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Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum | |
Berndt, Christian1; Planke, Sverre2,3; Zarikian, Carlos A. Alvarez A.4; Frieling, Joost5; Jones, Morgan T. T.3; Millett, John M. M.2,6; Brinkhuis, Henk7; Bunz, Stefan8; Svensen, Henrik H. H.3; Longman, Jack9,10; Scherer, Reed P. P.11; Karstens, Jens1; Manton, Ben2; Nelissen, Mei7; Reed, Brandon11; Faleide, Jan Inge3; Huismans, Ritske S. S.12; Agarwal, Amar13; Andrews, Graham D. M.14; Betlem, Peter3,15; Bhattacharya, Joyeeta16; Chatterjee, Sayantani17,18; Christopoulou, Marialena11; Clementi, Vincent J. J.19; Ferre, Eric C. C.20; Filina, Irina Y. Y.21; Guo, Pengyuan22; Harper, Dustin T. T.23; Lambart, Sarah23; Mohn, Geoffroy24; Nakaoka, Reina25; Tegner, Christian26; Varela, Natalia27; Wang, Mengyuan28; Xu, Weimu29,30; Yager, Stacy L. L.31 | |
2023-08-03 | |
发表期刊 | NATURE GEOSCIENCE |
ISSN | 1752-0894 |
页码 | 15 |
通讯作者 | Berndt, Christian([email protected]) |
摘要 | Widespread shallow-water hydrothermal venting in the North Atlantic, probably a source of methane, coincided with the onset of the Palaeocene-Eocene Thermal Maximum, according to borehole proxy records and seismic imaging. The Palaeocene-Eocene Thermal Maximum (PETM) was a global warming event of 5-6 & DEG;C around 56 million years ago caused by input of carbon into the ocean and atmosphere. Hydrothermal venting of greenhouse gases produced in contact aureoles surrounding magmatic intrusions in the North Atlantic Igneous Province have been proposed to play a key role in the PETM carbon-cycle perturbation, but the precise timing, magnitude and climatic impact of such venting remains uncertain. Here we present seismic data and the results of a five-borehole transect sampling the crater of a hydrothermal vent complex in the Northeast Atlantic. Stable carbon isotope stratigraphy and dinoflagellate cyst biostratigraphy reveal a negative carbon isotope excursion coincident with the appearance of the index taxon Apectodinium augustum in the vent crater, firmly tying the infill to the PETM. The shape of the crater and stratified sediments suggests large-scale explosive gas release during the initial phase of vent formation followed by rapid, but largely undisturbed, diatomite-rich infill. Moreover, we show that these vents erupted in very shallow water across the North Atlantic Igneous Province, such that volatile emissions would have entered the atmosphere almost directly without oxidation to CO2 and at the onset of the PETM. |
DOI | 10.1038/s41561-023-01246-8 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | Integrated Ocean Drilling Program; Research Council of Norway[336293]; Research Council of Norway[223272]; AkerBP (PDRILL project); IODP; Norwegian Petroleum Directorate; AkerBP (PDRILL project) |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:001045179900005 |
出版者 | NATURE PORTFOLIO |
WOS关键词 | NORTH-SEA ; METHANE ; RELEASE ; CARBON ; BASIN ; COMPLEXES ; CONSEQUENCES ; EVOLUTION ; ABUNDANCE ; CLIMATE |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/182739 |
专题 | 中国科学院海洋研究所 |
通讯作者 | Berndt, Christian |
作者单位 | 1.GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany 2.Volcan Basin Energy Res AS, Oslo, Norway 3.Univ Oslo, Dept Geosci, Oslo, Norway 4.Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA 5.Univ Oxford, Dept Earth Sci, Oxford, England 6.Univ Aberdeen, Kings Coll, Dept Geol & Geophys, Aberdeen, Scotland 7.NIOZ Royal Netherlands Inst Sea Res, Den Burg, Texel, Netherlands 8.UiT Arctic Univ Tromso, Dept Geol, Tromso, Norway 9.Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm ICBM, Marine Isotope Geochem, Oldenburg, Germany 10.Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne, England 11.Northern Illinois Univ, Dept Earth Atmosphere & Environm, De Kalb, IL USA 12.Univ Bergen, Dept Earth Sci, Bergen, Norway 13.Indian Inst Technol Kanpur, Dept Earth Sci, Appl Struct Geol, Kanpur, India 14.Univ Hull, Sch Environm Sci, Fac Sci & Engn, Kingston Upon Hull, England 15.Univ Ctr Svalbard, Dept Arctic Geol, Svalbard, Norway 16.Picarro Inc, Santa Clara, CA USA 17.Niigata Univ, Dept Geol, Niigata, Japan 18.Univ Tokyo, Earthquake Res Inst, Tokyo, Japan 19.Rutgers State Univ, Dept Marine & Coastal Sci, New Brunswick, NJ USA 20.Univ Louisiana Lafayette, Sch Geosci, Lafayette, LA USA 21.Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA 22.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China 23.Univ Utah, Dept Geol & Geophys, Salt Lake City, UT USA 24.CY Cergy Paris Univ, Lab Geosci & Environm Cergy GEC, Neuville Sur Oise, France 25.Kobe Univ, Dept Planetol, Kobe, Japan 26.Aarhus Univ, Dept Geosci, Aarhus, Denmark 27.Virginia Tech, Dept Geosci, Blacksburg, VA USA 28.Sun Yat Sen Univ, Sch Marine Sci, Zhuhai, Peoples R China 29.Univ Coll Dublin, Sch Earth Sci, Dublin, Ireland 30.Univ Coll Dublin, SFI Res Ctr Appl Geosci iCRAG, Dublin, Ireland 31.Ball State Univ, Dept Environm Geol & Nat Resources, Muncie, IN USA |
推荐引用方式 GB/T 7714 | Berndt, Christian,Planke, Sverre,Zarikian, Carlos A. Alvarez A.,et al. Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum[J]. NATURE GEOSCIENCE,2023:15. |
APA | Berndt, Christian.,Planke, Sverre.,Zarikian, Carlos A. Alvarez A..,Frieling, Joost.,Jones, Morgan T. T..,...&Yager, Stacy L. L..(2023).Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum.NATURE GEOSCIENCE,15. |
MLA | Berndt, Christian,et al."Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum".NATURE GEOSCIENCE (2023):15. |
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