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had been used to look at resedimentation impacts, but not in habitats<br />

ecologically analogous to areas like the CCFZ. The ecology <strong>of</strong> the<br />

oligotrophic deep sea was so different from that <strong>of</strong> shallow waters or even<br />

the continental slope that it was difficult to extrapolate results.<br />

A biologist suggested that turbidite flows might be the nearest<br />

natural event to deep-sea mining. A paper on one such event, at least<br />

1000 years ago on the Madeira Abyssal Plain (MAP) in the northeast<br />

Atlantic Ocean, 26 concluded that it had badly affected polychaetes but the<br />

diversity <strong>of</strong> nematodes had been reduced only slightly (see chapter 16<br />

below). This followed a pattern seen in shallow water, that larger animals<br />

such as polychaetes were much more affected by such events than<br />

nematodes. One reason might have to do with how they fed: nematodes<br />

were suspension feeders, not surface feeders. Another explanation might<br />

concern scale: a nematode was readily picked up <strong>and</strong> placed elsewhere,<br />

just as a high wind that might blow a man over <strong>and</strong> break his skull merely<br />

moved an insect from one place to another.<br />

Another participant noted that there had been studies <strong>of</strong> volcanic<br />

ash deposition in a shallower environment, foram distributions, turbidite<br />

flows, slumping <strong>and</strong> mass wasting. However, many such events were<br />

difficult to date because they had happened so long ago. The authors <strong>of</strong><br />

the paper on the MAP site were unsure whether the effects they had<br />

observed were due to low production or to the historical event. Not only<br />

were these events in different environments, they also seemed like a<br />

fundamentally different kind <strong>of</strong> phenomenon because they involved burial<br />

or deposition on top, not completely rechurning the sediments. Thus, in<br />

terms <strong>of</strong> both habitat <strong>and</strong> kind <strong>of</strong> disturbance, it was hard to compare such<br />

natural phenomena with what might be expected from mining.<br />

Economic value <strong>of</strong> seabed biota<br />

Asked whether the life on the ocean bottom had any economic<br />

value aside from its worth as an ecosystem, Smith responded by citing<br />

biodiversity <strong>and</strong> the use <strong>of</strong> genetic diversity in biotechnology. He mentioned<br />

his collaboration with a biotechnology company from San Diego, California,<br />

that was interested in prospecting an extreme environment for unusual<br />

genes that could be used in products such as cold-water detergents. Its<br />

interest in the deep sea was due to the tremendous diversity <strong>and</strong> extreme<br />

biological conditions there, including low temperature <strong>and</strong> high pressure.<br />

The CCFZ contained great evolutionary diversity <strong>and</strong> considerable genetic<br />

resources <strong>of</strong> potential use in biotechnology. The company wanted him to<br />

INTERNATIONAL SEABED AUTHORITY 82

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