@article {RN2447,
	title = {Laminatubus (Serpulidae, Annelida) from eastern Pacific hydrothermal vents and methane seeps, with description of two new species},
	journal = {Zootaxa},
	volume = {4915},
	number = {1},
	year = {2021},
	pages = {1-27},
	type = {Journal Article},
	doi = {10.11646/zootaxa.4915.1.1},
	url = {https://app.dimensions.ai/details/publication/pub.1134705261},
	author = {Rouse, Greg W. and Kupriyanova, Elena K.}
}
@article {RN2490,
	title = {Large-scale protein level comparison of Deltaproteobacteria reveals cohesive metabolic groups},
	journal = {Isme Journal},
	year = {2021},
	type = {Journal Article},
	issn = {1751-7362},
	doi = {10.1038/s41396-021-01057-y},
	author = {Langwig, M. V. and De Anda, V. and Dombrowski, N. and Seitz, K. W. and Rambo, I. M. and Greening, C. and Teske, A. P. and Baker, B. J.}
}
@article {RN2481,
	title = {LOC Manuscript for Global Biogeochemical Cycles Using radiocarbon to assess the abundance, distribution, and nature of labile organic carbon in marine sediments},
	journal = {Global Biogeochemical Cycles},
	year = {2021},
	type = {Journal Article},
	doi = {10.1029/2020gb006676},
	url = {https://app.dimensions.ai/details/publication/pub.1138401852},
	author = {DeMaster, D. J. and Taylor, R. S. and Smith, C. R. and Isla, E. and Thomas, C. J.}
}
@article {RN2362,
	title = {Lipid biomarker patterns reflect different formation environments of mussel- and tubeworm-dominated seep carbonates from the Gulf of Mexico (Atwater Valley and Green Canyon)},
	journal = {Chemical Geology},
	volume = {505},
	year = {2019},
	pages = {36-47},
	type = {Journal Article},
	issn = {0009-2541},
	doi = {10.1016/j.chemgeo.2018.12.005},
	author = {Guan, H. X. and Feng, D. and Birgel, D. and Peckmann, J. and Roberts, H. H. and Wu, N. Y. and Chen, D. F.}
}
@article {RN2340,
	title = {A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked},
	journal = {Geophysical Research Letters},
	volume = {45},
	number = {20},
	year = {2018},
	pages = {11095-11103},
	type = {Journal Article},
	issn = {0094-8276},
	doi = {10.1029/2018GL079519},
	author = {McGuire, J. J. and Collins, J. A. and Davis, E. and Becker, K. and Heesemann, M.}
}
@article {RN2348,
	title = {The largest deep-ocean silicic volcanic eruption of the past century},
	journal = {Science Advances},
	volume = {4},
	number = {1},
	year = {2018},
	pages = {e1701121},
	type = {Journal Article},
	doi = {10.1126/sciadv.1701121},
	url = {http://advances.sciencemag.org/content/4/1/e1701121.abstract},
	author = {Carey, Rebecca and Soule, S. Adam and Manga, Michael and White, James D. L. and McPhie, Jocelyn and Wysoczanski, Richard and Jutzeler, Martin and Tani, Kenichiro and Yoerger, Dana and Fornari, Daniel and Caratori-Tontini, Fabio and Houghton, Bruce and Mitchell, Samuel and Ikegami, Fumihiko and Conway, Chris and Murch, Arran and Fauria, Kristen and Jones, Meghan and Cahalan, Ryan and McKenzie, Warren}
}
@article {RN2352,
	title = {Long-Term Stability of Back-Arc Basin Hydrothermal Vents},
	journal = {Frontiers in Marine Science},
	volume = {5},
	year = {2018},
	pages = {54},
	type = {Journal Article},
	issn = {2296-7745},
	doi = {10.3389/fmars.2018.00054},
	url = {https://www.frontiersin.org/article/10.3389/fmars.2018.00054},
	author = {Du Preez, Cherisse and Fisher, Charles R.}
}
@article {Lin2016,
	title = {{Linkages between mineralogy, fluid chemistry, and microbial communities within hydrothermal chimneys from the Endeavour Segment, Juan de Fuca Ridge}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {17},
	year = {2016},
	pages = {300{\textendash}323},
	abstract = {Rock and fluid samples were collected from three hydrothermal chimneys at the Endeavour Segment, Juan de Fuca Ridge to evaluate linkages among mineralogy, fluid chemistry, and microbial community composition within the chimneys. M{\"o}ssbauer, midinfrared thermal emission, and visible-near infrared spectroscopies were utilized for the first time to characterize vent mineralogy, in addition to thin-section petrography, X-ray diffraction, and elemental analyses. A 282{\textdegree}C venting chimney from the Bastille edifice was composed primarily of sulfide minerals such as chalcopyrite, marcasite, and sphalerite. In contrast, samples from a 300{\textdegree}C venting chimney from the Dante edifice and a 321{\textdegree}C venting chimney from the Hot Harold edifice contained a high abundance of the sulfate mineral anhydrite. Geochemical modeling of mixed vent fluids suggested the oxic-anoxic transition zone was above 100{\textdegree}C at all three vents, and that the thermodynamic energy available for autotrophic microbial redox reactions favored aerobic sulfide and methane oxidation. As predicted, microbes within the Dante and Hot Harold chimneys were most closely related to mesophilic and thermophilic aerobes of the Betaproteobacteria and Gammaproteobacteria and sulfide-oxidizing autotrophic Epsilonproteobacteria. However, most of the microbes within the Bastille chimney were most closely related to mesophilic and thermophilic anaerobes of the Deltaproteobacteria, especially sulfate reducers, and anaerobic hyperthermophilic archaea. The predominance of anaerobes in the Bastille chimney indicated that other environmental factors promote anoxic conditions. Possibilities include the maturity or fluid flow characteristics of the chimney, abiotic Fe2+ and S2- oxidation in the vent fluids, or O2 depletion by aerobic respiration on the chimney outer wall.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1002/2015GC006091},
	author = {Lin, T J and Ver Eecke, H C and Breves, E A and Dyar, M D and Jamieson, J W and Hannington, M D and Dahle, H and Bishop, J L and Lane, M D and Butterfield, D A and Kelley, D S and Lilley, M D and Baross, J A and Holden, J F}
}
@article {ISI:000351847600028,
	title = {{Long-term explosive degassing and debris flow activity at West Mata submarine volcano}},
	journal = {GEOPHYSICAL RESEARCH LETTERS},
	volume = {42},
	number = {5},
	year = {2015},
	month = {mar},
	pages = {1480{\textendash}1487},
	type = {Article},
	abstract = {West Mata is a 1200m deep submarine volcano where explosive boninite eruptions were observed in 2009. The acoustic signatures from the volcano{\textquoteright}s summit eruptive vents Hades and Prometheus were recorded with an in situ (similar to 25m range) hydrophone during ROV dives in May 2009 and with local (similar to 5km range) moored hydrophones between December 2009 and August 2011. The sensors recorded low frequency (1-40Hz), short duration explosions consistent with magma bubble bursts from Hades, and broadband, 1-5min duration signals associated with episodes of fragmentation degassing from Prometheus. Long-term eruptive degassing signals, recorded through May 2010, preceded a several month period of declining activity. Degassing episodes were not recorded acoustically after early 2011, although quieter effusive eruption activity may have continued. Synchronous optical measurements of turbidity made between December 2009 and April 2010 indicate that turbidity maxima resulted from occasional south flank slope failures triggered by the collapse of accumulated debris during eruption intervals.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0094-8276},
	doi = {10.1002/2014GL062603},
	author = {Dziak, R P and Bohnenstiehl, D R and Baker, E T and Matsumoto, H and Caplan-Auerbach, J and Embley, R W and Merle, S G and Walker, S L and Lau, T-K. and Chadwick Jr., W W}
}
@article {Seyfried2015,
	title = {{The Lost City hydrothermal system: Constraints imposed by vent fluid chemistry and reaction path models on subseafloor heat and mass transfer processes}},
	journal = {Geochimica et Cosmochimica Acta},
	volume = {163},
	year = {2015},
	pages = {59{\textendash}79},
	abstract = {Since the first reported discovery of the Lost City hydrothermal system in 2001, it was recognized that seawater alteration of ultramafic rocks plays a key role in the composition of the coexisting vent fluids. The unusually high pH and high concentrations of H2 and CH4 provide compelling evidence for this. Here we report the chemistry of hydrothermal fluids sampled from two vent structures (Beehive: \~{}90{\textendash}116 {\textdegree}C, and M6: \~{}75 {\textdegree}C) at Lost City in 2008 during cruise KNOX18RR using ROV Jason 2 and R/V Revelle assets. The vent fluid chemistry at both sites reveals considerable overlap in concentrations of dissolved gases (H2, CH4), trace elements (Cs, Rb, Li, B and Sr), and major elements (SO4, Ca, K, Na, Cl), including a surprising decrease in dissolved Cl, suggesting a common source fluid is feeding both sites. The absence of Mg and relatively high concentrations of Ca and sulfate suggest solubility control by serpentine{\textendash}diopside{\textendash}anhydrite, while trace alkali concentrations, especially Rb and Cs, are high, assuming a depleted mantle protolith. In both cases, but especially for Beehive vent fluid, the silica concentrations are well in excess of those expected for peridotite alteration and the coexistence of serpentine{\textendash}brucite at all reasonable temperatures. However, both the measured pH and silica values are in better agreement with serpentine{\textendash}diopside{\textendash}tremolite-equilibria. Geochemical modeling demonstrates that reaction of plagioclase with serpentinized peridotite can shift the chemical system away from brucite and into the tremolite stability field. This is consistent with the complex intermingling of peridotite and gabbroic bodies commonly observed within the Atlantis Massif. We speculate the existence of such plagioclase bearing peridotite may also account for the highly enriched trace alkali (Cs, Rb) concentrations in the Lost City vent fluids. Additionally, reactive transport modeling taking explicit account of temperature dependent rates of mineral dissolution and precipitation clarifies the feedback between permeability, heat loss, and changes in the dissolved Si of the vent fluids. Assuming both the Beehive and M6 vent fluids were sourced at similar subseafloor conditions (tremolite buffered at 200 {\textdegree}C), model results indicate loss of approximately 30{\%} Si upon cooling to \~{}150 {\textdegree}C during upflow. However, Si concentrations remained largely conservative with continued cooling to lower temperatures owing to unfavorable reaction kinetics. While consistent with the Beehive endmember composition, these results fail to explain the relative Si depletion in the lower temperature M6 fluids. Thus, it may be that more robust kinetic models for silicates are needed to accurately account for the mechanism and rate of silica removal in the unusually high pH of the Lost City vent fluids.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	doi = {10.1016/j.gca.2015.04.040},
	author = {Seyfried, W E and Pester, N J and Tutolo, B M and Ding, K}
}
@article {ISI:000345820100015,
	title = {{A large volume particulate and water multi-sampler with in situ preservation for microbial and biogeochemical studies}},
	journal = {DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS},
	volume = {94},
	year = {2014},
	month = {dec},
	pages = {195{\textendash}206},
	type = {Article},
	abstract = {A new tool was developed for large volume sampling to facilitate marine microbiology and biogeochemical studies. It was developed for remotely operated vehicle and hydrocast deployments, and allows for rapid collection of multiple sample types from the water column and dynamic, variable environments such as rising hydrothermal plumes. It was used successfully during a cruise to the hydrothermal vent systems of the Mid-Cayman Rise. The Suspended Particulate Rosette V2 large volume multi-sampling system allows for the collection of 14 sample sets per deployment. Each sample set can include filtered material, whole (unfiltered) water, and filtrate. Suspended particulate can be collected on filters up to 142 mm in diameter and pore sizes down to 0.2 mu m. Filtration is typically at flowrates of 2 L min(-1) For particulate material, filtered volume is constrained only by sampling time and filter capacity, with all sample volumes recorded by digital flowmeter. The suspended particulate filter holders can be filled with preservative and sealed immediately after sample collection. Up to 2 L of whole water, filtrate, or a combination of the two, can be collected as part of each sample set. The system is constructed of plastics with titanium fasteners and nickel alloy spring loaded seals. There are no ferrous alloys in the sampling system. Individual sample lines are prefilled with filtered, deionized water prior to deployment and remain sealed unless a sample is actively being collected. This system is intended to facilitate studies concerning the relationship between marine microbiology and ocean biogeochemistry. (C) 2014 Elsevier Ltd. All rights reserved.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2014.08.008},
	author = {Breier, J A and Sheik, C S and Gomez-Ibanez, D and Sayre-McCord, R T and Sanger, R and Rauch, C and Coleman, M and Bennett, S A and Cron, B R and Li, M and German, C R and Toner, B M and Dick, G J}
}
@article {Panieri2014,
	title = {{Late Holocene Foraminifera of Blake Ridge Diapir: Assemblage Variation and Stable-Isotope Record in gas-hydrate bearing sediments}},
	journal = {Marine Geology},
	volume = {353},
	year = {2014},
	pages = {99{\textendash}107},
	abstract = {The presence of gas hydrates on the Blake Ridge diapir, northeastern Atlantic Ocean, offers an opportunity to study the impact of methane seepage on the ecology and geochemistry of benthic foraminifera in the late Holocene. Three push cores, covering a time span of {\~{}}~1000~yrs, were retrieved from three distinct microhabitats at the top of the diapir at a water depth of {\~{}}~2150~m: (i) sediments away from seepage (control core), (ii) sediments overlain by clusters of methanotrophic and thiotrophic bivalves, and (iii) chemoautotrophic microbial mats. The foraminiferal assemblages at the two seep sites are marked by a reduction in benthic foraminiferal species diversity, coupled with a near-absence of agglutinated species. However, an opportunistic population rise in CH4- or H2S-tolerant calcareous species (e.g., Globocassidulina subglobosa and Cassidulina laevigata) that utilize the abundant trophic resources at the seeps has led to an increase in the overall assemblage density there. The $δ$18O and $δ$13C values of three species of benthic foraminifera - Gyroidinoides laevigatus, Globocassidulina subglobosa, and Uvigerina peregrina - and the planktonic species Globorotalia menardii were acquired from all three cores. The benthic species from methane seeps yield $δ$13C values of 0.1 to {\textendash}4.2 ({\textperthousand}VPDB), that are distinctly more 13C-depleted relative to the $δ$13C of 0.4 to {\textendash}1.0 ({\textperthousand}VPDB) at the control (off seep) site. The species from a mussel-bed site exhibit more negative $δ$13C values than those from microbial mats, possibly reflecting different food sources and higher rate of anaerobic oxidation of methane. The positive $δ$13C values in the paired planktonic species suggest that authigenic carbonate precipitation did not overprint the observed 13C depletions. Hence the probable cause of negative $δ$13C of benthic foraminifera is primary calcification from Dissolved Inorganic Carbon (DIC) containing mixed carbon fractions from (a) highly 13C-depleted, microbially-oxidized methane and (b) a seawater source.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3227},
	doi = {10.1016/j.margeo.2014.03.020},
	url = {http://www.sciencedirect.com/science/article/pii/S0025322714000826},
	author = {Panieri, G and Aharon, Paul and Sen Gupta, B K and Camerlenghi, A and Ferrer, F P and Cacho, I}
}
@article {ISI:000331005900001,
	title = {{Low temperature geomicrobiology follows host rock composition along a geochemical gradient in Lau Basin}},
	journal = {FRONTIERS IN MICROBIOLOGY},
	volume = {4},
	year = {2013},
	month = {mar},
	type = {Article},
	abstract = {The East Lau Spreading Center (ELSC) and Valu Fa Ridge (VFR) comprise a ridge segment in the southwest Pacific Ocean where rapid transitions in the underlying mantle chemistry manifest themselves as gradients in seafloor rock geochemistry. We studied the geology and microbial diversity of three silicate rock samples and three inactive sulfide chimney samples collected, from north to south, at the vent fields Kilo Moana, ABE, Tui Malila, and Mariner. This is the first study of microbial populations on basaltic andesite, which was sampled at Mariner vent field. Silicate rock geochemistry exhibits clear latitudinal trends that are mirrored by changes in bacterial community composition. alpha-proteobacteria, epsilon-proteobacteria, and Bacteroidetes are most common on a silicate collected from Kilo Moana and their proportions decrease linearly on silicates collected further south. Conversely, a silicate from Mariner vent field hosts high proportions of a unique lineage of Chloroflexi unrelated ({\textless}90{\%} sequence similarity) to previously recovered environmental clones or isolates, which decrease at ABE and are absent at Kilo Moana. The exteriors of inactive sulfide structures are dominated by lineages of sulfur oxidizing alpha-proteobacteria, gamma-proteobacteria, and epsilon-proteobacteria, while the interior of one chimney is dominated by putative sulfur-reducing delta-proteobacteria. A comparison of bacterial communities on inactive sulfides from this and previous studies reveals the presence of a clade of uncultured Bacteroidetes exclusive to sulfidic environments, and a high degree of heterogeneity in bacterial community composition from one sulfide structure to another. In light of the heterogeneous nature of bacterial communities observed here and in previous studies of both active and inactive hydrothermal sulfide structures, the presence of numerous niches may be detected on these structures in the future by finer scale sampling and analysis.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1664-302X},
	doi = {10.3389/fmicb.2013.00061},
	author = {Sylvan, Jason B and Sia, Tiffany Y and Haddad, Amanda G and Briscoe, Lindsey J and Toner, Brandy M and Girguis, Peter R and Edwards, Katrina J}
}
@article {ISI:000323828800015,
	title = {{A low-relief shield volcano origin for the South Kaua{\{}{\textquoteright}{\textquoteright}{\}}i Swell}},
	journal = {GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS},
	volume = {14},
	number = {7},
	year = {2013},
	month = {jul},
	pages = {2328{\textendash}2348},
	type = {Article},
	abstract = {The South Kauai Swell (SKS) is a 110 km x 80 km ovoid bathymetric feature that stands {\textgreater}2 km high and abuts the southern flank of the island of Kauai. The origin of the SKS was investigated using multibeam bathymetry and acoustic backscatter, gravity data, radiometric ages, and geochemistry of rock samples. Most of the SKS rock samples are tholeiitic in composition with ages of 3.9-5.4 Ma indicating they were derived from shield volcanism. The ages and compositions of the SKS rocks partially overlap with those of the nearby Niihau, Kauai and West Kaena volcano complexes. The SKS was originally described as a landslide; however, this interpretation is problematic given the ovoid shape of SKS, its relatively smooth, flat-to-convex surface, and the lack of an obvious source region that could accommodate what would be one of Earth{\textquoteright}s most voluminous (6 x 10(3) km(3)) landslides. The morphology, size, and the surrounding gravity anomaly are more consistent with the SKS being a low-relief shield volcano, which was partially covered with a small volume of landside debris from south Kauai and later with some secondary volcanic seamounts. A shield origin would imply that Hawaiian and possibly other hotspot shield volcanoes can take on a wider variety of forms than is commonly thought, ranging from tall island-building shields, to smaller edifices such as Kaena Ridge and Mahukona, to even lower-relief volcanoes represented by the SKS and possibly the South West Oahu Volcanic Field.},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1002/ggge.20159},
	author = {Ito, Garrett and Garcia, Michael O and Smith, John R and Taylor, Brian and Flinders, Ashton and Jicha, Brian and Yamasaki, Seiko and Weis, Dominique and Swinnard, Lisa and Blay, Chuck}
}
@article {Tivey2012,
	title = {{Links from Mantle to Microbe at the Lau Integrated Study Site:Insights from a Back-Arc Spreading Center}},
	journal = {Oceanography},
	volume = {25},
	number = {1},
	year = {2012},
	month = {mar},
	pages = {62{\textendash}77},
	abstract = {The Lau Integrated Study Site (ISS) has provided unique opportunities for study of ridge processes because of its back-arc setting in the southwestern Pacific. Its location allows study of a biogeographical province distinct from those of eastern Pacific and mid-Atlantic ridges, and crustal compositions along the ridge lie outside the range of mid-ocean ridge crustal compositions. The Lau ISS is located above a subduction zone, at an oblique angle. The underlying mantle receives water and other elements derived from the downgoing lithospheric slab, with an increase in slab influence from north to south. Water lowers the mantle melting temperature and leads to greater melt production where the water flux is greater, and to distinctive regional-scale gradients along the ridge. There are deeper faulted axial valleys with basaltic volcanism in the north and inflated axial highs with andesites in the south. Differences in igneous rock composition and release of magmatic volatiles affect compositions of vent fluids and deposits. Differences in vent fluid compositions and small-scale diffuse-flow regimes correlate with regional-scale patterns in microbial and megafaunal distributions. The interdisciplinary research effort at the Lau ISS has successfully identified linkages between subsurface processes and deep-sea biological communities, from mantle to microbe to megafauna.},
	keywords = {AUV ABE (Autonomous Benthic Explorer), ROV Jason (Remotely Operated Vehicle)},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2012.04},
	author = {Tivey, M K and Becker, E and Beinart, R and Fisher, C R and Girguis, P R and Langmuir, C H and Michael, P J and Reysenbach, A -L}
}
@article {ISI:000301095200020,
	title = {{Low-Temperature Hydrothermal Plumes in the Near-Bottom Boundary Layer at Endeavour Segment, Juan de Fuca Ridge}},
	journal = {OCEANOGRAPHY},
	volume = {25},
	number = {1, SI},
	year = {2012},
	month = {mar},
	pages = {192{\textendash}195},
	type = {Article},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	issn = {1042-8275},
	author = {Hautala, Susan and Johnson, H Paul and Pruis, Matthew and Garcia-Berdeal, Irene and Bjorklund, Tor}
}
@article {Cruse2010,
	title = {{Low-molecular weight hydrocarbons in vent fluids from the Main Endeavour Field, northern Juan de Fuca Ridge}},
	journal = {Geochimica et Cosmochimica Acta},
	volume = {74},
	number = {21},
	year = {2010},
	pages = {6126{\textendash}6140},
	abstract = {Despite its location on sediment-free basalt, vent fluids from the Main Endeavour Field (MEF) contain chemical species that indicate fluids have interacted with sediments during circulation. We report on the distribution and isotopic abundances of organic compounds (C1{\textendash}C3 alkanes and alkenes, benzene and toluene) in fluids collected from the Main Endeavour Field (MEF) in July, 2000, to understand the processes that regulate their abundances and characterize fluid sources. Aqueous organic compounds are derived from the thermal alteration of sedimentary organic matter and subsequently undergo further oxidation reactions during fluid flow. Fluid:sediment mass ratios calculated using $Σ$NH4 concentrations indicate that the sediments are distal to the MEF, resulting in a common reservoir of fluids for all of the vents. Following the generation from sediment alteration, aqueous organic compounds undergo secondary alteration reactions via a stepwise oxidation reaction mechanism. Alkane distributions and isotopic compositions indicate that organic compounds in MEF fluids have undergone a greater extent of alteration as compared to Middle Valley fluids, either due to differences in subsurface redox conditions or the residence time of fluids at subsurface conditions. The distributions of the aromatic compounds benzene and toluene are qualitatively consistent with the subsurface conditions indicated by equilibration of aqueous alkanes and alkanes. However, benzene and toluene do not achieve chemical equilibrium in the subsurface. Methane and CO2 also do not equilibrate chemically or isotopically at reaction zone temperatures, a likely result of an insufficient reaction time after addition of CO2 from magmatic sources during upflow. The organic geochemistry supports the assumption that the sediments with which MEF fluids interact has the same composition as sediments present in Middle Valley itself, and highlight differences in subsurface reaction zone conditions and fluid flow pathways at these two sites.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0016-7037},
	doi = {10.1016/j.gca.2010.07.013},
	url = {http://dx.doi.org/10.1016/j.gca.2010.07.013},
	author = {Cruse, A M and Seewald, J S}
}
@article {White2009,
	title = {{Laser Raman spectroscopy as a technique for identification of seafloor hydrothermal and cold seep minerals}},
	journal = {Chemical Geology},
	volume = {259},
	number = {3-4},
	year = {2009},
	pages = {240{\textendash}252},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0009-2541},
	doi = {10.1016/j.chemgeo.2008.11.008},
	url = {http://dx.doi.org/10.1016/j.chemgeo.2008.11.008},
	author = {White, S N}
}
@article {Solomon2009,
	title = {{Long-term hydrogeochemical records in the oceanic basement and forearc prism at the Costa Rica subduction zone}},
	journal = {Earth and Planetary Science Letters},
	volume = {282},
	number = {1-4},
	year = {2009},
	pages = {240{\textendash}251},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2009.03.022},
	url = {http://dx.doi.org/10.1016/j.epsl.2009.03.022},
	author = {Solomon, E A and Kastner, M and Wheat, C G and Jannasch, H W and Robertson, G and Davis, E E and Morris, J D}
}
@article {Thistle2008,
	title = {{Large, motile epifauna interact strongly with harpacticoid copepods and polychaetes at a bathyal site}},
	journal = {Deep-Sea Research. Part I: Oceanographic Research Papers},
	volume = {55},
	number = {3},
	year = {2008},
	pages = {324{\textendash}331},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2007.11.008},
	url = {http://dx.doi.org/10.1016/j.dsr.2007.11.008},
	author = {Thistle, D and Eckman, J E and Paterson, G L J}
}
@article {Drazen2008,
	title = {{Lipid, sterols and fatty acid composition of abyssal holothurians and ophiuroids from the North-East Pacific Ocean: Food web implications}},
	journal = {Comparative Biochemistry and Physiology B-Biochemistry {\&} Molecular Biology},
	year = {2008},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1096-4959},
	doi = {10.1016/j.cbpb.2008.05.013},
	url = {http://dx.doi.org/10.1016/j.cbpb.2008.05.013},
	author = {Drazen, J C and Phleger, C F and Guest, M A and Nichols, P D}
}
@article {141,
	title = {{Lockheed Martin designs new scientific research mini-sub}},
	journal = {Ocean News {\&} Technology},
	volume = {14},
	number = {1},
	year = {2008},
	pages = {20{\textendash}21},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1082-6106},
	url = {http://www.mydigitalpublication.com/publication/?i=2811{\&}p=21}
}
@article {Chan2007,
	title = {{Lithium contents and isotopic compositions of ferromanganese deposits from the global ocean}},
	journal = {Deep-Sea Research. Part II: Topical Studies in Oceanography},
	volume = {54},
	number = {11-13},
	year = {2007},
	pages = {1147{\textendash}1162},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0645},
	doi = {10.1016/j.dsr2.2007.04.003},
	url = {http://dx.doi.org/10.1016/j.dsr2.2007.04.003},
	author = {Chan, L H and Hein, J R}
}
@article {Kelley2007,
	title = {{The Lost City Hydrothermal Field revisited}},
	journal = {Oceanography},
	volume = {20},
	number = {4},
	year = {2007},
	pages = {90{\textendash}99},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle)},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2007.09},
	author = {Kelley, D S and Fruh-Green, G L and Karson, J A and Ludwig, K A}
}
@article {Embley2006,
	title = {{Long-term eruptive activity at a submarine arc volcano}},
	journal = {Nature},
	volume = {441},
	number = {7092},
	year = {2006},
	pages = {494{\textendash}497},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0028-0836},
	doi = {10.1038/nature04762},
	url = {http://dx.doi.org/10.1038/nature04762},
	author = {Embley, R W and Chadwick, W W and Baker, E T and Butterfield, D A and Resing, J A}
}
@article {Proskurowski2006,
	title = {{Low temperature volatile production at the Lost City Hydrothermal Field: evidence from a hydrogen stable isotope geothermometer}},
	journal = {Chemical Geology},
	volume = {229},
	number = {4},
	year = {2006},
	pages = {331{\textendash}343},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0009-2541},
	doi = {10.1016/j.chemgeo.2005.11.005},
	url = {http://dx.doi.org/10.1016/j.chemgeo.2005.11.005},
	author = {Proskurowski, G and Lilley, M D and Kelley, D S and Olson, E J}
}
@mastersthesis {Eustice2005,
	title = {{Large-area visually augmented navigation for autonomous underwater vehicles}},
	volume = {Ph.D.},
	year = {2005},
	pages = {187},
	school = {Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution},
	type = {phd},
	address = {Cambridge, Mass. and Woods Hole, Mass.},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1575/1912/1414},
	url = {http://hdl.handle.net/1912/1414},
	author = {Eustice, R M}
}
@article {Phleger2005a,
	title = {{Lipid biomarkers of deep-sea hydrothermal vent polychaetes - Alvinella pompejana, A-caudata, Paralvinella grasslei and Hesiolyra bergii}},
	journal = {Deep-Sea Research. Part I: Oceanographic Research Papers},
	volume = {52},
	number = {12},
	year = {2005},
	pages = {2333{\textendash}2352},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2005.08.001},
	url = {http://dx.doi.org/10.1016/j.dsr.2005.08.001},
	author = {Phleger, C F and Nelson, M M and Groce, A K and Cary, S C and Coyne, K J and Gibson, J A E and Nichols, P D}
}
@article {Phleger2005,
	title = {{Lipid composition of deep-sea hydrothermal vent tubeworm Riftia packyptila, crabs Munidopsis subsquatnosa and Bythograea thermydron, mussels Bathymodiolus sp and limpets Lepetodrilus spp}},
	journal = {Comparative Biochemistry and Physiology B-Biochemistry {\&} Molecular Biology},
	volume = {141},
	number = {2},
	year = {2005},
	pages = {196{\textendash}210},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1096-4959},
	doi = {10.1016/j.cbpc.2005.03.001},
	url = {http://dx.doi.org/10.1016/j.cbpc.2005.03.001},
	author = {Phleger, C F and Nelson, M M and Groce, A K and Cary, S C and Coyne, K J and Nichols, P D}
}
@article {Lein2005,
	title = {{Lipids in hydrothermal sulfide ores from the 9 degrees 50{\textquoteright} N field of the East Pacific Rise}},
	journal = {Doklady Earth Sciences},
	volume = {405},
	number = {8},
	year = {2005},
	pages = {1231{\textendash}1234},
	issn = {1028-334X},
	author = {Lein, A Y and Peresypkin, V I and Bogdanov, Y A and Ivanov, M V}
}
@article {Kelley2005,
	title = {{The Lost City Hydrothermal Field}},
	journal = {Oceanography},
	volume = {18},
	number = {3},
	year = {2005},
	pages = {32{\textendash}45},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle)},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2005.23},
	author = {Kelley, D S}
}
@article {Wirsen2004,
	title = {{Is life thriving deep beneath the seafloor? Recent discoveries hint at a potentially huge and diverse subsurface biosphere}},
	journal = {Oceanus},
	volume = {42},
	number = {2},
	year = {2004},
	pages = {72{\textendash}77},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0029-8182},
	author = {Wirsen, C O}
}
@article {Schrenk2004,
	title = {{Low archaeal diversity linked to subseafloor geochemical processes at the Lost City Hydrothermal Field, Mid-Atlantic Ridge}},
	journal = {Environmental Microbiology},
	volume = {6},
	number = {10},
	year = {2004},
	pages = {1086{\textendash}1095},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1462-2912},
	doi = {10.1111/j.1462-2920.2004.00650.x},
	url = {http://dx.doi.org/10.1111/j.1462-2920.2004.00650.x},
	author = {Schrenk, M O and Kelley, D S and Bolton, S A and Baross, J A}
}
@article {VanDover2003,
	title = {{Local, regional, and biogeographic variation in community structure within hydrothermal-vent mussel beds of the East Pacific Rise}},
	journal = {Marine Ecology Progress Series},
	volume = {253},
	year = {2003},
	pages = {55{\textendash}56},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0171-8630},
	doi = {10.3354/meps253055},
	url = {http://dx.doi.org/10.3354/meps253055},
	author = {Van Dover, C L}
}
@article {Marsh2001,
	title = {{Larval dispersal potential of the tubeworm Riftia pachyptila at deep-sea hydrothermal vents}},
	journal = {Nature},
	volume = {411},
	number = {6833},
	year = {2001},
	pages = {77{\textendash}80},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0028-0836},
	doi = {10.1038/35075063},
	url = {http://dx.doi.org/10.1038/35075063},
	author = {Marsh, A G and Mullineaux, L S and Young, C M and Manahan, D T}
}
@article {Lutz2001a,
	title = {{Life after death in the deep sea}},
	journal = {American Scientist},
	volume = {89},
	number = {5},
	year = {2001},
	pages = {422{\textendash}431},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0003-0996},
	doi = {10.1511/2001.34.744},
	url = {http://dx.doi.org/10.1511/2001.34.744},
	author = {Lutz, R A and Shank, T M and Evans, R}
}
@article {Beaulieu2001,
	title = {{Life on glass houses: sponge stalk communities in the deep sea}},
	journal = {Marine Biology},
	volume = {138},
	number = {4},
	year = {2001},
	pages = {803{\textendash}817},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3162},
	doi = {10.1007/s002270000500},
	url = {http://dx.doi.org/10.1007/s002270000500},
	author = {Beaulieu, S E}
}
@article {Allen2001,
	title = {{Lipid composition of the hydrothermal vent clam Calyptogena pacifica (Mollusca: Bivalvia) as a trophic indicator}},
	journal = {Journal of the Marine Biological Association of the United Kingdom},
	volume = {81},
	number = {5},
	year = {2001},
	pages = {817{\textendash}821},
	abstract = {Specimens of the chemoautotrophic symbiont-bearing hydrothermal vent clam Calyptogena pacifica were collected from hydrothermal vents at the Endeavour segment of the Juan de Fuca Ridge. Total lipid was extracted from gill, foot and mantle tissues, and lipid class and fatty acid composition determined by thin layer chromatography with flame ionization detection (TLC{\textendash}FID), gas chromatography (GC) and gas chromatography with mass spectrometry (GC{\textendash}MS). An abundance of n{\textendash}7 monounsaturated fatty acids (MUFA), especially in the gill, reflected the large contribution of chemoautotrophic symbiotic bacteria to the nutrition of this clam. The absence of n{\textendash}8 MUFA suggests that C. pacifica does not contain methanotrophic symbiotic bacteria. Low levels of highly unsaturated fatty acids (HUFA) such as 20:5 n{\textendash}3 and 22:6 n{\textendash}3 were detected in C. pacifica and their presence is attributed to a source other than chemoautotrophic symbiotic bacteria. Significant levels of non-methylene interrupted dienoic fatty acids and eicosatrienoic acid (20:3) were also detected in C. pacifica and it is suggested that these fatty acids are synthesized from n{\textendash}7 MUFA as alternatives to HUFA. In contrast to shallow water bivalves, elevated levels of triglyceride were detected in the gills compared to the mantle.},
	issn = {0125-3154},
	doi = {10.1017/S0025315401004647},
	url = {http://dx.doi.org/10.1017/S0025315401004647},
	author = {Allen, C E and Tyler, P A and Van Dover, C L}
}
@article {VonDamm2001,
	title = {{Lost City found}},
	journal = {Nature},
	volume = {412},
	number = {6843},
	year = {2001},
	pages = {127{\textendash}128},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0028-0836},
	doi = {10.1038/35084297},
	url = {http://dx.doi.org/10.1038/35084297},
	author = {Von Damm, K L}
}
@article {Hissman2000,
	title = {{Lanice arakani, a new species of the family Terebellidae (Polychaeta: Sedentaria) from seamounts of the West Mariana Ridge}},
	journal = {Journal of the Marine Biological Association of the United Kingdom},
	volume = {80},
	number = {2},
	year = {2000},
	pages = {249{\textendash}257},
	issn = {0025-3154},
	doi = {10.1017/S0025315499001824},
	url = {http://dx.doi.org/10.1017/S0025315499001824},
	author = {Hissman, K}
}
@article {Takeuchi2000,
	title = {{Large earthquakes and bottom disturbances in the Okushiri Ridge along the eastern margin of Japan Sea}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {16},
	year = {2000},
	pages = {29{\textendash}46},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/16{\_}02{\_}04.pdf},
	author = {Takeuchi, A and Okamura, Y and Kato, Y and Ikehara, K and Zhang, J and Satake, K and Nagao, T and Hirano, M and Watanabe, M}
}
@article {Sell2000,
	title = {{Life in the extreme environment at a hydrothermal vent: Haemoglobin in a deep-sea copepod}},
	journal = {Proceedings of the Royal Society B: Biological Sciences},
	volume = {267},
	number = {1459},
	year = {2000},
	pages = {2323{\textendash}2326},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0962-8452},
	doi = {10.1098/rspb.2000.1286},
	url = {http://dx.doi.org/10.1098/rspb.2000.1286},
	author = {Sell, A F}
}
@article {Paull2000,
	title = {{Lithoherms on the Florida-Hatteras Slope}},
	journal = {Marine Geology},
	volume = {166},
	number = {1-4},
	year = {2000},
	pages = {83{\textendash}101},
	issn = {0025-3227},
	doi = {10.1016/S0025-3227(00)00003-7},
	url = {http://dx.doi.org/10.1016/S0025-3227(00)00003-7},
	author = {Paull, C K and Neumann, A C and am Ende, B A and Ussler, W and Rodriguez, N M}
}
@article {Galgani2000,
	title = {{Litter on the sea floor along European coasts}},
	journal = {Marine Pollution Bulletin},
	volume = {40},
	number = {6},
	year = {2000},
	pages = {516{\textendash}527},
	issn = {0025-326X},
	doi = {10.1016/S0025-326X(99)00234-9},
	url = {http://dx.doi.org/10.1016/S0025-326X(99)00234-9},
	author = {Galgani, F and Leaute, J P and Moguedet, P and Souplet, A and Verin, Y and Carpentier, A and Goraguer, H and Latrouite, D and Andral, B and Cadiou, Y and Mahe, J C and Poulard, J C and Nerisson, P}
}
@article {Karson1999a,
	title = {{Large-scale Argo II digital images of upper crustal structures at Hess Deep}},
	journal = {RIDGE Events},
	volume = {10},
	number = {1},
	year = {1999},
	pages = {29{\textendash}32},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	url = {http://www.ridge2000.org/science/downloads/newsletters/R2KNews0699.pdf},
	author = {Karson, J A and Hurst, S D and Klein, E M and Party, Hess Deep {\textquoteright}99 Scientific}
}
@article {Normark1999,
	title = {{Late Pleistocene channel-levee development on Monterey submarine fan, central California}},
	journal = {Geo-Marine Letters},
	volume = {18},
	number = {3},
	year = {1999},
	pages = {179{\textendash}188},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0276-0460},
	doi = {10.1007/s003670050066},
	url = {http://dx.doi.org/10.1007/s003670050066},
	author = {Normark, W R}
}
@article {Mochizuki1999,
	title = {{Long-term ocean bottom earthquake observation in the East Pacific Rise}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {14},
	year = {1999},
	pages = {43{\textendash}51},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/14{\_}04.pdf},
	author = {Mochizuki, M and Kanazawa, T and Nishizawa, A and Kishimoto, K and Urabe, T}
}
@article {Fujimoto1999,
	title = {{Long-term ocean bottom pressure measurement and acoustic ranging across the spreading axis of the southern East Pacific Rise}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {14},
	year = {1999},
	pages = {35{\textendash}42},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/14{\_}03.pdf},
	author = {Fujimoto, H}
}
@article {Childress1995a,
	title = {{Life in sulfidic environments: historical perspective and current research trends}},
	journal = {American Zoologist},
	volume = {35},
	number = {2},
	year = {1995},
	pages = {83{\textendash}90},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0003-1569},
	doi = {10.1093/icb/35.2.83},
	url = {http://dx.doi.org/10.1093/icb/35.2.83},
	author = {Childress, J J}
}
@article {Kinoshita1995,
	title = {{Long-term heat flow measurement on the TAG hydrothermal mound in Mid-Atlantic Ridge}},
	journal = {JAMSTEC Journal of Deep Sea Research},
	number = {11},
	year = {1995},
	pages = {137{\textendash}147},
	issn = {1340-7848},
	url = {http://docsrv.godac.jp/MSV2{\_}DATA/23/11{\_}13.pdf},
	author = {Kinoshita, M and Matsubayashi, O and Fujioka, K}
}
@article {Chadwick1994,
	title = {{Lava flows from a mid-1980s submarine eruption on the Cleft Segment, Juan de Fuca Ridge}},
	journal = {Journal of Geophysical Research},
	volume = {99},
	number = {B3},
	year = {1994},
	pages = {4761{\textendash}4776},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/93JB02041},
	url = {http://dx.doi.org/10.1029/93JB02041},
	author = {Chadwick, W W and Emblew, R W}
}
@article {Robigou1993,
	title = {{Large massive sulphide deposits in a newly discovered active hydrothermal system, the High-Rise Field, Endeavour Segment, Juan de Fuca Ridge}},
	journal = {Geophysical Research Letters},
	volume = {20},
	number = {17},
	year = {1993},
	pages = {1887{\textendash}1890},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0094-8276},
	doi = {10.1029/93GL01399},
	url = {http://dx.doi.org/10.1029/93GL01399},
	author = {Robigou, V and Delaney, J R and Stakes, D}
}
@book {Ballard1993c,
	title = {{The Lost Ships of Guadalcanal}},
	year = {1993},
	pages = {227},
	publisher = {Warner Books},
	organization = {Warner Books},
	address = {New York},
	isbn = {0-446-51636-8},
	author = {Ballard, R D and Archbold, R}
}
@article {Tivey1992a,
	title = {{Leg 139 drilling tests magnetic models}},
	journal = {JOI/USSAC Newsletter},
	volume = {5},
	number = {2},
	year = {1992},
	author = {Tivey, M A}
}
@article {Peter1990,
	title = {{Liquid hydrocarbon-bearing inclusions in modern hydrothermal chimmeys and mounds from the southern trough of Guaymas Basin, Gulf of California}},
	journal = {Applied Geochemistry},
	volume = {5},
	number = {1-2},
	year = {1990},
	pages = {51{\textendash}63},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0883-2927},
	doi = {10.1016/0883-2927(90)90035-4},
	url = {http://dx.doi.org/10.1016/0883-2927(90)90035-4},
	author = {Peter, J M and Simoneit, B R T and Kawka, O E and Scott, S D}
}
@book {Ballard1990a,
	title = {{The Lost Wreck of the Isis}},
	year = {1990},
	pages = {63},
	publisher = {Scholastic},
	organization = {Scholastic},
	address = {New York},
	keywords = {ROV Jason (Remotely Operated Vehicle)},
	isbn = {0-590-43852-2},
	author = {Ballard, R D and Archbold, R}
}
@inbook {Fiala-Medioni1990,
	title = {{Lysosomic resorption of bacterial symbionts in deep-sea bivalves}},
	booktitle = {Endocytobiology IV: 4th International Colloquium on Endocytobiology and Symbiosis},
	year = {1990},
	pages = {3335{\textendash}3338},
	publisher = {Institut National de la Recherche Agronomique},
	organization = {Institut National de la Recherche Agronomique},
	address = {Paris},
	isbn = {2-7380-0241-2},
	author = {Fiala-Medioni, A and Felbeck, H and Childress, J J and Fisher, C R and Vetter, R D},
	editor = {Nardon, P}
}
@article {Tyre1989,
	title = {{Live TV broadcasts from ocean floor bring new depth to science education}},
	journal = {Technological Horizons in Education Journal},
	volume = {17},
	number = {1},
	year = {1989},
	pages = {42,44{\textendash}46},
	keywords = {ROV Jason (Remotely Operated Vehicle), ROV Medea (Remotely Operated Vehicle)},
	issn = {0192-592X},
	author = {Tyre, T}
}
@inbook {Saint1988,
	title = {{Les megalopodes et jeunes stades crabe de trois especes du genre Bythograea Williams 1980 (Crustacea Decapoda Branchyura) = Megalopae and early crab stages of three species of the genus Bythograea Williams, 1980 (Crustacea, Decapoda, Brachyura)}},
	booktitle = {De Colloque Les Sources Hydrothermales De La Ride Du Pacifique Oriental. Biologie et Ecologie Paris 4-7 November 1985.},
	series = {Oceanologica acta},
	number = {8},
	year = {1988},
	pages = {99{\textendash}107},
	publisher = {Gauthier-Villars},
	organization = {Gauthier-Villars},
	address = {Montrouge, France},
	isbn = {2040148965},
	author = {Saint, L M}
}
@article {Jannasch1988a,
	title = {{Life at deep sea hydrothermal vents}},
	journal = {Forhandlingen Kgl. Norske Videnskabers Selskabs},
	volume = {1988},
	year = {1988},
	pages = {75{\textendash}93},
	author = {Jannasch, H W}
}
@article {Ballard1987a,
	title = {{Live deep-sea expedition video coverage planned for scientists ashore}},
	journal = {Oceanus},
	volume = {30},
	number = {3},
	year = {1987},
	pages = {11{\textendash}15},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0029-8182},
	author = {Ballard, R D and von Alt, C and Hersey, W J}
}
@article {TenHove1986,
	title = {{Laminatubus alvini gen. et sp.n. and Protis hydrothermica sp.n. (Polychaeta, Serpulidae) from the bathyal hydrothermal vent communities in the eastern Pacific}},
	journal = {Zoologica Scripta},
	volume = {15},
	number = {1},
	year = {1986},
	pages = {21{\textendash}31},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0300-3256},
	doi = {10.1111/j.1463-6409.1986.tb00205.x},
	url = {http://dx.doi.org/10.1111/j.1463-6409.1986.tb00205.x},
	author = {Ten Hove, H A and Zibrowius, H}
}
@article {Ballard1986,
	title = {{A long last look at Titanic}},
	journal = {National Geographic Magazine},
	volume = {170},
	number = {6},
	year = {1986},
	pages = {697{\textendash}727},
	issn = {0027-9358},
	author = {Ballard, R D}
}
@article {Jannasch1985b,
	title = {{Leben in der Tiefsee auf chemosynthetischer Basis}},
	journal = {Naturwissenschaften},
	volume = {72},
	number = {6},
	year = {1985},
	pages = {285{\textendash}290},
	issn = {0028-1042},
	doi = {10.1007/BF00454769},
	url = {http://dx.doi.org/10.1007/BF00454769},
	author = {Jannasch, H W}
}
@inbook {Giermann1985,
	title = {{Les submersibles de recherche en geologie marine}},
	booktitle = {Deuxiemes Journees d{\textquoteright}etude sur la plongee scientifique},
	year = {1985},
	pages = {75{\textendash}83},
	publisher = {Musee Oceanographique},
	organization = {Musee Oceanographique},
	address = {Monaco-Ville},
	isbn = {272600136x},
	author = {Giermann, G},
	editor = {Roy, P}
}
@inbook {Laubier1985,
	title = {{L{\textquoteright}utilisation des sous-marins habites pour l{\textquoteright}etude de l{\textquoteright}ecosysteme abyssal: Le cas particulier des sources hydrothermales}},
	booktitle = {Deuxiemes Journees d{\textquoteright}etude sur la plongee scientifique},
	year = {1985},
	pages = {107{\textendash}129},
	publisher = {Musee Oceanographique},
	organization = {Musee Oceanographique},
	address = {Monaco-Ville},
	isbn = {272600136x},
	author = {Laubier, L and Reyss, D and Sibuet, M},
	editor = {Roy, P}
}
@article {Ballard1979d,
	title = {{Life where the earth is renewed}},
	journal = {World Book{\textquoteright}s Science Year in Review},
	volume = {1979},
	year = {1979},
	pages = {12{\textendash}27},
	issn = {1537-5870},
	author = {Ballard, R D}
}
@inbook {Grassle1978,
	title = {{Life histories and genetic variation in marine invertebrates}},
	booktitle = {Marine Organisms: Genetics, Ecology, and Evolution},
	series = {NATO conference series. IV, Marine sciences},
	year = {1978},
	pages = {347{\textendash}364.},
	publisher = {Plenum Press},
	organization = {Plenum Press},
	address = {New York, N.Y.},
	isbn = {0306400200},
	author = {Grassle, J F},
	editor = {Battaglia, B}
}
@article {Neumann1978,
	title = {{Lithotherms in the Straits of Florida: Comment and reply}},
	journal = {Geology},
	volume = {6},
	number = {1},
	year = {1978},
	pages = {7{\textendash}8},
	issn = {0091-7613},
	doi = {10.1130/0091-7613(1978)6<7:LITSOF>2.0.CO;2},
	url = {http://dx.doi.org/10.1130/0091-7613(1978)6{\%}3C7:LITSOF{\%}3E2.0.CO 2},
	author = {Neumann, A C}
}
@article {Schlager1978,
	title = {{Low-magnesian calcite limestones forming at the deep-sea floor, Tongue of the Ocean, Bahamas}},
	journal = {Sedimentology},
	volume = {25},
	number = {5},
	year = {1978},
	pages = {675{\textendash}699},
	issn = {0037-0746},
	doi = {10.1111/j.1365-3091.1978.tb00325.x},
	url = {http://dx.doi.org/10.1111/j.1365-3091.1978.tb00325.x},
	author = {Schlager, W and James, N P}
}
@article {Neumann1977,
	title = {{Lithotherms in the Straits of Florida}},
	journal = {Geology},
	volume = {5},
	number = {1},
	year = {1977},
	pages = {4{\textendash}10},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0091-7613},
	doi = {10.1130/0091-7613(1977)5<4:LITSOF>2.0.CO;2},
	url = {http://dx.doi.org/10.1130/0091-7613(1977)5{\%}3C4:LITSOF{\%}3E2.0.CO 2},
	author = {Neumann, A C and Kofoed, J W and Keller, G H}
}
@book {Shultz1966,
	title = {{Long term exposure and cycling tests of syntactic foam buoyancy material used in DSRV Alvin}},
	series = {WHOI technical memoranda},
	year = {1966},
	pages = {21},
	publisher = {Woods Hole Oceanographic Institution},
	organization = {Woods Hole Oceanographic Institution},
	address = {Woods Hole, Mass.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	author = {Shultz, W S and Omohundro, F P}
}
