Climate Change and Biodiversity in Melanesia
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The Southwest Pacific: U.S
Order Code RL34086 The Southwest Pacific: U.S. Interests and China’s Growing Influence July 6, 2007 Thomas Lum Specialist in Asian Affairs Foreign Affairs, Defense, and Trade Division Bruce Vaughn Specialist in Asian Affairs Foreign Affairs, Defense, and Trade Division The Southwest Pacific: U.S. Interests and China’s Growing Influence Summary This report focuses on the 14 sovereign nations of the Southwest Pacific, or Pacific Islands region, and the major external powers (the United States, Australia, New Zealand, France, Japan, and China). It provides an explanation of the region’s main geographical, political, and economic characteristics and discusses United States interests in the Pacific and the increased influence of China, which has become a growing force in the region. The report describes policy options as considered at the Pacific Islands Conference of Leaders, held in Washington, DC, in March 2007. Although small in total population (approximately 8 million) and relatively low in economic development, the Southwest Pacific is strategically important. The United States plays an overarching security role in the region, but it is not the only provider of security, nor the principal source of foreign aid. It has relied upon Australia and New Zealand to help promote development and maintain political stability in the region. Key components of U.S. engagement in the Pacific include its territories (Guam, the Northern Mariana Islands, and American Samoa), the Freely Associated States (Marshall Islands, Micronesia, and Palau), military bases on Guam and Kwajalein atoll (Marshall Islands), and relatively limited aid and economic programs. Some experts argue that U.S. involvement in the Southwest Pacific has waned since the end of the Cold War, leaving a power vacuum, and that the United States should pay greater attention to the region and its problems. -
Internal Tides in the Solomon Sea in Contrasted ENSO Conditions
Ocean Sci., 16, 615–635, 2020 https://doi.org/10.5194/os-16-615-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Internal tides in the Solomon Sea in contrasted ENSO conditions Michel Tchilibou1, Lionel Gourdeau1, Florent Lyard1, Rosemary Morrow1, Ariane Koch Larrouy1, Damien Allain1, and Bughsin Djath2 1Laboratoire d’Etude en Géophysique et Océanographie Spatiales (LEGOS), Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France 2Helmholtz-Zentrum Geesthacht, Max-Planck-Straße 1, Geesthacht, Germany Correspondence: Michel Tchilibou ([email protected]), Lionel Gourdeau ([email protected]), Florent Lyard (fl[email protected]), Rosemary Morrow ([email protected]), Ariane Koch Larrouy ([email protected]), Damien Allain ([email protected]), and Bughsin Djath ([email protected]) Received: 1 August 2019 – Discussion started: 26 September 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 15 May 2020 Abstract. Intense equatorward western boundary currents the tidal effects over a longer time. However, when averaged transit the Solomon Sea, where active mesoscale structures over the Solomon Sea, the tidal effect on water mass transfor- exist with energetic internal tides. In this marginal sea, the mation is an order of magnitude less than that observed at the mixing induced by these features can play a role in the ob- entrance and exits of the Solomon Sea. These localized sites served water mass transformation. The objective of this paper appear crucial for diapycnal mixing, since most of the baro- is to document the M2 internal tides in the Solomon Sea and clinic tidal energy is generated and dissipated locally here, their impacts on the circulation and water masses, based on and the different currents entering/exiting the Solomon Sea two regional simulations with and without tides. -
(V&A) Assessment for Ontong Java Atoll, Solomon Islands
PACC TECHNICAL REPORT 4 JUNE 2014 Vulnerability and adaptation (V&A) assessment for Ontong Java Atoll, Solomon Islands SPREP LIBRARY/IRC CATALOGUING-IN-PUBLICATION DATA Vulnerability and adaptation (V&A) assessment for Ontong Java Atoll, Solomon Islands. Apia, Samoa : SPREP, 2014. p. cm. (PACC Technical Report No.4) ISSN 2312-8224 Secretariat of the Pacific Regional Environment Programme authorises the reproduction of this material, whole or in part, provided appropriate acknowledgement is given. SPREP, PO Box 240, Apia, Samoa T: +685 21929 F: +685 20231 E: [email protected] W: www.sprep.org This publication is also available electronically from SPREP’s website: www.sprep.org SPREP Vision: The Pacific environment, sustaining our livelihoods and natural heritage in harmony with our cultures. www.sprep.org PACC TECHNICAL REPORT 4 JUNE 2014 Vulnerability and adaptation (V&A) assessment for Ontong Java Atoll, Solomon Islands TABLE OF CONTENTS ACKNOWLEDGEMENTS Iv EXECUTIVE SUMMARY v ABBREVIATIONS vii 1. INTRODUCTION 1 2. BACKGROUND 3 2.1. Natural and human systems of Ontong Java Atoll 4 2.1.1. Vegetation 4 2.1.2. The marine ecosystem 4 2.1.3. People and land systems 5 2.2. Current climate and sea level 6 2.2.1. Temperature and rainfall 6 2.2.2. Extreme events 7 2.2.3. Sea level 8 2.3. Climate and sea level projections 9 2.3.1. Temperature and rainfall projections 9 2.3.2. Sea level projections 11 2.4. Climate change impacts 11 3. THE ASSESSMENT AND ITS OBJECTIVES 12 4. METHODOLOGY 12 4.1. Household survey 13 4.1.1. -
Analysis of Existing Marine Assessments in the South West
WEALTH FROM OCEANS Analysis of existing marine assessments in the South West Pacific For the United Nations Regional Regular Process workshop, th th Brisbane Australia, 25 to 27 February, 2013. Piers Dunstan, Karen Evans, Tim Caruthers and Paul Anderson Wealth From Oceans Citation Dunstan, PK, Evans K, Caruthers T and Anderson P. (2013) . Updated analysis of existing marine assessments in the South West Pacific. CSIRO Wealth from Oceans and the Secretariat of the Pacific Regional Environment Programme. Important disclaimer CSIRO advises that the information contained in this publication comprises general statements based on scientific research. The reader is advised and needs to be aware that such information may be incomplete or unable to be used in any specific situation. No reliance or actions must therefore be made on that information without seeking prior expert professional, scientific and technical advice. To the extent permitted by law, CSIRO (including its employees and consultants) excludes all liability to any person for any consequences, including but not limited to all losses, damages, costs, expenses and any other compensation, arising directly or indirectly from using this publication (in part or in whole) and any information or material contained in it. Contents Acknowledgments .............................................................................................................................................. 4 1 Introduction ......................................................................................................................................... -
Species-Edition-Melanesian-Geo.Pdf
Nature Melanesian www.melanesiangeo.com Geo Tranquility 6 14 18 24 34 66 72 74 82 6 Herping the final frontier 42 Seahabitats and dugongs in the Lau Lagoon 10 Community-based response to protecting biodiversity in East 46 Herping the sunset islands Kwaio, Solomon Islands 50 Freshwater secrets Ocean 14 Leatherback turtle community monitoring 54 Freshwater hidden treasures 18 Monkey-faced bats and flying foxes 58 Choiseul Island: A biogeographic in the Western Solomon Islands stepping-stone for reptiles and amphibians of the Solomon Islands 22 The diversity and resilience of flying foxes to logging 64 Conservation Development 24 Feasibility studies for conserving 66 Chasing clouds Santa Cruz Ground-dove 72 Tetepare’s turtle rodeo and their 26 Network Building: Building a conservation effort network to meet local and national development aspirations in 74 Secrets of Tetepare Culture Western Province 76 Understanding plant & kastom 28 Local rangers undergo legal knowledge on Tetepare training 78 Grassroots approach to Marine 30 Propagation techniques for Tubi Management 34 Phantoms of the forest 82 Conservation in Solomon Islands: acts without actions 38 Choiseul Island: Protecting Mt Cover page The newly discovered Vangunu Maetambe to Kolombangara River Island endemic rat, Uromys vika. Image watershed credit: Velizar Simeonovski, Field Museum. wildernesssolomons.com WWW.MELANESIANGEO.COM | 3 Melanesian EDITORS NOTE Geo PRODUCTION TEAM Government Of Founder/Editor: Patrick Pikacha of the priority species listed in the Critical Ecosystem [email protected] Solomon Islands Hails Partnership Fund’s investment strategy for the East Assistant editor: Tamara Osborne Melanesian Islands. [email protected] Barana Community The Critical Ecosystem Partnership Fund (CEPF) Contributing editor: David Boseto [email protected] is designed to safeguard Earth’s most biologically rich Prepress layout: Patrick Pikacha Nature Park Initiative and threatened regions, known as biodiversity hotspots. -
How Is the Solomon Sea Impacted by Enso ? A
HOW IS THE SOLOMON SEA IMPACTED BY ENSO ? A. MELET1,2,, L. GOURDEAU 3,, N. DJATH1, W. KESSLER4, J. VERRON1 1. CNRS/LEGI, FrancE 3. IRD/LEGOS, FrancE 2. Currently at Princeton UnivErsity / GFDL, USA 4. NOAA/PMEL, USA 1. Mo?vaon 2. Methodology 3. Thermocline circulaon and ENSO The interannual variaons of the Solomon Sea WBC The Solomon Sea is a key region of the southwest Pacific where Low Latude An original modeling strategy based on model nesngs (Fig 2) has been thermocline transPorts are related to ENSO. A Western Boundary Currents (LLWBCs) connect the subtroPical and equatorial implemented to realis?cally resolve the comPlex bathymetry of the comPrehensive diagnosis of ENSO influence on the circulaons through narrow straits (Fig 1). Since the LLWBCs are the main sources Solomon Sea, notably the network of narrow straits connec?ng it to the thermocline circulaon is performed through the of the Equatorial Undercurrent (EUC), they could play a major role in the low Equatorial Pacific. construc?on of compositE anomaliEs for El Niño (APr 87, frequency modulaon of El Niño Southern Oscillaon (ENSO). Therefore, the A 1/12° model of the Solomon Sea is interac?vely nested (AGRIF 92, 98, Jan 2003) and La Niña (APr 89 & 97, Jan 2000) Solomon Sea is of Par?cular interest in a climac context and is a focal Point in sohware, 2-way) in a regional ¼° model of the southwest Pacific, itself states. The ENSO related thermocline circulaon the South PacifIc Circulaon and Climate Experiment (SPICE). In recent work, the embedded in a ¼° global simulaon (Drakkar project). -
Pacific Islander Migration to Australia: the 1980S and Beyond’ Christine Mcmurray and David Lucas
Pacific islander migration to Australia: the 1980s and beyond’ Christine McMurray and David Lucas The 1981 Census of Australia counted 34,826 sume that a large proportion of those in the persons born in Melanesia and Polynesia; by category 0-4 years were residents. 1986 this figure had increased by 39 per cent to Most of the Papua New Guinea-born are 48,536. Prior to 1981 those born in Papua New children of Australians or others born outside Guinea were not distinguished from Papua New Guinea. Connel12 estimated that Australians in the census. However, if the only about 10 per cent were Papua New Papua New Guinea-born are excluded from the Guinea nationals in 1981. In 1986 only 12 per figures for 1981 and 1986 the increase is even cent did not have Australian citizenship, and more striking. In 1976 there were 9663 Pacific- hence could have been Papua New Guinea na- born (including the catch-all category ‘Other tionals. Similarly, many migrants born in New Oceania’but excluding Papua New Guinea and Caledonia, where the Melanesian Kanaks are New Zealand). By 1981 there were 16,129 from now in the minority, could be children of Melanesia and Polynesia alone, and by 1986 French settlers. However, most of those born in there were 27,185; an increase of more than other Pacific states can be assumed to be of 180 per cent in the ten-year period. This paper Polynesian, Melanesian, Indo-Fijian or considers the implications of this change and Micronesian descent. In Fiji, the Melanesians whether migration from this source can be ex- are predominantly Christian, compared with pected to accelerate or decelerate in the next only a small percentage of the Indo-Fijians. -
Mid-Holocene Social Interaction in Melanesia: New Evidence from Hammer-Dressed Obsidian Stemmed Tools
Mid-Holocene Social Interaction in Melanesia: New Evidence from Hammer-Dressed Obsidian Stemmed Tools ROBIN TORRENCE, PAMELA SWADLING, NINA KONONENKO, WALLACE AMBROSE, PIP RATH, AND MICHAEL D. GLASCOCK introduction Proposals that large-scale interaction and ceremonial exchange in the Pacific region began during the time of Lapita pottery (c. 3300–2000 b.p.) (e.g., Friedman 1981; Hayden 1983; Kirch 1997; Spriggs 1997) are seriously challenged by the extensive areal distribution of a class of retouched obsidian artifacts dated to the early and middle Holocene (c. 10,000–3300 b.p.) and known as ‘‘stemmed tools’’ (Araho et al. 2002). Find spots of obsidian stemmed tools stretch from mainland New Guinea to Bougainville Island and include the Trobriand Islands, various islands in Manus province, New Britain and New Ireland (Araho et al. 2002; Golson 2005; Specht 2005; Swadling and Hide 2005) (Fig. 1). Although other forms of tanged and waisted stone tool are known in Melanesia (e.g., Bulmer 2005; Fredericksen 1994, 2000; Golson 1972, 2001), the two types defined by Araho et al. (2002) as ‘‘stemmed tools’’ comprise distinctive classes because they usually have deep notches that delineate very well-defined and pronounced tangs. Type 1 stemmed tools are made from prismatic blades and have large and clearly demarcated, oval-shaped tangs. In contrast, the Type 2 group is more vari- able.Itisdefinedprimarilybytheuseof Kombewa flakes (i.e., those removed fromthebulbarfaceofalargeflake)forthe blank form, as described in detail in Robin Torrence is Principal Research Scientist in Anthropology, Australian Museum, Sydney NSW, [email protected]; Pamela Swadling is a Visiting Research Fellow, Archaeol- ogy and Natural History, Research School of Pacific Studies, Australian National University, Can- berra ACT, [email protected]; Nina Kononenko is an ARC post-doctoral fellow in the School of Philosophical and Historical Inquiry, University of Sydney, kononenko.nina@hotmail. -
Towards Establishing a Melanesia Biosecurity & Invasive Species Advisory Committee
Towards establishing a Melanesia Biosecurity & Invasive Species Advisory Committee October 2016 Report prepared for the Secretariat of the Pacific Regional Environment Programme & the Government of Vanuatu Port Vila, Vanuatu DEPARTMENT OF ENVIRONMENTAL PROTECTION AND CONSERVATION REPUBLIC OF VANUATU 1 | P a g e Executive Summary The Pacific Islands Countries and Territories (PICTs) represent a unique scattering of islands, ecosystems and cultural diversity that is incomparable anywhere in the world. Many islands host species that have evolved and adapted to island conditions making them special from a scientific and cultural perspective but also vulnerable to threats. Human migration and subsequent settling of islands brought about major changes to the ecosystems, with dire consequences to island adapted species. The deliberate and indirect introductions of mammals contributed considerably to the decline of native and endemic species. Today, these introduced species continue to cause harm to island ecosystems and are assisted by even more deadly new introduced predators. Invasive species are one of three leading causes of biodiversity loss at the global scale. In the Pacific Islands they are the biggest cause of species extinction. The prognosis for island endemic species, as well as island ecosystems, does not look good, as more species are being transported to islands. It is imperative that coordinated efforts at all levels must be prioritised and implemented to give native and endemic species a fighting chance against invasive species, and to safeguard the foundation of island communities and economies. Local, national and regional efforts to safeguard island species as well as the wellbeing of communities and economic aspirations of countries are starting to make an impact in this area. -
Subduction History in the Melanesian Borderlands Region, SW Pacific
Subduction history in the Melanesian Borderlands region, SW Pacific Maria Seton1, Nicolas Flament, R. Dietmar Müller Keywords: Coral Sea, Melanesia, subduction, seafloor-spreading, SW Pacific, tectonics, geodynamics Abstract The easternmost Coral Sea region is an underexplored area at the northeasternmost corner of the Australian plate. Situated between the Mellish Rise, southern Solomon Islands, northern Vanuatu and New Caledonia, it represents one of the most dynamic and tectonically complex submarine regions of the world. Interactions between the Pacific and Australian plate boundaries have resulted in an intricate assemblage of deep oceanic basins and ridges, continental fragments and volcanic products; yet there is currently no clear conceptual framework to describe their formation. Due to the paucity of geological and geophysical data from the area to constrain plate tectonic models, a novel approach has been developed whereby the history of subduction based on a plate kinematic model is mapped to present-day seismic tomography models. A plate kinematic model, which includes a self-consistent mosaic of evolving plate boundaries through time is used to compute plate velocity fields and palaeo- oceanic age grids for each plate in 1 million year intervals. Figure 1. Regional digital elevation model (ETOPO2) of the eastern Coral Forward geodynamic models, with imposed surface plate velocity Sea. CT = Cato Trough, ERIR = East Rennell Island Ridge, LT = Louisiade trough, RFZ = Rennell Fracture Zone, RIR = Rennell Island Ridge, RT = constraints are computed using the 3D spherical finite element Rennell trough, SCT = San Cristobal Trench, SRT = South Rennell Trough, convection code CitcomS. A comparison between the present-day WTP = West Torres Plateau. -
Melanesia and Polynesia
Community Conserved Areas: A review of status & needs in Melanesia and Polynesia Hugh Govan With Alifereti Tawake, Kesaia Tabunakawai, Aaron Jenkins, Antoine Lasgorceix, Erika Techera, Hugo Tafea, Jeff Kinch, Jess Feehely, Pulea Ifopo, Roy Hills, Semese Alefaio, Semisi Meo, Shauna Troniak, Siola’a Malimali, Sylvia George, Talavou Tauaefa, Tevi Obed. February 2009 Acknowledgments Gratitude for interviews and correspondence is due to: Aliti Vunisea, Ana Tiraa, Allan Bero, Anne-Maree Schwarz, Bill Aalbersberg, Bruno Manele, Caroline Vieux, Delvene Notere, Daniel Afzal, Barry Lally, Bob Gillett, Brendon Pasisi, Christopher Bartlett, Christophe Chevillon, Christopher Bartlett, Dave Fisk, David Malick, Eroni Tulala Rasalato, Helen Sykes, Hugh Walton, Etika Rupeni, Francis Mamou, Franck Magron, Grazia Borrini-Feyerabend, Helen Perks, Hugh Walton, Isoa Korovulavula, James Comley, Jackie Thomas, Jacqueline Evans, Jane Mogina, Jo Axford, Johann Bell, John Parks, John Pita, Jointly Sisiolo, Julie Petit, Louise Heaps, Paul Anderson, Pip Cohen, Kiribati Taniera, Kori Raumea, Luanne Losi, Lucy Fish, Ludwig Kumoru, Magali Verducci, Malama Momoemausu, Manuai Matawai, Meghan Gombos, Modi Pontio, Mona Matepi, Olofa Tuaopepe, Pam Seeto, Paul Lokani, Peter Ramohia, Polangu Kusunan, Potuku Chantong, Rebecca Samuel, Ron Vave, Richard Hamilton, Seini Tawakelevu, Selaina Vaitautolu, Selarn Kaluwin, Shankar Aswani, Silverio Wale, Simon Foale, Simon Tiller, Stuart Chape, Sue Taei, Susan Ewen, Suzie Kukuian, Tamlong Tabb, Tanya O’Garra, Victor Bonito, Web Kanawi, -
Australia and Oceania: Physical Geography
R E S O U R C E L I B R A R Y E N C Y C L O P E D I C E N T RY Australia and Oceania: Physical Geography Encyclopedic entry. Oceania is a region made up of thousands of islands throughout the South Pacific Ocean. G R A D E S 6 - 12+ S U B J E C T S Biology, Earth Science, Geology, Geography, Human Geography, Physical Geography C O N T E N T S 10 Images For the complete encyclopedic entry with media resources, visit: http://www.nationalgeographic.org/encyclopedia/oceania-physical-geography/ Oceania is a region made up of thousands of islands throughout the Central and South Pacific Ocean. It includes Australia, the smallest continent in terms of total land area. Most of Australia and Oceania is under the Pacific, a vast body of water that is larger than all the Earth’s continental landmasses and islands combined. The name “Oceania” justly establishes the Pacific Ocean as the defining characteristic of the continent. Oceania is dominated by the nation of Australia. The other two major landmasses of Oceania are the microcontinent of Zealandia, which includes the country of New Zealand, and the eastern half of the island of New Guinea, made up of the nation of Papua New Guinea. Oceania also includes three island regions: Melanesia, Micronesia, and Polynesia (including the U.S. state of Hawaii). Oceania’s physical geography, environment and resources, and human geography can be considered separately. Oceania can be divided into three island groups: continental islands, high islands, and low islands.