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A biological study of Durvillaea antarctica (Chamisso) Hariot and D ...

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613<br />

numerous narrow channels. On the Kaikoura coast, particularly<br />

between Oaro <strong>and</strong> the Kahutara River, this t.ype <strong>of</strong> shore is periodically<br />

subjected to the deposition <strong>of</strong> shingle <strong>and</strong> s<strong>and</strong>. \Vhen storms undercut<br />

the road embankment further inshore, loose rna terial is depo S1 'ted<br />

temporarily in the upper sublittoral <strong>and</strong> sublitt.oral fringe,. D.<br />

willana la~minae <strong>and</strong> holdfasts are abraded, until the shingle <strong>and</strong> s<strong>and</strong><br />

is deposited elsewhere. This usually occurs before the plants are<br />

seriously damaged. If the input <strong>of</strong> shingle was more·-or-less<br />

continuous, then I am sure that small D. willana plants would be<br />

unable to become established, <strong>and</strong> that. the holdfasts <strong>of</strong> large plants<br />

l'lOuld be severely damaged.<br />

Intolerance <strong>of</strong> D. willana to shifting deposits <strong>of</strong> shingle <strong>and</strong><br />

s<strong>and</strong> perhaps explains why this species is less common on the<br />

Kaikoura Coast north <strong>of</strong> Kaikoura Peninsula, 'chan on the southern<br />

coast. On the south side, the shore slopes very steeply. Within<br />

1 km <strong>of</strong> the shore the depth is 200 ro. Shingle is quickly washed down<br />

the slope, <strong>and</strong> is only temporarily deposited amongst the D. willana.<br />

North <strong>of</strong> the Peninsula the shore slopes less steeply. Small deposits<br />

<strong>of</strong> loose material are a permanent feature <strong>of</strong> the slLblittoral fringe<br />

<strong>and</strong> upper sublittoral.<br />

(v)<br />

Salinity<br />

In New Zeal<strong>and</strong>, the only areas <strong>of</strong> open rocky coast that are<br />

at least periodically immersed in brackish water «25°~o) occur near<br />

river mouths. Both Du~viZZaea species grow within 0.5 kID <strong>of</strong> the<br />

Kahutara River near Kaikoura. Salinity at the mouth <strong>of</strong> this river<br />

is 22%0 (13 August 1975). Slightly further south (0.8 km) the<br />

salinity ",as only slightly less than normal (32%0). Presu..I"tlably<br />

much lower values would be obtained this distance from the river<br />

mouth ... 1hen the river is in flood. Water samples collected at intervals<br />

over the tidal cycle from amongst D. anta:t'etiaa growing a't the<br />

mouth <strong>of</strong> the Tautuku River (August 1975) shO\\l'ed that the salinity drops<br />

to 7" 4%'() '.\Then the tide recedes, <strong>and</strong> returns to normal shortly after<br />

low wateL At the Nile RiVer, 20 Jan south <strong>of</strong> Cape Foulwind., both<br />

species grm

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