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

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15S<br />

<strong>of</strong> the Ohau but these were easily identified, <strong>and</strong><br />

could be excluded from calculations.<br />

Mortalities <strong>of</strong> the smallest. <strong>and</strong> size<br />

tha·t <strong>of</strong> the entire at Ohau Point are illustrated in 1.<br />

<strong>and</strong> may be with the data from Tautuku 7.14) • l:-.t<br />

Tautuku, the three curves in were t the<br />

size I the smallest then the entire<br />

AtOhau<br />

the<br />

again the mortality rate <strong>of</strong> the<br />

size class was less than that measured for the entire<br />

The reason for this difference can be seen in Fig 7.19. Instead<br />

<strong>of</strong> a "u" shaped curVe, the at ohau Point was for<br />

mortality rate to increase with size. Therefore, medium sized<br />

plants at Ohau Point had a<br />

ra'ce than small plants"<br />

Data Ohau Point were less useful than Tautuku data for<br />

stUdying seasonal fluctuations in mortality. Persistent easterly<br />

<strong>and</strong> the fact that censusing was<br />

to<br />

spring tides, meant that censuses at Ohau Point were more<br />

<strong>and</strong> less frequent than at Tautuku. More however, was<br />

the fact that the composition <strong>of</strong> the Ohau sample changed<br />

throughout the course <strong>of</strong> the <strong>study</strong>.<br />

This was because marked plants at Ohau Point grew in a<br />

<strong>of</strong> wave exposures, Mortality was highest in areas where wave<br />

was <strong>and</strong> the sample was I with time, domina ted<br />

by growing in semisheltered positions such as on the lee<br />

side <strong>of</strong> boulders. The obtained at Ohau Point<br />

(Table 7.6) therefol':"e<br />

the overall mortality<br />

<strong>of</strong> D. antarotiaa in that coastal area. This trend did not occur on<br />

First at Tautuku, because "tIl the marked plants \'lere exposed<br />

to much the same degree <strong>of</strong> wave force.<br />

There was less fluctuation between summer <strong>and</strong> winter mortalities<br />

a.t Ohau than at Tautuku. Mortality at Ohau Point was also<br />

highest<br />

during<br />

(Table 7.7).<br />

summer (Table 7.6). <strong>and</strong> not, as was the case at Tautuku,<br />

was caused a<br />

<strong>of</strong> small<br />

late <strong>and</strong> summer<br />

During the 1972-73 summer for<br />

e~.amp~e,<br />

58% <strong>of</strong> the<br />

lost at Ohau Point were shorter .ti1an 0.75 m; whereas the<br />

autumn <strong>and</strong> , plants this<br />

only 36%<br />

total<br />

on the other exhibited a

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