Redalyc.A Jurassic (Bathonian-Callovian
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Letter to the Editor
GeoArabia, Vol. 10, No. 3, 2005 Gulf PetroLink, Bahrain LETTER TO THE EDITOR from Ghaida Al-Sahlan ([email protected]), Kuwait Oil Company, Ahmadi, Kuwait n the recent GeoArabia, Haq and Al-Qahtani (2005) updated the chronostratigraphic Arabian Plate Iframework of Sharland et al. (2001). These studies cite the paper by Yousif and Nouman (1997) to represent the Jurassic type section of Kuwait. Yousif and Nouman published the composite log for the Minagish-27 well (see Figure on page 194) and depicted the Jurassic formations and stages, side-by- side, but only in a generalized manner. In order to refine the ages for this section, I would like to share some preliminary unpublished biostratigraphic and Sr isotope data (see Table and Notes) from analyses by Varol Research (1997 unpublished report), ExxonMobil (1998 unpublished report) and Fugro-Robertson (2004 unpublished report). To convert Sr ages (Ma) to biostages, or biostages to ages, I have used the Geological Time Scale (GTS) 2004 (Gradstein et al., 2004). I thank G.W. Hughes, A. Lomando, M. Miller and O. Varol for their comments. Unit or Boundary Age and Stage Gradstein et al. (2004) Makhul (Offshore) Tithonian-Berriasian (Bio) Base Makhul (N. Kuwait) No younger than Tithonian (Bio) greater than 145.5 + 4.0 Top Hith (W. Kuwait) 150.0 (Sr) = c. Tithonian/Kimmeridgian ? 150.8 + 4.0 Upper Najmah (S. Kuwait) 155.0 (Sr) = c. Kimmeridgian/Oxfordian 155.7 + 4.0 Najmah (N. Kuwait) No older than Oxfordian (Bio) less than 161.2 + 4.0 Lower Najmah Shale (N. Kuwait) middle and late Bathonian (Bio) 166.7 to 164.7 + 4.0 Top Sargelu (S. -
A Comparison of the Dinosaur Communities from the Middle
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 31 July 2018 doi:10.20944/preprints201807.0610.v1 Peer-reviewed version available at Geosciences 2018, 8, 327; doi:10.3390/geosciences8090327 1 Review 2 A comparison of the dinosaur communities from 3 the Middle Jurassic of the Cleveland (Yorkshire) 4 and Hebrides (Skye) basins, based on their ichnites 5 6 Mike Romano 1*, Neil D. L. Clark 2 and Stephen L. Brusatte 3 7 1 Independent Researcher, 14 Green Lane, Dronfield, Sheffield S18 2LZ, England, United Kingdom; 8 [email protected] 9 2 Curator of Palaeontology, The Hunterian, University of Glasgow, University Avenue, Glasgow 10 G12 8QQ, Scotland, United Kingdom; [email protected] 11 3 Chancellor's Fellow in Vertebrate Palaeontology, School of Geosciences, University of Edinburgh, 12 Grant Institute, The King's Buildings, James Hutton Road, Edinburgh EH9 3FE, Scotland, United Kingdom; 13 [email protected] 14 * Correspondence: [email protected]; Tel.: 01246 417330 15 16 Abstract: 17 Despite the Hebrides and Cleveland basins being geographically close, research has not 18 previously been carried out to determine faunal similarities and assess the possibility of links 19 between the dinosaur populations. The palaeogeography of both areas during the Middle Jurassic 20 shows that there were no elevated landmasses being eroded to produce conglomeratic material in 21 the basins at that time. The low-lying landscape and connected shorelines may have provided 22 connectivity between the two dinosaur populations. 23 The dinosaur fauna of the Hebrides and Cleveland basins has been assessed based primarily 24 on the abundant ichnites found in both areas as well as their skeletal remains. -
Upper Bajocian– Callovian) of the Polish Jura Chain and Holy Cross Mountains (South-Central Poland)
1661-8726/07/010153-12 Swiss j. geosci. 100 (2007) 153–164 DOI 10.1007/s00015-007-1207-3 Birkhäuser Verlag, Basel, 2007 A diverse crinoid fauna from the Middle Jurassic (Upper Bajocian– Callovian) of the Polish Jura Chain and Holy Cross Mountains (south-central Poland) MARIUSZ A. SALAMON*& MICHA¸ ZATO¡ Key words: crinoids, Middle Jurassic, Poland, palaeobiogeography, taphonomy, epibiontism ABSTRACT ZUSAMMENFASSUNG A systematic account of a diverse crinoid fauna from the Middle Jurassic Aus mitteljurassischen (Bajocian–Callovian) Sedimenten des südlichen (Upper Bajocian–Callovian) of the Polish Jura Chain and Holy Cross Moun- Zentralpolens (Krakow–Cz´stochowa Hochland und Heilig-Kreuz Gebirge) tains (south-central Poland) is presented. The description is supplemented wird eine diverse Crinoidenfauna systematisch beschrieben und stratigra- with a list of all crinoid species found hitherto in the Tatra Mountains and the phisch eingestuft. Die Beschreibung wird durch eine Zusammenstellung sämt- Pieniny Klippen Belt (Poland), which were a part of the northern margin of licher Crinoiden-Spezies ergänzt, die bislang im Tatra-Gebirge und im Pieniny the Tethys during Middle Jurassic time. Balanocrinus hessi seems to be en- Klippen-Gürtel gefunden wurden. Beide Regionen waren während des Mitt- demic and established its own population in the epicontinental sea. Other leren Jura Teil des Nordrandes der Tethys. Balanocrinus hessi bildete eigen- stalked crinoids entered from the Tethys through the East-Carpathian Gate or ständige Populationen in diesem epikontinentalen Meeresbereich und scheint from a westerly way, and constitute a typical Mediterranean fauna. Stemless endemisch gewesen zu sein. Andere gestielte Crinoiden drangen aus der forms are regarded to be unsuccessful immigrants. -
Ammonites from Bathonian and Callovian (Middle Jurassic)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 253 Zitteliana 89 Ammonites from Bathonian and Callovian (Middle Jurassic) North of Damghan, Paläontologie Bayerische EasternGeoBio- Alborz, North Iran & Geobiologie Staatssammlung Center LMU München LMU München für Paläontologie und Geologie Kazem Seyed-Emami1* & Ahmad Raoufian2 München, 01.07.2017 1School of Mining Engineering, University College of Engineering, University of Tehran, Manuscript received P.O. Box 11365-4563, Tehran, Iran 2 26.09.2016; revision Daneshvar Center, Farhangian University, Neyshapour, Iran accepted 30.10.2016 *Corresponding author; E-mail: [email protected] ISSN 0373-9627 ISBN 978-3-946705-00-0 Zitteliana 89, 253–270. Abstract The following Middle Jurassic ammonite families (subfamilies) are described from the Dalichai Formation north of Damghan (eastern Alborz), some of them for the first time: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Stephanoceratidae (Cadomitinae), Tulitidae and Reineckeiidae. The fauna is typically Northwest-Tethyan and closely related to Central Europe (Subboreal – Submediterra- nean Provinces). Key words: Ammonites, Dalichai Formation, Middle Jurassic, Alborz, Iran Zusammenfassung Aus der Dalichai Formation nördlich von Damghan (Ostalborz) werden einige mitteljurassische Ammoniten, teils zum ersten Mal, beschrieben. Folgende Familien und Unterfamilien sind vertreten: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Steph- anoceratidae (Cadomitinae), Tulitidae und Reineckeiidae. Die Fauna ist typisch für die Nordwest-Tethys und zeigt enge Beziehungen zu Zentraleuropa (Subboreale und Submediterrane Faunenprovinz). Schlüsselwörter: Ammoniten, Dalichai Formation, Mittlerer Jura, Alborz, Iran Introduction the frame of a MSc. thesis. For the present study, a new section nearby was chosen and collections The present study is a continuation of a larger re- were made by A. -
Pliensbachian Nannofossils from Kachchh: Implications on the Earliest Jurassic Transgressive Event on the Western Indian Margin
53 he A Rei Series A/ Zitteliana An International Journal of Palaeontology and Geobiology Series A /Reihe A Mitteilungen der Bayerischen Staatssammlung für Paläontologie und Geologie 53 An International Journal of Palaeontology and Geobiology München 2013 Zitteliana Zitteliana A 53 (2013) 105 Pliensbachian nannofossils from Kachchh: Implications on the earliest Jurassic transgressive event on the western Indian margin Jyotsana Rai1 & Sreepat Jain2* Zitteliana A 53, 105 – 120 1Birbal Sahni Institute of Palaeobotany, 53 University Road, 226007, Lucknow, India München, 31.12.2013 2DG–2, Flat no. 52D, SFS Flats, Vikas Puri, New Delhi, 110018, India Manuscript received *Author for correspondence and reprint requests: E-mail: [email protected] 05.04.2013; revision accepted 16.11.2013 ISSN 1612 - 412X Abstract The oldest rocks within the Kachchh Basin belong to the sediments of Kaladongar Formation exposed in Kuar Bet, Pachchham Island (western India). The Formation’s lowest unit, the Dingi Hill Member has yielded a moderately diversified calcareous nannofossil assembla- ge that includes the marker species of Lotharingius contractus and Triscutum sullivanii of late Early Aalenian age associated with reworked species of Biscutum finchii, Bussonius prinsii, Crucirhabdus primulus, Crepidolithus pliensbachensis, Discorhabdus criotus and D. striatus suggesting an age spanning NJ4a to NJ7 Zones (Early Pliensbachian, Tethyan ammonite Jamesoni Zone to Middle Toarcian, Variabilis Zone). Additionally, samples from four other Kachchh domal localities (Kachchh Mainland: Jara, Jumara and Habo and the Island belt, Waagad) have also yielded reworked Pliensbachian-Toarcian age (~183 Ma) nannotaxa viz. Crepidolithus granulatus, Diductius constans, Mazaganella protensa, Mitrolithus elegans, Parhabdolithus liasicus, Similiscutum orbiculus, and Triscutum tiziense. This nannotaxa age is much earlier than the ammonite-based Earliest Bajocian date (~171.6 Ma) based on the presence of ammonite Calliphylloceras hetero- phylloides (Oppel). -
GEOLOGIC TIME SCALE V
GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE -
The Jurassic (Pliensbachian to Oxfordian) Palynology of the Algarve Basin and the Carrapateira Outlier, Southern Portugal
1 The Jurassic (Pliensbachian to Kimmeridgian) palynology of the Algarve Basin and the 2 Carrapateira outlier, southern Portugal 3 4 Marisa E.N. Borges a,b, James B. Riding c*, Paulo Fernandes a, Zélia Pereira b 5 6 a CIMA - Centro de Investigação Marinha e Ambiental. Universidade do Algarve, 7 Campus de Gambelas, 8005-139 Faro, Portugal 8 b LNEG-LGM, Rua da Amieira, 4465-965 S. Mamede Infesta, Portugal 9 c British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 10 5GG, UK 11 12 * Corresponding author. Tel.: +44(0)115 9363447. 13 E-mail addresses: [email protected] (M.E.N. Borges), [email protected] (J.B. 14 Riding), [email protected] (P. Fernandes), [email protected] (Z. Pereira). 15 16 ABSTRACT 17 The palynology of the Jurassic (Upper Pliensbachian to Lower Kimmeridgian) 18 fill of the Algarve Basin and the Carrapateira outlier, southern Portugal was 19 investigated. Samples were collected from Armação Nova Bay, Mareta Beach, Cilheta 20 Beach and the Carrapateira outlier. At Armação Nova Bay the Upper Pliensbachian- 21 Lower Toarcian succession proved barren, or yielded sparse, non age-diagnostic 22 palynomorphs. Dinoflagellate cysts are confined to the Upper Bajocian to Upper 23 Callovian sedimentary rocks exposed at Mareta and Cilheta beaches and the Lower 24 Kimmeridgian strata of the Carrapateira outlier. At Mareta Beach, the Upper Bajocian, 25 Bathonian and Callovian produced relatively low to moderate diversity dinoflagellate 26 cyst assemblages. Several key bioevents confirm the Bathonian and Callovian ages of 27 the succession; no age-significant Late Bajocian bioevents were noted. -
Mississippi Geology, V
THE DEPARTMENT OF ENVIRONMENTAL QUALITY • • Office of Geology P. 0. Box 20307 Volume 17 Number 1 Jackson, Mississippi 39289-1307 March 1996 TOWARD A REVISION OF THE GENERALIZED STRATIGRAPHIC COLUMN OF MISSISSIPPI David T . D ock ery III Mississippi Office of Geology INTRODUCTION The state's Precambrian subsurface stratigraphy is from Thomas and Osborne (1987), and the Cambrian-Permsylva The stratigraphic columns presented here are a more nian section is modified from Dockery ( 1981) . References informative revision on the state's 1981 column published as for the Cambrian-Ordovician section of the 1981 column one sheet (Dockery, 1981). This revision wasmade forafuture include Mellen (1974, 1977); this stratigraphy is also found in text on " An Overview of Mississippi's Geology" and follows Henderson ( 1991 ). the general format and stratigraphy as pub}jshed in the Corre When subdivided in oil test records, the state's Ordovi lation of Stratigraphic Units of North America (COSUNA) ciansection generally contains the Knox Dolomite, the Stones charts (see Thomas and Osborne, 1987, and Dockery, 1988). River Group (see AJberstadt and Repetski, 1989), and the The following discussion is a brief background, giving the Nashville Group, while the Silurian contains the Wayne major sources used in the chart preparations. Suggestions for Group and Brownsport Formation. The Termessee Valley improvements may be directed to the author. Autl10rity's (1977) description of a 1,326-foot core hole at their proposed Yellow Creek Nuclear Plant site in northeast em Tishomingo Catmty greatly refined the stratigraphy be PALEOZOJCSTRATJGRAPffiCUNITS tween the Lower Ordovician Knox Dolomite and the Ross Formation of Devonian age. -
2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
2009 GEOLOGIC TIME SCALE CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST. HIST. ANOM. ANOM. (Ma) CHRON. CHRO HOLOCENE 65.5 1 C1 QUATER- 0.01 30 C30 542 CALABRIAN MAASTRICHTIAN NARY PLEISTOCENE 1.8 31 C31 251 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 70.6 254 2A PIACENZIAN 32 C32 L 630 C2A 3.6 WUCHIAPINGIAN PLIOCENE 260 260 3 ZANCLEAN 33 CAMPANIAN CAPITANIAN 5 C3 5.3 266 750 NEOPRO- CRYOGENIAN 80 C33 M WORDIAN MESSINIAN LATE 268 TEROZOIC 3A C3A 83.5 ROADIAN 7.2 SANTONIAN 271 85.8 KUNGURIAN 850 4 276 C4 CONIACIAN 280 4A 89.3 ARTINSKIAN TONIAN C4A L TORTONIAN 90 284 TURONIAN PERMIAN 10 5 93.5 E 1000 1000 C5 SAKMARIAN 11.6 CENOMANIAN 297 99.6 ASSELIAN STENIAN SERRAVALLIAN 34 C34 299.0 5A 100 300 GZELIAN C5A 13.8 M KASIMOVIAN 304 1200 PENNSYL- 306 1250 15 5B LANGHIAN ALBIAN MOSCOVIAN MESOPRO- C5B VANIAN 312 ECTASIAN 5C 16.0 110 BASHKIRIAN TEROZOIC C5C 112 5D C5D MIOCENE 320 318 1400 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 326 6 C6 APTIAN 20 120 1500 CALYMMIAN E 20.4 6A C6A EARLY MISSIS- M0r 125 VISEAN 1600 6B C6B AQUITANIAN M1 340 SIPPIAN M3 BARREMIAN C6C 23.0 345 6C CRETACEOUS 130 M5 130 STATHERIAN CARBONIFEROUS TOURNAISIAN 7 C7 HAUTERIVIAN 1750 25 7A M10 C7A 136 359 8 C8 L CHATTIAN M12 VALANGINIAN 360 L 1800 140 M14 140 9 C9 M16 FAMENNIAN BERRIASIAN M18 PROTEROZOIC OROSIRIAN 10 C10 28.4 145.5 M20 2000 30 11 C11 TITHONIAN 374 PALEOPRO- 150 M22 2050 12 E RUPELIAN -
Ammonites from Bathonian and Callovian (Middle Jurassic) North Of
253 Zitteliana 89 Ammonites from Bathonian and Callovian (Middle Jurassic) North of Damghan, Paläontologie Bayerische EasternGeoBio- Alborz, North Iran & Geobiologie Staatssammlung Center LMU München LMU München für Paläontologie und Geologie Kazem Seyed-Emami1* & Ahmad Raoufian2 München, 01.07.2017 1School of Mining Engineering, University College of Engineering, University of Tehran, Manuscript received P.O. Box 11365-4563, Tehran, Iran 2 26.09.2016; revision Daneshvar Center, Farhangian University, Neyshapour, Iran accepted 30.10.2016 *Corresponding author; E-mail: [email protected] ISSN 0373-9627 ISBN 978-3-946705-00-0 Zitteliana 89, 253–270. Abstract The following Middle Jurassic ammonite families (subfamilies) are described from the Dalichai Formation north of Damghan (eastern Alborz), some of them for the first time: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Stephanoceratidae (Cadomitinae), Tulitidae and Reineckeiidae. The fauna is typically Northwest-Tethyan and closely related to Central Europe (Subboreal – Submediterra- nean Provinces). Key words: Ammonites, Dalichai Formation, Middle Jurassic, Alborz, Iran Zusammenfassung Aus der Dalichai Formation nördlich von Damghan (Ostalborz) werden einige mitteljurassische Ammoniten, teils zum ersten Mal, beschrieben. Folgende Familien und Unterfamilien sind vertreten: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Steph- anoceratidae (Cadomitinae), Tulitidae und Reineckeiidae. Die Fauna ist typisch für die Nordwest-Tethys und zeigt enge Beziehungen zu Zentraleuropa (Subboreale und Submediterrane Faunenprovinz). Schlüsselwörter: Ammoniten, Dalichai Formation, Mittlerer Jura, Alborz, Iran Introduction the frame of a MSc. thesis. For the present study, a new section nearby was chosen and collections The present study is a continuation of a larger re- were made by A. Raoufian (2015). search project on the ammonite fauna of the Dali- The greater part of the Morphoceratidae from Talu chai and Lar formations in eastern Alborz and Bina- and Kelariz (Fig. -
Aalenian – Bathonian) of the Mecsek Mountains, Southern Hungary
GEOLOGICA CARPATHICA, APRIL 2018, 69, 2, 117–127 doi: 10.1515/geoca-2018-0007 Carbon cycle history through the Middle Jurassic (Aalenian – Bathonian) of the Mecsek Mountains, Southern Hungary GREGORY D. PRICE 1, , ISTVÁN FŐZY 2 and ANDRÁS GALÁCZ 3 1 School of Geography, Earth & Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, United Kingdom; [email protected] 2 Department of Palaeontology and Geology, Hungarian Natural History Museum, POB 137, Budapest, H-1431 Hungary; [email protected] 3 Department of Palaeontology, Eötvös Loránd University, Pázmány P. sétány 1/C, Budapest, H-1117 Hungary; [email protected] (Manuscript received June 9, 2017; accepted in revised form January 16, 2018) Abstract: A carbonate carbon isotope curve from the Aalenian–Bathonian interval is presented from the Óbánya valley, of the Mecsek Mountains, Hungary. This interval is certainly less well constrained and studied than other Jurassic time slices. The Óbánya valley lies in the eastern part of the Mecsek Mountains, between Óbánya and Kisújbánya and provides exposures of an Aalenian to Lower Cretaceous sequence. It is not strongly affected by tectonics, as compared to other sections of eastern Mecsek of the same age. In parts, a rich fossil assemblage has been collected, with Bathonian ammonites being especially valuable at this locality. The pelagic Middle Jurassic is represented by the Komló Calcareous Marl Formation and thin-bedded limestones of the Óbánya Limestone Formation. These are overlain by Upper Jurassic siliceous limestones and radiolarites of the Fonyászó Limestone Formation. Our new data indicate a series of carbon isotope anomalies within the late Aalenian and early-middle Bajocian. -
Aalenian– Bathonian) of the Mecsek 2 Mountains, Southern Hungary 3 GREGORY D
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences Carbon cycle history through the Middle Jurassic (AalenianBathonian) of the Mecsek Mountains, Southern Hungary Price, GD http://hdl.handle.net/10026.1/11231 10.1515/geoca-2018-0007 Geologica Carpathica De Gruyter Open All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. 1 Carbon cycle history through the Middle Jurassic (Aalenian– Bathonian) of the Mecsek 2 Mountains, Southern Hungary 3 GREGORY D. PRICE1, ISTVÁN FŐZY2, and ANDRAS GALÁCZ3 4 5 1School of Geography, Earth & Environmental Sciences, University of Plymouth, Drake Circus, 6 Plymouth, PL4 8AA, United Kingdom ([email protected]) 7 2Department of Palaeontology and Geology, Hungarian Natural History Museum, POB 137, 8 Budapest, H-1431 Hungary ([email protected]) 9 3Department of Palaeontology, Eötvös Loránd University, Pázmány P. sétány 1/C, Budapest, H-1117 10 Hungary ([email protected]) 11 12 Corresponding Author: Gregory D. Price, email [email protected]; tel: +44 1752 584771; fax: 13 +44 1752 584776 14 15 Abstract. A carbonate carbon isotope curve from the Aalenian–Bathonian interval is presented 16 from the Óbánya valley, of the Mecsek Mountains, Hungary. This interval is certainly less well 17 constrained and studied than other Jurassic time slices.