@article {RN2501,
	title = {Three-dimensional magnetic stripes require slow cooling in fast-spread lower ocean crust},
	journal = {Nature},
	volume = {597},
	number = {7877},
	year = {2021},
	pages = {511-515},
	type = {Journal Article},
	doi = {10.1038/s41586-021-03831-6},
	url = {https://app.dimensions.ai/details/publication/pub.1141298634},
	author = {Maher, Sarah M. and Gee, Jeffrey S. and Cheadle, Michael J. and John, Barbara E.}
}
@article {RN2480,
	title = {Toward a global calibration for quantifying past oxygenation in oxygen minimum zones using benthic Foraminifera},
	journal = {Biogeosciences},
	volume = {18},
	number = {9},
	year = {2021},
	pages = {2827-2841},
	type = {Journal Article},
	doi = {10.5194/bg-18-2827-2021},
	url = {https://app.dimensions.ai/details/publication/pub.1137883445 https://bg.copernicus.org/articles/18/2827/2021/bg-18-2827-2021.pdf},
	author = {Tetard, Martin and Licari, Laetitia and Ovsepyan, Ekaterina and Tachikawa, Kazuyo and Beaufort, Luc}
}
@article {RN2521,
	title = {Toward a revision of the bamboo corals: Part 3, deconstructing the Family Isididae},
	journal = {Zootaxa},
	volume = {5047},
	number = {3},
	year = {2021},
	pages = {247-272},
	type = {Journal Article},
	issn = {1175-5326},
	doi = {10.11646/zootaxa.5047.3.2},
	author = {Saucier, E. H. and France, S. C. and Watling, L.}
}
@article {RN2467,
	title = {Transcriptomic Responses of Deep-Sea Corals Experimentally Exposed to Crude Oil and Dispersant},
	journal = {Frontiers in Marine Science},
	volume = {8},
	year = {2021},
	pages = {649909},
	type = {Journal Article},
	doi = {10.3389/fmars.2021.649909},
	url = {https://app.dimensions.ai/details/publication/pub.1136987963 http://dx.doi.org/10.3389/fmars.2021.649909},
	author = {DeLeo, Danielle M. and Glazier, Amanda and Herrera, Santiago and Barkman, Alexandria and Cordes, Erik E.}
}
@article {RN2443,
	title = {Time-series transcriptomics from cold, oxic subseafloor crustal fluids reveals a motile, mixotrophic microbial community},
	journal = {Isme Journal},
	year = {2020},
	type = {Journal Article},
	issn = {1751-7362},
	doi = {10.1038/s41396-020-00843-4},
	author = {Seyler, L. M. and Trembath-Reichert, E. and Tully, B. J. and Huber, J. A.}
}
@article {RN2402,
	title = {Trace element proxies of seafloor hydrothermal fluids based on secondary ion mass spectrometry (SIMS) of black smoker chimney linings},
	journal = {Geochimica Et Cosmochimica Acta},
	volume = {269},
	year = {2020},
	pages = {346-375},
	type = {Journal Article},
	issn = {0016-7037},
	doi = {10.1016/j.gca.2019.09.038},
	author = {Evans, G. N. and Tivey, M. K. and Monteleone, B. and Shimizu, N. and Seewald, J. S. and Rouxel, O. J.}
}
@article {RN2336,
	title = {Temperature control of cold-water coral (Lophelia) mound growth by climate-cycle forcing, Northeast Gulf of Mexico},
	journal = {Deep-Sea Research Part I-Oceanographic Research Papers},
	volume = {140},
	year = {2018},
	pages = {142-158},
	type = {Journal Article},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2018.08.002},
	author = {Roberts, H. H. and Kohl, B.}
}
@article {ISI:000400818400021,
	title = {{Telepresence is a potentially transformative tool for field science}},
	journal = {PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA},
	volume = {114},
	number = {19},
	year = {2017},
	month = {may},
	pages = {4841{\textendash}4844},
	publisher = {NATL ACAD SCIENCES},
	address = {2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA},
	keywords = {AUV Sentry (Autonomous Underwater Vehicle), HOV Alvin (Human Occupied Vehicle)},
	issn = {0027-8424},
	doi = {10.1073/pnas.1703514114},
	author = {Marlow, Jeffrey and Borrelli, Chiara and Jungbluth, Sean P and Hoffman, Colleen and Marlow, Jennifer and Girguis, Peter R and Team, AT-36}
}
@article {Johansen2017,
	title = {{Time series video analysis of bubble release processes at natural hydrocarbon seeps in the Northern Gulf of Mexico}},
	journal = {Marine and Petroleum Geology},
	volume = {82},
	year = {2017},
	pages = {21{\textendash}34},
	abstract = {This research quantifies the rate and volume of oil and gas released from two natural seep sites in the Gulf of Mexico: lease blocks GC600 (1200 m depth) and MC118 (850 m depth). Our objectives were to determine variability in release rates and bubble size at five individual vents and to investigate the effects of tidal fluctuations on bubble release. Observations with autonomous video cameras captured the formation of individual bubbles as they were released through partially exposed deposits of gas hydrate. Image processing techniques determined bubble type (oily, gaseous, and mixed: oily and gaseous), size distribution, release rate, and temporal variations (observation intervals ranged from 3 h to 26 d). A semi-automatic bubble counting algorithm was developed to analyze bubble count and release rates from video data. This method is suitable for discrete vents with small bubble streams commonly seen at seeps and is adaptable to multiple in situ set-ups. Two vents at GC600 (Birthday Candles 1 and Birthday Candles 2) were analyzed. They released oily bubbles with an average diameter of 5.0 mm at a rate of 4.7 bubbles s-1, and 1.3 bubbles s-1, respectively. Approximately 1 km away, within the GC600 seep site, two more vents (Mega Plume 1 and Mega Plume 2) were analyzed. These vents released a mixture of oily and gaseous bubbles with an average diameter of 3.9 mm at a rate of 49 bubbles s-1, and 81 bubbles s-1, respectively. The fifth vent at MC118 (Rudyville) released gaseous bubbles with an average diameter of 3.0 mm at a rate of 127 bubbles s-1. Pressure records at Mega Plume and Rudyville showed a diurnal tidal cycle (24.5 h). Rudyville was the only vent that demonstrated any positive correlation ($\rho$ = 0.60) to the 24.5 h diurnal tidal cycle. However, these observations were not conclusive regarding tidal effects on bubble release.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1016/j.marpetgeo.2017.01.014},
	author = {Johansen, C and Todd, A C and MacDonald, I R}
}
@article {Lee2017,
	title = {{The transfer of bomb radiocarbon and anthropogenic lead to the deep North Atlantic Ocean observed from a deep sea coral}},
	journal = {Earth and Planetary Science Letters},
	volume = {458},
	year = {2017},
	pages = {223{\textendash}232},
	abstract = {Deep-ocean, View the MathML source$Δ$C14, Pb concentrations, and Pb isotopes were reconstructed from a deep-sea coral Enallopsammia rostrata from 1410 m depth off of Bermuda. Our high-resolution time series is created from closely spaced radial cross sections, with samples taken from the center of concentric coral growth bands that we show to be the oldest portion of the section. Prebomb radiocarbon ages from the coral demonstrate that the vertical growth rate of the coral is linear, and the age of the coral is estimated to be 560{\textendash}630 yr old based on the growth rate. Using this age model to reconstruct View the MathML source$Δ$C14 in deep seawater, we first detect bomb radiocarbon at the coral growth site around 1980, and show that View the MathML source$Δ$C14 increased from -80{\textpm}1{\textperthousand}-80{\textpm}1{\textperthousand} (average 1930{\textendash}1979) to a plateau at -39{\textpm}3{\textperthousand}-39{\textpm}3{\textperthousand} (1999{\textendash}2001). Pb/Ca of the coral ranges between 1.1{\textendash}4.5 nmol/mol during the 16th and 17th centuries, and Pb isotope ratios (206Pb/207Pb = 1.21, 208Pb/207Pb = 2.495) in this period agree with pre-anthropogenic values found in the pelagic sediments of the North Atlantic Ocean basin. Coral Pb/Ca is slightly elevated to 6.2{\textpm}0.9 nmol/mol6.2{\textpm}0.9 nmol/mol between the 1740s and the 1850s and then increases to 25.1{\textpm}0.2 nmol/mol25.1{\textpm}0.2 nmol/mol in the 1990s. The increase in coral Pb/Ca is accompanied by a decrease in coral 206Pb/207Pb and 208Pb/207Pb, indicating that the increase was caused by the infiltration of anthropogenic Pb to the coral growth site. Comparing our data to the surface coral View the MathML source$Δ$C14 and Pb records from Bermuda reveals a time scale of tracer transport from the surface ocean to the coral growth site. Some characteristic features, e.g., the bomb-derived View the MathML source$Δ$C14 increase, appear in the deep ocean approximately 25 yr later than the surface, but the overall increase of View the MathML source$Δ$C14 and Pb in the deep ocean is smaller and slower than the surface, showing the importance of mixing during the transport of these tracers.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1016/j.epsl.2016.10.049},
	author = {Lee, J M and Eltgroth, S F and Boyle, E A and Adkins, J F}
}
@article {ISI:000373276200001,
	title = {{Temperature and Redox Effect on Mineral Colonization in Juan de Fuca Ridge Flank Subsurface Crustal Fluids}},
	journal = {FRONTIERS IN MICROBIOLOGY},
	volume = {7},
	year = {2016},
	month = {mar},
	type = {Article},
	abstract = {To examine microbe-mineral interactions in subsurface oceanic crust, we evaluated microbial colonization on crustal minerals that were incubated in borehole fluids for 1 year at the seafloor wellhead of a crustal borehole observatory (IODP Hole U1301A, Juan de Fuca Ridge flank) as compared to an experiment that was not exposed to subsurface crustal fluids (at nearby IODP Hole U1301B). In comparison to previous studies at these same sites, this approach allowed assessment of the effects of temperature, fluid chemistry, and/or mineralogy on colonization patterns of different mineral substrates, and an opportunity to verify the approach of deploying colonization experiments at an observatory wellhead at the seafloor instead of within the borehole. The Hole U1301B deployment did not have biofilm growth, based on microscopy and DNA extraction, thereby confirming the integrity of the colonization design against bottom seawater intrusion. In contrast, the Hole U1301A deployment supported biofilms dominated by Epsilonproteobacteria (43.5{\%} of 370 16S rRNA gene clone sequences) and Gammaproteobacteria (29.3{\%}). Sequence analysis revealed overlap in microbial communities between different minerals incubated at the Hole U1301A wellhead, indicating that mineralogy did not separate biofilm structure within the 1-year colonization experiment. Differences in the Hole U1301A wellhead biofilm community composition relative to previous studies from within the borehole using similar mineral substrates suggest that temperature and the diffusion of dissolved oxygen through plastic components influenced the mineral colonization experiments positioned at the wellhead. This highlights the capacity of low abundance crustal fluid taxa to rapidly establish communities on diverse mineral substrates under changing environmental conditions such as from temperature and oxygen.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1664-302X},
	doi = {10.3339/fmicb.2016.00396},
	author = {Baquiran, Jean-Paul M and Ramirez, Gustavo A and Haddad, Amanda G and Toner, Brandy M and Hulme, Samuel and Wheat, Charles G and Edwards, Katrina J and Orcutt, Beth N}
}
@article {ISI:000371481100019,
	title = {{Thermal and geochemical influences on microbial biogeography in the hydrothermal sediments of Guaymas Basin, Gulf of California}},
	journal = {ENVIRONMENTAL MICROBIOLOGY REPORTS},
	volume = {8},
	number = {1},
	year = {2016},
	month = {feb},
	pages = {150{\textendash}161},
	type = {Article},
	abstract = {Extreme thermal gradients and compressed metabolic zones limit the depth range of microbial colonization in hydrothermally active sediments at Guaymas Basin. We investigated the physicochemical characteristics of this ecosystem and their influence on microbial community structure. Temperature-related trends of C-13 values of methane and dissolved inorganic carbon from 36 sediment cores suggest in situ thermal limits for microbial anaerobic methane oxidation and organic carbon re-mineralization near 80 degrees C and 100 degrees C respectively. Temperature logging probes deposited in hydrothermal sediments for 8 days demonstrate substantial thermal fluctuations of up to 25 degrees C. Putative anaerobic methanotroph (ANME) populations dominate the archaeal community, transitioning from ANME-1 archaea in warm surficial sediments towards ANME-1 Guaymas archaea as temperatures increase downcore. Since ANME archaea performing anaerobic oxidation of methane double on longer time scales (months) compared with relatively rapid in situ temperature fluctuations (hours to days), we conclude that ANME archaea possess a high tolerance for short-term shifts in the thermal regime.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1758-2229},
	doi = {10.1111/1758-2229.12365},
	author = {McKay, Luke and Klokman, Vincent W and Mendlovitz, Howard P and LaRowe, Douglas E and Hoer, Daniel R and Albert, Daniel and Amend, Jan P and Teske, Andreas}
}
@article {ISI:000372952900002,
	title = {{Tracing the production and fate of individual archaeal intact polar lipids using stable isotope probing}},
	journal = {ORGANIC GEOCHEMISTRY},
	volume = {95},
	year = {2016},
	month = {may},
	pages = {13{\textendash}20},
	type = {Article},
	abstract = {Analysis of cellular membrane lipids has been widely applied to describe the microbial community composition in natural systems. When combined with stable isotope probing (SIP) experiments, deuterium label (D2O) uptake into lipids enables assessment of microbial biomass production. We performed SIP on methane-rich, hydrothermally-heated sediments to examine the de novo production of individual archaeal intact polar lipids (IPLs) by mesophilic anaerobic methane oxidizing group-1 archaea (ANME-1). The greatest extent of label uptake was by phosphatidyl glycerol archaeol (PG-AR), reaching 50{\%} of the medium{\textquoteright}s label concentration in only 10 days. This indicates PG-AR as an important cell membrane lipid during the active growth phase of mesophilic ANME-1. Much less label uptake was into intact polar glycerol dibiphytanyl glycerol tetraethers (GDGTs), especially for those bound to diglycosidic head groups. The low production of these GDGTs contrasts with their predominance in ANME-1-dominated natural samples. We attribute the differential label uptake among individual IPLs to the ANME-1 tetraether biosynthetic pathway. This mechanism likely involves head-to-head condensation of two molecules of PG-AR and progressive substitution of PG by glycosidic head groups. The observation that ANME-1 invest in the synthesis of diethers during optimum growth suggests intact ARs and/or phosphate-bearing tetraethers as important biomarkers for actively growing populations in natural environments, while the diglycosidic GDGTs appear to signal stationary ANME-1 communities. (C) 2016 Elsevier Ltd. All rights reserved.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0146-6380},
	doi = {10.1016/j.orggeochem.2016.02.004},
	author = {Kellermann, Matthias Y and Yoshinaga, Marcos Y and Wegener, Gunter and Krukenberg, Viola and Hinrichs, Kai-Uwe}
}
@article {ISI:000370971600005,
	title = {{Transcription, Signaling Receptor Activity, Oxidative Phosphorylation, and Fatty Acid Metabolism Mediate the Presence of Closely Related Species in Distinct Intertidal and Cold-Seep Habitats}},
	journal = {GENOME BIOLOGY AND EVOLUTION},
	volume = {8},
	number = {1},
	year = {2016},
	month = {jan},
	pages = {51{\textendash}69},
	type = {Article},
	abstract = {Bathyal cold seeps are isolated extreme deep-sea environments characterized by low species diversity while biomass can be high. The Hakon Mosby mud volcano (Barents Sea, 1,280 m) is a rather stable chemosynthetic driven habitat characterized by prominent surface bacterial mats with high sulfide concentrations and low oxygen levels. Here, the nematode Halomonhystera hermesithrives in high abundances (11,000 individuals 10 cm(-2)). Halomonhystera hermesi is a member of the intertidal Halomonhystera disjuncta species complex that includes five cryptic species (GD 1-5). GD1-5{\textquoteright}s common habitat is characterized by strong environmental fluctuations. Here, we compared the transcriptomes of H. hermesi and GD1, H. hermesi{\textquoteright}s closest relative. Genes encoding proteins involved in oxidative phosphorylation are more strongly expressed in H. hermesi than in GD1, and many genes were only observed in H. hermesi while being completely absent in GD1. Both observations could in part be attributed to high sulfide concentrations and low oxygen levels. Additionally, fatty acid elongation was also prominent in H. hermesi confirming the importance of highly unsaturated fatty acids in this species. Significant higher amounts of transcription factors and genes involved in signaling receptor activity were observed in GD1 (many of which were completely absent in H. hermesi), allowing fast signaling and transcriptional reprogramming which can mediate survival in dynamic intertidal environments. GC content was approximately 8{\%} higher in H. hermesi coding unigenes resulting in differential codon usage between both species and a higher proportion of amino acids with GC-rich codons in H. hermesi. In general our results showed that most pathways were active in both environments and that only three genes are under natural selection. This indicates that also plasticity should be taken in consideration in the evolutionary history of Halomonhystera species. Such plasticity, as well as possible preadaptation to low oxygen and high sulfide levels might have played an important role in the establishment of a cold-seep Halomonhystera population.},
	keywords = {AUV Sentry (Autonomous Underwater Vehicle)},
	issn = {1759-6653},
	doi = {10.1093/gbe/evv242},
	author = {Van Campenhout, Jelle and Vanreusel, Ann and Van Belleghem, Steven and Derycke, Sofie}
}
@article {Garcia-Pineda2016,
	title = {{Transience and persistence of natural hydrocarbon seepage in Mississippi Canyon, Gulf of Mexico}},
	journal = {Deep Sea Research Part II: Topical Studies in Oceanography},
	volume = {129},
	year = {2016},
	pages = {119{\textendash}129},
	abstract = {Analysis of the magnitude of oil discharged from natural hydrocarbon seeps can improve understanding of the carbon cycle and the Gulf of Mexico (GOM) ecosystem. With use of a large archive of remote sensing data, in combination with geophysical and multibeam data, we identified, mapped, and characterized natural hydrocarbon seeps in the Macondo prospect region near the wreck site of the drill-rig Deepwater Horizon (DWH). Satellite image processing and the cluster analysis revealed locations of previously undetected seep zones. Including duplicate detections, a total of 562 individual gas plumes were also observed in multibeam surveys. In total, SAR imagery confirmed 52 oil-producing seep zones in the study area. In almost all cases gas plumes were associated with oil-producing seep zones. The cluster of seeps in the vicinity of lease block MC302 appeared to host the most persistent and prolific oil vents. Oil slicks and gas plumes observed over the DWH site were consistent with discharges of residual oil from the wreckage. In contrast with highly persistent oil seeps observed in the Green Canyon and Garden Banks lease areas, the seeps in the vicinity of Macondo Prospect were intermittent. The difference in the number of seeps and the quantity of surface oil detected in Green Canyon was almost two orders of magnitude greater than in Mississippi Canyon.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1016/j.dsr2.2015.05.011},
	author = {Garcia-Pineda, O and MacDonald, I and Silva, M and Shedd, W and Daneshgar Asl, S and Schumaker, B}
}
@article {ISI:000367801400177,
	title = {{Trophosome of the Deep-Sea Tubeworm Riftia pachyptila Inhibits Bacterial Growth}},
	journal = {PLOS ONE},
	volume = {11},
	number = {1},
	year = {2016},
	month = {jan},
	type = {Article},
	abstract = {The giant tubeworm Riftia pachyptila lives in symbiosis with the chemoautotrophic gamma-proteobacterium Cand. Endoriftia persephone. Symbionts are released back into the environment upon host death in high-pressure experiments, while microbial fouling is not involved in trophosome degradation. Therefore, we examined the antimicrobial effect of the tubeworm{\textquoteright}s trophosome and skin. The growth of all four tested Gram-positive, but only of one of the tested Gram-negative bacterial strains was inhibited by freshly fixed and degrading trophosome (incubated up to ten days at either warm or cold temperature), while no effect on Saccharomyces cerevisiae was observed. The skin did not show antimicrobial effects. A liquid chromatography-mass spectrometric analysis of the ethanol supernatant of fixed trophosomes lead to the tentative identification of the phospholipids 1-palmitoleyl-2-lyso- phosphatidylethanolamine, 2-palmitoleyl-1-lyso-phosphatidylethanolamine and the free fatty acids palmitoleic, palmitic and oleic acid, which are known to have an antimicrobial effect. As a result of tissue autolysis, the abundance of the free fatty acids increased with longer incubation time of trophosome samples. This correlated with an increasing growth inhibition of Bacillus subtilis and Listeria welshimeri, but not of the other bacterial strains. Therefore, the free fatty acids produced upon host degradation could be the cause of inhibition of at least these two bacterial strains.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1932-6203},
	doi = {10.1371/journal.pone.0146446},
	author = {Klose, Julia and Aistleitner, Karin and Horn, Matthias and Krenn, Liselotte and Dirsch, Verena and Zehl, Martin and Bright, Monika}
}
@article {Lee2015,
	title = {{Temporal and spatial variation in temperature experienced by macrofauna at Main Endeavour hydrothermal vent field}},
	journal = {Deep-Sea Research Part I: Oceanographic Research Papers},
	volume = {106},
	year = {2015},
	pages = {154{\textendash}166},
	abstract = {A significant focus of hydrothermal vent ecological studies has been to understand how species cope with various stressors through physiological tolerance and biochemical resistance. Yet, the environmental conditions experienced by vent species have not been well characterized. This objective requires continuous observations over time intervals that can capture environmental variability at scales that are relevant to animals. We used autonomous temperature logger arrays (four roughly parallel linear arrays of 12 loggers spaced every 10{\textendash}12 cm) to study spatial and temporal variations in the thermal regime experienced by hydrothermal vent macrofauna at a diffuse flow vent. Hourly temperatures were recorded over eight months from 2010 to 2011 at Grotto vent in the Main Endeavour vent field on the Juan de Fuca Ridge, a focus area of the Ocean Networks Canada cabled observatory. The conspicuous animal assemblages in video footage contained Ridgeia piscesae tubeworms, gastropods (primarily Lepetodrilus fucensis), and polychaetes (polynoid scaleworms and the palm worm Paralvinella palmiformis). Two dimensional spatial gradients in temperature were generally stable over the deployment period. The average temperature recorded by all arrays, and in some individual loggers, revealed distinctive fluctuations in temperature that often corresponded with the tidal cycle. We postulate that this may be related to changes in bottom currents or fluctuations in vent discharge. A marked transient temperature increase lasting over a period of days was observed in April 2011. While the distributions and behavior of Juan de Fuca Ridge vent invertebrates may be partially constrained by environmental temperature and temperature tolerance, except for the one transient high-temperature event, observed fluid temperatures were generally similar to the thermal preferences for some species, and typically well below lethal temperatures for all species. Average temperatures of the four arrays ranged from 4.1 to 11.0 {\textdegree}C during the deployment, indicating that on an hourly timescale the temperature conditions in this tubeworm community were fairly moderate and stable. The generality of these findings and behavioral responses of vent organisms to predictable},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1016/j.dsr.2015.10.004},
	author = {Lee, R W and Robert, K and Matabos, M and Bates, A E and Juniper, S K}
}
@article {Quattrini2015,
	title = {{Testing the depth-differentiation hypothesis in a deepwater octocoral}},
	journal = {Proceedings of the Royal Society B: Biological Sciences},
	volume = {282},
	number = {1807},
	year = {2015},
	pages = {20150008},
	abstract = {The depth-differentiation hypothesis proposes that the bathyal region is a source of genetic diversity and an area where there is a high rate of species formation. Genetic differentiation should thus occur over relatively small vertical distances, particularly along the upper continental slope (200-1000 m) where oceanography varies greatly over small differences in depth. To test whether genetic differentiation within deepwater octocorals is greater over vertical rather than geographical distances, Callogorgia delta was targeted. This species commonly occurs throughout the northern Gulf of Mexico at depths ranging from 400 to 900 m. We found significant genetic differentiation (FST = 0.042) across seven sites spanning 400 km of distance and 400 m of depth. A pattern of isolation by depth emerged, but geographical distance between sites may further limit gene flow. Water mass boundaries may serve to isolate populations across depth; however, adaptive divergence with depth is also a possible scenario. Microsatellite markers also revealed significant genetic differentiation (FST = 0.434) between C. delta and a closely related species, Callogorgia americana, demonstrating the utility of microsatellites in species delimitation of octocorals. Results provided support for the depth-differentiation hypothesis, strengthening the notion that factors covarying with depth serve as isolation mechanisms in deep-sea populations.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1098/rspb.2015.0008},
	author = {Quattrini, A M and Baums, I B and Shank, T M and Morrison, C and Cordes, E E}
}
@article {Findlay2015,
	title = {{Trace metal concentration and partitioning in the first 1.5 m of hydrothermal vent plumes along the Mid-Atlantic Ridge: TAG, Snakepit, and Rainbow}},
	journal = {Chemical Geology},
	volume = {412},
	year = {2015},
	pages = {117{\textendash}131},
	abstract = {To determine the significance of metal fluxes from hydrothermal vents, understanding the speciation, reactivity, and possible transformations of metals and metal sulfides within the hydrothermal plume is critical. In this study, we measure the concentration and partitioning of trace metals (Fe, Mn, Cu, Cd, Co, Pb, Ni) and sulfide phases within the first 1.5 m of the rising plume at three vent fields (TAG, Snakepit, and Rainbow) along the Mid-Atlantic Ridge. A HCl/HNO3 leaching method was used to differentiate metals present in metal mono-sulfides from those in pyrite and chalcopyrite. At all three vent sites, Mn and Fe are primarily in the {\textless} 0.2 $μ$m (filtered) portion, whereas Cu, Co, Cd, and Pb are mainly in the unfiltered fraction. Significant concentrations of HNO3-extractable metals were found in the {\textless} 0.2 $μ$m fraction at all three vent sites, indicating that they likely exist in a recalcitrant nanoparticulate phase such as pyrite or chalcopyrite. At TAG and Snakepit, Cu is correlated with Co, as Co enters into chalcopyrite and other CuFeS phases and Zn is correlated with Cd and Pb as they form discrete metal sulfide phases. At Rainbow, Zn, Cd, and Pb are correlated, but Cu and Co are not correlated. The Rainbow data are consistent with the higher metal to sulfide ratio found at Rainbow. These speciation differences are significant as both mineral type and size will affect the amount of metal transported from the vent site and its availability for biogeochemical processes.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1016/j.chemgeo.2015.07.021},
	author = {Findlay, A J and Gartman, A and Shaw, T J and Luther, G W}
}
@article {Feng2014,
	title = {{Time integrated variation of sources of fluids and seepage dynamics archived in authigenic carbonates from Gulf of Mexico Gas Hydrate Seafloor Observatory}},
	journal = {Chemical Geology},
	volume = {385},
	year = {2014},
	pages = {129{\textendash}139},
	abstract = {Authigenic carbonate rocks recovered from the Gulf of Mexico Gas Hydrate Seafloor Observatory in Mississippi Canyon block 118 (MC118) at approximately 900 m water depth were studied using mineralogical, bulk geochemical, and lipid biomarker analyses. Carbonate rocks occurred as fractured blocks and nodular masses incorporated in carbonate breccias. The carbonates were comprised mainly of high-Mg-calcite and aragonite. The stable carbon isotope composition ($δ$13C) of authigenic carbonate varied from - 29.8{\textperthousand} to - 18.1{\textperthousand} vs. V-PDB, suggesting a complex mixture of various carbon sources, including dissolved marine inorganic carbon (DIC), oil, as well as methane. Oxygen isotopes ($δ$18O) varied from + 3.4{\textperthousand} to + 5.8{\textperthousand}. The observed 18O-enrichment in relation to calculated equilibrium values in the carbonates probably reflects decomposition of gas hydrates. The most abundant lipid biomarkers in the carbonates were isoprenoidal glycerol dibiphytanyl glycerol tetraethers (GDGTs), predominated by GDGT-2 and GDGT-3, which are typically indicators of anaerobic methane oxidizing archaea (ANMEs). Mono- and bicyclic biphytanes (derived after ether cleavage of GDGT-2 and GDGT-3) showed strong 13C-depletion, which is characteristic for ANMEs. Interestingly, large differences between the $δ$13C values of the archaeal diether archaeol and acyclic biphytane on the one hand and monocyclic biphytane on the other hand suggest the presence of archaea other than ANMEs. Archaeol and GDGT-0 (containing two acyclic biphytane moieties) are commonly assigned to various methanogenic archaea. Where methane seepage activity is intermediate or low within acoustic wipeout zones at the MC118 gas hydrate site nowadays, microbial communities must have coped with changing conditions as well as longer-term fluctuations in oil and gas seepage or the temporary cessation of hydrocarbon flux in the past. The change from methane seepage to oil seepage or vice versa in addition to flux variability apparently favors the establishment of complex prokaryotic communities dominated by archaea. In addition to anaerobic oxidation of methane, local production of methane is apparently prominent at the study site based on the occurrence of biomarkers of methanogens in the authigenic carbonate. This finding adds to the ongoing multidisciplinary effort to better constrain the environment at the MC118 observatory site and to determine the locally dominant biogeochemical processes.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1016/j.chemgeo.2014.07.020},
	author = {Feng, D and Birgel, D and Peckmann, J and Roberts, H H and Joye, S B and Sassen, R and Liu, X-L and Hinrichs, K -U and Chen, D}
}
@article {Yuecel2013,
	title = {{Temporal trends in vent fluid iron and sulfide chemistry following the 2005/2006 eruption at East Pacific Rise, 9 degrees 50 {\textquoteright} N}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {14},
	number = {4},
	year = {2013},
	pages = {759{\textendash}765},
	abstract = {The chemistry of vent fluids that emanate to the seafloor undergoes dramatic changes after volcanic eruptions. Data on these changes are still limited, but the best studied example is the East Pacific Rise (EPR) at 9{\textdegree}50'N, where the temporal evolution of the vent fluid chemistry after the 1991/1992 eruption was documented. The area underwent another eruption sequence during late 2005/early 2006, and here we show that a similar evolution is recurring in the iron and sulfide contents of the high-temperature fluids sampled in June 2006, January 2007, and June 2008. The vents have had increasing dissolved iron and decreasing acid-volatile sulfide (free sulfide plus FeS) concentrations with 1 order of magnitude variation. In addition, chromium reducible sulfide (mainly pyrite) also had fivefold decreasing concentrations over the 3 years. Our results confirm a pattern that was noted only once before for 9{\textdegree}50'N EPR and emphasize the dramatic yearly variability in the concentrations of iron-sulfur species emanating from vents.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1525-2027},
	doi = {10.1002/ggge.20088},
	author = {Yuecel, M and Luther, G W}
}
@article {Bennett2013,
	title = {{Trophic regions of a hydrothermal plume dispersing away from an ultramafic-hosted vent-system: Von Damm vent-site, Mid-Cayman Rise}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {14},
	number = {2},
	year = {2013},
	pages = {317{\textendash}327},
	abstract = {Deep-sea ultramafic-hosted vent systems have the potential to provide large amounts of metabolic energy to both autotrophic and heterotrophic microorganisms in their dispersing hydrothermal plumes. Such vent-systems release large quantities of hydrogen and methane to the water column, both of which can be exploited by autotrophic microorganisms. Carbon cycling in these hydrothermal plumes may, therefore, have an important influence on open-ocean biogeochemistry. In this study, we investigated an ultramafic-hosted system on the Mid-Cayman Rise, emitting metal-poor and hydrogen sulfide-, methane-, and hydrogen-rich hydrothermal fluids. Total organic carbon concentrations in the plume ranged between 42.1 and 51.1 $μ$M (background = 43.2 {\textpm} 0.7 $μ$M (n = 5)) and near-field plume samples with elevated methane concentrations imply the presence of chemoautotrophic primary production and in particular methanotrophy. In parts of the plume characterized by persistent potential temperature anomalies but lacking elevated methane concentrations, we found elevated organic carbon concentrations of up to 51.1 $μ$M, most likely resulting from the presence of heterotrophic communities, their extracellular products and vent larvae. Elevated carbon concentrations up to 47.4 $μ$M were detected even in far-field plume samples. Within the Von Damm hydrothermal plume, we have used our data to hypothesize a microbial food web in which chemoautotrophy supports a heterotrophic community of microorganisms. Such an active microbial food web would provide a source of labile organic carbon to the deep ocean that should be considered in any future studies evaluating sources and sinks of carbon from hydrothermal venting to the deep ocean.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1002/ggge.20063},
	url = {http://dx.doi.org/10.1002/ggge.20063},
	author = {Bennett, S A and Coleman, Max and Huber, J A and Reddington, E and Kinsey, J C and McIntyre, C and Seewald, J S and German, C R}
}
@article {ISI:000312516200003,
	title = {{Thermosulfurimonas dismutans gen. nov., sp nov., an extremely thermophilic sulfur-disproportionating bacterium from a deep-sea hydrothermal vent}},
	journal = {INTERNATIONAL JOURNAL OF SYSTEMATIC AND EVOLUTIONARY MICROBIOLOGY},
	volume = {62},
	number = {11},
	year = {2012},
	month = {nov},
	pages = {2565{\textendash}2571},
	type = {Article},
	abstract = {An extremely thermophilic, anaerobic, chemolithoautotrophic bacterium (strain S95(T)) was isolated from a deep-sea hydrothermal vent chimney located on the Eastern Lau Spreading Center, Pacific Ocean, at a depth of 1910 m. Cells of strain S95(T) were oval to short Gram-negative rods, 0.5-0.6 mu m in diameter and 1.0-1.5 mu m in length, growing singly or in pairs. Cells were motile with a single polar flagellum. The temperature range for growth was 50-92 degrees C, with an optimum at 74 degrees C. The pH range for growth was 5.5-8.0, with an optimum at pH 7.0. Growth of strain S95(T) was observed at NaCl concentrations ranging from 1.5 to 3.50/o (w/v). Strain S95(T) grew anaerobically with elemental sulfur as an energy source and bicarbonate/CO2 as a carbon source. Elemental sulfur was disproportionated to sulfide and sulfate. Growth was enhanced in the presence of poorly crystalline iron(III) oxide (ferrihydrite) as a sulfide-scavenging agent. Strain S95(T) was also able to grow by disproportionation of thiosulfate and sulfite. Sulfate was not used as an electron acceptor. Analysis of the 16S rRNA gene sequence revealed that the isolate belongs to the phylum Thermodesulfobacteria. On the basis of its physiological properties and results of phylogenetic analyses, it is proposed that the isolate represents the sole species of a new genus, Thermosulfurimonas dismutans gen. nov., sp. nov.; S95(T) (=DSM 24515(T)=VKM B-2683(T)) is the type strain of the type species. This is the first description of a thermophilic microorganism that disproportionates elemental sulfur.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1466-5026},
	doi = {10.1099/ijs.0.034397-0},
	author = {Slobodkin, A I and Reysenbach, A -L. and Slobodkina, G B and Baslerov, R V and Kostrikina, N A and Wagner, I D and Bonch-Osmolovskaya, E A}
}
@article {ISI:000308207400009,
	title = {{The Transcriptome of Bathymodiolus azoricus Gill Reveals Expression of Genes from Endosymbionts and Free-Living Deep-Sea Bacteria}},
	journal = {MARINE DRUGS},
	volume = {10},
	number = {8},
	year = {2012},
	month = {aug},
	pages = {1765{\textendash}1783},
	type = {Article},
	abstract = {Deep-sea environments are largely unexplored habitats where a surprising number of species may be found in large communities, thriving regardless of the darkness, extreme cold, and high pressure. Their unique geochemical features result in reducing environments rich in methane and sulfides, sustaining complex chemosynthetic ecosystems that represent one of the most surprising findings in oceans in the last 40 years. The deep-sea Lucky Strike hydrothermal vent field, located in the Mid Atlantic Ridge, is home to large vent mussel communities where Bathymodiolus azoricus represents the dominant faunal biomass, owing its survival to symbiotic associations with methylotrophic or methanotrophic and thiotrophic bacteria. The recent transcriptome sequencing and analysis of gill tissues from B. azoricus revealed a number of genes of bacterial origin, hereby analyzed to provide a functional insight into the gill microbial community. The transcripts supported a metabolically active microbiome and a variety of mechanisms and pathways, evidencing also the sulfur and methane metabolisms. Taxonomic affiliation of transcripts and 16S rRNA community profiling revealed a microbial community dominated by thiotrophic and methanotrophic endosymbionts of B. azoricus and the presence of a Sulfurovum-like epsilonbacterium.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1660-3397},
	doi = {10.3390/md10081765},
	author = {Egas, Conceicao and Pinheiro, Miguel and Gomes, Paula and Barroso, Cristina and Bettencourt, Raul}
}
@article {ISI:000208863500072,
	title = {{Thermodynamics and kinetics of sulfide oxidation by oxygen: a look at inorganically controlled reactions and biologically mediated processes in the environment}},
	journal = {FRONTIERS IN MICROBIOLOGY},
	volume = {2},
	year = {2011},
	type = {Article},
	abstract = {The thermodynamics for the first electron transfer step for sulfide and oxygen indicates that the reaction is unfavorable as unstable superoxide and bisulfide radical ions would need to be produced. However, a two-electron transfer is favorable as stable S(0) and peroxide would be formed, but the partially filled orbitals in oxygen that accept electrons prevent rapid kinetics. Abiotic sulfide oxidation kinetics improve when reduced iron and/or manganese are oxidized by oxygen to form oxidized metals which in turn oxidize sulfide. Biological sulfur oxidation relies on enzymes that have evolved to overcome these kinetic constraints to affect rapid sulfide oxidation. Here we review the available thermodynamic and kinetic data for H2S and HS center dot as well as O-2, reactive oxygen species, nitrate, nitrite, and NOx species. We also present new kinetic data for abiotic sulfide oxidation with oxygen in trace metal clean solutions that constrain abiotic rates of sulfide oxidation in metal free solution and agree with the kinetic and thermodynamic calculations. Moreover, we present experimental data that give insight on rates of chemolithotrophic and photolithotrophic sulfide oxidation in the environment. We demonstrate that both anaerobic photolithotrophic and aerobic chemolithotrophic sulfide oxidation rates are three or more orders of magnitude higher than abiotic rates suggesting that in most environments biotic sulfide oxidation rates will far exceed abiotic rates due to the thermodynamic and kinetic constraints discussed in the first section of the paper. Such data reshape our thinking about the biotic and abiotic contributions to sulfide oxidation in the environment.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1664-302X},
	doi = {10.3389/fmicb.2011.00062},
	author = {Luther III, George W and Findlay, Alyssa J and MacDonald, Daniel J and Owings, Shannon M and Hanson, Thomas E and Beinart, Roxanne A and Girguis, Peter R}
}
@article {Luther2011,
	title = {{Thermodynamics and kinetics of sulfide oxidation by oxygen: a look at inorganically controlled reactions and biologically mediated processes in the environment}},
	journal = {Frontiers in Microbiology},
	volume = {2},
	year = {2011},
	pages = {62},
	publisher = {FRONTIERS RESEARCH FOUNDATION},
	address = {LAUSANNE; PO BOX 110, LAUSANNE, 1015, SWITZERLAND},
	abstract = {The thermodynamics for the first electron transfer step for sulfide and oxygen indicates that the reaction is unfavorable as unstable superoxide and bisulfide radical ions would need to be produced. However, a two-electron transfer is favorable as stable S(0) and peroxide would be formed, but the partially filled orbitals in oxygen that accept electrons prevent rapid kinetics. Abiotic sulfide oxidation kinetics improve when reduced iron and/or manganese are oxidized by oxygen to form oxidized metals which in turn oxidize sulfide. Biological sulfur oxidation relies on enzymes that have evolved to overcome these kinetic constraints to affect rapid sulfide oxidation. Here we review the available thermodynamic and kinetic data for H2S and HS center dot as well as O-2, reactive oxygen species, nitrate, nitrite, and NOx species. We also present new kinetic data for abiotic sulfide oxidation with oxygen in trace metal clean solutions that constrain abiotic rates of sulfide oxidation in metal free solution and agree with the kinetic and thermodynamic calculations. Moreover, we present experimental data that give insight on rates of chemolithotrophic and photolithotrophic sulfide oxidation in the environment. We demonstrate that both anaerobic photolithotrophic and aerobic chemolithotrophic sulfide oxidation rates are three or more orders of magnitude higher than abiotic rates suggesting that in most environments biotic sulfide oxidation rates will far exceed abiotic rates due to the thermodynamic and kinetic constraints discussed in the first section of the paper. Such data reshape our thinking about the biotic and abiotic contributions to sulfide oxidation in the environment.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1664-302X},
	doi = {10.3389/fmicb.2011.00062},
	author = {Luther, G W and Findlay, A J and MacDonald, D J and Owings, S M and Hanson, T E and Beinart, R A and Girguis, P R}
}
@article {ISI:000299052400011,
	title = {{Thermophilic anaerobic oxidation of methane by marine microbial consortia}},
	journal = {ISME JOURNAL},
	volume = {5},
	number = {12},
	year = {2011},
	month = {dec},
	pages = {1946{\textendash}1956},
	type = {Article},
	abstract = {The anaerobic oxidation of methane (AOM) with sulfate controls the emission of the greenhouse gas methane from the ocean floor. AOM is performed by microbial consortia of archaea (ANME) associated with partners related to sulfate-reducing bacteria. In vitro enrichments of AOM were so far only successful at temperatures {\textless}= 25 degrees C; however, energy gain for growth by AOM with sulfate is in principle also possible at higher temperatures. Sequences of 16S rRNA genes and core lipids characteristic for ANME as well as hints of in situ AOM activity were indeed reported for geothermally heated marine environments, yet no direct evidence for thermophilic growth of marine ANME consortia was obtained to date. To study possible thermophilic AOM, we investigated hydrothermally influenced sediment from the Guaymas Basin. In vitro incubations showed activity of sulfate-dependent methane oxidation between 5 and 70 degrees C with an apparent optimum between 45 and 60 degrees C. AOM was absent at temperatures {\textgreater}= 75 degrees C. Long-term enrichment of AOM was fastest at 50 degrees C, yielding a 13-fold increase of methane-dependent sulfate reduction within 250 days, equivalent to an apparent doubling time of 68 days. The enrichments were dominated by novel ANME-1 consortia, mostly associated with bacterial partners of the deltaproteobacterial HotSeep-1 cluster, a deeply branching phylogenetic group previously found in a butane-amended 60 degrees C-enrichment culture of Guaymas sediments. The closest relatives (Desulfurella spp.; Hippea maritima) are moderately thermophilic sulfur reducers. Results indicate that AOM and ANME archaea could be of biogeochemical relevance not only in cold to moderate but also in hot marine habitats. The ISME Journal (2011) 5, 1946-1956; doi: 10.1038/ismej.2011.77; published online 23 June 2011},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1751-7362},
	doi = {10.1038/ismej.2011.77},
	author = {Holler, Thomas and Widdel, Friedrich and Knittel, Katrin and Amann, Rudolf and Kellermann, Matthias Y and Hinrichs, Kai-Uwe and Teske, Andreas and Boetius, Antje and Wegener, Gunter}
}
@article {ISI:000294119400002,
	title = {{Three new species of pennatulacean octocorals with the ability to attach to rocky substrata (Cnidaria: Anthozoa: Pennatulacea)}},
	journal = {ZOOTAXA},
	number = {3001},
	year = {2011},
	month = {aug},
	pages = {33{\textendash}48},
	type = {Article},
	abstract = {All sea pens have been thought to anchor in soft sediment using a basal, sausage-shaped, muscular peduncle. Based on underwater images and examination of specimens, we report an adaptation of the proximal portion of the peduncle for attachment to solid surfaces. We document four species with this adaptation, three new, Anthoptilum lithophilum sp. nov. (California, 669-700 m), A. gowlettholmesae sp. nov. (Tasmania, 729-1803 m), and Calibelemnon francei sp. nov. (the Bahamas, 1969 m), and one known, A. decipiens Thomson {\&} Henderson, 1906 (Sri Lanka, 925 m). The peduncle of a colony with this adaptation is greatly expanded by an outgrowth of the coenenchyme that forms a sucker-like structure, beneath which a conical mass of tough tissue surrounds the proximal end of the internal axis. We infer this structure affects suction, increasing or decreasing the strength of adhesion to the substratum, and discuss the systematics and functional morphology of this new ecological phenomenon-pennatulaceans fastened to hard substrata. We alter the definition of the genus Anthoptilum to accommodate this morphology, reporting on specimens of the type species, A. grandiflorum; compare the two sea pen families-Anthoptilidae and Scleroptilidae- and the two genera; and present a key to the known rock-inhabiting species.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1175-5326},
	author = {Williams, Gary C and Alderslade, Philip}
}
@article {Bennett2011a,
	title = {{Tracing iron-fueled microbial carbon production within the hydrothermal plume at the Loihi Seamount}},
	journal = {Geochimica et Cosmochimica Acta},
	volume = {75},
	number = {19},
	year = {2011},
	pages = {5526{\textendash}5539},
	abstract = {The Loihi hydrothermal plume provides an opportunity to investigate iron (Fe) oxidation and microbial processes in a system that is truly Fe dominated and distinct from mid-ocean ridge spreading centers. The lack of hydrogen sulfide within the Loihi hydrothermal fluids and the presence of an oxygen minimum zone at this submarine volcano{\textquoteright}s summit, results in a prolonged presence of reduced Fe within the dispersing non-buoyant plume. In this study, we have investigated the potential for microbial carbon fixation within the Loihi plume. We sampled for both particulate and dissolved organic carbon in hydrothermal fluids, microbial mats growing around vents, and the dispersing plume, and carried out stable carbon isotope analysis on the particulate fraction. The $δ$13C values of the microbial mats ranged from -23{\textperthousand} to -28{\textperthousand}, and are distinct from those of deep-ocean particulate organic carbon (POC). The mats and hydrothermal fluids were also elevated in dissolved organic carbon (DOC) compared to background seawater. Within the hydrothermal plume, DOC and POC concentrations were elevated and the isotopic composition of POC within the plume suggests mixing between background seawater POC and a 13C-depleted hydrothermal component. The combination of both DOC and POC increasing in the dispersing plume that cannot solely be the result of entrainment and DOC adsorption, provides strong evidence for in-situ microbial productivity by chemolithoautotrophs, including a likelihood for iron-oxidizing microorganisms.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0016-7037},
	doi = {10.1016/j.gca.2011.06.039},
	url = {http://dx.doi.org/10.1016/j.gca.2011.06.039},
	author = {Bennett, S A and Hansman, R L and Sessions, A L and Nakamura, K and Edwards, K J}
}
@article {Thresher2010,
	title = {{Temperature effects on the calcite skeletal composition of deep-water gorgonians (isididae)}},
	journal = {Geochimica et Cosmochimica Acta},
	volume = {74},
	number = {16},
	year = {2010},
	pages = {4655{\textendash}4670},
	abstract = {We test for and calibrate a proxy for ocean temperature based on the skeletal composition of the widely distributed, deep-sea gorgonians in the family Isididae (bamboo corals), through use of three complementary methods: a short-term comparison of element/Ca ratios to a four-year temperature record, a long-term comparison with oceanographic records spanning forty years, and a geographic comparison of Isidids collected at sites ranging from the tropics to Antarctica. The assays consistently support a temperature-dependency for Mg/Ca ratios and suggest S/Ca is indirectly affected by temperature, but indicate little or no effect of temperature on P/Ca and Sr/Ca. The consensus relationship between Mg/Ca and temperature for Isidid calcite from the comparisons with the temperature time-series is T = -0.505 + 0.048 Mg/Ca, where T is in {\textdegree}C, Mg/Ca is in mmol/mol, and the applicable range is 3{\textendash}6 {\textdegree}C. The results of the geographic assay, though imprecise, suggest the applicable range extends to temperatures below freezing. The scatter of data points around the regression of temperature and Mg/Ca is wide in all assays. This could reflect the effect of factors other than temperature on Mg/Ca ratios, but is also likely to reflect limitations of the field data, the effects of assumed constant growth rates in the corals and instrumental analytical error. The combined effects of micro-scale variability in growth rates and wide confidence intervals for each data point suggests that environmental reconstruction from Isidid internode calcite from sparse data or at time scales less than decades be done with caution. Comparisons within and among colonies do not indicate strong vital effects on ontogenetic variability in the corals, other than possibly close to the central pore of the coral. However, similar Mg/Ca ratios for Isidids from Antarctic and more temperate regions suggest adaptation to local conditions and hence a role for physiology at higher taxonomic levels, at least. Taxonomically higher level vital effects are also suggested by large differences between gorgonian families in their regressions between Mg/Ca and temperature, by Mg/Ca ratios that overlap over a wide temperature and habitat range, and for a non-linear relationship between temperature and the slope of the Mg/Ca-temperature relationship across the order.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0016-7037},
	doi = {10.1016/j.gca.2010.05.024},
	url = {http://dx.doi.org/10.1016/j.gca.2010.05.024},
	author = {Thresher, R E and Wilson, N C and MacRae, C M and Neil, H}
}
@mastersthesis {Waters2010,
	title = {{Temporal and petrogenetic constraints on volcanic accretionary processes at 9-10 degrees north East Pacific Rise}},
	volume = {Ph.D.},
	year = {2010},
	pages = {258},
	school = {Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution},
	type = {phd},
	address = {Cambridge, MA and Woods Hole, MA},
	abstract = {Volcanic accretion at the fast-spreading East Pacific Rise (EPR) occurs over a {\~{}}2-4 km wide neo-volcanic zone on either side of the axial summit trough (AST). Eruption ages are critical for understanding the distribution and timing of volcanic and magmatic activity. Uranium series nuclides are susceptible to fractionation by magmatic processes that occur beneath mid-ocean ridges, and the half-lives of 226Ra (1.6 kyrs) and 230Th (75 kyrs) make them ideally suited for determining eruption ages and placing constraints on eruption frequency and temporal changes in magma chemistry. Accordingly, major and trace element, and long-lived radiogenic and 238U-230Th-226Ra isotope compositions were measured in basalts from 9{\textordmasculine}-10{\textordmasculine}N EPR to determine eruption ages and to place temporal constraints on volcanic and magmatic processes. At 9{\textordmasculine}30{\textquoteright}N EPR, 238U-230Th-226Ra compositions indicate that trace elementally and isotopically enriched mid-ocean ridge basalt (MORB) collected off-axis erupted {\textgreater}8 ka and that E-MORB magmatism is interspersed with normal, depleted MORB magmatism. Lava ages are consistent with eruption from the AST and flow down the ridge flanks, which is in contrast to previous studies that suggested E-MORB erupted from off-axis vents. At 9{\textordmasculine}50{\textquoteright}N EPR, discrete eruptive units are distinguished by high precision 238U, 232Th, and 226Ra sample concentrations, but because the resolution of the 230Th-226Ra model age dating technique is {\~{}}{\textpm}1 kyrs, the surprisingly young ages of these lavas prohibit the construction of an explicit, time-constrained lava stratigraphy. Nonetheless, seven different flows identified within 0.8-2.0 km west of the AST imply greater frequency of flows to these distances than previously recognized. Model age dating of ferrobasalts, basaltic andesites, andesites, and dacites sampled from the east limb of the overlapping spreading center at 9{\textordmasculine}03{\textquoteright}N EPR is difficult due to uncertainties in magma residence times. However, (226Ra/230Th) disequilibria indicate recent basaltic volcanism ({\textless}{\textless}8 ka) up to {\~{}}4 km off-axis. The axial graben at the rise crest sources the most recent volcanic activity and is the dominant location for eruption of high-silica magmas. Major element, trace element, 87Sr/86Sr, and (234U/238U) isotope compositions are consistent with the formation of dacite magmas by extensive crystallization, and 238U-230Th-226Ra systematics imply crustal residence times of {\~{}}8 kyrs.},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1575/1912/3750},
	url = {http://hdl.handle.net/1912/3750},
	author = {Waters, C L}
}
@article {ISI:000280049400003,
	title = {{Thermally stimulated {\textquoteleft}{\textquoteleft}runaway{\{}{\textquoteright}{\textquoteright}{\}} downhole flow in a superhydrostatic ocean crustal borehole: Observations, simulations, and inferences regarding crustal permeability}},
	journal = {JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH},
	volume = {115},
	year = {2010},
	month = {jul},
	type = {Article},
	abstract = {An array of boreholes, drilled through a regionally continuous hydrologically confining layer of sediments into extrusive igneous basement rocks of the Juan de Fuca Ridge eastern flank, has been instrumented with CORK hydrologic observatories for long-term monitoring and fluid sampling. Omission of seals between nested casing strings reaching into basement at one site created a low-resistance connection between basement and the overlying water column, and despite the natural superhydrostatic state of basement water at that location, a {\textquoteleft}{\textquoteleft}runaway{\{}{\textquoteright}{\textquoteright}{\}} condition of cold seawater downhole flow into the crust was established, which persisted for more than 4 years. The existence of this condition, along with perturbations generated by it and by initial drilling operations observed at a properly sealed hole 2.4 km away, have been used with analytic and finite element model solutions to constrain formation permeability. The minimum threshold permeability allowing stable downhole flow is roughly 4 x 10(-13) m(2). A value of permeability similar to this (3-4 x 10(-13) m(2)) is estimated on the basis of the elapsed time for initial perturbations to propagate between the sites (similar to 2.5 days). The amplitude of the long-term flow perturbation observed at the sealed site (roughly 1.7 kPa) is smaller than that predicted by modeling (5-10 kPa). Models for flow in an anisotropically permeable layer show that this could be the consequence of low vertical permeability (e. g., arising from massive volcanic or sediment interlayering) or high permeability in the direction of the tectonic fabric generated at the ridge axis. Disagreement between the permeabilities estimated here with previous large-scale estimates appropriate for the cross-strike direction (the primary direction between the borehole sites) (10(-10)-10(-9) m(2)) is difficult to reconcile; it is possible that the holes are poorly connected to zones of high permeability that facilitate the large lateral fluid and heat fluxes previously inferred at this young crustal site.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2009JB006986},
	author = {Davis, Earl E and LaBonte, Alison and He, Jiangheng and Becker, Keir and Fisher, Andrew}
}
@article {Moore2009,
	title = {{Time-series chemical and temperature habitat characterization of diffuse flow hydrothermal sites at 9 degrees 50'N East Pacific Rise}},
	journal = {Deep-Sea Research. Part II: Topical Studies in Oceanography},
	volume = {56},
	number = {19-20},
	year = {2009},
	pages = {1616{\textendash}1621},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0645},
	doi = {10.1016/j.dsr2.2009.05.008},
	url = {http://dx.doi.org/10.1016/j.dsr2.2009.05.008},
	author = {Moore, T S and Shank, T M and Nuzzio, D B and Luther, G W}
}
@article {Komai2008,
	title = {{Taxonomic review of the hydrothermal vent shrimp Genera Rimicaris Williams {\&} Rona and Chorocaris Martin {\&} Hessler (Crustacea: Decapoda: Caridea: Alvinocarididae)}},
	journal = {Journal of Shellfish Research},
	volume = {27},
	number = {1},
	year = {2008},
	pages = {21{\textendash}41},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0730-8000},
	doi = {10.2983/0730-8000(2008)27[21:TROTHV]2.0.CO;2},
	url = {http://dx.doi.org/10.2983/0730-8000(2008)27[21:TROTHV]2.0.CO 2},
	author = {Komai, T and Segonzac, M}
}
@article {McLean2008,
	title = {{Three new species of the family Neolepetopsidae (Patellogastropoda) from hydrothermal vents and whale falls in the Northeastern Pacific}},
	journal = {Journal of Shellfish Research},
	volume = {27},
	number = {1},
	year = {2008},
	pages = {15{\textendash}20},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0730-8000},
	doi = {10.2983/0730-8000(2008)27[15:TNSOTF]2.0.CO;2},
	url = {http://dx.doi.org/10.2983/0730-8000(2008)27[15:TNSOTF]2.0.CO 2},
	author = {McLean, J H}
}
@article {Yoerger2007a,
	title = {{Techniques for deep sea near bottom survey using an autonomous underwater vehicle}},
	journal = {International Journal of Robotics Research},
	volume = {26},
	number = {1},
	year = {2007},
	pages = {41{\textendash}54},
	keywords = {AUV ABE (Autonomous Benthic Explorer)},
	issn = {0278-3649},
	doi = {10.1007/978-3-540-48113-3_36},
	url = {http://dx.doi.org/10.1007/978-3-540-48113-3{\_}36},
	author = {Yoerger, D R and Jakuba, M V and Bradley, A M and Bingham, B}
}
@article {Sheader2007,
	title = {{Temporal and spatial variation in the reproductive ecology of the vent-endemic amphipod Ventiella sulfuris in the eastern Pacific}},
	journal = {Marine Ecology Progress Series},
	volume = {331},
	year = {2007},
	pages = {181{\textendash}194},
	abstract = {Populations of the vent-endemic amphipod Ventiella sulfuris were compared from 6 East Pacific Rise (EPR) vent sites of different ages, 3 from the northern EPR and 3 from the southern EPR. Although vent age affected amphipod abundance, with no individuals at the oldest vent, other population/reproductive parameters were found to be site dependent rather than vent age dependent. There was little within-site variation in population structure and reproductive output, probably the result of high within-site motility. However, there were significant between-site and between-field differences, indicating a high degree of population and reproductive variability and a moderate degree of vent fidelity. Since population structure and reproductive output varied between sites, the possibility of their use as biomarkers of vent {\textquoteright}condition{\textquoteright} is discussed. The reproductive ecology of V. sulfuris is described for the first time and compared to that of other vent amphipod species. Unlike other species studied, reproductive output is relatively high. Adults move to the periphery of vents to reproduce and brood; after brooding, they moult again, return to feed at vent habitats (e.g. mussel and tube worm beds), and undergo a new phase of gonad maturation and emigration.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0171-8630},
	doi = {10.3354/meps331181},
	author = {Sheader, M and Van Dover, C L}
}
@article {Hornbach2007,
	title = {{Three-dimensional structure of fluid conduits sustaining an active deep marine cold seep}},
	journal = {Geophysical Research Letters},
	volume = {34},
	number = {5},
	year = {2007},
	pages = {L05601},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0094-8276},
	doi = {10.1029/2006gl028859},
	url = {http://dx.doi.org/10.1029/2006gl028859},
	author = {Hornbach, M J and Ruppel, C D and Van Dover, C L}
}
@article {Shank2007,
	title = {{Toward a mechanistic understanding of larval dispersal: insights from genomic fingerprinting of the deep-sea hydrothermal vent tubeworm Riftia pachyptila}},
	journal = {Marine Ecology},
	volume = {28},
	number = {1},
	year = {2007},
	pages = {25{\textendash}35},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0173-9565},
	doi = {10.1111/j.1439-0485.2007.00146.x},
	url = {http://dx.doi.org/10.1111/j.1439-0485.2007.00146.x},
	author = {Shank, T M and Halanych, K M}
}
@article {Singh2007a,
	title = {{Towards high-resolution imaging from underwater vehicles}},
	journal = {International Journal of Robotics Research},
	volume = {26},
	number = {1},
	year = {2007},
	pages = {55{\textendash}74},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0278-3649},
	doi = {10.1007/978-3-540-48113-3_37},
	url = {http://dx.doi.org/10.1007/978-3-540-48113-3{\_}37},
	author = {Singh, H and Roman, C and Pizarro, O and Eustice, R and Can, A}
}
@article {Prieto2007,
	title = {{Transparent exopolymer particles in a deep-sea hydrothermal system: Guaymas Basin, Gulf of California}},
	journal = {Marine Biology},
	volume = {150},
	number = {6},
	year = {2007},
	pages = {1093{\textendash}1101},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3162},
	doi = {10.1007/s00227-006-0430-1},
	url = {http://dx.doi.org/10.1007/s00227-006-0430-1},
	author = {Prieto, L and Cowen, J P}
}
@article {Gollner2007,
	title = {{Tubeworm-associated permanent meiobenthic communities from two chemically different hydrothermal vent sites on the East Pacific Rise}},
	journal = {Marine Ecology Progress Series},
	volume = {337},
	year = {2007},
	pages = {39{\textendash}49},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0171-8630},
	doi = {10.3354/meps337039},
	url = {http://dx.doi.org/10.3354/meps337039},
	author = {Gollner, S and Zekeley, J and Govenar, B and Le Bris, N and Nemeschkal, H L and Fisher, C R and Bright, M}
}
@article {Larsen2006,
	title = {{Tanaidacea (Crustacea; Peracarida) from chemically reduced habitats - the hydrothermal vent system of the Juan de Fuca Ridge, Escabana Trough and Gorda Ridge, northeast Pacific}},
	journal = {Zootaxa},
	number = {1164},
	year = {2006},
	pages = {1{\textendash}33},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {1175-5326},
	url = {http://www.mapress.com/zootaxa/2006/zt01164p033.pdf},
	author = {Larsen, K}
}
@article {Scheirer2006,
	title = {{Temperature variations at diffuse and focused flow hydrothermal vent sites along the northern East Pacific Rise}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {7},
	year = {2006},
	pages = {Q03002},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2005gc001094},
	url = {http://dx.doi.org/10.1029/2005gc001094},
	author = {Scheirer, D S and Shank, T M and Fornari, D J}
}
@article {Davis2006,
	title = {{Transient formation fluid pressures and temperatures in the Costa Rica forearc prism and subducting oceanic basement: CORK monitoring at ODP Sites 1253 and 1255}},
	journal = {Earth and Planetary Science Letters},
	volume = {245},
	number = {1-2},
	year = {2006},
	pages = {232{\textendash}244},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2006.02.042},
	url = {http://dx.doi.org/10.1016/j.epsl.2006.02.042},
	author = {Davis, E E and Villinger, H W}
}
@article {Pollock2005,
	title = {{Temporal and spatial variability in the composition of lavas exposed along the Western Blanco Transform Fault}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {6},
	year = {2005},
	pages = {Q11009},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2005gc001026},
	url = {http://dx.doi.org/10.1029/2005gc001026},
	author = {Pollock, M A and Klein, E M and Karson, J A and Tivey, M A}
}
@article {Becker2004,
	title = {{Temperature and video logs from the upper oceanic crust, Holes 504B and 896A, Costa Rica Rift flank: implications for the permeability of upper oceanic crust}},
	journal = {Earth and Planetary Science Letters},
	volume = {222},
	number = {3-4},
	year = {2004},
	pages = {881{\textendash}896},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2004.03.033},
	url = {http://dx.doi.org/10.1016/j.epsl.2004.03.033},
	author = {Becker, K and Davis, E E and Spiess, F N and DeMoustier, C P}
}
@article {Hunt2004,
	title = {{Testing biological control of colonization by vestimentiferan tubeworms at deep-sea hydrothermal vents (East Pacific Rise, 9 degrees 50{\textquoteright}N)}},
	journal = {Deep-Sea Research. Part I: Oceanographic Research Papers},
	volume = {51},
	number = {2},
	year = {2004},
	pages = {225{\textendash}234},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2003.10.008},
	url = {http://dx.doi.org/10.1016/j.dsr.2003.10.008},
	author = {Hunt, H L and Metaxas, A and Jennings, R L and Halanych, K M and Mullineaux, L S}
}
@article {Vetriani2004,
	title = {{Thermovibrio ammonificans sp. nov.: A thermophilic, chemolithotrophic, nitrate ammonifying bacterium from deep-sea hydrothermal vents.}},
	journal = {International Journal of Systematic and Evolutionary Microbiology},
	volume = {54},
	number = {1},
	year = {2004},
	pages = {175{\textendash}181},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1456-5026},
	doi = {10.1099/ijs.0.02781-0},
	url = {http://dx.doi.org/10.1099/ijs.0.02781-0},
	author = {Vetriani, C and Speck, M D and Ellor, S V and Lutz, R A and Starovoytov, V}
}
@article {Raulfs2004,
	title = {{Tissue and symbiont condition of mussels (Bathymodiolus thermophilus) exposed to varying levels of hydrothermal activity}},
	journal = {Journal of the Marine Biological Association of the United Kingdom},
	volume = {84},
	number = {1},
	year = {2004},
	pages = {229{\textendash}234},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3154},
	doi = {10.1017/S0025315404009087h},
	url = {http://dx.doi.org/10.1017/S0025315404009087h},
	author = {Raulfs, E C and Macko, S A and Van Dover, C L}
}
@article {Pizarro2003,
	title = {{Toward large-area mosaicing for underwater scientific applications}},
	journal = {IEEE Journal of Oceanic Engineering},
	volume = {28},
	number = {4},
	year = {2003},
	pages = {651{\textendash}672},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0364-9059},
	doi = {10.1109/JOE.2003.819154},
	url = {http://dx.doi.org/10.1109/JOE.2003.819154},
	author = {Pizarro, O and Singh, H}
}
@article {Govenar2002,
	title = {{Three Ridgeia piscesae assemblages from a single Juan de Fuca Ridge sulphide edifice: Structurally different and functionally similar}},
	journal = {Cahiers de Biologie Marine},
	volume = {43},
	number = {3-4},
	year = {2002},
	pages = {247{\textendash}252},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0007-9723},
	url = {http://cbm-online.sb-roscoff.fr/pdf/cb43-3-247-252.pdf},
	author = {Govenar, B W and Bergquist, D C and Urcuyo, I A and Eckner, J T and Fisher, C R}
}
@article {Wheat2002,
	title = {{Trace element and REE composition of a low-temperature ridge flank hydrothermal spring}},
	journal = {Geochimica et Cosmochimica Acta},
	volume = {66},
	number = {21},
	year = {2002},
	pages = {3693{\textendash}3705},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0016-7037},
	doi = {10.1016/S0016-7037(02)00894-3},
	url = {http://dx.doi.org/10.1016/S0016-7037(02)00894-3},
	author = {Wheat, C G and Mottl, M J and Rudniki, M}
}
@article {VanDover2002a,
	title = {{Trophic relationships among invertebrates at the Kairei hydrothermal vent field (Central Indian Ridge)}},
	journal = {Marine Biology},
	volume = {141},
	number = {4},
	year = {2002},
	pages = {761{\textendash}772},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0025-3162},
	doi = {10.1007/s00227-002-0865-y},
	url = {http://dx.doi.org/10.1007/s00227-002-0865-y},
	author = {Van Dover, C L}
}
@article {Williams2001,
	title = {{Tidal currents at hydrothermal vents, Juan de Fuca Ridge}},
	journal = {Sea Technology},
	volume = {42},
	number = {6},
	year = {2001},
	pages = {62{\textendash}96},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0093-3651},
	author = {Williams, A J and Tivey, M K}
}
@article {Chevaldonne2000,
	title = {{Thermotolerance and the {\textquoteleft}Pompeii worms{\textquoteright}}},
	journal = {Marine Ecology Progress Series},
	volume = {208},
	year = {2000},
	pages = {293{\textendash}295},
	author = {Chevaldonne, P and Fisher, C R and Childress, J J and Desbruyeres, D and Jollivet, D and Zal, F and Toulmond, A}
}
@article {Mullineaux2000,
	title = {{Tubeworm succession at hydrothermal vents: Use of biogenic cues to reduce habitat selection error?}},
	journal = {Oecologia},
	volume = {123},
	number = {2},
	year = {2000},
	pages = {275{\textendash}284},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0029-8549},
	doi = {10.1007/s004420051014},
	url = {http://dx.doi.org/10.1007/s004420051014},
	author = {Mullineaux, L S and Fisher, C R and Peterson, C H and Schaeffer, S W}
}
@article {Hirano1999,
	title = {{Temporal changes of cracks in the oceanward slope of northern Japan Trench off Sanriku: Six-year observation by submersibles}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {14},
	year = {1999},
	pages = {445{\textendash}454},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/14{\_}36.pdf},
	author = {Hirano, S and Ogawa, Y and Yujiro, F and Fujioka, K and Kawamura, K}
}
@article {Mitsuzawa1999,
	title = {{Ten-days observation period on a low-temperature hydrothermal field at the Southern East Pacific Rise}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {14},
	year = {1999},
	pages = {79{\textendash}90},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/14{\_}08.pdf},
	author = {Mitsuzawa, K and Sugawara, T and Nakamura, K and Urabe, T and Fujioka, K}
}
@article {Davis1999,
	title = {{Tidal pumping of fluids within and from the oceanic crust: new observations and opportunities for sampling the crustal hydrosphere}},
	journal = {Earth and Planetary Science Letters},
	volume = {172},
	number = {1-2},
	year = {1999},
	pages = {141{\textendash}149},
	issn = {0012-821X},
	doi = {10.1016/S0012-821X(99)00197-1},
	url = {http://dx.doi.org/10.1016/S0012-821X(99)00197-1},
	author = {Davis, E E and Becker, K}
}
@article {Tebbens1998,
	title = {{Teaching marine science to the next generation: Innovative programs for 6th-8th graders gain momentum}},
	journal = {EOS, Transactions, American Geophysical Union},
	volume = {79},
	number = {1},
	year = {1998},
	pages = {137,141},
	issn = {0096-3941},
	doi = {10.1029/98EO00096},
	url = {http://dx.doi.org/10.1029/98EO00096},
	author = {Tebbens, S F and Coble, P G and Greely, T}
}
@article {Sayers1998,
	title = {{Teleprogramming for subsea teleoperation using acoustic communication}},
	journal = {IEEE Journal of Oceanic Engineering},
	volume = {23},
	number = {1},
	year = {1998},
	pages = {60{\textendash}71},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0364-9059},
	doi = {10.1109/48.659450},
	url = {http://dx.doi.org/10.1109/48.659450},
	author = {Sayers, C P and Paul, R P and Whitcomb, L L and Yoerger, D R}
}
@article {Fisher1998,
	title = {{Temperature and sulphide tolerance of hydrothermal vent fauna}},
	journal = {Cahiers de Biologie Marine},
	volume = {39},
	number = {3-4},
	year = {1998},
	pages = {283{\textendash}286},
	issn = {0007-9723},
	author = {Fisher, C R}
}
@article {Shank1998,
	title = {{Temporal and spatial patterns of biological community development at nascent deep-sea hydrothermal vents (9 degrees 50{\textquoteright}N, East Pacific Rise)}},
	journal = {Deep-Sea Research. Part II: Topical Studies in Oceanography},
	volume = {45},
	number = {1-3},
	year = {1998},
	pages = {465{\textendash}515},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0645},
	doi = {10.1016/S0967-0645(97)00089-1},
	url = {http://dx.doi.org/10.1016/S0967-0645(97)00089-1},
	author = {Shank, T M and Fornari, D J and Von Damm, K L and Lilley, M D and Haymon, R M and Lutz, R A}
}
@article {Beaulieu1998,
	title = {{Temporal variability in currents and the benthic boundary layer at an abyssal station off central California}},
	journal = {Deep-Sea Research. Part II: Topical Studies in Oceanography},
	volume = {45},
	number = {4-5},
	year = {1998},
	pages = {587{\textendash}615},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0645},
	doi = {10.1016/S0967-0645(97)00095-7},
	url = {http://dx.doi.org/10.1016/S0967-0645(97)00095-7},
	author = {Beaulieu, S E and Baldwin, R}
}
@article {Holden1998,
	title = {{Thermophilic and hyperthermophilic microorganisms in 3{\textendash}30{\textdegree}C hydrothermal fluids following a deep-sea volcanic eruption}},
	journal = {FEMS Microbiology Ecology},
	volume = {25},
	number = {1},
	year = {1998},
	pages = {33{\textendash}41},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0168-6496},
	doi = {10.1111/j.1574-6941.1998.tb00458.x},
	url = {http://dx.doi.org/10.1111/j.1574-6941.1998.tb00458.x},
	author = {Holden, J F and Summit, M and Baross, J A}
}
@article {Tivey1998a,
	title = {{Thickness of a submarine lava flow determined from near-bottom magnetic field mapping by autonomous underwater vehicle}},
	journal = {Geophysical Research Letters},
	volume = {25},
	number = {6},
	year = {1998},
	pages = {805{\textendash}808},
	keywords = {AUV ABE (Autonomous Benthic Explorer)},
	issn = {0094-8276},
	doi = {10.1029/98GL00442},
	url = {http://dx.doi.org/10.1029/98GL00442},
	author = {Tivey, M A and Johnson, P H and Bradley, A and Yoerger, D R}
}
@article {Fornari1998b,
	title = {{Time-series temperature measurements at high-temperature hydrothermal vents, East Pacific Rise 9 degrees 49{\textquoteright}-51{\textquoteright}N; evidence for monitoring a crustal cracking event}},
	journal = {Earth and Planetary Science Letters},
	volume = {160},
	number = {3-4},
	year = {1998},
	pages = {419{\textendash}431},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/S0012-821X(98)00101-0},
	url = {http://dx.doi.org/10.1016/S0012-821X(98)00101-0},
	author = {Fornari, D J and Shank, T M and Von Damm, K L and Gregg, T K P and Lilley, M and Levai, G and Bray, A and Haymon, R M and Perfit, M R and Lutz, R}
}
@inbook {Karson1997a,
	title = {{Tectonic setting of serpentinite exposures on the western median valley wall of the MARK area in the vicinity of Site 920}},
	booktitle = {Proceedings of the Ocean Drilling Program, Scientific Results},
	volume = {153},
	year = {1997},
	pages = {5{\textendash}21},
	publisher = {Ocean Drilling Program, Texas A{\&}M University},
	organization = {Ocean Drilling Program, Texas A{\&}M University},
	address = {College Station, Tex.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.2973/odp.proc.sr.153.001.1997},
	url = {http://dx.doi.org/10.2973/odp.proc.sr.153.001.1997},
	author = {Karson, J A and Lawrence, R M},
	editor = {Stokking, L}
}
@inbook {Karson1997b,
	title = {{Tectonic synthesis of the MARK Area: Episodic crustal stretching and magmatism on the Mid-Atlantic Ridge}},
	booktitle = {Proceedings of the Ocean Drilling Program, Scientific Results},
	volume = {153},
	year = {1997},
	pages = {5{\textendash}21},
	publisher = {Ocean Drilling Program, Texas A{\&}M University},
	organization = {Ocean Drilling Program, Texas A{\&}M University},
	address = {College Station, Tex.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.2973/odp.proc.sr.153.001.1997},
	url = {http://dx.doi.org/10.2973/odp.proc.sr.153.001.1997},
	author = {Karson, J A and Cannat, M},
	editor = {Stocking, L}
}
@inbook {Karson1997,
	title = {{Tectonic window into Gabbroic rocks of the middle oceanic crust in the MARK area near sites 921-924}},
	booktitle = {Proceedings of the Ocean Drilling Program, Scientific Results},
	volume = {153},
	year = {1997},
	pages = {61{\textendash}76},
	publisher = {Ocean Drilling Program, Texas A{\&}M University},
	organization = {Ocean Drilling Program, Texas A{\&}M University},
	address = {College Station, Tex.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.2973/odp.proc.sr.153.005.1997},
	url = {http://dx.doi.org/10.2973/odp.proc.sr.153.005.1997},
	author = {Karson, J A and Lawrence, R M},
	editor = {Stokking, L}
}
@article {Stewart1996,
	title = {{Three-dimensional stochastic modeling using sonar sensing for undersea robotics}},
	journal = {Autonomous Robots},
	volume = {3},
	number = {2-3},
	year = {1996},
	pages = {121{\textendash}143},
	issn = {0929-5593},
	doi = {10.1007/BF00141151},
	url = {http://dx.doi.org/10.1007/BF00141151},
	author = {Stewart, W K}
}
@article {Cairns1996,
	title = {{A time domain electromagnetic survey of the TAG hydrothermal mound}},
	journal = {Geophysical Research Letters},
	volume = {23},
	number = {23},
	year = {1996},
	pages = {3455{\textendash}3458},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0094-8276},
	doi = {10.1029/96GL03233},
	url = {http://dx.doi.org/10.1029/96GL03233},
	author = {Cairns, G W and Evans, R L and Edwards, R N}
}
@inbook {Fornari1995b,
	title = {{Tectonic and volcanic controls on hydrothermal processes at the Mid-Ocean Ridge: An overview based on near-bottom and submersible studies}},
	booktitle = {Seafloor Hydrothermal Systems: Physical, Chemical, Biological, and Geochemical Interactions},
	series = {Geophysical Monograph},
	number = {91},
	year = {1995},
	pages = {1{\textendash}46},
	publisher = {American Geophysical Union},
	organization = {American Geophysical Union},
	address = {Washington, D.C.},
	isbn = {0-87590-048-8},
	author = {Fornari, D J and Embley, R W},
	editor = {Humphris, S E}
}
@inbook {Tang1995,
	title = {{Texture classification using wavelet packet and fourier transforms}},
	booktitle = {Oceans {\textquoteright}95 : "Challenges of our changing global environment" : conference proceedings, October 9-12, 1995, San Diego, California},
	volume = {1},
	year = {1995},
	pages = {387{\textendash}396},
	publisher = {Oceans {\textquoteright}95 MTS/IEEE Conference Committee},
	organization = {Oceans {\textquoteright}95 MTS/IEEE Conference Committee},
	address = {San Diego, Calif.},
	isbn = {0-9339571-4-9},
	doi = {10.1109/OCEANS.1995.526799},
	url = {http://dx.doi.org/10.1109/OCEANS.1995.526799},
	author = {Tang, X and Stewart, W K}
}
@inbook {Fisher1995,
	title = {{Toward an appreciation of hydrothermal-vent animals: their environment, physiological ecology, and tissue stable isotope values}},
	booktitle = {Seafloor Hydrothermal Systems: Physical, Chemical, Biological, and Geochemical Interactions},
	series = {Geophysical Monograph},
	number = {91},
	year = {1995},
	pages = {297{\textendash}316},
	publisher = {American Geophysical Union},
	organization = {American Geophysical Union},
	address = {Washington, D.C.},
	isbn = {0-87590-048-8},
	author = {Fisher, C R},
	editor = {Humphris, S E}
}
@article {Massoth1994,
	title = {{Temporal and spatial variability of hydrothermal manganese and iron at Cleft segment, Juan de Fuca Ridge}},
	journal = {Journal of Geophysical Research},
	volume = {99},
	number = {B3},
	year = {1994},
	pages = {4905{\textendash}4923},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/93JB02799},
	url = {http://dx.doi.org/10.1029/93JB02799},
	author = {Massoth, G J and Baker, E T and Lupton, J E and Feely, R A and Butterfield, D A and Von Damm, K L and Roe, K K and Lebon, G T}
}
@article {Fornari1994,
	title = {{Temporal variation in the morphology and structure of the axial summit caldera and young volcanic flows, and relationship to hydrothermal venting on the East Pacific Rise crest 9 30-51{\textquoteright}N}},
	journal = {EOS, Transactions, American Geophysical Union},
	volume = {75},
	number = {Fall meet. suppl.},
	year = {1994},
	pages = {618},
	issn = {0096-3941},
	author = {Fornari, D J and Perfit, M R and Smith, M and Haymon, R M and Edwards, M H and Cochran, J R and Coakely, B and Von Damm, K L and Lilley, M}
}
@article {Blondel1993b,
	title = {{Textural analysis and geological mapping of high-resolution sonar images: Applications to Endeavour Segment, Juan de Fuca Ridge}},
	journal = {EOS, Transactions, American Geophysical Union},
	volume = {74},
	number = {43 (Fall Meet. Suppl.)},
	year = {1993},
	pages = {573},
	issn = {0096-3941},
	author = {Blondel, P and Semp{\'e}r{\'e}, J C and Robigou, V and Delaney, J R}
}
@inbook {Blondel1993a,
	title = {{Textural analysis and structure-tracking for geological mapping: Applications to sonar data from the Endeavour Segment, Juan de Fuca Ridge}},
	booktitle = {Oceans {\textquoteright}93: Engineering in harmony with the ocean: Proceedings},
	volume = {3},
	year = {1993},
	pages = {III208{\textendash}III213},
	publisher = {IEEE},
	organization = {IEEE},
	address = {New York, N.Y.},
	isbn = {0-7803-1385-2},
	doi = {10.1109/OCEANS.1993.326187},
	url = {http://dx.doi.org/10.1109/OCEANS.1993.326187},
	author = {Blondel, P and Semp{\'e}r{\'e}, J C and Robigou, V}
}
@article {Karson1992a,
	title = {{Tectonic rotations of dikes in fast-spread oceanic crust exposed near Hess Deep}},
	journal = {Geology},
	volume = {20},
	number = {8},
	year = {1992},
	pages = {685{\textendash}688},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0091-7613},
	doi = {10.1130/0091-7613(1992)020<0685:TRODIF>2.3.CO;2},
	url = {http://dx.doi.org/10.1130/0091-7613(1992)020{\%}3C0685:TRODIF{\%}3E2.3.CO 2},
	author = {Karson, J A and Hurst, S D and Lonsdale, P}
}
@article {Heppenheimer1992,
	title = {{To the bottom of the sea}},
	journal = {American Heritage of Invention {\&} Technology},
	volume = {8},
	number = {1},
	year = {1992},
	pages = {28{\textendash}38},
	issn = {8756-7296},
	url = {http://www.americanheritage.com/articles/magazine/it/1992/1/1992{\_}1{\_}28.shtml},
	author = {Heppenheimer, T A}
}
@article {Karson1991a,
	title = {{Tectonics of slow-spreading mid-ocean ridges}},
	journal = {Oceanus},
	volume = {34},
	number = {4},
	year = {1991},
	pages = {51{\textendash}59},
	issn = {0029-8182},
	author = {Karson, J A}
}
@inbook {Bowen1991,
	title = {{A telerobotics workstation for remote control shipboard or satellite-linked operations}},
	booktitle = {Intervention/ROV {\textquoteright}91 Conference {\&} Exposition: May 21-23, 1991, Diplomat Resort and Convention Center, Hollywood, Florida},
	year = {1991},
	pages = {85{\textendash}89},
	publisher = {Marine Technology Society ROV Committee},
	organization = {Marine Technology Society ROV Committee},
	address = {San Diego, Calif.},
	author = {Bowen, M F and Somers, T}
}
@article {Phipps1991,
	title = {{Transform zone migration: implications of bookshelf faulting for oceanic and Icelandic propagating rifts}},
	journal = {Tectonics},
	volume = {10},
	number = {5},
	year = {1991},
	pages = {920{\textendash}935},
	issn = {0278-7407},
	author = {Phipps, M J and Kleinrock, M C}
}
@inbook {Mindell1991,
	title = {{Transputer-based distributed processing for underwater robotic vehicle control}},
	booktitle = {1991 American Control Conference Proceedings. Boston, June 26-28, 1991},
	volume = {1},
	year = {1991},
	pages = {389{\textendash}397},
	publisher = {IEEE},
	organization = {IEEE},
	address = {New York},
	isbn = {0-8794-2565-2},
	author = {Mindell, D A and Yoerger, D R}
}
@inbook {Karson1990a,
	title = {{Tectonic disruption of volcanic units of the oceanic crust}},
	booktitle = {Proceedings of a Workshop on the Physical Properties of Volcanic Seafloor: April 24-26, 1990},
	year = {1990},
	pages = {138{\textendash}142},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	author = {Karson, J A},
	editor = {Purdy, G M}
}
@article {Neuner1990,
	title = {{Thermococcus litoralis sp. nov.: a novel species of extremely thermophilic marine archaebacteria}},
	journal = {Archives of Microbiology},
	volume = {153},
	number = {2},
	year = {1990},
	pages = {205{\textendash}207},
	issn = {0302-8933},
	doi = {10.1007/BF00247822},
	url = {http://dx.doi.org/10.1007/BF00247822},
	author = {Neuner, A and Jannasch, H W and Belkin, S and Stetter, K O}
}
@article {Jorgensen1990,
	title = {{Thermophilic bacterial sulfate reduction in deep-sea sediments at the Guaymas Basin hydrothermal vent site (Gulf of California)}},
	journal = {Deep-Sea Research. Part A, Oceanographic Research Papers},
	volume = {37},
	number = {4},
	year = {1990},
	pages = {695{\textendash}710},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0198-0149},
	doi = {10.1016/0198-0149(90)90099-H},
	url = {http://dx.doi.org/10.1016/0198-0149(90)90099-H},
	author = {Jorgensen, B B and Zawacki, L X and Jannasch, H W}
}
@article {Okutani1990,
	title = {{Two new species of Provanna (Gastropoda: Cerithiacea) from snail pit in the hydrothermal vent site at the Mariana Back-Arc Basin}},
	journal = {Venus the Japanese Journal of Malacology},
	volume = {49},
	number = {1},
	year = {1990},
	pages = {19{\textendash}24},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0042-3580},
	author = {Okutani, T}
}
@article {Kleinrock1989a,
	title = {{Tectonics of the failing spreading system associated with the 95.5 degrees W Galapagos propagator}},
	journal = {Journal of Geophysical Research},
	volume = {94},
	number = {B10},
	year = {1989},
	pages = {13,813{\textendash}839,857},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/JB094iB10p13839},
	url = {http://dx.doi.org/10.1029/JB094iB10p13839},
	author = {Kleinrock, M C and Searle, R C and Hey, R N}
}
@inbook {Stewart1989,
	title = {{Three-dimensional modeling of seaflorr backscatter from sidescan sonar for autonomous classfication and navigation}},
	booktitle = {Proceedings of the 6th International Symposium on Unmanned Untethered Submersible Technology, June 12-14, 1989},
	year = {1989},
	pages = {21 pages},
	publisher = {Marine Systems Engineering Laboratory, University of New Hampshire},
	organization = {Marine Systems Engineering Laboratory, University of New Hampshire},
	address = {Durham, N.H.},
	author = {Stewart, W K}
}
@article {Roth1989,
	title = {{Transport and settling of organic material in a deep-sea hydrothermal plume: evidence from particle flux measurements}},
	journal = {Deep-Sea Research. Part A, Oceanographic Research Papers},
	volume = {36},
	number = {8},
	year = {1989},
	pages = {1237{\textendash}1254},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0198-0149},
	doi = {10.1016/0198-0149(89)90103-9},
	url = {http://dx.doi.org/10.1016/0198-0149(89)90103-9},
	author = {Roth, S and Dymond, J}
}
@article {Somero1989,
	title = {{Transport, metabolism and detoxification of hydrogen sulfide in animals from sulfide rich marine environments}},
	journal = {Reviews in Aquatic Sciences},
	volume = {1},
	number = {4},
	year = {1989},
	pages = {591{\textendash}614},
	issn = {0891-4117},
	author = {Somero, G N and Childress, J J and Anderson, A E}
}
@article {Pettibone1989,
	title = {{Two new species of Harmothoinae (Polychaeta: Polynoidae) from the East Pacific Rise, collected by Alvin dives 2000 and 2003}},
	journal = {Proceedings of the Biological Society of Washington},
	volume = {102},
	number = {2},
	year = {1989},
	pages = {305{\textendash}310},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0006-324X},
	author = {Pettibone, M H}
}
@article {Choukroune1988,
	title = {{Tectonics of an incipient oceanic rift}},
	journal = {Marine Geophysical Researches},
	volume = {9},
	number = {2},
	year = {1988},
	pages = {147{\textendash}163},
	issn = {0025-3235},
	doi = {10.1007/BF00369246},
	url = {http://dx.doi.org/10.1007/BF00369246},
	author = {Choukroune, P and Francheteau, J and Auvray, B and Auzende, J M and Brun, J P and Sichler, B and Arthaud, F and Lepine, J C}
}
@article {Hessler1988a,
	title = {{Temporal change in megafauna at the Rose Garden hydrothermal vent (Galapagos Rift; eastern tropical Pacific)}},
	journal = {Deep-Sea Research. Part A, Oceanographic Research Papers},
	volume = {35},
	number = {10-11},
	year = {1988},
	pages = {1681{\textendash}1710},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0198-0149},
	doi = {10.1016/0198-0149(88)90044-1},
	url = {http://dx.doi.org/10.1016/0198-0149(88)90044-1},
	author = {Hessler, R R and Smithey, W M and Boudrias, M A and Keller, C H and Lutz, R A and Childress, J J}
}
@article {Little1988,
	title = {{Tidal current effects on temperature measurements in diffuse hydrothermal flow: Guaymas Basin}},
	journal = {Geophysical Research Letters},
	volume = {15},
	number = {13},
	year = {1988},
	pages = {1491{\textendash}1494},
	issn = {0094-8276},
	doi = {10.1029/GL015i013p01491},
	url = {http://dx.doi.org/10.1029/GL015i013p01491},
	author = {Little, S A and Stolzenbach, K D and Grassle, J F}
}
@article {Fisher1986,
	title = {{Translocation of fixed carbon from symbiotic bacteria to host tissues in the gutless bivalve Solemya reidi}},
	journal = {Marine Biology},
	volume = {93},
	number = {1},
	year = {1986},
	pages = {59{\textendash}68},
	issn = {0025-3162},
	doi = {10.1007/BF00428655},
	url = {http://dx.doi.org/10.1007/BF00428655},
	author = {Fisher, C R and Childress, J J}
}
@article {Gowing1986,
	title = {{Trophic relationships of deep-sea calanoid copepods from the benthic boundary layer of the Santa Catalina Basin, California}},
	journal = {Deep-Sea Research. Part A, Oceanographic Research Papers},
	volume = {33},
	number = {7},
	year = {1986},
	pages = {939{\textendash}961},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0198-0149},
	doi = {10.1016/0198-0149(86)90008-7},
	url = {http://dx.doi.org/10.1016/0198-0149(86)90008-7},
	author = {Gowing, M M and Wishner, K F}
}
@article {Goud1985,
	title = {{Tectonics of short-offset, slow-slipping transform zones in the FAMOUS area, Mid-Atlantic Ridge}},
	journal = {Marine Geophysical Researches},
	volume = {7},
	number = {4},
	year = {1985},
	pages = {489{\textendash}514},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3235},
	doi = {10.1007/BF00368952},
	url = {http://dx.doi.org/10.1007/BF00368952},
	author = {Goud, M R and Karson, J A}
}
@article {Jannasch1985,
	title = {{Thiomicrospira crunogena sp. nov., a colorless sulfur-oxidizing bacterium from a deep-sea hydrothermal vent}},
	journal = {International Journal of Systematic Bacteriology},
	volume = {35},
	number = {4},
	year = {1985},
	pages = {422{\textendash}424},
	issn = {0020-7713},
	author = {Jannasch, H W and Wirsen, C O and Nelson, D C and Robertson, L A}
}
@article {Johnson1985,
	title = {{Time-series measurements of hydrothermal activity on northern Juan De Fuca Ridge}},
	journal = {Geophysical Research Letters},
	volume = {12},
	number = {10},
	year = {1985},
	pages = {685{\textendash}688},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0094-8276},
	doi = {10.1029/GL012i010p00685},
	url = {http://dx.doi.org/10.1029/GL012i010p00685},
	author = {Johnson, H and Tunnicliffe, V}
}
@article {Team1984a,
	title = {{Tectonics at the intersection of the East Pacific Rise with Tamayo Transform fault}},
	journal = {Marine Geophysical Researches},
	volume = {6},
	number = {2},
	year = {1984},
	pages = {159{\textendash}185},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3235},
	doi = {10.1007/BF00285958},
	url = {http://dx.doi.org/10.1007/BF00285958},
	author = {Team, Tamayo Tectonic and Gallo, D G and Kidd, W S F and Fox, P J and Karson, J A and Macdonald, K and Crane, K T and Choukroune, P and Seguret, M and Moody, R and Kastens, K}
}
@article {Karl1984,
	title = {{Themophilic microbial activity in samples from deep sea hydrothermal vents}},
	journal = {Marine Biology Letters},
	volume = {5},
	number = {4},
	year = {1984},
	pages = {227{\textendash}231},
	issn = {0165-859X},
	author = {Karl, D M and Burns, D and Orrett, K and Jannasch, H W}
}
@article {Karson1983,
	title = {{Tectonics of ridge-transform intersections at the Kane fracture zone}},
	journal = {Marine Geophysical Researches},
	volume = {6},
	number = {1},
	year = {1983},
	pages = {51{\textendash}98},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3235},
	doi = {10.1007/BF00300398},
	url = {http://dx.doi.org/10.1007/BF00300398},
	author = {Karson, J A and Dick, H J B}
}
@inbook {Corliss1983,
	title = {{The thermal springs of the Galapagos Rift: Their implications for biology and the chemistry of sea water}},
	booktitle = {Patterns of evolution in Galapagos organisms},
	year = {1983},
	pages = {25{\textendash}31},
	publisher = {Pacific Division, American Association for the Advancement of Science},
	organization = {Pacific Division, American Association for the Advancement of Science},
	address = {San Francisco, Calif.},
	isbn = {0934394059},
	author = {Corliss, J B},
	editor = {Bowman, R}
}
@article {Zottoli1982,
	title = {{Two new genera of deep-sea polychaete worms of the family Ampharetidae and the role of one species in deep-sea ecosystems}},
	journal = {Proceedings of the Biological Society of Washington},
	volume = {95},
	number = {1},
	year = {1982},
	pages = {48{\textendash}57},
	issn = {0006-324X},
	author = {Zottoli, R}
}
@article {Filatova1980,
	title = {{On the thermophilic deep-sea bottom faunal communities of the Pacific Ocean rift zones}},
	journal = {Oceanology},
	volume = {20},
	number = {3},
	year = {1980},
	pages = {520{\textendash}524},
	issn = {0001-4370},
	author = {Filatova, Z A}
}
@article {Filatova1980a,
	title = {{Thermophylic communities of deep-sea bottom fauna in rift zones of the Pacific Ocean}},
	journal = {Oceanology},
	volume = {20},
	number = {3},
	year = {1980},
	pages = {339{\textendash}341},
	issn = {0001-4370},
	author = {Filatova, Z A}
}
@inbook {Grassle1977,
	title = {{Temporal adaptations in sibling species of Capitella}},
	booktitle = {Ecology of Marine Benthos},
	series = {Belle W. Baruch Library in Marine Science},
	number = {6},
	year = {1977},
	pages = {177{\textendash}189},
	publisher = {University of South Carolina Press},
	organization = {University of South Carolina Press},
	address = {Columbia, S.C.},
	isbn = {0872493555},
	author = {Grassle, J F},
	editor = {Coull, B C}
}
@book {Hays1976,
	title = {{Technical report, ARPA Program final report: 1 February 1971-31 December 1975}},
	series = {WHOI technical reports},
	volume = {76-9},
	year = {1976},
	pages = {29},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Hays, E E}
}
@article {Ballard1975,
	title = {{Triassic rift structure in the Gulf of Maine}},
	journal = {AAPG Bulletin},
	volume = {59},
	number = {7},
	year = {1975},
	pages = {1041{\textendash}1072},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0149-1423},
	author = {Ballard, R D and Uchupi, E}
}
@book {Ballard1974a,
	title = {{Technical progress report: Advanced marine technology 1 August 1973 - 31 January 1974}},
	series = {WHOI technical reports},
	volume = {74-27},
	year = {1974},
	pages = {44},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Ballard, R D and Hays, E E and Hess, F R and Marquet, W M and McCamis, M J and McElroy, P T and Winget, C L}
}
@book {Hosom1974,
	title = {{Technical progress report: Advanced marine technology 1 February 1974 - 31 July 1974}},
	series = {WHOI technical reports},
	volume = {74-100},
	year = {1974},
	pages = {22},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Hosom, D S and Hays, E E and Hess, F R and McElroy, P T and Marquet, W M and Porter, R P and Spindel, R C and Winget, C L and Striffler, F L}
}
@book {Rowe1974,
	title = {{Time-lapse photography of the biological reworking of sediments in Hudson Submarine Canyon}},
	series = {WHOI technical reports},
	volume = {74-79},
	year = {1974},
	pages = {552},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Rowe, G T and Keller, G and Edgerton, H E and Staresinic, N and MacIlvaine, J C}
}
@book {Aldrich1973a,
	title = {{Technical progress report: Advanced marine technology 1 August 1972 - 31 January 1973}},
	series = {WHOI technical reports},
	volume = {73-37},
	year = {1973},
	pages = {51},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Aldrich, T C and Maxwell, A E and Bowin, C O and Luyendyk, B P and Phillips, J D and Hess, F R and Vine, A C and Ballard, R D and Marquet, W M and Porter, D and McCamis, M J and Winget, C L and Von Herzen, R P and Williams, D L}
}
@book {Ballard1973,
	title = {{Technical progress report: Advanced marine technology 1 February 1973 - 31 July 1973}},
	series = {WHOI technical reports},
	volume = {73-92},
	year = {1973},
	pages = {82},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Ballard, R D and Maxwell, A E and Davis, R E and Eliason, A H and Hess, F R and McCamis, M J and McElroy, P T and Marquet, W M and Von Herzen, R P and Williams, D L and Winget, C L}
}
@book {Aldrich1973,
	title = {{Technical progress report: Advanced marine technology 1 February 1972 - 31 July 1972}},
	series = {WHOI technical reports},
	volume = {73-20},
	year = {1973},
	pages = {var. p.},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Aldrich, T C and Maxwell, A E and Ballard, R D and Bowin, C O and Luyendyk, B P and McCamis, M J and Phillips, J D and Porter, D and Vine, A C and Teal, J M and Marquet, W M and Winget, C L and Von Herzen, R P and Williams, D L}
}
@book {Palermo1973,
	title = {{Titanium sphere for Alvin/Autec pressure design considerations}},
	year = {1973},
	pages = {22},
	publisher = {Naval Ship Engineering Center},
	organization = {Naval Ship Engineering Center},
	address = {Washington, D.C.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Palermo, P M and Kiernan, T J and Sharp, A G and Ferrara, W}
}
@book {Thomas1973,
	title = {{Training in the underwater terrain navigation and reconnaissance trainer simulator}},
	series = {Technical report},
	year = {1973},
	pages = {51},
	publisher = {Naval Training Equipment Center},
	organization = {Naval Training Equipment Center},
	address = {Orlando, Fla.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Thomas, R C}
}
@book {Aldrich1972,
	title = {{Technical progress report: Advanced marine technology 1 August 1971 - 31 January 1972}},
	series = {WHOI technical reports},
	volume = {72-90},
	year = {1972},
	pages = {66},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Aldrich, T C and Maxwell, A E and Bowin, C O and Luyendyk, B P and Phillips, J D and Hess, F R and Vine, A C and Teal, J and Marquet, W M and Uchupi, E and Wiebe, P H and Rowe, G T and Smith, K L and Von Herzen, R P and Williams, D L}
}
@book {Bryan1972,
	title = {{Technical progress report: Advanced marine technology 1 February 1971 - 31 July 1971}},
	series = {WHOI technical reports},
	volume = {72-33},
	year = {1972},
	pages = {48},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Bryan, W B and Maxwell, A E and Bowin, C O and Ballard, R D and Phillips, J D and Hess, F R and Vine, A C and Teal, J and Marquet, W M and Uchupi, E and Wiebe, P H and Zafiriou, O C and Rowe, G T and Smith, K L and Von Herzen, R P}
}
@book {Walden1971,
	title = {{Torpedo recovery device for DSV Turtle}},
	series = {WHOI technical memoranda},
	year = {1971},
	pages = {2},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Walden, B}
}
@book {Sharp1970,
	title = {{Torque tests of a full size model of the Alvin/Autec emergency sphere release}},
	series = {WHOI technical reports},
	volume = {70-60},
	year = {1970},
	pages = {var. p.},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Sharp, A G and Sullivan, J R}
}
@article {Emery1968,
	title = {{Topography and sediments of a small area of the continental slope south of Martha{\textquoteright}s Vineyard}},
	journal = {Deep-Sea Research and Oceanographic Abstracts},
	volume = {15},
	number = {4},
	year = {1968},
	pages = {415{\textendash}422},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0011-7471},
	doi = {10.1016/0011-7471(68)90049-1},
	url = {http://dx.doi.org/10.1016/0011-7471(68)90049-1},
	author = {Emery, K O and Ross, D A}
}
@book {Winget1967,
	title = {{A technical guide to the deep submergence research vehicle (DSRV) Alvin for use in planning scientific missions}},
	series = {WHOI technical reports},
	volume = {67-67},
	year = {1967},
	pages = {var. p.},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Winget, C L and McCamis, M J}
}
@book {Sharp1967,
	title = {{Tests of propellers for Alvin side propulsion units}},
	series = {WHOI technical memoranda},
	year = {1967},
	pages = {var. p.},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1575/1912/640},
	url = {http://hdl.handle.net/1912/640},
	author = {Sharp, A G and Sullivan, J R}
}
@article {Mavor1966,
	title = {{Ten months with Alvin}},
	journal = {Geomarine Technology},
	volume = {2},
	number = {2},
	year = {1966},
	pages = {8{\textendash}18},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0435-4265},
	author = {Mavor, J W}
}
@book {Smith1966,
	title = {{Terrain relief models and operational sketches as used in the Task Force Sixty-Five nuclear weapon recovery effort}},
	series = {Technical note},
	year = {1966},
	pages = {23},
	publisher = {Naval Civil Engineering Lab},
	organization = {Naval Civil Engineering Lab},
	address = {Hueneme, Calif.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Smith, R J}
}
@article {Scott1964,
	title = {{A thousand fathoms and beyond}},
	journal = {Sea Frontiers},
	volume = {10},
	number = {1},
	year = {1964},
	pages = {37{\textendash}45},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0897-2249},
	author = {Scott, M K}
}
@book {Learnard1964,
	title = {{Twenty-four (24) man-hour test of Alvin{\textquoteright}s environmental system}},
	series = {WHOI technical memoranda},
	year = {1964},
	pages = {9},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, MA},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Learnard, H H and Marquet, W M and McCamis, M J}
}
