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Ranfurly Bank<br />

Map ID number:<br />

10<br />

Locati<strong>on</strong>: Ranfurly Bank is<br />

located <strong>on</strong> <strong>the</strong> c<strong>on</strong>tinental<br />

shelf, 17km east-north-east <strong>of</strong><br />

East Cape.<br />

Approximate area: 17,437km 2<br />

Descripti<strong>on</strong> <strong>of</strong> area:<br />

The Bank rises from about 130m depth to a<br />

minimum <strong>of</strong> 25m and is ba<strong>the</strong>d by <strong>the</strong> East<br />

Cape Current as it sweeps around <strong>the</strong> cape<br />

<strong>on</strong> its southward passage al<strong>on</strong>g <strong>the</strong> North<br />

Island margin. This st<strong>on</strong>g flow, toge<strong>the</strong>r with<br />

<strong>the</strong> tides, is liable to inhibit accumulati<strong>on</strong> <strong>of</strong><br />

muddy sediment discharged from <strong>the</strong> nearby<br />

Waiapu River – by far New Zealand’s largest<br />

river in terms <strong>of</strong> sediment discharge (Li<strong>on</strong>el<br />

Carter, pers<strong>on</strong>al communicati<strong>on</strong> 2004).<br />

Biological attributes:<br />

Sampling undertaken so far has revealed<br />

unusual/unexpected distributi<strong>on</strong>s.<br />

Observati<strong>on</strong>s <strong>of</strong> this area indicate that <strong>the</strong>re<br />

are endemic species <strong>of</strong> algae. For example,<br />

Adamsiella lorata is known <strong>on</strong>ly from Lottin<br />

Point and A. melchior is known <strong>on</strong>ly from<br />

<strong>the</strong> Three Kings Islands.<br />

Criteria applied:<br />

Endemism.<br />

Status and management:<br />

Not recorded during <strong>the</strong> workshop<br />

State <strong>of</strong> informati<strong>on</strong>:<br />

Collecti<strong>on</strong>s that have been made to date are<br />

few. The area warrants closer attenti<strong>on</strong> and a<br />

well-structured sampling programme.<br />

References and fur<strong>the</strong>r reading:<br />

Phillips (2002).<br />

C<strong>on</strong>vergent margin<br />

cold seeps<br />

Map ID number:<br />

11<br />

Locati<strong>on</strong>: C<strong>on</strong>vergent margin<br />

cold seeps are found <strong>on</strong><br />

<strong>the</strong> East Coast <strong>of</strong> <strong>the</strong> North<br />

Island and <strong>the</strong> sou<strong>the</strong>ast and<br />

southwest coasts <strong>of</strong> <strong>the</strong> South<br />

Island.<br />

Approximate area: Not<br />

precisely known. Probably<br />

less than 300km 2 in total<br />

aerial extent for all 13 known<br />

sites. (Area 11 <strong>on</strong> <strong>the</strong> map is<br />

6,534km 2 )<br />

Descripti<strong>on</strong> <strong>of</strong> area:<br />

Cold seeps are methanogenic and<br />

methylotrophic ecosystems. In buried sea<br />

floor sediments, <strong>org</strong>anic compounds derived<br />

from marine life are chemically altered by<br />

heat, pressure, and bacteria. The compounds<br />

percolate upwards through <strong>the</strong> sediments to<br />

be released as <strong>org</strong>anic-enriched fluids and<br />

gases, e.g. methane.<br />

Biological attributes:<br />

Methane-rich seeps are home to siboglinid<br />

tubeworms and highly adapted suspensi<strong>on</strong>feeding<br />

bivalves, most <strong>of</strong> which are endemic.<br />

Criteria applied:<br />

Endemism; trophic distinctiveness;<br />

adaptati<strong>on</strong> to extreme envir<strong>on</strong>ment; special<br />

c<strong>on</strong>diti<strong>on</strong>s and special <strong>org</strong>anisms.<br />

Status and management:<br />

Not managed.<br />

State <strong>of</strong> informati<strong>on</strong>:<br />

Only <strong>the</strong> following paper has been published<br />

<strong>on</strong> New Zealand c<strong>on</strong>vergent-margin seeps.<br />

References and fur<strong>the</strong>r reading:<br />

Lewis and Marshall (1996).<br />

56 ■ BIODIVERSITY – NEW ZEALAND’S MARINE ECOREGION

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