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There was an increasing appreciation that productivity regimes in the open<br />

ocean varied on seasonal, interannual (e.g., El Niño) <strong>and</strong> decadal scales,<br />

including specific decadal oscillation, <strong>and</strong> they were likely to vary with global<br />

warming. A recent study showed that changes in temperature <strong>of</strong> the<br />

surface ocean altered the amount <strong>of</strong> carbon exported from it, so that even<br />

on global warming time scales there would be changes. The major<br />

challenge was to underst<strong>and</strong> natural patterns <strong>of</strong> variability in time <strong>and</strong><br />

space in these systems in order to be able to remove natural variability from<br />

any anthropogenic influences due to mining.<br />

SUMMARY OF DISCUSSION<br />

CCFZ variability<br />

A participant observed that the CCFZ seemed to be a transition zone<br />

between the equatorial region <strong>and</strong> the central gyres, with characteristics <strong>of</strong><br />

both. Oceanic productivity was generally much lower than in coastal<br />

regions but there seemed to be a gradient from exceptionally low<br />

productivity in the central gyre to areas <strong>of</strong> intermediate character.<br />

Smith agreed that the CCFZ was an enormous zone with longitudinal<br />

<strong>and</strong> especially latitudinal gradients in POC flux <strong>and</strong> many other parameters.<br />

As one moved from east to west <strong>and</strong> from south to north, there were<br />

dramatic reductions in the rain rate <strong>of</strong> organic matter <strong>and</strong> in productivity.<br />

The latitudinal gradients were probably quite a bit steeper that the<br />

longitudinal ones, although the flux measured in the JGOFS study was<br />

similar to that measured north <strong>of</strong> Hawaii, which was supposed to be an<br />

oligotrophic site.<br />

Recolonisation rates<br />

Questions were raised about the idea <strong>of</strong> studying recolonisation<br />

rates by placing trays <strong>of</strong> azoic sediments onto the seabed in a patch where<br />

the native sediment had been removed. One participant thought that might<br />

work for the larger animals but might be misleading for smaller ones such<br />

as the mei<strong>of</strong>auna, because they probably came up from underneath rather<br />

than from outside, even if the trays were placed in the middle <strong>of</strong> a large<br />

patch.<br />

Smith responded that an experiment in which the top few<br />

millimetres <strong>of</strong> sediment were removed along with all the fauna over a large<br />

area <strong>of</strong> perhaps one kilometre in diameter should give a good idea <strong>of</strong><br />

79 INTERNATIONAL SEABED AUTHORITY

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