化学自养促进深海甲烷渗漏沉积物中铁和磷的再循环

IF 5.5 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES
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,&nbsp;Jing Sun,&nbsp;Xiaotian Zhou,&nbsp;Cheng Zhong,&nbsp;Xingyu Yang,&nbsp;Liuqian Yu,&nbsp;Jin Sun,&nbsp;Pei-Yuan Qian,&nbsp;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,&nbsp;Jing Sun,&nbsp;Xiaotian Zhou,&nbsp;Cheng Zhong,&nbsp;Xingyu Yang,&nbsp;Liuqian Yu,&nbsp;Jin Sun,&nbsp;Pei-Yuan Qian,&nbsp;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}
引用次数: 0

摘要

富含甲烷的冷渗漏是深海中生命的绿洲,在那里,微生物的有机物化学合成维持着不依赖于太阳能的繁荣生态系统。在这里,我们揭示了一个以前被忽视的作用,即在渗漏中化学自养作为稀缺营养物质铁(Fe)和磷(P)的强大回收者。对海马冷渗沉积物(1300 - 1500 m深)不同甲烷渗流强度的调查表明,尽管有机质再矿化率相当,但渗渗沉积物释放的溶解铁和磷酸盐比背景沉积物多几个数量级。在海马高甲烷渗漏区,沉积物磷通量为2.00 ~ 15.8µmol m−2 d−1,溶解铁通量为2.24 ~ 47.4µmol m−2 d−1,而背景磷通量为1.21µmol m−2 d−1,溶解铁通量为0.412µmol m−2 d−1。这种营养循环的增强源于甲烷厌氧氧化(AOM)驱动的一系列耦合生物地球化学过程。甲烷氧化还原了铁氧化物,释放出溶解的铁和铁结合的铁。AOM还将硫酸盐还原为硫化物,沉淀溶解的铁,抑制结合磷的铁氧化物的再生,进一步促进磷的释放。这些机制维持了渗漏中不成比例的高底生物铁和磷的再循环,这可能会显著影响区域和全球的营养收支,考虑到数千次有记录的渗漏和全球海洋中潜在的未发现的数量级。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Chemoautotrophy Enhances Iron and Phosphorus Recycling From Sediments at Deep-Sea Methane Seeps

Chemoautotrophy Enhances Iron and Phosphorus Recycling From Sediments at Deep-Sea Methane Seeps

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.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
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.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信