Biology Reference
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distributed in the sub-Antarctic islands (Clayton 1994 ). These regions share a
considerable number of cold-temperate species, e.g., the brown alga Adenocystis
utricularis , the red alga Iridaea cordata and Gigartina skottsbergii , however, some
endemic Antarctic species such as Himantothallus grandifolius and Ascoseira
mirabilis do not inhabit the sub-Antarctic islands (Luning 1990 ; Clayton 1994 ).
The distribution of the endemic Antarctic rhodophyte Palmaria decipiens just
extends to Macquarie Island (Wiencke and Clayton 2002 ). On the other hand, the
circumpolar kelps Macrocystis pyrifera and Lessonia spp . as well as the large
intertidal fucoid Durvillaea antarctica are absent from the Antarctic (John et al.
1994 ; Clayton et al. 1997 ).
The general zonation pattern for the shores of Macquarie Island has been
described to comprise an upper littoral Porphyra zone, a “bare” zone (dominated
by siphonariid mollusc Kerguelenella lateralis ), an upper red algal zone
( Rhodymenia sp., Chaetangium fastigiatum , Palmaria georgica , Acrosiphonia
pacifica , Porphyra columbina ), a kelp zone ( Durvillaea antarctica ), and lower red
algal zone below the infralittoral with understory species such as Delesseria spp.,
Iridaea sp., and Desmarestia sp. (Kenny and Haysom 1962 ; Smith and Simpson
2002 ). Similarly, in Marion Island, D. antarctica is the dominant species at the
infralittoral fringe, while Desmarestia rossii and Durvillaea sp. occur in a zone of
3-6m. Encrusting coralline algae are particularly abundant in shallow areas (Beckley
and Branch 1992 ). At subtidal locations, beds of the endemic Macrocystis laevis are
abundant (Perissinotto and McQuaid 1992 ; Beckley and Branch 1992 ). In general,
infralittoral D. antarctica , shallow-water encrusting coralline algae, Desmarestia
spp., and subtidal Macrocystis beds seem to overall characterize the benthic seaweed
communities in many sub-Antarctic islands (Beckley and Branch 1992 ).
For the sub-Antarctic islands near New Zealand, 14-148 seaweed species have
been reported, with the highest species richness being recorded for Chatham Islands
and the lowest for the Bounty Island (Parsons 1985 ). Although notable differences
in species composition and dominance patterns can exist among islands (Freeman
et al. 2011 ), Durvillaea antarctica and Macrocystis pyrifera occur in all these island
groups, Lessonia flavicans reported for Auckland, Campbell, the Antipodes, and
Bounty. The fucalean Xiphophora chondrophylla is present in all the island groups,
except for the Bounty (L
uning 1990 ). Endemic Durvillaea species have been
proposed for the Antipodes (undescribed species) and Chatham Island ( D.
chathamensis ) (Cheshire et al. 1995 ; Fraser et al. 2010b ; Fig. 14.3 ). In the light of
a re-examination of the description of Porphyra columbina using molecular
techniques, this species is distributed in the Auckland, Campbell, Antipodes,
Chatham, and Falkland Islands, with a very restricted distribution in mainland
New Zealand (Nelson and Broom 2010 ).
In the Chatham Island, the shallowest subtidal areas are dominated by Durvillaea .
Several fucalean species (e.g., Xiphophora chondrophylla , Carpophyllum
plumosum and C. maschalocarpum ) are abundant to a depth of around 10 m, C.
flexuosum occurring mostly in deeper waters (9-20 m). The endemic Lessonia
tholiformis and L. variegata are abundant at 2.5-15 m depth. In some sites,
Macrocystis pyrifera forms dense beds at 15-20 m depth. In the Auckland Islands,
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