Skarke, A., Ruppel, C., Kodis, M., Brothers, D. & Lobecker, E. Widespread methane leakage from the sea floor on the northern US Atlantic margin. Nat. Geosci. 7, 657–661 (2014).
Johnson, H. P. et al. Anomalous Concentration of Methane Emissions at the Continental Shelf Edge of the Northern Cascadia Margin. J. Geophys. Res. Solid Earth 1–15 https://doi.org/10.1029/2018jb016453. (2019)
Sen, A. et al. Atypical biological features of a new cold seep site on the Lofoten-Vesterålen continental margin (northern Norway). Sci. Rep. 9, 1–14 (2019).
Karstens, J. et al. Glacigenic sedimentation pulses triggered post-glacial gas hydrate dissociation. Nat. Commun. 9, 635 (2018).
Dickens, G. Hydrocarbon-driven warming. Nature 429, 513–515 (2004).
Reeburgh, W. Oceanic methane biogeochemistry. Am. Chem. Soc. 107, 486–513 (2007).
Saunois, M. et al. The global methane budget 2000–2012. Earth Syst. Sci. Data 8, 697–751 (2016).
Berndt, C. et al. Temporal Constraints on Hydrate-Controlled Methane Seepage off Svalbard. Science 343, 284–288 (2014).
Gutjahr, M. et al. Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum. Nature 548, 573–577 (2017).
Egger, M., Riedinger, N., Mogollón, J. M. & Jørgensen, B. B. Global diffusive fluxes of methane in marine sediments. Nat. Geosci. 11, 421–425 (2018).
Boetius, A. & Wenzhöfer, F. Seafloor oxygen consumption fuelled by methane from cold seeps. Nat. Geosci. 6, 725–734 (2013).
Schmale, O., Greinert, J. & Rehder, G. Methane emission from high-intensity marine gas seeps in the Black Sea into the atmosphere. Geophys. Res. Lett. 32, (2005).
Boetius, A. et al. A marine microbial consortium apparently mediating anaerobic oxidation of methane. Nature 407, 623–626 (2000).
Beal, E. J., House, C. H. & Orphan, V. J. Manganese- and iron-dependent marine methane oxidation. Science 325, 184–187 (2009).
Luff, R. & Wallmann, K. Fluid flow, methane fluxes, carbonate precipitation and biogeochemical turnover in gas hydrate-bearing sediments at Hydrate Ridge, Cascadia Margin: Numerical modeling and mass balances. Geochim. Cosmochim. Acta 67, 3403–3421 (2003).
Oppo, D., Capozzi, R., Picotti, V. & Ponza, A. A genetic model of hydrocarbon-derived carbonate chimneys in shelfal fine-grained sediments: The Enza River field, Northern Apennines (Italy). Mar. Pet. Geol. 66, 555–565 (2015).
Reitner, J. et al. Concretionary methane-seep carbonates and associated microbial communities in Black Sea sediments. Palaeogeogr. Palaeoclimatol. Palaeoecol. 227, 18–30 (2005).
Judd, A. G. et al. The geological methane budget at Continental Margins and its influence on climate change. Geofluids 2, 109–126 (2002).
Capozzi, R., Oppo, D. & Taviani, M. Cold seepages: An economic tool for hydrocarbon appraisal. AAPG Bull. 101, 617-623 (2017).
Kiel, S. Global hydrocarbon seep-carbonate precipitation correlates with deep-water temperatures and eustatic sea-level fluctuations since the Late Jurassic. Terra Nova 21, 279–284 (2009).
Miller, K. G., Mountain, G., Wright, J. & Browning, J. V. A 180-Million-Year Record of Sea Level and Ice Volume Variations from Continental Margin and Deep-Sea Isotopic Records. Oceanography 24, 40–53 (2011).
Miller, K. G. et al. The phanerozoic record of global sea-level change. Science 310, 1293–1298 (2005).
Muller, R. D., Sdrolias, M., Gaina, C., Steinberger, B. & Heine, C. Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics. Science 319, 1357–1362 (2008).
Cramer, B. S., Miller, K. G., Barrett, P. J. & Wright, J. D. Late Cretaceous-Neogene trends in deep ocean temperature and continental ice volume: Reconciling records of benthic foraminiferal geochemistry (δ18O and Mg/Ca) with sea level history. J. Geophys. Res. Oceans 116, 1–23 (2011).
Li, G. & Elderfield, H. Evolution of carbon cycle over the past 100 million years. Geochim. Cosmochim. Acta 103, 11–25 (2013).
Dean, J. F. et al. Methane Feedbacks to the Global Climate System in a Warmer World. Rev. Geophys. 56, 207–250 (2018).
Andreassen, K. et al. Massive blow-out craters formed by hydrate-controlled methane expulsion from the Arctic seafloor. Science 356, 948–953 (2017).
Kirkham, C., Cartwright, J., Hermanrud, C. & Jebsen, C. The formation of giant clastic extrusions at the end of the Messinian Salinity Crisis. Earth Planet. Sci. Lett. 482, 434–445 (2018).
Gay, A. et al. 3D morphology and timing of the giant fossil pockmark of Beauvoisin, SE Basin of France. J. Geol. Soc. 176, 61-77 (2018)
Oppo, D. & Capozzi, R. Spatial association of mud volcano and sandstone intrusions, Boyadag anticline, western Turkmenistan. Basin Res. 28, 827–839 (2016).
Agirrezabala, L. M., Kiel, S., Blumenberg, M., Schäfer, N. & Reitner, J. Outcrop analogues of pockmarks and associated methane-seep carbonates: A case study from the Lower Cretaceous (Albian) of the Basque-Cantabrian Basin, western Pyrenees. Palaeogeogr. Palaeoclimatol. Palaeoecol. 390, 94–115 (2013).
Ruppel, C. D. & Kessler, J. D. The interaction of climate change and methane hydrates. Rev. Geophys. 55, 126–168 (2017).
Bangs, N. L. B., Musgrave, R. J. & Tréhu, A. M. Upward shifts in the southern Hydrate Ridge gas hydrate stability zone following postglacial warming, offshore Oregon. J. Geophys. Res. Solid Earth 110, (2005).
Xu, W. & Ruppel, C. Predicting the occurrence, distribution, and evolution of methane gas hydrate in porous marine sediments. J. Geophys. Res. Solid Earth 104, 5081–5095 (1999).
Dickens, G. R. Sulfate profiles and barium fronts in sediment on the Blake Ridge: present and past methane fluxes through a large gas hydrate reservoir. Geochim. Cosmochim. Acta 65, 529–543 (2001).
Kemp, D. B., Coe, A. L., Cohen, A. S. & Schwark, L. Astronomical pacing of methane release in the Early Jurassic period. Nature 437, 396-399 (2005).
Svensen, H. et al. Release of methane from a volcanic basin as a mechanism for initial Eocene global warming. Nature 429, 542–545 (2004).
Reitner, J., Peckmann, J., Reimer, A., Schumann, G. & Thiel, V. Methane-derived carbonate build-ups and associated microbial communities at cold seeps on the lower Crimean shelf (Black Sea). Facies 51, 66–79 (2005).
Birgel, D. & Peckmann, J. Aerobic methanotrophy at ancient marine methane seeps: A synthesis. Org. Geochem. 39, 1659–1667 (2008).
Peckmann, J. & Thiel, V. Carbon cycling at ancient methane–seeps. Chem. Geol. 205, 443–467 (2004).
Feng, D. et al. Time integrated variation of sources of fluids and seepage dynamics archived in authigenic carbonates from Gulf of Mexico Gas Hydrate Seafloor Observatory. Chem. Geol. 385, 129–139 (2014).
Talbot, H. M. et al. Variability in aerobic methane oxidation over the past 1.2Myrs recorded in microbial biomarker signatures from Congo fan sediments. Geochim. Cosmochim. Acta 133, 387–401 (2014).
Panieri, G. et al. Diagenetic Mg-calcite overgrowths on foraminiferal tests in the vicinity of methane seeps. Earth Planet. Sci. Lett. 458, 203–212 (2017).
Panieri, G., Graves, C. A. & James, R. H. Paleo-methane emissions recorded in foraminifera near the landward limit of the gas hydrate stability zone offshore western Svalbard. Geochem. Geophys. Geosystems 17, 521–537 (2016).
Martin, R. A., Nesbitt, E. A. & Campbell, K. A. The effects of anaerobic methane oxidation on benthic foraminiferal assemblages and stable isotopes on the Hikurangi Margin of eastern New Zealand. Mar. Geol. 272, 270–284 (2010).
Hill, T. M. et al. Climatically driven emissions of hydrocarbons from marine sediments during deglaciation. Proc. Natl. Acad. Sci. 103, 13570–13574 (2006).
Yamamoto, M., Yamamuro, M. & Tada, R. Late quaternary records of organic carbon, calcium carbonate, and biomarkers from site 1016 off Point Conception, California margin. Proc. Ocean Drill. Program Sci. Results 167, 183–194 (2000).
Jiang, G., Kennedy, M. J. & Christie-Blick, N. Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates. Nature 426, 822–826 (2003).
Teichert, B. M. A. et al. U/Th Systematics and ages of authigenic carbonates from Hydrate Ridge, Cascadia Margin: Recorders of fluid flow variations. Geochim. Cosmochim. Acta 67, 3845–3857 (2003).
Bayon, G., Henderson, G. M. & Bohn, M. U–Th stratigraphy of a cold seep carbonate crust. Chem. Geol. 260, 47–56 (2009).
Kiel, S., Hansen, C., Nitzsche, K. N. & Hansen, B. T. Using 87 Sr/86 Sr Ratios to Date Fossil Methane Seep Deposits: Methodological Requirements and an Example from the Great Valley Group, California. J. Geol. 122, 353–366 (2014).
Hawkesworth, C., Cawood, P., Kemp, T., Storey, C. & Dhuime, B. A Matter of Preservation. Science 323, 49–50 (2009).
Dunhill, A. M., Hannisdal, B. & Benton, M. J. Disentangling rock record bias and common-cause from redundancy in the British fossil record. Nat. Commun. 5, 4818 (2014).
Peters, S. E. Environmental determinants of extinction selectivity in the fossil record. Nature 454, 626–629 (2008).
Kiel, S. et al. Cretaceous methane-seep deposits from New Zealand and their fauna. Palaeogeogr. Palaeoclimatol. Palaeoecol. 390, 17–34 (2013).
Peters, S. E. & Foote, M. Determinants of extinction in the fossil record. Nature 416, 420–424 (2002).
Luff, R., Wallmann, K. & Aloisi, G. Numerical modeling of carbonate crust formation at cold vent sites: significance for fluid and methane budgets and chemosynthetic biological communities. Earth Planet. Sci. Lett. 221, 337–353 (2004).
Mentaschi, L. et al. The transformed-stationary approach: a generic and simplified methodology for non-stationary extreme value analysis. Hydrol. Earth Syst. Sci. 20, 3527–3547 (2016).
Wortmann, U. G. & Paytan, A. Rapid Variability of Seawater Chemistry Over the Past 130 Million Years. Science 337, 334–336 (2012).
Husson, J. M. & Peters, S. E. Atmospheric oxygenation driven by unsteady growth of the continental sedimentary reservoir. Earth Planet. Sci. Lett. 460, 68–75 (2017).
Davies, R. J., Maqueda, M. Á. M., Li, A. & Ganopolski, A. Millennial-scale shifts in the methane hydrate stability zone due to Quaternary climate change. Geology 45, 1027–1030 (2017).
Dzyuba, O. S., Izokh, O. P. & Shurygin, B. N. Carbon isotope excursions in Boreal Jurassic–Cretaceous boundary sections and their correlation potential. Palaeogeogr. Palaeoclimatol. Palaeoecol. 381–382, 33–46 (2013).
Jahren, A. H., Arens, N. C., Sarmiento, G., Guerrero, J. & Amundson, R. Terrestrial record of methane hydrate dissociation in the Early Cretaceous. Geology 29, 159–162 (2001).
Cui, Y. et al. Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum. Nat. Geosci. 4, 481–485 (2011).
Dickens, G. R., O’Neil, J. R., Rea, D. K. & Owen, R. M. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene. Paleoceanography 10, 965–971 (1995).
Katz, M. E. The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum. Science 286, 1531–1533 (1999).
Kurtz, A. C., Kump, L. R., Arthur, M. A., Zachos, J. C. & Paytan, A. Early Cenozoic decoupling of the global carbon and sulfur cycles. Paleoceanography 18, 1–14 (2003).
DeConto, R. M. et al. Past extreme warming events linked to massive carbon release from thawing permafrost. Nature 484, 87–91 (2012).
Frieling, J. et al. Thermogenic methane release as a cause for the long duration of the PETM. Proc. Natl. Acad. Sci. 113, 12059–12064 (2016).
Carozza, D. A., Mysak, L. A. & Schmidt, G. A. Methane and environmental change during the Paleocene-Eocene thermal maximum (PETM): Modeling the PETM onset as a two-stage event. Geophys. Res. Lett. 38, L05702 (2011).
Pearson, P. N. & Palmer, M. R. Atmospheric carbon dioxide concentrations over the past 60 million years. Nature 406, 695–699 (2000).
Zachos, J. C., Pagani, M., Sloan, L., Thomas, E. & Billups, K. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292, 686–693 (2001).
Etiope, G. Natural Gas Seepage: The Earth’s Hydrocarbon Degassing. (Springer International Publishing, 2015).
Watanabe, Y., Nakai, S., Hiruta, A., Matsumoto, R. & Yoshida, K. U–Th dating of carbonate nodules from methane seeps off Joetsu, Eastern Margin of Japan Sea. Earth Planet. Sci. Lett. 272, 89–96 (2008).
Tong, H. et al. Authigenic carbonates from seeps on the northern continental slope of the South China Sea: New insights into fluid sources and geochronology. Mar. Pet. Geol. 43, 260–271 (2013).
Wallmann, K. et al. Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming. Nat. Commun. 9, 83 (2018).
Bayon, G. et al. Formation of carbonate chimneys in the Mediterranean Sea linked to deep-water oxygen depletion. Nat. Geosci. 6, 755–760 (2013).
Trincardi, F., Cattaneo, A., Correggiari, A. & Ridente, D. Evidence of soft sediment deformation, fluid escape, sediment failure and regional weak layers within the late Quaternary mud deposits of the Adriatic Sea. Mar. Geol. 29, 91–119 (2004).
Oppo, D., Capozzi, R. & Picotti, V. A new model of the petroleum system in the Northern Apennines, Italy. Mar. Pet. Geol. 48, 57–76 (2013).
Hantschel, T. & Kauerauf, A. I. Fundamentals of Basin and Petroleum Systems Modeling. (Springer, Berlin, Heidelberg, 2009)
Müller, R. D. & Dutkiewicz, A. Oceanic crustal carbon cycle drives 26-million-year atmospheric carbon dioxide periodicities. Sci. Adv. 4, eaaq0500 (2018).
Rampino, M. R. & Caldeira, K. Episodes Of Terrestrial Geologic Activity During The Past 260 Million Years: A Quantitative Approach. In Dynamics and Evolution of Minor Bodies with Galactic and Geological Implications (eds. Clube, S. V. M., Yabushita, S. & Henrard, J.) 143–159 (Springer Netherlands, 1992).
Rampino, M. R. & Caldeira, K. Periodic impact cratering and extinction events over the last 260 million years. Mon. Not. R. Astron. Soc. 454, 3480–3484 (2015).
Boulila, S. Coupling between Grand cycles and Events in Earth’s climate during the past 115 million years. Sci. Rep. 9, 327 (2019).
Boulila, S., Galbrun, B., Laskar, J. & Pälike, H. A ~9myr cycle in Cenozoic δ13C record and long-term orbital eccentricity modulation: Is there a link? Earth Planet. Sci. Lett. 317–318, 273–281 (2012).
Martinez, M. & Dera, G. Orbital pacing of carbon fluxes by a ∼9-My eccentricity cycle during the Mesozoic. Proc. Natl. Acad. Sci. 112, 12604–12609 (2015).
Middelburg, J. J. & Levin, L. A. Coastal hypoxia and sediment biogeochemistry. Biogeosciences 6, 1273–1293 (2009).
Yamamoto, A., Yamanaka, Y., Oka, A. & Abe-Ouchi, A. Ocean oxygen depletion due to decomposition of submarine methane hydrate. Geophys. Res. Lett. 41, 5075–5083 (2014).
Pohlman, J. W. et al. Enhanced CO2 uptake at a shallow Arctic Ocean seep field overwhelms the positive warming potential of emitted methane. Proc. Natl. Acad. Sci. 114, 5355–5360 (2017).
Kiel, S. & Peckmann, J. Resource partitioning among brachiopods and bivalves at ancient hydrocarbon seeps: A hypothesis. PLOS ONE 14, e0221887 (2019).
Ing, C.-K. & Wei, C.-Z. Order selection for same-realization predictions in autoregressive processes. Ann. Stat. 33, 2423–2474 (2005).
Rabiner, L. On the use of autocorrelation analysis for pitch detection. IEEE Trans. Acoust. Speech Signal Process. 25, 24–33 (1977).
Manolakis, D. G. & Ingle, V. K. Applied digital signal processing: theory and practice. (New York: Cambridge University Press, 2011).
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