this study, the ammonia-oxidation rates, abundance and identity of ammonia-oxidizing bacteria (AOB) and archaea (AOA) were evaluated in the marine surface layer (to 30 m depth) in Chile Bay (Greenwich Island, WAP) over three consecutive late-summer periods (2017, 2018, and 2019). Ammonia-oxidation rates of 68.31 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> (2018) and 37.28 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> (2019) were detected from illuminated 2 m seawater incubations. However, high ammonia-oxidation rates between 267.75 and 109.38 nmol N L&lt;sup>-1&lt;/sup> day&lt;sup>-1&lt;/sup> were obtained under the dark condition at 30 m in 2018 and 2019, respectively. During the late-summer sampling periods both stratifying and mixing events occurring in the water column over short timescales (February-March). Metagenomic analysis of seven nitrogen cycle modules revealed the presence of ammonia-oxidizers, such as the Archaea &lt;i>Nitrosopumilus&lt;/i> and the Bacteria &lt;i>Nitrosomonas&lt;/i> and &lt;i>Nitrosospira&lt;/i>, with AOA often being more abundant than AOB. However, quantification of specific &lt;i>amo&lt;/i>A gene transcripts showed number of AOB being two orders of magnitude higher than AOA, with &lt;i>Nitrosomonas&lt;/i> representing the most transcriptionally active AOB in the surface waters. Additionally, &lt;i>Candidatus&lt;/i> Nitrosopelagicus and &lt;i>Nitrosopumilus&lt;/i>, phylogenetically related to surface members of the NP-ε and NP-γ clades respectively, were the predominant AOA. Our findings expand the known distribution of ammonium-oxidizers to the marine surface layer, exposing their potential ecological role in supporting the marine Antarctic system during the productive summer periods.</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022</publication><modification>2026-04-08T17:26:41.061Z</modification><creation>2025-04-04T23:03:10.643Z</creation></dates><accession>S-EPMC8992545</accession><cross_references><pubmed>35401462</pubmed><doi>10.3389/fmicb.2022.821902</doi></cross_references></HashMap>