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Squeezed Dry : the Historical Trajectory of the Lower Jordan River Basin
2 Squeezed Dry: the Historical Trajectory of the Lower Jordan River Basin Mauro Van Aken,1* François Molle2** and Jean-Philippe Venot3*** 1University of Milan-Bicocca, Italy; 2Centre IRD, Montpellier, France; 3International Water Management Institute, Accra, Ghana; e-mails: *[email protected]; **[email protected]; ***[email protected] Introduction response options are interdependent and reveal the political and contested nature of The lower Jordan River basin (LJRB) provides resource sharing and water management (Molle a fascinating tale of coupled social and environ- et al., 2007). This chapter describes how these mental transformations of a waterscape. In this processes, constrained by the drastic natural semi-arid to desert area, water is an essential conditions of the basin, have unfolded since determinant of life, cultural values, social struc- the late 1950s and explores possible futures. tures, economic activities, power and politics. The trajectory of this basin from a nomadic agro-pastoral Bedouin culture to an urbanized Features of the Lower Jordan River Basin region where water circulation is highly artifi- cial, illustrates how a particular resource The Jordan River is an international river endowment is valued, mobilized, shared, used which drains a total area of about 18,000 km². and fought for. Its three headwater tributaries originate in This chapter first recounts past water Lebanon and Syria and flow into Lake Tiberius, resource development in the LJRB – defined as a freshwater reservoir now used almost exclu- the Jordanian part of the Jordan River basin, sively by Israel (Fig. 2.1). The Jordan River downstream of Lake Tiberius – and dwells on then flows southward before discharging into the specific relationships between water, local the Dead Sea. -
A Window Into Paleocene to Early Eocene Depositional History in Egypt Basedoncoccolithstratigraphy
The Dababiya Core: A window into Paleocene to Early Eocene depositional history in Egypt basedoncoccolithstratigraphy Marie-Pierre Aubry1 and Rehab Salem1,2 1Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, NJ 08854-8066, USA email: [email protected] 2Geology Department, Faculty of Science, Tanta University, 31527, Tanta, Egypt [email protected] ABSTRACT: The composite Paleocene-lower Eocene Dababiya section recovered in the Dababiya Quarry core and accessible in out- crop in the Dababiya Quarry exhibits an unexpected contrast in thickness between the Lower Eocene succession (~Esna Shales) and the Paleocene one (~Dakhla Shales and Tarawan Chalk). We investigate the significance of this contrast by reviewing calcareous nannofossil stratigraphic studies performed on sections throughout Egypt. We show that a regional pattern occurs, and distinguish six areas—Nile Valley, Eastern Desert and western Sinai, Central and eastern Sinai, northern Egypt and Western Desert. Based on patterns related to thicknesses of selected lithobiostratigraphic intervals and distribution of main stratigraphic gaps, we propose that the differences in the stratigraphic architecture between these regions result from differential latest Paleocene and Early Eocene subsidence following intense Middle to Late Paleocene tectonic activity in the Syrian Arc folds as a result of the closure of the Neo-Tethys. INTRODUCTION view of coccolithophore studies in Egypt since their inception During the Late Cretaceous and Early Paleogene Egypt was (1968). Coccolith-bearing sedimentary rocks as old as part of a vast epicontinental shelf at the edge of the southern Cenomanian outcrop in central Sinai (Thamed area; Bauer et al. Tethys (text-fig. 1). Bounded by the Arabian-Nubian craton to 2001; Faris and Abu Shama 2003). -
The Birds (Aves) of Oromia, Ethiopia – an Annotated Checklist
European Journal of Taxonomy 306: 1–69 ISSN 2118-9773 https://doi.org/10.5852/ejt.2017.306 www.europeanjournaloftaxonomy.eu 2017 · Gedeon K. et al. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:A32EAE51-9051-458A-81DD-8EA921901CDC The birds (Aves) of Oromia, Ethiopia – an annotated checklist Kai GEDEON 1,*, Chemere ZEWDIE 2 & Till TÖPFER 3 1 Saxon Ornithologists’ Society, P.O. Box 1129, 09331 Hohenstein-Ernstthal, Germany. 2 Oromia Forest and Wildlife Enterprise, P.O. Box 1075, Debre Zeit, Ethiopia. 3 Zoological Research Museum Alexander Koenig, Centre for Taxonomy and Evolutionary Research, Adenauerallee 160, 53113 Bonn, Germany. * Corresponding author: [email protected] 2 Email: [email protected] 3 Email: [email protected] 1 urn:lsid:zoobank.org:author:F46B3F50-41E2-4629-9951-778F69A5BBA2 2 urn:lsid:zoobank.org:author:F59FEDB3-627A-4D52-A6CB-4F26846C0FC5 3 urn:lsid:zoobank.org:author:A87BE9B4-8FC6-4E11-8DB4-BDBB3CFBBEAA Abstract. Oromia is the largest National Regional State of Ethiopia. Here we present the first comprehensive checklist of its birds. A total of 804 bird species has been recorded, 601 of them confirmed (443) or assumed (158) to be breeding birds. At least 561 are all-year residents (and 31 more potentially so), at least 73 are Afrotropical migrants and visitors (and 44 more potentially so), and 184 are Palaearctic migrants and visitors (and eight more potentially so). Three species are endemic to Oromia, 18 to Ethiopia and 43 to the Horn of Africa. 170 Oromia bird species are biome restricted: 57 to the Afrotropical Highlands biome, 95 to the Somali-Masai biome, and 18 to the Sudan-Guinea Savanna biome. -
Fish Species Assemblages in Two Riverine Systems of Mujib Basin in Jordan and the Effects of Impoundment
Volume 7, Number 3, September .2014 ISSN 1995-6673 JJBS Pages 179 - 185 Jordan Journal of Biological Sciences Fish Species Assemblages in Two Riverine Systems of Mujib Basin in Jordan and the Effects of Impoundment Nashat A. F. Hamidan* Royal Society for the Conservation of Nature [RSCN], Jordan; and Centre for Conservation Ecology and Environmental Science, School of Applied Sciences, Bournemouth University, Poole, BH12 5BB, United Kingdom. Received: April 4, 2014 Revised: May 6, 2014 Accepted: May 15, 2014 Abstract Mujib and Haidan rivers were sampled in July 2011 to identify fish populations in the riverine system, and to investigate the impact caused by the existence of two dams. Fishes were sampled by electofishing gear through 14 sampling points distributed along the two rivers. The Mujib Dam lake was sampled by gillnets. A total of 2,854 fish specimen were caught during the study of which most consisted of native species but included small numbers of invasive species. The native Capoeta damascina and Oxynoemacheilus insignis were found in both rivers but Garra rufa was only recorded below their confluence to the west. Four invasive species were recorded. The cichlids Oreochromis aureus and Tilapia zillii were sampled along Mujib River, and the African Catfish Clarias gariepinus and the Common Carp Cyprinus carpio were observed only in the lake of Mujib Dam but were not sampled. The construction of the two dams has led to significant changes in the habitats, water flow, and hydrology of the two rivers both upstream and downstream, and enhanced the colonisation of invasive species. There is, therefore, an urgent need to review the management of the system across all stakeholders and to continue monitoring on a regular basis. -
SMART-MOVE BMBF Funding No.: 02WM1355B
Sustainable Management of Available Water Resources with Innovative Technologies Management of Highly Variable Water Resources in semi- arid Regions" - Israel (ISR), Jordan, Palestine (PSE) SMART-MOVE BMBF Funding No.: 02WM1355B Working Package 3: Wastewater Management towards Groundwater Protection Deliverable No. 3.3: Roll-out investment project for regional implementation of DWWT&R systems Authors: Mi-Yong Becker (UFZ) Ganbaatar Khurelbaatar (UFZ) Manfred van Afferden (UFZ) Ali Subha (MWI) Roland A. Müller (UFZ) Date: 30.11.2018 Funded by Roll-out investment project for regional implementation of DWWT&R systems ii CONTENT 1 DELIVERABLE 3.3 – ROLL-OUT INVESTMENT PROJECT FOR REGIONAL IMPLEMENTATION OF DWWT&R SYSTEMS .............................. 1 2 TASK 3.3.1: DEFINITION OF REQUIREMENTS FOR A DWWM SYSTEM AS A TOOL FOR THE PROTECTION OF GROUNDWATER IN PRIORITY AREAS OF JORDAN .............................................................. 2 2.1 Hot spots and vulnerable water resources ........................................... 2 2.2 Al-Balqa Governorate ....................................................................... 3 3 TASK 3.3.2: ECONOMIC EFFICIENCY OF DIFFERENT SCENARIOS OF GROUNDWATER PROTECTION ............................................................. 5 3.1 Objective ........................................................................................ 6 3.2 Study Area ...................................................................................... 6 3.3 Assessment of current situation ........................................................ -
Origin of the Sinai-Negev Erg, Egypt and Israel: Mineralogical and Geochemical Evidence for the Importance of the Nile and Sea Level History Daniel R
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- ubP lished Research US Geological Survey 2013 Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. Muhs U.S. Geological Survey, [email protected] Joel Roskin Ben-Gurion University of the Negev Haim Tsoar Ben-Gurion University of the Negev Gary Skipp U.S. Geological Survey, [email protected] James Budahn U.S. Geological Survey See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Geology Commons, Oceanography and Atmospheric Sciences and Meteorology Commons, Other Earth Sciences Commons, and the Other Environmental Sciences Commons Muhs, Daniel R.; Roskin, Joel; Tsoar, Haim; Skipp, Gary; Budahn, James; Sneh, Amihai; Porat, Naomi; Stanley, Jean-Daniel; Katra, Itzhak; and Blumberg, Dan G., "Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history" (2013). USGS Staff -- Published Research. 931. https://digitalcommons.unl.edu/usgsstaffpub/931 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- ubP lished Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Daniel R. Muhs, Joel Roskin, Haim Tsoar, Gary Skipp, James Budahn, Amihai Sneh, Naomi Porat, Jean-Daniel Stanley, Itzhak Katra, and Dan G. Blumberg This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/usgsstaffpub/931 Quaternary Science Reviews 69 (2013) 28e48 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Origin of the SinaieNegev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. -
Buckbird Journeys
BUCKBIRD JOURNEYS YEMEN and SOCOTRA Tuesday 8 – Sunday 18 November 2007 Participants Louise Augustine (LA), Hugh Buck (HB), David Daniels (DD), David Hoddinott (DH), Pearl Jordan (PJ), Werner Suter (WS), David Bradford (DB – Socotra only) This trip was designed to try for all the Southwest Arabia and Socotra endemics in a relatively brief time scale. It also represented an opportunity for regional listers to add an enticing selection of “African” species only entering Asia in Southwest Arabia and a selection of “Asian” species found in Africa rarely outside of Socotra. That the trip was successful on all counts is a tribute to Yousuf Mohageb (YM) of Arabian Eco- Tours in Sana’a who designed, with HB, the itinerary, accompanied us throughout Yemen and knew all the best birding spots, Ali his redoubtable co-driver and Ahmed Saeid Suliman (AS) on Socotra whose knowledge and love of all things on his island home is second to none. Our multinational group (three Americans, two Brits, a South African and a Swiss) kept to the pace admirably, provided exceptional spotting skills and, in WS, some wonderful photographic documentation and memories. Day by Day Thursday 8 November HB, DD and DH meet up at Dubai International Airport for the short Emirates Airlines flight to Sana’a where they are met by YM, Ali in traditional Yemeni costume and LA and PJ who have arrived the previous evening. Under the high bright sun, which will be the norm for the next 10 days, we traverse Sana’a’s sprawling outskirts to the Funduk Arabia Felix, an interesting hotel made up a several old traditional houses right at the edge of the historic and UNESCO rated old town. -
AERC Wplist July 2015
AERC Western Palearctic list, July 2015 About the list: 1) The limits of the Western Palearctic region follow for convenience the limits defined in the “Birds of the Western Palearctic” (BWP) series (Oxford University Press). 2) The AERC WP list follows the systematics of Voous (1973; 1977a; 1977b) modified by the changes listed in the AERC TAC systematic recommendations published online on the AERC web site. For species not in Voous (a few introduced or accidental species) the default systematics is the IOC world bird list. 3) Only species either admitted into an "official" national list (for countries with a national avifaunistic commission or national rarities committee) or whose occurrence in the WP has been published in detail (description or photo and circumstances allowing review of the evidence, usually in a journal) have been admitted on the list. Category D species have not been admitted. 4) The information in the "remarks" column is by no mean exhaustive. It is aimed at providing some supporting information for the species whose status on the WP list is less well known than average. This is obviously a subjective criterion. Citation: Crochet P.-A., Joynt G. (2015). AERC list of Western Palearctic birds. July 2015 version. Available at http://www.aerc.eu/tac.html Families Voous sequence 2015 INTERNATIONAL ENGLISH NAME SCIENTIFIC NAME remarks changes since last edition ORDER STRUTHIONIFORMES OSTRICHES Family Struthionidae Ostrich Struthio camelus ORDER ANSERIFORMES DUCKS, GEESE, SWANS Family Anatidae Fulvous Whistling Duck Dendrocygna bicolor cat. A/D in Morocco (flock of 11-12 suggesting natural vagrancy, hence accepted here) Lesser Whistling Duck Dendrocygna javanica cat. -
Download the Latest Bird List Here (Pdf)
Birds of the ‘Lolldaiga-Mukogodo-Ewaso N’yiro Important Bird and Biodiversity Area’ Threatened Species (13 species) Critically Endangered (4 species) Tyigonoceps occipitalis White-headed vulture Necrosyrtes monachus Hooded vulture Gyps africanus White-backed vulture Gyps rueppellii Rüppell’s vulture Endangered (5 species) Ardeola idae Madagascar pond heron Neophron percnopterus Egyptian vulture Torgos tracheliotus Lappet-faced vulture Aquila nipalensis Steppe eagle Balearica regulorum Grey crowned crane Vulnerable (4 species) Falco fasciinucha Taita falcon Sagittarius serpentarius Secretarybird Polemaetus bellicosus Martial eagle Bucorvus leadbeateri Southern ground hornbill Near Threatened (12 species) Oxyura maccoa Maccoa duck 1 Phoeniconaias minor Lesser flamingo Falco vespertinus Red-footed falcon Falco concolor Sooty falcon Gypaetus barbatus Lammergeier Terathopius ecaudatus Bateleur Circus macrourus Pallid harrier Stephanoaetus coronatus Crowned eagle Ardeotis kori Kori bustard Numenius arquata Eurasian curlew Calidris ferruginea Curlew sandpiper Euplectes jacksoni Jackson’s widowbird _________________________________________________________________________________________ Birds of the ‘Lolldaiga-Mukogodo-Ewaso N’yiro Important Bird and Biodiversity Area’¹ Order and scientific name² Common name² Threat3 Comments Struthionidae Ostrich Struthio camelus Common ostrich LC Numididae Guineafowl Numida meleagris Helmeted guineafowl LC Acryllium vulturinum Vulturine guineafowl LC Phasianidae Stone partridge, francolins, spurfowl, quails -
Serpentinites in the Eastern Desert, Egypt: Fragments of Forearc Mantle
Neoproterozoic (835–720 Ma) Serpentinites in the Eastern Desert, Egypt: Fragments of Forearc Mantle Mokhles K. Azer and Robert J. Stern1 Geology Department, National Research Centre, Al-Behoos Street, 12622-Dokki, Cairo, Egypt (e-mail: [email protected]) ABSTRACT Most Neoproterozoic ophiolites of the Arabian-Nubian Shield show compositions consistent with formation in a suprasubduction zone environment, but it has not been clear whether this was in a forearc or back-arc setting. Ophiolitic serpentinites are common in the Eastern Desert of Egypt, but their composition and significance are not well understood. Here we report new petrographic, mineral, chemical, and whole-rock compositional data for ser- pentinites from Wadi Semna, the northernmost ophiolitic serpentinites in the Eastern Desert, and use these to provide insights into the significance of other Eastern Desert serpentinite locales. The Wadi Semna serpentinites are composed essentially of antigorite, chrysotile, and lizardite, with minor carbonate, chromite, magnetite, magnesite, and chlorite, and they were tectonically emplaced. The alteration of chrome spinel to ferritchromite was accompanied by the formation of chloritic aureoles due to the release of Al from spinel. Major-element compositions indicate that, except for the addition of water, the serpentinites have not experienced extensive element mobility; these were originally ϩ CaO- and Al2O3-depleted harzburgites similar to peridotites from modern oceanic forearcs. High Cr# (Cr/(Cr Al) ) in the relict spinels (average p 0.69 ) indicates that these are residual after extensive partial melting, similar to spinels in modern forearc peridotites. These characteristics of Wadi Semna serpentinites also typify 22 other Eastern Desert serpentinite localities. We infer that Eastern Desert ophiolitic serpentinites, except perhaps Gebel Gerf, originated by forearc seafloor spreading during subduction initiation associated with the closing of the Neoproterozoic Mozam- bique Ocean. -
Water Reuse and Environmental Conservation Project Contract No
WATER REUSE AND ENVIRONMENTAL CONSERVATION PROJECT CONTRACT NO. EDH–I–00–08–00024–00 ORDER NO. 04 PRELIMINARY SITE ASSESSMENT FOR WATER REUSE PILOT AT AL-LAJJOUN December 2014 IMPLEMENTED BY AECOM December 2014 This document was produced for review by the United States Agency for International Development. It was prepared by AECOM. i WATER REUSE AND ENVIRONMENTAL CONSERVATION PROJECT CONTRACT NO. EDH–I–00–08– 00024–00 ORDER NO. 04 PRELIMINARY SITE ASSESSMENT FOR WATER REUSE PILOT AT AL-LAJJOUN DECEMBER 2014 Submitted to: USAID Jordan Prepared by: AECOM DISCLAIMER: The authors‟ views expressed in this document do not necessarily reflect the views of the United States Agency for International Development or the United States Government. Table of Contents Contents 1. Introduction and Baseline Assessment ..................................................................... 1 1.1 Introduction ..................................................................................................................... 1 1.1.1 Background .............................................................................................................. 1 1.1.2 Summary of conclusions .......................................................................................... 2 1.2 Baseline Study ................................................................................................................. 2 1.2.1 Site Description........................................................................................................ 3 1.3 Biophysical Environment -
Sequence Stratigraphy and Depositional Environments of Late Cretaceous–Early Palaeogene Succession, North Eastern Desert, Egypt
Swiss J Geosci (2015) 108:345–359 DOI 10.1007/s00015-015-0201-4 Sequence stratigraphy and depositional environments of Late Cretaceous–Early Palaeogene succession, North Eastern Desert, Egypt 1,2 1 Mohamed Youssef • Mahmoud Hefny Received: 25 March 2015 / Accepted: 21 September 2015 / Published online: 14 November 2015 Ó Swiss Geological Society 2015 Abstract The foraminiferal contents and geochemistry of controlled by both eustatic sea-level changes and tectonic 199 samples collected from three surface sections in the movements that prevailed during deposition. southern Galala Sub-basin, North Eastern Desert of Egypt, have been studied in detail. From south to north these Keywords Depositional environments Á High resolution sections are situated at Gebel Tarboul, Wadi Tarfa, and Bir sequence stratigraphy Á Cretaceous Á Palaeogene Á Eastern Dakhl. The results allow reconstructing of the depositional Desert Á Egypt environments and high resolution sequence stratigraphy of the Upper Cretaceous–Palaeogene succession. The quan- titative and qualitative distribution patterns of benthic 1 Introduction foraminifera of the Upper Cretaceous–Lower Palaeogene succession suggests a depositional environment from outer The Cretaceous–Palaeogene interval provides one of the neritic to bathyal, at 200 to *700 m water-depth. Based on best opportunities to calibrate depositional sequences sequence stratigraphic analyses, ten complete third order against an integrated stratigraphic framework. This can be depositional sequences have been recognized. These examined in the rocks of Cretaceous–Palaeogene age that depositional sequences from base to top are as follows: are widely distributed in Northern Africa along the south- CaSGB-1 sequence, CaSGB-2 sequence, MaSGB-1 ern margin of the Tethys Ocean.