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second part <strong>of</strong> BIE, beginning in 2001, Yuzhmorgeologia had started its own<br />

ecological investigation in the Russian Experimental Polygon (REP). In<br />

selecting the site for the BIE experiment, the researchers had looked for an<br />

area <strong>of</strong> clear sediment without manganese nodules or with low nodule<br />

density.<br />

Sediment disturbance associated with nodule mining would create<br />

in the first place an impact on the benthic community. It was presumed<br />

that benthic organisms would be influenced by direct physical contact with<br />

the mining device, burial under a layer <strong>of</strong> resuspended sediment <strong>and</strong> a<br />

decrease in available food. The need to study this problem before<br />

commercial mining took place in the Clarion-Clipperton Fracture Zone<br />

(CCFZ) had been the main motivation for several international model<br />

experiments impacting the deep-sea benthos, including BIE, the Japan<br />

Deep-Sea Impact Experiment (JET), the Indian Deep-sea Environment<br />

Experiment (INDEX) <strong>and</strong> work done by IOM.<br />

The main design <strong>of</strong> the Russian experiment had been to create a<br />

relatively large disturbance <strong>of</strong> the upper sediment layer, using a miningsimulation<br />

device, in order to investigate the ecosystem’s response to the<br />

disturbance immediately <strong>and</strong> some years afterward. The project had<br />

included baseline investigation within the selected polygons, the benthic<br />

ecosystem disturbance itself, <strong>and</strong> monitoring <strong>of</strong> the disturbed site <strong>and</strong> a<br />

reference site. The studies had been carried out immediately after the<br />

disturbance, one year later <strong>and</strong> seven years later – close to the timetable <strong>of</strong><br />

the DISCOL experiment. The resuspended sediment plume had been<br />

tracked using near-bottom CTD (conductivity-temperature-depth) pr<strong>of</strong>iles.<br />

The thickness <strong>of</strong> the resuspended sediment had been measured with<br />

sediment traps, current-meter stations, transmissometers <strong>and</strong> X-ray photos<br />

<strong>of</strong> sediment cores. Locations <strong>of</strong> all underwater devices had been fixed with<br />

a global positioning system (GPS) using navigation satellites <strong>and</strong> an<br />

acoustic underwater navigation system, ASMOD, created within<br />

Yuzhmorgeologia. At the centre <strong>of</strong> the experiment was the disturber,<br />

designed by the United States firm Sound Ocean Systems, Inc. That<br />

company had created a first generation disturber, <strong>and</strong> for the BIE-II<br />

experiment it had built a more powerful second generation device. A similar<br />

device had been lost during the Japanese experiment. All BIE cruises had<br />

been carried out on the Russian vessel Yuzhmorgeologia, a large capacity<br />

ship <strong>of</strong> 5600 tons with a big bottom tank <strong>and</strong> an excellent wire-cable winch.<br />

272 INTERNATIONAL SEABED AUTHORITY

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