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/ Platform | Operation | Year | Dive Number | References |
TN-167A R/V Thompson/ ROPOS | Not found | 2004 March | Not found | YK05-09-Leg2 cruise report |
YK05-09 Yokosuka/ Shinkai 6500 | WHATS, ROCS, Bag with high temperature probe, pH, pCO2, ORO sensors | 2005 July-August | 903, 905 | YK05-09-Leg2 cruise report |
YK10-10 Yokosuka/ Shinkai 6500 | Not found | 2010 August | 1216, 1217 | YK10-10 cruise report |
YK10-11 Yokosuka/ Shinkai 6500 | Not found | 2010 September | 1221, 1223, 1224 | YK10-11 cruise report |
Table 2: Vent activity and host rocks
Activity and Host Rocks | References | |
Activity | Active | Yoshikawa et al., 2012, Ikehata et al., 2015; Kato et al., 2010 |
Host Rocks | Basalt and Andesite | Toki et al., 2015 |
Table 3: Vent fluid characteristics
Vent Fluids | References | |
Temperature (οC) | 93 οC-343 οC | Toki et al., 2015; Ikehata et al., 2015 |
pH | 3 (at 25 οC) | Ishibashi et al., 2006 |
2.94 | Toki et al., 2015 | |
Composition | K rich with low Cl concentrations and low pH. | Ishibashi et al., 2004 |
High concentrations of H2S | Ishibashi et al., 2006; Kato et al., 2010 | |
CO2 (mM) | 6.4-32.6 | Toki et al., 2015 |
H2 (μM) | 466 | Toki et al., 2015 |
Mn (mM) | 1.06-1.2 | Toki et al., 2015 |
Fe (mM) | 2.55-3.00 | Toki et al., 2015 |
He (μM) | 2.1 | Toki et al., 2015 |
CH4 (μM) | 115 | Toki et al., 2015 |
Table 4: Vent Biology
General name | Phylum | Class / Order | Family | Genus/Species | References |
Bacteria | Aquificae | Aquificales | Hydrogenothermaceae | Persephonella | Kato et al., 2012 |
Bacteria | Proteobacteria | Gammaproteobacteria | Kato et al., 2010 | ||
Bacteria | Proteobacteria | Epsilonproteobacteria | Campylobacterales | Hydrogenimonas | Kato et al., 2010; Kato et al., 2012 |
Bacteria | Proteobacteria | Epsilonproteobacteria | Campylobacterales | Sulfurimonas | Kato et al., 2010; Kato et al., 2012 |
Bacteroidetes | Kato et al., 2010 | ||||
Barnacle | Arthropoda | Multicrustacea | Neoverrucidae | Neoverruca brachylepadoformis | Kumagai et al., 2015 |
Shrimp | Arthropoda | Malacostraca | Alvinocarididae | Chorocaris vandoverae | Kumagai et al., 2015 |
Snail | Mollusca | Gastropoda | Provannidae | Alviniconcha hessleri | Kumagai et al., 2015 |
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