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3.4. Benthic <strong>and</strong> demersal community composition<br />

The benthic <strong>and</strong> demersal communities in the CCFZ <strong>and</strong> the Indian<br />

Ocean claim area have not yet been adequately characterised. Generally, in<br />

both <strong>of</strong> these deep-seabed areas as well as in other deep ocean basins, the<br />

communities are essentially dependent for their nutrition on the organic<br />

content <strong>of</strong> falling detrital material from surface waters. No active<br />

hydrothermal vent communities are known in these areas <strong>and</strong>, obviously,<br />

no photosynthesis is possible.<br />

Environmental impacts <strong>of</strong> mining on the benthic communities are<br />

probably the most poorly understood class <strong>of</strong> impacts <strong>of</strong> all those that must<br />

be considered. Growth rates <strong>of</strong> individuals <strong>and</strong> recovery rates <strong>of</strong><br />

populations following disturbance may be very slow <strong>and</strong> need to be<br />

estimated before reasonable impact assessment can be attempted.<br />

Establishment <strong>of</strong> an adequate <strong>environmental</strong> baseline<br />

characterisation for the benthic communities in the contractors’ exploration<br />

areas is probably the most challenging problem that must be faced in the<br />

<strong>environmental</strong> assessment <strong>of</strong> deep-seabed mining. Certainly one <strong>of</strong> the<br />

highest priorities for this Workshop should be the development <strong>of</strong> st<strong>and</strong>ards<br />

that can be used to integrate existing collections <strong>and</strong> observations into<br />

comparable <strong>data</strong> sets, <strong>and</strong> to promote uniform collection methods in future<br />

investigations<br />

3.5. Climate, ocean circulation <strong>and</strong> water chemistry<br />

The climate in the Indian Ocean is dominated by the monsoon<br />

seasons, including the northeast monsoon (December to April) <strong>and</strong><br />

southwest monsoon (June to October). Tropical cyclones occur during<br />

January-February. Several currents make up the Indian Ocean's current<br />

system. The North Equatorial (November-April) <strong>and</strong> South Equatorial<br />

currents, Monsoon Drift, northeast monsoon (in April) <strong>and</strong> Antarctic<br />

Circumpolar currents all affect the flow <strong>of</strong> currents in the Indian Ocean. In<br />

the Indian claim area, these all contribute to a net westward flow <strong>of</strong> the<br />

surface currents year round. 10 General seawater components in the Indian<br />

claim area are representative <strong>of</strong> the low nutrient, oligotrophic tropical<br />

environments typical <strong>of</strong> both the central Indian Ocean <strong>and</strong> the CCFZ.<br />

The climate in the CCFZ is similarly tropical <strong>and</strong> subtropical, <strong>and</strong> is<br />

dominated by the northeastern trade winds during much <strong>of</strong> the year. In the<br />

107 INTERNATIONAL SEABED AUTHORITY

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