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Durham Research Online
Durham Research Online Deposited in DRO: 13 April 2015 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Kaislaniemi, L. and van Hunen, J. (2014) 'Dynamics of lithospheric thinning and mantle melting by edge-driven convection : application to Moroccan Atlas mountains.', Geochemistry, geophysics, geosystems., 15 (8). pp. 3175-3189. Further information on publisher's website: http://dx.doi.org/10.1002/2014GC005414 Publisher's copyright statement: c 2014. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modications or adaptations are made. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk PUBLICATIONS Geochemistry, -
Morocco): Clues from Trace Elements and Sr–Nd–Pb–Hf Isotopes
Lithos 205 (2014) 247–265 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Lithospheric origin for Neogene–Quaternary Middle Atlas lavas (Morocco): Clues from trace elements and Sr–Nd–Pb–Hf isotopes Delphine Bosch a,⁎, René C. Maury b,M'hammedElAzzouzib,c,ClaireBollingerd, Hervé Bellon b, Patrick Verdoux e a UMR-UM2-CNRS 5243 Géosciences Montpellier, Université de Montpellier II, place E. Bataillon, c.c. 060, 34095 Montpellier, France b UMR-CNRS 6538 Domaines océaniques, Institut Universitaire Européen de la Mer (IUEM), IUEM, Université de Brest, Université Européenne de Bretagne, place Nicolas Copernic, 29280 Plouzané, France c Faculté des Sciences, Université Mohammed-V, av. Ibn Batouta, BP 1014, 10100 Rabat, Maroc d UMS-CNRS 3113 Pôle de spectrométrie océan, IUEM, Université de Brest, Université Européenne de Bretagne, place Nicolas Copernic, 29280 Plouzané, France e Laboratoire de Géochimie Isotopique environnementale, Université de Nîmes/Site GIS, UMR-CNRS 7330, rue Georges Besse, 30035 Nîmes Cedex 1, France article info abstract Article history: This study presents new geochemical data on 26 mafic lavas from the Middle Atlas and Central Morocco volcanic Received 17 April 2014 provinces, including Miocene nephelinites and Pliocene–Quaternary (3.9–0.6 Ma) nephelinites, basanites, alkali Accepted 11 July 2014 and subalkaline basalts. Most of them represent near-primary magmas, although some alkali basalts were derived Available online 21 July 2014 from the minor fractionation of olivine and diopside phenocrysts. These evolved samples and the subalkaline basalt display higher 207Pb/204Pb and Zr/Nb ratios and lower εNd consistent with their contamination by lower crustal Keywords: Intraplate alkali basalts granulites during an open fractionation process. -
(Ammotragus Lervia) in Northern Algeria? Farid Bounaceur, Naceur Benamor, Fatima Zohra Bissaad, Abedelkader Abdi, Stéphane Aulagnier
Is there a future for the last populations of Aoudad (Ammotragus lervia) in northern Algeria? Farid Bounaceur, Naceur Benamor, Fatima Zohra Bissaad, Abedelkader Abdi, Stéphane Aulagnier To cite this version: Farid Bounaceur, Naceur Benamor, Fatima Zohra Bissaad, Abedelkader Abdi, Stéphane Aulagnier. Is there a future for the last populations of Aoudad (Ammotragus lervia) in northern Algeria?. Pakistan Journal of Zoology, 2016, 48 (6), pp.1727-1731. hal-01608784 HAL Id: hal-01608784 https://hal.archives-ouvertes.fr/hal-01608784 Submitted on 27 May 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Pakistan J. Zool., vol. 48(6), pp. 1727-1731, 2016. Is There a Future for the Last Populations of Aoudad (Ammotragus lervia) in Northern Algeria? Farid Bounaceur,1,* Naceur Benamor,1 Fatima Zohra Bissaad,2 Abedelkader Abdi1 and Stéphane Aulagnier3 1Research Team Conservation Biology in Arid and Semi Arid, Laboratory of Biotechnology and Nutrition in Semi-Arid. Faculty of Natural Sciences and Life, University Campus Karmane Ibn Khaldoun, Tiaret, Algeria 14000 2Laboratory Technologies Soft, Promotion, Physical Chemistry of Biological Materials and Biodiversity, Science Faculty, University M'Hamed Bougara, Article Information BP 35000 Boumerdes, Algeria Received 31 August 2015 3 Revised 25 February 2016 Behavior and Ecology of Wildlife, I.N.R.A., CS 52627, 31326 Accepted 23 April 2016 Castanet Tolosan Cedex, France Available online 25 September 2016 Authors’ Contribution A B S T R A C T FB conceived and designed the study. -
Cic Pheonotype List Caprinae©
v. 5.25.12 CIC PHEONOTYPE LIST CAPRINAE © ARGALI 1. Altai Argali Ovis ammon ammon (aka Altay Argali) 2. Khangai Argali Ovis ammon darwini (aka Hangai & Mid Altai Argali) 3. Gobi Argali Ovis ammon darwini 4. Northern Chinese Argali - extinct Ovis ammon jubata (aka Shansi & Jubata Argali) 5. Northern Tibetan Argali Ovis ammon hodgsonii (aka Gansu & Altun Shan Argali) 6. Tibetan Argali Ovis ammon hodgsonii (aka Himalaya Argali) 7. Kuruk Tagh Argali Ovis ammon adametzi (aka Kuruktag Argali) 8. Karaganda Argali Ovis ammon collium (aka Kazakhstan & Semipalatinsk Argali) 9. Sair Argali Ovis ammon sairensis 10. Dzungarian Argali Ovis ammon littledalei (aka Littledale’s Argali) 11. Tian Shan Argali Ovis ammon karelini (aka Karelini Argali) 12. Kyrgyz Argali Ovis ammon humei (aka Kashgarian & Hume’s Argali) 13. Pamir Argali Ovis ammon polii (aka Marco Polo Argali) 14. Kara Tau Argali Ovis ammon nigrimontana (aka Bukharan & Turkestan Argali) 15. Nura Tau Argali Ovis ammon severtzovi (aka Kyzyl Kum & Severtzov Argali) MOUFLON 16. Tyrrhenian Mouflon Ovis aries musimon (aka Sardinian & Corsican Mouflon) 17. Introd. European Mouflon Ovis aries musimon (aka European Mouflon) 18. Cyprus Mouflon Ovis aries ophion (aka Cyprian Mouflon) 19. Konya Mouflon Ovis gmelini anatolica (aka Anatolian & Turkish Mouflon) 20. Armenian Mouflon Ovis gmelini gmelinii (aka Transcaucasus or Asiatic Mouflon, regionally as Arak Sheep) 21. Esfahan Mouflon Ovis gmelini isphahanica (aka Isfahan Mouflon) 22. Larestan Mouflon Ovis gmelini laristanica (aka Laristan Mouflon) URIALS 23. Transcaspian Urial Ovis vignei arkal (Depending on locality aka Kopet Dagh, Ustyurt & Turkmen Urial) 24. Bukhara Urial Ovis vignei bocharensis 25. Afghan Urial Ovis vignei cycloceros 26. -
Cervid Mixed-Species Table That Was Included in the 2014 Cervid RC
Appendix III. Cervid Mixed Species Attempts (Successful) Species Birds Ungulates Small Mammals Alces alces Trumpeter Swans Moose Axis axis Saurus Crane, Stanley Crane, Turkey, Sandhill Crane Sambar, Nilgai, Mouflon, Indian Rhino, Przewalski Horse, Sable, Gemsbok, Addax, Fallow Deer, Waterbuck, Persian Spotted Deer Goitered Gazelle, Reeves Muntjac, Blackbuck, Whitetailed deer Axis calamianensis Pronghorn, Bighorned Sheep Calamian Deer Axis kuhili Kuhl’s or Bawean Deer Axis porcinus Saurus Crane Sika, Sambar, Pere David's Deer, Wisent, Waterbuffalo, Muntjac Hog Deer Capreolus capreolus Western Roe Deer Cervus albirostris Urial, Markhor, Fallow Deer, MacNeil's Deer, Barbary Deer, Bactrian Wapiti, Wisent, Banteng, Sambar, Pere White-lipped Deer David's Deer, Sika Cervus alfredi Philipine Spotted Deer Cervus duvauceli Saurus Crane Mouflon, Goitered Gazelle, Axis Deer, Indian Rhino, Indian Muntjac, Sika, Nilgai, Sambar Barasingha Cervus elaphus Turkey, Roadrunner Sand Gazelle, Fallow Deer, White-lipped Deer, Axis Deer, Sika, Scimitar-horned Oryx, Addra Gazelle, Ankole, Red Deer or Elk Dromedary Camel, Bison, Pronghorn, Giraffe, Grant's Zebra, Wildebeest, Addax, Blesbok, Bontebok Cervus eldii Urial, Markhor, Sambar, Sika, Wisent, Waterbuffalo Burmese Brow-antlered Deer Cervus nippon Saurus Crane, Pheasant Mouflon, Urial, Markhor, Hog Deer, Sambar, Barasingha, Nilgai, Wisent, Pere David's Deer Sika 52 Cervus unicolor Mouflon, Urial, Markhor, Barasingha, Nilgai, Rusa, Sika, Indian Rhino Sambar Dama dama Rhea Llama, Tapirs European Fallow Deer -
Seismic Velocity Structure of the Continental Lithosphere from Controlled Source Data
Seismic Velocity Structure of the Continental Lithosphere from Controlled Source Data Walter D. Mooney US Geological Survey, Menlo Park, CA, USA Claus Prodehl University of Karlsruhe, Karlsruhe, Germany Nina I. Pavlenkova RAS Institute of the Physics of the Earth, Moscow, Russia 1. Introduction Year Authors Areas covered J/A/B a The purpose of this chapter is to provide a summary of the seismic velocity structure of the continental lithosphere, 1971 Heacock N-America B 1973 Meissner World J i.e., the crust and uppermost mantle. We define the crust as 1973 Mueller World B the outer layer of the Earth that is separated from the under- 1975 Makris E-Africa, Iceland A lying mantle by the Mohorovi6i6 discontinuity (Moho). We 1977 Bamford and Prodehl Europe, N-America J adopted the usual convention of defining the seismic Moho 1977 Heacock Europe, N-America B as the level in the Earth where the seismic compressional- 1977 Mueller Europe, N-America A 1977 Prodehl Europe, N-America A wave (P-wave) velocity increases rapidly or gradually to 1978 Mueller World A a value greater than or equal to 7.6 km sec -1 (Steinhart, 1967), 1980 Zverev and Kosminskaya Europe, Asia B defined in the data by the so-called "Pn" phase (P-normal). 1982 Soller et al. World J Here we use the term uppermost mantle to refer to the 50- 1984 Prodehl World A 200+ km thick lithospheric mantle that forms the root of the 1986 Meissner Continents B 1987 Orcutt Oceans J continents and that is attached to the crust (i.e., moves with the 1989 Mooney and Braile N-America A continental plates). -
Energy in Africa Challenges and Opportunities
SPRINGER BRIEFS IN ENERGY Manfred Hafner · Simone Tagliapietra Lucia de Strasser Energy in Africa Challenges and Opportunities SpringerBriefs in Energy SpringerBriefs in Energy presents concise summaries of cutting-edge research and practical applications in all aspects of Energy. Featuring compact volumes of 50– 125 pages, the series covers a range of content from professional to academic. Typical topics might include: • A snapshot of a hot or emerging topic • A contextual literature review • A timely report of state-of-the art analytical techniques • An in-depth case study • A presentation of core concepts that students must understand in order to make independent contributions. Briefs allow authors to present their ideas and readers to absorb them with minimal time investment. Briefs will be published as part of Springer’s eBook collection, with millions of users worldwide. In addition, Briefs will be available for individual print and electronic purchase. Briefs are characterized by fast, global electronic dissemina- tion, standard publishing contracts, easy-to-use manuscript preparation and formatting guidelines, and expedited production schedules. We aim for publication 8–12 weeks after acceptance. Both solicited and unsolicited manuscripts are considered for publication in this series. Briefs can also arise from the scale up of a planned chapter. Instead of simply contributing to an edited volume, the author gets an authored book with the space necessary to provide more data, fundamentals and background on the subject, methodology, future outlook, etc. SpringerBriefs in Energy contains a distinct subseries focusing on Energy Analysis and edited by Charles Hall, State University of New York. Books for this subseries will emphasize quantitative accounting of energy use and availability, including the potential and limitations of new technologies in terms of energy returned on energy invested. -
Berber Languages and Linguistics Mena B
Berber Languages and Linguistics Mena B. Lafkioui LAST MODIFIED: 24 MAY 2018 DOI: 10.1093/OBO/9780199772810-0219 Introduction Berber (aka Tamazight) is a branch of the Afro-Asiatic language phylum and counts about forty languages, which entirely cover North Africa, stretching from Morocco to Egypt, as well as from the Mediterranean Sea to the Sahara and the northern and western Sahel, including Mali, Niger, and Burkina Faso. The number of Berber speakers is estimated at more than forty million, of which the majority lives in Morocco (about 70 percent speaks Berber, mainly along with other languages). Berber has a general “continuum” makeup, which means that one Berber language gradually merges into another Berber language when they are contiguous. As a result, Berber forms a tightly knit and coherent bloc, which makes its subclassification very tricky. On the typological level, three major subdivisions can be made. The first is Northern Berber, which mainly contains Tarifit (including Senhaja Berber; North, Northeast, and Northwest Morocco), Tamazight of the Middle Atlas (Central Morocco), Figuig Berber (East Morocco), Kabyle Berber (North Algeria), Tashawit (Aures, Northeast Algeria), and some oasis languages like Berber of Mzab (South Algeria) and of Ouargla (South Algeria). The second is Southern Berber, which comprises languages such as Zenaga (Mauritania), Tashelhit (South Morocco), and Tetserret and Tuareg Berber (Sahara, Sahel). The third is Eastern Berber, which includes languages such as Berber spoken in Siwa (West Egypt), Sokna and El-Fogaha (Fezzan, Central Libya), Yefren and Zuara (Tripolitania, North Libya), and Ghadames (East Libya), as well as all the Berber languages of Tunisia (e.g., Jerba, Tamazret, and Sened). -
International Single Species Action Plan for the Conservation of the Argali Ovis Ammon
International Single Species Action Plan for the Conservation of the Argali Ovis ammon 1 This Single Species Action Plan has been prepared to assist the fulfillment of obligations under: Convention on the Conservation of Migratory Species of Wild Animals (CMS) International Single Species Action Plan for the Conservation of the Argali Ovis ammon CMS Technical Series No. XX April 2014 Prepared and printed with funding from 2 Support for this action plan: The development and production of this action plan has been achieved with the financial support of the European Union via the Deutsche Gesellschaft für Internationale Zusammenarbeit GmbH (GIZ) in the framework of the FLERMONECA Regional Project Forest and Biodiversity Governance Including Environmental Monitoring. Compiled by: David Mallon, Navinder Singh, Christiane Röttger1, UNEP / CMS Secretariat, United Nations Premises, Platz der Vereinten Nationen 1 , 53113 Bonn, Germany E-mail for correspondence: [email protected] List of Contributors: Muhibullah Fazli (Afghanistan); Alexander Berber, Maksim Levitin (Kazakhstan); Askar Davletbakov, Nadezhda Emel’yanova, Almaz Musaev, (Kyrgyzstan); Tarun Kathula (India); Onon Yondon, Sukh Amgalanbaatar (Mongolia); Dinesh Prasad Parajuli (Nepal); Nurali Saidov, Munavvar Alidodov, Abdulkadyrkhon Maskaev (Tajikistan); Tatiana Yudina (Russian Federation); Alexandr Grigoryants (Uzbekistan); Sergey Sklyarenko (Association for the Conservation of Biodiversity of Kazakhstan, ACBK); Gerhard Damm, Kai-Uwe Wollscheid (International Council for Game and Wildlife -
Wild, Feral and Domesticated Breeds of Sheep G
Seasonal cycles in the blood plasma concentration of FSH, inhibin and testosterone, and testicular size in rams of wild, feral and domesticated breeds of sheep G. A. Lincoln, C. E. Lincoln and A. S. McNeilly MRC Reproductive Biology Unit, Centre for Reproductive Biology, 37 Chalmers Street, Edinburgh EH3 9EW, UK; and *Kirkton Cottages, Auchtertool, Fife KY2 5XQ, UK Summary. Seasonal cycles in testicular activity in rams were monitored in groups of wild (mouflon), feral (Soay) and domesticated breeds of sheep (Shetland, Blackface, Herdwick, Norfolk, Wiltshire, Portland and Merino) living outdoors near Edinburgh (56\s=deg\N).The changes in the blood plasma concentrations of FSH, inhibin and testoster- one, and the diameter of the testis were measured every half calendar month from 1 to 3 years of age. There were significant differences between breeds in the magnitude and timing of the seasonal reproductive cycle. In the mouflon rams, the seasonal changes were very pronounced with a 6\p=n-\15-foldincrease in the plasma concentrations of FSH, inhibin and testosterone from summer to autumn, and a late peak in testicular diameter in October. In the Soay rams and most of the domesticated breeds, the seasonal increase in the reproductive hormones occurred 1\p=n-\2months earlier with the peak in testicular size in September or October. In the two southern breeds (Portland and Merino), the early onset of testicular activity was more extreme with the seasonal maxi- mum in August. In cross-bred rams, produced by mating Soay ewes (highly seasonal breed) with Portland or Merino rams (less seasonal breeds), there was a seasonal repro- ductive cycle that was intermediate compared to that of the parents. -
Mixed-Species Exhibits with Pigs (Suidae)
Mixed-species exhibits with Pigs (Suidae) Written by KRISZTIÁN SVÁBIK Team Leader, Toni’s Zoo, Rothenburg, Luzern, Switzerland Email: [email protected] 9th May 2021 Cover photo © Krisztián Svábik Mixed-species exhibits with Pigs (Suidae) 1 CONTENTS INTRODUCTION ........................................................................................................... 3 Use of space and enclosure furnishings ................................................................... 3 Feeding ..................................................................................................................... 3 Breeding ................................................................................................................... 4 Choice of species and individuals ............................................................................ 4 List of mixed-species exhibits involving Suids ........................................................ 5 LIST OF SPECIES COMBINATIONS – SUIDAE .......................................................... 6 Sulawesi Babirusa, Babyrousa celebensis ...............................................................7 Common Warthog, Phacochoerus africanus ......................................................... 8 Giant Forest Hog, Hylochoerus meinertzhageni ..................................................10 Bushpig, Potamochoerus larvatus ........................................................................ 11 Red River Hog, Potamochoerus porcus ............................................................... -
Ovis Ammon Linnaeus, 1758) with All Subspecies Is Proposed to Be Included in Appendix II of the Convention
1 of 32 Proposal II / 1 PROPOSAL FOR INCLUSION OF SPECIES ON THE APPENDICES OF THE CONVENTION ON THE CONSERVATION OF MIGRATORY SPECIES OF WILD ANIMALS A. PROPOSAL: The species argali (Ovis ammon Linnaeus, 1758) with all subspecies is proposed to be included in Appendix II of the Convention B. PROPONENT: Republic of Tajikistan and Republic of Kazakhstan C. SUPPORTING STATEMENT: 1. Taxon 1.1 Classis : Mammalia 1.2 Ordo : Cetartiodactyla 1.3 Familia : Bovidae 1.4 Genus or Species : Ovis ammon (Linnaeus, 1758) 1.5 Common name(s) : English - Argali, Wild Sheep French - Mouflon D'Asie, Mouflon D'Eurasie, Mouflon Vrai Spanish - Muflón Argal 2. Biological data 2.1 Distribution (current and historical) Currently nine subspecies of argali are recognized (Wilson and Reeder, 2005 and Fedosenko and Blank, 2005): Altai argali (Ovis ammon ammon) Karaganda argali (Ovis ammon collium) Gobi argali (Ovis ammon darwini) Tibetan argali (Ovis ammon hodgsoni) North China argali (Ovis ammon jubata) (=comosa) Tian Shan argali, (Ovis ammon karelini) Karatau argali (Ovis ammon nigrimontana) Marco Polo argali (Ovis ammon polii) Severtzov argali, (Ovis ammon severtzovi) Argali live over a vast geographic range, but are separated into more-or-less disjunctive populations, some of which are morphologically identifiable. How much (if any) of the taxon’s disjunctive distribution is natural and how much the result of anthropogenic influence remains open to date. Similarly, how (and even whether) various populations should be classified subspecifically remains contentious.