Update on the Cetacean Fauna of the Mediterranean Levantine Basin
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In the Mediterranean Sea (Aegean, Greece)
Aquatic Invasions (2007) Volume 2, Issue 2: 152-154 Open Access doi: http://dx.doi.org/10.3391/ai.2007.2.2.12 © 2007 The Author(s) Journal compilation © 2007 REABIC Short communication A new record of the Lessepsian invasive fish Etrumeus teres (Osteichthyes: Clupeidae) in the Mediterranean Sea (Aegean, Greece) Panagiotis Kasapidis*, Panagiota Peristeraki, Georgios Tserpes and Antonios Magoulas Hellenic Centre for Marine Research, Institute of Marine Biology and Genetics, P.O.Box 2214, 71003 Heraklion, Greece *Corresponding author E-mail: [email protected] (PK) Received: 6 March 2007 / Accepted: 11 May 2007 Abstract The Lessepsian invasive fish Etrumeus teres was recorded for the first time off Crete, Greece in July 2005. Their abundance suggests that the species may become of commercial importance in the south Aegean Sea. Key words: Etrumeus teres, Lessepsian invasive fish, Mediterranean, Aegean, new record The opening of the Suez Canal in 1869 reported that the species is occasionally connected the Red Sea to the Mediterranean and abundant in the western Cretan Sea, with a haul allowed the introduction of numerous Indo- of 2500 kg taken by a purse-seine in Chania Bay Pacific species into the Mediterranean (Golani in June 2004. They refer to the species as 1998a, 1998b), including Etrumeus teres (White- “gavrofrisa”, a combination of the common head 1963). This is the first record of the species Greek names for anchovy and round sardinella. off Crete, Greece (Figure 1). The suggested Greek common name is Etrumeus teres (round herring) is a pelagic, “stroggulosardela” (round sardine) (Economidis mainly inshore clupeid fish, found in the Red and Koutrakis 2001). -
West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date
Part I: North Africa Part II: West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date: AFRI CA Overview RICA lies at the heart of the earth's land Then, during the nineteenth century, masses. It sits astride the equator, with European traders began setting up trading sta . almost half the continent to the north tions along the coast of West Africa. The of the equator, and half to the south. It con traders, and their governments, soon saw great tains some of the world's greatest deserts, as opportunity for profit in Africa. Eventually, well as some of the world's greatest rivers. It many European countries took control of the has snow-capped mountains, and parched, arid land and divided it into colonies. plains. The first humans came from Africa. By the middle of the twentieth century, peo And in the millennia since those fust humans ple all across Africa had demanded indepen walked the plains of Africa, many different cul dence from colonial rule. By the end of the tures have arisen there. century, government had passed firmly into Physically, Africa is one enormous plateau. It African hands. However, the newly independ has no continental-scale mountain chains, no ent nations must still deal with the legacy of peninsulas, no deep fjords. Most of the conti colonialism. The boundaries the European nent is more than 1000 feet (300m) above sea powers created often cut across ethnic and cul level; over half is above 2500 feet (800 m). tural groups. Many African nations today are Africa's early history reflects the wide stretch still struggling to reconcile the different cul of the continent. -
Emigrating Animals and Migratory Humans: Belonging, Prosperity and Security in More-Than-Human World
Emigrating Animals and Migratory Humans: Belonging, Prosperity and Security in More-Than-Human World Dates: 10—11 September 2019 Venue: Na Florenci 3 (Lower Hall), Prague 1, Czech Republic Workshop organised by Luděk Brož, Giovanna Capponi, Paul Keil, Jiří Krejčík & Virginie Vaté Kindly supported by Strategy 21 – Global Conflicts and Local Interactions & Institute of Ethnology and Institute of Sociology, Czech Academy of Sciences (CAS) and CEFRES (CNRS-MEAE) DAY 1 9.45 Getting to know each other over a cup of tea or coffee 10.00—10.30 Welcome address and introduction (Luděk Brož, Giovanna Capponi, Jiří Krejčík & Virginie Vaté) Session 1. Chair: Daniel Sosna, Institute of Ethnology CAS 10.30—11.00 Aníbal G. Arregui University of Barcelona Porcine Proto-Ecologies: Activating an Infra-Species Cosmopolitics The increasing movement of wild-boars between the Collserola forests and the periphery of Barcelona is problematizing not only dual categories of pigs as species (e.g. wild vs. domestic), but also the boundaries of what is commonly understood as a ‚city‘ (e.g. urban vs. rural). The transit of wild boars between different ecological niches—which transforms these niches themselves—is traceable from at least three scales of anthropogenic influence: On a global, climatologic scale, wild boars proliferate due to global warming (Vetter et al. 2015). On a geographically localized level, wild boars are ‚invited‘ into the city by food availability in trash, pet feeding spots, water reservoirs, etc. At the scale of interactions between individuals, it becomes evident that, while some citizens ‚care‘ for the wild boars (e.g. petting or feeding them), other reject them for being ‚wild‘, ‚dangerous‘ and ‚dirty‘ animals. -
Geog 120: World Geography American University of Phnom Penh
Geog 120: World Geography American University of Phnom Penh Map Quizzes: List of physical features 1. Africa Atlas Drakensberg Seas and Oceans Deserts Mediterranean Atlantic Kalahari Strait of Gibraltar Namib Suez Canal Sahara Mozambique Channel Ogaden Red Sea Libyan Gulf of Suez 2. Asia Lakes Lake Chad Seas and Oceans Lake Malawi (Nyasa) Lake Tanganyika Andaman Sea Lake Victoria Arabian Sea Lake Albert Aral Sea Lake Rudolph Arctic Ocean Atlantic Ocean Rivers Black Sea Caspian Sea Congo East China Sea Limpopo Indian Ocean Niger Inland Sea (also know as Setonaikai, Zambezi Japan) Nile Mediterranean Sea Orange Pacific Ocean Vaal Red Sea Sea of Japan Mountains Sea of Okhotsk 2 South China Sea Mountain Ranges Yellow Sea Caucuses Elburz Straits, Channels, Bays and Gulfs Himalayas Hindu Kush Bay of Bengal Ural Bosporus Zagros Dardanelles Gulf of Aden Gulf of Suez Deserts Gulf of Thailand Arabian Gulf of Tonkin Dasht-E-Kavir Persian Gulf Gobi Strait of Taiwan Negev Strait of Malacca Takla Makan Strait of Hormuz Strait of Sunda Suez Canal 3. The Americas Lakes Seas and Oceans Baykal Bering Tonle Sap Caribbean Sea Atlantic Ocean Pacific Ocean Rivers Straits, Channels, Bays and Gulfs Amur Brahmaputra Gulf of Mexico Chang Jiang Hudson Bay Euphrates Panama Canal Ganges Strait of Magellan Huang He (Yellow) Indus Lakes Irrawaddy Mekong Great Salt Tigris Great Lakes (Lakes Tonle Sap (River and Lake) Superior, Michigan, Huron, 3 Erie, and Ontario) 4. Australia and the Pacific Manitoba Titicaca Winnipeg Seas and Oceans Coral Sea Rivers Tasman Sea Pacific Ocean Amazon Indian Ocean Colorado Columbia Hudson Straits, Channels, Bays and Gulfs Mississippi Bass Strait Missouri Cook Strait Ohio Gulf of Carpentaria Orinoco Torres Strait Paraguay Plata Parana Rivers Rio Grande Darling St. -
Intefwaitional EXPLORATIWWTS O Meetlnq-NO~~R Sketch
INTEfWAiTIONAL EXPLORATIWWTS Om sparsrs to have been sutured onto the Brazilian Shield near MEETlNQ-NO~~R14,laMJ the end of the Paleozoic. There is considerable controverav concerning is origin and original Iffietion, as well as the THOMAS E. O'CONNOR-Biographical Sketch nature of the suturina of the two maasifa. ~h~~..F nTnnnnr ie Asaocisted withthe Brazilian Shield ars two marine Vice President of Aminoil Paleozoic basins in the northern portion of the country. The Internationel, Incorporated. Tarija Basin is largely represented in BollrEa where it is the developing international ex- cemer of considerable exploration for and prdwtion of ptoration opportunltiea. Tom natural gas. Farther east is the large, imacmtonlc Cham- overviews three production Parena Basin which extends wuthweatdy from Paraguay areas (Indonesia, North Sea and Brazil. To date it has proved to be WenBf hydrocarbons. and Argentine) and directdl Along the western and southern margins of thesnlarged the exploration activity in lulesozoic continental mass of Argentina ie a saries of marina nine exploration contract basins which were present prior to We EoHloian and onset of areas. He received a B.S. subduction of the PeciPicplataduriw(hp Ladr hawob/Early degree ingedogyfromSfan- Tertiary. These western, leading kjnawere wiginally ford University in 1968 and simple in format end structural sQde untll zheowrpfimdf the an M.S. degree in geology Andean Orogeny and associated -rd-verging over- from the University of thrusts deformed their wastern margins. To varying degrees. Colorado in 1961. Since all of the marginal cretonic beaina have proved lo be hydro- 1983. he has been Adjunct Research Professor in the Earth carbon-bearing, inclwlingrecentdiawverieain the Megallanas/ Sciences and Resources Institute at the University of South Malvinas area. -
Bioinvasions in the Mediterranean Sea 2 7
Metamorphoses: Bioinvasions in the Mediterranean Sea 2 7 B. S. Galil and Menachem Goren Abstract Six hundred and eighty alien marine multicellular species have been recorded in the Mediterranean Sea, with many establishing viable populations and dispersing along its coastline. A brief history of bioinvasions research in the Mediterranean Sea is presented. Particular attention is paid to gelatinous invasive species: the temporal and spatial spread of four alien scyphozoans and two alien ctenophores is outlined. We highlight few of the dis- cernible, and sometimes dramatic, physical alterations to habitats associated with invasive aliens in the Mediterranean littoral, as well as food web interactions of alien and native fi sh. The propagule pressure driving the Erythraean invasion is powerful in the establishment and spread of alien species in the eastern and central Mediterranean. The implications of the enlargement of Suez Canal, refl ecting patterns in global trade and economy, are briefl y discussed. Keywords Alien • Vectors • Trends • Propagule pressure • Trophic levels • Jellyfi sh • Mediterranean Sea Brief History of Bioinvasion Research came suddenly with the much publicized plans of the in the Mediterranean Sea Saint- Simonians for a “Canal de jonction des deux mers” at the Isthmus of Suez. Even before the Suez Canal was fully The eminent European marine naturalists of the sixteenth excavated, the French zoologist Léon Vaillant ( 1865 ) argued century – Belon, Rondelet, Salviani, Gesner and Aldrovandi – that the breaching of the isthmus will bring about species recorded solely species native to the Mediterranean Sea, migration and mixing of faunas, and advocated what would though mercantile horizons have already expanded with be considered nowadays a ‘baseline study’. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics. -
Oil Rights in the Gulf of Suez Richard A
Louisiana Law Review Volume 38 | Number 4 Summer 1978 Oil Rights in the Gulf of Suez Richard A. Curry Repository Citation Richard A. Curry, Oil Rights in the Gulf of Suez, 38 La. L. Rev. (1978) Available at: https://digitalcommons.law.lsu.edu/lalrev/vol38/iss4/4 This Comment is brought to you for free and open access by the Law Reviews and Journals at LSU Law Digital Commons. It has been accepted for inclusion in Louisiana Law Review by an authorized editor of LSU Law Digital Commons. For more information, please contact [email protected]. OIL RIGHTS IN THE GULF OF SUEZ International law recognizes that coastal nations have the right to exploit natural resources found in continental shelf areas beneath adja- cent water bodies. In most situations the coastal nation entitled to this right is easily identified as the sovereign in actual control of the land immediately adjacent to the water body. However, the nation in physi- cal control of such land may not be the sovereign thereof. In such a case, both the nation having actual control and the nation claiming sov- ereignty may assert the right to exploit natural resources in the adjacent continental shelf. Such a situation currently exists in the Gulf of Suez. When Israel invaded the Sinai in 1967 it acquired the possession but not the sovereignty of that territory. Now, both Egypt, as sovereign, and Israel, as occupant, claim the right to drill for oil in the adjacent conti- nental shelf. The Gulf of Suez is a semi-enclosed body of water which opens into the Red Sea at the south and narrows into the Suez Canal at the north. -
Multi-Surface Restoration and Petroleum System Evaluation in the Gulf of Suez*
Multi-Surface Restoration and Petroleum System Evaluation in the Gulf of Suez* Isabelle Moretti1 and Julien Gargani2 Search and Discovery Article #40405 Posted April 30, 2008 *Adapted from extended abstract prepared for presentation at AAPG Annual Convention, San Antonio, Texas, April 20-23, 2008 1Cepsa, Madrid, Spain ([email protected]) 2Institut Français du Petrole, Rueil Malmaison, France Abstract A large scale regional study has been carried out at the scale of the Suez rift, using surface restoration. Its aim was to propose a coherent 3D interpretation of geological structures of the Suez rift in order to understand its North-South variations. Results highlight the role of the pre-existing transverse structures on the development of the land-locked basins and salt depocenter in the central and southern Gulf of Suez and Red Sea. Introduction Restoration tools are useful in hydrocarbon exploration in improving the geometry of the model and therefore reducing the uncertainty on the prospects that have to be drilled. The computed past geometries may be used to study the evolution of the basin versus time. Restoration is also interesting in solving more academic questions, as for instance the modeling of the paleogeography of the areas and the regional extension and shortening quantification. In this study, we have completed a 3D surface restoration of the synrift series of the Gulf of Suez. This work has various goals: first to have a 3D model of the Gulf where up to now only cross-sections have been prepared, then to get surface restorations in order to understand the various depocenters during rift evolution. -
Fault Blocks of Abu Darag Basin, Northern Gulf of Suez, Egypt, As Deduced from Potential Field Data Interpretation
ANALYSISANALYSIS ARTICLE 11(25), March 1, 2014 ISSN 2278–5469 EISSN 2278–5450 Discovery Fault blocks of Abu Darag Basin, Northern Gulf of Suez, Egypt, as deduced from potential field data interpretation Ahmad A Azab, Ahmed A El-Khafeef Exploration Department Egyptian Petroleum Research Institute (EPRI), Nasr City, Cairo, Egypt. E-mail: [email protected] Publication History Received: 04 January 2014 Accepted: 08 February 2014 Published: 1 March 2014 Citation Ahmad A Azab, Ahmed A El-Khafeef. Fault blocks of Abu Darag Basin, Northern Gulf of Suez, Egypt, as deduced from potential field data interpretation. Discovery, 2014, 11(25), 9-19 Publication License This work is licensed under a Creative Commons Attribution 4.0 International License. General Note Article is recommended to print as color digital version in recycled paper. ABSTRACT Herein, an integrated approaches to image the main fault blocks and related structures that characterize "AbuDarag Basin" at the extreme northern part of the Gulf of Suez. The potential field data were analyzed qualitatively and quantitatively for identifying and locating the gravity and magnetic lineaments including faults and/or contacts. The Bouguer and RTP aeromagnetic anomalies were implemented and emphasized using different techniques, concerning anomaly resolution, fault locations and trend analysis. As well, the interpreted structure was supported and refined by constructing 2.5-Dgravity/magnetic joint models, invented and guided by available drilled wells. All outcomes were incorporated to construct a structural map for the basement surface. The structural elements map illustrates that the basement relief is dominated by low and high tectonic features of NW orientation, with some significant structural discontinuity to the NE. -
Fish Biodiversity Changes in the Central Mediterranean
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Digital.CSIC Azzurro E.1*, Soto S.2, Garofalo G.3, Maynou F.2 Fistularia commersonii in the Mediterranean Sea: Invasion history and distribution modeling based on presence-only records 1ISPRA, National Institute for Environmental Protection and Research, Piazzale dei Marmi 2, 57128 Livorno, Italy 2Institut de Ciències del Mar (CSIC) Passeig Marítim de la Barceloneta, 37-49, E-08003 Barcelona, Spain 3IAMC-CNR, Institute for Coastal Marine Environment, Via L. Vaccara 61, 91026 Mazara del Vallo, Italy Running title: Fistularia commersonii in the Mediterranean Sea 1 Author to whom correspondence should be addressed. email: [email protected] Abstract The bluespotted cornetfish (Fistularia commersonii) (Osteichtyes, Fistulariidae) is considered to be one of the most invasive species of the Mediterranean Sea and Europe but only scattered information exists on its distribution and abundance. Here we collated the available species records, following its first detection in the Mediterranean Sea, in January 2000, until October 2011. A total of 191 observations were used to reconstruct the invasion sequence, to provide estimates of the rate of spread and to construct an environmental suitability model based on six biophysical variables and the maximum entropy approach (MaxEnt). The results showed that colonization of the Mediterranean Sea proceeded in parallel along the southern and northern rim of the Basin at speeds that reached 1000- 1500 km · yr-1 with a clear decrease in the rate of spread at the Sicily Strait. The most important explanatory variables for describing the distribution of F. -
New Records of Non-Indigenous Molluscs from the Eastern Mediterranean Sea
BioInvasions Records (2018) Volume 7, Issue 3: 245–257 Open Access DOI: https://doi.org/10.3391/bir.2018.7.3.05 © 2018 The Author(s). Journal compilation © 2018 REABIC Research Article New records of non-indigenous molluscs from the eastern Mediterranean Sea Jan Steger1,*, Martina Stockinger1, Angelina Ivkić1,2, Bella S. Galil3 and Paolo G. Albano1 1Department of Palaeontology, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria 2Faculty of Geosciences, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, The Netherlands 3The Steinhardt Museum of Natural History, Israel National Center for Biodiversity Studies, Tel Aviv University, Tel Aviv 69978, Israel Author e-mails: [email protected] (JS), [email protected] (MS), [email protected] (AI), [email protected] (BSG), [email protected] (PGA) *Corresponding author Received: 15 June 2018 / Accepted: 11 July 2018 / Published online: 2 August 2018 Handling editor: Fred Wells Abstract We report new findings of non-indigenous Indo-Pacific molluscs from shallow water habitats off Israel, Greece and Egypt, eastern Mediterranean Sea. The bivalves Pillucina vietnamica Zorina, 1978 and Alveinus miliaceus (Issel, 1869) were collected from sandy bottoms off Israel, whereas Gregariella cf. ehrenbergi (Issel, 1869) was recovered from a buoy originating from Port Said, Egypt, and stranded on the Israeli coast. The three species are first records for the Mediterranean Sea. Additionally, we report range extensions for several gastropods: Varicopeza pauxilla (A. Adams, 1855) is recorded from Israel, Phidiana militaris (Alder and Hancock, 1864) from southern Israel (Ashqelon), and Viriola cf. bayani Jousseaume, 1884 from Israel and Crete. Shells and valves of an unidentified lucinid bivalve morphologically distinct from any known Mediterranean species were found along the Israeli Mediterranean shore.