Maug Vent

Latitude: 20.021οN                  Longitude: 145.222οE             Depth: 54 m bsl

Maug is an extinct volcano located in the Central Seamount Province (Bloomer et al., 1989). Maug consists of three islands arranged in a circular pattern around a caldera in which sits a resurgent dome that almost reaches sealevel (Submarine Ring of Fire, 2003). ROV dives found several diffuse vents clustered on the ENE quadrant of the central cone (Embley et al., 2007). Fluids released from weak vents around the central dome show elevated 3He levels and suggest that the central dome is actively degassing. These fluids are also enriched in CO2, TDMn, TDFe, pFe, and pMn (Resing et al., 2009). Maug is one of the few places on earth where photosynthetic and chemosynthetic life coexist. This unique community is composed of Bacteria, Fish, Soft corals, Gorgonians, Brittle stars, Worms and Mussels (Pala, 2009).

Table 1: Operations history for Maug vent

Ship/ PlatformOperationYearDive NumberReferences
TN-153 R/V T. G. ThompsonEM 300 multibeam2003 February – MarchNot foundSubmarine Ring of Fire 2003
TN-167 R/V T. G. ThompsonCTD Verical cast; ROPOS2004 March- AprilR789, R790Submarine Ring of Fire 2004

Table 2: Vent activity and host rocks

Activity and host rocksReferences
ActivityActiveBaker et al., 2008
Host RocksDaciteBasaltEmbley et al., 2007Woodhead., 1989

Table 3: Vent fluid characteristics

Vent FluidsReferences
Temperature (οC)60 οC (at 30 feet deep)Low T (<100 οC)Pala., 2009Embley et al., 2007
pH6.07Pala., 2009
ΔpH-0.17Resing et al., 2009
CompositionLarge concentrations of methane, total (particulate plus dissolved) Fe, and total Mn.CO2 and alkalinitySubmarine Ring of Fire 2003Resing et al., 2009
CO2 (mM)Not found
ΔCO2 (mM)119Resing et al., 2009
H2 (mM)Not found
Particulate Fe (nmol/kg)1238Resing et al., 2009
TDMn (nM)98Resing et al., 2009
TDFe (nM)700Resing et al., 2009
Δ3He (fM)12.8Resing et al., 2009
3He (μM)Not found
CH4 (nM)90Resing et al., 2009

* ΔpH, ΔCO– Measured relative to the regional background; Δ3He – Measured above the background.

Table 4: Vent Biology

General namePhylumReferences
BacteriaBacteriaPala., 2009
FishChordataPala., 2009
Soft coralsCnidariaPala., 2009
GorgoniansCnidariaPala., 2009
Brittle starsEchinodermataPala., 2009
WormsPala., 2009
MusselsMolluscaPala., 2009

Images:

Video Links: None known

References:

  1. Baker, E. T., Embley, R. W., Walker, S. L., Resing, J. A., Lupton, J. E., Nakamura, K., de Ronde, C. E. J., Massoth, G. J., 2008. Hydrothermal activity and volcano distribution along the Mariana arc: Journal of Geophysical Research 113 (B8), 1-16.
  2. Bloomer, S. H., Stern, R. J., Smoot, N. C., 1989. Physical volcanology of the submarine Mariana and Volcano arcs. Bull Volc 51, 210-224.
  3. Embley, R. W., Baker, E. T., Butterfield, D. A., Chadwick, W. W. Jr., Lupton, J. E., Resing, J. A., de Ronde, C. E. J., Nakamura, K., Tunnicliffe, V., Dower, J. F., Merle, S. G., 2007. Exploring the submarine ring of fire: Mariana Arc- Western Pacific, Oceanography 20, 68–79.
  4. Pala, C., 2009. The Pacific Ocean’s Acidification. Environmental Science and Technology 43, 6451–6452.
  5. Resing, J. A., Baker, E. T., Lupton, J. E., Walker, S. L., Butterfield, D. A., Massoth, G. J., Nakamura, K., 2009. Chemistry of hydrothermal plumes above submarine volcanoes of the Mariana Arc. Geochemistry, Geophysics, Geosystems 10 (2), 1-23.

Website References:

  1. Submarine Ring of Fire 2003 http://oceanexplorer.noaa.gov/explorations/03fire/logs/feb24/feb24.html (accessed 11/19/2015)
  2. Submarine Ring of Fire 2004 http://oceanexplorer.noaa.gov/explorations/04fire/logs/april09/media/corals_maug.html (accessed 11/19/2015)

Cruise Reports:

  1. Submarine Ring of Fire 2003 http://oceanexplorer.noaa.gov/explorations/03fire/logs/summary/marianas_cruisereport.pdf (accessed 11/19/2015)
  2. Submarine Ring of Fire 2004 http://oceanexplorer.noaa.gov/explorations/04fire/logs/summary/media/marianas2004cruisereport.pdf (accessed 11/19/2015)