The Kermadec Islands Marine Reserve (29 to 31°S), New Zealand, harbours one of the world's highest latitude scleractinian coral communities, situated close to the lower thermal limits for coral survival. An understanding of how and why similarities and differences exist between so-called 'marginal' coral communities can provide insight into the physical and biological factors that influence coral distributions. In this study, a depth-stratified survey of benthic community structure and coral species assemblages was conducted at 9 sites around the Kermadec Islands. All coral species identified were subtropical non-reef building species, or species with a wide geographic range. Scleractinian coral cover (16 species) was low and variable between sites and depths (5.3 ± 13.9%, mean ± SD) with macroalgae contributing between 36 to 95% of the benthic cover. Multivariate analyses revealed small-scale spatial variability between closely located sites. Resulting data on coral species diversity were compared to published data from coral communities at other 'marginal' locations, as well as those from a range of Australian locations. On a global scale, the Kermadec Islands coral community exhibits greatest affinity with southeastern Australian sites. In comparison, there was a lack of affinity for Australian tropical sites and other high latitude sites, both in Australia and globally. Our analyses suggest that the low diversity, highly variable coral communities of the Kermadec Islands are likely shaped by their isolation and high wave energy, in addition to the low annual temperatures experienced.KEY WORDS: High latitude · Coral community · Kermadec Islands · Regional affinities · Subtropical · New Zealand
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 400: [101][102][103][104][105][106][107][108][109][110][111][112][113] 2010 Marginal reefs and communities frequently occur at high latitudes (subtropics) i.e. above 25°S and 25°N, with well known examples being those of the Persian Gulf, Bermuda, Japan and Lord Howe Island, Australia. Development and coral species diversity of these high-latitude assemblages, at both biogeographic and local scales, are largely regulated by low mean annual and seasonally variable temperatures and irradiances, and the low aragonite saturation state (Buddemeier 1997, Kleypas et al. 1999). Other parameters with local importance include wave exposure (Harriott et al. 1994, Benzoni et al. 2003, Nozawa et al. 2008, low and variable salinity and high turbidity (Harriott & Smith 2002, Manzello & Lirman 2003. Macroalgae play a dominant role in many of these high latitude coral assemblages, their rapid growth out-competing corals for space (Johannes et al. 1983). Further, many high latitude coral assemblages are small and isolated (e.g. Babcock et al. 1986, Brook 1999, Hughes et al. 2002, meaning that they are likely to be largely self-seeding in terms of larval supply (Ayre et al. 1997).Patterns of diversity and distribution in high latit...