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Marine Ecosystems Research Department - jamstec japan agency ...

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JAMSTEC 2002 Annual Report<br />

<strong>Marine</strong> <strong>Ecosystems</strong> <strong>Research</strong> <strong>Department</strong><br />

populations directly and indirectly incorporate substances<br />

ejected from the seafloor, and are thought to<br />

contribute significantly to the circulation of these<br />

ejected substances. Making use of deep-sea research<br />

systems such as submersibles and ROVs, this<br />

research aims to clarify the interrelationship between<br />

substances ejected from within the earth and deep-sea<br />

chemosynthetic ecosystems, and the basic physiological<br />

and ecological characteristics of deep-sea<br />

chemosynthetic populations.<br />

From May to July , geochemical, microbiological<br />

and zoological investigations were conducted using<br />

the submersible 'Shinkai ' at a hydrothermal vent<br />

field, the Hatoma Knoll in the Okinawa Trough, and a<br />

methane seep field, the Kuroshima Knoll (Fig. ) off<br />

Sakishima Islands. The purpose of this investigation<br />

included; ) geochemical analysis of water at vent<br />

communities and vent fluids, ) physical environmental<br />

factor analysis at vent communities and vent fluids,<br />

) estimation of energy sources for vent ecosystems,<br />

) biodiversity of vent communities, ) estimation of<br />

biomass of vent communities, ) estimation of productivity<br />

of vent communities, ) relationships of biomass<br />

and productivity between microbial communities and<br />

benthic communities, ) comparisons between the<br />

Kuroshima Knoll and the Hatoma Knoll, ) physiological<br />

and embryological studies of vent benthic species.<br />

Data and samples collected during the investigation<br />

are now being analyzed.<br />

Fig. 6 Bathymodiolus short-type dominated community associated<br />

with methane seep in the Hatoma Knoll.<br />

<strong>Research</strong> on the characteristics of the deep seawater<br />

in Suruga Bay and the cascade method of deep<br />

seawater utilization<br />

Period: FY-FY<br />

Shizuoka Prefecture is carrying out the project for<br />

the effective utilization of deep seawater in Suruga<br />

Bay. In September the Prefecture installed intake<br />

facilities for surface water (depth of m) and deep<br />

water (depths of m and m), and began distributing<br />

the water to private companies and households.<br />

The objectives of this research are to contribute to the<br />

efficient promotion of the project, and to the establishment<br />

of practical deep seawater utilization technology.<br />

To this end, we are working together with Shizuoka<br />

Prefecture to deploy analysis and observation systems,<br />

research deep seawater near the Suruga Bay intake<br />

and its surrounding area, and examine the cascade<br />

method for the effective use of deep seawater.<br />

The following are the major research results for<br />

fiscal .<br />

(a) Characteristics of deep seawater<br />

In October we conducted surveys in and around<br />

the deep seawater intake area using CTD and also<br />

through vertical multilayer water sampling. Our use of<br />

an altimeter in CTD observations enabled us to measure<br />

down to five meters directly above the seafloor. In relation<br />

to the issue of suspended matter, the vertical distribution<br />

of the attenuation coefficient (Fig. ; high values<br />

indicate high turbidity) calculated from a flux transmissometer<br />

fitted to the CTD system tends to show a high<br />

attenuation coefficient in water shallower than m and<br />

water between a depth of m and the seafloor<br />

(m). Similarly, the vertical distribution of suspended<br />

matter concentration (Fig. ) in seawater collected in<br />

the same cast as this measurement shows a high reading<br />

in water shallower than m and water deeper than<br />

m. Deep seawater intakes are established at depths<br />

of m and m, and the opening that draws in seawater<br />

is m above the seafloor. Therefore water with<br />

relatively high concentrations of suspended matter is<br />

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