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

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91<br />

the huge populations <strong>of</strong> large limpets, It is hardly surprising<br />

that DurviZZaea has not become established on cold or warm temperate<br />

south African shores,<br />

(e) The absence <strong>of</strong> D. <strong>antarctica</strong> from Tristan da cunha L:<br />

There is no DurviZlaea on Tristan da Cunha, but xli: grows<br />

abundantly on Gough X, 370 krn to the southeast. Chamberlain (1965:<br />

178) sta.ted that algal zonation on Gough L is typical <strong>of</strong> the subantarctic<br />

pattern, whereas that <strong>of</strong> Tristan da Cunha has more in<br />

common wlth South African shores. This she claimed corresponded with<br />

the fact that Gough I. is well south <strong>of</strong> the Subtropical Convergence<br />

whereas Tristan is near its mean position. I do not consider that<br />

this, in itself, is an adequate explanation for the floristic<br />

difference between the two isl<strong>and</strong>s. The Chatham Is also straddle<br />

ll:he Subtropical Convergence, <strong>and</strong> two DurviUaea species grow there<br />

in abundance. The nearest popUlation <strong>of</strong> DuTviZZaea to the Chatham<br />

Is is much further away t.han the distance between Tristan <strong>and</strong> Gough<br />

Isl<strong>and</strong>s. As mentioned earlier, differences in sea temperatures can<br />

<strong>of</strong>fer no simpl~ explanation. Although Tristan is warmer than Gough,<br />

temperatures there are still lower than in other places Nhere<br />

DurvilZaea grows.<br />

Doth isl<strong>and</strong>s are partly under the influence <strong>of</strong> the Cape Horn<br />

<strong>and</strong> Falkl<strong>and</strong> Isl<strong>and</strong> CUrrents. Baardseth (1941:157) calculated that<br />

the Cape Horn Current would carry "drifting matters" across the<br />

South Atlantic to reach Tristan in 120 days. It is unlikely that<br />

the absence <strong>of</strong> Du:t"ViUaea on '}~ristan<br />

<strong>of</strong> ocean currents 0<br />

can be attributed to the pattern<br />

Laminaria paZlida grows on Tristan da Cunha but is absent from<br />

Gough Isl<strong>and</strong>. On Tristan this alga extends up into the narrow<br />

littoral region (1.05 m between neaps) to about MLWN. One can but<br />

speculate as to ~lhether this larninarian prevents D, <strong>antarctica</strong> from<br />

becoming esteblished. Nowhere do the two kelps grm., together.<br />

(f)<br />

Isl<strong>and</strong>s:<br />

Delepine (1963) suggested that the alga is absent because these<br />

isl<strong>and</strong>s lie north <strong>of</strong> the Subb::opical Convergence. As mentioned<br />

earlier I I do not th ink that this alone is an adequate explanation,<br />

rt is perhaps significcmt: that Laminaria pall'ida grovls on l:hese

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