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standardization of environmental data and information - International ...

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?? Investigate the plankton community in the upper 200 m;<br />

?? Evaluate bioturbation rates;<br />

?? Obtain <strong>data</strong> on the flux <strong>of</strong> materials from the upper water column<br />

down to the deep sea;<br />

?? Determine the frequency, duration <strong>and</strong> spatial distribution <strong>of</strong><br />

baseline monitoring.<br />

5. Environmental characterisation <strong>of</strong> claim areas<br />

Two regions in the deep seabed currently have exploration claims<br />

registered with ISA. First, the Government <strong>of</strong> India has claimed an area in<br />

the south central Indian Ocean between 10-17° south latitude <strong>and</strong> 72-82°<br />

east longitude. Second, six States <strong>and</strong> an intergovernmental group (China,<br />

France, India, Japan, Republic <strong>of</strong> Korea, Russian Federation <strong>and</strong> an Eastern<br />

European group) have claims in the northeastern tropical Pacific Ocean (the<br />

CCFZ) between 7-18° N <strong>and</strong> 157-118° west longitude (see figure 2).<br />

This section summarises the <strong>environmental</strong> baseline <strong>information</strong><br />

presented in Morgan, Odunton <strong>and</strong> Jones. 12 It outlines the <strong>environmental</strong><br />

<strong>information</strong> available for the claim areas <strong>and</strong> focuses on general<br />

parameters relevant to <strong>environmental</strong> impact assessment.<br />

5.1. Occurrence <strong>of</strong> commercial nodule deposits<br />

Manganese nodules form along gradients <strong>of</strong> ambient water<br />

chemistry in which waters traverse from relatively acidic <strong>and</strong> low oxygen<br />

levels into relatively high levels (see section 3.1 above). Acidic, poorly<br />

oxygenated waters can contain significant amounts <strong>of</strong> dissolved <strong>and</strong><br />

organically complexed metals. Where these waters pick up oxygen <strong>and</strong><br />

usually at the same time lose some acidity, many metals will rapidly oxidise<br />

<strong>and</strong> precipitate out. This situation commonly occurs at the water/sediment<br />

interface in lakes <strong>and</strong> oceans, which is where manganese nodules are<br />

usually found. Iron <strong>and</strong> manganese are the most common transition metals<br />

in the earth’s crust, <strong>and</strong> thus form the bulk <strong>of</strong> the precipitated material.<br />

Manganese oxides also have special surfaces that are particularly effective<br />

in collecting <strong>and</strong> holding more manganese <strong>and</strong> other metals, scavenging<br />

them preferentially from the bypassing water flow.<br />

INTERNATIONAL SEABED AUTHORITY 112

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