Wallonia, a Region of Great Natural Wealth in the Heart of Europe

Total Page:16

File Type:pdf, Size:1020Kb

Wallonia, a Region of Great Natural Wealth in the Heart of Europe Wallonia, a region of great natural wealth in the heart of Europe The Herve Plateau Montagu’s Bordering Hautes-Fagnes (High Fens) and This also applies to the network of old haw- Harrier JG CPDT the river Vesdre, the Herve plateau offers thorn hedges, formerly used to mark the SR Grass snake JD quite an outstanding landscape, result of a meadows’ boundaries. All these features are North of the Sambre Cart tracks also offer refuge to small animals long farming history. Ponds surrounded by essential nowadays to protect the fauna (bat- Gaume or that are similar to those in the hedgerows (corn pollarded trees are created in old watering rachians such as common frogs, common and Meuse Valley buntings and hedgehogs). Some tall standard places dug for the cattle. Numerous orchards toads, newts, Natterjack toads and birds such Belgian Lorraine Soil quality is one of the main features of this orchards are also still to be found here and rows were planted long ago to increase the farm- as little owls) in an area now used for intensive Belgian Lorraine lays on three limestone terraces, Grasshoppers can also be found here and, in fertile area devoted to large fields of crops of pollarded willows (north of Tournai region, ers’ income (standard pear trees mainly). cattle farming (for dairy production). the Cuestas, crossing through it from west to east. wetter areas, the meadow fritillary and the west- and bringing together the Scheldt valley, the « le Pays des Collines »), a few wetter meadows Here the soil is fairly porous, of a sandy-loamy ern marsh orchid. plateaux of Hesbaye and the outskirts of the at the bottom of the valley and other features type alternating with chalky hills that used to be On the slopes of these valleys and the southern Liège area. These large spaces are not lacking that are essential to the ecological network extensively grazed and where even more orchids edges of the Cuestas, attractive networks of very in interest to biodiversity: skylarks, quails, corn (ditches, the grassy borders of fields and grassy can be found. This area is regarded as the richest, varied hedgerows have developed. A few old or- buntings and partridges nest on the ground here. headlands). along with Fagne-Famenne, as far as biodiversity chards of tall standard trees have been preserved is concerned. This is mainly due to farming that in the villages. has remained fairly non-intensive in many areas The gentle slopes and the upper part of the hill- and for quite a long time now. In the main val- sides host fields of cereal crops that, from time to leys of Semois, Vire and Ton, there are still quite time, also provide shelter to a variety of cornfield Common frog CS a number of wet meadows and non-intensive hay flowers become rare such as the cornflower, corn meadows. They harbour a range of typical plants marigold, the field cowwheat, the round-leaved species such as the meadow hawksbeard, field fluellen, the corn violet, the stoneseed and the yel- scabious, meadow salsify and the autumn crocus. low pea or vetch. Hare HK Corn bunting JMP Ardennes draft horse PS Burnet AO Old world swallowtail JD EG Condroz Fagne-Famenne The specific relief of Condroz concerns the A land of forests and meadows, Fagne- alternation of sandstone plateaux, mainly oc- Famenne is a long and narrow depression cupied by crops or broad-leaved woods, and squeezed between the Ardennes and Condroz, SR Black stork JMP limestone depressions, where the meadows parted in two by the Meuse river. Rocks peep dominate on clayey-loamy ground. This pro- through in numerous areas, schistose in the duces a patchwork of environments with a north and limestone in the south (Calestienne). The Ardennes mixture of crops, meadows, forest edges and Its clayey, impermeable valleys aren’t quite suit- Green-winged The soil quality and the climate restrict the ability streams. A few wet meadows and hay mead- able for intensive farming. On the other hand, orchid EW to grow crops. This region is, therefore, essentially ows with quite a rich diversity brighten up its limestone hillsides are characterised by dry wooded and used for raising cattle. Extensive the entire region. A large variety of flora and meadows (called limestone grassland) where meadows at the bottom of valleys, often wet fauna is found here: little owls, bats, kingfish- several magnificent species of orchids can be or even marshy, can provide hiding places for ers as well as wild boar, roe deer and badgers. observed. birds (the whinchat and the meadow pipit) and Agrogeographic areas Quickset hedges and the remains of orchards Most species of harvest flowers (field cow- butterflies (such as the copper butterfly and the “Ardennais are still to be found next to the villages. Par- wheat, corn violet, etc.) have survived in the Area boundaries bog fritillary). The region also hosts plants with roux” sheep CM ticularly interesting for wildlife, the Sorée pla- cultivated fields located in the limestone parts Outside agrogeographic areas sub-mountainous characteristics such as alpine teau, close to Gesves, contains a network of of this region. (Haine, Sambre and Meuse fennel, wood cranesbill and the great burnet. In ponds in particular, where several species of river valleys) the Upper Ardennes, the network of hedgerows batrachians, dragonflies and many other en- Chief towns of districts is one of the most developed in Wallonia (the dangered species live together. SR hedged farmland of Malmédy). Watercourses Sources : Zones agrogéographiques : DGATLP 1997 / Noyaux : INS 1991 / Occupation du sol : IGN.
Recommended publications
  • ROCHEFORT, V1
    ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 644000 646000 648000 650000 652000 654000 656000 658000 660000 ! ! ! ! 5°1'0"E !5°2'0"E 5°3'0"E 5°4'0"E 5°5'0"E 5°6'0"E 5°7'0"E 5°8'0"E 5°9'0"E 5°10'0"E ! 5°11'0"E 5°12'0"E 5°13'0"E 5°14'0"E ! ! ! ! ! ! ! ! N " ! ! GLIDE number: N/A Activation ID: EMSR518 0 ! ' ! 3 ! 1 ! ! ° ! ! Int. Charter Act. ID: N/A Product N.: 02ROCHEFORT, v1 0 5 ! ! ! F R ! ! ! o ! u ! n ! i ! s ! i ! d Dén s ! ! Rochefort - BELGIUM d ! e ! ! ! ! e a ! ! ! u ! ! ! R ! ! e d ! ! ! 0 ! 0 Flood - Situation as of 17/07/2021 u u ! ! ! ! 0 0 ! x ! 0 ! 0 ! ! ! Lavis ! ! 4 4 ! ! 6 ! 6 ! ! ! ! ! Delineation MONIT01 - Detail map 02 5 ! ! 5 5 ! 5 ! R ! ! ! ! u ! ! d is Noord-Brabant ! ! e se ! Marche-en-Famenne Arnsberg D! a ! ! o u ! Limburg Dusseldorf ! ! Custinne nn ! Prov. ! ! e ! u ! (NL) ! x ! Antwerpen ! ! ! e ! ! n ! N L ig ! " Prov. 'Iwoigne 0 ! ! o ! ' ! w 2 1 ! Y Navaugle! ° Limburg l' ! 0 H! umain 5 ! R Prov. ! u Netherlands l ! a (BE) ! i ! Vlaams-Brabant ! s M ! s ! L ! North Sea 'Ywo e igne o Havrenne ! r a Koln s N u ! ! " ! Prov. 01 a R 0 ! Belgium ' y d ! 2 Brabant h e e 1 ! ! i ! ° ! ! n 0 Wallon x ! e Germany 5 n ! , ! u a ! ! r ^ W a i ! h B Brussels a ! a ! c ! e se l ! u a u L Me Prov. Liege ! V sea uis ! ! e R s ! L ge , Lahn ! s Lo Prov.
    [Show full text]
  • Bankfull Discharge Recurrence Interval in Gravel-Bed Rivers
    EARTH SURFACE PROCESSES AND LANDFORMS, VOL 22, 685±693 (1997) BANKFULL DISCHARGE RECURRENCE INTERVAL IN GRAVEL-BED RIVERS F. PETIT* AND A. PAUQUET Department of Physical Geography, University of LiÁege, Institut de GÂeographie, AllÂee du AoÃut, 2, Sart Tilman, BÃatiment B11, B4000 LiÁege, Belgium Received 17 February 1995; Revised 22 August 1996; Accepted 31 August 1996 ABSTRACT Bankfull discharge was identi®ed in some 30 gravel-bed rivers representing in total c. 40 gauging stations. The catchment sizes vary from 4km2 to nearly 2700km2. Bankfull discharge value increases with basin size. In the case of gravel-bed 1´044 rivers developed on an impermeable substratum, the following equation emerges: Qb=0´087 A . Bankfull discharge recurrence interval was determined by ®tting maximum annual ¯oods (Ta) into Gumbel's distribution and then using the partial duration series (Tp) in this same distribution. Recurrence interval is below 0´7 years (Tp) for small pebble-bed rivers developed on an impermeable substratum; it reaches 1´1 to 1´5 years when the catchment size of these rivers exceeds 250km2. Rivers incised in the soft schists of the Famenne show larger channel capacity at bankfull stage, a small width/ depth ratio and thus higher recurrence intervals (1´4±5´3 years with Ta and 1±4´4 years with Tp). Base¯ow-dominated gravel-bed streams and sandy or silty rivers experience less frequent bankfull discharges, with a recurrence interval higher than 2 or even 3 years (Tp). 1997 by John Wiley & Sons, Ltd. Earth surf. process. landforms, 22, 685±693 (1997) No. of ®gures: 5 No.
    [Show full text]
  • Wabmagazine Discover a Region That Combines Technical Knowhow with Quality of Life
    wallonia and brussels summer 2020 wabmagazine Discover a region that combines technical knowhow with quality of life THE GREAT ESCAPE WALLONIA LAUNCHES SUMMER TOURISM CAMPAIGN Covid-19: Local companies join global response to fight the pandemic Meet the fashion designers growing their brands internationally .CONTENTS 6 Editorial The unprecedented challenge of Covid-19 drew a sharp Wallonia and Brussels - Contact response from key sectors across Wallonia. As companies as well as individuals took action to confront the crisis, www.wallonia.be their actions were pivotal for their economic survival as www.wbi.be well as the safety of their employees. For audio-visual en- terprise KeyWall, the combination of high-tech expertise and creativity proved critical. Managing director Thibault Baras (pictured, above) tells us how, with global activities curtailed, new opportunities emerged to ensure the com- pany continues to thrive. Investment, innovation and job creation have been crucial in the mobilisation of the region’s biotech, pharmaceutical and medical fields. Our focus article on page 14 outlines their pursuit of urgent research and development projects, from diagnosis and vaccine research to personal protec- tion equipment and data science. Experts from a variety of fields are united in meeting the challenge. Underpinned by financial and technical support from public authori- ties, local companies are joining the international fight to Editor Sarah Crew better understand and address the global pandemic. We Deputy editor Sally Tipper look forward to following their ground-breaking journey Reporters Andy Furniere, Tomáš Miklica, Saffina Rana, Sarah Schug towards safeguarding public health. Art director Liesbet Jacobs Managing director Hans De Loore Don’t forget to download the WAB AWEX/WBI and Ackroyd Publications magazine app, available for Android Pascale Delcomminette – AWEX/WBI and iOS.
    [Show full text]
  • Cerfontaine : Cerfontaine Tité De Cerfontaine (Voir Encadré)
    Ouvertures et châssis Protection de l’habitat traditionnel Dans le bâti traditionnel de l’entité de Cer- Afin de préserver au mieux le caractère de fontaine, les ouvertures de forme verticale Dispositifs de protection appliqués sont dominantes. nos villages, différentes mesures réglemen- taires spécifiques sont appliquées dans l’en- à l’entité de Cerfontaine : Cerfontaine tité de Cerfontaine (voir encadré). - la commune comporte 5 monuments et si- Certaines de ces mesures permettent d’oc- tes classés Monument Historique troyer des primes pour la rénovation et l’em- imposte - 115 biens sont repris à l’inventaire du Pa- Cerfontaine bellissement extérieur d’immeubles d’habi- trimoine Monumental de la Belgique et se tation. répartissent dans les différents villages de Daussois deux ouvrants Toutes ces mesures sont reprises dans le l’entité Senzeilles Code Wallon de l’Aménagement du Ter- Le châssis est un élément secondaire important pour le bon équilibre de ritoire, de l’Urbanisme et du Patrimoine Silenrieux la façade. Les fenêtres à imposte fixe et comportant deux ouvrants, ap- (CWATUP). Soumoy pelés généralement châssis en T, sont les plus fréquentes dans l’habitat traditionnel et les mieux adaptées. N’hésitez pas à consulter le service urba- Villers-deux-Eglises nisme de votre commune si vous désirez en savoir plus sur ces prescriptions La porte de grange est l’ouverture principale et le témoin de l’ancien- ne fonction agricole. La forme de la porte de grange peut varier selon En savoir plus la date de construction où la région où elle se trouve. Différentes brochures de découverte, de sensibilisation et de conseil en aménagement du territoire, urbanisme et patrimoine sont disponibles au sein des services et associations Linteau droit Linteau droit Cintré en retrait avec auvent en bois actives sur le territoire.
    [Show full text]
  • Trip Description Loop Bike Tour in the Heart of the Ardennes and Meuse
    Trip description Loop bike tour in the heart of the Ardennes and Meuse river You will have so much to explore in this undisclosed region of Belgium by bike: ride through the Ardennes and its green countryside, discover the provincial folklore and picturesque villages and relax along the banks of the majestic Meuse river. What a pleasant way of living the Belgian dream! Destination Europe Location Belgique Duration 5 days Difficulty Level Easy Validity from March to November Minimum age 12 years old Reference WA0501 Type of stay loop trip Itinerary Leave your problems behind as suggests a famous Belgian proverb and be part of this fabulous bike trip in the great outdoors of both the Ardennes and along the Meuse river. Naturally you will be amazed by the renowned Belgian good mood! Your trip begins in Dinant, the city where Adolphe Sax, the inventor of the musical instrument, was born. Enjoy the most charming places of the Ardennes such as Rochefort, Marche-en-Famenne or Durbuy and cross picturesque landscapes. You ride sometimes on small countryside roads, on large cycle paths or along the Meuse river between Huy and Dinant passing by Namur, the capital of Wallonia. All the ingredients are combined in this loop bike tour to enjoy a great adventure! Eager for culture? Explore the citadels of Namur and Dinant, the castel of Modave or the fort of Huy. Keen to relax in the nature? The natural area of Leffe and Famenne regions or the peaceful banks of the Meuse river await you! Not to mention the Belgian gastronomy with its French fries, its waffles, its chocolate or all types of beers: all your senses will be awake! Day 1 Dinant - Rochefort Get onto your bike for a perfect adventure! Dinant is your starting point and you will find plenty of activities to enjoy there.
    [Show full text]
  • Evaluation of Belgian Clays for Manufacturing Compressed Earth Blocks Lavie A
    GEOLOGICA BELGICA (2019) 22/3-4: 139-148 Evaluation of Belgian clays for manufacturing compressed earth blocks Lavie A. MANGO-ITULAMYA1*, Frédéric COLLIN2, Pascal PILATE3, Fabienne COURTEJOIE4 & Nathalie FAGEL1. 1Argiles, Géochimie et Environnement sédimentaires, University of Liège, Quartier Agora, 14 allée du 6 août, 4000 Liège, Belgium. 2Géotechnique, University of Liège, Quartier Polytech, 4000 Liège, Belgium. 3Belgian Ceramic Research Centre, 4 Av. du Gouverneur E. Cornez, 7000 Mons, Belgium. 4Architecture, University of Liège, 41 Boulevard de la Constitution, 4020 Liège, Belgium. * corresponding author: [email protected]. ABSTRACT. This study aims to characterize Belgian clays in order to evaluate their use for manufacture of compressed earth blocks (CEB). Nineteen Belgian clay deposits were sampled in 56 sites and 135 samples were collected and analyzed. The analyses focus on the determination of particle size, plasticity, nature and mineralogy as the main characteristics for assessing the suitability of the raw clays to make CEB. These analyses allow for classifying the sampled clay deposits in three categories: clays that can be used unchanged to make CEB (2 clay deposits), clays that are suitable for the manufacture of CEB but require addition of sand and gravel particles (13 clay deposits) and clays that are suitable for the manufacture of CEB if they are mixed with other raw clays (4 clay deposits). In order to verify the use of these clays, five of them served as a model for making CEB. The strength of these bricks was evaluated by testing for compressive strength and abrasion resistance. The results of these tests confirm the suitability or not of the sampled clays for the manufacture of CEB.
    [Show full text]
  • Fiche Descriptive Sur Les Zones Humides Ramsar
    Fiche descriptive sur les zones humides Ramsar (FDR) Catégories approuvées dans la Recommandation 4.7modifiée par la Résolution VIII.13 de la Conférence des Parties contractantes Note aux rédacteurs: 1. La FDR doit être remplie conformément à la Note explicative et mode d’emploi pour remplir la Fiche d’information sur les zones humides Ramsar ci-jointe. Les rédacteurs sont vivement invités à lire le mode d’emploi avant de remplir la FDR. 2. La FDR remplie (et la ou les carte(s) qui l’accompagne(nt)) doit être remise au Bureau Ramsar. Les rédacteurs sont instamment priés de fournir une copie électronique (MS Word) de la FDR et, si possible, des copies numériques des cartes. 1. Nom et adresse du rédacteur de la FDR: USAGE INTERNE SEULEMENT Philippe Frankard et Pascal Ghiette J M A Centre de recherche de la Nature, des Forêts et du Bois c/o Station scientifique des Hautes-Fagnes Mont-Rigi Date d’inscription Numéro de référence du site B-4950 Robertville Belgique 2. Date à laquelle la FDR a été remplie ou mise à jour: 19 juin 2002 3. Pays: Belgique 4. Nom du site Ramsar: Les Hautes Fagnes 5. Carte du site incluse: a) copie imprimée (nécessaire pour inscription du site sur la Liste de Ramsar): oui π -ou- non π b) format numérique (électronique) (optionnel): oui π -ou- non π 6. Coordonnées géographiques (latitude/longitude): 50°32' N 06°06' E 7. Localisation générale: Province de Liège. Liège: chef-lieu de la province du même nom, 250.000 habitants. Distance Liège/Hautes-Fagnes: 40 km.
    [Show full text]
  • Marche-En-Famenne N° 54/7-8
    AYE MARCHE-EN-FAMENNE 54/7-8 CARTE GÉOLOGIQUE DE WALLONIE ÉCHELLE : 1/25 000 NOTICE EXPLICATIVE Plus d'infos concernant la carte géologique de Wallonie : http://geologie.wallonie.be [email protected] Un document édité par le Service public de Wallonie, Direction générale de l’Agriculture, des Ressources naturelles et de l’Environnement. Dépôt légal : D/2014/11802/76 Éditeur responsable : José Renard, Directeur général a. i., DGARNE - Avenue Prince de Liège, 15 - B-5100 Namur. Reproduction interdite. SPW | Éditions, CARTES N° vert : 0800/11 901 - Site : www.wallonie.be AYE - MARCHE-EN- FAMENNE Laurent BARCHY & Jean-Marc MARION Université de Liège Service de paléontologie animale et humaine Sart-Tilman, B 18, B-4000 Liège http://www.ulg.ac.be/paleont/ Photographie de couverture : La chapelle de Waha (1060) construite sur et avec les grès de la Formation de la Lomme. Les vitraux ont été réalisés par J.-M. Folon NOTICE EXPLICATIVE 2014 Déposée : juin 2006 Acceptée pour publication : décembre 2009 Carte Aye – Marche-en-Famenne n° 54/7-8 Résumé Située à cheval sur les provinces de Namur et de Luxembourg, la portion de territoire couverte par la carte montre des contrastes géomorphologiques importants qui permettent d’y reconnaître quatre régions géographiques : la transition Condroz-Famenne, la Famenne proprement dite, la Calestienne et le premier contrefort de l’Ardenne. Le sous-sol est constitué par des dépôts paléozoïques qui s’étagent depuis l’Emsien jusqu’au Famennien supérieur. Ces séries sédimentaires dévoniennes, divisées en formations, sont formées de roches carbonatées et siliciclastiques qui ont subi l’orogenèse varisque.
    [Show full text]
  • ROCHEFORT, V1 0 ' 8 2 ° 0 5 Rochefort - BELGIUM Flood - Situation As of 17/07/2021 0 0
    640000 650000 660000 670000 680000 690000 700000 5°2'0"E 5°9'0"E 5°16'0"E 5°23'0"E 5°30'0"E 5°37'0"E 5°44'0"E GLIDE number: N/A Activation ID: EMSR518 N " Int. Charter Act. ID: N/A Product N.: 02ROCHEFORT, v1 0 ' 8 2 ° 0 5 Rochefort - BELGIUM Flood - Situation as of 17/07/2021 0 0 0 0 Delineation MONIT01 - Overview map 01 0 0 0 0 9 9 5 5 5 5 Noord-Brabant Arnsberg Limburg Dusseldorf Prov. (NL) Antwerpen Prov. Limburg Prov. Netherlands Vlaams-Brabant (BE) KoNolrtnh Sea Prov. 01 Belgium R Brabant h in Wallon e , Germany ^ W Brussels a e al Meus Prov. Liege m, Lahn France Oh Prov. Namur 02 Koblenz !( e l l Rochefort e Trier o s Detail 03 M , Prov. e tt 25 lo Luxembourg Sure e km s Mo N " (BE) Luxembourg 0 ' 1 2 ° 0 5 ! Durbuy 0 0 Cartographic Information 0 0 0 0 0 0 8 8 N 5 5 " 5 5 0 ' 1:90000 Full color A1, 200 dpi resolution 1 2 ° 0 5 0 2 4 8 km Grid: WGS 1984 UTM Zone 31N map coordinate system Tick marks: WGS 84 geographical coordinate system ± Legend Crisis Information Hydrography Transportation Flooded Area River Highway (17/07/2021 17:32 UTC) Previous Flooded Area Stream Primary Road (15/07/2021 05:50 UTC) General Lake Secondary Road Information Land Subject to Long-distance railway Inundation Area of Interest Reservoir Tramway Detail map River Helipad Administrative Physiography, Land Use, Land boundaries Facilities Cover, Facilities area feature and Province Navigable canal Built-Up area ! ! ! ! ! ! Municipality Dam Features available in the vector package Placenames ÏÏÏ Berthing Structure 0 0 ! Placename 0 0 0 0 0 0 7 7 Consequences
    [Show full text]
  • Country Pasture/Forage Resource Profiles BELGIUM
    Country Pasture/Forage Resource Profiles BELGIUM by Alain Peeters The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views of FAO. All rights reserved. FAO encourages the reproduction and dissemination of material in this information product. Non-commercial uses will be authorized free of charge, upon request. Reproduction for resale or other commercial purposes, including educational purposes, may incur fees. Applications for permission to reproduce or disseminate FAO copyright materials, and all queries concerning rights and licences, should be addressed by e-mail to [email protected] or to the Chief, Publishing Policy and Support Branch, Office of Knowledge Exchange, Research and Extension, FAO, Viale delle Terme di Caracalla, 00153 Rome, Italy. © FAO 2010 3 CONTENTS 1. INTRODUCTION 5 Country location 5 2. SOILS AND TOPOGRAPHY 8 Topography and geology 8 Soil types 10 3. CLIMATE AND AGRO-ECOLOGICAL ZONES 11 Climate 11 Geographical regions 13 Agro-ecological regions 14 Forests 22 4.
    [Show full text]
  • Late Middle to Late Frasnian Atrypida, Pentamerida, and Terebratulida
    Disponible en ligne sur www.sciencedirect.com Geobios 41 (2008) 493–513 http://france.elsevier.com/direct/GEOBIO/ Original article Late Middle to Late Frasnian Atrypida, Pentamerida, and Terebratulida (Brachiopoda) from the Namur–Dinant Basin (Belgium) Atrypida, Pentamerida et Terebratulida (Brachiopoda) de la partie supe´rieure du Frasnien moyen et du Frasnien terminal du Bassin de Namur-Dinant (Belgique) Bernard Mottequin a,b a Department of Geology, Trinity College, Dublin 2, Ireland b Paléontologie animale, université de Liège, bâtiment B18, 4000 Liège 1, Belgium Received 18 January 2007; accepted 17 October 2007 Available online 11 March 2008 Abstract In the Namur–Dinant Basin (Belgium), the last Atrypida and Pentamerida originate from the top of the Upper Palmatolepis rhenana Zone (Late Frasnian). Within this biozone, their representatives belong to the genera Costatrypa, Desquamatia (Desquamatia), Radiatrypa, Spinatrypa (Spinatrypa), Spinatrypina (Spinatrypina?), Spinatrypina (Exatrypa), Waiotrypa, Iowatrypa and Metabolipa. No representative of these orders occurs within the Palmatolepis linguiformis Zone. The disappearance of the last pentamerids, mostly confined to reefal ecosystems, is clearly related to the end of the edification of the carbonate mounds; it precedes shortly the atrypid one. This event, resulting from a transgressive episode, which induces a progressive and dramatic deterioration of the oxygenation conditions, takes place firstly in the most distal zones of the Namur– Dinant Basin (southern border of the Dinant Synclinorium; Lower P. rhenana Zone). It is only recorded within the Upper P. rhenana Zone in the Philippeville Anticlinorium, the Vesdre area, and the northern flank of the Dinant Synclinorium. It would seem that the terebratulids were absent during the Famennian in this basin, probably due to inappropriate facies.
    [Show full text]
  • Country Overview
    Belgium Overview This document provides an overview of LIFE in Belgium. It showcases key data and some of the latest LIFE projects. You will also find contact details and other useful resources and a full list of current and recently-finished LIFE projects. Every year calls for project proposals are launched covering the LIFE programme’s priority areas. ABOUT LIFE The LIFE programme is the EU's funding instrument for the environment and climate action. It has been running since 1992 and has co-financed more than 4 500 projects across the EU and in third countries, mobilising over €9 billion and contributing more than €4 billion to the protection of the environment and climate. The budget for the LIFE programme for 2014–2020 is set at €3.4 billion in current prices, with a sub-programme for environment and a sub-programme for climate action. Types of LIFE project: Other types of LIFE funding: Traditional (Environment and Resource Efficiency; Nature NGO operating grants and Biodiversity; Environmental Governance and Natural Capital Financing Facility (NCFF) Information; Climate Change Mitigation; Climate Change Private Finance for Energy Efficiency (PF4EE) Adaptation; Climate Governance and Information). Integrated (Environment, Nature or Climate Action) NCFF and PF4EE are joint initiatives with the European Preparatory Investment Bank, which manages the two funds. Capacity-building For more information visit: http://ec.europa.eu/life Last update: 21/11/18 European Commission/EASME (http://ec.europa.eu/life/) – Page 1 – LIFE Environment and Resource Efficiency This LIFE priority area is aimed at developing, testing and demonstrating best practices, solutions and integrated approaches to environmental challenges, as well as improving the related knowledge base.
    [Show full text]