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

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19<br />

The series <strong>of</strong> low ridges absorbs much <strong>of</strong> the force <strong>of</strong> waves, <strong>and</strong><br />

there is a wide spending area inshore <strong>of</strong> the DurlJi llaea beds.<br />

Wave<br />

force was rated as sernisheltered (Fig. 4.1f).<br />

(8) Maroa<br />

Two samples were collected near Akaroaj<br />

one at Gateway Point<br />

below the light near the entrance to the harbour (43°53'30"S, 172°59'10"E)<br />

<strong>and</strong> the other at Wainui 8 kID inside the harbour on the west side<br />

(45°49'50"S, 172°54'25"E).<br />

The kelp b<strong>and</strong> at Gateway Point is on the<br />

steep edge <strong>of</strong> a narrow tide platform which is fully exposed to southerly<br />

storms. Wave force is very strong. Wainui is sernisheltered by<br />

comparison. Barnacles <strong>and</strong> limpets dominate the shore above the D.<br />

<strong>antarctica</strong> b<strong>and</strong> in both areas.<br />

(9) Tautuku Peninsula (46"36'25"5, 169"26'20"E)<br />

The transect on East Rocks (Area 6) was exposed to rough seas<br />

from the northeast.<br />

The East Rocks consist <strong>of</strong> a series <strong>of</strong> ledges,<br />

<strong>and</strong> during strong easterly or southeasterly storms waves are funnelled<br />

along these ledges, thereby approaching Area 6 from above.<br />

The slope<br />

<strong>of</strong> Area 6 is 11° <strong>and</strong> both the D. <strong>antarctica</strong> <strong>and</strong> D. ~llana b<strong>and</strong>s are<br />

several metres wide (Fig. 2.38).<br />

All other belt transects were on First Slope (8-12°) where there<br />

is full exposure to swells from the east, southeast <strong>and</strong> south.<br />

Wave<br />

force decreases across the slope, <strong>and</strong> because there is such a large<br />

spending ground inshore <strong>of</strong> the kelp b<strong>and</strong>s, the impact component <strong>of</strong><br />

waves is weak.<br />

When the sea is rough, large swells crest over the<br />

back <strong>of</strong> First Slope sO that torrents run down the slope towards the<br />

D. <strong>antarctica</strong> b<strong>and</strong>. Wave force on both the East Rocks <strong>and</strong> First<br />

Slope was rated as very strong.<br />

Other samples <strong>of</strong> D. <strong>antarctica</strong> were collected from perpendicular<br />

cliff faces between First <strong>and</strong> Second Slopes. The shore above the<br />

D. <strong>antarctica</strong> is covered by barnacles <strong>and</strong> Apophlaea lyalZii Hook.f. et<br />

Harv. For sea surface temperatures see Appendix 1.<br />

(10) Ringaringa (46"54'30"5, 168"9'36"E)<br />

The transect traversed an uneven rock shore, <strong>and</strong> was similar to<br />

the area at Kean Point.<br />

The Area is protected from southerly <strong>and</strong><br />

southwesterly storms, but is exposed to the southeast <strong>and</strong> east,<br />

although Bench Isl<strong>and</strong>, Native Isl<strong>and</strong> <strong>and</strong> The Neck provide some shelter.<br />

Wave force was rated as moderate. Barnacles, limpets <strong>and</strong> Bostl·ychia<br />

dominate the shore above the D. anta~ctica.

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