Conical Vent

Latitude: 19.542οN                  Longitude: 146.648οE             Depth: 3144 m bsl

Conical Seamount is a smooth sided, nearly circular forearc serpentine mud volcano with a slightly flattened summit region (Fryer, 1996) that is located adjacent to a large forearc graben (Fryer et al., 1990; Fryer, 1992; Newsom, 1992). Conical Seamount is considered active because of the discovery of recent mud extrusions and the venting of fluids with deep slab origins [Fryer and Mottl, 1992]. The fluids are actively flowing through carbonate and silicate chimneys and have elevated pH, high alkalinity and enrichments in CH4, SiO2, SO42-, and H2S. Methane and sulfate in the fluids are probably generated during serpentinization reactions between peridotite and slab derived fluids (Fryer, 1990). Some bacterial mats, small limpets and gastropods are associated with these vents.

Table 1: Operations history for Conical vent

Ship/ PlatformOperationYearDive NumberReferences
KR06-15 KaikoNot found2006 November 0369JAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical”)KR06-15 cruise report
Not foundSeaMARK II bathymetry dataNot foundNot foundFryer et al., 1996; Fryer et al., 1992
Not foundSeasat A Satellite Scatterometer (SASS) dataNot foundNot foundFryer et al., 1996; Fryer et al., 1992
TN-154 Thompson/ ROV Jason-2Not found2003 AprilJ2-032Woods Hole Oceanographic Institution: ROV JASON/MEDEA: Operations Summary (note: click “Files- operations summary”)
YK03-07 Yokosuka/ Shinkai 6500Not found2003 September785YK03-07 cruise report

Table 2: Vent activity and host rocks

Activity and Host RocksReferences
ActivityActive mud volcanismFryer and Mottl., 1992; Fryer., 1990;  IODP-MCME 366 Proposal; Savov et al., 2005
Host RocksSerpentinized harzburgite and duniteFryer et al., 1990; Savov et al., 2005

Table 3: Vent fluid characteristics

Bottom seawaterVent FluidsReferences
Distance from the trench (km)90IODP-MCME 366 Proposal
Temperature (οC)13.5 οC (hole 780D); 1.5οCFryer et al., 1990(c); Mottl et al., 2003
pH7.729.28Fryer et al., 1990
>9.2, 12.5Hulme et al., 2010, Fryer et al., 1990 b
CompositionIndicate deep seated serpentinization sources, enriched in CH4, SiO2, SO42-, H2SFryer et al., 1990
Alkalinity (meq/kg)2.3High, 41Fryer et al., 1990
Clorinity (mmol/kg)542260IODP-MCME 366 Proposal
CH(mmol/kg)4×10-72±1Mottl et al., 2003
Mn (μmol/kg)0<0.01IODP-MCME 366 Proposal
Fe (μmol/kg)02IODP-MCME 366 Proposal
Sulfate  (mmol/kg)2846IODP-MCME 366 Proposal
Mg (mmol/kg)0.009Fryer et al., 1990 b
Ca (mmol/kg)0.6Fryer et al., 1990 b
Na (mmol/kg)466390IODP-MCME 366 Proposal
K (mmol/kg)10.115IODP-MCME 366 Proposal
Li (μmol/kg)261.6IODP-MCME 366 Proposal
Rb (μmol/kg)1.377.8IODP-MCME 366 Proposal
Sr (μmol/kg)9020IODP-MCME 366 Proposal
Ba (μmol/kg)0.140.1IODP-MCME 366 Proposal
B (μmol/kg)4103900IODP-MCME 366 Proposal
Si (μmol/kg)19060IODP-MCME 366 Proposal

* IODP-MCME 366- International Ocean Discovery Program-Mariana Convergent Margin Expedition 366.

Table 4: Vent Biology

General namePhylumClass/OrderFamilyGenus/SpeciesReferences
Bacterial matsBacteriaFryer et al., 1990
FishChordataAnguilliformesJAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical seamount”)
GastropodsMolluscaFryer et al., 1990
Sea anemoneCnidariaActiniariaBoloceroididaeJAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical seamount”)
Sea cucumbersEchinodermsHolothuroideaPelagothuriidaeEnypniastes eximiaJAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical seamount”)
ShrimpArthropodaDecapodaJAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical seamount”)
Small LimpetsMolluscaFryer et al., 1990
SpongePoriferaJAMSTEC E-library of Deep-sea Images (JEDI) (note: search “Conical seamount”)


Images:

Video Links: None known

References:

  1. Fryer, P., Saboda, K. L., Johnson, L. B., Mackay, M. E., Moore, G. F., Sto¡ers, P., 1990. Conical Seamount: SeaMARK II, Alvin submersible, and seismic reflection studies. Proc. ODP Init. Rep. 125, 69-80.
  2. Fryer, P., Mottl, M. J., 1992. Lithology, mineralogy, and origin of serpentine muds recovered from Conical and Torishima forearc seamounts: results of Leg 125 drilling, Proc. ODP Sci. Results 125, 343-362.
  3. Fryer, P, 1996. Evolution of the Mariana convergent plate margin system. Reviews of Geophysics 31 (1), 89-125.
  4. Mottl, M. J., Komor, S. C., Fryer, P., Moyer, C. L., 2003. Deep-slab fluids fuel extremophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195. Geochemistry, Geophysics, Geosystems 4 (11) 9009, doi: 10.1029/2003GC000588.
  5. Savov, I. P., Ryan, J. G., D’Antonio, M., Kelley, K., Mattie, P., 2005. Geochemistry of serpentinized peridotites from the Mariana Forearc Conical Seamount, ODP Leg 125: Implications for the elemental recycling at subduction zones. Geochem.Geophys. Geosyst., 6, Q04J15, doi: 10.1029/2004GC000777.

Website References:

  1. J-EDI JAMSTEC (Japan Agency for Marine Earth Science and Technology) E-library of Deep-sea Images: http://www.godac.jamstec.go.jp/jedi/public/Sec101.jsf (accessed 11/24/2015)
  2. Woods Hole Oceanographic Institution: ROV JASON/MEDEA: Operations Summary http://www.whoi.edu/main/jason/operations-summary (accessed 11/24/2015)

Cruise Reports:

  1. IODP Mariana Convergent Margin Expedition 366, unpublished IODP proposal http://iodp.tamu.edu/scienceops/precruise/mariana/505-Full5.pdf (accessed 01/19/2016)
  2. Kairei cruise report KR06-15 http://www.godac.jamstec.go.jp/catalog/data/doc_catalog/media/KR06-15_leg1-2_all.pdf (accessed 01/19/2016)
  3. Yokosuka cruise report YK03-07 http://www.godac.jamstec.go.jp/catalog/data/doc_catalog/media/YK03-07_all.pdf (accessed 01/19/2016)