CTI Sulu-Celebes Sea SFMP Project Document.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

CTI Sulu-Celebes Sea SFMP Project Document.Pdf UNDP Project Document Governments of Indonesia, Malaysia, Philippines United Nations Development Programme Implementation of the Sulu-Celebes Sea Sustainable Fisheries Management Project Brief Description The Sulu-Celebes Sea (SCS) is a Large Marine Ecosystem in the tropical seas of Asia bounded by three countries – Indonesia, Malaysia and the Philippines. Being at the heart of the most bio-diverse marine area in the world, the SCS is also a very rich fishing ground for large and small pelagic as well as bay and coral reef fishes, providing livelihoods to the coastal inhabitants and food for the entire region and beyond. The fishery resources, however, have declined due to various threats, including overexploitation, habitat and community modification and global climate change. The goal of the Project is to have an economically and ecologically sustainable marine fisheries in the SCS, for the benefit of communities who are dependent on these resources for livelihood and for the global community who benefit in the conservation of highly diverse marine ecosystems and its ecosystems services The objective of the Project is to improve the condition of fisheries and their habitats in the SCS through an integrated, collaborative and participatory management at the local, national and tri-national levels. The three countries and other stakeholders, including NGOs, have worked together to develop the Sulu-Sulawesi Marine Ecoregion Conservation Plan and formally put in place a regional institutional mechanism to implement the plan. The Project activities, outcomes and outputs will build on these strong regional and national initiatives. There are five major outcomes of the Project. The first is the achievement of a regional consensus on trans-boundary priorities and their immediate and root causes by updating an earlier Trans-boundary Diagnostic Analysis for the SCS and focusing on unsustainable exploitation of fisheries. The second outcome is agreement on regional measures for improved fisheries management through coordination in the formulation of a Strategic Action Program, which will build on the existing Ecoregion Conservation Plan. The third outcome is the strengthening of institutions and introduction of reforms to catalyze implementation of policies on reducing overfishing and improving fisheries management. The primary target for institutional strengthening is the Sulu-Sulawesi Marine Ecoregion Tri-National Committee and its Sub-Committees, in particular the Sub-Committee on Sustainable Fisheries. The fourth outcome is increased fish stocks of small pelagics through the implementation of best fisheries management practices in demonstration sites. The fifth outcome is the capture, application and dissemination of knowledge, lessons and best practices within the SCS and other LMEs. 1 Table of Contents SECTION I: ELABORATION OF THE NARRATIVE ........................................................................................... 5 PART I: SITUATION ANALYSIS .................................................................................................................................... 5 PART II: STRATEGY ................................................................................................................................................... 33 PART III: MANAGEMENT ARRANGEMENTS ............................................................................................................... 64 PART IV: MONITORING AND EVALUATION PLAN AND BUDGET ............................................................................... 68 PART V: LEGAL CONTEXT ....................................................................................................................................... 72 SECTION II: GEF INCREMENT AND STRATEGIC RESULTS FRAMEWORK ......................................... 75 PART I: INCREMENTAL COST AND PROJECT FINANCING ....................................................................................... 75 PART II: LOGICAL FRAMEWORK ANALYSIS ............................................................................................................ 79 SECTION III: TOTAL BUDGET AND WORK PLAN ......................................................................................... 93 SECTION IV: ADDITIONAL INFORMATION ................................................................................................... 101 PART I: OTHER AGREEMENTS ................................................................................................................................ 101 PART II: TERMS OF REFERENCE FOR KEY PROJECT STAFF AND KEY SUBCONTRACTS FUNDED BY GEF .............. 102 PART III: STAKEHOLDER INVOLVEMENT PLAN ......................................................................................... 106 SIGNATURE PAGE .................................................................................................................................................. 138 ANNEX 1 ..................................................................................................................................................................... 140 ANNEX 2 ..................................................................................................................................................................... 146 ANNEX 3 ..................................................................................................................................................................... 147 ANNEX 4 ..................................................................................................................................................................... 150 ANNEX 5 ..................................................................................................................................................................... 152 ANNEX 6 ..................................................................................................................................................................... 163 2 List of Acronyms ADB Asian Development Bank ASEAN Association of Southeast Asian Nations BFAR Bureau of Fisheries and Aquatic Resources (Philippines) BIMP-EAGA Brunei-Indonesia-Malaysia-Philippines East Asia Growth Area CI Conservation International COBSEA Coordinating Body on the Seas of East Asia CPUE Catch per Unit Effort CTI Coral Triangle Initiative CTI CFFC Coral Triangle Initiative on Coral Reefs, Fisheries and Food Securities and Adaptation to Climate Change CT6 Coral Triangle (6 countries) DOF Department of Fisheries, Sabah ECP Ecoregion Conservation Plan for SSME FAO Food and Agriculture Organisation, United Nations GEF Global Environment Facility GIWA Global International Waters Assessment IMP Indonesia, Malaysia, Philippines LME Large Marine Ecosystem MMAF Ministry of Marine Affairs and Fisheries (Indonesia) NPOA National Program of Action for CT countries PEMSEA Partnerships in Environmental Management for the Seas of East Asia PMU Project Management Unit PPG Project Preparation Grant RPOA Regional Program of Action for CT countries RPM Regional Program Manager SAP Strategic Action Program SEAFDEC Southeast Asian Fisheries Development Center SCS Sulu-Celebes Sea Large Marine Ecosystem SCS-SFM Sulu-Celebes Sea Sustainable Fisheries Management Project SSME Sulu-Sulawesi Marine Ecoregion TDA Transboundary Diagnostic Analysis TNC The Nature Conservancy 3 UNDP United Nations Development Program USAID United States Agency for International Development WWF World Wide Fund for Nature 4 SECTION I: ELABORATION OF THE NARRATIVE PART I: Situation Analysis Context and global significance Sulu-Celebes Sea Large Marine Ecosystem 1. The Sulu-Celebes Sea1 (SCS) is a Large Marine Ecosystem2 (LME) in the tropical seas of Asia, containing a geographically distinct assemblage of natural communities that share a large number of common species, dynamics, and conditions3. The SCS is a semi-enclosed LME with an area of 900,000 km2, and is composed of two marine basins – the Sulu Sea and the Celebes- Sulawesi Sea. The two marine basins are separated by the Tawi-Tawi Ridge but are inter- connected by the movement of marine waters4. The Pacific Ocean flows into Sulu Sea in northern Mindanao and between Sangihe-Talaud Archipelago, North Sulawesi. Surface waters from one basin overflow to the other every two weeks and through-flows through the Tawi- Tawi-Sulu Archipelago occur during monsoons. An internal wave moves back and forth from the Tubbataha Ridge towards the east coast of Palawan Island. 2. The dynamic movement of marine waters in the Sulu-Celebes Sea circulates rich nutrients and larval stages of many marine species across political boundaries. The upwelling along the northwestern edge of the Tawi-Tawi Ridge enriches surface waters that are exchanged between Sulu and Sulawesi Seas and are circulated around by monsoonal winds. The circulation of waters explain the export of larvae from a spawning ground to distant settlement habitats, e.g., from Tubbataha Reef to Palawan Island and Sabah, north Borneo, from Surigao to Bohol Sea. 3. The direction of transport of nutrients and larval stages varies with the monsoons5. During the northeast monsoon, the waters from the Pacific Ocean enter Sulu Sea north of Mindanao and divide into two – one moving northward towards Mindoro Island and exiting to the South China Sea, and the other moving southward and clock-wise to Tawi-Tawi, east coast of Sabah, and exiting through Balabac Strait to the South China Sea. In Sulawesi Sea, the marine waters enter Makassar
Recommended publications
  • Mantle Structure and Tectonic History of SE Asia
    Nature and Demise of the Proto-South China Sea ROBERT HALL, H. TIM BREITFELD SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey, TW20 0EX, United Kingdom Abstract: The term Proto-South China Sea has been used in a number of different ways. It was originally introduced to describe oceanic crust that formerly occupied the region north of Borneo where the modern South China Sea is situated. This oceanic crust was inferred to have been Mesozoic, and to have been eliminated by subduction beneath Borneo. Subduction was interpreted to have begun in Early Cenozoic and terminated in the Miocene. Subsequently the term was also used for inferred oceanic crust, now disappeared, of quite different age, notably that interpreted to have been subducted during the Late Cretaceous below Sarawak. More recently, some authors have considered that southeast-directed subduction continued until much later in the Neogene than originally proposed, based on the supposition that the NW Borneo Trough and Palawan Trough are, or were recently, sites of subduction. Others have challenged the existence of the Proto-South China Sea completely, or suggested it was much smaller than envisaged when the term was introduced. We review the different usage of the term and the evidence for subduction, particularly under Sabah. We suggest that the term Proto-South China Sea should be used only for the slab subducted beneath Sabah and Cagayan between the Eocene and Early Miocene. Oceanic crust subducted during earlier episodes of subduction in other areas should be named differently and we use the term Paleo- Pacific Ocean for lithosphere subducted under Borneo in the Cretaceous.
    [Show full text]
  • A Gravity High in Darvel Bay
    Ceol. Soc. MaLaYJia, BulLetill 59, July 1996,. pp. 1lJ-122 A gravity high in Darvel Bay PATRICK J.e. RYALL! AND DWAYNE BEATTIE2 1 Department of Geology Dalhousie University Halifax, Nova Scotia Canada B3H 3J5 2Geoterrex Ltd. 2060 Walkley Road Ottawa, Ontario Canada K1 G 3P5 Abstract: A gravity survey was carried out along the coastlines of Darvel Bay and many of the islands (e.g. Sakar, Tabauwan, Silumpat) in the Bay. In addition stations were located along the road from Kunak to Lahad Datu. The resulting Bouguer anomaly map shows a broad gravity high of at least 60 mgal which strikes west northwest with its maximum on the southern coast of Pulau Sakar. The anomaly narrows and decreases where it comes ashore and may continue along the Silam-Beeston Complex. This large positive anomaly suggests that there is an extensive ultramafic body beneath Darvel Bay. The gravity anomaly can best be modelled as a 3 to 5 km thick slab of ultramafic rock under the Bay with amphibolites on its northern and southern edges dipping away from the Bay. This model is consistent with a folded structure which brings upper mantle rocks to the surface. It is unlikely that there is a significant thickness of Chert-Spilite Formation beneath Darvel Bay, although the gravity data w.ould permit a thickness of up to a few hundred metres. INTRODUCTION Hutchison (1968,1975) considers the ophiolitic rocks of Darvel Bay as part of a strongly arcuate Borneo line which runs from the Sulu Archipelago in the northeast, through Darvel Bay and northwestern The island of Borneo is located in a complex Sabah and along Palawan (Fig.
    [Show full text]
  • Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey
    Downloaded from orbit.dtu.dk on: Oct 05, 2021 Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey Fauzi Nordin, Ahmad; Jamil, Hassan; Noor Isa, Mohd; Mohamed, Azhari; Hj. Tahir, Sanudin; Musta, Baba ; Forsberg, René; Olesen, Arne Vestergaard; Nielsen, Jens Emil; Majid A. Kadir, Abd Total number of authors: 13 Published in: Borneo Science, The Journal of Science and Technology Publication date: 2016 Document Version Publisher's PDF, also known as Version of record Link back to DTU Orbit Citation (APA): Fauzi Nordin, A., Jamil, H., Noor Isa, M., Mohamed, A., Hj. Tahir, S., Musta, B., Forsberg, R., Olesen, A. V., Nielsen, J. E., Majid A. Kadir, A., Fahmi Abd Majid, A., Talib, K., & Aman Sulaiman, S. (2016). Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey. Borneo Science, The Journal of Science and Technology, 37(2), 14-27. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Users may download and print one copy of any publication from the public portal for the purpose of private study or research. You may not further distribute the material or use it for any profit-making activity or commercial gain You may freely distribute the URL identifying the publication in the public portal If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim.
    [Show full text]
  • Curriculum Vite
    BIODATA Ejria Binti Saleh Senior Lecturer, Borneo Marine Research Institute, Universiti Malaysia Sabah, Malaysia BIO SUMMARY - LIM AI YIM - MALAYSIA CURRICULUM VITE PERSONAL INFORMATION Name Name of Current Employer: Borneo Marine Research Institute Ejria Binti Saleh Universiti Malaysia Sabah Corresponding Address: E-mail: Borneo Marine Research Institute, [email protected]/[email protected] Universiti Malaysia Sabah, 88999 Kota Kinabalu, Sabah Malaysia Tel: 6088-320000 ext: 2594 Fax: 6088-320261 NRIC: 710201-12-5042 Nationality: Malaysian Date of Birth: 01 January 1971 Sex: Female ACADEMIC QUALIFICATION Diploma/Degree Name of University Year Major Doctor of Philosophy Universiti Malaysia 2007 Physical Oceanography Sabah, Malaysia. Master Science University of Liverpool, 1997 Recent Environmental United Kingdom. Change Bachelor of Fisheries Universiti Putra 1996 Marine science Sc. (Marine Sciences) Malaysia, Malaysia. 1 Diploma in Fisheries Universiti Putra 1993 Fisheries Malaysia, Malaysia. RESEARCH PROJECTS Project Project Title Role Year Funder Status No. B-08-0- Tidal effects on salinity Co- 2002-2003 FRGS Completed 12ER intrusion and suspended Researcher sediment discharged in Manggatal River Estuary, Sabah SCF0019- Study of the factors regulating Co- 2006 -2009 Science Completed AGR-2006 the bloom mechanisms of Researcher Fund harmful algal species in Sabah SCF0015- Coastal processes and Co- 2006 -2009 Science Completed ENV-2006 geomorphologic Researcher Fund characteristics of major coastal towns in East Sabah for assessment
    [Show full text]
  • South-East Asia Second Edition CHARLES S
    Geological Evolution of South-East Asia Second Edition CHARLES S. HUTCHISON Geological Society of Malaysia 2007 Geological Evolution of South-east Asia Second edition CHARLES S. HUTCHISON Professor emeritus, Department of geology University of Malaya Geological Society of Malaysia 2007 Geological Society of Malaysia Department of Geology University of Malaya 50603 Kuala Lumpur Malaysia All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior permission of the Geological Society of Malaysia ©Charles S. Hutchison 1989 First published by Oxford University Press 1989 This edition published with the permission of Oxford University Press 1996 ISBN 978-983-99102-5-4 Printed in Malaysia by Art Printing Works Sdn. Bhd. This book is dedicated to the former professors at the University of Malaya. It is my privilege to have collabo­ rated with Professors C. S. Pichamuthu, T. H. F. Klompe, N. S. Haile, K. F. G. Hosking and P. H. Stauffer. Their teaching and publications laid the foundations for our present understanding of the geology of this complex region. I also salute D. ]. Gobbett for having the foresight to establish the Geological Society of Malaysia and Professor Robert Hall for his ongoing fascination with this region. Preface to this edition The original edition of this book was published by known throughout the region of South-east Asia. Oxford University Press in 1989 as number 13 of the Unfortunately the stock has become depleted in 2007. Oxford monographs on geology and geophysics.
    [Show full text]
  • 25 the Land Capability Classification of Sabah Volume 2 the Sandakan Residency
    25 The land capability classification of Sabah Volume 2 The Sandakan Residency Q&ffls) (Kteg®QflK§@© EAï98©8CöXjCb Ö^!ÖfiCfDÖ©ÖGr^7 CsX? (§XÄH7©©©© Cß>SFMCS0®E«XÄJD(SCn3ß Scanned from original by ISRIC - World Soil Information, as i(_su /Vorld Data Centre for Soils. The purpose is to make a safe jepository for endangered documents and to make the accrued nformation available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the naterials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the >riginators. For questions please contact soil.isricOwur.nl ndicating the item reference number concerned. The land capability classification of Sabah Volume 2 The Sandakan Residency 1M 5>5 Land Resources Division The land capability classification of Sabah Volume 2 The Sandakan Residency P Thomas, F K C Lo and A J Hepburn Land Resource Study 25 Land Resources Division, Ministry of Overseas Development Tolworth Tower, Surbiton, Surrey, England KT6 7DY 1976 in THE LAND RESOURCES DIVISION The Land Resources Division of the Ministry of Overseas Development assists developing countries in mapping, investigating and assessing land resources, and makes recommendations on the use of these resources for the development of agriculture, livestock husbandry and forestry; it also gives advice on related subjects to overseas governments and organisations, makes scientific personnel available for appointment abroad and provides lectures and training courses in the basic techniques of resource appraisal. The Division works in close co-operation with government departments, research institutes, universities and international organisations concerned with land resource assessment and development planning.
    [Show full text]
  • INDIGENOUS GROUPS of SABAH: an Annotated Bibliography of Linguistic and Anthropological Sources
    INDIGENOUS GROUPS OF SABAH: An Annotated Bibliography of Linguistic and Anthropological Sources Part 1: Authors Compiled by Hans J. B. Combrink, Craig Soderberg, Michael E. Boutin, and Alanna Y. Boutin SIL International SIL e-Books 7 ©2008 SIL International Library of Congress Catalog Number: 2008932444 ISBN: 978-155671-218-0 Fair Use Policy Books published in the SIL e-Books series are intended for scholarly research and educational use. You may make copies of these publications for research or instructional purposes (under fair use guidelines) free of charge and without further permission. Republication or commercial use of SILEB or the documents contained therein is expressly prohibited without the written consent of the copyright holder(s). Series Editor Mary Ruth Wise Volume Editor Mae Zook Compositor Mae Zook The 1st edition was published in 1984 as the Sabah Museum Monograph, No. 1. nd The 2 edition was published in 1986 as the Sabah Museum Monograph, No. 1, Part 2. The revised and updated edition was published in 2006 in two volumes by the Malaysia Branch of SIL International in cooperation with the Govt. of the State of Sabah, Malaysia. This 2008 edition is published by SIL International in single column format that preserves the pagination of the 2006 print edition as much as possible. Printed copies of Indigenous groups of Sabah: An annotated bibliography of linguistic and anthropological sources ©2006, ISSN 1511-6964 may be obtained from The Sabah Museum Handicraft Shop Main Building Sabah Museum Complex, Kota Kinabalu, Sabah,
    [Show full text]
  • Geological Heritage Features of Tawau Volcanic Sequence, Sabah
    Bulletin of the Geological Society of Malaysia 56 (2010) 79 – 85 Geological heritage features of Tawau volcanic sequence, Sabah Sanudin Tahir, BaBa MuSTa & iSMail aBd rahiM Geology Programme, School of Science and Technology Universiti Malaysia Sabah, 88999 Kota Kinabalu, Sabah Abstract­­— Semporna Peninsula area was built up by thick Tertiary sequence of volcanic flows and volcaniclastic rocks. Early Cretaceous tholeiite basalt is the oldest sequence of volcanic rocks interpreted to have formed as part of a wide spread submarine volcano or volcanic complex within an MORB characterized by rapid volcanism. Miocene to Quaternary volcanisms from volcanic arcs contributed sequences of lava flows and pyroclastic rocks of dacitic, andesitic and basaltic rock types forming the major mountain chains of southeast Sabah. This Neogene volcanic sequence is dominated by low to high K-calc alkaline andesitic to dacitic volcanic rocks similar to modern island arc type. The subaerial of the latest lava flows of the region indicates volcanism consistent with tholeiitic basalt type. It has been accepted that during the Cenozoic, Sabah has been subjected to series of major tectonic regimes. A number of deformation phases have been determined include: Middle Eocene, Middle Miocene and Plio-Pleistocene phases of crustal movements of this region. The area appeared, therefore, to have been subjected to compressional tectonic regime throughout much of the late Cenozoic. However, the structural and sedimentological expression of these tectonic regimes varies considerably. It is suggested here that compressional episodes were interspersed with periods of active transtensional basin formation and that Late Miocene extension of the eastern part of Sabah which was related to compressional forces.
    [Show full text]
  • Status of Coral Reefs in Malaysia, 2019
    Status of Coral Reefs in Malaysia, 2019 Reef Check Malaysia Contents Executive Summary 1 1 Introduction 2 2 Reef Check 3 2.1 Background 3 2.2 Survey Methodology 3 2.3 Survey Sites 4 3 2019 Survey Results & Analysis 5 3.1 Status of Coral Reefs in Malaysia 5 3.2 Status of Coral Reefs in Key Eco-regions in Malaysia 10 Sunda Shelf 12 Malacca Strait 36 North Borneo 42 4 Reef Check Data Over the Year 60 4.1 Peninsular versus East Malaysia over 13 Years 60 4.2 Changing Reef Health in Selected Areas 65 5 Summary and Recommendations 75 5.1 Summary 75 5.2 Recommendations 76 5.3 Conclusion 77 Acknowledgements 78 References 81 Appendix 1: 2019 Survey Sites 82 Saving Our Reefs Research, Education, Conservation Executive Summary 1. A total of 180 sites were surveyed in 2019 (2018: 212), 97 in Peninsular Malaysia and 83 in East Malaysia. The surveys are a continuation of a successful National Reef Check Survey Programme that has now run for thirteen years. 2. The surveys were carried out by trained volunteers as well as government officials from Marine Parks Malaysia, reflecting commitment from the Government in further improving management of Malaysia’s coral reefs. Surveys were carried out on several islands off Peninsular Malaysia’s East and West coast, covering both established Marine Protected Areas (MPAs) and non-protected areas, and in various parts of East Malaysia, both Sabah and Sarawak. 3. The results indicate that the Malaysian coral reefs surveyed have a relatively high level of living coral, at 40.63% (2018: 42.42%).
    [Show full text]
  • Borneo: Treasure Island at Risk
    Borneo: Treasure Island at Risk Status of Forest, Wildlife and related Threats on the Island of Borneo Acknowledgement The following persons provided valuable advice and information to this report: - Fitrian Ardiansyah, WWF Indonesia - Stuart Chapman, WWF Indonesia - David S. Edwards, University of Brunei Darussalam - Nina Griesshammer, WWF Germany - Mirjam Müller, WWF Germany - Bambang Supriyanto, WWF Indonesia - Junaidi Payne, WWF Malaysia - Florian Siegert, Ludwig-Maximilians-University of Munich - Lely Rulia Siregar, Indonesian Ministry of Forestry - Alois Vedder, WWF Germany - Stefan Ziegler, WWF Germany Published by: WWF Germany, Frankfurt am Main, June 2005 Authors: Mario Rautner, Consultant, Borealis Centre for Environment and Trade Research Martin Hardiono (maps), Consultant Raymond J. Alfred (Sabah maps), WWF Malaysia Coordinator: Markus Radday, WWF Germany, Assistance: Mirjam Müller, WWF Germany Contact: Markus Radday, WWF Germany, phone +49 69 7 91 44-189; e-mail: [email protected] Layout text: Astrid Ernst Production Rainer Litty, WWF Germany Printed on recycled paper © 2005 WWF Germany, Frankfurt am Main Any reproduction in full or in part of this publication must mention the title and credit of the above mentioned publisher as the copyright owner. Cover photo: © WWF Jikkie Jonkman / Alain Compost Preface The forests of Borneo are rapidly disappearing: A man-made disaster. A few decades ago the third largest island on our planet was still covered by a vast green carpet of lush rainforest. These forests are invaluable because of the diversity of unique plants and animals they harbour: Majestic species such as orang-utans, elephants and rhinos, to name but a few. Equally important: They are of critical value to people, both as a prized natural heritage and for the goods and services that they provide.
    [Show full text]
  • PROCEEDINGS NATIONAL GEOSCIENCE CONFERENCE 2012 Pullman Hotel Kuching, Sarawak 23 – 24 June 2012 Geoscience I Every Life
    PERSATUAN GEOLOGI MALAYSIA GEOLOGICAL SOCIETY OF MALAYSIA PROCEEDINGS NATIONAL GEOSCIENCE CONFERENCE 2012 Pullman Hotel Kuching, Sarawak 23 – 24 June 2012 Geoscience I Every Life Co-organisers Minerals & Geoscience Academy of Sciences Department Malaysia Malaysia PERSATUAN GEOLOGI MALAYSIA Geological Society of Malaysia Council 2012/2013 President : Joy Jacqueline Pereira Vice President : Mazlan Madon Secretary : Ling Nan Ley Assistant Secretary : Lim Choun Sian Treasurer : Ahmad Nizam Hasan Editor : Ng Tham Fatt Immediate Past President : Dato’ Yunus Abdul Razak Councillors : Gan Lay Chin Liaw Kim Kiat Meor Hakif Amir Hassan Nicholas Jacob Nur Iskandar Taib Robert Wong Tan Boon Kong Tanot Unjah NATIONAL GEOSCIENCE CONFERENCE 2012 Organising Committee Advisor : Joy Jacqueline Pereira Alexander Unya Ambun Chairman : Richard Mani Banda Secretary I : Mohd Yusop Ramli Secretary II : Thomson Galin Treasurer : Redzuan Ahmad Banjar Ahmad Nizam Hasan ASM Representative : P. Loganathan Technical Programme : Roslan Rajali Ng Tham Fatt Ling Nan Ley Che Abd. Rahman Jaafar Richard Batoi Protocol And Souvenir : Japri Bujang Azuddin Shebli Hermawati Tambeng Venue and Registration : Manggon Abot Halimat Mat Anna Lim Rosmah Usup Poster and Exhibition : Paulius Godwin SegarVelayutham Logistics : Zamzuri Ghazali Md. Shahrizal Md. Sharifoddin Geri Ginung IT Facilities and AV : Ajon Winnie Sylvia Joseph Nurul Shiema Shahadan Field Trip : Dana Badang Nazirrahmat Suleiman Master Of Ceremony : Pandi Kipli Marina Mardzuki Kennedy Mohd. Imran Publicity : Iskandar Taib Photography : Edward Muol Yong Mei Ling Khalid Kasdi PERSATUAN GEOLOGI MALAYSIA GEOLOGICAL SOCIETY OF MALAYSIA Proceedings NATIONAL GEOSCIENCE CONFERENCE 2012 Pullman Hotel Kuching, Sarawak 23 – 24 June 2012 Geoscience I EveryCompilers: Ng Tham Fatt Life Richard Mani Banda Mohd Yusop Ramli Roslan Rajali Ling Nan Ley Wong Yien Lim Co-organisers Minerals & Geoscience Academy of Sciences Department Malaysia Malaysia ISBN 978-983-99102-9-2 Copyright: Geological Society of Malaysia, 2012 All rights reserved.
    [Show full text]
  • ABSTRACT the Bajau Laut Or Sea Bajau Or Also Often Referred to with the Derogatory Label Palauh by Other Communities, Are Known
    Jurnal Kinabalu Bil. 26(2), 183-196, Disember 2020 E-ISSN 2600-867X© Wan Shawaluddin Wan Hassan & Diana Peters THE VULNERABILITY OF BAJAU LAUT AS STATELESS PEOPLE IN SABAH WAN SHAWALUDDIN WAN HASSAN1 DIANA PETERS2 1&2Faculty of Social Sciences and Humanities, Universiti Malaysia Sabah, 88400 Kota Kinabalu, Sabah. [email protected] Date Received: 16 July 2020 / Date Accepted: 10 October 2020 ABSTRACT The Bajau Laut or Sea Bajau or also often referred to with the derogatory label Palauh by other communities, are known to be living within their ancestral domain of the Sulu and the Celebes Seas or the Sulu- Semporna-South Sulawesi Triangle. During the pre-British period, their mobility around this region was well established as part of their civilization and was not an issue with other peoples in the land-based territories. However, the legal status of the Bajau Laut became problematic when citizenship and territories were formalized by the emergence of the nation- states of the Philippines, Malaysia and Indonesia. In the case of the Bajau Laut population located on the Malaysian side of Sabah, the dynamics of their own internal development has become more complicated. In Sabah, there are three groups of Bajau: The West Coast Bajau, the various groups of East Coast Bajau and the Bajau Laut who can be found along Sabah’s east coast, and around the islands off of Semporna. These three groups can be differentiated by their language and dialects, as well as livelihood, status in life, education, community structure and their general worldviews. The West Coast Bajau and the East Coast Bajau have slowly integrated themselves into the Malaysian society, while the Bajau Laut continues their semi- nomadic life at sea and are generally regarded as stateless by the Malaysian Government.
    [Show full text]