Some Topics for Coral Reefs of the Persian Gulf
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Rare Birds in Iran in the Late 1960S and 1970S
Podoces, 2008, 3(1/2): 1–30 Rare Birds in Iran in the Late 1960s and 1970s DEREK A. SCOTT Castletownbere Post Office, Castletownbere, Co. Cork, Ireland. Email: [email protected] Received 26 July 2008; accepted 14 September 2008 Abstract: The 12-year period from 1967 to 1978 was a period of intense ornithological activity in Iran. The Ornithology Unit in the Department of the Environment carried out numerous surveys throughout the country; several important international ornithological expeditions visited Iran and subsequently published their findings, and a number of resident and visiting bird-watchers kept detailed records of their observations and submitted these to the Ornithology Unit. These activities added greatly to our knowledge of the status and distribution of birds in Iran, and produced many records of birds which had rarely if ever been recorded in Iran before. This paper gives details of all records known to the author of 92 species that were recorded as rarities in Iran during the 12-year period under review. These include 18 species that had not previously been recorded in Iran, a further 67 species that were recorded on fewer than 13 occasions, and seven slightly commoner species for which there were very few records prior to 1967. All records of four distinctive subspecies are also included. The 29 species that were known from Iran prior to 1967 but not recorded during the period under review are listed in an Appendix. Keywords: Rare birds, rarities, 1970s, status, distribution, Iran. INTRODUCTION Eftekhar, E. Kahrom and J. Mansoori, several of whom quickly became keen ornithologists. -
Pierced Salt Domes in the Persian Gulf and in the Zagros Mountain Ranges
J. Rahnama-Rad et al. / Iranian Journal of Earth Sciences 1 (2009) / 57-72 57 Pierced salt domes in the Persian Gulf and in the Zagros mountain ranges Islamic Azad University Mashhad Branch in southern Iran and their relationship to hydrocarbon and basement tectonics J. Rahnama-Rad*1, G. Farhoudi 2, H. Ghorbani 3 Sh. Habibi Mood 1 and R. Derakhshani 4 1. Department of Geology, Islamic Azad University, Zahedan Branch, Zahedan, Iran, 2. Islamic Azad University, Shiraz Branch, Shiraz, Iran. 3. Lar Consultant, Tehran, Iran. 4. Department of Geology, Faculty of basic science, Shahid Bahonar University, Kerman, Iran Received 4 February 2008; accepted: 8 September 2009 Abstract The most enigmatic problems with the nearly 200 salt domes pierced in the Persian Gulf and in the Zagros Mountain Ranges (ZMR) in southern Iran, a unique morphology in the world, have been the matter of this study, which is based on a combination of field work, enhancement of satellite and aerial photographs etc. In the ZMR, structural anomalies are frequently associated with similar facies distribution patterns. In the eastern portion of the region, emergent salt plugs of Infra-Cambrian age exhibit the same alignment patterns. Such trends bear no apparent genetic relationship to the Tertiary folding responsible for the present Zagros fold belt, but rather indicate their affinity with linear basement features which are readily observable on Land sat imagery and aerial photographs. Bending of anticlines in the competent cover rock, combined with minor strike-slip faults and horizontal displacements of parts of folded structures, strongly point to the presence of these basement faults. -
State of the Marine Environment Report in the ROPME Sea Area 2013
State of the Marine Environment Report 2013 R O P M E Regional Organization for the Protection of the Marine Environment - Kuwait State of the Marine Environment Report 2013 R O P M E Regional Organization for the Protection of the Marine Environment - Kuwait Regional Organization for the Protection of the Marine Environment (ROPME) P.O.Box 26388 13124 Safat State of Kuwait. Tel: +965 25312140 Fax: +965 25324172 / 25335243 E-Mail:[email protected] www.ropme.org Copyright @ 2013 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording or any information storage For bibliographic purposes, this document should be cited as: and retrieval system, without the prior ROPME (2013). State of the Marine Environment Report- 2013. ROPME/ written permission GC-16 /1-ii Regional Organization for the Protection of the Marine from ROPME. Environment, Kuwait, 225 p. ii State of the Marine Environment Report - 2013 g In the name of God the Compassionate, the Merciful Blank Page TABLE OF CONTENTS Page FOREWORD xxi PREFACE xxiii EXECUTIVE SUMMARY xxv ABBREVIATIONS AND ACRONYMS xxxi CHAPTER 1: INTRODUCTION 1 1.1 Definition and Geographic Limits of the ROPME Sea Area 1 1.1.1 Geographical Divisions of the RSA 1 1.1.2 Geology and Geomorphology of RSA 2 1.1.3 Bathymetry 6 1.2 Brief Description on the Approach of SOMER-2013 7 CHAPTER 2: SOCIO-ECONOMIC ACTIVITIES AND DRIVERS 9 KEY MESSAGES 9 2.1 Demographic Indicators 10 2.1.1 Urban Sprawl in the Coastal Areas 13 2.2 Economic Indicators 16 2.2.1 Economies of the RSA Countries 17 2.2.2 Major Industries and Industrial Production 17 i. -
Tectonic Geomorphology of Iran's Salt Structures
Open Journal of Geology, 2015, 5, 61-72 Published Online February 2015 in SciRes. http://www.scirp.org/journal/ojg http://dx.doi.org/10.4236/ojg.2015.52006 Tectonic Geomorphology of Iran’s Salt Structures Mehran Arian1, Hamideh Noroozpour2 1Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran 2Department of Geology, Faculty of Science, Payame Noor University, Tehran, Iran Email: [email protected] Received 13 January 2015; accepted 9 February 2015; published 13 February 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract Iran has a various salt structures that their tectonic geomorphology is subject of this paper. Geo- logic situation of salt structures in Iran have determinate. According to age and geological setting of salt deposits that revealed by tectonic geomorphology methods, salt structure provinces of the Central and Southern Iran have been distinguished. Also, critical concepts of salt diapirism in the Southern Iran and Central Iran salt basins have explained. Therefore, Central Iran’s salt diapirs have triggered by tectonic forces, but salt diapirism in the Southern Iran has triggered by haloki- nesis, then it has effected by tectonic forces, especially in Zagros fold and thrust belt. Keywords Tectonic Geomorphology, Salt Structures, Diapir, Iran, Halokinesis 1. Introduction Tectonic geomorphology is the study of the interaction between tectonics and surface processes that form the structure during geologic times. Salt diapir or piercement structure with a central, nearly equidimensional salt plug, generally one to two kilometers or more in diameter, which has risen through the enclosing sediments from a mother salt bed beneath the top of the plug, is called salt dome [1]. -
Central Iran ىزﮐرﻣ نارﯾا
©Lonely Planet Publications Pty Ltd ايران مرکزی Central Iran Includes ¨ Why Go? Qom 147 Central Iran, encompassing the magnificent cities of Esfa- Kashan 151 han, Yazd and Shiraz, is the cultural tour-de-force of Iran. Esfahan 158 Wedged between the Zagros Mountains to the west and the Dasht-e Kavir 178 Dasht-e Kavir to the east, it offers the quintessential Persian experience and it’s no coincidence that it attracts the most Yazd 182 visitors. But in an age that celebrates getting off the beat- Shiraz 195 en track, this is one destination where this is a redundant Persepolis 207 quest: for centuries people have crossed this land, following Pasargadae 210 in the footsteps of ancient empire builders, their journeys commemorated in the artistic wonders at Persepolis. You can continue that journey today, tracing the silk route along desert byways, through city bazaars and across Best Places to mountain passes – in much the same manner as the region’s Eat famous nomads. Many of the caravanserai and khans that dot these routes have been restored and overnighting in one ¨ Abbasi Teahouse & of these hospitable lodgings serves as an appointment with Traditional Restaurant (p172) history. ¨ Bastani Traditional Restaurant (p171) ¨ Shahrzad (p172) When to Go ¨ Ghavam (p205) Visit in the spring when Persian gardens are in bud, mountain orchards are full of flowers and the rose fields around Kashan ¨ Talar Yazd (p190) are at their fragrant best. Although there is some difference in climate from region to region, generally travelling in the extreme heat of summer Best Places to when temperatures can reach 50°C or more is not much fun Sleep between June to September. -
Geotourism Attractions of Hormuz Island, Iran
GeoJournal of Tourism and Geosites Year XII, vol. 28, no. 1, 2020, p.232-245 ISSN 2065-1198, E-ISSN 2065-0817 DOI 10.30892/gtg.28118-465 GEOTOURISM ATTRACTIONS OF HORMUZ ISLAND, IRAN Mohsen RANJBARAN* School of Geology, College of Science, University of Tehran, Tehran, Iran, e-mail: [email protected] Syed Mohammad ZAMANZADEH Department of Geography, University of Tehran, Tehran, Iran, Tehran, Iran, e-mail: [email protected] Farzad SOTOHIAN Faculty of Natural Resources, Department: Environmental Science Department, University of Guilan, Iran, e-mail: [email protected] Citation: Ranjbaran, M., Zamanzadeh, S.M. & Sotohian, F. (2020). GEOTOURISM ATTRACTIONS OF HORMUZ ISLAND, IRAN. GeoJournal of Tourism and Geosites, 28(1), 232–245. https://doi.org/10.30892/gtg.28118-465 Abstract: Hormuz Island is a salt dome situated in the Persian Gulf waters near the mouth of Hormuz Strait in Hormuzgan province, at 8 kilometers distance from Bandar Abbas. The island is elliptical, and its rock is mostly of the igneous and often volcanic type. Hormuz is one of the most beautiful Islands of the Persian Gulf due to its geological phenomena and related landforms. This island is a mature salt diapir with great mineralogical and lithological diversity. In this research, we focused on fieldwork, which included data gathering and taking photographs and also a review of the published papers and books. The main geotourism attractions of the island include various landforms resulted from differential erosion, as well as very attractive geomorphologic structures such as rocky and sandy beaches, sea caves, colorful salt domes, coral reefs, etc. -
Kerman Xv.—Xvi
KERMAN XV.—XVI. LANGUAGES 301 968. Robert Joseph Dillon, “Carpet Capitalism and the Trade of the Kerman Consular District for the Year Craft Involution in Kirman. Iran: A Study in Economic 1902-03 by Major P. Sykes, His Majesty’s Consul,” Anthropology,” Ph.D. diss., Columbia University, 1976. House of Commons Pari iamentary Papers, Annual Series Arthur Cecil Edwards, The Persian Carpet: A Survey of o f Trade Reports, Cd.1386, 1903. Idem, “Report for the the Carpet-Weaving Industry of Persia, London, 1975. Year 1905-06 on the Trade of the Kerman Consular Dis A. H. Gleadowe-Newcomen, Report on the Commercial trict,” House of Commons Parliamentary Papers, Annual Mission to South-Eastern Persia During 1904-1905, Series of Trade Reports, Cd.2682, 1906. Ahmad-'Ali Calcutta, 1906. James Gustafson, “Opium, Carpets, and Khan Waziri Kermani, Jografia-ye Kerman, ed. Moham- Constitutionalists: A Social History of the Elite House mad-Ebrahim Bastani Parizi, 2nd ed., Tehran, 1974. holds of Kirman, 1859-1914,” Ph.D. diss., University of Hans E. Wulff, The Traditional Crafts of Persia: Their Washington, 2010. Leonard Michael Helfgott, Ties that Development, Technology, and Influence on Eastern and Bind: A Social History o f the Iranian Carpet, Washing Western Civilization, London, 1966. ton, D.C., 1 994. L. Haworth, “Diary for the Week Ending (J a m e s M. G u s t a f s o n ) November 12 1905,” U. K. National Archives, Kew, F.O. 248/846. International Monetary Fund, Islamic Republic of Iran—Statistical Appendix, IMF Country Report No. 04/307, September, 2004. -
Iranian Coral Reefs Status with Particular Reference to Kish Island, Persian Gulf
International Coral Reef Initiative Indian Ocean Regional Workshop, Muzambique, Nov. 26-28, 2001 IRANIAN CORAL REEFS STATUS WITH PARTICULAR REFERENCE TO KISH ISLAND, PERSIAN GULF 1 2 SEYED MOHAMMAD REZA FATEMI , MOHAMMAD REZA SHOKRI 1Dept. of Fisheries and Marine Biology, Science and Research Unit, Islamic Azad University, Hesarak, PO BOX: 14155-5655, Tehran, IRAN. Email: <[email protected]> 2Iranian National Center for Oceanography, #51, Bozorgmehr Ave., I4168, PO BOX: 14155- 4781, Tehran, IRAN. Email: <[email protected]> Abstract In this paper, the coral status of Iranian waters in the Persian Gulf are reviewed and discussed based on the obtained results and information after three years of field surveys in Nay Band Bay, Kish and Farur islands. Altogether, 27 species of corals were identified from the studied areas, belonging to 9 families and 20 genera. Faviidae with 6 genera and 8 species is the most diverse of all families. On the other hand, Poritidae with 2 genera and 4 species is the most abundant corals in all areas. In the last 10 years, Acropora has declined from being the most abundant genus in shallow waters of fringing islands, to almost absennt, due to environmental stresses and human impacts. Anacropora forbesi is reported for the first time from the area. Regarding the coral health, the live coral coverage ranges from 9 to 30%, with minimum coverage in Kish Island and maximum in Nay Band Bay. During this study, no new bleached coral was observed at the surveyed areas, though in the past few years, considerable bleaching events have occurred throughout the area. -
Influence of Environmental Factors on the Characteristics of Macrobenthic
Hydroécol. Appl. (2021) Tome 21, pp. 93–113 https://www.hydroecologie.org © EDF, 2021 https://doi.org/10.1051/hydro/2021002 Influence of environmental factors on the characteristics of macrobenthic communities in soft bottoms around coral reefs of Larak Island (Persian Gulf) Influence des facteurs environnementaux sur les caractéristiques des communautés macrobenthiques des fonds meubles autour des récifs coralliens de l’île de Larak (golfe Persique) (traduit par la rédaction) Shima Tavanayan1, Sana Sharifian1,*, Ehsan Kamrani2, Mohammad Seddiq Mortazavi3, Siamak Behzadi3 1 Department of Marine Biology, University of Hormozgan, Bandar Abbas, Iran sharifi[email protected] 2 Fishery Department, University of Hormozgan, Bandar Abbas, Iran 3 Persian Gulf and Oman Sea Ecological Research Institute, Iranian Fisheries Sciences Research Institute, Agricultural Research Education and Extension Organization (AREEO), Bandar Abbas, Hormozgan, Iran Abstract – The effective conservation of coastal ecosystems including soft bottoms around coral reefs of Larak Island, Persian Gulf is requiring basis data on community structure at different relevant spatial scales. In this regard, the diversity and the abundance of the macrobenthic communities in soft bottoms around coral reefs of this area were described in relation to different environmental factors. A seasonal sampling was conducted at two stations located in the east and west of Larak Island, respectively, during 4 seasons, from spring to winter 2012. A total of 20 species which belong to 20 genera and 14 families were identified. The macrobenthic density showed significant differences among seasons. The Shannon-Wiener index ranged from 2.07 to 2.89 indicating a moderate diversity in both stations. The maximum diversity of macrobenthic organisms was observed during spring. -
Geochronology and Geochemistry of Rhyolites from Hormuz Island, Southern Iran: a New Record of Cadomian Arc Magmatism in the Hormuz Formation
Lithos 236–237 (2015) 203–211 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Geochronology and geochemistry of rhyolites from Hormuz Island, southern Iran: A new record of Cadomian arc magmatism in the Hormuz Formation Narges Sadat Faramarzi a,b,⁎, Sadraddin Amini a,c, Axel Karl Schmitt c, Jamshid Hassanzadeh d, Gregor Borg e, Kevin McKeegan c, Seyed Mohammad Hosein Razavi a, Seyed Mohsen Mortazavi f a Department of Geology, Kharazmi University, 49 Mofatteh Avenue, Tehran 15614, Islamic Republic of Iran b Department of Research and Development (R & D), Pars Kani Co., Tehran 1593663415, Islamic Republic of Iran c Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA d Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA e Institute of Geosciences and Geography, Martin-Luther-University Halle, Wittenberg, Germany f Department of Geology, Hormozgan University, Bandar Abbas, Islamic Republic of Iran article info abstract Article history: Hormuz Island, a salt-gypsum dome in the Persian Gulf in southern Iran, is a complex halotectonic melange Received 21 December 2014 comprising evaporites, carbonates, volcanic and volcaniclastic rocks, as well as low-grade metamorphic and Accepted 26 August 2015 sedimentary rocks. Based on trace element (including rare earth elements REE) compositions of whole rocks Available online 12 September 2015 and zircon, Hormuz rhyolites are inferred to have formed from subduction-related magmas generated in an active continental margin setting. Ion microprobe analyses of zircon crystals yielded concordant U–Pb ages Editor: Lin Chung Sun- with weighted mean 206Pb/238U age of 558 ± 7 Ma (juvenile zircons in contrast to those from previous magmatic Keywords: episodes or xenocrysts) along with younger and older discordant ages which likely represent Pb loss and the Hormuz presence of xenocrystic domains, respectively. -
A LIST of MARINE ALGAE from SEASHORES of IRAN (HORMOZGAN PROVINCE) by J
--------------------------------------------------------- Qatar Univ. Sci J. (1999), 19: A LIST OF MARINE ALGAE FROM SEASHORES OF IRAN (HORMOZGAN PROVINCE) By J. Sohrabipour and R. Rabii. Natural Resources and Animal Research Center of Hormozgan. P.O.Box. 79145- 1468, Bandar Abbas, Iran. ABSTRACT Seashores of Hromzgan province in south of Iran were studied for collection and recogna tion of algal flora (1991-1996). 150 species of marine algae were recognized, including 36 Chlorophyta (16 new). 33 Phaeophyta (15 new). 75 Rhodophyta (42 new), 3 Xanthophyta (2 new) and 3 Cyanophyta (2 new). In this study number of algal species from iranian sea shores are increased to 201 species. INTRODUCTION shores. In Nizamuddin and Gessner re Marine algae of Persian Gulf for the first port's (1970) one species was reported time were studied by Endlicher and Die form Abudhabi seashores. sign (1845). they recorded 8 species of al gae based on Kotschy collection from Jones ( 1986) described and illustrated 67 Kharck islnad in northwest of the Gulf. sppecies of algae from seashores of Ku Borgesen (1939) recorded 102 species of wait and Persian Gulf. Al-Hassan and marine algae from Iraian Gulf which 76 Jones (1989) recorded105 species of algae species of them were collected from Irani from Kuwait seashores. Easson et al an seashores and others form Arabian re ( 1989) recorded 88 species of agae form gions of the Gulf. Nizamuddin and Gess Bahrain seashores. Msheghni and Dugham ner (1970) descirbed 68 species of algae (1987) published benthic marin agae from from Iranian seashores and Pakistan sea Qatar seashores. Easson ( 1992) published shores based on algal collection which had a chacklist of algae of the Gulf. -
Salt Plugs in the Eastern Zagros, Iran: Results of Regional Geological Reconnaissance
GeoLines (Praha), 7 (1998) 3 Salt Plugs in the Eastern Zagros, Iran: Results of Regional Geological Reconnaissance Pavel BOSÁK1, Josef JAROŠ2, Jiøí SPUDIL3, Petr SULOVSKÝ4 and Vladimír VÁCLAVEK5 1 Geological Institute, Czech Academy of Sciences, Rozvojová 135, 165 02 Praha 6, Czech Republic; e-mail: [email protected] 2 Institute of Geology and Paleontology, Faculty of Natural Sciences, Charles University, Albertov 6, 128 43 Praha 2, Czech Republic 3 GET Ltd., Korunovaèní 29, 170 00 Praha 7, Czech Republic, e-mail: [email protected] 4 Department of Mineralogy, Petrology and Geochemistry, Masaryk University, Kotláøská 2, 611 37 Brno, Czech Republic; e-mail: [email protected] 5 Pod Spoøilovem 2779, 141 00 Praha 4, Czech Republic ABSTRACT. Regional reconnaissance study of salt plugs cov- temperature is needed to start the glacier flow. Unbreached ered the area of about 50,000 square kilometers (coordinates salt plugs were discussed. Their occurrence is highly limited. It 53o50' to 56o30' E and 26o30' to 28o15‘N). Altogether 68 salt is shown, that “collapse structures” are connected rather with plugs were characterized from the viewpoint of their position other processes than solution collapse after leached salt. Tec- in the structure of area, morphological and evolution stages, tonic effects, erosion and pedimentation took part substantial- rock content and mineralization. ly in the formation of cauldrons. Linear cauldrons are connect- Prevailing amount of plugs lies in the flanks of anticline ed with tension regime in the apical zone of anticlines. Primary folds and is bounded to fold plunges and sigmoidal bends, where and secondary rim synclines have not been yet detected.