Yuxuan Lin, Jing Sun, Xiaotian Zhou, Cheng Zhong, Xingyu Yang, Liuqian Yu, Jin Sun, Pei-Yuan Qian, Jiying Li
{"title":"化学自养促进深海甲烷渗漏沉积物中铁和磷的再循环","authors":"Yuxuan Lin, Jing Sun, Xiaotian Zhou, Cheng Zhong, Xingyu Yang, Liuqian Yu, Jin Sun, Pei-Yuan Qian, Jiying Li","doi":"10.1029/2025GB008735","DOIUrl":null,"url":null,"abstract":"<p>Methane-rich cold seeps are oases of life in the deep sea, where microbial chemosynthesis of organic matter sustains thriving ecosystems independent of sunlight-derived energy. Here, we reveal a previously overlooked role of chemoautotrophy at seeps as powerful recyclers of scarce nutrients iron (Fe) and phosphorus (P). Investigations of sediments at Haima cold seeps (1,300–1,500 m deep) across varying methane seepage intensities showed that seep sediments released orders of magnitude more dissolved Fe and phosphate than background sediments, despite comparable organic matter remineralization rates. At Haima seeps with high methane, sediment phosphate effluxes reached 2.00–15.8 µmol m<sup>−2</sup> d<sup>−1</sup>and dissolved Fe effluxes reached 2.24–47.4 µmol m<sup>−2</sup> d<sup>−1</sup>, compared to background phosphate efflux of 1.21 µmol m<sup>−2</sup> d<sup>−1</sup> and dissolved Fe efflux of 0.412 µmol m<sup>−2</sup> d<sup>−1</sup>. This enhancement in nutrient recycling stems from a cascade of coupled biogeochemical processes driven by the anaerobic oxidation of methane (AOM). Methane oxidation reduces Fe oxides, releasing both dissolved Fe and Fe-bound P. AOM also reduces sulfate to sulfide, precipitates dissolved Fe and suppresses the regeneration of P-binding Fe oxides, further promoting P release. These mechanisms maintained the disproportionately high benthic Fe and P recycling at seeps, which may significantly impact regional and global nutrient budgets, given the thousands of documented seeps and potentially orders of magnitude more undiscovered in the global ocean.</p>","PeriodicalId":12729,"journal":{"name":"Global Biogeochemical Cycles","volume":"39 8","pages":""},"PeriodicalIF":5.5000,"publicationDate":"2025-08-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Chemoautotrophy Enhances Iron and Phosphorus Recycling From Sediments at Deep-Sea Methane Seeps\",\"authors\":\"Yuxuan Lin, Jing Sun, Xiaotian Zhou, Cheng Zhong, Xingyu Yang, Liuqian Yu, Jin Sun, Pei-Yuan Qian, Jiying Li\",\"doi\":\"10.1029/2025GB008735\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Methane-rich cold seeps are oases of life in the deep sea, where microbial chemosynthesis of organic matter sustains thriving ecosystems independent of sunlight-derived energy. Here, we reveal a previously overlooked role of chemoautotrophy at seeps as powerful recyclers of scarce nutrients iron (Fe) and phosphorus (P). Investigations of sediments at Haima cold seeps (1,300–1,500 m deep) across varying methane seepage intensities showed that seep sediments released orders of magnitude more dissolved Fe and phosphate than background sediments, despite comparable organic matter remineralization rates. At Haima seeps with high methane, sediment phosphate effluxes reached 2.00–15.8 µmol m<sup>−2</sup> d<sup>−1</sup>and dissolved Fe effluxes reached 2.24–47.4 µmol m<sup>−2</sup> d<sup>−1</sup>, compared to background phosphate efflux of 1.21 µmol m<sup>−2</sup> d<sup>−1</sup> and dissolved Fe efflux of 0.412 µmol m<sup>−2</sup> d<sup>−1</sup>. This enhancement in nutrient recycling stems from a cascade of coupled biogeochemical processes driven by the anaerobic oxidation of methane (AOM). Methane oxidation reduces Fe oxides, releasing both dissolved Fe and Fe-bound P. AOM also reduces sulfate to sulfide, precipitates dissolved Fe and suppresses the regeneration of P-binding Fe oxides, further promoting P release. These mechanisms maintained the disproportionately high benthic Fe and P recycling at seeps, which may significantly impact regional and global nutrient budgets, given the thousands of documented seeps and potentially orders of magnitude more undiscovered in the global ocean.</p>\",\"PeriodicalId\":12729,\"journal\":{\"name\":\"Global Biogeochemical Cycles\",\"volume\":\"39 8\",\"pages\":\"\"},\"PeriodicalIF\":5.5000,\"publicationDate\":\"2025-08-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Global Biogeochemical Cycles\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GB008735\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global Biogeochemical Cycles","FirstCategoryId":"89","ListUrlMain":"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GB008735","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Chemoautotrophy Enhances Iron and Phosphorus Recycling From Sediments at Deep-Sea Methane Seeps
Methane-rich cold seeps are oases of life in the deep sea, where microbial chemosynthesis of organic matter sustains thriving ecosystems independent of sunlight-derived energy. Here, we reveal a previously overlooked role of chemoautotrophy at seeps as powerful recyclers of scarce nutrients iron (Fe) and phosphorus (P). Investigations of sediments at Haima cold seeps (1,300–1,500 m deep) across varying methane seepage intensities showed that seep sediments released orders of magnitude more dissolved Fe and phosphate than background sediments, despite comparable organic matter remineralization rates. At Haima seeps with high methane, sediment phosphate effluxes reached 2.00–15.8 µmol m−2 d−1and dissolved Fe effluxes reached 2.24–47.4 µmol m−2 d−1, compared to background phosphate efflux of 1.21 µmol m−2 d−1 and dissolved Fe efflux of 0.412 µmol m−2 d−1. This enhancement in nutrient recycling stems from a cascade of coupled biogeochemical processes driven by the anaerobic oxidation of methane (AOM). Methane oxidation reduces Fe oxides, releasing both dissolved Fe and Fe-bound P. AOM also reduces sulfate to sulfide, precipitates dissolved Fe and suppresses the regeneration of P-binding Fe oxides, further promoting P release. These mechanisms maintained the disproportionately high benthic Fe and P recycling at seeps, which may significantly impact regional and global nutrient budgets, given the thousands of documented seeps and potentially orders of magnitude more undiscovered in the global ocean.
期刊介绍:
Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.