Linked to Environmental Changes in the Early Oxfordian Marine Polish Basin
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Evolution and Presence of Diurnal Predatory Birds in the Carpathian Basin
Ornis Hungarica 2018. 26(1): 102–123. DOI: 10.1515/orhu-2018-0008 Evolution and presence of diurnal predatory birds in the Carpathian Basin Jenő (Eugen) KESSLER Received: February 05, 2018 – Revised: May 03, 2018 – Accepted: May 08, 2018 Kessler, J. (E.) 2018. Evolution and presence of diurnal predatory birds (Ord. Accipitriformes, and Falconiformes) in the Carpathian Basin. – Ornis Hungarica 26(1): 102–123. DOI: 10.1515/ orhu-2018-0008 Abstract The author describes the presence of the oldest extinct diurnal birds of prey species in the world and fossilized representatives of different families, as well as the presence of recent species in the Car- pathian Basin among fossilized remains. In case of ospreys, one of the oldest known materials is classified as a new extinct species named Pandion pannonicus. The text is supplemented by a plate and a size chart. Keywords: birds of prey, evolution, Carpathian Basin, Osprey, eagles, buzzards, vultures, falcons, Pandion pan- nonicus sp.n. Összefoglalás A szerző bemutatja a nappali ragadozók kihalt fajait és a különböző családok fosszilis képviselő- it, valamint a recens fajok Kárpát-medencei jelenlétét a fosszilis maradványokban. A halászsasok között itt kerül először leírásra egy új faj is (Pandion pannonicus), amely egyben az egyik legrégebbi is az eddig ismert anyagok- ból. A szöveget egy ábra és egy mérettáblázat egészíti ki. Kulcsszavak: ragadozó madarak, evolúció, Kárpát-medence, halászsas, sas, ölyv, keselyű, sólyom, Pandion pan- nonicus sp.n. Department of Paleontology, Eötvös Loránd University, 1117 Budapest, Pázmány Péter sétány 1/c, Hungary, e-mail: [email protected] Introduction Accipitridae is the most populous family in terms of species (eagles, goshawks, kites, harri- ers and vultures belong in the group). -
Învârtita Din Luna-Turda
ÎNVÂRTITA DIN LUNA-TURDA Romanian PRONUNCIATION: eun-veur-TEE-tah deen LOO-nah-TOOR-dah (eu approximately as in "fleur-de- lis") TRANSLATION: Spinning dance from the area of the towns of Luna and Turda. SOURCE: Dick Oakes learned this dance from Sunni Bloland who learned it from Costea Constantin during Sunni's research trip to Romania in 1967-68 and introduced it to folk dancers in the United States in 1969. Sunni taught the dance at the 1970 California Kolo Festival, at the 1979 Laguna Folk Dance Festival in Laguna, California, and at the 1982 San Diego State University Folk Dance Conference. BACKGROUND: The word "învârtita" comes from the verb "învârti" meaning to whirl around or to spin. This învârtita was found in the area of the towns of Luna and Turda (near Cluj in Transylvania) by Costea Costantin, a dance researcher at the Institute of Ethnography and Folklore in Bucharest (Bucureşti). Turda is situated on the Arieş River. The Turda Gorge is a natural reserve situated about 4 miles west of Turda with marked trails for scenic hikes crossing streams and bridges. In 1918, Transylvania united with Romania, and Turda with it. In 1944, the Battle of Turda took place here, between German and Hungarian forces on one side and Soviet and Romanian forces on the other. It was the largest battle fought in Transylvania during World War II. There is evidence of human settlement in the area dating to the Middle Paleolithic, some 60,000 years ago. The Potaissa salt mines were worked in the area since prehistoric times. -
Evolution of Galliformes and Their Presence in the Carpathian Basin
Ornis Hungarica 2019. 27(2): 142–174. DOI: 10.2478/orhu-2019-0021 Evolution of Galliformes and their presence in the Carpathian Basin Jenő (Eugen) KESSLER Received: April 23, 2019 – Revised: May 13, 2019 – Accepted: May 15, 2019 Kessler, J. (E.) 2019. Evolution of Galliformes and their presence in the Carpathian Basin. – Or- nis Hungarica 27(2): 142–174. DOI: 10.2478/orhu-2019-0021 Abstract Due to the number of specimen, their size and weaker flight capabilities they are one of the favorite preys of furred and feathered carnivores. Due to this factor quite a number of skeletal fragments remained and fossilized over millions of years, especially in caves. Their presence in Europe can be traced back to the Eocene, but the majority of finds come from the Neogene and the Quaternary. In the Car- pathian Basin they are known since the beginning of the Neogene. The text is complemented with the bibliogra- phy concerning the fossilized material, one figure and six table. Keywords: Europe, Carpathian Basin, evolution, Galliformes, grouses Összefoglalás Egyedszámuk, méretük, életmódjuk, és gyengébb repülési képességük következtében kedvenc prédaállataik a tollas és szőrmés ragadozóknak. Az előbbieknek köszönhetően így elég sok vázrészük fennma- radt és fosszilizálódhatott az évmilliók folyamán, főleg a barlangi lelőhelyeken. Európai jelenlétüket már az eo- céntól követni lehet, de a leletek többsége a neogénből és a kvarterből származik. A Kárpát-medencéből a neo- gén elejétől ismertek. A szöveget kiegészíti a fosszilis anyagot felölelő irodalomjegyzék, egy ábra és hat táblázat. Kulcsszavak: Európa, Kárpát-medence, evolúció, tyúkfélék, fajdok Department of Paleontology, Eötvös Loránd University, 1117 Budapest, Pázmány Péter sétány 1/c, Hungary, e-mail: [email protected] Introduction Their dimensions vary (sexual dimorphism is a usual characteristic), they are herbivores or omnivores. -
S Romania Is Situated in South-East Europe and Has an Area of Form a Discontinuous Range Between the Danube and Someș River 237,500 Km2
Important Bird Areas in Europe – Romania ■ ROMANIA DAN MUNTEANU Dalmatian Pelican Pelecanus crispus. (PHOTO: DOMINIQUE ROBERT) GENERAL INTRODUCTION lie between the Prahova river valley to the east and the Timiș and Cerna river valleys to the west. The Western Carpathians Romania is situated in south-east Europe and has an area of form a discontinuous range between the Danube and Someș river 237,500 km2. It borders Ukraine to the north, Moldova to the north- valleys. east, Bulgaria to the south, Yugoslavia to the south-west and Lying on the northern edge of the Dobruja region, the Danube Hungary to the west. The human population in 1993 was 22,789,000. delta covers c.5,054 km2, of which 4,536 km2 are in Romania. It is Romania is divided into eight historical provinces—Maramureș, the largest European wetland after the Volga delta, and includes Crișana, Transylvania, Banat, Moldavia, Dobrogea (Dobruja), one of the most extensive reedbeds (Phragmites) in the world. Sand- Oltenia and Muntenia (the two latter were once known as dunes, large sandy beaches and several fresh or salt-water lakes are Walachia)—and 40 counties. found along the Black Sea coast. Romania’s topography is dominated by the Carpathian Forty-four Important Bird Areas (IBAs) have been identified in Mountains, and can be divided into three parts: the Eastern, Southern Romania (Table 1), covering a total area of 6,557 km2, or 3% of and Western Carpathians. The Eastern Carpathians extend from the country’s land area. The sites are not uniformly distributed the northern frontier to the Prahova river valley, reaching their (Map 1)—most are wetlands found along the Danube and other main maximum height in the Rodna mountains. -
Nummulite Biostratigraphy of the Eocene Succession in the Bahariya Depression, Egypt: Implications for Timing of Iron
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/301620370 Nummulite biostratigraphy of the Eocene succession in the Bahariya Depression, Egypt: Implications for timing of iron... Article in Journal of African Earth Sciences · April 2016 DOI: 10.1016/j.jafrearsci.2016.04.016 CITATIONS READS 0 44 1 author: Adel Mady Complutense University of Madrid 10 PUBLICATIONS 13 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Mineralogy, Petrology and Genesis of Different Types of Ferromanganese Deposits View project All content following this page was uploaded by Adel Mady on 25 April 2016. 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. Accepted Manuscript Nummulite biostratigraphy of the Eocene succession in the Bahariya Depression, Egypt: Implications for timing of iron mineralization A.M. Afify, J. Serra-Kiel, M.E. Sanz-Montero, J.P. Calvo, E.S. Sallam PII: S1464-343X(16)30132-7 DOI: 10.1016/j.jafrearsci.2016.04.016 Reference: AES 2552 To appear in: Journal of African Earth Sciences Received Date: 2 February 2016 Revised Date: 14 April 2016 Accepted Date: 19 April 2016 Please cite this article as: Afify, A.M., Serra-Kiel, J., Sanz-Montero, M.E., Calvo, J.P., Sallam, E.S., Nummulite biostratigraphy of the Eocene succession in the Bahariya Depression, Egypt: Implications for timing of iron mineralization, Journal of African Earth Sciences (2016), doi: 10.1016/ j.jafrearsci.2016.04.016. -
Grasslands of the Arieş Valley and the Comana Natural Park, Romania a Stapledon Travelling Fellowship Report
July 2018 Grasslands of the Arieş Valley and the Comana Natural Park, Romania A Stapledon Travelling Fellowship Report O.L. Pescott ([email protected]), CEH Wallingford, UK July 2018 Acknowledgements I am deeply indebted to the Stapledon Memorial Trust for making this incredible trip possible; thank you in particular to Mike Steele, Trust Secretary, for advice and support during the application process. Thank you also to Richard Pywell for suggesting that I might apply in the first place. The trip would not have been possible without the support, advice, and botanical expertise of Owen Mountford and Mari Onete (Romanian Institute of Biology), and they both receive my heartfelt thanks and appreciation. Thank you also to Valentin Grigore, Andra Nuță, and other rangers of the Comana Natural Park for making us very welcome, and for introducing us to many fascinating and beautiful sites in the area. Finally, thank you to my Stapledon co-fundee Jodey Peyton, for much pre- trip coordination, and for being a wonderful travelling companion and co-appreciator of Romania’s spectacular natural diversity. Contents Acknowledgements ................................................................................................................................. 2 Overview ................................................................................................................................................. 3 Day 1 – An introduction to Comana Natural Park .................................................................................. 3 Day 2 -
Fish Communities of the Small Rivers of Turda and Tureni Gorges Aurel
STUDIA UNIVERSITATIS BABEŞ-BOLYAI BIOLOGIA, LXI, 2, 2016 (p. 69-80) Fish communities of the small rivers of Turda and Tureni Gorges Aurel Năstase1, and Katarina Tošić2 SUMMARY. In 2014 the fish fauna of watercourses from the following two Natura 2000 SCIs were investigated: Tureni Gorge (ROSCI0034) and Turda Gorge (ROSCI0035). The research focused on fish species of community interest (Habitats Directive, Annex II), their position in the ichthyocoenose (numerical abundance, biomass, ecological significance and IBI). Ten fish species were captured in the investigated SCI Rivers, half of them being fish species of community interest present in Annex II of the Habitats Directive. Keywords: abundance, biomass, fish ecological parameters Introduction The Tureni Gorge (ROSCI0034) includes a small SCI area with a total surface of 134 ha, out of which aquatic surfaces represent less than 1%. The area has a small number of habitats (according to standard Natura 2000 Form), crisscrossed by the small Valea Racilor River. The Tureni Gorge protected area is the result of karst phenomena manifested in Jurassic limestone (tithonic) located at the contact of the Trascău Mountains with the Turda-Alba Iulia Depression (part of the Transylvanian Basin). The appearance of the area is that of a karst canyon, V-shaped, with limestone walls rising between 20 meters (in Tureni quarry right at the entrance to the gorge) and 105 meters high within the gorge. The distance between the walls increases in the second half of the gorge, reaching 160 meters at the exit towards the Copăceni locality. The length of the watercourse of the Valea Racilor River is 1850 meters. -
Politica De Vecinătate, Vector De Bază
GeoJournal of Tourism and Geosites Year VIII, no. 2, vol. 16, November 2015, p.198-205 ISSN 2065-0817, E-ISSN 2065-1198 Article no. 16107-191 THE IMPORTANCE OF ADDRESSING ANTHROPOGENIC THREATS IN THE ASSESSMENT OF KARST GEOSITES IN THE APUSENI MOUNTAINS (ROMANIA) Gabriela COCEAN* Babeş-Bolyai University, Faculty of Geography, 5-7 Clinicilor Street, Cluj-Napoca, Romania; Romanian Academy, Cluj-Napoca Branch, Geography Department, 42 Treboniu Laurian Street, Cluj-Napoca, Romania, e-mail: [email protected] Abstract: Geosites’ vulnerability and the anthropogenic threats within their perimeters are issues that arise in most of the established methods of assessment and inventory of geosites. This fact is due to the high vulnerability to anthropic pressure of some geosites, karst geosites in particular, that can be easily altered or even destroyed. Their primal, geomorphologic value is most threatened by industrial activities such as the exploitation of carbonate rocks which has had pronounced effects on some of the geosites in the Apuseni Mountains. The brutal interventions of such activities have caused changes in the physiognomy of the affected areas, considerably lowering the value of some geosites, mainly gorges which have been the main target of quarrying. Other human activities such as pastoral practices and forestry impact on the additional values of geosites (ecologic, aesthetic, geotourist etc.), thus they must also be considered in any geosite assessment. The sometimes random development of infrastructures and the damaged older constructions often lower the aesthetic value of geosites. Some tourist forms represent a perturbing factor for geosites of higher vulnerability (speleosites in particular) and also generate tourist pollution which, alongside the dumping of domestic waste represents a risk factor for karst groundwater. -
Contribution to the Pseudoscorpion Fauna of Transylvania and the Eastern and Southern Carpathians, Romania (Arachnida: Pseudoscorpiones)
NORTH-WESTERN JOURNAL OF ZOOLOGY 15 (2): 127-134 ©NWJZ, Oradea, Romania, 2019 Article No.: e181302 http://biozoojournals.ro/nwjz/index.html Contribution to the pseudoscorpion fauna of Transylvania and the Eastern and Southern Carpathians, Romania (Arachnida: Pseudoscorpiones) János NOVÁK1*, Daniel JABLONSKI2 and Jana CHRISTOPHORYOVÁ2 1. Department of Systematic Zoology and Ecology, Eötvös Loránd University, Pázmány Pétersétány 1/C, H-1117 Budapest, Hungary. 2. Department of Zoology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, Ilkovičova 6, SK–842 15 Bratislava, Slovakia. *Corresponding author, J. Novák, E-mail: [email protected] Received: 03. February 2017 / Accepted: 12. November 2018 / Available online: 19. November 2018 / Printed: December 2019 Abstract. New records for the pseudoscorpion fauna of Transylvania and the Eastern and Southern Carpathians (Romania) are presented, based on material in the Hungarian Natural History Museum (HNHM) and the Bakony Museum of the HNHM, along with material collected by the authors. Eighteen species of five families are recorded; one of the species, Chthonius carinthiacus Beier, 1951, is new for the fauna of Romania. New data concerning the recently described Neobisium tothi Novák, 2017 are presented. The number of pseudoscorpion species recorded for Romania is raised to 77. Neobisium blothroides (Tömösváry, 1882) is removed from the fauna of Croatia. Keywords: Carpathians, new records, pseudoscorpions, Romania, Transylvania. Introduction ern Carpathians (Dumitresco & Orghidan 1969), with D. bal- canicus (Redikorzev, 1929). Gardini (2014) synonymised two Romania covers a great variety of geographical areas and species, Chthonius diophthalmus Daday, 1889, described from natural habitats, from the coasts of the Black Sea across the ‘Mehádia’ (southern Carpathians) (Daday 1889a), and C. -
Redalyc.An Inventory of the Marine and Transitional Middle/Upper Eocene Deposits of the Southeastern Pyrenean Foreland Basin (
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Serra Kiel, J.; Mató, E.; Travé, A.; Ferrández Cañadell, C.; Busquets, P.; Samsó, J. M.; Tosquella, J.; Barnolas, A.; Álvarez Pérez, G.; Franqués, J.; Romero, J. An inventory of the marine and transitional Middle/Upper Eocene deposits of the Southeastern Pyrenean Foreland Basin (NE Spain) Geologica Acta: an international earth science journal, vol. 1, núm. 2, 2003, pp. 201-229 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50520109 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.1, Nº2, 2003, 201-229 Available online at www.geologica-acta.com An inventory of the marine and transitional Middle/Upper Eocene deposits of the Southeastern Pyrenean Foreland Basin (NE Spain) J. SERRA-KIEL 1 E. MATÓ 3 E. SAULA 3 A. TRAVÉ 2 C. FERRÀNDEZ-CAÑADELL 1 P. BUSQUETS 1 J.M. SAMSÓ 4 J. TOSQUELLA 5 A. BARNOLAS 1 G. ÀLVAREZ-PÉREZ 1 J. FRANQUÈS 1 and J. ROMERO 6 1 Departament d’Estratigrafia, Paleontologia i Geociències Marines. Grup de Recerca Consolidat de Geodinàmica i Anàlisi de Conques. Facultat de Geologia. Universitat de Barcelona. Zona Universitària de Pedralbes, 08028 Barcelona 2 Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia. Universitat de Barcelona. Zona Universitària de Pedralbes, 08028 Barcelona 3 Institut Cartogràfic de Catalunya, Servei Geològic de Catalunya. -
New Nummulite (Foraminiferida) Species from the Eocene of Northern Oman
New nummulite (Foraminiferida) species from the Eocene of Northern Oman ANDREW RACEY Geochem Group Limited, Chester Street, Saltney, Chester, CH4 8RD ABSTRACT Threenew speciesofnummulites;Nummulitesminutussp.nov.,N.omanensis sp.nov. andN.schaubisp.nov., are described and illustrated from the Eocene of Northem Oman. N. omanensis sp. nov. and N. schaubi sp. nov. are shown to range from Early to Middle Lutetian whilstn]. minutus sp. nov. ranges from Late Ypresian to Early Lutetian. N. minutiis sp. nov. is far smaller in all major dimensions than any species of Nummulites previously described and if found in isolation would be assumed to be very primitive and probably dated as Late Palaeocene. However, N.minutus sp. nov. was found in association with an unreworked Lutetian fauna. The commonly held belief that proloculus size and test size are smallest in the most primitive (i.e. oldest) species must therefore be treated with some degree of caution. J. Micropalaeontol., 11 (2), 189-195, December 1992. INTRODUCTION During a detailed study of the nummulitid fauna of Northern Oman some sixty-six species of nummulitid, including 38 loo krn belonging to Nummulites, were identified, described and L illustrated (Racey 1988, Racey, in press). Of these, three are new and constitute the basis of this paper. All three species Ivere found in Early Lutetian shallow marine, ramp limestones \ IRAN of the Seeb Limestone Formation (formerlycalled the Dammam Formation, a term widely used throughout the Arabian Peninsula) at Wadi Rusayl in Northern Oman (Fig. 1).One of the species, N.minutus sp. nov. was also found in the southern foothillsatWadiBaniKhalid (Fig.1). -
Ghid Sintentic De Monitorizare Pentru
Instrumente Structurale UNIUNEA EUROPEANĂ GUVERNUL ROMÂNIEI 2007 - 2013 Investimî n mediu. Credem în viitor! Institutul de Biologia București - Academia Română Splaiul Independenței nr. 296, sector 6, București - 060031 Institut coordonator al proiectului Monitorizarea stării de conservare a speciilor şi habitatelor din România în baza articolului 17 din Directiva Habitate, finanţat în cadrul Programului Operaţional Sectorial” Mediu” şi co-finanţat din Fondul European de Dezvoltare Regională. Institutul Național de Cercetare-Dezvoltare pentru Protecția Mediului subunitatea Institutul Național de Cercetare-Dezvoltare ”Delta Dunării” str. Babadag nr. 165, Tulcea 820112, jud. Tulcea, România Lider al proiectului Servicii pentru monitorizarea stării de conservare a speciilor de reptile și amfibieni din România (contract nr. 2326/IBB/26.06.2012). Societatea Română de Herpetologie str. Clinicilor nr. 5 – 9, Cluj Napoca 400006, jud. Cluj Asociatî n proiectul Servicii pentru monitorizarea stării de conservare a speciilor de reptile și amfibieni din România (contract nr. 2326/IBB/26.06.2012). Török (Zs.), Ghira (I.(, Sas (I.), Zamfirescu (Șt.), 2013 – Ghid sintetic de monitorizare a speciilor comunitare de reptile și amfibieni din România. Editura Centrul de Informare Tehnologică Delta Dunării, Tulcea, România ISBN 978-973-88117-6-8 DOI: 10.7427/DDI.B.01.2013 Ghid sintetic de monitorizare a speciilor comunitare de reptile și amfibieni din România TÖRÖK Zsolt GHIRA Ioan SAS István ZAMFIRESCU Ștefan Editura Centrul de Informare Tehnologică ”Delta Dunării” Tulcea 2013 Publicație realizată în cadrul proiectului Monitorizarea stării de conservare a speciilor şi habitatelor din România în baza articolului 17 din Directiva Habitate, finanţat în cadrul Programului Operaţional Sectorial ”Mediu” şi co-finanţat din Fondul European de Dezvoltare Regională.