Klap2011 1-2.Indb

Total Page:16

File Type:pdf, Size:1020Kb

Klap2011 1-2.Indb P��lishe� M�y 5 2011 Klapalekiana, 47: 21–28, 2011 ISSN 1210-6100 Zabrus (Pelor) skoupyi sp. nov. (Coleoptera: Carabidae) from Greece Zabrus (Pelor) skoupyi sp. nov. (Coleoptera: Carabidae) z Řecka Jiří� �� ��J��� Wolkerova ���11��8, ��-����������8 01 Kra�li�e, ��e� �ep��li� e-�������ail: a�ara�voln����y.cz Taxonomy, Coleoptera, Carabidae, �abrini,abrini, Zabrus, new species, distribution, Palaearctic region Abstract. Zabrus (Pelor) skoupyi sp. nov. from northwestern Greece is �escri�e� ��re� ��������n� comp���������re� with rel�te� B�lk�n species of the s���en�s Pelor Bonelli, 1810� Te new �pe�ie� live� in te �ra��o�o� �ro�ro� �o�ntain�ntain� in te alpine �eadow� at an altit�de of 2000–2200 � a���l� Zabrus (P.) albanicus �pfel�eck 1904 s. l�t. is recor�e� a� new for �ree�e� New data on te di�tri��tion of Z. (P.) aetolus S�a��, 186� �� lat�, Z. (P.) brevicollis S�a��, 18�� and Z. (P.) peristericus �pfel�eck 1901 �are����������� pre�ented�.� INT��DU�TI�N �i�ht t�x� (species or subspecies) of the subgen�s Pelor Bonelli 1810 of the �en�s Zabrus Cl�irville 1806 �re known from continent�l northwestern Greece (Fre��e 1989): Z. aetolus matejkai M�ř�n 1940 (Vermion Oros Mo�nt�ins); Z. aetolus purkynei M�ř�n 1940 (type loc�lity in Mo�nt ��jm�kč�l�n on the �or�er �etween Greece �n� the Rep��lic of M�ce�o- nia) Z. brevicollis S�a��, 18�� (nortwe�tern and �entral �ree�e) Z. ganglbaueri gan� glbaueri �pfel�eck 1906 (�l��ni� �n� northwestern Greece); Z. graecus subtilis S�a��, 1862 (nortwe�tern and �entral �ree�e) Z. incrassatus (�hrens 1814) (B�lk�n Penins�l�); Z. peristericus �pfel�eck 1901 (����������������kmos Oros Mo�nt�ins);ins); �andn� Z. spinipes insignis �� �ül- ler 1932 (Greece). �n ���ition�l species of the s���en�s Pelor fro� te �entioned area i� �escri�e� �elow. �lso �nother species of this s���en�s is recor�e� from Greece for the rst ti�e in ti� paper� M�T�RI�� �ND M�T�ODS The specimens of new species �re �eposite� in the followin� collections: coll. G. D����lt S�vi�ny-s�r-Or�e Fr�nce; coll. J. �ejk�l �r�slice Czech Republic; coll. P. �r�ša, Saarlo�is Germ�ny; coll. �. Orsz�lik Frý�ek-Mí�stek Czech Rep��lic; coll. V. Sko�pý Žilin� Czech Rep��lic; coll. P. Štěpánek �l��no Czech Rep��lic. Me�s�rements were m��e with � MBS–10 stereo microscope �t m��nic�tions of 8× to 56×. Me�s�rements of �o�y p�rts �n� �o�y r�tios �se� in the text were t�ken �s follows: tot�l len�th = len�th me�s�re� from �nterior m�r�in of l��r�m to elytron �pex; len�th of me�i�n lo�e (penis) = len�th of me�i�n lo�e in �ors�l view; wi�th of me�i�n lo�e (penis) = m�xim�l wi�th of me�i�n lo�e in �ors�l view; r�tio of wi�th/len�th of pronot�m = r�tio of m�xim�l wi�th of pronot�m/len�th of pronot�m me�s�re� �lon� mi�-line; r�tio of �nterior m�r�in/posterior m�r�in of pronot�m = r�tio of wi�th of pronot�m �etween �nterior �n�les/wi�th of pronot�m �etween posterior �n�les; r�tio of len�th/wi�th of elytr� = r�tio of len�th of lon�er elytron me�s�re� from ��s�l �or�er to �pex/m�xim�l wi�th of �oth elytr� com�ine�; r�tio of len�th/wi�th of �pex of me�i�n lo�e (�pex of penis) = r�tio of len�th of �pex me�s�re� from �pic�l �or�er of intern�l s�c to tip of me�i�n lo�e/m�xim�l wi�th of �pex in �ors�l view. 21 T�XONOMIC P�RT Zabrus (Pelor) skoupyi sp. nov. (Fi�s 1–5 10 11) Type material. �olotype: ♂ labelle� “Gr. M�ce�. �etomilits� – Gr�mos mts. 23.6.2004 �lpin Sko�pý le�.” collecte� in northwestern Greece �t the �or�er �etween �pir�s �n� West M�ce�oni� peripheries Gr�mmos Oros Mo�nt�ins north of �etomilitsa, �lpine meadows �n�er stone ne�r snow-eld, c�. 2100 m �.s.l. (Fi�. 1 �n� V. Sko�pý pers. comm.) c�. 40�°��20�� N 20�°����50 �E, �����������coll. V. Sko������pý. P�r���������������types: Nos 1–6 4 ♂♂, 2 ♀♀ labelle� ���“GR��EE�������C� occ. Gr���mos��� Mts. �etomilits� env. ���������29.v.2001 �����lpin �����������2000–�������������2200 m �������S. Bene�ikt������ le�.��” �����������������3 km northwest of �etomilitsa, mo�nt�in r�n�e e�stern slope �n�er stones ne�r sm�ll snow-el�s (S. Bene�ikt pers. comm.) coll. J.�� �ejk����l����������� No� 7�������–���12,����� �4 ♂♂, 2 ♀♀ s���me ��da��t� ����������s Nos 1–��6 �����������coll. V. Sko��������pý; Nos 13��–1����, 2 ♂♂, �a�e data a� No� 1���–��6, �����oll� �G.��� D��uba���lt �����No� 1�5��–��1����, 2 ♂♂, 1 ♀, la�elled “�ree�e, Ioánina, M. Gr�moz �etomilitsa, 29.5.2001 2000 m P. �r�s� le�.” coll. P. �r�š�; Nos 18–�����29 8 ♂♂, � ♀♀ s�me dat� �s holotype coll. V. Sko�pý; Nos 30���–������1, 1 ♂, 1 ♀, �a����������������e data a� olot����pe, coll. J. �ejk�l; Nos 32���–��34���, 1 ♂, 2 ♀♀ lab��elle������������� ������“�����Gr. M���ce�. ����������������etomilits� – Gr����mos ���������14.6.2006 Sko�pý le�.”” coll.����������� V. Sko�pý;������������� Nos 35���–������6, 1 ♂, 1 ♀ l��ab������������elle� ������“Gr.����� M�ce���.� �etomilits���������������� – Gr�mos��� 14.6.2006 Štěpánek le�.”” �����������������������coll. P. Štěpánek; Nos 3�7���–���������8, 1 ♂, 1 ♀ l��ab���������elle� “�����GR��EE��C� ���������or. occ. Gr�mmos mts. �etomilisa, 6.6.2008 2100 m l�t. Orsz�lik””, ������oll� �K������� �rszu�����lik� Description. Win�less species with me�i�m-size� �n� rel�tively n�rrow �o�y (Fi�. 2). Tot�l len�th 12.9��������–�������14.5 mm �������������������������������������mostly 13.1��������������������������–�������������������������13.5 mm (holotype 14.0 mm �ver�����������e 13.5 mm n = 39). Dors�l si�e ��rk �rown. ���r�m re�-�rown to ��rk �rown. Dors�l si�e shiny in m�les �n� with sli�ht l�stre to ��ll with elytr� less shiny th�n he�� �n� pronot�m in fem�les. Ventr�l si�e re�-�rown to ��rk �rown. M�n�i�les re�-�rown to ��rk �rown. �ntenn�e �n� le�s re�- �rown to �rown. M�xill�ry �n� l��i�l p�lpi p�le re�-�rown to re�-�rown. �e�� thickene� sp�rsely to �ensely �n� very nely p�nct�te (p�nct�tion visi�le in 30× magnic�tion) with eyes short �n� sli�htly (in holotype) to m�rke�ly convex. �nterior m�r�in of l��r�m with six setifero�s p�nct�res. �nterior p�rt of clype�s with �rc��te c�ll�s. Front�l f�rrows short mostly n�rrow �n� sh�llow. �ntenn�e re�chin� ��se of pronot�m when recli- ne�. �ntennomere 1 very �ro��. Ment�m with simple (i.e. not �i�) ro�n�e� (exception�lly rect�n��l�r) �n� �ro�� me�i�n tooth. Pronot�m tr�nsverse (r�tio of wi�th/len�th = 1.56–1.66–1.66 ��������������holotype 1.62) stron����������ly convex wi�est �ehin� mi��le m�rke�ly n�rrowe� tow�r� �nterior �n�les (r�tio of �nterior m�r�in/ posterior m�r�in = 0.�4–0.80–0.80 �����������holotype 0.��) l�ter����l m�r��������ins sli��������������������������htly convex (in holotype) to str�i�ht �efore posterior �n�les. �nterior m�r�in of pronot�m very sh�llowly em�r�in�te �nterior �n�les sli�htly protruding, ro�n�e�. Posterior �n�les m�rke�ly (in holotype) to sli�htly o�t�se with �pex shortly ro�n�e�. Pronot�l base sh�llowly em�r�in�te (exception�lly �lmost str�i�ht in p�r�type No 30). Inner ��s�l impression sh�llow �n� wi�e (in holotype) or ��sent. O�ter ��s�l impression ��sent. �nterior p�rt of pronot�m sp�rsely to �ensely �n� nely p�nct�te. Later�l m�r�in of pronot�m n�rrowly fl�ttene� (fl�ttenin� mo�er�tely wi�ene� posteri��) very sp�rsely �n� nely p�nct�te witho�t set�. Pronot�l ��se �ensely to sp�rsely (in holotype) �n� nely to co�rsely p�nct�te. Later�l �ead of pronot�m n�rrow not thickene�. �piple�ron of pronot�m smooth (mostly) or very sp�rsely �n� nely p�nct�te. �lytr� rel�tively n�rrow (wi�th = 5.3�������–������6.3 mm ����������������holotype 6.0 mm) ��������n� elon�������te (r�������tio of len�th/wi�th = 1.48–1.5–1.5� ��������������holotype 1.53) ����������very stron����������ly convex �������������������eclivity of elytr� �efore 22 Fi�. 1. M�p of Greece in�ic�tin� loc�lity of Zabrus skoupyi �p� nov� O�r. 1. M�p� Řeck� s vyzn�čeno� lok�lito� Zabrus skoupyi �p� nov� �pex steep to �lmost vertic�l in l�ter�l view. Interv�ls sli�htly convex (in holotype) or fl�t. Stri�e �istinct mo�er�tely �eepened, very nely (in holotype) to nely p�nct�te.
Recommended publications
  • Greek Tourism 2009 the National Herald, September 26, 2009
    The National Herald a b September 26, 2009 www.thenationalherald.com 2 GREEK TOURISM 2009 THE NATIONAL HERALD, SEPTEMBER 26, 2009 RELIGIOUS TOURISM Discover The Other Face of Greece God. In the early 11th century the spring, a little way beyond, were Agios Nikolaos of Philanthropenoi. first anachorites living in the caves considered to be his sacred fount It is situated on the island of Lake in Meteora wanted to find a place (hagiasma). Pamvotis in Ioannina. It was found- to pray, to communicate with God Thessalonica: The city was ed at the end of the 13th c by the and devote to him. In the 14th cen- founded by Cassander in 315 B.C. Philanthropenoi, a noble Constan- tury, Athanassios the Meteorite and named after his wife, Thessa- tinople family. The church's fres- founded the Great Meteora. Since lonike, sister of Alexander the coes dated to the 16th c. are excel- then, and for more than 600 years, Great. Paul the Apostle reached the lent samples of post-Byzantine hundreds of monks and thousands city in autumn of 49 A.D. painting. Visitors should not miss in of believers have travelled to this Splendid Early Christian and the northern outer narthex the fa- holy site in order to pray. Byzantine Temples of very impor- mous fresco depicting the great The monks faced enormous tant historical value, such as the Greek philosophers and symboliz- problems due to the 400 meter Acheiropoietos (5th century A.D.) ing the union between the ancient height of the Holy Rocks. They built and the Church of the Holy Wisdom Greek spirit and Christianity.
    [Show full text]
  • Karyotaxonomy of Myosotis Alpestris Group
    Preslia 78: 345–352, 2006 345 Karyotaxonomy of Myosotis alpestris group Chromozomové počty a taxonomické poznámky k zástupcům skupiny Myosotis alpestris Jitka Š t ě p á n k o v á Institute of Botany, Academy of Sciences of the Czech Republic, CZ-252 43 Průhonice, e-mail: [email protected] Štěpánková J. (2006): Karyotaxonomy of Myosotis alpestris group. – Preslia 78: 345–352. Chromosome numbers of taxa belonging to the Myosotis alpestris group are provided and/or con- firmed. A chromosome count is reported for the first time for M. olympica. A new ploidy level (2n = 24) was revealed within M. stenophylla for which previously only tetraploid cytotypes are reported. Myosotis stenophylla is identified for the first time from Greece. Previous chromosome counts for M. ambigens, M. alpestris, M. atlantica, M. corsicana, M. lithospermifolia, and M. suaveolens are confirmed based on plants originating from karyologically poorly investigated parts of the distribu- tion areas of this polyploid complex. K e y w o r d s : distribution area, karyogeography, Morocco, Myosotis alpestris group, ploidy level, South Europe, taxonomy, Turkey Introduction Representatives of the Myosotis alpestris group are arcto-alpine species with conspicuously scattered distribution areas. The population system of island differentiation is characteristic of this complex; suitable habitats are relatively small but scattered over a large region. Thus, a typical variation pattern develops as a result of limited gene flow, selection pressure of the environment and genetic drift. Along with morphological variation, extensive variability in ploidy level is found in this group. Several factors acting interactively must be invoked to ex- plain the considerably complicated pattern of variability within the M.
    [Show full text]
  • Northern Pindos the INSTITUTION of PROTECTED AREAS
    MANAGEMENT AGENCY OF VIKOS – AOOS AND PINDOS NATIONAL PARKS DISCOVERING Northern Pindos THE INSTITUTION OF PROTECTED AREAS The «introduction» of protected areas in Greece seems to go way back in history. In ancient Greece many forests were connected with religion and were considered «sacred forests» so they were strictly protected and left to evolve naturally over the centuries. The world‘ s first national park was established in 1872 in Yellowstone, USA. In Europe the protected areas created were less extensive and in their regions human populated areas and several human activities were included. The first protected areas in Greece were the Mount Olympus National Forest and the Parnassos National Forest, both founded in 1938. Aoos gorge 3 The areas of the Pan-European Network of protected areas «NATURA 2000» THE NORTHERN PINDOS NATIONAL PARK belonging to the National Park are the following: AND ITS SPECIAL ECOLOGICAL VALUE NAME DESIGNATION CODE AREA The Northern Pindos National Park was created in 2005 by Joint Ministerial Decision OF SITE OF SITE (ha) / Decree 23069/ Government Gazette 639D ‘(14/6/2005). It is located in northwestern Greece within the limits of Ioannina and Grevena Prefectures. It is the largest terrestrial Mount Vassilitsa SCI GR 1310001 8.012,78 National Park of Greece, with an area of 1,969,741 acres and it geographically unifies Valia Kalda and AooS Artificial SPA GR 1310002 14.660,48 the pre-existing National Forests of Pindos (Valia Kalda) and Vikos-Aoos, with their Lake in-between geographical region, which covers the entire region of Zagori, areas of Konitsa and Metsovo as well as the western part of the Grevena Prefecture.
    [Show full text]
  • Report on Species of Plants Requiring Protection in Greece and Measures for Securing Their Protection
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by I-Revues REPORT ON SPECIES OF PLANTS REQUIRING PROTECTION IN GREECE AND MEASURES FOR SECURING THEIR PROTECTION BY Const. GOULIMIS 21, rue Hippocrate Athens (Greece) This report has been divided in three parts. The first part deals with a list of species and other taxa of the Greek flora requiring protection. The second part deals with the destruction of rare plants and its causes and the third part deals with suggested remedies. PART 1. A list of species and other taxa of the Greek flora requiring protection. A list of the species and other taxa of the Greek flora which, in my opinion, require protection is annexed to this report. ln order to explain the comparatively great number of plants which appear in this list, 1 would mention that the flora of this country is one of the richest of Europe. containing about 6,000 taxa, a number consid� erably larger than that of France, Belgium and Switzerland put together, in spite of the fact that the total expanse of these countries is more than six times that of Greece. ln addition, as mentioned below, this country has a very large number of endemics, in fact, in proportion to her size, Greece has more endemics than any other European country. For the compilation of this list, 1 have reviewed the flora of the following districts of Greece : l. Continental Greece ( Sterea He lias). 2. Peloponnese. 3. Thessaly. 4. Epirus. 5. The island of Euboea (including the Sporades islands).
    [Show full text]
  • Commission Implementing Decision of 16 November 2012 Adopting A
    26.1.2013 EN Official Journal of the European Union L 24/647 COMMISSION IMPLEMENTING DECISION of 16 November 2012 adopting a sixth updated list of sites of Community importance for the Mediterranean biogeographical region (notified under document C(2012) 8233) (2013/29/EU) THE EUROPEAN COMMISSION, (4) In the context of a dynamic adaptation of the Natura 2000 network, the lists of sites of Community importance are reviewed. An update of the list of sites Having regard to the Treaty on the Functioning of the European of Community importance for the Mediterranean biogeo­ Union, graphical region is therefore necessary. Having regard to Council Directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and (5) On the one hand, the update of the list of sites of flora ( 1), and in particular the third subparagraph of Article 4(2) Community importance for the Mediterranean biogeo­ thereof, graphical region is necessary in order to include additional sites that have been proposed since 2010 by Whereas: Member States as sites of Community importance for the Mediterranean biogeographical region within the meaning of Article 1 of Directive 92/43/EEC. For these (1) The Mediterranean biogeographical region referred to in additional sites, the obligations resulting from Articles Article 1(c)(iii) of Directive 92/43/EEC comprises the 4(4) and 6(1) of Directive 92/43/EEC should apply as Union territories of Greece, Cyprus, in accordance with soon as possible and within six years at most from the Article 1 of Protocol No 10 of the 2003 Act of Acces­ adoption of this Decision.
    [Show full text]
  • Middle Palaeolithic Chert Exploitation in the Pindus Mountains of Western Macedonia, Greece
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università degli Studi di Venezia Ca' Foscari Middle Palaeolithic chert exploitation in the Pindus Mountains of western Macedonia, Greece N. Efstratiou, P. Biagi, D. E. Angelucci & R. Nisbet The study region The Pindus chain of western Macedonia represents the second mountain range of Greece after the Olympus. The highest peak is Mt. Smolikas (2477m asl), which is followed by the Gurgulu and Bogdani, above 2200m asl (Figure 1). This mountain region is inhabited mainly by Vlachs, a romance speaking population of almost unknown origin, whose first appearance, according to literary sources, is in the seventh century AD. Their history is narrated in the seminal work by Wace and Thompson (1913), who accurately described their pastoral, transhumance activities mostly in the area surrounding one of their main villages, Samarina, along the south-eastern fringes of Mt. Gurgulu. Figure 1. Samarina: the surveyed region, from the south-east, with indication of the uppermost limits of Mousterian chert tool scatters and isolated finds (vertical bars) (photograph P. Biagi). Figure 2. Location of the study area with summary distribution of the most important Middle Palaeolithic sites (red dots). The discoveries Archaeological surveys and excavations carried out in the Samarina region since 2002, promoted by Aristotle University, Thessaloniki, have led to the discovery of hundreds of high-altitude sites (Figure 2), most of which can be Antiquity 85: http://www.antiquity.ac.uk/projgall/biagi328/ attributed to the Middle Palaeolithic, Mousterian Levalloisian culture. They are mainly distributed along the watersheds that surround Samarina, and the ridges of the Gurgulu, up to an altitude of around 2100m asl (Efstratiou et al.
    [Show full text]
  • Glaciation in Greece
    The University of Manchester Research Glaciation in Greece. A new record of cold stage environments in the mediterranean. DOI: 10.1016/B978-0-444-53447-7.00015-5 Link to publication record in Manchester Research Explorer Citation for published version (APA): Woodward, J. C., & Hughes, P. D. (2011). Glaciation in Greece. A new record of cold stage environments in the mediterranean. In Developments in Quaternary Science|Dev. Quat. Sci. (1st ed., Vol. 15, pp. 175-198). Elsevier BV. https://doi.org/10.1016/B978-0-444-53447-7.00015-5 Published in: Developments in Quaternary Science|Dev. Quat. Sci. Citing this paper Please note that where the full-text provided on Manchester Research Explorer is the Author Accepted Manuscript or Proof version this may differ from the final Published version. If citing, it is advised that you check and use the publisher's definitive version. General rights Copyright and moral rights for the publications made accessible in the Research Explorer are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Takedown policy If you believe that this document breaches copyright please refer to the University of Manchester’s Takedown Procedures [http://man.ac.uk/04Y6Bo] or contact [email protected] providing relevant details, so we can investigate your claim. Download date:03. Oct. 2021 Provided for non-commercial research and educational use only. Not for reproduction, distribution or commercial use. This chapter was originally published in the book Developments in Quaternary Science, Vol.15, published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non- commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who know you, and providing a copy to your institution’s administrator.
    [Show full text]
  • High-Elevation Inter-Site Differences in Mount Smolikas Tree-Ring Width Data
    Dendrochronologia 44 (2017) 164–173 Contents lists available at ScienceDirect Dendrochronologia journal homepage: www.elsevier.com/locate/dendro High-elevation inter-site differences in Mount Smolikas tree-ring width data MARK ⁎ Lara Klippela, , Paul J. Krusicb,c, Robert Brandesd, Claudia Hartl-Meiera, Valerie Trouete, Matthew Mekoe, Jan Espera a Department of Geography, Johannes Gutenberg University, 55099 Mainz, Germany b Department of Geography, University of Cambridge, Cambridge CB2 3EN, United Kingdom c Navarino Environmental Observatory, Messinia, Greece d Department of Geography, Friedrich-Alexander University Erlangen-Nürnberg, 91058 Erlangen, Germany e Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ 85721, USA ARTICLE INFO ABSTRACT Keywords: We present the longest high-elevation tree-ring width dataset in the Mediterranean reaching back to the 6th Pinus heldreichii century CE. The network includes 101 living and 92 relict Pinus heldreichii Christ trees from four differently Dendroclimatology exposed sites in the 2100–2200 m a.s.l. elevation range of Mt. Smolikas in the Pindus Mountains in Greece. Mediterranean climate Though the sites were all sampled within a distance of < 1 km, inter-site correlations are surprisingly low Greece (r – = 0.65–0.87), indicating site exposure might affect tree-ring formation. We here explore the con- Tree-ring width 1550 2014 sequence of exposure differences on the climate signals in an eastern Mediterranean treeline ecotone. Treeline ecotone Temporally stable growth/climate relationships reveal similar seasonal patterns among the four sites, but dif- ferences in signal strength. P. heldreichii growth at Mt. Smolikas is significantly controlled by temperature in April (r1951–2014 = 0.33–0.50) and precipitation in June-July (r1951–2014 = 0.23–0.42), which emphasizes the overall importance of an early growth onset and subsequent moisture conditions.
    [Show full text]
  • Euscorpius. 2014
    Three New Species of Euscorpius (Scorpiones: Euscorpiidae) from Greece Gioele Tropea, Victor Fet, Aristeidis Parmakelis, Panayiota Kotsakiozi & Iasmi Stathi October 2014 — No. 190 Euscorpius Occasional Publications in Scorpiology EDITOR: Victor Fet, Marshall University, ‘[email protected]’ ASSOCIATE EDITOR: Michael E. Soleglad, ‘[email protected]’ Euscorpius is the first research publication completely devoted to scorpions (Arachnida: Scorpiones). Euscorpius takes advantage of the rapidly evolving medium of quick online publication, at the same time maintaining high research standards for the burgeoning field of scorpion science (scorpiology). Euscorpius is an expedient and viable medium for the publication of serious papers in scorpiology, including (but not limited to): systematics, evolution, ecology, biogeography, and general biology of scorpions. Review papers, descriptions of new taxa, faunistic surveys, lists of museum collections, and book reviews are welcome. Derivatio Nominis The name Euscorpius Thorell, 1876 refers to the most common genus of scorpions in the Mediterranean region and southern Europe (family Euscorpiidae). Euscorpius is located at: http://www.science.marshall.edu/fet/Euscorpius (Marshall University, Huntington, West Virginia 25755-2510, USA) ICZN COMPLIANCE OF ELECTRONIC PUBLICATIONS: Electronic (“e-only”) publications are fully compliant with ICZN (International Code of Zoological Nomenclature) (i.e. for the purposes of new names and new nomenclatural acts) when properly archived and registered. All Euscorpius issues starting from No. 156 (2013) are archived in two electronic archives: Biotaxa, http://biotaxa.org/Euscorpius (ICZN-approved and ZooBank-enabled) Marshall Digital Scholar, http://mds.marshall.edu/euscorpius/. (This website also archives all Euscorpius issues previously published on CD-ROMs.) Between 2000 and 2013, ICZN did not accept online texts as "published work" (Article 9.8).
    [Show full text]
  • Commission Implementing Decision
    15.2.2021 EN Offi cial Jour nal of the European Union L 51/187 COMMISSION IMPLEMENTING DECISION (EU) 2021/159 of 21 January 2021 adopting the fourteenth update of the list of sites of Community importance for the Mediterranean biogeographical region (notified under document C(2021) 19) THE EUROPEAN COMMISSION, Having regard to the Treaty on the Functioning of the European Union, Having regard to Council Directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and flora (1), and in particular the third subparagraph of Article 4(2) thereof, Whereas: (1) The Mediterranean biogeographical region referred to in Article 1(c)(iii) of Directive 92/43/EEC comprises the Union territories of Greece, Cyprus, in accordance with Article 1 of Protocol No 10 of the 2003 Act of Accession, and Malta, parts of the Union territories of Spain, France, Italy, Portugal and Croatia, and, in accordance with Article 355(3) of the Treaty, the territory of Gibraltar, for which the United Kingdom is responsible for external relations, as specified in the biogeographical map approved on 20 April 2005 by the committee set up by Article 20 of that Directive (the ‘Habitats Committee’). (2) The initial list of sites of Community importance for the Mediterranean biogeographical region, within the meaning of Directive 92/43/EEC, was adopted by Commission Decision 2006/613/EC (2). That list was last updated by Commission Implementing Decision (EU) 2020/96 (3). (3) The sites included in the lists of Community importance for the Mediterranean biogeographical region form part of the Natura 2000 network which is an essential element of the protection of biodiversity in the Union.
    [Show full text]
  • In Praise of Greek Mountains
    JGRHARDING In Praise of Greek Mountains (Plates 33, 34) o country has captured the romantic imagination more completely N than Greece yet few are subject to greater misconceptions. In this birthplace of Jason, Odysseus, Niarchos and Onassis, the sea is omni­ present, with no part of the mainland more than fifty miles away from it. To those who know only its beaches, its coast and islands, Greece personi­ fies the quintessential Mediterranean paradise - the gift of sun and sea. Yet in reality, four-fifths of mainland Greece is mountain and the stark lime­ stone ranges that stretch out into the Aegean, like the fingers of a skeletal hand, mirror the harsher face of a country whose hard-edged character is personified in the life of its mountain peoples. This paradox is reflected in commonplace British perceptions of Greece. Although, year in and out, Greece and its islands are amongst the most popular British summer holiday venues, it also vies with Switzerland as the most mountainous country in Europe. Furthermore, unlike Switzerland, it still retains those raw, rough edges much cherished by mountain travellers. For all this, the mountains of Greece remain a blank on the map for most British climbers. In British mountaineering compendia, such as Wilfrid Noyce's magisterial WorldAtlasofMountaineering, I the mountains of Greece get no mention, while Edward Pyatt's Guinness Book ofMountains 2 confines its comments to classical mountain mythology and the monastic sanctuaries of Meteora and Athos. Why should this be and was it always thus? To Western Europe, Greece became something of a land apart after the fall of Rome and the rise of Greek Byzantium.
    [Show full text]
  • Aberystwyth University Permafrost Conditions in the Mediterranean Region Since the Last Glaciation
    Aberystwyth University Permafrost conditions in the Mediterranean region since the Last Glaciation Oliva, M.; Žebre, M.; Guglielmin, M.; Hughes, P. D.; Çiner, A.; Vieira, G.; Bodin, X.; Andrés, N.; Colucci, R. R.; García-Hernández, C.; Mora, C.; Nofre, J.; Palacios, D.; Pérez-Alberti, A.; Ribolini, A.; Ruiz-Fernández, J.; Sarkaya, M. A.; Serrano, E.; Urdea, P.; Valcárcel, M. Published in: Earth-Science Reviews DOI: 10.1016/j.earscirev.2018.06.018 Publication date: 2018 Citation for published version (APA): Oliva, M., Žebre, M., Guglielmin, M., Hughes, P. D., Çiner, A., Vieira, G., Bodin, X., Andrés, N., Colucci, R. R., García-Hernández, C., Mora, C., Nofre, J., Palacios, D., Pérez-Alberti, A., Ribolini, A., Ruiz-Fernández, J., Sarkaya, M. A., Serrano, E., Urdea, P., ... Yldrm, C. (2018). Permafrost conditions in the Mediterranean region since the Last Glaciation. Earth-Science Reviews, 185, 397-436. https://doi.org/10.1016/j.earscirev.2018.06.018 Document License CC BY-NC-ND General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim.
    [Show full text]