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

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

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216<br />

half <strong>of</strong> ·the s uprali ttoral fringe, together wi t.h the 1l.lidli ttoral <strong>and</strong><br />

the sublittoral fringe comprised the littoraL The sublittoral zone<br />

was belo"! ELWS; the sublittoral fringe I-Jas that part <strong>of</strong> the littoral<br />

exposed only by the lowest tides <strong>and</strong> during the suck-back <strong>of</strong> waves.<br />

They claimed that on most temperate <strong>and</strong> cold water coas<br />

the \-Jorld thesubli'ctoral fringe \vas essentially a zone <strong>of</strong> large brohln<br />

algae: usually laminarians <strong>and</strong> fucoids,<br />

Womersley <strong>and</strong> Edmonds (1952) ammended the Stephenson's schel'rte<br />

because they found i:hat zonation on some south Australian shores did<br />

not fit in/co it na turall y . They proposed tha t the term Ii ttoral be<br />

restricted to the region between the upper limit <strong>of</strong> barnacles <strong>and</strong><br />

MLWN; i.e, the region which the StephensonS called the midlittoral<br />

zone. 'I'hey divided the litt.oral into upper I mid <strong>and</strong> low, <strong>and</strong>,<br />

restricted the term sublittoral fringe only to localities where there<br />

was a true fringing zone <strong>of</strong> algae or ani.mals not extending below<br />

ELWS. In the absence <strong>of</strong> any true fringing species they deemed it<br />

better to proceed directly from the littoral zone into the upper<br />

s ubI ittoral.<br />

As mentioned in Chapter 4, D. <strong>antarctica</strong> extends vertically from<br />

about MLWS to a level (depending on wave force) between highest LWN<br />

<strong>and</strong> MSL. It does not fit neatly into either <strong>of</strong> che two schemes<br />

described above because it occupies the upper hnlf <strong>of</strong> the sublittoral<br />

fringe <strong>and</strong> all or part <strong>of</strong> the 10Vl littoraL D. liJillana extends<br />

downwards from MLWS to approximately two metres below ELWS. Because<br />

only the upper part <strong>of</strong> the D. wiZlcma b<strong>and</strong> would come IIlithin the<br />

Stephensons sublittoral fringe it cannot be regarded as a true<br />

fringing species. Its distribution fits more naturally into<br />

Womersley <strong>and</strong> Edmond's upper sublittoral zone.<br />

D. potatoPUm <strong>and</strong> Do chathamica, on the other h<strong>and</strong>, are true<br />

fringing species, occupying the sublittoral fringe 0<br />

In general, the zonation <strong>of</strong> JJu:pvilZaea spp. fits more naturally<br />

into the scheme proposed by Womersley <strong>and</strong> Edmonds, them into t.he<br />

less flexible universal scheme proposed earlier by the Stephensons,<br />

10.3<br />

Even from the earliest developmental stages it is possible to<br />

distinguish between young D. antaX'ctica <strong>and</strong> D. wi Zlana , Cl.lthongh as<br />

has been shown (Chapter 5), both species demonstrate a high degree <strong>of</strong><br />

phenotypic varia"tion attributable in large part to the same causi tive<br />

iigents.<br />

Morphological variation is mostly independent <strong>of</strong> age, but

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