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Minerals Report - International Seabed Authority

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deep seafloor. Another tool used was to determine if there were elevated<br />

levels of metal particles in the normal deep-sea sediments. Thus is because<br />

the metal particles coming out of the black smokers would also be carried out<br />

by the currents over great distances and would settle on the deep-sea<br />

sediments. By following concentration gradients of these metals in the water<br />

column and in the sediments on the seafloor, Professor Rona stated that his<br />

team felt that it would progressively get close to the possible source of these<br />

materials.<br />

Using slides, Professor Rona took participants on a tour of the<br />

exploration work that was conducted. There were images of the dives by the<br />

submersible Alvin, the production of bathymetric contour maps using satellite<br />

navigation, discovery of the target deposit, photographs of the deposit,<br />

sampling of the deposit, identification of new life forms and drilling the<br />

deposit to enable its volume to be determined.<br />

With regard to some of the technologies used, Dr. Rona presented<br />

participants with images of, inter alia, the water sampling bottle used to<br />

ascertain if there were elevated levels of certain metals in the water column, a<br />

sediment core showing dark layers of sediment containing enriched metals in<br />

the sediment, the echo sounder(s) used to determine the depth and shape of<br />

the seafloor, how satellite navigation is used to give positioned accuracy and<br />

how instruments aboard the Alvin submersible were used to make various<br />

measurements like temperature, to sample and to drill the deposit.<br />

Professor Rona presented some slides of the TAG hydrothermal field<br />

showing the broad array of biodiversity that is to be found in association with<br />

the massive sulphides deposit. Starting in normal seafloor around the<br />

mound, lava flowed normally and deep sea sediments were shown looking<br />

very much like a desert. Suddenly, the colour oasis of the mound came into<br />

view, followed by the hot springs themselves. There were bright green rocks<br />

(massive sulphides) and different types of fish. There were also chimneys up<br />

to several metres high that are no longer active. Closer to the mound were<br />

dome shaped chimneys, several metres high that were discharging blue-white<br />

smoke. These are the white smokers made up primarily of iron sulphides<br />

(pyrite). Professor Rona informed participants that because these dome<br />

shaped chimneys reminded his team of the domes on Old Russian churches<br />

INTERNATIONAL SEABED AUTHORITY 101

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