Nutrient concentrations and primary productivity at the Peros Banhos and Salomon atolls in the Chagos Archipelago

Coral atolls are areas of high biological productivity even though they are usually located in regions of the tropical ocean characterized by low primary production and extremely low levels of vital dissolved nutrient materials. Recent studies have indicated the possible importance of in situ dinitrogen fixation on shallow reef flats in supplementing low oceanic nitrate levels and thus contributing to the maintenance of high reef productivity. Variations in the structure of atolls may have a direct bearing on the accumulation of fixed nitrogen and other nutrient materials, and consequently on lagoonal and reefal primary productivity. This paper investigates the effect of differing atoll configurations by comparing neighbouring, but structurally dissimilar, mid-ocean atolls. The findings are discussed in terms of ecosystem function and possible influences on the structural evolution of atolls.     

Utility of the Hadley Centre sea ice and sea surface temperature data set (HadISST1) in two widely contrasting coral reef areas

The HadISST1 sea surface temperature data set is examined for two contrasting areas: the Chagos Archipelago, central Indian Ocean which has a small (approximately 3 degrees C) annual temperature fluctuation, and Abu Dhabi in the southern Arabian Gulf whose annual air temperature fluctuation of approximately 24 degrees C is the largest known for coral reef habitats. The HadISST1 data are shown to match air temperature records closely, both in terms of annual moving averages and residual analysis. Temperatures in 1998 caused massive mortality of corals in the Indian Ocean: sea surface temperature (SST) values causing this were 33.8 degrees C in the Arabian Gulf at a time when average daily air temperature was over 40 degrees C, while in Chagos the SST lethal to corals was 29.8-29.9 degrees C, when air temperatures peaked at about 31 degrees C. The HadISST1 record was searched back to 1870 for previous abnormal peaks: one of 29.7 degrees C was found for Chagos SST in 1972, though this did not cause coral mortality. Analysis of 12-month running means of the residuals from the annual cycle show that, between 1870 and 1999, the largest SST deviations occurred between October 1997 and May 1998 in Chagos and between August 1998 and July 1999 near Abu Dhabi. The event of 1998-1999 was the largest in these regions for at least 130 years. SSTs have risen over the last three decades at rates of about 0.22 degrees or 0.23 degrees per decade in both locations.     

Response to the article by Peter Harris: Fortress,safe haven or home? The Chagos MPA in political context

I welcome the contribution by Harris to the ongoing debates around the Chagos Islands. He presents the complex tangle of issues with some clarity and relative balance that is often absent from many contributions on this subject.However, marrying scientific and political issues as Harris sets out to do is less helpful in this instance than distinguishing between the two. Blurring these boundaries can risk the future of the Chagos Marine Preservation Area (MPA) and the invaluable protection it affords the many species (including important food species) now thriving in the Chagos Archipelago. CCT works to study and protect this unique environment, and we would like to make some important distinctions clear.     

Fortress conservation at sea: A commentary on the Chagos marine protected area

The world's largest no-take Marine Protected Area in Chagos is examined in light of the Convention on Biological Diversity's provisions on Access and Benefit Sharing, as well as terrestrial experiences with fortress conservation. It is acknowledged that this closure presents a unique opportunity to preserve an ecologically 'pristine' area. However, the means by which the political process unfolded are brought into question. In particular, the fact that the UK proceeded with designating the area whilst the European Court of Human Rights was deliberating the right of native Chagossians to return to the island is questioned. In addition it is argued that the scale of the area poses significant management and enforcement challenges, which are not necessarily taken into consideration in the rush for large, no-take Marine Protected Areas.     

Pre- and post-1998 ENSO records of shallow-water octocorals (Alcyonacea) in the Chagos Archipelago

When compared, principal octocorals collected in the Chagos Archipelago before and after the 1998 ENSO shared many common taxa. While a few discontinuities in their biodiversity revealed subtle changes in more persistent genera (Lobophytum, Sarcophyton), some fast-growing “fugitive” genera (e.g. Cespitularia, Efflatounaria, Heteroxenia) disappeared after the ENSO-related coral bleaching. Such transient fugitives might thus be eliminated from soft coral communities on isolated reef systems, possibly in the long term, by events of this nature. The appearance of Carijoa riseii, a species often considered a fouling organism, even an invasive, may well be indicative of reef degradation during the ENSO event. The post-ENSO recovery manifested by this fauna nevertheless gives cause for hope for their survival in the face of climate change.