CARBONIFEROUS AND PERMIAN FAUNAS

Transkript

1 CARBONIFEROUS AND PERMIAN FAUNAS AND THEIR OCCURENCE IN THE LIMNIC BASINS OF THE CZECH REPUBLIC STANISLAV TAMBERG JAROSLAV ZAJÍC Museum of Eastern Bohemia Eli ãino nábfieïí Hradec Králové Czech Republic 2008

2 Carboniferous and Permian faunas and their occurence in the limnic basins of the Czech Republic Stanislav tamberg 1 Jaroslav Zajíc 2 Museum of Eastern Bohemia at Hradec Králové Eli ãino nábfieïí Hradec Králové Museum of Eastern Bohemia at Hradec Králové, Eli ãino nábfieïí 465, Hradec Králové, Czech Republic; s.stamberg@muzeumhk.cz 2 Institute of Geology, Academy of Sciences of the Czech Republic, v.v.i., Rozvojová 269, Praha 6 Lysolaje, Czech Republic; zajic@gli.cas.cz Stanislav tamberg & Jaroslav Zajíc (2008): Carboniferous and Permian faunas and their occurence in the limnic basins of the Czech Republic Published by Muzeum v chodních âech v Hradci Králové, 2008 Graphics Olga âermáková, Hradec Králové, 2008 Print H.R.G. Litomy l, 2008 ISBN

3 Contents CONTENTS Abstract Souhrn Introduction Acknowledgement Geology and Stratigraphy List of Localities and Boreholes Localities Boreholes List of Faunas Coelenterata Leuckart, 1847; Scyphozoa Götte, Annelida Lamarck, 1809; Clitellata Grube, Bivalvia Linnaeus, Gastropoda Cuvier, Tentaculitoidea Lyashenko, Merostomata Dana, Arachnida Cuvier, Branchiopoda Latreille, Ostracoda Latreille, Malacostraca Latreille, Myriapoda Latreille, 1796; Diplopoda Blainville in Gervais, Insecta Linnaeus, Chondrichthyes Huxley, Acanthodii Owen, Osteichthyes Huxley, 1880; Actinopterygii Cope, Osteichthyes Huxley, 1880; Dipnoiformes Cloutier, Osteichthyes Huxley, 1880; Crossopterygii Cope, Tetrapoda Goodrich, 1930; Amphibia Linnaeus, Reptilia Laurenti, References Index

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5 Abstract, Souhrn ABSTRACT Several limnic Permo-Carboniferous basins comprise a significant part of the geological structure of the Bohemian Massif. Paleontological research has been actively conducted in these basins for nearly two hundred years, during which time many researchers have participated in describing the several hundred species of Permo-Carboniferous fauna contained in them. More recently, many species have been the subject of redefinition due to occurrence of synonyms given by various authors, while others have been separated into different genera and species. The present article lists the localities and names as they are used at the present time, and with the present view of their stratigraphical range. This survey of the fauna of the limnic Permo-Carboniferous basins of the Bohemian Massif records the present taxonomical concepts, the revision of older material, and new findings. Furthermore, it revises the state of the type material, reviews the type material stored mainly in collections in the Czech Republic, and draws attention to some important specimens and collections of fossils suitable for further study. The list of localities contains 205 places and 104 boreholes from which specimens have been described in the literature. The list of faunas encompasses 399 species and enumerates groups of specimens that have not yet been classified. Permo-Carboniferous faunas of the limnic basins of the Czech Republic are comprised of Coelenterata (1 species), Annelida (4 species), Bivalvia (10 species), Gastropoda (2 genera), Tentaculitoidea (2 species), Merostomata (3 species), Arachnida (40 species), Branchiopoda (6 species), Ostracoda (2 species), Malacostraca (3 species), Myriapoda (35 species), Insecta (180 species), Chondrichthyes (17 species), Acanthodii ( 5 species), Actinopterygii (27 species), Dipnoi (2 species), Crossopterygii (1 species), Amphibia (47 species), and Reptilia (13 species). SOUHRN Stfiedoãeské a západoãeské svrchnopaleozoické pánve, podkrkono ská pánev, vnitrosudetská pánev, boskovická a blanická brázda jsou sladkovodní pánve tvofiící v znamnou ãást geologické stavby âeského masivu. Paleontologick v zkum v tûchto pánvích probíhá jiï témûfi dvû století a podílelo se na nûm mnoho badatelû, ktefií popsali nûkolik stovek druhû fauny. Nûkteré druhy byly pfiejmenovány, zaãlenûny do jin ch druhû, nebo naopak byly rozdûlovány na nûkolik druhû nebo rodû. V pfiedloïené práci je podán seznam lokalit pod místními geografick mi názvy tak, jak jsou pouïívány v souãasné dobû a s vyznaãením jejich stratigrafického zafiazení. Soupis fauny limnick ch permokarbonsk ch pánví âeského masivu je sestaven v souladu se souãasn m pohledem na taxonomii jednotliv ch faunistick ch skupin. V soupisu jsou zahrnuty v sledky revizí star ího materiálu i nové nálezy. Seznam fauny zahrnuje i pfiehled typového a dal ího srovnávacího materiálu, místo jeho uloïení, a je upozornûno na nûkteré v znamné soubory fauny vhodné k dal ímu studiu. Seznam lokalit obsahuje 205 lokalit a 104 vrtû, ze kter ch byla zmiàována fauna v literárních pramenech. V seznamu fauny je uveden v ãet 399 druhû a mnoïství skupin jedincû, ktefií dosud nebyli dostateãnû studováni. Permokarbonská fauna sladkovodních pánví âeské republiky obsahuje Coelenterata (1 druh), Annelida (4 druhy), Bivalvia (10 druhû), Gastropoda (2 rody), Tentaculoidea (2 druhy), Merostomata (3 druhy), Arachnida (40 druhû), Branchiopoda (6 druhû), Ostracoda (2 druhy), Malacostraca (3 druhy), Myriapoda (35 druhû), Insecta (180 druhû), Chondrichthyes (17 druhû), Acanthodii ( 5 druhû), Actinopterygii (27 druhû), Dipnoi (2 druhy), Crossopterygii (1 druh), Amphibia (47 druhû), Reptilia (13 druhû). Stanislav tamberg 1 Jaroslav Zajíc 2 Carboniferous and Permian faunas and their occurence in the limnic basins of the Czech Republic 1 Museum of Eastern Bohemia at Hradec Králové, Eli ãino nábfieïí 465, Hradec Králové, Czech Republic; s.stamberg@muzeumhk.cz 2 Institute of Geology, Academy of Sciences of the Czech Republic, v.v.i., Rozvojová 269, Praha 6 Lysolaje, Czech Republic; zajic@gli.cas.cz Key words: Permian, Carboniferous, Fauna, Bohemian Massif 5

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7 Introduction INTRODUCTION The Central and West Bohemian Late Paleozoic Basins, Krkono e Piedmont Basin, Intrasudetic Basin, Boskovice Graben, and Blanice Graben are limnic Permo-Carboniferous basins that form a significant part of the geological structure of the Bohemian Massif. Paleontological research in these basins has been actively conducted for nearly two hundred years. This ongoing research continues to provide new evidence of the geological structure and stratigraphy of these basins, and further reveals their relations to other analogous basins in Europe. Knowledge of the fauna that occurs in these Permo-Carboniferous basins has increased along with the progress in understanding their geological structure. The earliest known discoveries of faunal remains occurred in connection with the mining of coal, copper ores, and limestones. The first invertebrate specimen to be described was of the scorpion Cyclophthalmus senior from the collections of Count ternberk, which was referred to by A. Corda in the year Subsequent papers about invertebrate specimens were published by J. Krejãí and later by J. Ku ta. The first vertebrate fossil to be described from these basins was that of the actinopterygian fish Amblypterus vratislaviensis, which was described by L. Agassiz ( ). Agassiz chose the species name vratislaviensis, indicating that he obtained the specimen from the museum in Wroclaw, Poland (the Czech version of this name, Vratislav, was widely used in historical Latin documents), but the fish originates from the Lower Permian limestone from the Intrasudetic Basin, probably from the Ruprechtice locality. Further descriptions of actinopterygian fishes from the Krkono e Piedmont Basin continued to appear during the twenty years following Heckel s work. Later in the nineteenth century, new finds from the Boskovice Graben were briefly described by Makowsky (1876) and Rzehak (1881). Despite this considerable previous work, the fundamental understanding of the Permo-Carboniferous faunas began with the research of Prof. Antonín Friã. The discovery of rich faunal remains in the gas-coal at the Humboldt mine in N fiany provided most of the impetus for his work. Friã s studies led to his monumental four-volume work Fauna der Gaskohle und der Kalksteine der Permformation Böhmens. This outstanding work was issued in 15 parts from 1879 to 1901, and contains the results of his study of the faunas of the Central and West Bohemian Carboniferous Basins, Krkono e Piedmont Basin, Intrasudetic Basin, Blanice Graben and partly also the Boskovice Graben. Fritsch s work provided a new basis for studying of the Permo-Carboniferous faunas of the Bohemian Massif, and it has served as an indispensable resource for many subsequent studies by researchers from around the world even up to the present day (Augusta, Brough, Carroll, Gardiner, Milner, Petrunkevitch, Reisz, Romer, Schneider, Werneburg, Steen, Westoll, and many others). Even numerous taxons described initially by Friã remain valid, though they have been reviewed several times during the course of a hundred years. They also form the basis of the list of fauna contained in the present publication. Research on the fauna of the limnic basins of the Bohemian Massif continued during the first half of the twentieth century mainly in the Boskovice Graben. J. Augusta continued the study of amphibians described earlier by A. Makowski and A. Friã, and discovered many promising localities. The excavations of Z. pinar and J. Kukalová- Peck in the 1950s utilized and advanced Augusta s discoveries in the Boskovice Graben, as pinar further developed the study of discosauriscid amphibians, and J. Kukalová-Peck discovered several localities with an unusually rich insect fauna. These investigations continued through the second half of the twentieth century, and much research is being actively pursued at the present time. For example, J. Schneider studies insects from the Boskovice Graben and Krkono e Piedmont Basin, J. Zajíc reviews the Stephanian and Lower Permian Acanthodians, S. tamberg has opened several localities in the Krkono e Piedmont Basin and Boskovice Graben and reviews and describes actinopterygians, while J. Klembara reviews the discosauriscid amphibians of the Boskovice Graben. Many more researchers than are mentioned in the previous short introduction have participated in the description of the Permo-Carboniferous fauna of the Bohemian Massif throughout the past 170 years, during which time several hundred taxons have been described. Many of these initial taxons have been subjected to redefinition, become recognized as synonyms for others, or have been combined with others or separated into different genera and species. Furthermore, knowledge of the stratigraphy of the Permo-Carboniferous basins of the Bohemian Massif has gone through many changes and has become more exact as a result. Such progressive changes in recognizing the taxonomic range of the fauna and the stratigraphy of localities naturally created considerable, but temporary confusion. The Summary of the Permocarboniferous Fauna of the limnic basins of Bohemia and Moravia (Zajíc & tamberg 1985), published more than twenty years ago, was limited to giving a short review of the most significant localities and enumerating the taxons of the Permo- Carboniferous Fauna. We subsequently conceived the idea of preparing a new Summary in the interest of providing a more comprehensive survey of the localities and boreholes, an updated survey of the fauna with references to types and other important material, and including revisions made during the past few years. In preparing the present contribution, the authors have had the following purposes in mind: To give a list of localities with names as they are used at the present time, and with respect to the present view of their stratigraphical range. 7

8 Introduction To summarize the survey of the fauna of the limnic Permo-Carboniferous basins of the Bohemian Massif, and to record the present taxonomical conceptions, the revision of older material, and new findings. To revise the state of the type material, to review the type material that exists mainly in collections in the Czech Republic, and to draw attention to some important specimens and collection of fossils suitable for study. The present article does not discuss the fauna of the sediments of the Moravian Culm and the fauna of the paralic Upper Silesian coal Basin, which were studied by ehofi & ehofiová (1973). ACKNOWLEDGEMENT The investigation and preparation of this book was supported by the projects of Ministry of Culture DE06P04OMG003 (Actinopterygians from the Permocarboniferous of the Krkono e Piedmont Basin), RK01P03OMG032 (List of the localities and fauna of the limnic Permocarboniferous basins of Bohemia and Moravia), Institutional project Z (Earth system at the intersection of geological processes, evolution of life, climatic and anthropogenic impacts) and was connected with the IGCP 491 project (Middle Palaeozoic Vertebrate Biogeography, Palaeogeography and Climate). Parts concerning the Línû Formation and Stephanian sharks were supported by the Grant Agency of the Academy of Sciences of the Czech Republic as a part of the project IAA (Paleoecology, Paleogeography, Stratigraphy and Climatic Changes of the Upper Stephanian (Gzhelian) of the Central and Western Bohemian Basins). Special thanks of all go to the staff of the Paleontological Department of the National Museum, Prague especially to our colleagues Dr Vojtûch Turek and Dr Boris Ekrt for their effort in the searching for the types and amicable athmosphere on their laboratories. To Dr Rudolf Prokop we thank for the loan of the photos and remember on some older localities. Many colleagues in Museums and Universities helped to us with the searching for the types and gave as the advices as regards of the taxonomy of different groups of the Late Palaeozoic Faunas. We thank in this respect especially to colleagues Dr Mathias Harzhauser and Dr Ortwin Schultz (Naturhistorisches Museum, Vienna), Dr Jozef Klembara (Comenius University, Bratislava), Dr Jörg Schneider (Bergakademie Freiberg), Dr Ulf Linnemann (Museum für Mineralogie und Geologie, Dresden), Dr Andrew Milner (British Museum (Natural History)), London and to Dr Jarmila Peck. Closer to home, special appreciation goes to Dr Jaroslav Marek, Dr Jakub Prokop and Dr Martin Ko Èák (Paleontological Institute of Charles University, Prague), Dr Josef P eniãka (West Bohemian Museum in Pilsen), Dr RÛÏena Gregorová and Dr Stanislava Hrdliãková (Moravian Museum, Brno). We are appreciative to the private collectors, Mr Jifií Holub and Mr Martin Lapacík for worthwhile field information and for important specimens providing for the study. Many thanks for important information belong to our colleagues Dr Karel Martínek and Dr Stanislav Oplu til (Institute of Geology and Palaeontology, Charles University, Prague) and Dr Zbynûk imûnek (Czech Geological Survey, Prague). Finally, we extend thanks to Mrs Olga âermáková for typographical design of the paper and make up of the photos. 8

9 1. Geology and Stratigraphy 1. GEOLOGY AND STRATIGRAPHY GEOLOGY The present list of fauna and fossiliferous sites is restricted to the Carboniferous and Permian limnic basins of the Czech Republic. The mostly paralic Upper Silesian and Nûmãiãky basins do not fall within our interest. Furthermore, the faunal content of the paralic Upper Silesian Basin has already been described by ehofi & ehofiová (1973). The areas of the Carboniferous and Permian limnic basins were defined by the Working Group for Regional Geological Classification of the Bohemian Massif, first in Czech (Holub & Pe ek 1992) and subsequently published in English (Holub & Pe ek 1994). Four areas were defined (Fig. 1) by the above-mentioned Working Group at the former Czechoslovak Stratigraphic Commission (Czech version: Holub & Pe ek 1992; English version: Holub & Pe ek 1994). We slightly modify the terminology from these earlier publications, but their names for the areas, basins and outcrops are used here. The Sudetic Area (Originally referred to as Sudetic (Lugicum) Late Paleozoic) includes deposits of northeastern, northern, and eastern Bohemia lying on the crystalline basement of the West Sudetes. Its stratigraphic sequence consists of sediments and volcanic rocks of the Mississippian (Visean) to the Triassic (middle or later) age. The area is comprised of the following basins and outcrop occurrences: The Intra-Sudetic Basin (Czech side) [Vnitrosudetská pánev (ãeská ãást)] The obsolete synonyms for this area are the Inner Sudetic depression, the Lower Silesian Basin, the Lower Silesian- Czech Basin, and the Îacléfi-Waldenburg Basin. The Îacléfi-SvatoÀovice Basin is partially synonymous with it. The Hronov-Pofiíãí fault forms the southwestern border of the basin and separates it from the Krkono e Piedmont Basin. The age of the continental deposits is Visean to Triassic. The Krkono e Piedmont Basin [Podkrkono ská pánev] The obsolete synonyms for this basin include the Permian at the foot of the Krkono e Mts., the Krkono e piedmont synclinorium, the Hronov-Pofiíãí graben, the Trutnov- Náchod Depression, the Zbeãník graben, and the Rtynû basin-shaped valley. This basin is located at the foot of the Krkono e-jizerské hory crystalline complex. The eastern border is formed by the Hronov-Pofiíãí fault and the western one by the Lusatian lineament and the Rovensko dislocation. The Trutnov-Náchod Depression comprises part of the basin. The denudation occurrences on the Hofiice elevation and Zviãina accompany the basin. The age of the continental deposits in this basin is Westphalian C to Triassic. The Mnichovo Hradi tû Basin [Mnichovohradi Èská pánev] This basin is almost entirely covered by Upper Cretaceous sediments. Outcrops occur just along the Lusatian lineament as a narrow strip between Svûtlá pod Je tûdem and Malá Skála (north of Turnov). The eastern border is formed by the Lusatian lineament and the Rovensko dislocation. The Mar ovice-bezdûz and Lu tûnice elevations form the western boundary. The age of these continental deposits, which contain abundant volcanic rocks, is Westphalian D to Autunian. The âeská Kamenice Basin [âeskokamenická pánev] This entire basin is covered mostly by Upper Cretaceous sediments. It is located between the Mnichovo Hradi tû Basin and the Kru né hory Mts. Partial units occur in the Îandov and the Srbsko-Kamenice depressions, which have been incorrectly classified as separate basins. The age of sediments and volcanoclastic materials is Stephanian C and Autunian. The Orlice Basin [Orlická pánev] The obsolete synonyms for this basin are the Poorlice furrow, The Podorlice furrow, the Orlice graben, the Podorlice graben, and the Poorlice graben. This basin is situated north of the Boskovice Basin. Its southern boundary is formed by the Malonín elevation. The age of its nonfossiliferous Permian (perhaps Autunian and Saxonian) sediments have not yet been precisely determined. 9

10 1. Geology and Stratigraphy Fig the Sudetic Area: 1a the âeská Kamenice Basin, 1b the Mnichovo Hradi tû Basin, 1c the Krkono e Piedmont Basin (1c1 the occurrence near Zviãina, 1c2 the occurrence at the Hofiice elevation), 1d the Intra-Sudetic Basin (Czech part), 1e the Permian occurrences in the Orlické hory Mts., 1f the Orlice Basin, 2 - the Central and Western Bohemia Area: 2a the PlzeÀ Basin, 2b the Manûtín Basin, 2c the Radnice Basin, 2d the Îihle Basin, 2e the Kladno-Rakovník Basin, 2f the M eno-roudnice Basin, 2g the occurrence near Kravafie, 3 - the Kru né hory Mts. Area: 3a - the occurrence near Brandov, 3b the occurrences between Moldava and Teplice, 4 the Furrows Area: 4a Blanice Basin (4a1 the northern part near âesk Brod, 4a2 the central part, the occurrences near Vla im, 4a3 - the central part, the occurrences near Tábor, 4a4 the southern part near âeské Budûjovice), 4b the Boskovice Basin (4b1 the occurrence near Miroslav), 4c - the occurrences in the Îelezné hory Mts. and near Hradec Králové (4c1 the occurrence in the Îelezné hory Mts., 4c2 - the occurrence near Hradec Králové). Modified according to Holub & Pe ek (1992, 1994). 10

11 1. Geology and Stratigraphy Occurrences of Permian outcrops in the Orlické hory Mts. The denudation remnants seem to indicate an original linkage between the Orlice Basin and the Trutnov-Náchod depression. The nonfossiliferous Permian sediments are likely to be of Saxonian age. The Kru né hory Mts. Area (Originally referred to as the Late Paleozoic of the Kru né hory Mts.) is represented by small occurrences on the Czech side of the Kru né hory (Erzgebirge) Mts. The occurrence near Brandov (the obsolete synonym of which is the Brandov Basin) is linked to that near the Olbernhau Basin in Saxony. German authors have united both occurrences into the Olbernhau-Brandov Basin. Small Carboniferous outcrops occur at several localities between Moldava and Teplice. The coal-bearing sequence is associated with volcanic rocks and volcanoclastic materials of the Teplice rhyolite. The age of the sediments and volcanoclastic materials is Westphalian A-C and Permian. The Central and Western Bohemia Area (Originally referred to as the Late Paleozoic of central and western Bohemia) is separated from the Sudetic Area by the Hefimánky granitoid massif to the north and by the Mar ovice-bezdûz and Lu tûnice elevations to the northeast. The sedimentary deposits of the area are distributed among several basins, the names of which are of historical origin and have no relation to the geological structures. The basins are rimmed by small concurrent exposures to the south and west, which were earlier incorrectly considered as separate basins. Age of sediments and volcanoclastic materials is Westphalian B to Autunian. The PlzeÀ Basin [PlzeÀská pánev] This basin is situated between Plasy and Dobfiany. The age of the sediments is Westphalian B and Stephanian C. The Manûtín Basin [Manûtínská pánev] The age of the sediments is Westphalian D and Stephanian. The Radnice Basin [Radnická pánev] This basin is comprised of a series of sunken blocks in the vicinity of Radnice. The age of the sediments is Westphalian B-D. The Îihle Basin [Îihelská pánev] The age of the sediments is Westphalian B-C and Stephanian. The Kladno-Rakovník Basin [Kladensko-rakovnická pánev] The eastern boundary of this basin runs northward along the Vltava river from Kralupy nad Vltavou to Nová Ves, and then towards the northwest to âíïkovice. The central and northern parts of this basin are covered by mostly Upper Cretaceous and locally Tertiary sediments and volcanic rocks. The basin is divided into two parts: the western Rakovník part, and the eastern Kladno part. The boundary between these two parts is formed by the Bílichov elevation and its extension to north-northwest (from Ruda near Nové Stra ecí to Mnichov near Louny). The M eno-roudnice Basin [M ensko-roudnická pánev] This basin is almost entirely covered by Upper Cretaceous sediments. It is divided into two parts: the western Roudnice part, and the eastern M eno part. The boundary between these two parts runs from the north of Neratovice, along the Labe river to its confluence with the Libûchovka river, and then northwards to Zátyní (NW of Dubá). Carboniferous occurrences (denudation remnants) The numerous Carboniferous denudation remnants of Central and Western Bohemia were not originally recognized as a homogenous group due to the diverse conditions of their various locations. The main occurrences are as follows: the Kfiivce remnant, the Tûchlovice remnant, the Skapce remnant, the Merklín remnant (previously known also as the Merklín Basin), the Letkov remnant (previously known also as the Letkov Basin), the Miro ov remnant (previously known also as the Miro ov Basin), the Holoubkov remnant, the Îebrák remnant (previously known also as the Îebrák Basin), the H skov remnant (previously known also as the Lísek Basin), the Pfiílepy remnant (previously known also as the Pfiílepy Basin), and the Kravafie remnant (previously known also as the Kravafie Basin). These occurrences are not represented in Figure 1. For their geographic positions see Pe ek et al. (2001; Supplement 5). The Furrows Area (Originally referred to as the Late Paleozoic of the furrows) The use of the term furrow (brázda in Czech) is historical, in addition to which the terms graben and halfgraben were also used in reference to separate, narrow sedimentary occurrences. However, these structures are of markedly reduced sizes, and their actual nature is not yet sufficiently known. For this reason, we use the less genetic term basin when referring to them. The remaining sedimentary fills are mostly tectonically confined and are elongated to the north-northeast and southsouthwest. 11

12 1. Geology and Stratigraphy The Boskovice Basin [Boskovická brázda] (originally referred to as the Boskovice Furrow) The southern part of this basin is sometimes incorrectly referred to as the Rosice-Oslavany basin. Its northern border with the Orlice Basin is formed by the Malotín elevation in the southern vicinity of Moravská Tfiebová. An isolated outcrop occurs near Miroslav (northeast of Znojmo). The sedimentary fill is of Stephanian C and Lower Permian (Autunian to Saxonian) age. Partial segments occur (from south to north) in the Rosice-Oslavany depression, the Ti nov-kufiim elevation, and the Boskovice depression. The southernmost occurrence is situated near Zöbing in Austria. The Blanice Basin [Blanická brázda] (originally referred to as the Blanice Furrow) The Blanice Basin is comprised of isolated outcrops that occur between âesk Brod to the north and âeské Budûjovice to the south. These outcrops are exposed in a strip tending north-northeast/south-southwest. The sedimentary fill is of Stephanian C and Lower Permian (Autunian) age. The largest northern part is situated near âesk Brod and Kostelec nad âern mi lesy. The central part is formed by outcrops in the vicinity of Vla im and Tábor. The southern outcrops are situated near âeské Budûjovice. The occurrences in the Îelezné hory Mts. and those buried under Upper Cretaceous sediments in the vicinity of Hradec Králové and Pardubice have sometimes been interpreted as the Jihlava Furrow. Based on their lithology, these sediments are judged to be probably of Stephanian age. STRATIGRAPHY The latest official subdivision of the Carboniferous System is presented in Heckel & Clayton (2006). One problem presented by this new subdivision concerns the incorporation of the Lower Autunian into the Carboniferous as the equivalent of the upper part of Gzhelian, when neither the lower nor the entire Autunian has yet been defined. We therefore continue to use the traditional division for the purposes of the present contribution. The local bio- and ecostratigraphy is based on the occurrence of actinopterygian fishes and sharks (Zajíc 2000, 2004). However, amphibians (e.g. Werneburg & Schneider, 2006), insects (e.g. Schneider & Werneburg, 2006), conchostracans (e.g. Martens, 1972), and other animal groups and ichnotaxa (e.g. Lucas, 2007, Lucas & Hunt 2006) have also been used for biostratigraphic purposes. The various biostratigraphical concepts have been evaluated by Lucas, Schneider & Cassinis (2006). Two different lithostratigraphic charts are used in the Czech part of the Sudetic Area. The first of these was compiled for the Czech side of the Intra-Sudetic Basin (Fig. 2), and the second one for the Krkono e Piedmont Basin (Fig. 3). The lithostratigraphic units of the second chart are also applied to the Mnichovo Hradi tû Basin and partly to the âeská Kamenice Basin. One stratigraphic chart is used for the entire Central and Western Bohemian Area (Fig. 4). Other lithostratigraphic charts were compiled for the Boskovice (Fig. 5) and Blanice (Fig. 6) Basins. 12

13 1. Geology and Stratigraphy Fig. 2 Stratigraphic chart of the Intra-Sudetic Basin (Sudetic area, Czech part). Modified according to Zajíc (2000). 13

14 1. Geology and Stratigraphy 14 Fig. 3. Stratigraphic chart of the Krkono e Piedmont and Mnichovo Hradi tû Basins (Sudetic area). The âeská Kamenice Basin adopts the same lithostratigraphy. Modified according to Zajíc (2000, 2007).

15 Fig. 4. Stratigraphic chart of basins and occurrences of the Central and Western Bohemian Area. Modified according to Zajíc (2000). Fig. 5. Stratigraphic chart of the Boskovice Basin. The Baãov, Míchov, and Kochov Horizons probably represent one unit or stratigraphic level. Modified according to Zajíc (2005) and Zajíc & tamberg (2004). 15 Fig. 6. Stratigraphic chart of the Blanice Basin. Modified according to Martínek, Drábková, Mikulá, imûnek & Zajíc (2001) 1. Geology and Stratigraphy

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17 2. List of Localities and Boreholes 2. LIST OF LOCALITIES AND BOREHOLES The locality list is arranged alphabetically. The first row contains the name of the locality as it is used at the present time. Other relevant names, such as those used earlier (if they are known), are indicated in parenthesis. The second row contains, in brackets, the English translation of the locality name, unless it is a geographical name used on maps (for example: Ko Èálov Za hospodou = Ko Èálov Behind the tavern ). The third row contains the name of the district, and the last row the abbreviation of the basin and the stratigraphical range of the locality. All photos of the localities were made by S. tamberg unless otherwise noted. The boreholes are given in a separate list following that of the localities. Some localities with unspecified fauna (e.g. Rieger 1971) are not quoted in the list. The terminology in reference to the basins has been modified in accordance with Holub & Pe ek (1993). For further details, see the chapter entitled Geology and Stratigraphy. NOTES The Lib tát locality (= Lieb tát; Zajíc & tamberg 1986) is necessary to exclude from the list because the fossiliferous outcrops surely belong to the present Ko Èálov cadastre (no sediments of the Rudník Horizon are known from the present Lib tát cadastre). Some specimens in diverse collections are still labelled with this locality name. The Lib tát locality is also mentioned in some previous papers like Augusta (1939b), Danûk (1902), Friã (1912), Zajíc (1988), and Zajíc & tamberg (1986). The most correct name is therefore Ko Èálov, unspecified. However, these finds probably come from the vicinity of Ko Èálov railway station (formerly Lib tát railway station). The Rybnice Hrádeck creek locality is also known as Háje nad Jizerou ( tamberg 1993, 1999b) or Roprachtice (Rieger 1971) but is located in the Rybnice cadastre. The Pfiíkr HonkÛv creek locality is also known as Rybnice ( tamberg 2000). Current situation of fossiliferous localities of the Boskovice Graben is described by Ivanov (2003), localities of the Olivûtín Member of the Intrasudetic basin are described by tamberg (1999a). Skoãek (1993) stated very bed preserved and problematic remains from the Lhotice Member (Blanice Basin). He interpreted them as foraminifers, spicula of marine calcic sponges, echinoderm fragments and ostracodes. However, he noted that a redeposition from an overlying stratum can t be ruled out. ABBREVIATIONS We used following abbreviations for the list of fossiliferous outcrops and boreholes (the marks in the square brackets behind the name of basin are the same as in the Fig. 1): BLF the Blanice Basin [4a] BOF the Boskovice Basin [4b] CKB the âeská Kamenice Basin [1a] ISB the Intra-Sudetic Basin [1d] KPB the Krkono e Piedmont Basin [1c] KRB the Kladno-Rakovník Basin [2e] MHB MIB the Mnichovo Hradi tû Basin [1b] the Miro ov occurrece (earlier known as the Miro ov Basin) [east of the PlzeÀ Basin and south of the Radnice Basin] MRB the M eno-roudnice Basin [2f] PB the PlzeÀ Basin [2a] RAB the Radnice Basib [2c] The H skov denudation remnant (earlier known e. g. as the Lísek Basin) is situated west of Beroun. LOCALITIES Arnultovice Lev bfieh âisté [Arnultovice Left bank of âistá stream ] Trutnov district [KPB; Kalná H.] Arnultovice Prav bfieh âisté [Arnultovice Right bank of âistá stream ] Trutnov district [KPB; Kalná H.] Baãov Lom Na skalkách (= 3. baãovsk lom; Baãov I) [Baãov Na skalkách quarry ] Blansko district [BOF; Baãov H.] 17

18 2. List of Localities and Boreholes Fig. 7. Locality Baãov Na skalkách quarry. Exposure of the upper part of the quarry in the year Bdín Rakovník district [KRB; Kounov M.] Beãkov V choz jz od kapliãky [Beãkov An outcrop SW of the chapel ] Trutnov district [ISB;?Beãkov H.] Boskovice U Otylky Blansko district [BOF; Baãov H.] Boskovice Údolí Semíãe v poli (= Baãov III) Boskovice Semíã valley in the field Blansko district [BOF; Baãov H.] Bradlecká Lhota Les Zlatník [Bradlecká Lhota Zlatník wood ] Semily district [KPB; PlouÏnice H.] Broumov Náchod district [ISB; Ruprechtice H.] Broumov Západní okolí [Broumov West environs ] (outcrop along the road Broumov Police nad Metují) Náchod district [ISB; Jetfiichov H.; Hejtmánkovice H.] Broumov RoÏmitál (=RoÏmitál u Broumova) (the localisation RoÏmitál near Bruntál in Zajíc & tamberg 1986 is mistaken) Náchod district [ISB; ViÏÀov Horizon] Bylany u âeského Brodu Kolín district [BLF; probably Lhotce M.] âerná Hora Záfiez nedokonãené dálnice [âerná Hora Uncompleted motorway cut ] Blansko district [BOF; probably Zbonûk-Svitávka H.] âerná Hora (unidentified) Blansko district [BOF; probably Zbonûk-Svitávka H.] âeské Budûjovice âeské Budûjovice district [BLF; Lhotice M.] Bítouchov (u Veselé) (= Bitouchov, Bítouchov u Lomnice, Vitouchov unweit Lomnitz, Bituchow bei Lomnitz, Bytouchov, Vitochov) [Bítouchov (near Veselá)] Semily district [KPB; Veselá H.] âesk Brod (unidentified) Kolín district [BLF; Ch nov M.] âesk Brod JiÏní okraj obce Peklov [âesk Brod Southern periphery Peklov ] 18

19 2. List of Localities and Boreholes Kolín district [BLF; Ch nov M.] âesk Brod Skalka (= Skalka u âeského Brodu, Na Skalce) Kolín district [BLF; Ch nov M.] âistá (= Lauterwasser) Kolín district [BLF; Ch nov M.] Dolní Kalná (unspecified) (= Kalna bei Starkenbach) Trutnov district [KPB; Kalná H.] Dolní Kalná LÛmek [Dolní Kalná Little quarry ] Trutnov district [KPB; Kalná H.] Dolní Kalná Nosek Trutnov district [KPB; Kalná H.] [Hluboké Dvory Skaliãka, uncompleted motorway cut ] Brno-venkov district [BOF; Lubû H.] Horní Kalná (unspecified) (= Kalna bei Starkenbach, Oberkalná, Ober-Kalna) Trutnov district [KPB; Kalná H.] Horní Kalná Zanikl lûmek [Horní Kalná Defunct quarry ] (close to Horní Kalná-Zálesní Lhota road, about 200 m from the intersection) Trutnov district [KPB; Kalná H.] Horní Kalná V choz v lese [Horní Kalná Outcrop in the wood ] (to the north of Horní Kalná-Zálesní Lhota road, about 750 m from the intersection) Trutnov district [KPB; Kalná H.] Dolní Sytová Semily district [KPB; Rudník H.] Dolní tûpanice (= Nieder-Stepanitz) Semily district [KPB; tûpanice-âikvásky H.] Doubravãice Rokle u hájovny [Doubravãice A gulch near the gamekeeper s lodge ] Kolín district [BLF; Peklov M.] Drválovice Vûtrn ml n (= Drbálovice; Vanovice) [Drválovice Windmill ] Note: The locality contains several outcrops in the vicinity of the former windmill. Blansko district [BOF; Kochov H.] Hejtmánkovice Náchod district [ISB; Hejtmánkovice H.] Hluboké Dvory (= Hlubok u Ti nova; Hluboky bei Tischnowitz) Brno-venkov district [BOF; Lubû H.] Hluboké Dvory Skaliãka, dálnice Fig. 8. Locality Dolní Kalná Little quarry. Exposure of the quarry in the year 1998 (now takes to earth). 19

20 2. List of Localities and Boreholes Fig. 9. Locality Horní Kalná Dump of the Adam mine. Horní Kalná Odval dolu Adam [Horní Kalná Dump of the Adam mine ] Trutnov district [KPB; Kalná H.] Horní Kalná Odval dolu Eva [Horní Kalná Dump of the Eva mine ] Trutnov district [KPB; Kalná H.] Horní Kalná Za garáïí [Horní Kalná Behind the garage ] Trutnov district [KPB; Kalná H.] Horní Kalná DÛl Fortuna [Horní Kalná Fortuna mine ] Trutnov district [KPB; Kalná H.] Horní Kalná Odval dolu Vítûz [Horní Kalná Dump of the Vítûz mine ] Trutnov district [KPB; Kalná H.] Hfiedle (=Hfiedl) Rakovník district [KRB; Kounov M.] Hvûzda Kladno district [KRB; Kounov M.] Hynãice Prav bfieh Stûnavy [Hynãice Right bank of Stûnava river ] Náchod district [ISB; Ruprechtice H.] Chobot (= Chobot u Vla imi) (settlement of Nesperská Lhota) Bene ov district [BLF; Lhotice M.] Chomle u Radnic (= Chomle bei Radnitz) (Originally in former quarry close to the Malinovec pond near Chomle.) Rokycany district [RAB; Radnice Coal Seams] Chomle u Radnic DÛl Pokrok (= dûl Pokrok (závod Ovãín) u Radnic) [Chomle u Radnic Pokrok mine ] Rokycany district [RAB; Radnice Coal Seams] Chvaleã (= Qualisch bei Trautenau, Chvaleã near Trutnov) (probably dump of the Celest n Mine) Trutnov district [ISB; Radvanice Coal Seams] Chotíkov PlzeÀ-sever district [PB; Kounov M.] 20

21 2. List of Localities and Boreholes Ivanãice Panovského cihelna [Ivanãice Brickfield of Panovsk ] Brno-venkov district [BOF; Padochov F. (?)] Janov u Miro ova Rokycany district [MIB; N fiany M.] Janovice Odval dolu Franti ek [Janovice Dump of the Franti ek mine ] Trutnov district [KPB; Rudník H.] Jedomûlice Kladno district [KRB; Kounov M.] Kladno Hnidousy DÛl Ronna (= Nr. VII, dûl Gottwald III) [Kladno Hnidousy Ronna mine (= Nr. VII, Gottwald III Mine) Kladno district [KRB; Radnice Coal Seams] Kladno, Vrapice Kladno district [KRB; Radnice Coal Seams] Kladoruby Dolní pepfiík Blansko district [BOF; Zbonûk-Svitávka H. or Lubû H.] Kladoruby Horní pepfiík (=Kladeroby; Trávník Horní pepfiík ) Blansko district [BOF; Kochov H.] Klá terská Lhota (= Mönchsdorf an der Kleinen Elbe) Trutnov district [KPB; Kalná H.] Klobuky tola (= Klobuk bei Schlan, Klabuk bei Perutz) [Klobuky Adit ] (The old adit was situated above the mill on the hillside between Klobuky and âeradice.) Kladno district [KRB; Klobuky H.] Klobuky Cukrovar [Klobuky Sugar rafinery ] (Near the storage holes.) Kladno district [KRB; Klobuky H.] Klobuky LÛmek (= Klobuk bei Schlan, Klobuk bei Perutz) [Klobuky Quarry ] (The former quarry in carbonates was situated on the western margin of the village.) Kladno district [KRB; Klobuky H.] Fig. 10. Locality Klá terská Lhota. 21

22 2. List of Localities and Boreholes Klobuky Svah [Klobuky Slope ] (Above the driveway to the east of the sugar rafinery.) Kladno district [KRB; Klobuky H.] Klobuky V chod [Klobuky East ] (The slope near the road between the church and sugar rafinery.) Kladno district [KRB; Klobuky H.] KnûÏeves (= KnûÏoves) Rakovník district [KRB; M ec M.] Kocléfiov Lysé vrchy [Kocléfiov Lysé Hills ] Trutnov district [KPB;?Kalná H.] Kochov Horka (=Kochov - vrch Horka) Blansko district [BOF; Kochov H.] Kochov V potocích (= Kochov Noviãí) [Kochov In the streams ] Blansko district [BOF; Kochov H.] Kochov V lese (= Kochov L; Kochov - sever) [Kochov In the forest ] Blansko district [BOF; Kochov H.] Ko Èálov (unspecified) (= Ko tialov; Lib tát = Lieb tát) Semily district [KPB; Rudník H.] Ko Èálov Za internátem [Ko Èálov Behind the hostel ] Semily district [KPB; Rudník H.] Ko Èálov Za hospodou [Ko Èálov Behind the tavern ] Semily district [KPB; Rudník H.] Ko Èálov Odval toly Nadûje (= Vyniklá Sutice) [Ko Èálov Dump of the adit Nadûje ] Semily district [KPB; tûpanice-âikvásky H.] Ko Èálov KováfiÛv ml n [Ko Èálov Kováfi s mill ] Semily district [KPB; Rudník H.] Fig. 11. Locality Kochov In the streams. Collecting of fossils in the year

23 2. List of Localities and Boreholes Fig. 12. Locality Ko Èálov Kováfi s mill. Ko Èálov Valdice Semily district [KPB; Rudník H.] Ko Èálov U koupali tû [Ko Èálov Near open air pool ] Semily district [KPB; Rudník H.] Kounov Rakovník district [KRB; Kounov M.] Kouty toly Adolf a Glück (= Kobylík) [Kouty Adolf and Glück adits ] Semily district [KPB; tûpanice-âikvásky H.] Kozinec u Jilemnice (= Kozinec) Kozinec hill near Jilemnice (old mining dumps) Semily district [KPB; Kozinec H.] Kralupy B val kopec âervená hûrka (= Kralup) [Kralupy Former hill âervená hûrka (= Kralup) ] Mûlník district [KRB; Radnice Coal Seams] Kromle Jiãín district [KPB; PlouÏnice H.] Krouãová Halda dolu Adolf [Krouãová Dump of the Adolf mine ] Rakovník district [KRB; Kounov M.] Krsmol (= Krsmol bei Lomnitz) Jiãín district [KPB; PlouÏnice H.] Kruh 1 Semily district [KPB; Kalná H.] Kruh 2 Semily district [KPB; Kalná H.] Krupá Rakovník district [KRB; M ec M.] Kru ovice V kop pro ropovod [Kru ovice Pipeline excavation ] Rakovník district [KRB; M ec M.] Kfieãovice pod Troskami (= Kfieãowic bei Rowensko, Kfieãovice u Rovenska) Semily district [KPB; Veselá H.] 23

24 2. List of Localities and Boreholes Kundratice Doly Semily district [KPB; Rudník H.] Kyje Záfiez trati (unspecified) [Kyje Railroad cut ] Jiãín district [KPB; PlouÏnice H.] Ledce V propastech (carbonate nodules in the ravine V propastech) PlzeÀ-sever district [PB; Kounov M.] Letovice Jindfiichov Blansko district [BOF; probably Zbonûk-Svitávka H.] Lhotice Odval dolu Etna [Lhotice Dump of the Etna mine ] âeské Budûjovice district [BLF; Lhotice M.] Lhotice achta (= Lhota; Lhotic) [Lhotice Shaft ] âeské Budûjovice district [BLF; Lhotice M.] Libu ín u Kladna DÛl Schöller (= dûl Nejedl I, = dûl Nosek) [Libu ín u Kladna Schöller mine ] Kladno district [KRB; Radnice M.] Lísek u Berouna Nad ml nem Dibfií (= Lisek bei Beraun, Dibfii, Dybfií, Stradonitz) [Lísek u Berouna Above the millhouse Dibfií ] Beroun district [KRB H skov denudation remnant; Radnice Coal Seams] Lomnice nad Popelkou (okolí) [Lomnice nad Popelkou (surroundings)] (cand flag sandstone.) Semily district [KPB; Semily F. or Vrchlabí F.] Loukov ëáblûv ml n (Loukov ëábloviny ) [Loukov Devil s Mill ] Semily district [KPB; Rudník H.] Lubû (= Lubie, Luba, Lubic) Blansko district [BOF; Lubû H.] Lubná (= Lubna) Rakovník district [KRB; Lubná Coal Seams] Malá Lhota Podhájí Blansko district [BOF; probably Lubû H.] Malá Lhota Pfiíãná zmola (= Lhotka bei Raitz; Klein-Lhotta; Klein-Lhota bei Czernahora) Blansko district [BOF; probably Zbonûk-Svitávka H.] Malesice PlzeÀ-mûsto district [PB; M ec M.] Malé SvatoÀovice Tmav dûl Trutnov district [ISB; SvatoÀovice Coal Seams] Míchov Blansko district [BOF; Míchov H.] Moravsk Krumlov Údolí Rokytné (= Kromau, Krommau Za lesním závodem, Za lesním úfiadem, Behind the Forestry Office, Moravsk Krumlov II; Moravsk Krumlov Údolí Rokytné ) [Moravsk Krumlov Rokytná river valley ] Znojmo district [BOF; Padochov F.] Moravsk Krumlov Tylova ulice Krumlov I) [Moravsk Krumlov Tylova street ] Znojmo district [BOF; Padochov F.] Mutûjovice DÛl Perun II [Mutûjovice Perun II mine ] Rakovník district [KRB; Kounov M.] Nabdín Kladno district [KRB; Kounov M.] Nedvûzí tola Otto [Nedvûzí Otto adit ] Semily district [KPB; tûpanice-âikvásky H.] Nedvûzí tola Rohan [Nedvûzí Rohan adit ] (=Moravsk (= Vyniklá - Sutice) 24

25 2. List of Localities and Boreholes Semily district [KPB; tûpanice-âikvásky H.] Neslovice Rybiãková skála (= Nesslowitz; Rybiãková skála 1; Neslovice, Pod Knovízem) [Neslovice Fishrock ] Note: protected locality Brno-venkov district [BOF; íãany H.] Neslovice Rybiãková skála 2 (= údolí Neslovického potoka;) [Neslovice Fishrock 2 ] Brno-venkov district [BOF; íãany H.] NiÏbor Osada Stradonice (= Stradonitz) [NiÏbor Stradonice settlement ] (The locality was in Zajíc & tamberg 1986 confused with Stradonice u Peruce with different lithostratigraphy.) Beoun district [KRB H skov denudation remnant; Radnice M.] Nová Paka Leti tû [Nová Paka Aerodrome ] Jiãín district [KPB; PlouÏnice H.] Nová Ves nad Popelkou Pole u Îìáru u Kumburku [Nová Ves nad Popelkou Field near Îìár u Kumburku ] Semily district [KPB; PlouÏnice H.] Noviãí Blansko district [BOF; Kochov H.] N fiany Dálnice [N fiany Motorway ] PlzeÀ-sever district [PB; M ec M.] N fiany DÛl Humboldt (= Nyfian bei Pilsen) [N fiany Humboldt mine ] PlzeÀ-sever district [PB; N fiany M.] Obora (= JabloÀany; Obora I, II, III) Blansko district [BOF; probably Baãov or Kochov H.] Olivûtín (= Oelberg) Náchod district [ISB; Ruprechtice H.] Olivûtín Nad náhonem (= Oelberg) [Olivûtín Over lead ] Náchod district [ISB; Ruprechtice H.] Oslavany Lev bfieh Oslavy [Oslavany Left bank of the river Oslava ] Brno-venkov district [BOF; Rosice-Oslavany F., Zb ov H.] Fig. 13. Locality Neslovice Fishrock. Exposure of the outcrop in the year

26 2. List of Localities and Boreholes Oslavany Odval dolu Kukla (= odval dolu V. Nosek) [Oslavany Kukla mine dump ] Brno-venkov district [BOF; Rosice-Oslavany F.] Otovice âern potok [Otovice âern brook ] Náchod district [ISB; Otovice H.] Otovice Chmelnice [Otovice Hop-field ] Náchod district [ISB; Otovice H.] Otovice Vápenka [Otovice Limekiln ] Note: The locality contains several outcrops in the vicinity of the former adit ( tamberg 1999a) Náchod district [ISB; Otovice H.] Otovice (unspecified) (= Ottendorf) Náchod district [ISB; Otovice H.] Otvovice (= Votvovice, Votovice, Wotovic bei Kladno) Kladno district [KRB; Radnice Coal Seams] Ovãín Povrchov dûl [Ovãín Opencast mine ] Rokycany district [RAB; Radnice Coal Seams] Padochov V kop pro plynovod (= Padochau) [Padochov Pipeline excavation ] Brno-venkov district [BOF; Zb ov H.] Páleãek Kladno district [KRB; Klobuky H.] Panensk T nec Louny district [KRB; Klobuky H.] Peruc Údolí Débefiského potoka (=údolí strádonické pod Perucí; Tal von Stradonic bei Peruc; Stradonic bei Peruc, Stradonice u Peruce) [Peruc Valley of Débefisk brook ] Louny district [KRB; Klobuky H.] Petrovice Halda (= Petrovic, Petrovic bei Rakonitz) [Petrovice Dump ] Rakovník district [KRB; Radnice Coal Seams] Fig. 14. Locality Otovice âern brook. Exposure of the outcrop in the year

27 2. List of Localities and Boreholes PlouÏnice (unspecified) (=Plouãnice) Semily district [KPB; PlouÏnice H.] PlouÏnice Záfiez trati profil 0,0 1,3 m [PlouÏnice Railroad cut m of the section ] (see Zajíc in Blecha et al. 1997) Semily district [KPB; PlouÏnice H.] PlouÏnice Záfiez trati imûnkûv v kop ã. 1 [PlouÏnice Railroad cut imûnek s excavation No. 1 ] (see Zajíc in Blecha et al. 1997) Semily district [KPB; PlouÏnice H.] PlouÏnice Záfiez trati kilometrovník 60,5 [PlouÏnice Railroad cut milestone 60.5 ] Semily district [KPB; PlouÏnice H.] Podolí Blansko district [BOF; probably Zbonûk-Svitávka H.] Polánka (= Polanka) Znojmo district [BOF; Zb ov H.] Proseã pod Je tûdem Liberec district [MHB; Rudník H.] Prostfiední Lánov Kováfisko (=Schmidtdorf) Trutnov district [KPB; Rudník H.] Prostfiední Lánov Za továrnou [Prostfiední Lánov Behind the factory ] Trutnov district [KPB; Rudník H.] Prostfiední Lánov V chodní svah údolí Malého Labe [Prostfiední Lánov Eastern slope of Malé Labe valley ] Trutnov district [KPB; Rudník H.] Prostfiední Lánov Jz svah kopce piãka (=Prostfiední Lánov, Lánovsk kopec, Mittel Langenau, Zirmkoppe) [Prostfiední Lánov Sw slope of piãka hill ] Trutnov district [KPB; Rudník H.] Pfierubenice Rakovník district [KRB; Kounov M.] Fig. 15. Locality PlouÏnice Railroad cut milestone

28 2. List of Localities and Boreholes Pfiíãina Na brantech Rakovník district [KRB; Radnice Coal Seams] Pfiíkr HonkÛv potok [Pfiíkr HonkÛv creek ] Semily district [KPB; Rudník H.] Pfiíkr Pfiítok Honkova potoka [Pfiíkr Tributary of HonkÛv creek ] Semily district [KPB; Rudník H.] Pfiistoupim (= Pfiistoupín) (conchostracans in carbonate nodules) Kolín district [BLF; Ch nov M.] Radnice Rokycany district [RAB; Radnice Coal Saems] Radvanice DÛl Katefiina (= dûl Stachanov) [Radvanice Katefiina mine ] Trutnov district [ISB; Radvanice Coal Seam complex] Rakovník DÛl Moravia (= Rakonitz) [Rakovník Moravia mine (= Rakonitz)] (in the former Kavan pond) Rakovník district [KRB; Radnice Coal Seams] Roprachtice Dokumentaãní bod 409d [Roprachtice Documentation point 409d ] Semily district [KPB; Horní Branná H.] Rtynû v Podkrkono í, (dump of Z. Nejedl mine) Trutnov district [ISB; Prkenn DÛl-Îìárky M.] Rudník (= Hermannseifen, Herrmannsseifen, Sajfy, Hefimanovy Sejfy) (probably diverse outcrops) Trutnov district [KPB; Rudník H.] Ruprechtice (= Ruppersdorf) Náchod district [ISB; Ruprechtice H.] Ruprechtice Pod Svûtlinou Náchod district [ISB; Ruprechtice H.] Ruprechtice Vápencové lomy (= Ruppersdorf) [Ruprechtice Limestone quarries ] Náchod district [ISB; Ruprechtice H.] Rybnice Hrádeck potok [Rybnice Hrádeck creek ] (Correct locality cadastre for Háje nad Jizerou sensu tamberg (1993) and Roprachtice sensu Rieger (1971).) Semily district [KPB; Rudník H.] Rybníãek (mine dump; settlement of Bernartice) Trutnov district [ISB; Vernéfiovice H.] íãany (= íãany u Brna) Brno-venkov district [BOF; íãany H.] Sebranice Údolí Rasovna [Sebranice Rasovna valley ] Blansko district [BOF;?Zbraslavec H.] Sebranice Úboãí vrchu Podsedky (= Sasina) [Sebranice Podsedky hillside ] Blansko district [BOF;?Zbonûk-Svitávka H.] Semily (unspecified) Semily district [KPB; Rudník H.] Semily Lev bfieh Jizery [Semily Left bank of Jizera river ] Semily district [KPB; Rudník H.] Semily Rokle v Nouzovû [Semily Ravine in Nouzov ] Semily district [KPB; Rudník H.] Slan Jáma [Slan Mine ] Kladno district [KRB; N fiany M.; M ec M.] 28