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The Great Astrolabe Reef Lagoon (Fiji)

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l1........' ",,;0,.,­_._ ----­• 'Ii il .,.." n .... p ....... lh .... ....a- .• .. ....... _. • 7 ...... ".... 11 .ul ; U • • l'e')'ntl;~ r""lçaiu ft• \I\JC\~i(/ \ 1 L'Institut français de recherche scientifique pour le développement en coopération ~'IUlrp~' I ..oï.·_ ~ 'hnrl)~'·nollbnud ~'Inlld(·_ :'\.·"'.·11 l'.·,,·,· Tlu· G......t .\st..ohabe R.·.·f I~..gooll .t"iji. : R.·su1ts of th.· F.-.·n(·h.•'ijian ~\STRO .·xp.·.lition OCEANOGRAPH 1E Notes et documents ne 46 1996 Centre ORSrOM de Tahiti Polynésie Française OCÉANOGRAPHIE Notcs et docunlcnts nO 46 1996 ISSN-0755-3412 General introduction L. Charpy. Phytoplankton biomass andproductivity in The Great Astrolabe Lagoon ,.. ,. , p.l L. Charpy, N. Harrison and M. Maata. Nutrients and Particulate organic matter in The Great Astrolabe ReefLagoon p.5 C. Chevillon, G. Yeo and A. Di Matteo. Sedirnent constituents in the Great Astrolabe Reeflagoon (Fiji) , p.ll J. Clavier, P. Newell, C. Garrigue, B. Richer de Forges and A. Di Matteo. Soft substrate macrobenthos ofFiji's Great Astrolabe Reeflagoon. List of taxons, densifies and their biomass p.17 G. Boucher and J. Kotta. Composition et diversité de la méiofaune du lagon de « Great Astrolabe Reef» (Fiji). , p. 47 C. Charpy-Roubaud. Microphytobenthic biomass andproduction ofthe Great Astrolabe Reeflagoon sediments , , p.53 G. Sarazin and C. Charpy-Roubaud. Some main processes oforganic matter mineralization and marientflu.xes at the sediment-water interface in the Great Astrolabe lagoon (Fiji) p.60 J. Blanchot. Report ofpicophytoplankton study during the astro cruise ln the Great Astrolabe Reef(18°45 '8-178°30 'E) Fiji p.69 J.-P. Torréton. Biomass, production and heterotrophic activity of bacterioplankton in the Great Astrolabe ReefLagoon p.78 C. Charpy-Roubaud, G. Sarazin and R. Buscail. Organic carbon, nitrogen andphosphorus in the Great Astrolabe Reeflagoon sediments. Preliminary results p. 91 Centre OR8TOM de Ta hiti BP 529 - Papeete (Polynésie Française) Genera/Introduction Notes et Doc Océanogr. J996, 46 General introduction Tbis work was carried out in Fiji as part of the (Figure 1). The Astrolabe Islands are a group of international cooperation in marine biology between volcanie islands 3.3 to 3.5 million years old France and Fiji. This cooperation was initiated in (Howorth & Carman, 1992). The climate is humid 1991 between the Tahiti ORSTOM Center and the tropical with an average temperature of 25"C and Institute of Marine Resources (The University of rainfall of 2596 mm. Prevailing winds are from the South Pacifie, Suva). south cast. There are 13 islands, 4 of which 4 are In 1988, a Marine Pollution Research Group was inhabited (l000 inhabitants). Fish is the major forrned at USP to coordinate the work in this field at source of protein for the villagers in the group the University. The group decided to carry out a (Naqasima et al., 1992). 2 baseline study of the Astrolabe lagoon and reef. The 'Ibe lagoon surface area is approximately 210 km . development of Dravuni as an important center for The maximum depth is about 37.5m and the average reef and lagoon research, attracting scientists from depth is 20m (Naqasima et al., 1992). The residence around the world was also envisaged (Morrison & time for the Astrolabe lagoon was estimated 15-25 Naqasima, 1992). days in tirst approximation by MacLeod (1992). In 1991, the ORSTOM CYEL program in French Preliminary results on marine biology, water quality, Polynesian atolls began, with the object of creating a shellfish quality and sediments were published by models for the operating system of atoll lagoons. Naqasima & Sandy (1992), Morrison & Maata Contacts were made between US? and ORSTOM (1992), Morrison et al. (1992), Morrison & Naidu scientists and the site of the Great Astrolabe Reef (1992). lagoon was choosen for a join study. A preliminary expedition was donc in 1993 and a proposaI Thirteen scientists have studied the GAR lagoon in (ASTRO) was drawn up to complete the baseline May 1994 (Table 1). study of the Great Astrolabe Reef lagoon and to A part of them was based in the field research compare the GAR lagoon with French Polynesian station of Dravuni Island with the support of the lagoons. USP APHAREUS research vessel ship and the The description of the Great Astrolabe Reef and others in the üRSTOM ALiS research vessel ship. lagoon appears in Morrison & Naqasima (1992) : This volume presents 10 papers redacted by 16 The Great Astrolabe Reef (I8°45'S, 178°30'E) is scientists from 9 institutes (Table 1) situated north-cast of Kadavu and south of Viti Levu IS(r. ! 15'5- FIJI /YASAWA ,1' 17Cl5- , ,1:1 Q pKORO OVALAU ~ LEVIJKA • <;JNAIRAI IBOS SUVA D8EQA iJ.VATIJ~LELEltl <;]MOALA GREA T ASTROLABE . REEF AND LAGOON ONQ ~ KABARAO.- '.' KAOAVU 1 D 1 ~ 4 1 1 178'E 179'E 180' 179'W «'igure 1 : Location of Great Astrolabe Reef General Introduction. Notes et Doc. Océanogr. 1996. 46 Table 1: List of the participants in the ASTRO expedition and authors ofthis ,'olume Name Institute ~peciàlt)t Blanchot 1. ORSTOM Nouméa ASTRO Picoplankton Boucher G. MNHNParis Meiofauna Buscail R. Univ. de Perpignan Geochimist Charpy L.* üRSTOM Tahiti ASTRO Primary production Charpy-Roubaud C** ORSTOM Tahiti ASTRO Microphytobenthos Clavier J. ORSTOM Brest ASTRO Zoobenthos Di Matteo A. üRSTOM Nouméa Zoobenthos Garrigue C. o ORSTOM Nouméa Phytobenthos Harrison N. USP (Fiji) ASTRO Chemistry Kotta J. t-.1NHN Paris Meiofauna Lo L. EVAAM Tahiti ASTRO Chemistry Maata M. USP (Fiji) AS'fRO Chemistry Maihota N. üRSTOM Tahiti ASTRO Diver Manuelli F. USP (Fiji) ASTRO Diver Newel P. USP (Fiji) ASTRO Zoobenthos Richer de Forges B. üRSTOM Nouméa Zoobenthos Sarazin G. Univ. Paris VII ASTRO Geochemistry Torreton J.-P. üRSTOM Tahiti ASTRO Bacteria YeoG. o USP (Fiji) ASTRO Sediments '" Expedition leader for the water column study u Expedition leader for the benthos study Funding support was provided by the French MacLeod B. (1992). Hydrodynamics, in' Morrison RJ, Embassy in Suva, the üRSTüM program CYEL Naqa<;ima M.R. (eds) Fiji 's Great Astrolabe Reel and Lagoon. A baseline sudy. Environment31 Sudies Report 56: (Tahiti), the ORSTOM program FLUPAC (New 17-22 Caledonia), the IMR (Suva), the Schoal of Pure and Morrison R.J, Gangaiya P., Naqasima M.R. (1992). Shellfish Applied Science (USP, Suva) and the University of quality. in: Morrison RJ., Naqasima M.R. (cds). Fiji 's Great Paris VII. Astrolabe Reel and Lagoon: A baseline sudy. Environmenlal Sudies Report 56: 135-138. Morrison RJ., l.avelawa F., Naqasima M.R. (1992). General ACKNOWLEDGMENTS features of the Astrolabe Lagoon. in: Morrison RJ., Naqasima M.R. (eds). Fiji's Great Astrolabe Reel and We thank Pr. R. South, who initiated of the French­ Lagoon: A. baseline sudy. Environmental Sudies Report 56: Fijian cooperation, M. Bourelon who \vas in charge 5-16. Morrison RJ., Maata M., Aalbersberg W., Koshy K., Harrison of Regional Cooperation at the French Embassy and N.L, Peter W., Vuki M., Fuavao V.A., Naidu S., Dixon W. M. 1.-A. Costilhes, French Ambassador in Fiji and (1992). Water quality. in: Morrison RJ., Naqasima M.R. M. Boccas, Director ofthe Tahiti üRSTüM Center. (eds), Fiji 's Great Astrolabe Ree/ and Lagoon: A baseli/le sudy. Environmental Sudies Report 56: 117-134. We al 50 thank the crews of the research vessels Morrison RJ., Naidu R. (1992). Sediments. Chemistey and mineralogy. in: Morrison RJ" Naqa<;ima M.R. (eds). Fiji 's ALIS and APHAREUS for their kind and efficient Great Astrolabe Reef and Lagoon: A baseline sudy. help on board, the leader of the Dravuni field Environmenlal Sudies Report 56: 139-150. Station. Morrison RJ., Naqa<;ima M.R. (1992). Fiji's Great Astrolabe Reef and Lagoon: A baseline sudy. Environmental Sudies We also thank very waJmly the traditional Report 56: 150pp. landowners of Dravuni Island for allowing us to Morrison RJ., Naqasima M.R. (1992). General introduction. in: Morrison RJ., Naqasima M.R, (eds). Fiji's Great Astrolabe work in the lagoon and aIl the lnhabitants of the Reel and Lagoon: A baseline sudy. Environmentai Sudies Island for their kind welcome. Report 56: 1-3 Naqasima M.R., Bandy M. (1992). Marine Biology. in: Morrison References RJ., Naqasima M.R (eds). Fiji's Great Astrolabe Reeland Lagoon: A baseline sudy. Environmental Sudies Report 56: 65-116. Haworth R., Carman G. (1992). Geology of the Astrolabe Nunn P.D. (1992). Geomorphology. in: Morrison RJ., Naqasima Islands. in: Morrison RJ., Naqasima M.R. (cds). Fiji's Great M.R. (eds). Fiji 's Great Astrolabe Reef and Lagoon: A Astrolabe Reeland Lagoon: A baseline sudy. Environmental baseline sudy. Environmental Sudies Report 56: 47-64. Sudies Report 56: 2J-46 Phytop/ankton production ofthe GA R /agoon Notes et Doc Océanogr /996, 46.' /-4 Phytoplankton biomass and productivity in The Great Astrolabe Lagoon by Loïc Charpy ORSTOM, Centre d'Océanologie de Marseille, traverse de la Batterie des Lions, F-13007 Marseille, France. Abstract LI-COR solarimeter. Following incubation, bottles were filtered through 3 Ilm Nuclepore filters ; Phytoplankton biomass and productivity of the pressure heads during fractionation never exceeded Great Astrolabe Reef lagoon were studied using 0.004 atm. The filtrates were immediately refiltered measurements of chlorophyll concentration and onto 1 Ilm Nuclepore filters and then onto 25 mm carbon uptake. Average chlorophyll concentration Whatman GF/F glass fiber filters. Filters were was 0.8 mg m-3 with 45% of phytoplankton passing aciditied with 250 III of O.5N HCI to remove through 31lm. Primary production was 1.3 gC m'2 inorganic carbon. Radioactivity was measured with dail (30m depth) with 47 % due to phytoplankton a liquid scintillation counter. Areal production was <3Jlm. ca1culated by trapezoidal Integration and daily production estimated by dividing the production 1. Introduction measured during the incubation period by the fraction oftotal daily irradiance during that period.
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    Filling the gaps: identifying candidate sites to expand Fiji's national protected area network Outcomes report from provincial planning meeting, 20-21 September 2010 Stacy Jupiter1, Kasaqa Tora2, Morena Mills3, Rebecca Weeks1,3, Vanessa Adams3, Ingrid Qauqau1, Alumeci Nakeke4, Thomas Tui4, Yashika Nand1, Naushad Yakub1 1 Wildlife Conservation Society Fiji Country Program 2 National Trust of Fiji 3 ARC Centre of Excellence for Coral Reef Studies, James Cook University 4 SeaWeb Asia-Pacific Program This work was supported by an Early Action Grant to the national Protected Area Committee from UNDP‐GEF and a grant to the Wildlife Conservation Society from the John D. and Catherine T. MacArthur Foundation (#10‐94985‐000‐GSS) © 2011 Wildlife Conservation Society This document to be cited as: Jupiter S, Tora K, Mills M, Weeks R, Adams V, Qauqau I, Nakeke A, Tui T, Nand Y, Yakub N (2011) Filling the gaps: identifying candidate sites to expand Fiji's national protected area network. Outcomes report from provincial planning meeting, 20‐21 September 2010. Wildlife Conservation Society, Suva, Fiji, 65 pp. Executive Summary The Fiji national Protected Area Committee (PAC) was established in 2008 under section 8(2) of Fiji's Environment Management Act 2005 in order to advance Fiji's commitments under the Convention on Biological Diversity (CBD)'s Programme of Work on Protected Areas (PoWPA). To date, the PAC has: established national targets for conservation and management; collated existing and new data on species and habitats; identified current protected area boundaries; and determined how much of Fiji's biodiversity is currently protected through terrestrial and marine gap analyses.
  • Status of Coral Reefs in the Fiji Islands 2007

    Status of Coral Reefs in the Fiji Islands 2007

    COMPONENT 2A - Project 2A2 Knowledge, monitoring, management and beneficial use of coral reef ecosystems January 2009 REEF MONITORING SOUTH-WEST PACIFIC STATUS OF CORAL REEFS REPORT 2007 Edited by Cherrie WHIPPY-MORRIS Institute of Marine Resources With the support of: Photo: E. CLUA The CRISP programme is implemented as part of the Regional Environment Programme for a contribution to conservation and sustainable development of coral T (CRISP), sponsored by France and prepared by the French Development Agency (AFD) as part of an inter-ministerial project from 2002 onwards, aims to develop a vi- sion for the future of these unique eco-systems and the communities that depend on them and to introduce strategies and projects to conserve their biodiversity, while developing the economic and environmental services that they provide both locally and globally. Also, it is designed as a factor for integration between developed coun- - land developing countries. The CRISP Programme comprises three major components, which are: Component 1A: Integrated Coastal Management and watershed management - 1A1: Marine biodiversity conservation planning - 1A2: Marine Protected Areas - 1A3: Institutional strengthening and networking - 1A4: Integrated coastal reef zone and watershed management CRISP Coordinating Unit (CCU) Component 2: Development of Coral Ecosystems Programme manager : Eric CLUA - 2A: Knowledge, monitoring and management of coral reef ecosytems SPC - PoBox D5 - 2B: Reef rehabilitation 98848 Noumea Cedex - 2C: Development of active marine substances
  • Insights and Regrets of a Foreign Geoscientist in the Pacific Islands

    Insights and Regrets of a Foreign Geoscientist in the Pacific Islands

    geosciences Article O cei na Vulavula? Insights and Regrets of a Foreign Geoscientist in the Pacific Islands Patrick D. Nunn School of Law and Society, Australian Centre for Pacific Islands Research, University of the Sunshine Coast, Maroochydore, QLD 4558, Australia; [email protected] Abstract: From over three decades of close contact with Pacific Islands geoscience, the author reflects on key issues (what he wished he had known earlier) about the nature of islands, their landscapes and their peoples. Experience elsewhere in the world rarely prepares you for the Pacific, from its youthful and often tectonically unstable landscapes to the understandings of its inhabitants, which are sometimes time-consuming and difficult to access yet frequently illuminating. Mysteries abound in Pacific geoscience, often in places as difficult to access as they ever were, yet which have the potential to inform global ideas about earth-surface evolution. Geoscience research and enterprise remain largely foreigner-driven in the Pacific Islands, which is often anathemic to sustainability, privileging ideas that are uncritically assumed to be shared by their peoples. An opportunity exists for Pacific peoples to own the geoscientific knowledge and potential of their islands. Keywords: Pacific; knowledge; island geology; traditions; last interglacial; sea-level change; island flank collapse; lithospheric flexure; radiocarbon dating Citation: Nunn, P.D. O cei na Vulavula? Insights and Regrets of a 1. Background Foreign Geoscientist in the Pacific A few days after I arrived in Fiji, so did Eric and Nigel, the first tropical cyclones to hit Islands. Geosciences 2021, 11, 182. Suva directly in more than forty years.