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standardization of environmental data and information - International ...

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Sediment-trap levels<br />

The Workshop discussed a suggestion to add a sediment trap below<br />

the two proposed by LTC, the lower <strong>of</strong> which would be at 500 m above the<br />

bottom. One proponent <strong>of</strong> this idea noted that the depth <strong>of</strong> sediment <strong>and</strong><br />

nodule separation was still unknown; while another urged deep placement<br />

– perhaps 10 m above the seabed -- in order to collect baseline <strong>data</strong><br />

needed to assess mining impacts. Smith observed that a trap could not be<br />

used to track primary flux if it were put in the benthic boundary layer, 100-<br />

200 m above the seafloor; 500 m was a st<strong>and</strong>ard deployment to look at<br />

deep flux that was probably getting to the seafloor, without having the trap<br />

impacted by the benthic boundary layer. Another participant agreed that<br />

there must be a trap above this layer but argued that an additional trap<br />

near the bottom could provide <strong>information</strong> about resuspension material.<br />

Smith countered that the transmissometer (nephelometer)<br />

suggested for physical oceanographic measurements in the benthic<br />

boundary layer might provide even more <strong>data</strong> about resuspension than a<br />

sediment trap. However, it was pointed out that a transmissometer<br />

recorded <strong>data</strong> on small particles whereas a sediment trap collected large<br />

particles. The French had combined nephelometry <strong>and</strong> the sediment trap<br />

for more than ten years, employing a trap at 10 m together with a<br />

transmissometer <strong>and</strong> another trap at 200 m from the bottom.<br />

Bioturbation<br />

Smith remarked that bioturbation was an easily measured index <strong>of</strong><br />

one form <strong>of</strong> community activity that was useful in indicating the depths at<br />

which redeposited sediment would be mixed during community recovery<br />

from a redeposition event. The LTC recommendations called for contractors<br />

to gather <strong>data</strong> on the mixing <strong>of</strong> sediment by organisms. The Commission’s<br />

explanatory commentary suggested that rates <strong>of</strong> bioturbation be assessed<br />

with pr<strong>of</strong>iles <strong>of</strong> Pb-210, a st<strong>and</strong>ard isotope. It also suggested depth<br />

intervals going from 0-1 down to 14-15 cm, a range that was probably not<br />

relevant in the CCFZ, according to studies showing that bioturbation<br />

penetrated only about 2 cm. He therefore recommended measurement<br />

over a depth <strong>of</strong> 0-5 cm, which he expected to be uncontroversial. He<br />

further recommended that five replicate pr<strong>of</strong>iles be taken at each station to<br />

give a statistically valid sample size.<br />

INTERNATIONALSEABED AUTHORITY 301

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