Getting the Pacific Online: Access Issues, Challenges & Opportunities Igf2008
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The Effects of the Cyclones of 1983 on the Atolls of the Tuamotu Archipelago (French Polynesia)
THE EFFECTS OF THE CYCLONES OF 1983 ON THE ATOLLS OF THE TUAMOTU ARCHIPELAGO (FRENCH POLYNESIA) J. F. DUPON ORSTOM (French Institute ofScientific Research for Development through cooperation), 213 Rue Lafayette - 75480 Paris Cedex 10, France Abstract. In the TUAMOTU Archipelago, tropical cyclones may contribute to the destruction as well as to some building up of the atolls. The initial occupation by the Polynesians has not increased the vulnerability of these islands as much as have various recent alterations caused by European influence and the low frequency of the cyclone hazard itself. An unusual series of five cyclones, probably related to the general thermic imbalance of the Pacific Ocean between the tropics struck the group in 1983 and demonstrated this vulnerability through the damage that they caused to the environment and to the plantations and settle ments. However, the natural rehabilitation has been faster than expected and the cyclones had a beneficial result in making obvious the need to reinforce prevention measures and the protection of human settle ments. An appraisal of how the lack of prevention measures worsened the damage is first attempted, then the rehabilitation and the various steps taken to forestall such damage are described. I. About Atolls and Cyclones: Some General Information Among the islands of the intertropical area of the Pacific Ocean, most of the low-lying lands are atolls. The greatest number of them are found in this part of the world. Most atolls are characterized by a circular string of narrow islets rising only 3 to 10 m above the average ocean level. -
REP+ Des Tuamotu Et Gambier Who’S Who De L’Éducation Prioritaire
REP+ des Tuamotu et Gambier Who’s who de l’éducation prioritaire Vice-recteur de l’académie de Polynésie-Française M. Philippe COUTURAUD Directeur général de l’éducation et de l’enseignement supérieur M. Thierry DELMAS Chargée de mission de l’éducation prioritaire M. Erik DUPONT LES PILOTES Inspecteur de l’Education nationale (IEN) : Mme Dominique BATLLE Téléphone : 40.46.29.52 E-mail : [email protected] Inspecteur pédagogique régional référent (IA-IPR) : M. Didier RIGGOTARD E-mail : [email protected] Principaux de collège : Antenne de Hao Antenne de Makemo Antenne de Rangiroa M. Patrice LEROY M. Jean-Pierre MESNARD M. Hervé BIGOTTE Téléphone : 40.97.02.99 Téléphone : 40.98.03.69 Téléphone : 40.93.13.40 E-mail : E-mail : E-mail : [email protected] [email protected] [email protected] Conseillers pédagogiques d’éducation prioritaire Mme Herenui PRATX M. Andy CHANSAUD Téléphone : 40.46.29.55 Téléphone : 40.46.29.55 E-mail : [email protected] E-mail : [email protected] Coordonnateur de réseau d’éducation prioritaire Téléphone : 40.46.29.52 E-mail : LES ECOLES : ANTENNE DE HAO ATOLL ECOLE TELEPHONE COURRIEL Hao Ecole primaire TE TAHUA O FARIKI 40 97 03 85 [email protected] Nukutavake Ecole primaire NUKUTAVAKE 40 98 72 91 [email protected] Puka Puka Ecole primaire TE ONE MAHINA 40 97 42 35 [email protected] Rikitea Ecole primaire MAPUTEOA 40 97 82 93 [email protected] Tepoto Ecole primaire TEPOTO 40 97 32 50 [email protected] Napuka Ecole -
The Cultural Landscapes of the Pacific Islands Anita Smith 17
World Heritage Convention Cultural Landscapes of the Pacific Islands ICOMOS Thematic study Anita Smith and Kevin L. Jones December 2007 ICOMOS 49-51 rue de la Fédération – 75015 Paris Tel +33 (0)1 45 67 67 70 – Fax +33 (0)1 45 66 06 22 www.icomos.org – [email protected] Contents Part 1: Foreword Susan Denyer 3 Part 2: Context for the Thematic Study Anita Smith 5 - Purpose of the thematic study 5 - Background to the thematic study 6 - ICOMOS 2005 “Filling the Gaps - An Action Plan for the Future” 10 - Pacific Island Cultural Landscapes: making use of this study 13 Part 3: Thematic Essay: The Cultural Landscapes of the Pacific Islands Anita Smith 17 The Pacific Islands: a Geo-Cultural Region 17 - The environments and sub-regions of the Pacific 18 - Colonization of the Pacific Islands and the development of Pacific Island societies 22 - European contact, the colonial era and decolonisation 25 - The “transported landscapes” of the Pacific 28 - Principle factors contributing to the diversity of cultural Landscapes in the Pacific Islands 30 Organically Evolved Cultural Landscapes of the Pacific 31 - Pacific systems of horticulture – continuing cultural landscapes 32 - Change through time in horticultural systems - relict horticultural and agricultural cultural landscapes 37 - Arboriculture in the Pacific Islands 40 - Land tenure and settlement patterns 40 - Social systems and village structures 45 - Social, ceremonial and burial places 47 - Relict landscapes of war in the Pacific Islands 51 - Organically evolved cultural landscapes in the Pacific Islands: in conclusion 54 Cultural Landscapes of the Colonial Era 54 Associative Cultural Landscapes and Seascapes 57 - Storied landscapes and seascapes 58 - Traditional knowledge: associations with the land and sea 60 1 Part 4: Cultural Landscape Portfolio Kevin L. -
The Fisheries Industry of French Polynesia 4
SOUTH PAC/FH I THE FISHERIES INDUSTRY OF FRENCH POLYNESIA 4 by H, van Pel Fisheries Officer South Pacific Commission and L, C. Devambez Assistant Fisheries Officer South Pacific Commission Noumea South Pacific Commission 1957 U*~Mo'- ^-^ INTRODUCTION 1 GEOGRAPHY General ., .. 1 Tahiti and Moorea .. .. 2 Raiatea, Tahaa, Bora Bora 2 Takaroa, Takapoto ., , 2 Meteorological data 3 THE EXISTING FISHERIES INDUSTRY General , 3 Tahiti Cannery 5 Imports of canned fish, crustaceans and molluscs (Table i). .. 6 Mother of Pearl shell exports (Table II) 6 Production of Mother of Pearl Shell - Tuamotu/Gambier area (Table III) 7 OBSERVATIONS AND RECOMMENDATIONS Tahiti 10 Fish Consumption (Table IV) 14 Trochus niloticus 17 Fish Culture in Ponds 19 Raiatea 19 Tahaa 20 Bora Bora .. 20 Moorea .. .. 20 Tuamotu Islands - Mother of Pearl Oyster 21 Takaroa and Takapoto , 22 Trochus 28 SUMMARY OF RECOMMENDATIONS A. Fish - Oysters - Crustacea 29 B. Mother of Pearl Oysters „ 29 C. Trochus .. .. 29 METEOROLOGICAL DATA APPENDIX I LIBRARY (i) SOUTH Pi 4., L t S * A HK YY T^4EE FISHERIES INDUSTRY OF FRENCH POLYNESIA SOUTH PACcinr"i ! COMM"SSiC'N INTRODUCTION At the request of the Administration of French Polynesia, we nade a general investigation of fisheries in Tahiti, Moorea, Raiatea, Tahaa and Bora Bora in the Society Islands, and in the atolls of Takaroa and Takapoto in the Tuamotou archipelago . The above-mentioned islands were reached by seaplane or by ship, and local investigations were conducted using small boats and motorcars. The keenest interest in the survey and some very helpful encouragement was expressed by His Excellency the Governor of French Polynesia. -
Law of Thesea
Division for Ocean Affairs and the Law of the Sea Office of Legal Affairs Law of the Sea Bulletin No. 82 asdf United Nations New York, 2014 NOTE The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. Furthermore, publication in the Bulletin of information concerning developments relating to the law of the sea emanating from actions and decisions taken by States does not imply recognition by the United Nations of the validity of the actions and decisions in question. IF ANY MATERIAL CONTAINED IN THE BULLETIN IS REPRODUCED IN PART OR IN WHOLE, DUE ACKNOWLEDGEMENT SHOULD BE GIVEN. Copyright © United Nations, 2013 Page I. UNITED NATIONS CONVENTION ON THE LAW OF THE SEA ......................................................... 1 Status of the United Nations Convention on the Law of the Sea, of the Agreement relating to the Implementation of Part XI of the Convention and of the Agreement for the Implementation of the Provisions of the Convention relating to the Conservation and Management of Straddling Fish Stocks and Highly Migratory Fish Stocks ................................................................................................................ 1 1. Table recapitulating the status of the Convention and of the related Agreements, as at 31 July 2013 ........................................................................................................................... 1 2. Chronological lists of ratifications of, accessions and successions to the Convention and the related Agreements, as at 31 July 2013 .......................................................................................... 9 a. The Convention ....................................................................................................................... 9 b. -
Sea-Level Changes Over the Past 1,000 Years in the Pacific Author(S): Patrick D
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of the South Pacific Electronic Research Repository Coastal Education & Research Foundation, Inc. Sea-Level Changes over the past 1,000 Years in the Pacific Author(s): Patrick D. Nunn Source: Journal of Coastal Research, Vol. 14, No. 1 (Winter, 1998), pp. 23-30 Published by: Coastal Education & Research Foundation, Inc. Stable URL: http://www.jstor.org/stable/4298758 . Accessed: 11/09/2013 18:35 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Coastal Education & Research Foundation, Inc. is collaborating with JSTOR to digitize, preserve and extend access to Journal of Coastal Research. http://www.jstor.org This content downloaded from 144.120.8.19 on Wed, 11 Sep 2013 18:35:10 PM All use subject to JSTOR Terms and Conditions JournalofCoastal Research 14 J 1 23-30 RoyalPalmBeach, Florida Winter1998 Sea-Level Changes over the Past 1,000 Years in the Pacific1 Patrick D. Nunn Department of Geography The University of the South Pacific P.O. Box 1168 Suva, FIJI ABSTRACTI Nunn, P.D., 1998. Sea-level changes over the past 1,000 years in the Pacific.Journal of CoastalResearch, 14(1), 23- ,S $00 ?00O av 30. -
Tuamotu Archipelago, French Polynesia)
PART I. ENVIRONMENT AND BIOTA OF THE TIKEHAU ATOLL (TUAMOTU ARCHIPELAGO, FRENCH POLYNESIA) A. INTES AND B. CAILLART THE REGIONAL BACKGROUND The islands of French Polynesia are scattered throughout a considerable oceanic area located on the eastern boundary of the Indo-Pacific Province. This area stretches from 134"28' W (Temoe Island) to 154"401W longitude (Scilly Island), and from 7"50' S (Motu one Island) to 27"36' S latitude (Xapa Island). Out of the 118 islands constituting French Polynesia, 35 are high volcanic islands and 83 are low-relief islands or atolls. Altogether, the territory of French Polynesia represents an area of 4000 km2 of dry land, 12,000 km2 of lagoonal water and a huge Exclusive Economic Zone (EEZ) covering 5,500,000 km2 of oceanic water (Gabrie and Salvat, 1985). French Polynesia is divided into five archipelagos all oriented parallel to a northwest- southeast axis (Fig. 1). These are the Society archipelago, the Tuamotu archipelago, the Austral archipelago, the Marquesas archipelago and the Gambier archipelago. The Tuamotu archipelago stretches over a distance of 1800 km. Its 76 atolls cover a total area of 13,500 km2 of which 600 km2 are dry land. GEOLOGY OF THE TUAMOTU ARCHEPELAGO As figured by Montaggioni (1985), the Tuamotu atolls cap the top of cone-like volcanoes which rise steeply from the floor of a huge ridge forming wide shelves ranging in depth from 1,500 to 3,000 rn. Geomorphological and geochronological evidences support the fact that the formation of the Tuamotu chain is much older than that of other neighboring islands of French Polynesia. -
A Reconnaissance Approach for Hydrology of Atoll Lagoons
Coral Reefs (2001) 20: 409-414 DOl 10.1007js00338-00 1-0192-7 R I. PO IU J. Pages . S. Andrefouet A reconnaissance approach for hydrology of atoll lagoons Received: 6 February 2001 / Accepted: I August 2001 / Published online: 5 October 2001 © Springer-Verlag 2001 Abstract As a reconnaissance tool of the hydrology of tors. In the course of a research program devoted to atoll lagoons in the micro-tidal environment of the Tu atoll lagoons, TypAtoll (Dufour and Harmelin-Vivien amotu Archipelago, we define and compute "potential" 1997), we tried to find out whether the biological and flow rates at lagoon scale under three swell regimes chemical differences found in 10 different lagoons might (high, average, and low swell) after assessment of ori be explained, at least in part, by their hydraulics. This entation and width of reef-flat spillways using satellite hypothesis was followed up, and the data base enlarged images. As a direct test, the "potential" flows were and improved with seven other atolls, in the course of compared with field measurements of (I) measured in a subsequent program, the Programme General de flows across the reef flat (for eight atolls), (2) net out Recherche sur la Nacre (PGRN2), dealing with pearl going flow through the pass (for three atolls), and (3) oyster culture and environment. lagoon-level variation rates (for four atolls). Absolute Material conditions during both programs precluded 2 values of "potential" and field flows agreed (r = 0.94, the usual approach of hydrodynamic modeling and n = 42, slope ~ 1). Computed average water renewal in-situ validation. -
Multilingualism in French Polynesia: Past and Future
Section VI Multilingualism in French Polynesia: Past and future Multilingualism is in its very essence unstable, as it make it possible to perceive major tendencies for involves living languages whose dynamics depend the next 20 to 30 years, with regard to multi- above all on extra-linguistic factors. This funda- lingualism in French Polynesia. The future of lan- mental instability renders virtually impossible any guages in the country as a whole can only be un- prediction beyond two generations. derstood through an analysis archipelago-by- However, the six years of field research that archipelago, and language-by-language. As we will Jean-Michel Charpentier has just carried out in see, knowledge of the recent history of each region French Polynesia in over twenty different locations will enable us to draw up their future perspectives. The Marquesas In the Marquesas Islands, Marquesan remains the As for the third island, Ua Huka, it was essen- daily language for the majority of islanders. The tially depopulated in the 19th century, before being existence of two dialects, with their lexical and repopulated by both northern and southern Mar- phonetic specificities for each island, does not quesans. This is why the island itself is known un- hinder this fundamental linguistic unity. der two different names, Ua Huka (with a /k/ The 2012 census (ISPF 2012) gave a population typical of the northern dialect) and Ua Huna (with of 9,261 for the archipelago, among which two an /n/ typical of southern Marquesan).63 thirds lived in the Northern Marquesas (Nuku Hiva 2,967; Ua Pou 2,175; Ua Huka 621), and one third The island of Hiva Oa, in southern Marquesas, (3,498 inhabitants) lived in the southern part. -
Toomey-Tahaa-2013.Pdf
Quaternary Science Reviews 77 (2013) 181e189 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Reconstructing mid-late Holocene cyclone variability in the Central Pacific using sedimentary records from Tahaa, French Polynesia Michael R. Toomey a,b,*, Jeffrey P. Donnelly a, Jonathan D. Woodruff c a Department of Geology & Geophysics, Woods Hole Oceanographic Institution, MS #22, 360 Woods Hole Rd., Woods Hole, MA 02543, USA b Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA c Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA article info abstract Article history: We lack an understanding of the geographic and temporal controls on South Pacific cyclone activity. Received 7 March 2013 Overwash records from backbarrier salt marshes and coastal ponds have been used to reconstruct Received in revised form tropical cyclone strikes in the North Atlantic basin. However, these specific backbarrier environments are 13 July 2013 scarce in the South Pacific, with cyclone records limited primarily to the period of modern observation. Accepted 15 July 2013 This instrumental record suggests a correlation with the El NiñoeSouthern Oscillation (ENSO), but longer Available online 24 August 2013 records are necessary to test this relationship over geologic timescales and explore other potential climate drivers of tropical cyclone variability. Deep lagoons behind coral reefs are widespread in the Keywords: fi Tropical cyclones Paci c and provide an alternative setting for developing long-term sedimentary reconstructions of South Pacific tropical cyclone occurrence. Coarse-grained event deposits within the sediments of a back-reef lagoon ENSO surrounding Tahaa reveal a 5000-year record of cyclone occurrences. -
Les Fourmis Communes De Polynésie Française (Livret, 32.P)
SOMMAIRE LA VIE DES FOURMIS EN COLONIE LA COMMUNICATION ..................................................................................... P3 L’ALIMENTATION............................................................................................ P3 L’ORGANISATION DE LA COLONIE................................................................... P5 LA FOURMILIÈRE........................................................................................... P5 L’ANATOMIE de la FOURMI............................................................................ P7 EXERCICEs DE TERRAIN SUR LES FOURMIS.......................................................... P11 LES PRÉFÉRENCES ALIMENTAIRES ............................................................... P12 LES PRÉFÉRENCES D’HABITATS..................................................................... P13 CARACTERISTIQUEs DES FOURMIS COMMUNES DE POLYNESIE FRANcAISE STATUT........................................................................................................... P15 RECONNAISSANCE......................................................................................... P16 SOUS-FAMILLE DES DOLICHODERINAE.......................................................... P18 • Tapinoma melanocephalum – La fourmi fantôme......................................... P18 • Technomyrmex vitiensis – La fourmi aux pattes blanches............................ P19 SOUS-FAMILLE DES FORMICINAE................................................................... P20 • Anoplolepis gracilipes – La fourmi à -
Typology of Atoll Rims in Tuamotu Archipelago (French Polynesia) at Landscape Scale Using SPOT HRV Images
INT. J. REMOTE SENSING, 2001, YOL. 22, NO. 6,987-1004 Typology of atoll rims in Tuamotu Archipelago (French Polynesia) at landscape scale using SPOT HRV images 3 4 s, S. ANDREFOUETI.2, M. CLAEREBOUDT • , P. MATSAKIS J. PAGES6 and P. DUFOUR3 I Laboratoire de Geosciences Marines et Teledetection, Universite Francaise du Pacifique, BP 6570 Faaa-Aeroport, Tahiti, French Polynesia 2Remote Sensing Biological Oceanography Lab., University of South Florida, Department of Marine Science, 140, 7th Avenue South, St Petersburg, FL 33701, USA 3IRD, Centre d'Oceanologie de Marseille, rue de la Batterie des Lions, F-1037 Marseille, France "College of Agriculture, Fisheries Dept., Sultan Qaboos University, P.O Box 34, Al-Khad 123, Sultanate of Oman SInstitut de Recherche en Informatique de Toulouse, Universite Paul Sabatier Toulouse-ll8, Route de Narbonne 31062 Toulouse Cedex, France "Centre IRD de Tahiti, BP 529 Papeete, Tahiti, French Polynesia (Received 31 August 1998; in final form 22 November 1999) Abstract. The lagoon of an atoll is separated from the ocean by a rim. As the rim controls the flux of water between ocean and lagoon, its structure is one of the major forcing factors of the biological processes that depend on the renewal rate of lagoonal water. Characterizing rim structure and its degree of hydro dynamic aperture is mandatory for comparing the functioning of different atoll lagoons. This paper characterizes at landscape scale the different types of rims of the atolls of the Tuamotu Archipelago (French Polynesia) using SPOT HRV multi-spectral images. The classification of 117 segments of rims highlights nine different rims.