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slope. According to Stranne et al. (2019),   manages to pass through this filter and   different locations. The objective is to study   oil equivalent (9.621 billion pre-salt), which
 this phenomenon produces faults and frac-  leak to the seafloor, forming giant plumes   the rates of biogenic methane generation   puts the country in a privileged position.
 tures that allow massive migration of gas-  of gas that reach heights of 900 m in the   by comparing drilling results, experimental   However, when looking specifically at the
 rich fluids through the GHSZ. This massive   water column. Rates of methane release to   models and numerical models, the relation-  issue of natural gas, the scenario changes,
 vertical flow fuels the anaerobic oxidation   the ocean were estimated to be between   ship between shallow versus deep sources   leaving Brazil in a fragile position. This is be-
 of methane, but most of the methane   46.44 and 304.1 MgCH4/year.  of biogenic methane and the biogeochem-  cause the constant water crises (droughts)
                  ical  reactions  that  affect  the  amount  of   resulting from climate change resulted in
 Looking to the future  methane accumulated in sediments, and   a  significant  increase  in  this  resource  for
                  how these impact the global carbon cycle   the  use  of  gas-dependent  thermoelectric
 From all the above, the great advance   Marion Dufresne. The objective is to study   and the transfer of carbon to the ocean.  plants. According to the Brazilian Associ-
 obtained in the knowledge of the occur-  the past climatic history of the equatorial   Such projects will allow Brazil to contin-  ation of Piped Gas Distributors (Abegás),
 rences of gas hydrates in Brazil is remark-  margin of Brazil over the last few million   ue studies on the potential use of this re-  in 2021 an average of 76.043 million m³/
 able, especially with regard to the areas of   years, to determine the behavior of gas hy-  source as  an  energy  source  in  the  future.   day of natural gas was consumed, and ap-
 Foz do Amazonas and Rio Grande Cone.   drates in relation to high-impact submarine   Today, national production of hydrocarbons   proximately 34 million were destined for
 Through the collection of samples carried   landslides and to assess the extent of gas   is mainly focused on the pre-salt layer. Ac-  thermoelectric  plants.  The  resumption  of
 out by the TUCUXI and CONEGÁS projects,   leaks in the Amazon Fan area, as a whole.   cording to the National Petroleum Agency   national economic growth will also lead to
 it was possible to characterize the associ-  CALYPSO piston cores will be used with the   (ANP), in February 2022, 3.754 million bar-  a rise in consumption of inputs. On the oth-
 ated gases and determine the geochemi-  ability to recover up to 70 m of sediment,   rels of oil equivalent per day were produced,   er hand, according to ANP reports, national
 cal and biological aspects that help in the   resulting in approximately 300 m of cores,   with 75% of this volume coming from pre-  production, although growing, was around
 understanding  of their  genesis and  their   recovered from different selected sites.  salt reservoirs. In 2021, Brazilian reserves   134 million m³/day, most of which came

 behavior over geological time. The works   In the area of  the Rio Grande Cone of   reached a volume of 13.24 billion barrels of   from gas associated with oil.
 resulting from these analyses arouse the   the Pelotas Basin, the IODP#394 mission will   Thanks
 interest of the world scientific communi-  possibly  be  executed,  an  accomplishment
 ty due to the importance of hydrates not   of the International Ocean Discovery Pro-  Our thanks to PETROBRAS for the   of the importance of the partnership with
 only as an alternative energy resource, but   gram (IODP) using the oceanographic ship   partnership and financial support to   SeaSeep Dados de Petróleo Ltda. and the
 also because of their importance for under-  JOIDES Resolution (Joint Oceanographic   the CONEGAS Project (2010-2021). We   teams of the vessels Inspector II (mission
 standing the carbon cycle and its impacts   Institutions for  Deep  Earth Sampling), a   also thank those who participated in the   TU15, 2015) and Teknik Perdana (mission
 on climate change. Thus, two international   ship of scientific drilling for the collection   oceanographic missions carried out during   TP15, 2015) without which the execution
 scientific cruises are planned. As in previ-  and studies of marine rocks and sediments.   this period, in particular the teams of the   of the TUCUXI Project would not have
 ous  cruises all samples were retrieved from   The studies will be carried out through the   scientific ships Marechal Rondon (mission   been possible.
 the most superficial part of the sedimenta-  cooperation of several international and   MR11, 2011), Marion Dufresne (missions   We are grateful to the National Petro-
 ry column (maximum 20 m in length), the   Brazilian institutions. Among the universi-  MD186, 2011 and MD195, 2013), Rig   leum Agency – ANP for providing the seis-
 new cruises will contemplate deeper cores.  ties are the Brazilian PUCRS, UFRGS, FURG   Supporter (mission NR12, 2012), EM Lead-  mic data. Finally, we thank the geologists
 In the Foz do Amazonas Basin, a coop-  and  USP,  Linnaeus  University  (Sweden),
 eration project is planned between Brazil-  the Lamont-Doherty Earth Observatory   er (mission EM14, 2014), and Super Pesa   Rosalia Barili and João P. Zielinski for re-
                                                            viewing the manuscript.
                  XIII (mission SP20, 2020). Our recognition
 ian universities (PUCRS, UFRGS, UNISINOS,   and Rice University (USA), the University of
 USP, UFF, UERJ and UFESP), Linnaeus Uni-  Bremen (Germany) and the Japan Agency
 versity, in Sweden, and French research   for Marine-Earth Science and Technology
 institutes (IFREMER, GEOAZUR and LSCE),   (Japan).  Five  wells  will  be  drilled,  with
 using the French oceanographic vessel,   depths  between 200  and  800 m,  in  five



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