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H. W. Jannasch and Wirsen, C. O., Microbial life in the deep sea, Scientific American, vol. 236, pp. 42–52, 1977.
H. W. Jannasch, Isolation of extremely thermophilic, fermentative archaebacteria from deep-sea geothermal sediments, in Bioprocessing and Biotreatment of Coal, D. L. Wise, Ed. New York: Marcel Dekker, 1990, pp. 417–428.
H. W. Jannasch, Experiments in deep-sea microbiology, Oceanus, vol. 21, pp. 50–57, 1978.
H. W. Jannasch, Cuhel, R. L., Wirsen, C. O., and Taylor, C. D., An approach for in situ studies of deep-sea amphipods and their microbial gut flora, Deep-Sea Research. Part A, Oceanographic Research Papers, vol. 27, pp. 867–872, 1980.
H. W. Jannasch, Eimhjellen, K., Wirsen, C. O., and Farmanfarmaian, A., Microbial degradation of organic matter in the deep sea, Science, vol. 171, pp. 672–675, 1971.
H. W. Jannasch and Mottl, M. J., Geomicrobiology of deep-sea hydrothermal vents, Science, vol. 229, pp. 717–725, 1985.
H. W. Jannasch, Chemolithotrophic productivity at deep-sea hydrothermal vents, in Recent advances in microbial ecology: Proceedings of the 5th International Symposium on Microbiology and Ecology, T. Hattori, Ed. Tokyo: Japan Scientific Societies Press, 1989, pp. 23–27.
H. W. Jannasch, Sulphur emissions and transformations at deep-sea hydrothermal vents, in Evolution of the Global Biogeochemical Sulphur Cycle, P. Brimblecombe, Ed. Chichester, Eng., and New York: Wiley, 1989, pp. 181–189.
H. W. Jannasch, Chemosynthetic production of biomass: An idea from a recent oceanographic discovery, Oceanus, vol. 22, pp. 59–63, 1979.
H. W. Jannasch, Microbiology of deep sea hydrothermal vents, Australian Microbiologist, vol. 11, pp. 370–372, 1990.
H. W. Jannasch, Leben in der Tiefsee auf chemosynthetischer Basis, Naturwissenschaften, vol. 72, pp. 285–290, 1985.
H. W. Jannasch, Interactions between the carbon and sulfur cycles in the marine environment, in Major biogeochemical cycles and their interactions, B. Bolin, Ed. New York, N.Y.: Wiley, 1983, pp. 517–525.
H. W. Jannasch, Chemosynthetically sustained ecosystems in the deep sea, in Autotrophic Bacteria, H. G. Schlegel, Ed. Madison, Wis., and Berlin: Science Tech Publ. and Springer-Verlag, 1989, pp. 147–166.
H. W. Jannasch, The ultimate sink, in Proceedings of the Workshop: Microbial Degradation of Pollutants in Marine Environments, Pensacola Beach, Florida, 9-14 April 1978, A. W. Bourquin, Ed. Gulf Breeze, Fla.: Environmental Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, 1979, pp. 3–9.
J. W. Jamieson, Hannington, M. D., Clague, D. A., Kelley, D. S., Delaney, J. R., Holden, J. F., Tivey, M. K., and Kimpe, L. E., Sulfide geochronology along the Endeavour Segment of the Juan de Fuca Ridge, Geochemistry, Geophysics, Geosystems, vol. 14, pp. 2084–2099, 2013.
J. W. Jamieson, Clague, D. A., and Hannington, M. D., Hydrothermal sulfide accumulation along the Endeavour Segment, Juan de Fuca Ridge, Earth and Planetary Science Letters, vol. 395, pp. 136–148, 2014.
M. V. Jakuba, Modeling and control of an autonomous underwater vehicle with combined foil/thruster actuators, Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution, Cambridge, MA and Woods Hole, MA, 2003.
M. V. Jakuba, Stochastic mapping for chemical plume source localization with application to autonomous hydrothermal vent discovery, Massachusetts Institutte of Technology and Woods Hole Oceanographic Institution, Cambridge, Mass. and Woods Hole, Mass., 2007.
A. Jacobson, Plouviez, S., Thaler, A. D., and Van Dover, C. L., Characterization of 13 polymorphic microsatellite loci in Rimicaris hybisae, a shrimp from deep-sea hydrothermal vents, Conservation Genetics Resources, vol. 5, pp. 449–451, 2013.
A. Jacobson, Plouviez, S., Thaler, A. D., and Van Dover, C. L., Characterization of 9 polymorphic microsatellite loci in Lamellibrachia sp 2, a tubeworm found at deep-sea hydrothermal vents and cold seeps, Conservation Genetics Resources, vol. 5, pp. 1005–1007, 2013.
P. R. Jackson, Ledwell, J. R., and Thurnherr, A. M., Dispersion of a tracer on the East Pacific Rise (9 degrees N–10 degrees N), including the influence of hydrothermal plumes, Deep-Sea Research. Part I: Oceanographic Research Papers, vol. 57, pp. 37–52, 2010.

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