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Cretaceous Boundary in Western Cuba (Sierra De Los Órganos)
GEOLOGICA CARPATHICA, JUNE 2013, 64, 3, 195—208 doi: 10.2478/geoca-2013-0014 Calpionellid distribution and microfacies across the Jurassic/ Cretaceous boundary in western Cuba (Sierra de los Órganos) RAFAEL LÓPEZ-MARTÍNEZ1, , RICARDO BARRAGÁN1, DANIELA REHÁKOVÁ2 and JORGE LUIS COBIELLA-REGUERA3 1Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Delegación Coyoacán, C.P. 04510, México D.F., México; [email protected] 2Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina G, 842 15 Bratislava, Slovak Republic; [email protected] 3Departamento de Geología, Universidad de Pinar del Río, Martí # 270, Pinar del Río, C.P. 20100, Cuba (Manuscript received May 21, 2012; accepted in revised form December 11, 2012) Abstract: A detailed bed-by-bed sampled stratigraphic section of the Guasasa Formation in the Rancho San Vicente area of the “Sierra de los Órganos”, western Cuba, provides well-supported evidence about facies and calpionellid distribution across the Jurassic/Cretaceous boundary. These new data allowed the definition of an updated and sound calpionellid biozonation scheme for the section. In this scheme, the drowning event of a carbonate platform displayed by the facies of the San Vicente Member, the lowermost unit of the section, is dated as Late Tithonian, Boneti Subzone. The Jurassic/Cretaceous boundary was recognized within the facies of the overlying El Americano Member on the basis of the acme of Calpionella alpina Lorenz. The boundary is placed nearly six meters above the contact between the San Vicente and the El Americano Members, in a facies linked to a sea-level drop. The recorded calpionellid bioevents should allow correlations of the Cuban biozonation scheme herein proposed, with other previously published schemes from distant areas of the Tethyan Domain. -
Redalyc.Salinites Grossicostatum (Imlay, 1939) and S. Finicostatum Sp. Nov. from the Latest Tithonian (Late Jurassic) of Northea
Boletín de la Sociedad Geológica Mexicana ISSN: 1405-3322 [email protected] Sociedad Geológica Mexicana, A.C. México Zell, Patrick; Stinnesbeck, Wolfgang Salinites grossicostatum (Imlay, 1939) and S. finicostatum sp. nov. from the latest Tithonian (Late Jurassic) of northeastern Mexico Boletín de la Sociedad Geológica Mexicana, vol. 68, núm. 2, 2016, pp. 305-311 Sociedad Geológica Mexicana, A.C. Distrito Federal, México Available in: http://www.redalyc.org/articulo.oa?id=94346152007 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Salinites grossicostatum and S. finicostatum sp. nov. from the latest Tithonian of northeastern Mexico 305 Boletín de la Sociedad Geológica Mexicana Volumen 68, núm. 2, 2016, p. 305-311 D GEOL DA Ó E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Salinites grossicostatum (Imlay, 1939) and S. finicostatum sp. nov. from the latest Tithonian (Late Jurassic) of northeastern Mexico Patrick Zell1,*, Wolfgang Stinnesbeck1 1 Institut für Geowissenschaften, Universität Heidelberg, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany. * [email protected] Abstract Based on our taxonomic revision of the ammonite Salinites grossicostatum from the uppermost Tithonian of the La Caja Formation at Puerto Piñones, in the state of Coahuila, northeastern Mexico, we suggest that some specimens described from other Tithonian sites of Cuba and Mexico assigned to S. grossicostatum belong to a new species, here presented as S. -
The Jurassic/Cretaceous Boundary and High Resolution Biostratigraphy
GEOLOGICA CARPATHICA, APRIL 2019, 70, 2, 153–182 doi: 10.2478/geoca-2019-0009 The Jurassic/Cretaceous boundary and high resolution biostratigraphy of the pelagic sequences of the Kurovice section (Outer Western Carpathians, the northern Tethyan margin) ANDREA SVOBODOVÁ1, , LILIAN ŠVÁBENICKÁ2, DANIELA REHÁKOVÁ3, MARCELA SVOBODOVÁ1, PETR SKUPIEN4, TIIU ELBRA1 and PETR SCHNABL1 1The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic; [email protected], [email protected], [email protected], [email protected] 2Czech Geological Survey, Klárov 131/3, 118 21 Prague, Czech Republic; [email protected] 3Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina G. Ilkovičova 6, 842 15 Bratislava, Slovakia; [email protected] 4Institute of Geological Engineering, VŠB — Technical University of Ostrava, 17. listopadu 15, 708 33 Ostrava-Poruba, Czech Republic; [email protected] (Manuscript received September 27, 2018; accepted in revised form March 12, 2019) Abstract: Microfacies and high resolution studies at the Kurovice quarry (Czech Republic, Outer Western Carpathians) on calpionellids, calcareous and non-calcareous dinoflagellate cysts, sporomorphs and calcareous nannofossils, aligned with paleomagnetism, allow construction of a detailed stratigraphy and paleoenvironmental interpretation across the Jurassic/Cretaceous (J/K) boundary. The Kurovice section consists of allodapic and micrite limestones and marlstones. Identified standard microfacies types SMF 2, SMF 3 and SMF 4 indicate that sediments were deposited on a deep shelf margin (FZ 3), with a change, later, into distal basin conditions and sediments (FZ 1). The sequence spans a stratigraphic range from the Early Tithonian calcareous dinoflagellate Malmica Zone, nannoplankton zone NJT 15 and magnetozone M 21r to the late Early Berriasian calpionellid Elliptica Subzone of the Calpionella Zone, nannoplankton NK-1 Zone and M 17r magnetozone. -
Remarks on the Tithonian–Berriasian Ammonite Biostratigraphy of West Central Argentina
Volumina Jurassica, 2015, Xiii (2): 23–52 DOI: 10.5604/17313708 .1185692 Remarks on the Tithonian–Berriasian ammonite biostratigraphy of west central Argentina Alberto C. RICCARDI 1 Key words: Tithonian–Berriasian, ammonites, west central Argentina, calpionellids, nannofossils, radiolarians, geochronology. Abstract. Status and correlation of Andean ammonite biozones are reviewed. Available calpionellid, nannofossil, and radiolarian data, as well as radioisotopic ages, are also considered, especially when directly related to ammonite zones. There is no attempt to deal with the definition of the Jurassic–Cretaceous limit. Correlation of the V. mendozanum Zone with the Semiforme Zone is ratified, but it is open to question if its lower part should be correlated with the upper part of the Darwini Zone. The Pseudolissoceras zitteli Zone is characterized by an assemblage also recorded from Mexico, Cuba and the Betic Ranges of Spain, indicative of the Semiforme–Fallauxi standard zones. The Aulacosphinctes proximus Zone, which is correlated with the Ponti Standard Zone, appears to be closely related to the overlying Wind hauseniceras internispinosum Zone, although its biostratigraphic status needs to be reconsidered. On the basis of ammonites, radiolarians and calpionellids the Windhauseniceras internispinosum Assemblage Zone is approximately equivalent to the Suarites bituberculatum Zone of Mexico, the Paralytohoplites caribbeanus Zone of Cuba and the Simplisphinctes/Microcanthum Zone of the Standard Zonation. The C. alternans Zone could be correlated with the uppermost Microcanthum and “Durangites” zones, although in west central Argentina it could be mostly restricted to levels equivalent to the “Durangites Zone”. The Substeueroceras koeneni Zone ranges into the Occitanica Zone, Subalpina and Privasensis subzones, the A. -
Numerical Criteria of Precise Delimitation of the Calpionellid Crassicollaria and Calpionella Zones in Relation to the Jurassic/Cretaceous System Boundary
GEOLOGICA BALCANICA, 24. 6, Sofia, Decem. 1994, p. 23-30 Numerical criteria of precise delimitation of the calpionellid Crassicollaria and Calpionella Zones in relation to the Jurassic/Cretaceous system boundary Iskra Lakova Geological !nstitttfl', Bulaarian Acadl'lll!f of Sciences, 1113 Sofia (Received 12 . 06. 1994; accrpted 21. 09. 1994) /1 . JlaKooa- Ko .w~ecmoeHHble Kpumepuu OA R 1110</HOZO onpeiJe.11'HUfl zpaHU t(bt Ate.?JCiJy Ka Ab nuoHe AAUO· HbtAtu 30IWAW Cra ssicollaria u Calpionella n C!lfi'JU c zpaHtt l( eii Ate:JKO!f 10 po t1 tt .III'AO-It. 8 CTaTbe npellCTaB neHbl CTaTH CTii'leCKHe .'laHHble 0 sepn!KaJJbHOM pacnpocrpaHelfloflf ll OTIIOC liTeJJbHOH 4<1CTOTe KaJibllHO· HeJJJJHil B .llBYX\feTpOBO~I HHTepBaJJe B fJJO)f(eHCKOH CBHTe B 3ana)lHbiX 5aJJKilHII.ll3X Ha rpaHMUe Me)f(.ll.Y 30HaMif Crassicollaria If Calpionella . n epeOIOTpeHbl lf3BeCTHble JlO CIIX nop KpMrepHH llJI!l npoBe.D.CHII!l Hlf)f(HeH rpaHMUbl 30 Hbl Ca/pionella. npeJtJJaraeTC!l onpeJleJJHTb 3TY rpaliHUbl Ha OCHOBaHHH MOpQJOJJO· rH4ecKoro M3~teBeHHH Calpionella alpina, 3KcnJJ03HH ccjlepH4ecKoi-i, 6oJtee MeJIKoif pa3IIOBH.'I.HOCTH 3TO· fO BH,!la, If yna,!lKe Y.ll•1HHeiiHOH, 6onee Kp y nHOii pa3HOBII.'I.HOCTH, KaK H Ha HC'Ie3HOBaHHH fOMeOMOpcpa Calpionella elli plica. noTsep)f(.D.aercH. 'ITO Crassicollaria brevis 11 Crassicollaria massutiniana TO)f(e HC- 4e3 a!OT npH 3TOi't rpaHIIUe HJIH He~IH OrO HH)f(e ee, HO ,.3KCHJI03HH" Bll,!la Ca/pione/la a[pina B UeJJOM B rp aHH4HOM HHTepsaJJe Be Ha6JJIOJiaeTC!l. Abstract. In thi s paper. -
Preliminary Geologic Map of the Greater Antilles and the Virgin Islands
Preliminary Geologic Map of the Greater Antilles and the Virgin Islands By Frederic H. Wilson, Greta Orris, and Floyd Gray Pamphlet to accompany Open-File Report 2019–1036 2019 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DAVID BERNHARDT, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Wilson, F.H., Orris, G., and Gray, F., 2019, Preliminary geologic map of the Greater Antilles and the Virgin Islands: U.S. Geological Survey Open-File Report 2019–1036, pamphlet 50 p., 2 sheets, scales 1:2,500,000 and 1:300,000, https://doi.org/10.3133/ofr20191036. ISSN 2331-1258 (online) Contents Introduction.....................................................................................................................................................1 Geologic Summary.........................................................................................................................................1 -
Environmental, Structural and Stratigraphical Evolution Carpathians
EESSESSE WWECAECA M. JAMRICH: Vápnité nanofosílie sarmatu (vrchného Reticulofenestra pseudoumbilicus (veľké variety); Holodiscolithus seravalu) Dunajskej a Viedenskej panvy Západných macroporus; Braarudosphaera bigelowii bigelowii, B. bigelowii Karpát “state of art” parvula, Sphenolithus abies. Hranica sarmat/panón je datovaná na 11,6 mil. rokov, korelovaná s hranicou seraval/tortón v medi- Katedra geológie a paleontológie Prírodovedeckej fakulty UK, Mlynská teránnej oblasti (Kováč et al., 2005). Sarmatské nanofosílie dolina, 842 15 Bratislava; [email protected] západokarpatského regiónu boli prvýkrát detailne preštudované vo vrte ŠVM-1 Tajná, v Dunajskej panve (Kováč et al., 2008). Vápnité nanofosílie, zvyšky morských rias, veľmi citlivo odrážajú Na báze sarmatu bola určená zóna Calcidiscus macintyrei s. l., klimatické a paleoceánografické zmeny a sú dôležité pri určovaní veku s podzónami: Calcidiscus macintyrei s. s.; paraakmé Calcidiscus sedimentov. V rámci Západných Karpát boli študované vápnité nano- macintyrei; Calcidiscus macintyrei s Perforocalcinella fusiformis. fosílie sarmatského veku z oblasti Dunajskej a Viedenskej panvy. Sarmat Vo vrchnom sarmate boli stanovené podzóny: Braarudosphaera je korelovaný s vrchnou časťou zóny NN6 Discoaster exilis a spodnou bigelowii parvula a Sphenolithus abies. Prvý rozsiahly výskum NN7 zónou Discoaster kugleri (Martini, 1971). Sarmat v centrálnej vápnitých nanofosílií sarmatského veku Viedenskej panvy bol Paratetýde korešponduje s vrchným seravalom v mediteránnej oblasti; uskutočnený v rámci multidisciplinárneho štúdia sedimentov vrtov konkom a spodným besarabom východnej Paratetýdy. K primárnym situovaných v oblasti Malacky a Jakubov. Koreláciou definovaných biostratigrafickým charakteristikám spoločenstiev vápnitých nanofosílií spoločenstiev vápnitých nanofosílií s foraminiferami bolo možné patrí absencia Sphenolithus heteromorphus, čo umožňuje vyčlenenie stanoviť predbežnú stratigrafickú pozíciu a paleoekologické biozóny vápnitých nanofosílií NN6 a prvý objav Discoaster kugleri, interpretácie. -
Maalaoui ACTA LAYAUT
Acta Geologica Polonica, Vol. 66 (2016), No. 1, pp. 43–58 DOI: 10.1515/agp-2016-0002 The lower and middle Berriasian in Central Tunisia: Integrated ammonite and calpionellid biostratigraphy of the Sidi Kralif Formation KAMEL MAALAOUI1, 2 and FOUAD ZARGOUNI 1 1 Department of Geology, Faculty of Sciences of Tunis, Science University of Tunisia, Tunis 2092 El Manar-I, Tunisia. 2 Geological Survey, National Office of Mines.24, Street of Energy, 2035-Charguia-Tunis.BP: 215-10801Tunis Cedex- Tunisia. E-mails: [email protected]; [email protected] ABSTRACT : Maalaoui, K. and Zargouni, F. 2016. The lower and middle Berriasian in Central Tunisia: Integrated ammonite and calpionellid biostratigraphy of the Sidi Kralif Formation. Acta Geologica Polonica, 66 (1), 43–58. Warszawa. The lower and middle Berriasian sedimentary succession of the Sidi Kralif Formation has been a subject of bios- tratigraphic study in two key sections in Central Tunisia. Our contribution is an attempt to better define the basal Berriasian interval, between the Berriasella jacobi Zone and the Subthurmannia occitanica Zone. Zonal schemes are established using ammonites and calpionellids, and these permit correlation with other regions of Mediterranean Tethys and beyond. The use of biomarkers afforded by microfossil groups has allowed charac- terization and direct correlation with four widely accepted calpionellid sub-zones, namely Calpionella alpina, Remaniella, Calpionella elliptica and Tintinopsella longa. The two ammonite zones of Berriasella jacobi and of Subthurmannia occitanica are recognised on the basis of their index species. The parallel ammonite and cal- pionellid zonations are useful as a tool for correlation and calibration in time and space, thus allowing a better definition of a J/K boundary. -
Tethyan Calpionellids in the Neuquen Basin (Argentine Andes), Their
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/317574255 Tethyan calpionellids in the Neuquén Basin (Argentine Andes), their significance in defining the Jurassic/Cretaceous boun.... Article in Journal of South American Earth Sciences · June 2017 DOI: 10.1016/j.jsames.2017.06.007 CITATIONS READS 4 254 6 authors, including: Rafael López-Martínez M. Beatriz Aguirre-Urreta Universidad Nacional Autónoma de México University of Buenos Aires 29 PUBLICATIONS 49 CITATIONS 166 PUBLICATIONS 2,198 CITATIONS SEE PROFILE SEE PROFILE Marina Lescano Andrea Concheyro National Scientific and Technical Research C… University of Buenos Aires 31 PUBLICATIONS 140 CITATIONS 90 PUBLICATIONS 648 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Uplifting of the southern Central Andes from the late Cretaceous to the present. View project Caracterización del margen occidental de Chilenia y su evolución durante el Orógeno Colisional Chánico (Devónico superior-Carbonífero inferior), Andes Centrales Argentinos (TORANDES) View project All content following this page was uploaded by Rafael López-Martínez on 30 June 2017. The user has requested enhancement of the downloaded file. Journal of South American Earth Sciences 78 (2017) 116e125 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Tethyan calpionellids in the Neuquen Basin (Argentine Andes), their significance -
9Th International Congress on the Juras Ic Ys Em, Jaipur, India Abstracts
9th International Congress on the Juras ic ys em, Jaipur, India Abstracts 9th International Congress on the Jurassic System, Jaipur, India Abstracts Dhirendra K. Pandey, Franz T. Fiirsich & Matthias Alberti (Eds.) Beringeria Special Issue 8 - Erlangen 2 014 Cover photographs Front: The facade of the Hawa Mahal or Palace of Winds in Jaipur. Back: A mural in the Nahargarh Fort near Jaipur. Addresses of the editors: DHIRENDRA K. PANDEY, Department of Geology, University of Rajasthan, Jaipur, 302004, India; E-mail: [email protected] FRANZ T. FiiRSICH, GeoZentrum Nordbayern, Fachgruppe PaUioumwelt der Friedrich-Alexander Universitat Erlangen-Niirnberg, Loewenichstr. 28, D-91054 Erlangen, Germany; E-mail: franz. [email protected] MATTHIAS ALBERTI, Institut fiir Geowissenschaften, Christian-Albrechts-Universitat zu Kiel, Ludewig-Meyn-Str. 10, D-24118 Kiel, Germany; E-mail: [email protected] Beringeria, Special Issue 8: 213 pages Erlangen, 01.12.2013 ISSN 093 7-0242 Publisher: Freunde der nordbayerischen Geowissenschaftene. V. Editorial Office: GeoZentrum Nordbayern, Fachgruppe Palaoumwelt, Friedrich-Alexander-Universitat Erlangen-N iirnberg Loewenichstr. 28, D-91054 Erlangen, Germany. Print: Tiwari Printers Jhotwara,Jaipur, 302012, India. 9th International Congress on the Jurassic System - Abstracts 3 Contents A sequence stratigraphic interpretation of the contact between the Lathi and 11 Jaisalmer formations, Jaisalmer Basin, Rajasthan, India by A. Agarwal, A. S. Kale & P. B. Jadhav Ammonites of the family Mayaitidae SPATH, 1928 from the Oxfordian of Kachchh, 13 western India by M. Alberti, D. K. Pandey,M. Hethke & F. T. Fiirsich Stratigraphy, facies analysis and reservoir characterization of the Upper Jurassic 16 Arab "C", Qatar, Arabian Gulf by H. Al-Saad & F. -
15. Calcisphaerulidae and Capionellidae from the Upper
15. CALCISPHAERULIDAE AND CALPIONELLIDAE FROM THE UPPER JURASSIC AND LOWER CRETACEOUS OF DEEP SEA DRILLING PROJECT HOLE 416A, MOROCCAN BASIN Hans M. Bolli, Department of Geology, Swiss Federal Institute of Technology, Zurich, and University of Zurich, Switzerland INTRODUCTION scope, the individual crystallites making up the layers cannot satisfactorily be distinguished. By the study of Upper Jurassic and Lower Cretaceous Calcisphaerul- isolated Calcisphaerulidae with the scanning electron idae and Calpionellidae were recovered from the Mo- microscope (SEM), shape and arrangement of the crys- roccan Basin, Hole 416A, between Cores 8 and 53 (Fig- tallites forming the individual layers provide an impor- ure 1). Most of the Calcisphaerulidae specimens are of tant additional criterion in Calcisphaerulidae taxon- the spherical Pithonella type, of which the species P. omy. thayeri Bolli, P. gustafsoni Bolli, P. sp. cf. P. sphaerica SEM investigations of isolated Calcisphaerulidae (Kaufmann), and P. sp. E are here distinguished. Fur- (Bolli, 1974, 1978a, b) indicate that the following fac- ther, Calcisphaerulidae tests which are distinctly pear tors influence the initial preservation of tests and our shaped also occur, although much less frequently. Pear- ability to identify them: (a) recrystallization or replace- shaped tests previously have been reported by Keupp ment of the original crystallites forming the test; (b) ef- (1977) as Pithonella piriformis, on the basis of SEM fects of corrosion on crystallites forming the test wall by views of broken limestone surfaces of the Upper Juras- CaCO3 dissolution. sic Solnhofener Plattenkalk. The characteristic pear- The inner space of the test may, under given condi- shaped tests differ so markedly from the spherical to tions, either remain hollow or become filled, often with elongate forms of Pithonella, as do the heart-shaped a very dense crystalline calcite core, as in the Hole 416A tests of Bonettocardiella, that the new genus Pirumella specimens described here. -
EGU2009-2119, 2009 EGU General Assembly 2009 © Author(S) 2009
Geophysical Research Abstracts, Vol. 11, EGU2009-2119, 2009 EGU General Assembly 2009 © Author(s) 2009 Final results on the Jurassic-Cretaceous boundary in the Gresten Klippenbelt (Austria): Macro-, micro-, nannofossils, isotopes, geochemistry, susceptibility, gamma-log and palaeomagnetic data as environmental proxies of the early Penninic Ocean history A. Lukeneder (1), E. Halásová (2), A. Kroh (1), S. Mayrhofer (3), P. Pruner (4), D. Reháková (2), P. Schnabl (4), and M. Sprovieri (5) (1) Geological and Palaeontological Department, Natural History Museum, Burgring 7, A-1010 Vienna, Austria ([email protected] / fax: +34 (1) 52177 - 459 / Phone: +34 (1) 52177 251), (2) Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina G-1, 842 15 Bratislava, Slovakia, (3) Department of Palaeontology, Geozentrum, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria ([email protected]), (4) Institute of Geology, Academy of Sciences of the Czech Republic v.v.i., Rozvojová 269, 165 00, Praha 6 – Lysolaje, Czech Republic, (5) Institute for marine and coastal environment (IAMC-CNR), Calata Porta di Massa (Interno Porto di Napoli), 80133, Napoli, Italy Jurassic to Lower Cretaceous pelagic sediments are well known to form a major element of the northernmost tectonic units of the Gresten Klippenbelt (Lower Austria). The Penninic Ocean was a side tract of the Central Atlantic Oceanic System intercalated between the European and the Austroalpine plates. Its opening started during the Mid Jurrasic, as rifting of the of the oceanic crust between the European and the Austroalpine plates. The turnover of the deposition on the European shelf (Helvetic Zone) from deep-water siliciclastics into pelagic carbonates is correlated with the deepening of this newly arising ocean.