Methane release from the southern Brazilian margin during the last glacial

[1]  S. Mulitza,et al.  The Impact of the AMOC Resumption in the Western South Atlantic Thermocline at the Onset of the Last Interglacial , 2017 .

[2]  H. Behling,et al.  Long-term vegetation, climate and ocean dynamics inferred from a 73,500 years old marine sediment core (GeoB2107-3) off southern Brazil , 2017 .

[3]  A. Demopoulos,et al.  Corrigendum to “Insights into methane dynamics from analysis of authigenic carbonates and chemosynthetic mussels at newly-discovered Atlantic Margin seeps” [Earth Planet. Sci. Lett. 449 (2016) 332–344] , 2017 .

[4]  S. Mulitza,et al.  Prolonged warming of the Brazil Current precedes deglaciations , 2017 .

[5]  C. Ruppel,et al.  The interaction of climate change and methane hydrates , 2017 .

[6]  M. M. de Mahiques,et al.  An extensive pockmark field on the upper Atlantic margin of Southeast Brazil: spatial analysis and its relationship with salt diapirism , 2017, Heliyon.

[7]  R. Wirth,et al.  Diagenetic Mg-calcite overgrowths on foraminiferal tests in the vicinity of methane seeps , 2017 .

[8]  L. Levin,et al.  Colonization of over a thousand Cibicidoides wuellerstorfi (foraminifera: Schwager, 1866) on artificial substrates in seep and adjacent off-seep locations in dysoxic, deep-sea environments , 2016 .

[9]  Lorraine E. Lisiecki,et al.  Regional and global benthic δ18O stacks for the last glacial cycle , 2016 .

[10]  U. S. Brink,et al.  Pockmark asymmetry and seafloor currents in the Santos Basin offshore Brazil , 2016, Geo-Marine Letters.

[11]  E. Eizirik,et al.  Discovery of a chemosynthesis-based community in the western South Atlantic Ocean , 2016 .

[12]  R. Portilho-Ramos,et al.  Variability of the upwelling system in the southeastern Brazilian margin for the last 110,000 years , 2015 .

[13]  J. Ketzer,et al.  Natural gas hydrates in the Rio Grande Cone (Brazil): A new province in the western South Atlantic , 2015 .

[14]  D. Connelly,et al.  Fluxes and fate of dissolved methane released at the seafloor at the landward limit of the gas hydrate stability zone offshore western Svalbard , 2015 .

[15]  R. Tiedemann,et al.  Novel high-pressure culture experiments on deep-sea benthic foraminifera — Evidence for methane seepage-related δ13C of Cibicides wuellerstorfi , 2015 .

[16]  A. Schmittner,et al.  Southwest Atlantic water mass evolution during the last deglaciation , 2015 .

[17]  Fabrício Ferreira,et al.  GLOBOROTALIA CRASSAFORMIS OPTIMUM EVENT: A NEW LATE QUATERNARY BIOSTRATIGRAPHIC MARKER FOR THE SOUTHEASTERN BRAZILIAN MARGIN , 2014 .

[18]  G. Westbrook,et al.  Record of methane emissions from the West Svalbard continental margin during the last 23.500yrs revealed by δ13C of benthic foraminifera , 2014 .

[19]  T. L. Rasmussen,et al.  Carbon isotope (δ 13 C) excursions suggest times of major methane release during the last 14 kyr in Fram Strait, the deep-water gateway to the Arctic , 2014 .

[20]  Adam Skarke,et al.  Widespread methane leakage from the sea floor on the northern US Atlantic margin , 2014 .

[21]  G. Jouet,et al.  Control of Quaternary sea‐level changes on gas seeps , 2014 .

[22]  G. Panieri,et al.  Late Holocene foraminifera of Blake Ridge diapir: Assemblage variation and stable-isotope record in gas-hydrate bearing sediments , 2014 .

[23]  Stanislas F. Dubois,et al.  Geophysical exploration of an active pockmark field in the Bay of Concarneau, southern Brittany, and implications for resident suspension feeders , 2014, Geo-Marine Letters.

[24]  William B. Curry,et al.  Improved oxygen isotope temperature calibrations for cosmopolitan benthic foraminifera , 2014 .

[25]  L. Somoza,et al.  Pockmarks on either side of the Strait of Gibraltar: formation from overpressured shallow contourite gas reservoirs and internal wave action during the last glacial sea-level lowstand? , 2014, Geo-Marine Letters.

[26]  M. Kuypers,et al.  Carbon isotope equilibration during sulphate-limited anaerobic oxidation of methane , 2014 .

[27]  E. Peltzer,et al.  Limits to the sensitivity of living benthic foraminifera to pore water carbon isotope anomalies in methane vent environments , 2014 .

[28]  T. L. Rasmussen,et al.  Carbon isotope ( δ 13 C ) excursions suggest times of major methane release during the last 14 kyr in Fram Strait , the deep-water gateway to the Arctic , 2014 .

[29]  C. Buck,et al.  IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP , 2013, Radiocarbon.

[30]  A. Mangini,et al.  U/Th-dating and post-depositional alteration of a cold seep carbonate chimney from the Campos Basin offshore Brazil , 2012 .

[31]  M. Meredith,et al.  Abrupt changes in high-latitude nutrient supply to the Atlantic during the last glacial cycle , 2012 .

[32]  C. Volzone,et al.  SO2 gas adsorption by modified kaolin clays: influence of previous heating and time acid treatments. , 2011, Journal of environmental management.

[33]  J. Christen,et al.  Flexible paleoclimate age-depth models using an autoregressive gamma process , 2011 .

[34]  K. Hinrichs,et al.  Repeated pulses of vertical methane flux recorded in glacial sediments from the southeast Bering Sea , 2011 .

[35]  Y. Masumoto,et al.  The reversal of the multi‐decadal trends of the equatorial Pacific easterly winds, and the Indonesian Throughflow and Leeuwin Current transports , 2011 .

[36]  M. Latif,et al.  Rising Arctic Ocean temperatures cause gas hydrate destabilization and ocean acidification , 2011 .

[37]  J. Bernhard,et al.  Combined carbonate carbon isotopic and cellular ultrastructural studies of individual benthic foraminifera: 2. Toward an understanding of apparent disequilibrium in hydrocarbon seeps , 2010 .

[38]  M. Torres,et al.  Post depositional alteration of foraminiferal shells in cold seep settings: New insights from flow-through time-resolved analyses of biogenic and inorganic seep carbonates , 2010 .

[39]  Q. Hua,et al.  Holocene marine 14C reservoir age variability: Evidence from 230Th‐dated corals in the South China Sea , 2010 .

[40]  J. Peckmann,et al.  Authigenic carbonates from methane seeps of the northern Congo fan: Microbial formation mechanism , 2010 .

[41]  J. Peckmann,et al.  Patterns of carbonate authigenesis at the Kouilou pockmarks on the Congo deep-sea fan , 2010 .

[42]  V. Brovkin,et al.  Ocean methane hydrates as a slow tipping point in the global carbon cycle , 2009, Proceedings of the National Academy of Sciences.

[43]  T. Stocker,et al.  Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years , 2008, Nature.

[44]  G. Panieri,et al.  Benthic Foraminifera of the Blake Ridge hydrate mound, Western North Atlantic Ocean , 2008 .

[45]  E. Cauquil,et al.  Sr/Ca and Mg/Ca ratios in Niger Delta sediments: Implications for authigenic carbonate genesis in cold seep environments , 2007 .

[46]  G. Wefer,et al.  Signature of the Brazil-Malvinas Confluence (Argentine Basin) in the isotopic composition of planktonic foraminifera from surface sediments , 2007 .

[47]  N. Sultana,et al.  Ca and Mg / Ca ratios in Niger Delta sediments : Implications for authigenic carbonate genesis in cold seep environments , 2007 .

[48]  R. Schlitzer.  Ocean Data View , 2007 .

[49]  G. Heil.  Abrupt Climate Shifts in the Western Tropical to Subtropical Atlantic Region during the Last Glacial , 2006 .

[50]  M. Sarnthein,et al.  Methane-driven late Pleistocene δ13C minima and overflow reversals in the southwestern Greenland Sea , 2005 .

[51]  J. Greinert,et al.  Simulation of long-term feedbacks from authigenic carbonate crust formation at cold vent sites , 2005 .

[52]  William B. Curry,et al.  Glacial water mass geometry and the distribution of δ13C of ΣCO2 in the western Atlantic Ocean , 2004 .

[53]  M. Hovland,et al.  Seabed pockmarks associated with deepwater corals off SE Brazilian continental slope, Santos Basin , 2004 .

[54]  Jonathan B. Martin,et al.  Relationships between the distribution and stable isotopic composition of living benthic foraminifera and cold methane seep biogeochemistry in Monterey Bay, California , 2003 .

[55]  A. Mix,et al.  Is methane venting at the seafloor recorded by δ13C of benthic foraminifera shells , 2003 .

[56]  R. Kowsmann,et al.  Erosional event causing gas-venting on the upper continental slope, Campos Basin, Brazil , 2002 .

[57]  C. Waelbroecka,et al.  Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records , 2001 .

[58]  Behl,et al.  Carbon isotopic evidence for methane hydrate instability during quaternary interstadials , 2000, Science.

[59]  L. Levin,et al.  Benthic foraminifera associated with cold methane seeps on the northern California margin: Ecology and stable isotopic composition , 2000 .

[60]  Ilson Dias da Silveira,et al.  A corrente do Brasil ao largo da costa leste brasileira , 2000 .

[61]  Matthew H. England,et al.  On the water masses and mean circulation of the South Atlantic Ocean , 1999 .

[62]  W. Borowski,et al.  Global and local variations of interstitial sulfate gradients in deep-water, continental margin sediments: Sensitivity to underlying methane and gas hydrates , 1999 .

[63]  F. Schott,et al.  The mean flow field of the tropical Atlantic Ocean , 1999 .

[64]  J. Faugères,et al.  Upper slope sand deposits: the example of Campos Basin, a latest Pleistocene-Holocene record of the interaction between alongslope and downslope currents , 1998, Geological Society, London, Special Publications.

[65]  F. Brandini,et al.  Planktic foraminifera from the southwestern Atlantic (30 °–60 °S): species-specific patterns in the upper 50 m , 1996 .

[66]  A. Mackensen,et al.  The δ13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models , 1993 .

[67]  Bo Barker Jørgensen,et al.  Anaerobic methane oxidation rates at the sulfate‐methane transition in marine sediments from Kattegat and Skagerrak (Denmark) , 1985 .

[68]  C. Neyra.  Crystal Structures of Clay Minerals and Their X-ray Identification , 1983 .

[69]  S. Gorshkov,et al.  World ocean atlas , 1976 .

[70]  G. Wollin,et al.  Pleistocene climates and chronology in deep-sea sediments. , 1968, Science.