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Nevertheless, the precise manner by which microbial and mineral properties drive MAOM formation efficiency and its subsequent response to elevated temperature at the regional scale remains unclear. Here, we employed isotopically labelled laboratory incubations (at 15\u00b0C and 25\u00b0C) with soil samples from a ~3000\u2009km transect across the Tibetan Plateau to elucidate the mechanisms underlying MAOM formation and its temperature response. The results indicated that both mineral protection and microbial properties were critical predictors of MAOM formation across the geographic gradient. The efficiency of MAOM formation was found to increase with the content of iron (Fe) oxides and their reactivity [i.e., the ratio of poorly crystalline Fe oxides to total Fe oxides (Fe\n                    <jats:sub>o<\/jats:sub>\n                    :Fe\n                    <jats:sub>d<\/jats:sub>\n                    )] but to decrease with the relative abundance of\n                    <jats:italic>Gammaproteobacteria<\/jats:italic>\n                    and\n                    <jats:italic>Actinobacteria<\/jats:italic>\n                    across the plateau. Moreover, a notable decline in MAOM formation efficiency was observed under elevated temperatures, which was concomitant with a reduction in the content and reactivity of Fe oxides, as well as the microbial assimilation of the labelled substrate. The attenuation of mineral\u2013organic associations was identified as the primary factor contributing to the warming\u2010induced reduction in MAOM formation. These findings highlight the necessity of incorporating organo\u2013mineral associations and microbial properties into Earth System Models to accurately project soil C dynamics under changing climate.\n                  <\/jats:p>","DOI":"10.1111\/gcb.70004","type":"journal-article","created":{"date-parts":[[2024,12,19]],"date-time":"2024-12-19T10:29:58Z","timestamp":1734604198000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":55,"title":["Mineral and Microbial Properties Drive the Formation of Mineral\u2010Associated Organic Matter and Its Response to Increased Temperature"],"prefix":"10.1111","volume":"30","author":[{"given":"Jianing","family":"Zhao","sequence":"first","affiliation":[{"name":"State Key Laboratory of Vegetation and Environmental Change, Institute of Botany Chinese Academy of Sciences  Beijing China"},{"name":"China National Botanical Garden  Beijing China"},{"name":"University of Chinese Academy of Sciences  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Xuehui","family":"Feng","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Vegetation and Environmental Change, Institute of Botany Chinese Academy of Sciences  Beijing China"},{"name":"China National Botanical Garden  Beijing China"},{"name":"University of Chinese Academy of Sciences  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jie","family":"Hu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Vegetation and Environmental Change, Institute of Botany Chinese Academy of Sciences  Beijing China"},{"name":"China National Botanical Garden  Beijing China"},{"name":"University of Chinese Academy of Sciences  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Mei","family":"He","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Vegetation and Environmental Change, Institute of Botany 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