Geol. Quart. 49 (3)
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Decapod Crustaceans from the Middle Jurassic Opalinus Clay of Northern Switzerland, with Comments on Crustacean Taphonomy
0012-9402/04/030381-12 Eclogae geol. Helv. 97 (2004) 381–392 DOI 10.1007/s00015-004-1137-2 Birkhäuser Verlag, Basel, 2004 Decapod crustaceans from the Middle Jurassic Opalinus Clay of northern Switzerland, with comments on crustacean taphonomy WALTER ETTER Key words: Decapoda, Peracarida, Jurassic, Switzerland, ecology, crustacean taphonomy ABSTRACT ZUSAMMENFASSUNG Four species of decapod crustaceans from the Middle Jurassic Opalinus Clay Aus dem Opalinuston (Mittlerer Jura, Aalenian) der Nordschweiz werden vier (Aalenian) of Northern Switzerland are described. Of these, Mecochirus cf. Arten von decapoden Krebsen beschrieben. Von Aeger sp., Eryma cf. bedelta eckerti is the most common one, while Eryma cf. bedelta, Glyphea sp. and und Glyphaea sp. wurden nur ganz wenige Exemplaren gefunden, während Aeger sp. were present as individuals, or only a few specimens. The preserva- Mecochirus cf. eckerti etwas häufiger ist. Die Erhaltungsbedingungen waren tion of these crustaceans ranges from moderate to excellent, reflecting the während der Ablagerung des Opalinustones günstig, was sich in einer geringen favourable taphonomic conditions of the depositional environment. An inter- Disartikulations- und Fragmentationsrate der Krebse widerspiegelt. Ein in- esting aspect of the taphocoenosis in the Opalinus Clay is that the decapod teressanter Aspekt der Taphocoenose ist die deutliche Dominanz der Klein- crustaceans are by far outnumbered by small peracarid crustaceans (isopods krebse (Peracarida: Isopoden und Tanaidaceen). Dies dürfte die Zahlenver- and tanaids). This is interpreted as reflecting the original differences in abun- hältnisse der ehemaligen Lebensgemeinschaft widerspiegeln. In den meisten dance. Yet this distribution is not frequently encountered in sedimentary se- Ablagerungen dominieren jedoch die decapoden Krebse, wogegen Peracarida quences where decapods (although rare) are far more common than isopods äusserst selten sind. -
Classification of Synoptic Conditions of Summer Floods in Polish
water Article Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains Ewa Bednorz 1,* , Dariusz Wrzesi ´nski 2 , Arkadiusz M. Tomczyk 1 and Dominika Jasik 2 1 Department of Climatology, Adam Mickiewicz University, 61-680 Pozna´n,Poland 2 Department of Hydrology and Water Management, Adam Mickiewicz University, 61-680 Pozna´n,Poland * Correspondence: [email protected]; Tel.: +48-61-829-6267 Received: 24 May 2019; Accepted: 12 July 2019; Published: 13 July 2019 Abstract: Atmospheric processes leading to extreme floods in the Polish Sudeten Mountains were described in this study. A direct impact of heavy precipitation on extremely high runoff episodes was confirmed, and an essential role of synoptic conditions in triggering abundant rainfall was proved. Synoptic conditions preceding each flood event were taken into consideration and the evolution of the pressure field as well as the moisture transport was investigated using the anomaly-based method. Maps of anomalies, constructed for the days prior to floods, enabled recognizing an early formation of negative centers of sea level pressure and also allowed distinguishing areas of positive departures of precipitable water content over Europe. Five cyclonic circulation patterns of different origin, and various extent and intensity, responsible for heavy, flood-triggering precipitation in the Sudetes, were assigned. Most rain-bringing cyclones form over the Mediterranean Sea and some of them over the Atlantic Ocean. A meridional southern transport of moisture was identified in most of the analyzed cases of floods. Recognizing the specific meteorological mechanisms of precipitation enhancement, involving evolution of pressure patterns, change in atmospheric moisture and occurrence of precipitation may contribute to a better understanding of the atmospheric forcing of floods in mountain areas and to improve predicting thereof. -
Soils of Lower Silesia [Gleby Dolnego Śląska]
GLEBY DOLNEGO ŚLĄSKA: geneza, różnorodność i ochrona SOILS OF LOWER SILESIA: origins, diversity and protection SOILS of Lower Silesia: origins, diversity and protection Monograph edited by Cezary Kabała Polish Society of Soil Science Wrocław Branch Polish Humic Substances Society Wrocław 2015 GLEBY Dolnego Śląska: geneza, różnorodność i ochrona Praca zbiorowa pod redakcją Cezarego Kabały Polskie Towarzystwo Gleboznawcze Oddział Wrocławski Polskie Towarzystwo Substancji Humusowych Wrocław 2015 Autorzy (w porządku alfabetycznym) Contributors (in alphabetic order) Jakub Bekier Andrzej Kocowicz Tomasz Bińczycki Mateusz Krupski Adam Bogacz Grzegorz Kusza Oskar Bojko Beata Łabaz Mateusz Cuske Marian Marzec Irmina Ćwieląg-Piasecka Agnieszka Medyńska-Juraszek Magdalena Dębicka Elżbieta Musztyfaga Bernard Gałka Zbigniew Perlak Leszek Gersztyn Artur Pędziwiatr Bartłomiej Glina Ewa Pora Elżbieta Jamroz Agnieszka Przybył Paweł Jezierski Stanisława Strączyńska Cezary Kabała Katarzyna Szopka Anna Karczewska Rafał Tyszka Jarosław Kaszubkiewicz Jarosław Waroszewski Dorota Kawałko Jerzy Weber Jakub Kierczak Przemysław Woźniczka Recenzenci Reviewers Tadeusz Chodak Michał Licznar Jerzy Drozd Stanisława Elżbieta Licznar Stanisław Laskowski Polskie Towarzystwo Gleboznawcze Oddział Wrocławski Polskie Towarzystwo Substancji Humusowych Redakcja: Uniwersytet Przyrodniczy we Wrocławiu Instytut Nauk o Glebie i Ochrony Środowiska 50-357 Wrocław, ul. Grunwaldzka 53 Druk i oprawa: Ultima-Druk Sp z o.o. 51-123 Wrocław, ul. W. Pola 77a ISBN 978-83-934096-4-8 Monografia -
Glubczyce Sklad B5 Ok.Indd
REGION GŁUBCZYCKO- -KRNOWSKI Hlubčicko-krnovský region Historia | Dějiny Turystyka | Turistika Gospodarka | Hospodářství Niniejsza publikacja została wsparta ze środków pomocowych Unii Euro- pejskiej. Wyrażone w niej poglądy są poglądami Wydawcy publikacji i w żadnym przypadku nie mogą być utożsamiane z ofi cjalnym stanowiskiem Unii Europejskiej Publikace byla vydána za podpory Evropské unie. Názory v ní vyjádřené jsou názory vydavatele a v žádném případě nemohou být ztotožňovány s ofi ciálním stanoviskem Evropské unie 1 GŁUBCZYCE - KRNÓW 2004 KIEROWNIK PROJEKTU | VEDOUCÍ PROJEKTU: Jadwiga Królikowska ZESPÓŁ REDAKCYJNY | REDAKČNÍ RADA: Jadwiga Królikowska - Paweł Maleńczyk - Rostislav Balner - Oldřich Mičan AUTORZY ZDJĘĆ | FOTOGRAFIE: Tomasz Michalewski Agencja Fotografi czna „Arte“ (fot. str. 41, 53-61, 63-67, 78, 88, 91, 95, 98, 100) Rostislav Balner (fot. str. 4-7, 12, 14-17, 50-51, 69-83, 85-91, 94) Ludmiła Włodkowska (fot. str. 92-93, 99) OPRACOWANIE HISTORII REGIONU GŁUBCZYCKO-KRNOWSKIEGO | ZPRACOVÁNÍ DĚJIN HLUBČICKO-KRNOVSKÉHO REGIONU: Katarzyna Maler AUTORZY PRZEKŁADU TEKSTU | PŘEKLAD na j. czeski, do češtiny: Tadeusz Kuchejda - Jarosław Radiměřský - Petr Neuman korekta: Tomáš Knopp na j. angielski, do angličtiny: Krystyna Kowalów na j. niemiecki, do němčiny: Andrzej Szypulski na j. francuski, do francouzštiny: Aneta Raik OPRACOWANIE GRAFICZNE, SKŁAD KOMPUTEROWY, KARTOGRAFICZNE OPRACO- WANIE MAP | GRAFICKÁ ÚPRAVA, POČÍTAČOVÁ SAZBA, KARTOGRAFICKÉ ZPRACOVÁNÍ MAP: Grażyna Kasprzak Drukarnia Sady - Krapkowice W publikacji wykorzystano - za zgodą Urzędu Miejskiego w Krnowie - mapę kartografi czną miasta Krnowa | V publikaci byla se souhlasem Městského úřadu v Krnově využita mapa města Krnova WYDAWCA | VYDAVATEL: Urząd Miejski w Głubczycach, ul. Niepodległości 14, 48-100 Głubczyce, tel. +48 77 485 30 21-27, fax 485 24 16, www.glubczyce.pl, www.bip.glubczyce.pl, e-mail: [email protected] DRUK |TISK: OFFSETdruk I MEDIA Spółka z o.o. -
Marine Reptiles
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Institutional Research Information System University of Turin Geobios 39 (2006) 346–354 http://france.elsevier.com/direct/GEOBIO/ Marine reptiles (Thalattosuchia) from the Early Jurassic of Lombardy (northern Italy) Rettili marini (Thalattosuchia) del Giurassico inferiore della Lombardia (Italia settentrionale) Reptiles marins (Thalattosuchia) du Jurassique inférieur de la Lombardie (Italie du nord) Massimo Delfino a,*, Cristiano Dal Sasso b a Dipartimento di Scienze della Terra, Università di Firenze, Via G. La Pira 4, 50121 Firenze, Italy b Museo Civico di Storia Naturale, Corso Venezia 55, 20121 Milano, Italy Received 24 May 2004; accepted 3 January 2005 Available online 28 February 2006 Abstract The fossil remains of two small reptiles recently discovered in the Sogno Formation (Lower Toarcian) near Cesana Brianza (Lecco Province), represent the first mesoeucrocodylians reported for Lombardy and some of the few Jurassic reptiles from Italy. Due to the absence of diagnostic skeletal elements (the skulls are lacking), it is not possible to refer the new specimens at genus level with confidence. Although the well devel- oped dermal armour would characterise Toarcian thalattosuchians of the genera Steneosaurus (Teleosauridae) and Pelagosaurus (Metriorhynch- idae), the peculiar morphology of the osteoderms allow to tentatively refer the remains to the latter taxon (cf. Pelagosaurus sp.). The small size, along with the opening of the neurocentral vertebral sutures and, possibly, the non sutured caudal pleurapophyses, indicate that the specimens were morphologically immature at death. These “marine crocodiles” confirm the affinities between the fauna of the Calcare di Sogno Formation and coeval outcrops of central Europe that also share the presence of similar fishes and crustaceans. -
Coleoptera: Byrrhoidea
P O L I S H JOU R NAL OF ENTOM O LOG Y POL SKIE PISMO ENTOMOL OGICZ N E VOL. 80: 397-409 Gdynia 30 June 2011 DOI: 10.2478/v10200-011-0027-y Faunistic review of Polish Micropeplinae (Coleoptera: Staphylinidae) PAWEŁ JAŁOSZYŃSKI1, MAREK WANAT2, ANDRZEJ MELKE3 1,2Museum of Natural History, University of Wrocław, Sienkiewicza 21, 50-335 Wrocław, Poland, e-mails: [email protected], [email protected]; 3ul. Św. Stanisława 11/5, 62-800 Kalisz, e-mail: [email protected] ABSTRACT. The distributions of the Micropeplinae (Staphylinidae) within the present-day territory of Poland are summarized on the basis of surveys of the literature and collections. An updated and annotated checklist of Polish micropeplines is given, comprising two genera and seven species. Micropeplus staphylinoides (MARSHAM) has been removed from the list; the occurrence of M. caelatus ERICHSON and M. longipennis KRAATZ, reported by previous authors, needs to be confirmed with new findings. Micropeplus latus HAMPE is reported for the first time from Poland, based on a specimen collected in the Małopolska Upland, close to the Świętokrzyskie Mts. An updated identification key for Polish Micropeplus spp. is presented and habitus photographs of M. latus are provided. KEY WORDS: Coleoptera, Staphylinidae, Micropeplinae, Micropeplus latus, new record, Poland. INTRODUCTION The Micropeplinae are a relatively small group of staphylinids associated with moist forest floor litter, water margins, plant debris or nests of mammals; they feed on mould spores and hyphae (reviewed by CAMPBELL 1968; LÖBL & BURCKHARDT 1988; NEWTON 1991; THAYER 2005). Despite their distinctive morphology, these small beetles have been inadequately studied, and even knowledge of the distributions of species occurring in Central Europe is rather fragmentary. -
Body Size and Life History Traits of the Fire Salamander Salamandra
Amphibia-Reptilia 41 (2020): 63-74 brill.com/amre Body size and life history traits of the fire salamander Salamandra salamandra from Poland Anna Najbar1,∗, Agnieszka Konowalik1, Konrad Halupka2, Bartłomiej Najbar3, Maria Ogielska1 Abstract. The fire salamander Salamandra salamandra is a widespread taxon in Europe, exhibiting great intraspecific diversity in phenotype and life history traits across its geographical distribution. Here, we studied body size, sexual dimorphism, age, growth rate and condition of fire salamanders from the north-eastern margin of its range. In total, 2,102 individuals from 23 populations representing the Polish parts of the Sudetes and the Carpathian Mountains were sampled between 2004 and 2016. Body traits and age showed significant differences between the western (the Sudetes) and eastern (the Carpathians) groups of populations. Salamanders from the Carpathians tended to be longer, heavier and older. Female-biased sexual size dimorphism was found only in the Carpathians. Body condition at the beginning of the season was poor, then increased to reach a peak in early June, and deteriorated toward the end of the season. Age estimated by skeletochronology on phalangeal bones ranged from 2 to 16 years in both females and males, with the highest share of 7- to 9-year-old individuals. Age of juveniles ranged from 1 to 5 years in the Sudetes and from 1 to 4 years in the Carpathians. Growth curves (fitted using von Bertalanffy’s model) were asymptotic throughout the individual lifespans, but exhibited differences between sexes and mountain ranges. Altitude did not explain differences in characteristics of populations living in the two mountain ranges, but these differences most probably resulted from habitat quality (better in the Carpathians) and adverse human impact (higher in the Sudetes). -
“Geochemical Characterisation of the Pliensbachian-Toarcian Boundary During the Onset of the Toarcian Oceanic Anoxic Event
“Geochemical characterisation of the Pliensbachian-Toarcian boundary during the onset of the Toarcian Oceanic Anoxic Event. North Yorkshire, UK” Najm-Eddin Salem A thesis submitted to Newcastle University In partial fulfilment of the requirements for the degree of Doctor of Philosophy in the Faculty of Science and Agriculture School of Civil Engineering and Geosciences, Newcastle University, UK. February 2013 I ABSTRACT The lower Whitby Mudstone Formation of the Cleveland Basin in North Yorkshire (UK) is a world renowned location for the Early Toarcian (T-OAE). Detailed climate records of the event have been reported from this location that shed new light on the forcing and timing of climate perturbations and associated development of ocean anoxia. Despite this extensive previous work, few studies have explored the well-preserved sediments below the event that document different phases finally leading to large-scale (global) anoxia, which is the focus of this project. We resampled the underlying Grey Shale Member at cm-scale resolution and conducted a detailed multi-proxy geochemical approach to reconstruct the redox history prior to the Toarcian OAE. The lower Whitby Mudstone Formation, subdivided into the Grey Shale Member overlain by the Jet Rock (T-OAE), is a cyclic transgressive succession that evolved from the relatively shallow water sediments of the Cleveland Ironstone Formation. The Grey Shale Member is characterised by three distinct layers of organic rich shales (~10-60 cm thick), locally named as the ‘sulphur bands’. Directly above and below these conspicuous beds, the sediments represent more normal marine mudstones. Further upwards the sequence sediments become increasingly laminated and organic carbon rich (up to 14 wt %) representing a period of maximum flooding that culminated in the deposition of the Jet Rock (T-OAE). -
Cainozoic Evolution of Lower Silesia, Sw Poland: a New Interpretation in the Light of Sub-Cainozoic and Sub-Quaternary Topography
Acta Geodyn. Geomater.Vol.1, No.3 (135), 7-29, 2004 CAINOZOIC EVOLUTION OF LOWER SILESIA, SW POLAND: A NEW INTERPRETATION IN THE LIGHT OF SUB-CAINOZOIC AND SUB-QUATERNARY TOPOGRAPHY Janusz BADURA 1) *, Bogusław PRZYBYLSKI 1) and Witold ZUCHIEWICZ 2) 1) Lower Silesian Branch, Polish Geological Institute, al. Jaworowa 19, 50-122 Wrocław, Poland 2) Institute of Geological Sciences, Jagiellonian University, ul. Oleandry 2A, 30-063 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received March 2004, accepted June 2004) ABSTRACT An analysis of the youngest tectonic movements by the use of either morphometric or instrumental techniques should take into account both exposed and buried fault zones. The sub-Cainozoic and sub-Quaternary surface maps presented in this study display buried palaeotopography whose interpretation proves helpful in identification of tectonic dislocations. Such a kind of analysis has been conducted for the area of Lower Silesia, including the Sudetes, Fore-Sudetic Block, and Fore-Sudetic Monocline. The maps have been constructed on the basis of well-bore data, vertical geoelectrical soundings, and detailed mapping of exposures of pre-Quaternary rocks. Well-bore data have been reinterpreted with a view to reconstruct the original depth to the top of the crystalline basement. Many archival borehole descriptions place the boundary between Tertiary strata and the Proterozoic-Palaeozoic substratum at the top of poorly weathered rocks, including regoliths of the crystalline substratum into the Tertiary cover. The presented maps portray for the first time the actual morphology of the sub-Cainozoic surface. A comparison between the sub-Cainozoic and sub-Quaternary surface maps enables us to document changes in tectonic mobility throughout Cainozoic times. -
Source Rock Investigations of a Middle Jurassic Posidonia Marl of the Ionian Zone of Albania
Source rock investigations of a Middle Jurassic Posidonia marl of the Ionian Zone of Albania 1 1 1 2 1 1 NEUMEISTER S. , GAWLICK H.J. , BECHTEL, R. , HOXHA, L. , MISSONI, S. , GRATZER, R. 3 & DUMITRICA, P. 1 University of Leoben, Department for Applied Geosciences and Geophysics, Prospection and Applied Sedimentology, Peter-Tunner-Straße 5, 8700 Leoben, Austria; 2 Geological Survey of Albania, Tirana, Albania; 3 Dennigkofenweg 33, 3073 Guemligen, Switzerland The understanding of genesis and source rock potential of sediments deposited in the course of the sedimentary history of development (trench formation, passive continental margin, active continental margin) and which build the orogenic belts today is of significant importance. Regarding the Ionian Zone of the Albanides in particular different potential source rocks in Jurassic successions should be connected with global anoxic events (OAE; e.g., Toarcian - JENKYNS 1988). Therefore we investigated in this study a Jurassic source rock of the Ionian Zone of southern Albania, estimated to be deposited in Toarcian (e.g., MECO & ALIAJ 2000), because these rocks have not been investigated in detail until now. In Late Early Jurassic (Toarcian) a slight deepening was interpreted as cause of the general sea- level rise in the Toarcian (e.g., MECO & ALIAJ 2000) or interpreted as attributed to a local rifting event (KARAKITSIOS 1995). According to KARAKITSIOS (1995) the deposition of deep-water sediments and also the accumulation of organic matter in the Ionian Zone should be directly related to the geometry of a synrift period of the “Ionian Basin”. He distinguished Lower (Toarcian) and Upper (Tithonian; resp. Callovian to Tithonian) Posidonia beds. -
A Synoptic Review of the Vertebrate Fauna from the “Green Series
A synoptic review of the vertebrate fauna from the “Green Series” (Toarcian) of northeastern Germany with descriptions of new taxa: A contribution to the knowledge of Early Jurassic vertebrate palaeobiodiversity patterns I n a u g u r a l d i s s e r t a t i o n zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Sebastian Stumpf geboren am 9. Oktober 1986 in Berlin-Hellersdorf Greifswald, Februar 2017 Dekan: Prof. Dr. Werner Weitschies 1. Gutachter: Prof. Dr. Ingelore Hinz-Schallreuter 2. Gutachter: Prof. Dr. Paul Martin Sander Tag des Promotionskolloquiums: 22. Juni 2017 2 Content 1. Introduction .................................................................................................................................. 4 2. Geological and Stratigraphic Framework .................................................................................... 5 3. Material and Methods ................................................................................................................... 8 4. Results and Conclusions ............................................................................................................... 9 4.1 Dinosaurs .................................................................................................................................. 10 4.2 Marine Reptiles ....................................................................................................................... -
Non-Marine Carbon-Isotope Stratigraphy of the Triassic-Jurassic
Earth-Science Reviews 210 (2020) 103383 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Review article Non-marine carbon-isotope stratigraphy of the Triassic-Jurassic transition in T the Polish Basin and its relationships to organic carbon preservation, pCO2 and palaeotemperature ⁎ Grzegorz Pieńkowskia, , Stephen P. Hesselbob, Maria Barbackac,e, Melanie J. Lengd,f a Polish Geological Institute – National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland b Camborne School of Mines and Environment and Sustainability Institute, University of Exeter, Penryn TR10 9FE, UK c W. Szafer Institute of Botany, PAN, ul. Lubicz 46, PL- 31-512 Kraków, Poland d National Environmental Isotope Facility, British Geological Survey, Nottingham NG12 5GG, UK e Department of Botany, Hungarian Natural History Museum, H-1476 Budapest, P.O. Box 222, Hungary f Centre for Environmental Geochemistry, School of Biosciences, University of Nottingham, LE12 5RD, UK ARTICLE INFO ABSTRACT 13 Keywords: New carbon-isotope data obtained from homogenous organic material (separated microfossil wood; δ Cwood) Chemostratigraphy from the upper Rhaetian and entire Lower Jurassic permit chemostratigraphic correlation of these marginal/ Correlation non-marine deposits with the biostratigraphically well-constrained Llanbedr (Mochras Farm) core in N Wales Paralic facies and other marine profiles, supported by sequence stratigraphic correlation and biostratigraphical markers. Palaeoclimate 13 Statistically significant (Rs = 0.61) positive exponential correlation between δ Cwood values and continental Carbon isotopes 13 TOC (TOCcont) concentrations occurs and can be defined empirically by equation. Changes of δ Cwood observed 13 in C3 plants depends on δ CO2 of atmosphere and can be modulated by other factors such as pCO2 causing fractionation (enrichment in 12C) of C isotopes in source C3 plants and, to lesser extent, by soil moisture content.