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The Carboniferous in Western Pomerania

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deformacji typu fałdowego. W strefie okalającej strukturę AenJleMOH KaK cyAeTCKo-caCKO-TYP"1HrCKaJl 30Ha, "1ni.t W"1- sudecką tworzyły się w tym czasie osady asocjacji flisz~ pe - KaK cppaHKo-YewcKaJl 30Ha. 0Tno>KeHi.tJl MopaacKo­ wej a na pograniczu obu stref utwory typu olistostromów, -clorne3cKoiir 30Hbl npi.tHaAne>KaT K BHewHeH uen1-1 eapo­ zachowane dziś fragmentarycznie w strukturze kaczawskiej nei:1cK1-1x Bap"1CU"1AOB . i bardzkiej. - Kap6oH a npeAenax paccMaTp1-1aaeMoro pai'loHa npeA­ Utwory węglonośne wchodzące w skład zapadliska CTaaneH OCaAKaMi.t, aynKaHi.tTaMi.t "' "1HTPY3"1JlM"1 rpaHi.tT0- Sudetów Środkowych okteślono jako molasę młodszą, "1AOB. Pa3HOCTb B03pacTa, cpau1-1anbHoro npeACTaaneHi.tJl która zdeponowana została w wewnętrznej strefie łuku 1-1 CTeneHi.t npeo6.pa>KeH"1Jl oTno>KeH"1H coceAYK>Llli.tX c co- waryscydów europejskich. 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YrneHOCHb1e oTno>KeHi.tR BXOAJlll.1"1e · a cocTaa npo­ Kap60HCK"1e OTno>KeH"1Jl t0ro-3anaAHOH nonbW"1 BXO­ rn6a ueHTpanbHblX CyAeToB np"1Yi.tcneHbl K MnaAwei:1 AJlT B COCTaB non"1reH"11.feCKOH cyAeTCKOH CTpyKTYPbl Monacce, oca>KAeHHOH BO BHyTpeHHeH 30He AYrl-1 eapo­ "1 MopaBCKO-C"1ne3CKOH 30Hbl, a TaK>Ke ee ceaepo-3anaA­ nei'lcKi.tX aap1-1cui.tAOB. B Ta6n"1ue 1 npeACTaaneHa Koppe­ HOrO npOAOn>KeH"1Jl B OCHOBe nepMCK"1X "1 Me3030HCK"1X nRUi.tR m1TOCTpaTi.1rpacp"1YeCK"1X eA"1H"1U C"1ne3a l.feWCKOH oCaAKOB npeACYAeTCKOH MOHOKn"1Han"1 (p"1C 1). CyAeT­ 1-1 nonbĆ:KoH yacTei'I npont6a UeHTpanbHblX Cy.QeToB. CKaJl CTPYKTypa, B COCTaB KOTOpOH BXOAJlT co6CTBeHHO YrneHocHaJl Monacca BepxHec1-1ne3cKoro yronbHoro 6ac­ CyAeTbl, npeACYAeTCK"1H 6noK "1 np"1nerat0L11aJ1 YaCTb cei:1Ha HaXOA"1TCR BO BHewHeH 30He sapi.tCU"1HCKOH Ayrn, npeACYAeTCKOM MOHOKn"1Han"1, COCTaBnJleT C060H cppar­ a ueHTpanbHOl.fell.ICKi.te yronbHb1e 6accei'IHbl pacnono>Ke­ MeHT BHyTpeHHeH uen"1 eaponeMCK"1X aap"1CU"1AOB, onpe- Hbt B npeAenax sap1-1cu1-1i:1cKoro Me>KropHoro Macc1-1sa. ANTONI M. ŻELICHOWSKI Geological Institute, Rakowiecka 4, 00-975 Warsaw THE CARBONIFEROUS IN WESTERN POMERANIA UKD 551-735.1/.2.022 : 561/562 : 552.5(438-16 Pomorze Zachodnie) In the last two decades, Carboniferous strata have R . Dadlez (1) proposed subdivision of the Lower Car­ been encountered in some tens drillings in western Pome­ boniferous into a few complexes. In the --faiier subdIVłsfoil,'­ rania. Both the Dinantian and Silesian have been recorded quartz sandstones encountered beneath the Permian in there. The bistory of studies on these rocks goes back to over a dozen boreholes were assigned to the Upper Carbo­ 1961 when J. Poborski and L. Cimaszewski· described niferous, in accordance with contemporaneous strati­ Lower Carboniferous dolomites and daystones from the graphic interpretations. borehole column Bobolice 1. The progress in drillings Stratigraphic studies on Carboniferous and Devonian· works, mainly carried out by the oil industry as well as strata, initiated at the beginning of the seventies, questioned the Geological Institute, gave new boreholes of the Car.:. severa} earlier views (7, 21). H. Matyja (12) and K . Ko­ boniferous. The studies on macrofauna, carried out by rejwo (8-10) showed Tournaisian age of several sequences K . Korejwo (7), showed the presence of the Tournaisian, hitherto regarded as the Visean. Palynological analyses Visean and Upper Carboniferous. Drillings made in carried out by E. Turnau ( 19 - 20) showed that a part - area between Kołobrzeg and Chojnice revealed the presence of rocks previously assigned to the Upper Carbóniferous of Carboniferous · rocks markedly differing in lithology actually represent the Dinantian whilst H. Krawczyńska­ from those known in northern G.D.R. (6, 17) whilst the -Grocholska (11) and H. Kmiecik evidenced the presence Silesian resetnbling coeval strata from Riigen and northern of the Westphalian. The stratigraphic works were accom­ Mecklenburgia were found in area between Trzebiatów panied by petrographic analyses (4, 13), supplementing and Kamień Pomorski not before the mid-seventies. lithostratigraphy (1, 21 ). The lithology of Diriantian strata The stratigraphic studies were accompanied by attempts is here discussed with reference to lithological subdivision to establish local lithostratigraphic subdivisions made proposed by R. Dadlez and subsequently modified by the by J. Kuchciński, B. Sikorski, J. Ryba and A. Łobza, present author (22) and the Silesian - with reference mainly on the basis of well logs. Taking into account to the subdivision proposed by the present author. lithological differentiation of strata in the interval between In western Pomerania, Carboniferous strata have been Upper Devonian carbonate compl ex and Permian rocks, found in a bełt stretching along the Baltic coast from the 356 CORRELATIONS OF THE CARBONIFEROUS IN NORTHERN GDR, NORTHERN POLAND AND LATVIA Northern GDR Northern Poland - Pomerania Latyia Northern Riigen Is. NW part Central part**, NE part Mecklemburgia and Hiddensee Is. Kamień Pomorski, Świdwin, (17) Koszalin, i (~_._?) '. Trzebiatów Bydgoszcz Brda 1 .,.._. Monchguter Sch. i::~ 160m ·a.§ ~ _.........._ ---- ,........ ......_ ....... / ~ ~ I -...... ~ "'-./" ~ '-./" 'v' Dziwna Formation Dziwna Fm. 68+170 m t5fr< 1 R amb" mer Sc h . - , 95 +248 m 150+170 m , · Trenter Sch. 100 _+130 m o brown-red siltstones Dornbusch Sch. Rega Fm. - 180_+200 m 130_+170m ~ u t-------....1 s 1 t<--- with ~" • .., • „ i... i.. Jasmunder Sch. sandstones and """ ~ ~ '.~ 270+310 m conglomerates at the sandstones, ~ ..c:: Wolin Fm base 180-330 m siltstones, coals, ~ -+-----------------1-ł 41_+282 m .(825 m) marine horizons I.I„"" ... """""""'"'"' .... ""' ...... "" ·107_+404 m ~ Lohmer Sch. 25_+50 m „ ~i.-----------------4-1 ~,,~J ~~ ... ~~~ ... ~~~~~ ... ~ < Wieker Sch. 50 + 70 m ,-„„ Hiddenseer Sch. 40 _+ 50 m J" i..""'"""' -: itfflh a~d 5Jalkow _s~~ ~- „ ' - -• .~;::s i:i:i cla'y"ollo~ ~ ~~ stones, stigmana ~ .: 1~-~~:'"rriri~ ,„ . - ,J . ' ,.. ,_. ", 1.o .............. .,. ... ,i.,. ... „i,.."'-...... .,.--.....~.... ~-ui....., "'""'~i..,,,..i..„ claystones, Riigenls. - Nadarzyce Complex Hiddensee sandstones, mar Is, over 250 m >"' sandstones, conglomerates limestones claystones 400_+500 m over over 300 m - 400m >"' Drzewiany d Q Kurowo Complex Complex oj ~"~ oj up to 400 m ~ "'.... ~ 400 m a gb oj > a > limestones a a oo~ o ,,,a I oo __Kurow9 Complex 500 m ~i)':~ dO >~ I o >.- or- over 150 m .; t1 ~ +. ~+ 8 uO >.o ;.:: .Q ~ ~~ - a a "'oo dO "'oo i::"' • o!"'"\ do E-< :at:.; + • O N i::"' ~~ + E-< Chmielno ; ~g ; ~o Łobżonka Complex Supercomplex d Eo- a-os„. d -~ -~ over 300 m up to 400 m <Il- ";;i -- gap e ..c:: e;::s ;::s o o -~] E-< E-< "' .... a "' -s - ~ g -~ e'i' a d I• a"'+(.) Q) ' E-< · ~ QO ·~8 L--------7 e .t:;: oo Sąpolno Complex Sąpolno ,~ d .., E-< a~- · ~+ over 130 m Complex · / o "O Q) -o Nic. su.* - d"' Oo o oj <Il -o- - - .-. .... "O "'J:) O+A ,y~-: ~-u.: Lie.-stL'*"" * "Nic - Ńicaskaja ISui te,: Lie - Lietiżhskaj~ j S11ite ~ ! Pap - Paplakskaja I Sui te. ** Strata here assigned to the Silesian are regarded as the Rotliegendes in (14, 15). 357 vicinities of Kamień Pomorski to Koszalin and also from grains, debris of trachytes, rhyolites and volcanic glass the latter town to Chojnice. South-west of the Koszalin - as well as quartz grains and micas. Among feldspars, Chojnice zone, single drillings entered the Carboniferous, K-feldspars varying in degree of alteration, kaolinitiza­ failing to reach its base. tion, carbonatization and sulfatization predominate. Some feldspars display regeneration rims. No direct sources LITHOLOG I CAL-ST RATIG RAP HIC of volcanic materiał were found in Pomerania and Dinan­ CHARACTERISTICS tian volcanism is here represented by diabase dykes only (4). Dinantian Sandstones occurring in eastern and western parts of this region are mainly built ·of quartz (Trzebiechów In western Pomerania, the Dinantian is subdivided complex). Some anhydrites from the Kołobrzeg area ori­ into a .few lithological complexes, i.e. informal units which ginated in result of epigenetic changes of feldspars and when formalized will correspond to the lithostratigraphic others - in result of evaporation. ones of the formation rank. The supercomplex differentiated The Chmielno supercomplex is 400 m thick, wedging here corresponds to group. out to NE. Using the available stratigraphic data (8, 10, The Sąpolno complex is regarded as the lowermost 12, 20), it is dated at the Tournaisian and Visean. Datings lithostratigraphic unit of the Dinantian. It is recognized obtained for the SW -NE section show that sedimenta­ in borehole columns in area between Trzebiatów, Kosza­ tion of its rocks started in the Early Tournaisian (Tnl b-2),
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    PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9.
  • The River Odra Estuary As a Gateway for Alien Species Immigration to the Baltic Sea Basin Das Oderästuar Als Pfad Für Die Einwanderung Von Alienspezies in Die Ostsee

    The River Odra Estuary As a Gateway for Alien Species Immigration to the Baltic Sea Basin Das Oderästuar Als Pfad Für Die Einwanderung Von Alienspezies in Die Ostsee

    Acta hydrochim. hydrobiol. 27 (1999) 5, 374-382 © WILEY-VCH Verlag GmbH, D-69451 Weinheim, 1999 0323 - 4320/99/0509-0374 $ 17.50+.50/0 The River Odra Estuary as a Gateway for Alien Species Immigration to the Baltic Sea Basin Das Oderästuar als Pfad für die Einwanderung von Alienspezies in die Ostsee Dr. Piotr Gruszka Department of Marine Ecology and Environmental Protection, Agricultural University in Szczecin, ul. Kazimierza Królewicza 4/H, PL 71-550 Szczecin, Poland E-mail: [email protected] Summary: The river Odra estuary belongs to those water bodies in the Baltic Sea area which are most exposed to immigration of alien species. Non-indigenous species that have appeared in the Szczecin Lagoon (i.a. Dreissena polymorpha, Potamopvrgus antipodarum, Corophium curvispinum) and in the Pomeranian Bay (Cordylophora caspia, Mya arenaria, Balanus improvisus, Acartia tonsa) in historical time and which now are dominant components of animal communities there as well as other and less abundant (or less common) alien species in the estuary (e.g. Branchiura sowerbyi, Eriocheir sinensis, Orconectes limosus) are presented. In addition, other newcomers - Marenzelleria viridis, Gammarus tigrinus, and Pontogammarus robustoides - found in the estuary in the recent ten years are described. The significance of the sea and inland water transport in the region for introduction of non-indigenous species is discussed against the background of the distribution pattern of these recently introduced polychaete and gammarid species. Keywords: Alien Species, Marenzelleria viridis, Gammarus tigrinus, Pontogammarus robustoides, River Odra Estuary Zusammenfassung: Das Oderästuar gehört zu den Bereichen der Ostsee, die am meisten der Einwanderung von Alienspezies ausgesetzt sind.
  • The Evolution of Trilobite Body Patterning

    The Evolution of Trilobite Body Patterning

    ANRV309-EA35-14 ARI 20 March 2007 15:54 The Evolution of Trilobite Body Patterning Nigel C. Hughes Department of Earth Sciences, University of California, Riverside, California 92521; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:401–34 Key Words First published online as a Review in Advance on Trilobita, trilobitomorph, segmentation, Cambrian, Ordovician, January 29, 2007 diversification, body plan The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The good fossil record of trilobite exoskeletal anatomy and on- 10.1146/annurev.earth.35.031306.140258 togeny, coupled with information on their nonbiomineralized tis- Copyright c 2007 by Annual Reviews. sues, permits analysis of how the trilobite body was organized and All rights reserved developed, and the various evolutionary modifications of such pat- 0084-6597/07/0530-0401$20.00 terning within the group. In several respects trilobite development and form appears comparable with that which may have charac- terized the ancestor of most or all euarthropods, giving studies of trilobite body organization special relevance in the light of recent advances in the understanding of arthropod evolution and devel- opment. The Cambrian diversification of trilobites displayed mod- Annu. Rev. Earth Planet. Sci. 2007.35:401-434. Downloaded from arjournals.annualreviews.org ifications in the patterning of the trunk region comparable with by UNIVERSITY OF CALIFORNIA - RIVERSIDE LIBRARY on 05/02/07. For personal use only. those seen among the closest relatives of Trilobita. In contrast, the Ordovician diversification of trilobites, although contributing greatly to the overall diversity within the clade, did so within a nar- rower range of trunk conditions.
  • Gryfino, 26.06.2017 R. Factors Governing How and Where Waterbirds

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    Gryfino, 26.06.2017 r. Factors governing how and where waterbirds forage in the Odra River Estuary (NW Poland) during the wintering season Dominik Marchowski The Odra estuary has been known for years as a site where large numbers of waterbirds congregate during the migration and wintering periods. The first accurate data were collected by Prof. Włodzimierz Meissner from the University of Gdansk:. He and his team carried out aerial counts of the entire estuary in three winter seasons: 1990/91, 1991/92 and 1992/93. It turned out that the Szczecin Lagoon, the Kamień Lagoon and Lake Dąbie are Poland's largest wintering areas for Greater Scaup Aythya marila (hereafter Scaup), Smew Mergellus albellus and Goosander Mergus merganser. In the 1990/91 winter season, for example, 96% of the Goosanders wintering on the Polish coast were present in the Odra estuary, and a single flock observed in December 1990 consisted of 60 000 birds. Moreover, 80% of Scaup and 54% of Smew wintering on the Polish coast did so in the Odra estuary. Prof. Meissner's team has also demonstrated the importance of the estuary to several other waterbird species, including Tufted Duck A. fuligula, Pochard A. ferina, Goldeneye Bucephala clangula and Coot Fulica atra. No data on the numbers of wintering birds were gathered for the next few years. Since the turn of the century, however, the West Pomeranian Nature Society (ZTP) has been monitoring (counting) these wintering populations on a regular basis, and the results from seasons 2001 – 2008 have been published in the ZTP’s bulletins and in the journal Ornis Polonica.
  • Plan Zagospodarowania Przestrzennego Województwa Wielkopolskiego

    Plan Zagospodarowania Przestrzennego Województwa Wielkopolskiego

    SPIS TREŚCI PLAN ZAGOSPODAROWANIA PRZESTRZENNEGO WOJEWÓDZTWA WIELKOPOLSKIEGO WPROWADZENIE .............................................................................................................. 13 1. Założenia ogólne ...................................................................................................... 14 2. Podstawa prawna .................................................................................................... 15 3. Części składowe Planu ............................................................................................ 16 4. Przebieg prac nad Planem ...................................................................................... 18 5. Zakres opracowania ................................................................................................ 20 5.1. Zakres przestrzenny .................................................................................... 20 5.2. Zakres czasowy ............................................................................................ 20 5.3. Zakres rzeczowy .......................................................................................... 20 6. Skutki prawne uchwalenia Planu .......................................................................... 22 UWARUNKOWANIA ROZWOJU PRZESTRZENNEGO ..................... 23 UWARUNKOWANIA ZEWNĘTRZNE ........................................................................... 23 7. Polityka przestrzenna Unii Europejskiej .............................................................. 24 8. Wielkopolska