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standardization of environmental data and information - International ...

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A participant observed that, if only 30% <strong>of</strong> an area was mined in<br />

patches about 30-50 km wide, much <strong>of</strong> the area surrounding the highly<br />

disturbed portion might give organisms the chance to recolonise.<br />

Craig Smith commented that 3-5 km did not sound far but it was a<br />

much greater distance than in the DISCOL area, which had taken seven<br />

years or more to recover. He did not think any macr<strong>of</strong>auna would survive<br />

after being picked up in a nodule harvester <strong>and</strong> blown up into the water<br />

column. When samples were washed, they had to be treated with a low<br />

flow rate on a screen to keep from destroying most <strong>of</strong> the polychaetes. Yet,<br />

the shear forces involved in washing sediments on a sieve were orders <strong>of</strong><br />

magnitude lower than the shears produced in any kind <strong>of</strong> mining head to<br />

separate water from the nodules. Thus, while recolonisation <strong>of</strong> an area 5<br />

km in diameter area would be fast when compared to an area 100 km<br />

across, it would still be slow. If the surface sediment were stripped from an<br />

area 5 km across, he would expect recovery to take at least two or three<br />

times longer than in the case <strong>of</strong> DISCOL. No <strong>information</strong> was available<br />

about rates <strong>of</strong> recovery in the middle <strong>of</strong> a large-scale, devastating<br />

disturbance. It could take 100 years or more.<br />

A questioner, noting that in DISCOL the sediment had been shifted<br />

aside by up to 10 m compared to the 10-12 km that would be shifted by<br />

mining, asked whether the time required for recolonisation could be<br />

calculated by dividing 12 km by 10 m <strong>and</strong> multiplying the quotient by seven<br />

years. Schriever replied that the processes were non-linear.<br />

Another questioner, citing <strong>data</strong> to the effect that mei<strong>of</strong>auna had<br />

reached a steady state by the time they were sampled three years after the<br />

impact, wondered whether a steady state would have been found if<br />

sampling had occurred two years after impact. Schriever responded that<br />

steady state in this case referred to abundance, not species composition.<br />

In any case, species composition <strong>and</strong> diversity were still different from the<br />

baseline. He added that the researchers had tried without success to find<br />

any correlation between these <strong>data</strong> <strong>and</strong> the shift from El Niño to La Niña<br />

conditions.<br />

Asked whether the control sites had changed along with the impact<br />

site, Schriever replied that neither the nematodes nor the megafauna at the<br />

control sites had changed much. The tremendous change in abundance<br />

had occurred only within the DISCOL area.<br />

INTERNATIONAL SEABED AUTHORITY 361

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