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TA31 Book.Indb 231 24/11/09 12:13:40 PM 232 Trevor H
10 Bird, mammal and reptile remains Trevor H. Worthy School of Biological, Earth and Environmental Sciences, The University of New South Wales Geoffrey Clark Department of Archaeology and Natural History, The Australian National University Introduction This chapter reports the non-fish remains from 10 archaeological excavations on Viti Levu and the Lau Group, including the reanalysis of a bird-bone assemblage from Lakeba Island excavated previously by Simon Best (1984). Bone remains from Natunuku and Ugaga were uncommon and the small assemblages were misplaced during collection relocation after bushfires destroyed the ANU archaeological storage facility in 2003, and these assemblages are not considered further. Three of the non-fish faunal assemblages are from the Lau Group (Qaranipuqa, Votua, Sovanibeka), one is from the north coast of Viti Levu (Navatu 17A), and the remainder are from the southwest Viti Levu region (Malaqereqere, Tuvu, Volivoli II, Volivoli III, Qaraninoso II) and Beqa Island (Kulu). This chapter presents the non-fish fauna from the Lau Group, followed by that from Viti Levu and Beqa Island. Faunal analysis began early in Fiji, with bone remains identified at Navatu and Vuda on Viti Levu by Gifford (1951:208–213). Gifford’s excavations demonstrated that pig, dog, chicken, turtle, fruit bat and humans were consumed during the ‘early period’ of Fiji. The study of archaeofauna declined after this promising start due to the absence of prehistoric fauna in sites such as Sigatoka and Karobo (Palmer 1965; Birks 1973), and the cursory identification of bone remains at sites like Yanuca and Natunuku (Birks and Birks 1978; Davidson et al. -
Sche MID-Pacavrgravone
TULV. 15:22. XXIV. No. 1. Cents a Copy. 41111111111111inta 11/ unummatommork mlluMatimmmummaleiniliiim sche MID-PACargv rAVONE and the BULLETIN OF THE PAN-PACIFIC UNION Cr; Wallace R. Farrington, Governor of Hawaii and President of the Pan-Pacific Union. accepting the flag of Japan sent to the Union by the late Premier Hara by Hon. C. Yada, the first Pan-Pacific Minister of Friendship. li err SIIHMIIIIIIIIMIIIIIIIIIIIII103031111111111111110011111111111111111:1111111111110161111111111111MMUM11111111111MIIMMIH11111134 JAVA NITED STATES AUSTRALASIA HAWAII ORIENT Ara. News Co. Gordon & Goteb Pan-Pacific Union Kelly & Walsh Javasche Boekhandel t 1'1' t' 1' r 't' mtttstAtAghttaftta Pan-Parifir Tinian Central Offices, Honolulu, Hawaii, at the Ocean's Crossroads. PRESIDENT, HON. WALLACE R. FARRINGTON, Governor of Hawaii. ALEXANDER HUME FORD, Director. DR. FRANK F. BUNKER, Executive Secretary. The Pan-Pacific Union, representing the lands about the greatest of oceans, is supported by appropriations from Pacific governments. It works chiefly through the calling of conferences, for the greater advancement of, and cooperati.on among, all the races -and peoples of the Pacific. HONORARY PRESIDENTS Warren G. Harding President of the United States William M. Hughes Prime Minister of Australia W. F. Massey Prime Minister of New Zealand Hsu Shih-chang President of China Arthur Meighen Premier of Canada Prince I. Tokugawa President, House of Peers, Tokyo His Majesty, Rama VI King of Siam HONORARY VICE-PRESIDENTS Charles Evans Hughes Secretary of State, United States Woodrow Wilson Ex-President of the United States Dr. L. S. Rowe Director-General Pan-American Union Yeh Kung Cho Minister of Communications, China Leonard Wood The Governor-General of the Philippines The Premiers of Australian States and of British Columbia The Governor-General of Java. -
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. -
Vanua Levu Viti Levu
MA019 Index of Maps Page Page 2 Number Page Name Number Page Name 1 1 Rotuma 48 South Vanua Balavu Fiji: 2 Cikobia 49 Mana and Malolo Lailai S ° 3 6 3 Vatauna 50 Nadi 1 Cyclone Winston- 4 Kia 51 West Central Viti Levu 8 Index to 1:100 000 5 Mouta 52 Central Viti Levu 4 5 6 7 6 Dogotuki 53 Laselevu 16 Topographical Maps 7 Nagasauva 54 Korovou Labasa 8 Naqelelevu 55 Levuka Northern 10 11 12 13 14 15 9 Yagaga 56 Wakaya and Batiki 9 Index to 1:100 000 Topographical 10 Macuata 57 Nairai Vanua Levu 23 24 25 Series (MA003) with numbers and 11 Sasa 58 Cicia 17 19 20 21 22 26 names 12 Labasa 59 Tuvuca and Katafaga Yasawa 18 Savusavu 13 Saqan 60 West Viti Levu 31 14 Rabi 61 Narewa 27 28 29 30 15 Yanuca 62 South Central Viti Levu 37 38 Northern 16 Nukubasaga 63 East Cental Viti Levu 33 34 35 Lau Rotuma 17 Yasawa North 64 Nausori 32 36 18 Yadua 65 Gau Vaileka 46 47 48 19 Bua 66 Nayau Tavua 42 43 45 Central 39 40 41 Ba 44 20 Vanua Levu 67 Eastern Atolls Western Lautoka Vatukoula Lamaiviti 21 Wailevu 68 South West Viti Levu 59 49 50 53 54 55 56 58 22 Savusavu 69 Sigatoka Viti Levu 52 57 23 Tonulou 70 Queens Road 51 Korovou Nadi 67 24 Wainikeli 71 Navau S 66 ° 8 60 61 62 Central FIJI 25 Laucala 72 Suva 1 63 64 65 26 Wallagi Lala 73 Lakeba Sigatoka 27 Yasawa South 74 Vatulele 72 68 69 70 71 73 28 Vuya 75 Yanuca and Bega Vanua Levu 77 29 South 76 Vanua Vatu 75 76 30 Waisa 77 Alwa and Oneata 74 Taveuni 79 31 South 78 Dravuni 80 81 78 Viwa and Eastern 32 Waya 79 Moala 85 86 Naiviti and 82 83 84 33 Narara 80 Tavu Na Siel 34 Naba 81 Moce, Komu and Ororua -
Moturiki, Lomaiviti Group
Archaeological History of a Fijian Island: Moturiki, Lomaiviti Group MARÍA Cruz BErrocal, Antonio UriartE GONZÁLEZ, SIDSEL MILLErstrom, SUSANA CONSUEGRA RODRÍGUEZ, Juana PÉREZ-ARIAS, AND Santiago ORMEÑO introduction In 2007, we started a project to record rock art in Fiji (Cruz Berrocal and Millerstrom 2013; Millerstrom and Cruz Berrocal 2009, 2010), focusing in 2008 on a site called Vatu Vola that had been discovered in 2006 in the Naisogorourou area on Moturiki ( pers. comm. Jone Balenaivalu, 13 September 2007). We designed our fieldwork there as a selective survey to understand the mechanisms of landscape construction associated with the making of rock art on small islands. The survey and further archaeological explorations of Moturiki rendered significant data and raised research questions presented in this article (Cruz Berrocal and Millerstrom 2013). Moturiki is one of the islands in the Lomaiviti group in central Fiji. The island’s surface is 1473 ha, including 1130 ha of mainland and 343 ha of mangrove (calcula- tions based on the cartographic base listed below). It is a volcanic outlier of Ovalau (Fig. 1). As a high island with maximum altitudes around 120 m (116 m according to the Digital Terrain Model of the island; source GDEM, below), it has a diversified landscape and, especially in the south, the topography is remarkable (Fig. 2). This set- ting provides different landscape contexts for archaeological inquiry. In addition, Mo- turiki has one of the oldest Lapita settlements (including a burial) found so far in Fiji ( Nunn et al. 2007), thus one of a limited number of sites with Lapita remains that can be analyzed ( Petchey et al. -
Global Reef Expedition Final Report June 2-28, 2013
Global Reef Expedition Final Report June 2-28, 2013 Andrew W. Bruckner, Alexandra Dempsey, Georgia Coward, Steve Saul, Elizabeth Rauer, & Amy Heemsoth i ©2016 Khaled bin Sultan Living Oceans Foundation. All Rights Reserved. Science Without Borders® All research was completed under the research permit approved by the Ministry of Education, Natural Heritage, Culture & Arts, RA 10/13 dated 11 April 2013. The information included in this document is submitted to fulfill the requirements of the Final Report for the Global Reef Expedition: Fiji Research Mission. Citation: Global Reef Expedition: Lau Province, Fiji. Final Report. Bruckner, A.W., Dempsey, A.C., Coward, G., Saul, S., Rauer, E.M. & Heemsoth, A. (2016). Khaled bin Sultan Living Oceans Foundation, Annapolis, MD. 113p. ISBN: 978-0-9975451-0-4 Khaled bin Sultan Living Oceans Foundation (KSLOF) was incorporated in California as a 501(c)(3), public benefit, Private Operating Foundation in September 2000. The Living Oceans Foundation is dedicated to providing science-based solutions to protect and restore ocean health. For more information, visit www.lof.org Facebook: www.facebook.com/livingoceansfoundation Twitter: @LivingOceansFdn Khaled bin Sultan Living Oceans Foundation 130 Severn Avenue Annapolis, MD, 21403, USA Executive Director Philip G. Renaud. Chief Scientist: Andrew W. Bruckner Images by Andrew Bruckner, unless noted. Habitat Mapping was completed by Steve Saul Front cover: Clownfish in an anemone by Derek Manzello Back cover: Coral reefs of Fiji by Derek Manzello Khaled bin Sultan Living Oceans Foundation Publication # 14 Khaled bin Sultan Living Oceans Foundation Global Reef Expedition Lau Province, Fiji June 2-28, 2013 FINAL REPORT Andrew W. -
Fiji Islands, and Their History of Early Early of History Their and Islands, Fiji the of Position Strategic the Despite
Micronesica 25(1): 41-70, 1992 A Preliminary Checklist of the Benthic Marine Algae of the Fiji Islands, South Pacific G. ROBIN SOUTH The University of the South Pacific , P.O. Box 1168, Suva, Republic of Fiji and HITOSHI KASAHARA Shizuoka-ken Kama-gun, Matsuzaki-cha Sakurada 47, 410-36 Japan Abstract-A preliminary checklist of 314 taxa of benthic marine algae is provided for the Fiji Islands, South Pacific, comprising 11 Cyano phyceae, 99 Chlorophyceae, 36 Phaeophyceae and 168 Rhodophyceae. Included are all previously published records, with the systematic ar rangement and nomenclature brought up to date. The flora is relatively poorly known, and many areas have yet to be phycologically studied, such as Rotuma, much of the Lau Group, most of Vanua Levu and Kandavu. Introduction The Fiji Islands occupy a central position in Oceania, spanning the 180th meridian and lying between 177 E and 178 W, and 16 to 20 S (Fig. 1 ). A land of area of some 18,276 sq. km is scattered over 332 islands, occupying 260,000 sq km of ocean (Fig. 1). There are four main islands in the group, Viti Levu, Vanua Levu, Taveuni and Kadavu, and three smaller island groups, the Yasawas, the Lomaiviti Group and the Lau Group. The small island ofRotuma is isolated from the rest of the Fiji group, some 300 km north of Viti Levu. Most of the islands are high islands of volcanic origin, although some low atolls are found in the east in the Lau Group. The islands are surrounded by barrier reefs, and there are many patch reefs throughout; the most significant barrier reef is the Great Astrolabe Reef, which occurs around the Kadavu Islands. -
Highlights Situation Overview
Fiji: Severe Tropical Cyclone Winston Situation Report No. 5 (as of 25 February 2016) This report is produced by the OCHA Regional Office for the Pacific (ROP) in collaboration with humanitarian partners. It covers the period from 24 to 25 February 2016. The next report will be issued on or around 26 February 2016. Highlights • On 20 and 21 February Category 5 Severe Tropical Cyclone Winston cut a path of destruction across Fiji. • The cyclone is estimated to be one of the most severe ever to hit the South Pacific. • The Fiji Government estimates almost 350,000 people living in the cyclone’s path could have been affected – 180,000 men and 170 000 women. • 41 people have been confirmed dead. • 131 people are injured. • Aid has begun arriving in cyclone affected communities, especially the hard hit outer islands and Rakiraki in the West. • Almost 50,000 people are currently sheltering in nearly 800 evacuation centres. • Damage to agriculture is estimated to be US$61 million with 100 per cent of crops destroyed in the worst affected areas. • At least 117 schools have been damaged • A 30 day State of Natural Disaster has been declared. 41 50,000 US $61m Confirmed fatalities People in in damage to evacuation centres agriculture Sit Rep Sources: Fiji Government, Fiji NEOC/NDMO, PHT Partners, NGO Community Situation Overview The scale of the task ahead is becoming clearer with the Fiji Government now estimating almost 350,000 people may have been affected by the cyclone, around a third of them children. Analysis of imagery produced from aerial surveillance flights has confirmed that the worst affected areas are: Northern Lau Group, the south and east coast of Taveuni, the south coast of Vanua Levu (Savusavu, Nasonisoni and Nabouwalu), Koro Island, Ovalau, Naigani and north east Viti Levu. -
This Keyword List Contains Pacific Ocean (Excluding Great Barrier Reef)
CoRIS Place Keyword Thesaurus by Ocean - 3/2/2016 Pacific Ocean (without the Great Barrier Reef) This keyword list contains Pacific Ocean (excluding Great Barrier Reef) place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. The same names are available from “Place Keywords by Country/Territory - Pacific Ocean (without Great Barrier Reef)” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Pacific Ocean OCEAN BASIN > Pacific Ocean > Albay Gulf > Cauit Reefs (13N123E0016) OCEAN BASIN > Pacific Ocean > Albay Gulf > Legaspi (13N123E0013) OCEAN BASIN > Pacific Ocean > Albay Gulf > Manito Reef (13N123E0015) OCEAN BASIN > Pacific Ocean > Albay Gulf > Matalibong ( Bariis ) (13N123E0006) OCEAN BASIN > Pacific Ocean > Albay Gulf > Rapu Rapu Island (13N124E0001) OCEAN BASIN > Pacific Ocean > Albay Gulf > Sto. Domingo (13N123E0002) OCEAN BASIN > Pacific Ocean > Amalau Bay (14S170E0012) OCEAN BASIN > Pacific Ocean > Amami-Gunto > Amami-Gunto (28N129E0001) OCEAN BASIN > Pacific Ocean > American Samoa > American Samoa (14S170W0000) OCEAN BASIN > Pacific Ocean > American Samoa > Manu'a Islands (14S170W0038) OCEAN BASIN > -
Curriculum Vitae
CURRICULUM VITAE Contents 1. Personal ................................................................................................... Page 1 2. Degrees received ..................................................................................... Page 2 3. Professional appointments ...................................................................... Page 2 4. Publications .............................................................................................. Page 4 5. Languages ............................................................................................. Page 25 6. Lecturing experience .............................................................................. Page 25 6.i. Courses taught .......................................................................... Page 25 6.ii. Special lectures ......................................................................... Page 26 6.iii. Conference posters ................................................................... Page 40 7. Current and recent postgraduate supervision and postdoc mentoring.... Page 42 8. Grants awarded ..................................................................................... Page 43 9. Principal university internal appointments ............................................. Page 48 10. Major recent consultancies ……………………………………………….. Page 48 11. Miscellaneous ........................................................................................ Page 49 1. Personal Name Patrick D. Nunn Address Sustainability Research Centre (Room -
Biophysically Special, Unique Marine Areas of FIJI © Stuart Chape
BIOPHYSICALLY SPECIAL, UNIQUE MARINE AREAS OF FIJI © Stuart Chape BIOPHYSICALLY SPECIAL, UNIQUE MARINE AREAS OF FIJI EFFECTIVE MANAGEMENT Marine and coastal ecosystems of the Pacific Ocean provide benefits for all people in and beyond the region. To better understand and improve the effective management of these values on the ground, Pacific Island Countries are increasingly building institutional and personal capacities for Blue Planning. But there is no need to reinvent the wheel, when learning from experiences of centuries of traditional management in Pacific Island Countries. Coupled with scientific approaches these experiences can strengthen effective management of the region’s rich natural capital, if lessons learnt are shared. The MACBIO project collaborates with national and regional stakeholders towards documenting effective approaches to sustainable marine resource management and conservation. The project encourages and supports stakeholders to share tried and tested concepts and instruments more widely throughout partner countries and the Oceania region. This report outlines the process undertaken to define and describe the special, unique marine areas of Fiji. These special, unique marine areas provide an important input to decisions about, for example, permits, licences, EIAs and where to place different types of marine protected areas, Locally-Managed Marine Area and tabu sites in Fiji. For a copy of all reports and communication material please visit www.macbio-pacific.info. MARINE ECOSYSTEM MARINE SPATIAL PLANNING EFFECTIVE MANAGEMENT SERVICE VALUATION BIOPHYSICALLY SPECIAL, UNIQUE MARINE AREAS OF FIJI AUTHORS: Helen Sykes1, Jimaima Le Grand2, Kate Davey3, Sahar Noor Kirmani4, Sangeeta Mangubhai5, Naushad Yakub3, Hans Wendt3, Marian Gauna3, Leanne Fernandes3 2018 SUGGESTED CITATION: Sykes H, Le Grand J, Davey K, Kirmani SN, Mangubhai S, Yakub N, Wendt H, Gauna M, Fernandes L (2018) Biophysically special, unique marine areas of Fiji. -
TA31 Book.Indb 407 24/11/09 12:15:36 PM 408 Geoffrey Clark and Atholl Anderson
16 Colonisation and culture change in the early prehistory of Fiji Geoffrey Clark Department of Archaeology and Natural History, The Australian National University Atholl Anderson Department of Archaeology and Natural History, The Australian National University Introduction The arrival of humans in the Fiji Islands at ca. 2950–3050 cal. BP was, in historical and ecological terms, a momentous event in Pacific prehistory that nonetheless comprised only a relatively small part of the Lapita expansion in Near and Remote Oceania. In turn, Lapita colonisation was only one of several prehistoric migratory movements in Oceania that began during the late Pleistocene movement to Near Oceania (Allen and O’Connell 2008), with the frequency and scale of maritime movements increasing during the late Holocene (Anderson 2001; Green 2003). In this chapter, we situate the colonisation of Fiji and the Early Prehistory of Fiji Project results in the Lapita expansion, contrasting it with human arrival in western Micronesia and the colonisation of East Polynesia. These prehistoric migratory movements suggest a preference for colonisation of uninhabited landmasses. In the case of Lapita migration, suspected avoidance of the main Solomon Islands and Samoa raises, among other critical issues, questions about seafaring capacity and colonisation pattern during the Lapita era. These are particularly important when considering human arrival in Fiji–West Polynesia because the 800+ km water gap separating Vanuatu–New Caledonia from Fiji was the largest inter-archipelagic