48 / 78
FROZEN HEAT
48
Felbeck, H. (1981). Chemoautotrophic potential of the hydrothermal
vent tube worm, Riftia pacjyptila Jones (Vestimentifera). Science, 213,
336-338
Fisher, C.R., MacDonald, I.R., Sassen, R., Young, C.M., Macko, S.A.,
Hourdez, S., Carney, R.S., Joye, S.B. and McMullin, E. (2000).
Methane ice worms: Hesiocaeca methanicola colonizing fossil fuel
reserves. Naturwissenschaften, 87, 184-187
Gee, M.J.R., Uy, H.S., Warren, J., Morley, C.K. and Lambiase, J.J. (2007).
The Brunei slide: A giant submarine landslide on the North West
Borneo Margin revealed by 3D seismic data. Mar. Geol., 246, 9-23.
doi: Doi 10.1016/J.Margeo.2007.07.009
Goedert, J.L. and Benham, S.R. (2003). Biogeochemical processes
at ancient methane seeps: the Bear River site in southwestern
Washington. In Western Cordillera and adjacent areas: Boulder,
Colorado (ed. T.W. Swanson). pp. 201-208. Geological Society of
America
Hansen, J., Fung, A., Lacis, A., Rind, D. and Lebedeff, S. (1988). Global
climate changes as forecast by Goddard Institute for Space Studies
3-D Model. J. Geophys. Res., 93, 9341-9364
Hanson, R.S. and Hanson, T.E. (1996). Methanotrophic bacteria.
Microbiol. Rev., 60, 439-471
Hedges, J.I. and Keil, R.G. (1995). Sedimentary organic-matter
preservation – An assessment and speculative synthesis. Mar. Chem.,
49, 81-115
Hornbach, M.J., Lavier, L.L. and Ruppel, C.D. (2007). Triggering
mechanism and tsunamogenic potential of the Cape Fear Slide
complex, U.S. Atlantic margin. Geochem. Geophy. Geosy., 8, Q12008,
doi: 12010.11029/12007GC001722, 001716 p.
Houghton, R. A. (2007), Balancing the global carbon budget, Annu. Rev.
Earth Planet. Sci., 35, 313-347
Hu, L., Yvon-Lewis, S.A., Kessler, J.D. and MacDonald, I.R. (2012).
Methane fluxes to the atmosphere from deepwater hydrocarbon
seeps in the northern Gulf of Mexico. J. Geophys. Res., 117. doi:
10.1029/2011jc007208
IPCC (2007). Climate Change 2007: The physical science basis.
Contribution of Working Group I to the fourth assessment report
of the Intergovernmental Panel on Climate Change 996 p. IPCC,
Cambridge, United Kingdom and New York, NY, USA
Jiang, G., Shi, X. and Zhang, S. (2006). Methane seeps, methane
hydrate destabilization, and the late Neoproterozoic postglacial cap
carbonates. Chin. Sci. Bull., 51, 1152-1173
Jørgensen, B.B. and Nelson, D.C. (2004). Sulfide oxidation in marine
sediments: Geochemistry meets microbiology. Geol. Soc. Am., Special
Paper 379, 63-81
Joye, S.B., Samarkin, V.A., Orcutt, B.N., MacDonald, I.R., Hinrichs, K.U.,
Elvert, M., Teske, A.P., Lloyd, K.G., Lever, M.A., Montoya, J.P. and
Meile, C.D. (2009). Metabolic variability in seafloor brines revealed
by carbon and sulphur dynamics. Nat. Geosci., 2, 349-354. doi: Doi
10.1038/Ngeo475
Judd, A.G., Hovland, M., Dimitrov, L.I., García Gil, S. and Jukes, V.
(2002). The geological methane budget at continental margins and its
influence on climate change. Geofluids, 2, 109-126
Kastner, M., Torres, M., Solomon, E. and Spivack, A. (2008). Marine pore
fluid profiles of dissolved sulfate; do they reflect in situ methane fluxes.
Fire in the Ice, NETL Methane Hydrate Newsletter, Summer, 6-8
Kayen, R.E. and Lee, H.J. (1991). Pleistocene slope instability of gas
hydrate-laden sediment on the Beaufort Sea Margin. Mar. Geotechnol.,
10, 125-141
Kiel, S. (2009). Global hydrocarbon seep-carbonate precipitation
correlates with deep-water temperatures and eustatic sea-level
fluctuations since the Late Jurassic. Terra Nova, 21, 279-284
Knittel, K. and Boetius, A. (2009). Anaerobic oxidation of methane:
progress with an unknown process. Annu. Rev. Microbiol., 63, 311-334
Kvalstad, T.J., Andresen, L., Forsberg, C.F., Berg, K., Bryn, P. and
Wangen, M. (2005). The Storegga slide: evaluation of triggering
sources and slide mechanics. Mar. Petrol. Geol., 22, 245-256. doi:
10.1016/J.Marpetgeo.2004.10.019
Lacis, A., Hansen, J., Lee, P., Mitchell, T. and Lebederr, S. (1981).
Greenhouse effects of trace gases. Geophys. Res. Lett., 8, 1035-1038
Lee, H.J. (2009). Timing of occurrence of large submarine landslides
on the Atlantic Ocean margin. Mar. Geol., 264, 53-64. doi: 10.1016/J.
Margeo.2008.09.009
Levin, L.A. (2005). Ecology of cold seep sediments: interactions of fauna
with flow, chemistry and microbes. Oceanogr. and Mar. Biol.: Ann.
Rev., 43, 1-46
Levin, L.A., Mendoza, G.F., Gonzalez, J.P., Thurber, A.R. and Cordes,
E.E. (2010). Diversity of bathyal macrofauna on the northeastern
Pacific margin: the influence of methane seeps and oxygen minimum
zones. Mar. Ecol.-Prog. Ser., 31, 94-110
Liu, X. and Flemings, P.B. (2006). Passing gas through the hydrate
stability zone at southern Hydrate Ridge, offshore Oregon. Earth
Planet Sc. Lett., 241, 211-226
Lopez, C., Spence, G., Hyndman, R. and Kelley, D. (2010). Frontal ridge
slope failure at the northern Cascadia margin: Margin-normal fault
and gas hydrate control. Geology, 38, 967-970. doi: Doi 10.1130/
G31136.1
Macdonald, I., Bender, L., Vardaro, M., Bernard, B. and Brooks, J. (2005).
Thermal and visual time-series at a seafloor gas hydrate deposit on the
Gulf of Mexico slope, Earth and Planetary Science Letters, 233(1-2),
45-59
MacDonald, I.R., Leifer, I., Sassen, R., Stine, P., Mitchell, R. and
Guinasso, N., Jr. (2002). Transfer of hydrocarbons from natural seeps
to the water column and atmosphere. Geofluids, 2, 95-107
Maslin, M., Owen, M., Day, S. and Long, D. (2004). Linking continental-
slope failures and climate change: Testing the clathrate gun
hypothesis. Geology, 32, 53-56. doi: 10.1130/G20114.1