Marine Ecosystems Research Department - jamstec japan agency ...
Marine Ecosystems Research Department - jamstec japan agency ...
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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