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Gravity complexes as a focus of seafloor fluid seepage : the Rio Grande Cone, SE Brazil

Ketzer, João Marcelo (author)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Praeg, D. (author)
Independent researcher
Augustin, A. H. (author)
Pontificia Universidade Catolica do Rio Grande do Sul, Brazil
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Rodrigues, L. F. (author)
Universidade Federal do Rio Grande, Brazil
Steiger, A. K. (author)
Pontificia Universidade Catolica do Rio Grande do Sul, Brazil
Rahmati-Abkenar, Mahboubeh (author)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Viana, A. R. (author)
Petrobras Petroleo Brasileiro SA, Brazil
Miller, D. J. (author)
Petrobras Petroleo Brasileiro SA, Brazil
Malinverno, A. (author)
Lamont-Doherty Earth Observatory of Columbia University, USA
Dickens, G. R. (author)
Trinity College Dublin, Ireland
Cupertino, J. A. (author)
Pontificia Universidade Catolica do Rio Grande do Sul, Brazil
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 (creator_code:org_t)
2023-03-21
2023
English.
In: Scientific Reports. - : Nature Publishing Group. - 2045-2322. ; 13:1
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Seafloor methane emissions can affect Earth’s climate and ocean chemistry. Vast quantities of methane formed by microbial decomposition of organic matter are locked within gas hydrate and free gas on continental slopes, particularly in large areas with high sediment accumulations such as deep-sea fans. The release of methane in slope environments has frequently been associated with dissociation of gas hydrates near the edge of the gas hydrate stability zone on the upper slope, with discharges in greater water depths less understood. Here we show, using data from the Rio Grande Cone (western South Atlantic), that the intrinsic, gravity-induced downslope collapse of thick slope sediment accumulations creates structures that serve as pathways for gas migration, unlocking methane and causing seafloor emissions via giant gas flares in the water column. The observed emissions in the study region (up to 310 Mg year−1) are three times greater than estimates for the entire US North Atlantic margin and reveal the importance of collapsing sediment accumulations for ocean carbon cycling. Similar outgassing systems on the Amazon and Niger fans suggest that gravity tectonics on passive margins is a common yet overlooked mechanism driving massive seafloor methane emissions in sediment-laden continental slopes. © 2023, The Author(s).

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

Natural Science
Naturvetenskap

Publication and Content Type

ref (subject category)
art (subject category)

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