Archaean Vent

Latitude: 12.939οN                  Longitude: 143.632οE             Depth: 3060 m bsl

The Archean site was discovered in 2004 at the top of a giant (50-m high) sulfide mound, located on the eastern flank of the Malano-Gadao Ridge spreading axis (Ishibashi et al., 2004) in the southern Mariana Trough. The site is an active hydrothermal system, with black smokers venting fluids as hot as 341°C (Yoshikwa et al., 2012). Chemistry of these fluids at that time was characterized by low pH, low Cl concentration (Ishibashi et al., 2006) and high H2S (Kato et al., 2010). The hydrothermal field has several discrete hydrothermal mounds with active and/or inactive chimneys (Ishibashi et al., 2006). On the basis of the associated geomorphological features, the Archean site is thought to have been created by prolonged hydrothermal activity (Yoshikawa et al., 2012). Biologically this site is enriched with different species of bacteria (Kato et al., 2010; Kato et al., 2012).

Table 1: Operations history for Archaean vent

Ship/ PlatformOperationYearDive NumberReferences
TN-167A R/V Thompson/ ROPOSNot found2004 MarchNot foundYK05-09-Leg2 cruise report
YK05-09 Yokosuka/ Shinkai 6500WHATS, ROCS, Bag with high temperature probe,  pH, pCO2, ORO sensors2005 July-August903, 905YK05-09-Leg2 cruise report
YK10-10 Yokosuka/ Shinkai 6500Not found2010 August1216, 1217YK10-10 cruise report
YK10-11 Yokosuka/ Shinkai 6500Not found2010 September1221, 1223, 1224YK10-11 cruise report

Table 2: Vent activity and host rocks

Activity and Host RocksReferences
ActivityActiveYoshikawa et al., 2012, Ikehata et al., 2015; Kato et al., 2010
Host RocksBasalt and AndesiteToki et al., 2015

Table 3: Vent fluid characteristics

Vent FluidsReferences
Temperature (οC)93 οC-343 οCToki et al., 2015; Ikehata et al., 2015
pH3 (at 25 οC)Ishibashi et al., 2006
2.94Toki et al., 2015
CompositionK rich with low Cl concentrations and low pH.Ishibashi et al., 2004
High concentrations of H2SIshibashi et al., 2006; Kato et al., 2010
CO2 (mM)6.4-32.6Toki et al., 2015
H(μM)466Toki et al., 2015
Mn (mM)1.06-1.2Toki et al., 2015
Fe (mM)2.55-3.00Toki et al., 2015
He (μM)2.1Toki et al., 2015
CH4 (μM)115Toki et al., 2015

Table 4: Vent Biology

General namePhylumClass / OrderFamilyGenus/SpeciesReferences
BacteriaAquificaeAquificalesHydrogenothermaceaePersephonellaKato et al., 2012
BacteriaProteobacteriaGammaproteobacteriaKato et al., 2010
BacteriaProteobacteriaEpsilonproteobacteriaCampylobacteralesHydrogenimonasKato et al., 2010;  Kato et al., 2012
BacteriaProteobacteriaEpsilonproteobacteriaCampylobacteralesSulfurimonasKato et al., 2010; Kato et al., 2012
BacteroidetesKato et al., 2010
BarnacleArthropodaMulticrustaceaNeoverrucidaeNeoverruca brachylepadoformisKumagai et al., 2015
ShrimpArthropodaMalacostracaAlvinocarididaeChorocaris vandoveraeKumagai et al., 2015
SnailMolluscaGastropodaProvannidaeAlviniconcha hessleriKumagai et al., 2015

Images:

Video Links:

References:

  1. Ikehata,K., Suzuki, R., Shimada, K., Ishibashi, J., Urabe, T., 2015. Mineralogical and Geochemical Characteristics of Hydrothermal Minerals Collected from Hydrothermal Vent Fields in the Southern Mariana Spreading Center. In: Ishibashi, J., Okino, K., Sunamura, M. (Eds.), Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, 275-287.
  2. Ishibashi, J., Suzuki, R., Yamanaka, T., Toki, T., Kimura, H., Noguchi, T., Urabe, T., 2006. Seafloor hydrothermal activity at offaxial seamounts of backarc spreading in southern Mariana Trough. Geochimica et Cosmochimica Acta 70 (18), A279-A279.
  3. Ishibashi, J., Yamanaka, T., Kimura, H., Hirota, A., Toki, T., Tsunogai, U., Gamo, T., Utsumi, M., Roe, K., Miyabe, S., Okamura, K. 2004. Geochemistry of Hydrothermal Fluids in South Mariana Backarc Spreading Center. American Geophysical Union, Fall Meeting 2004, abstract #V44A-05.
  4. Kato, S., Takano, Y., Kakegawa, T., Oba, H., Inoue, K., Kobayashi, C., Utsumi, M., Marumo, K., Kobayashi, K., Ito, Y., Ishibashi, J., Yamagishi, A., 2010. Biogeography and biodiversity in sulfide structures of active and inactive vents at deep-sea hydrothermal fields of the Southern Mariana Trough. Applied Environmental Microbiology 76 (9), 2968-2979.
  5. Kato, S., Nakamura, K., Toki, T., Ishibashi, J., Tsunogai, U., Hirota, A., Ohkuma, M., Yamagishi, A., 2012. Iron-based microbial ecosystem on and below the seafloor: a case study of hydrothermal fields of the Southern Mariana Trough. Frontiers in Microbiology 3, doi: 10.3389/fmicb.2012.00089.
  6. Kumagai, H., Watanabe, H., Yahagi, T., Kojima, S., Nakai, S., Toyoda, S., Ishibashi, J., 2015. Evaluating Hydrothermal System Evolution Using Geochronological Dating and Biological Diversity Analyses. In: Ishibashi, J., Okino, K., Sunamura, M. (Eds.), Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, 49-59.
  7. Toki, T., Ishibashi, J., Noguchi, T., Tawata, M., Tsunogai, U., Yamanaka, T., and Nakamura, K., 2015, Chemical and Isotopic Compositions of Hydrothermal Fluids at Snail, Archaean, Pika, and Urashima Sites in the Southern Mariana Trough. In: Ishibashi, J., Okino, K., Sunamura, M. (Eds.), Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, 587-602.
  8. Yoshikawa, S., Okino, K., and Asada, M., 2012. Geomorphological variations at hydrothermal sites in the southern Mariana Trough: Relationship between hydrothermal activity and topographic characteristics. Marine Geology 303-306, 172-182.

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 08/20/2015)

Cruise Reports:

  1. Yokosuka Cruise Report YK05-09-Leg2 http://www.godac.jamstec.go.jp/catalog/data/doc_catalog/media/YK05-09_leg2_all.pdf (accessed 11/26/2015)
  2. Yokosuka Cruise Report YK10-10 http://www.godac.jamstec.go.jp/catalog/data/doc_catalog/media/YK10-10_all.pdf (accessed 11/26/2015)
  3. Yokosuka Cruise Report YK-10-11 http://www.godac.jamstec.go.jp/catalog/data/doc_catalog/media/YK10-11_all.pdf (accessed 11/26/2015)