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Thawing, drainage, and erosion expose surface and deep sediments (&gt;\u20091\u2009m) to aerobic conditions, with saline deposits being particularly vulnerable due to freeze\u2010point depression. As organic carbon mineralization remains poorly constrained, we determined potentials with an aerobic one\u2010year long incubation at 10\u00b0C in permafrost upland, lake talik, lake cryopeg, and refrozen saline DLB sediments. We linked CO\n                    <jats:sub>2<\/jats:sub>\n                    production to biochemical, hydrochemical, and microbial factors, and assessed carbon alteration via repeated\n                    <jats:italic>n<\/jats:italic>\n                    \u2010alkane analyses. After 382\u2009days, average CO\n                    <jats:sub>2<\/jats:sub>\n                    production was 7.0\u2009\u00b1\u20090.4\u2009mg C g\n                    <jats:sup>\u22121<\/jats:sup>\n                    dry weight (DW), with DLB surface peat yielding the most (40.5\u2009\u00b1\u20092.7\u2009mg C g\n                    <jats:sup>\u22121<\/jats:sup>\n                    DW), and carbon\u2010poor cryopeg deposits (1.4\u2009\u00b1\u20090.1\u2009mg C g\n                    <jats:sup>\u22121<\/jats:sup>\n                    DW) and refrozen saline permafrost (1.5\u2009\u00b1\u20090.02\u2009mg C g\n                    <jats:sup>\u22121<\/jats:sup>\n                    DW) the least. Total organic carbon (TOC) was the main driver of CO\n                    <jats:sub>2<\/jats:sub>\n                    production, while age, nitrogen content, electrical conductivity, water content, pH, and microbial abundance also correlated significantly with CO\n                    <jats:sub>2<\/jats:sub>\n                    production. Normalizing production to TOC contents, saline permafrost and cryopeg sediments showed similar CO\n                    <jats:sub>2<\/jats:sub>\n                    production to active layers, stressing the importance of potentially carbon\u2010rich saline deposits. TOC normalization revealed that carbon characteristics (\u03b4\n                    <jats:sup>13<\/jats:sup>\n                    C, alkane content, ACL) also significantly influenced CO\n                    <jats:sub>2<\/jats:sub>\n                    production. The\n                    <jats:italic>n<\/jats:italic>\n                    \u2010alkane based quantification of carbon alterations during the incubation further contributes to the understanding of carbon cycling at the molecular level.\n                    <jats:italic>n<\/jats:italic>\n                    \u2010Alkane contents increased on average by 153% and the carbon preference index (CPI) rose from 13.2 to 15.8, likely due to newly produced alkanes, preferential degradation, and desorption processes. This indicates strong responses of the carbon pool and raises questions about the reliability of the CPI as a degradation proxy. Altogether, our study highlights the overlooked role of salinity in CO\n                    <jats:sub>2<\/jats:sub>\n                    production from Arctic coastal plains which could substantially shift carbon balances.\n                  <\/jats:p>","DOI":"10.1111\/gcb.70997","type":"journal-article","created":{"date-parts":[[2026,7,11]],"date-time":"2026-07-11T17:13:03Z","timestamp":1783789983000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Saline Permafrost and Cryopegs as Potentially Important Sources of\n                    <scp>\n                      CO\n                      <sub>2<\/sub>\n                    <\/scp>\n                    \u2014Assessing Organic Carbon Mineralization Potentials on the Alaskan Coastal Plain"],"prefix":"10.1111","volume":"32","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4933-2172","authenticated-orcid":false,"given":"Fabian","family":"Seemann","sequence":"first","affiliation":[{"name":"Permafrost Research Section Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research  Potsdam Germany"},{"name":"Institute of Geosciences University of Potsdam  Potsdam Germany"},{"name":"Physical Geography, Institute of Geography Technische Universit\u00e4t Dresden  Dresden Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9638-7497","authenticated-orcid":false,"given":"Mackenzie R.","family":"Baysinger","sequence":"additional","affiliation":[{"name":"Permafrost Research Section Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research  Potsdam Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9389-7093","authenticated-orcid":false,"given":"Susanne","family":"Liebner","sequence":"additional","affiliation":[{"name":"GFZ Helmholtz Centre for Geosciences, Section Geomicrobiology  Potsdam Germany"},{"name":"Institute of Biochemistry and Biology University of Potsdam  Potsdam Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1225-8178","authenticated-orcid":false,"given":"Claire","family":"Treat","sequence":"additional","affiliation":[{"name":"Land\u2010CRAFT Center, Department of Agroecology Aarhus University  Aarhus Denmark"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9586-0390","authenticated-orcid":false,"given":"Michael","family":"Zech","sequence":"additional","affiliation":[{"name":"Physical Geography, Institute of Geography Technische Universit\u00e4t Dresden  Dresden Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1330-7461","authenticated-orcid":false,"given":"Maren","family":"Jenrich","sequence":"additional","affiliation":[{"name":"Permafrost Research Section Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research  Potsdam Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5895-2141","authenticated-orcid":false,"given":"Guido","family":"Grosse","sequence":"additional","affiliation":[{"name":"Permafrost Research Section Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research  Potsdam Germany"},{"name":"Institute of Geosciences University of Potsdam  Potsdam Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1517-4711","authenticated-orcid":false,"given":"Benjamin M.","family":"Jones","sequence":"additional","affiliation":[{"name":"Institute of Northern Engineering University of Alaska Fairbanks  Fairbanks Alaska USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4678-4982","authenticated-orcid":false,"given":"Jens","family":"Strauss","sequence":"additional","affiliation":[{"name":"Permafrost Research Section Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research  Potsdam Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"311","published-online":{"date-parts":[[2026,7,11]]},"reference":[{"key":"e_1_2_11_2_1","unstructured":"Alaska Climate Research Center.2026.\u201cData Portal.\u201dhttps:\/\/akclimate.org\/data\/data\u2010portal\/."},{"key":"e_1_2_11_3_1","doi-asserted-by":"publisher","DOI":"10.1002\/2014JG002778"},{"key":"e_1_2_11_4_1","unstructured":"Baysinger M. 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