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Schriever replied that the device, which had been designed by the<br />

DISCOL team, had cost 30,000 German marks in 1988 (about $15,000 at<br />

the current rate) for four duplicate pieces kept onboard in case something<br />

was lost or went wrong. In mining, however, the nodules would have to be<br />

harvested, not ploughed under, so that a way had to be found to collect<br />

them. Moreover, the device was not <strong>environmental</strong>ly friendly because it<br />

created a big plume that could be observed about 20 m above the seafloor,<br />

even six hours later. He had therefore been glad to hear the Indian<br />

approach in developing collectors that did not have such a big impact. He<br />

welcomed the efforts during the past nine or ten years to instil<br />

<strong>environmental</strong> consciousness into everyone who would be involved in<br />

mining, not only scientists <strong>and</strong> <strong>environmental</strong>ists but also engineers <strong>and</strong><br />

politicians.<br />

Another participant cited <strong>information</strong> from the proceedings <strong>of</strong> the<br />

1998 Workshop <strong>of</strong> the <strong>International</strong> Seabed Authority 45 indicating that the<br />

plough-harrow system was much different from actual mining equipment<br />

because <strong>of</strong> the size <strong>of</strong> the area covered – a fact, he added, that had been<br />

recognized by Dr. Thiel.<br />

Schriever agreed that the impact from the plough-harrow was<br />

different from that <strong>of</strong> a mining system. The DISCOL researchers had<br />

pointed out that they had not simulated mining; rather, they had created an<br />

impact that might be comparable to what a mining system might create. A<br />

mining system would probably not be able to avoid disturbing the sediment<br />

surface because even a 10-ton system like the Indian model described by<br />

Dr. M. Ravindran (chapter 7 above) would penetrate into the sediment <strong>and</strong><br />

disturb the upper 10-15 cm. Because the sediment was s<strong>of</strong>t, especially in<br />

its upper centimetres – though this differed from locality to locality in the<br />

CCFZ as well as in the South Pacific -- it would be disturbed <strong>and</strong> most <strong>of</strong> the<br />

megafauna within the tracks would probably be killed. Most or at least<br />

some <strong>of</strong> the macr<strong>of</strong>auna <strong>and</strong> mei<strong>of</strong>auna would survive, especially the<br />

nematodes.<br />

Asked whether his group had ideas about the kind <strong>of</strong> disturber that<br />

could be designed for a future experiment, Schriever said no activity on this<br />

subject was under way in Germany. He thought it should be tackled after<br />

the results <strong>of</strong> the various BIEs had been correlated.<br />

INTERNATIONAL SEABED AUTHORITY 359

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