IOCAS-IR
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
ISSN1752-0894
页码15
通讯作者Berndt, Christian(cberndt@geomar.de)
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.
DOI10.1038/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
被引频次:8[WOS]   [WOS记录]     [WOS相关记录]
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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