353
Methane from Gas Hydrates
121. Hadley, C., Peters, D., Vaughan, A., “Gumusut-Kakap project: Geohazard characterisation and impact on field development plans,” International Petroleum Technology
Conference, 12554-MS, 15pp (2008).
122. Weitemeyer, K., Constable, S., Key K., “Marine EM techniques for gas-hydrate detection and hazard mitigation,” The Leading Edge, 25 (5), 629–632 (2006).
123. Bunz, S. and Meinert, J., “Overpressure distribution beneath hydrate-bearing sediments
at the Storegga Slide on the Mid-Norwegian margin,” Proceedings of the International
Conference on Gas Hydrates, June 13–16, Trondheim, Norway, Vol. 3, Paper 3007,
755–758 (2005).
124. Archer, D. et al., “Ocean methane hydrates as a slow tipping point in the global carbon cycle,” Proceedings of the National Academy of Sciences of the United States of
America, 106, 20596–20601 (2009).
125. Biastoch, A. et al., “Rising arctic ocean temperatures cause gas hydrate destabilization
and ocean acidification,” Geophysical Research Letters, 38, L08602 (2011).
126. Bock, M. et al., “Hydrogen isotopes preclude marine hydrate CH 4 emissions at the onset
of Dansgaard-Oeschger events,” Science, 328, 1686–1689 (2010).
127. Bohannon, J., “Weighing the climate risks of an untapped fossil fuel,” Science, 319,
1753 (2008).
128. Bowen, R.G. et al., “Geomorphology and gas release from pockmark features in the
Mackenzie Delta, Northwest Territories, Canada,” in Kane, D.L. and Hinkel, K.M.
(eds.), Proceedings of the 9th International Conference on Permafrost, Institute of
Northern Engineering, Fairbanks, AK, 171–176 (2008).
129. Dickens, G.R. et al., “Dissociation of oceanic methane hydrate as a cause of the carbon
isotope excursion at the end of the Paleocene,” Paleoceanography, 10, 965–971 (1995).
130. Dickens, G.R., “Down the rabbit hole: Toward appropriate discussion of methane
release from gas hydrate systems during the Paleocene-Eocene thermal maximum and
other past hyperthermal events,” Climate of the Past, 7, 831–846 (2011).
131. Harvey, L.D.D. and Huang, Z. “Evaluation of potential impact of methane clathrate
destabilization on future global warming,” Journal of Geophysical Research, 100,
2905–2926 (1995).
132. Hesselbo, S.P. et al., “Massive dissociation of gas hydrate during a Jurassic anoxic
event,” Nature, 406, 392–395 (2000).
133. Hinrichs, K.-U. and Boetius, A., “The anaerobic oxidation of methane: New insights in
microbial ecology and biochemistry,” in Wefer, G. et al. (eds.), Ocean Margin Systems.
Springer, Berlin, Germany, 457–477 (2002).
134. Hu, L. et al. “Methane fluxes to the atmosphere from deepwater hydrocarbon seeps in
the northern Gulf of Mexico,” Journal of Geophysical Research (2011).
135. Intergovernmental Panel on Climate Change (IPCC). Climate Change: The Scientific
Basis. Cambridge University Press, New York (2001).
136. Intergovernmental Panel on Climate Change (IPCC). Climate Change: The Physical
Basis. Cambridge University Press, New York (2007).
137. Jiang, G. et al., “Stable isotope evidence for methane seeps in Neoproterozoic postglacial cap carbonates,” Nature, 426, 822–826 (2003).
138. Judge, A.S. and Majorowicz, J.A., “Geothermal conditions for gas hydrate stability in the Beaufort-Mackenzie area: The global change aspect,” Palaeogeography,
Palaeoclimatology, Palaeoecology, 98, 251–263 (1992).
139. Kennett, J.P. et al., Methane Hydrates in Quaternary Climate Change: The Clathrate
Gun Hypothesis. American Geophysical Union, Washington, DC (2003).
140. Kessler, J.D. et al., “A persistent oxygen anomaly reveals the fate of spilled methane in
the deep Gulf of Mexico,” Science, 331, 312–315 (2011).
141. Krey, V. et al., “Gas hydrates: Entrance to a methane age or climate threat?” Environmental
Research Letters, 4, 034007 (2009).
Methane from Gas Hydrates
121. Hadley, C., Peters, D., Vaughan, A., “Gumusut-Kakap project: Geohazard characterisation and impact on field development plans,” International Petroleum Technology
Conference, 12554-MS, 15pp (2008).
122. Weitemeyer, K., Constable, S., Key K., “Marine EM techniques for gas-hydrate detection and hazard mitigation,” The Leading Edge, 25 (5), 629–632 (2006).
123. Bunz, S. and Meinert, J., “Overpressure distribution beneath hydrate-bearing sediments
at the Storegga Slide on the Mid-Norwegian margin,” Proceedings of the International
Conference on Gas Hydrates, June 13–16, Trondheim, Norway, Vol. 3, Paper 3007,
755–758 (2005).
124. Archer, D. et al., “Ocean methane hydrates as a slow tipping point in the global carbon cycle,” Proceedings of the National Academy of Sciences of the United States of
America, 106, 20596–20601 (2009).
125. Biastoch, A. et al., “Rising arctic ocean temperatures cause gas hydrate destabilization
and ocean acidification,” Geophysical Research Letters, 38, L08602 (2011).
126. Bock, M. et al., “Hydrogen isotopes preclude marine hydrate CH 4 emissions at the onset
of Dansgaard-Oeschger events,” Science, 328, 1686–1689 (2010).
127. Bohannon, J., “Weighing the climate risks of an untapped fossil fuel,” Science, 319,
1753 (2008).
128. Bowen, R.G. et al., “Geomorphology and gas release from pockmark features in the
Mackenzie Delta, Northwest Territories, Canada,” in Kane, D.L. and Hinkel, K.M.
(eds.), Proceedings of the 9th International Conference on Permafrost, Institute of
Northern Engineering, Fairbanks, AK, 171–176 (2008).
129. Dickens, G.R. et al., “Dissociation of oceanic methane hydrate as a cause of the carbon
isotope excursion at the end of the Paleocene,” Paleoceanography, 10, 965–971 (1995).
130. Dickens, G.R., “Down the rabbit hole: Toward appropriate discussion of methane
release from gas hydrate systems during the Paleocene-Eocene thermal maximum and
other past hyperthermal events,” Climate of the Past, 7, 831–846 (2011).
131. Harvey, L.D.D. and Huang, Z. “Evaluation of potential impact of methane clathrate
destabilization on future global warming,” Journal of Geophysical Research, 100,
2905–2926 (1995).
132. Hesselbo, S.P. et al., “Massive dissociation of gas hydrate during a Jurassic anoxic
event,” Nature, 406, 392–395 (2000).
133. Hinrichs, K.-U. and Boetius, A., “The anaerobic oxidation of methane: New insights in
microbial ecology and biochemistry,” in Wefer, G. et al. (eds.), Ocean Margin Systems.
Springer, Berlin, Germany, 457–477 (2002).
134. Hu, L. et al. “Methane fluxes to the atmosphere from deepwater hydrocarbon seeps in
the northern Gulf of Mexico,” Journal of Geophysical Research (2011).
135. Intergovernmental Panel on Climate Change (IPCC). Climate Change: The Scientific
Basis. Cambridge University Press, New York (2001).
136. Intergovernmental Panel on Climate Change (IPCC). Climate Change: The Physical
Basis. Cambridge University Press, New York (2007).
137. Jiang, G. et al., “Stable isotope evidence for methane seeps in Neoproterozoic postglacial cap carbonates,” Nature, 426, 822–826 (2003).
138. Judge, A.S. and Majorowicz, J.A., “Geothermal conditions for gas hydrate stability in the Beaufort-Mackenzie area: The global change aspect,” Palaeogeography,
Palaeoclimatology, Palaeoecology, 98, 251–263 (1992).
139. Kennett, J.P. et al., Methane Hydrates in Quaternary Climate Change: The Clathrate
Gun Hypothesis. American Geophysical Union, Washington, DC (2003).
140. Kessler, J.D. et al., “A persistent oxygen anomaly reveals the fate of spilled methane in
the deep Gulf of Mexico,” Science, 331, 312–315 (2011).
141. Krey, V. et al., “Gas hydrates: Entrance to a methane age or climate threat?” Environmental
Research Letters, 4, 034007 (2009).