Preliminary Checklist of Cetacea in the Indonesian Archipelago and Adjacent Waters
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Resolution 3.11 Conservation Plan for Black Sea Cetaceans
ACCOBAMS-MOP3/2007/Res.3.11 RESOLUTION 3.11 CONSERVATION PLAN FOR BLACK SEA CETACEANS The Meeting of the Parties to the Agreement on the Conservation of Cetaceans of the Black Sea, Mediterranean Sea and contiguous Atlantic area: On the recommendation of the ACCOBAMS Scientific Committee, Aware that all three Black Sea cetacean species, the harbour porpoise (Phocoena phocoena), the short-beaked common dolphin (Delphinus delphis) and the common bottlenose dolphin (Turpsiops truncatus), experienced a dramatic decline in abundance during the twentieth century, Taking into account that the International Union for the Conservation of Nature (IUCN)-ACCOBAMS workshop on the Red List Assessment of Cetaceans in the ACCOBAMS Area (Monaco, March 2006) concluded that the Black Sea populations of the harbour porpoise, common dolphin and bottlenose dolphin are endangered, Conscious that most of the factors responsible for their decline, such as current fisheries by-catches, extensive habitat degradation and other anthropogenic impacts, pose continuous threats to the existence of cetaceans in the Black Sea and contiguous waters, represented by the Sea of Azov, the Kerch strait and the Turkish straits system (including the Bosphorus strait, the Marmara Sea and the Dardanelles straits), Convinced that the plan is an integral component of discussions on Black Sea regional and national strategies, plans, programmes and projects concerned with the protection, exploration and management of the Black Sea environment, biodiversity, living resources, marine mammals -
Islam and Politics in Madura: Ulama and Other Local Leaders in Search of Influence (1990 – 2010)
Islam and Politics in Madura: Ulama and Other Local Leaders in Search of Influence (1990 – 2010) Islam and Politics in Madura: Ulama and Other Local Leaders in Search of Influence (1990 – 2010) Proefschrift ter verkrijging van de graad van Doctor aan de Universiteit Leiden, op gezag van Rector Magnificus prof.mr. C.J.J.M. Stolker, volgens besluit van het College voor Promoties te verdedigen op woensdag 28 augustus 2013 klokke 13.45 uur door Yanwar Pribadi geboren te Sukabumi in 1978 Promotiecommissie Promotor : Prof. dr. C. van Dijk Co-Promotor : Dr. N.J.G. Kaptein Overige Leden : Prof. dr. L.P.H.M. Buskens Prof. dr. D.E.F. Henley Dr. H.M.C. de Jonge Layout and cover design: Ade Jaya Suryani Contents Contents, ................................................................................ vii A note on the transliteration system, ..................................... xi List of tables and figures, ........................................................ xiii Acknowledgements, ................................................................ xv Maps, ....................................................................................... xviii Chapter 1 Introduction, .......................................................................... 1 Madura: an island of piety, tradition, and violence, .............. 1 Previous studies, ..................................................................... 3 Focus of the study, .................................................................. 9 Methods and sources, ............................................................ -
SCHAPPER, Antoinette and Emilie WELLFELT. 2018. 'Reconstructing
Reconstructing contact between Alor and Timor: Evidence from language and beyond a b Antoinette SCHAPPER and Emilie WELLFELT LACITO-CNRSa, University of Colognea, and Stockholm Universityb Despite being separated by a short sea-crossing, the neighbouring islands of Alor and Timor in south-eastern Wallacea have to date been treated as separate units of linguistic analysis and possible linguistic influence between them is yet to be investigated. Historical sources and oral traditions bear witness to the fact that the communities from both islands have been engaged with one another for a long time. This paper brings together evidence of various types including song, place names and lexemes to present the first account of the interactions between Timor and Alor. We show that the groups of southern and eastern Alor have had long-standing connections with those of north-central Timor, whose importance has generally been overlooked by historical and linguistic studies. 1. Introduction1 Alor and Timor are situated at the south-eastern corner of Wallacea in today’s Indonesia. Alor is a small mountainous island lying just 60 kilometres to the north of the equally mountainous but much larger island of Timor. Both Alor and Timor are home to a mix of over 50 distinct Papuan and Austronesian language-speaking peoples. The Papuan languages belong to the Timor-Alor-Pantar (TAP) family (Schapper et al. 2014). Austronesian languages have been spoken alongside the TAP languages for millennia, following the expansion of speakers of the Austronesian languages out of Taiwan some 3,000 years ago (Blust 1995). The long history of speakers of Austronesian and Papuan languages in the Timor region is a topic in need of systematic research. -
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Vol. 6: 173–184, 2008 ENDANGERED SPECIES RESEARCH Printed December 2008 doi: 10.3354/esr00102 Endang Species Res Published online August 21, 2008 Contribution to the Theme Section ‘The IUCN Red List of Threatened Species: assessing its utility and value’ OPENPEN ACCESSCCESS Challenges of assessing cetacean population recovery and conservation status Milton M. R. Freeman* Canadian Circumpolar Institute, University of Alberta, Edmonton, Alberta T6G 2E1, Canada ABSTRACT: This paper examines the extent to which depleted whale populations have recovered (or not) and their perceived current conservation status and prognosis for continued survival, as repre- sented in the International Union for Conservation of Nature and Natural Resources (IUCN) Red Lists. It is concluded that current hypothetical and untested predictions of extinction risk, while in many cases drawing attention to justifiable conservation needs, may seriously undervalue the resilience of species that have evolved to live in a dynamic and ever-changing reality including cen- turies of heavy exploitation by humankind. The paper questions the appropriateness of Red Listing criteria for long-lived highly mobile ocean-dwelling species that are scarcely affected by the princi- pal threats upon terrestrial or aquatic species living in relatively restricted areas subject to habitat fragmentation and/or loss. This analysis draws attention to the problems associated with objectively assessing the conservation status of charismatic species and the value conflicts that may override evidence-based scientific conservation assessments. KEY WORDS: Whales · Whaling · Conservation · Population recovery · Predicting extinction · Red Listing · Charismatic species Resale or republication not permitted without written consent of the publisher INTRODUCTION of the bowhead whale Balaena mysticetus; both are believed to number in the tens or low hundreds at this The history of whaling provides one of the best- time. -
Tribal Weaving of the Lesser Sunda Islands
TRIBAL WEAVING OF THE LESSER SUNDA ISLANDS The diverse Lesser Sunda Islands, stretching eastwards from Bali, offer the most amazing landscapes and a glorious cornucopia of weaving for textile lovers. Here women not only continue to make their traditional cloth on back-tension looms but continue to wear it as well. There is kaleidoscopic variety of patterns and designs – every region of every island has its own unique textile culture, its own style of dress, and its own motifs. Together we will explore the extraordinary ancestral traditions of these islands where textiles are the predominant form of artistic expression, still playing a central role in every significant stage of life, especially marriage and death. Some islanders tell us, “Without cloth we cannot marry.” However, change is underway series of evening talks. Please Note: The price of this cruise in even the remotest villages, and weavers are no longer does not include any domestic airfares to and from our start passing on their skills to the next generation. With this cruise, and end points. If you are booking by yourself, please check we will be given a unique opportunity to witness a dying art form with us first to find out the best routes to take, and to ensure before it is gone forever. We will enjoy the luxury of cruising that you arrive at your destination with plenty of time to spare. effortlessly from island to island, crossing a rugged, isolated Except for Bali, transfers to and from local airports to the boat region where travel by land can be difficult. -
Delineation of Sedimentary Subbasin and Subsurface Interpretation East Java Basin in the Madura Strait and Surrounding Area Based on Gravity Data Analysis
Bulletin of the Marine Geology, Vol. 34, No. 1, June 2019, pp. 1 to 16 Delineation of Sedimentary Subbasin and Subsurface Interpretation East Java Basin in the Madura Strait and Surrounding Area Based on Gravity Data Analysis Delineasi Subcekungan Sedimen dan Interpretasi Bawah Permukaan Cekungan Jawa Timur Wilayah Selat Madura dan Sekitarnya Berdasarkan Analisis Data Gayaberat Imam Setiadi1, Budi Setyanta2, Tumpal B. Nainggolan1, Joni Widodo1 1 Marine Geological Institute, Jl. Dr. Djundjunan No. 236, Bandung, 40174, Indonesia. 2 Centre for Geological Survey, Jl.Diponegoro No.57. Bandung, 40122, Indonesia. Corresponding author: [email protected] (Received 08 January 2019; in revised form 15 January 2019 accepted 27 March 2019) ABSTRACT: East Java basin is a very large sedimentary basin and has been proven produce hydrocarbons, this basin consists of several different sub-basins, one of the sub-basin is in the Madura Strait and surrounding areas. Gravity is one of the geophysical methods that can be used to determine geological subsurface configurations and delineate sedimentary sub-basin based on density parameter. The purposes of this study are to delineate sedimentary sub-basins, estimate the thickness of sedimentary rock, interpret subsurface geological model and identify geological structures in the Madura Strait and surrounding areas. Data analysis which used in this paper are spectral analysis, spectral decomposition filter and 2D forward modeling. The results of the spectral analysis show that the thickness of sedimentary rock is about 3.15 Km. Spectral decomposition is performed at four different wave numbers cut off, namely (0.36, 0.18, 0.07 and 0.04), each showing anomaly patterns at depth (1 Km, 2 Km, 3 Km and 4 Km). -
Holocene Climate Dynamics in Sumba Strait, Indonesia: a Preliminary Evidence from High Resolution Geochemical Records and Planktonic Foraminifera
Studia Quaternaria, vol. 37, no. 2 (2020): 91–99 DOI: 10.24425/sq.2020.133753 HOLOCENE CLIMATE DYNAMICS IN SUMBA STRAIT, INDONESIA: A PRELIMINARY EVIDENCE FROM HIGH RESOLUTION GEOCHEMICAL RECORDS AND PLANKTONIC FORAMINIFERA Purna Sulastya Putra*, Septriono Hari Nugroho Research Center for Geotechnology LIPI, Kompleks LIPI Gd 80, Jalan Sangkuriang Bandung 40135 Indonesia; e-mail: [email protected] * corresponding author Abstract: The dynamics of climatic conditions during the Holocene in the Sumba Strait is not well known, compared with in the Indian Ocean. The aim of this paper is to identify the possible Holocene climate dynamics in Sumba Strait, east- ern Indonesia by using deep-sea core sediments. A 243 cm core was taken aboard RV Baruna Jaya VIII during the Ekspedisi Widya Nusantara 2016 cruise. The core was analyzed for elemental, carbonate and organic matter content, and abundance of foraminifera. Based on geochemical and foraminifera data, we were able to identify at least six climatic changes during the Holocene in the Sumba Strait. By using the elemental ratio of terrigenous input parameter, we infer to interpret that the precipitation in the Sumba Strait during the Early Holocene was relatively higher compared with the Mid to Late Holocene. Key words: climate dynamics, planktonic foraminifera, Holocene deep-sea sediment, Sumba Strait Manuscript received 20 September 2019, accepted 9 March 2020 INTRODUCTION The Holocene climatic changes were recorded in the Sumba region, eastern Indonesia (Ardi, 2018). However, Global mean surface temperature warmed by 0.85°C most of the palaeoclimate reconstructions in this region between 1880 and 2012, as reported in the IPCC Fifth and adjacent area were based on coral data (e.g. -
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Composition and Distribution of Dolphin in Savu Sea National Marine Park, East Nusa Tenggara (Mujiyanto., et al) Available online at: http://ejournal-balitbang.kkp.go.id/index.php/ifrj e-mail:[email protected] INDONESIANFISHERIESRESEARCHJOURNAL Volume 23 Nomor 2 December 2017 p-ISSN: 0853-8980 e-ISSN: 2502-6569 Accreditation Number: 704/AU3/P2MI-LIPI/10/2015 COMPOSITION AND DISTRIBUTION OF DOLPHIN IN SAVU SEA NATIONAL MARINE PARK, EAST NUSA TENGGARA Mujiyanto*1, Riswanto1, Dharmadi2 and Wildan Ghiffary3 1Research Institute for Fisheries Enhancement and Conservation, Cilalawi Street No. 1, Jatiluhur Purwakarta, West Java Indonesia - 41152 2Center for Fisheries Research and Development, Ancol – Jakarta, Indonesia 3Fusion for Nature - Master Candidate of Wageningen University, Drovendaalsesteeg 4, 6708 PB Wageningen, Belanda Received; Februari 20-2017 Received in revised from December 22-2017; Accepted December 28-2017 ABSTRACT Dolphins are one of the most interesting cetacean types included in family Delphinidae or known as the oceanic dolphins from genus Stenella sp. and Tursiops sp. Migration and abundance of dolphins are affected by the presence of food and oceanographic conditions. The purpose of this research is to determine the composition and distribution of dolphins in relation to the water quality parameters. Benefits of this research are expected to provide information on the relationship between distributions of the family Delphinidae cetacean (oceanic dolphins) and oceanographic conditions. The method for this research is descriptive exploratory, with models onboard tracking survey. Field observations were done in November 2015 and period of March-April 2016 outside and inside Savu Sea National Marine Park waters. The sighting of dolphin in November and March- April found as much seven species: bottlenose dolphin, fraser’s dolphin, pantropical spotted dolphin, risso’s dolphin, rough-toothed dolphin, spinner dolphin and stripped dolphin. -
Order CETACEA Suborder MYSTICETI BALAENIDAE Eubalaena Glacialis (Müller, 1776) EUG En - Northern Right Whale; Fr - Baleine De Biscaye; Sp - Ballena Franca
click for previous page Cetacea 2041 Order CETACEA Suborder MYSTICETI BALAENIDAE Eubalaena glacialis (Müller, 1776) EUG En - Northern right whale; Fr - Baleine de Biscaye; Sp - Ballena franca. Adults common to 17 m, maximum to 18 m long.Body rotund with head to 1/3 of total length;no pleats in throat; dorsal fin absent. Mostly black or dark brown, may have white splotches on chin and belly.Commonly travel in groups of less than 12 in shallow water regions. IUCN Status: Endangered. BALAENOPTERIDAE Balaenoptera acutorostrata Lacepède, 1804 MIW En - Minke whale; Fr - Petit rorqual; Sp - Rorcual enano. Adult males maximum to slightly over 9 m long, females to 10.7 m.Head extremely pointed with prominent me- dian ridge. Body dark grey to black dorsally and white ventrally with streaks and lobes of intermediate shades along sides.Commonly travel singly or in groups of 2 or 3 in coastal and shore areas;may be found in groups of several hundred on feeding grounds. IUCN Status: Lower risk, near threatened. Balaenoptera borealis Lesson, 1828 SIW En - Sei whale; Fr - Rorqual de Rudolphi; Sp - Rorcual del norte. Adults to 18 m long. Typical rorqual body shape; dorsal fin tall and strongly curved, rises at a steep angle from back.Colour of body is mostly dark grey or blue-grey with a whitish area on belly and ventral pleats.Commonly travel in groups of 2 to 5 in open ocean waters. IUCN Status: Endangered. 2042 Marine Mammals Balaenoptera edeni Anderson, 1878 BRW En - Bryde’s whale; Fr - Rorqual de Bryde; Sp - Rorcual tropical. -
Indonesia Weather Bulletin for Shipping
BADAN METEOROLOGI KLIMATOLOGI DAN GEOFISIKA STASIUN METEOROLOGI MARITIM KLAS I TANJUNG PRIOK Jln. Padamarang no. 4A Pelabuhan Tanjung Priok Jakarta 14310 Telp. 43912041, 43901650, 4351366 Fax. 4351366 Email : [email protected] BMKG TANJUNG PRIOK, JUNE 16, 2015 INDONESIA WEATHER BULLETIN FOR SHIPPING I. PART ONE : NIL II. PART TWO : SYNOPTIC WEATHER ANALYSIS : FOR 00.00 UTC DATE JUNE 16, 2015 - GENERAL SITUATION WEAK TO MODERATE SOUTHEAST TO WEST WINDS. - INTER TROPICAL CONVERGENCE ZONE [ I.T.C.Z. ] PASSING OVER : NIL. - CONVERGENCE LINE (C.L.) PASSING OVER : SOUTH CHINA SEA, AND NORTH HALMAHERA PACIFIC OCEAN. - LOW PRESSURE AREA : NIL. III. PART THREE : SEA AREA FORECAST VALID 24 HOURS FROM : 10. 00 UTC DATE JUNE 16, 2015 AS FOLLOWS : A. WEATHER : 1. THE POSSIBILITY OF SCATTERED TO OVERCAST AND MODERATE RAIN OCCASIONALLY FOLLOWED BY THUNDERSTORM COULD OCCUR THE OVER AREAS OF : LHOKSEUMAWE WATERS, MALACA STRAIT, ANAMBAS- NATUNA ISLANDS WATERS, NATUNA SEA, RIAU ISLANDS WATERS, LINGGA ISLANDS WATERS, SINGKAWANG WATERS, TARAKAN WATERS, BALIKPAPAN WATERS, BITUNG-MANADO WATERS, SANGIHE-TALAUD ISLANDS WATERS, MALUKU SEA, HALMAHERA ISLANDS WATERS, HALMAHERA SEA, SULA ISLANDS WATERS, SORONG WATERS, CENDRAWASIH GULF, SARMI-JAYAPURA ISLANDS WATERS AND AMAMAPARE WATERS. 2. THE POSSIBILITY OF SCATTERED TO BROKEN CLOUDS AND RAIN OR LOCAL RAIN COULD OCCUR THE OVER AREAS OF : SIMEULUE-MEULABOH WATERS, SIBOLGA-NIAS ISLANDS WATERS, WEST SUMATRA AND MENTAWAI ISLANDS WATERS, BANGKA STRAIT, NORTH PANGKAL PINANG WATERS, KARIMATA STRAIT, PONTIANAK WATERS, KETAPANG WATERS, KOTABARU WATERS, MAKASAR STRAIT, NORTHERN SULAWESI ISLAND WATERS, TOMINI GULF, BANGGAI ISLANDS WATERS, SERAM SEA, MANOKWARI WATERS AND BIAK WATERS. B. WINDS DIRECTION AND SPEED FROM SURFACE UP TO 3000 FEET : WINDS OVER INDONESIA WATERS, NORTHERN EQUATOR GENERALLY SOUTHEAST TO SOUTHWEST AND SOUTHERN EQUATOR GENERALLY SOUTHEAST TO WEST AT ABOUT 3 TO 25 KNOTS. -
Marine Mammals and Sea Turtles of the Mediterranean and Black Seas
Marine mammals and sea turtles of the Mediterranean and Black Seas MEDITERRANEAN AND BLACK SEA BASINS Main seas, straits and gulfs in the Mediterranean and Black Sea basins, together with locations mentioned in the text for the distribution of marine mammals and sea turtles Ukraine Russia SEA OF AZOV Kerch Strait Crimea Romania Georgia Slovenia France Croatia BLACK SEA Bosnia & Herzegovina Bulgaria Monaco Bosphorus LIGURIAN SEA Montenegro Strait Pelagos Sanctuary Gulf of Italy Lion ADRIATIC SEA Albania Corsica Drini Bay Spain Dardanelles Strait Greece BALEARIC SEA Turkey Sardinia Algerian- TYRRHENIAN SEA AEGEAN SEA Balearic Islands Provençal IONIAN SEA Syria Basin Strait of Sicily Cyprus Strait of Sicily Gibraltar ALBORAN SEA Hellenic Trench Lebanon Tunisia Malta LEVANTINE SEA Israel Algeria West Morocco Bank Tunisian Plateau/Gulf of SirteMEDITERRANEAN SEA Gaza Strip Jordan Suez Canal Egypt Gulf of Sirte Libya RED SEA Marine mammals and sea turtles of the Mediterranean and Black Seas Compiled by María del Mar Otero and Michela Conigliaro The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by Compiled by María del Mar Otero IUCN Centre for Mediterranean Cooperation, Spain © IUCN, Gland, Switzerland, and Malaga, Spain Michela Conigliaro IUCN Centre for Mediterranean Cooperation, Spain Copyright © 2012 International Union for Conservation of Nature and Natural Resources With the support of Catherine Numa IUCN Centre for Mediterranean Cooperation, Spain Annabelle Cuttelod IUCN Species Programme, United Kingdom Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the sources are fully acknowledged. -
Quaternary Uplifted Coral Reef Terraces on Alor Island, East Indonesia
Coral Reefs (1994) 13:215-223 Coral Reefs Springer-Verlag 1994 Quaternary uplifted coral reef terraces on Alor Island, East Indonesia W. S. Hantoro 1'2, P. A. Pirazzoli 3, C. Jouaunic 4, H. Faure z, C. T. Hoang 5, U. Radtke 6, C. Causse 7, M. Borel Best 8, R. Lafont 2, S. Bieda 2 and K. Lambeck 9 1CGRD-LIPI, Jalan Cisitu 21/154D, Bandung 40135, Indonesia 2CNRS, Laboratoire de G~ologie du Quaternaire, Luminy, Case 907, F-13288 Marseille Cedex 9, France 3CNRS; Laboratoire de G~ographie Physique, 1 Place A. Briand, F-92190 Meudon-Bellevue, France *ORSTOM, Station de G~odynamique, BP 48, La Darse, F-06230 Villefranche-sur-Mer, France SCNRS-CEA, Centre des Faibles Radioactivit6s, F-91198 Gif-sur-Yvette Cedex, France 6Geographisches Institut, Heinrich-Heine Universit~it, D-40225 Dfisseldorf, Germany 7Museum National d'Histoire Naturelle, Laboratoire de G~ologie, 43 rue Buffon, F-75005 Paris, France 8National Natuurhistorisch Museum, PO Box 9517, NL-2300 RA Leiden, The Netherlands 9Institut de Physique du Globe, 4 Place Jussieu, F-75252 Paris Cedex 05, France Accepted 16 February 1994 Abstract. A flight of six major coral reef terraces, up to Introduction 700m in altitude, occurs along the eastern and northern sides of Kabola Peninsula, Alor Island, Indonesia. Some Sequences of superimposed raised marine terraces have radiometric dates have been obtained from unrecrystallized been reported from many coastal areas in the world. coral samples collected in growth position by three different In several cases dating methods have provided age estima- methods (14C, 23~ ESR). This enabled the identi- tions of middle- to late-Quaternary marine episodes.