Academic literature on the topic 'Biozonation'

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Journal articles on the topic "Biozonation"

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Berger, Jean-Pierre. "Redefinition of European Oligo - Miocene Charophyte Biozonation." Australian Journal of Botany 47, no. 3 (1999): 283. http://dx.doi.org/10.1071/bt97102.

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Recent studies concerning the Oligo–Miocene stratigraphy (35 to 5 million years ago) need the revision of the calibration of the European charophyte biozonation by Riveline et al. in 1996. Moreover, another charophyte biozonation elaborated in Spain by Feist et al. in 1994 also modifies this standard model. Presented here is a discussion and a possible solution to redefine the Standard European Charophyte biozonation during the Oligocene and Miocene.
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Noble, Paula, and Jonathan Aitchison. "Early Paleozoic radiolarian biozonation." Geology 28, no. 4 (April 2000): 367–70. http://dx.doi.org/10.1130/0091-7613(2000)028<0367:eprb>2.3.co;2.

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Noble, Paula, and Jonathan Aitchison. "Early Paleozoic radiolarian biozonation." Geology 28, no. 4 (2000): 367. http://dx.doi.org/10.1130/0091-7613(2000)28<367:eprb>2.0.co;2.

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Verniers, J., V. Nestor, F. Paris, P. Dufka, S. Sutherland, and G. Van Grootel. "A global Chitinozoa biozonation for the Silurian." Geological Magazine 132, no. 6 (November 1995): 651–66. http://dx.doi.org/10.1017/s0016756800018896.

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AbstractA global Chitinozoan biozonation for the Silurian Period is proposed. Each biozone is an interval range defined by the first occurrence of an index species, selected from well-defined species with a relatively short biostratigraphic range. To be included in the scheme, index species must have been recorded from at least two major Silurian palaeocontinents where usable Chitinozoa assemblages have been studied, that is, Avalonia—Baltica (which had already undergone collision by the Silurian), Laurentia, Gondwana and Southern China. Seventeen biozones are identified with seven in the Llandovery: the fragilis, postrobusta, electa, maennili, alargada, dolioliformis and longicollis biozones; four in the Wenlock: the margaritana, cingulata, pachycephala and lycoperdoides biozones; three in the Ludlow: the elongata, philipi and barrandei biozones; and three in the Přídolí: the kosovensis, elegans and superba biozones. Chronostratigraphic calibration is partly provided by reference to the range of the appropriate Chitinozoa index species in the global stratotype sections and points (GSSP) of the Silurian series, e.g. in Bohemia (Czech Republic) for the Přídolí and the Welsh Borderland in England for the Ludlow and part of the Wenlock. When this information was not available, independent biostratigraphic control was provided by calibration with graptolite biozones or in a few cases, conodont or trilobite biozonal schemes. The index and most characteristic species of each biozone are illustrated and their total stratigraphie range provided.
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Lirer, Fabrizio, Luca Maria Foresi, Silvia Maria Iaccarino, Gianfranco Salvatorini, Elena Turco, Claudia Cosentino, Francisco Javier Sierro, and Antonio Caruso. "Mediterranean Neogene planktonic foraminifer biozonation and biochronology." Earth-Science Reviews 196 (September 2019): 102869. http://dx.doi.org/10.1016/j.earscirev.2019.05.013.

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Zimmerman, Alexander N., Claudia C. Johnson, and P. David Polly. "Taxonomic and evolutionary pattern revisions resulting from geometric morphometric analysis of Pennsylvanian Neognathodus conodonts, Illinois Basin." Paleobiology 44, no. 4 (August 30, 2018): 660–83. http://dx.doi.org/10.1017/pab.2018.28.

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AbstractConodont fossils are highly valuable for Paleozoic biostratigraphy and for interpreting evolutionary change, but identifying and describing conodont morphologies, and characterizing gradual shape variation remain challenging. We used geometric morphometric (GM) analysis to conduct the first landmark-based morphometric analysis of the biostratigraphically useful conodont genus Neognathodus. Our objective is to assess whether previously defined morphotype groups are reliably distinct from one another. As such, we reevaluate patterns of morphologic change in Neognathodus P1elements, perform maximum-likelihood tests of evolutionary modes, and construct novel, GM-based biozonations through a Desmoinesian (Middle Pennsylvanian) section in the Illinois Basin. Our GM results record the entire spectrum of shape variability among Neognathodus morphotypes, thus alleviating the problem of documenting and classifying gradual morphologic transitions between morphotypes. Statistically distinct GM groups support previously established classifications of N. bassleri, N. bothrops, and N. roundyi. Statistically indistinct pairs of GM groups do not support literature designations of N. medadultimus and N. medexultimus, and N. dilatus and N. metanodosus, and we synonymize each pair. Maximum-likelihood tests of evolutionary modes provide the first statistical assessment of Neognathodus evolutionary models in the Desmoinesian. The most likely evolutionary models are an unbiased random walk or a general random walk. We name four distinct biozones through the Desmoinesian using GM results, and these align with previous biozonation structure based on the Neognathodus Index (NI), illustrating that Neognathodus-based biostratigraphic correlations would not change between GM or NI methods. The structural similarity between both biozonations showcases that determining GM-based biozones is not redundant, as this comparison validates using landmark-based GM work to construct viable biozonations for subsequent stratigraphic correlations. Although this study is limited to the Illinois Basin, our quantitative methodology can be applied broadly to test taxonomic designations of additional genera, interpret statistically robust evolutionary patterns, and construct valid biozones for this significant chordate group.
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Samuelsson, J., and J. Verniers. "Ordovician chitinozoan biozonation of the Brabant Massif, Belgium." Review of Palaeobotany and Palynology 113, no. 1-3 (December 2000): 105–29. http://dx.doi.org/10.1016/s0034-6667(00)00055-5.

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LÖFGREN, A. "Conodont biozonation in the upper Arenig of Sweden." Geological Magazine 137, no. 1 (January 2000): 53–65. http://dx.doi.org/10.1017/s0016756800003484.

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Conodont faunas from the Arenigian Lanna/Volkhov Stage in Baltoscandia have been the subject of intensive study, particularly during the last decade, and different biozonations based on them have been proposed. The application of some of these zones is discussed here. The present investigation is mainly based on 64 samples from ten sections in Sweden, but conodont collections from Bornholm (Denmark) and Tamsalu (Estonia) have also been studied. Lindström's (1971) concept of the upper Arenigian Microzarkodina parva Zone is essentially replaced by a revised Baltoniodus norrlandicus Zone. The zone corresponds closely to Bagnoli & Stouge's (1997) recently distinguished B. norrlandicus and Lenodus antivariabilis zones, which can be recognized in sections where a more detailed subdivision and correlation is possible under the names of the T. quadrangulum Subzone and the L. antivariabilis Subzone, respectively.
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Boomer, Ian D. "Lower Jurassic Ostracod Biozonation of the Mochras Borehole." Journal of Micropalaeontology 9, no. 2 (March 1, 1991): 205–18. http://dx.doi.org/10.1144/jm.9.2.205.

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Abstract. The extensive Lower Jurassic sequence at Mochras has yielded a diverse ostracod fauna which includes many new taxa. Poor preservation precludes a complete taxonomic review of this material although four new species (Cytherella praetoarcensis, Ogmoconcha convexa, Lophodentina striata and Oligocythereis? mochrasensis) are erected herein. Changes in the faunal composition and the rates of faunal turnover are briefly described. An ostracod biozonation is proposed for the section, comparison with established Lower Jurassic zonal schemes reveals that the present section is distinct from most other European sequences.
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Schönfeld, Joachim, and Jackie Burnett. "Biostratigraphical correlation of the Campanian–Maastrichtian boundary: Lägerdorf–Hemmoor (northwestern Germany), DSDP Sites 548A, 549 and 551 (eastern North Atlantic) with palaeobiogeographical and palaeoceanographical implications." Geological Magazine 128, no. 5 (September 1991): 479–503. http://dx.doi.org/10.1017/s001675680001863x.

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AbstractA correlation of the Campanian–Maastrichtian boundary is attempted using foraminiferal and nannoplankton data from two areas: the eastern North Atlantic and northwestern Germany. The Boreal benthic and Tethyan planktonic foraminiferal zonation schemes are applied to Site 548A, where both foraminiferal groups occur frequently. A direct comparison of both biozonations reveals that the base of the Maastrichtian, according to planktonic foraminifers, has to be placed in the Upper Campanian of the Boreal benthic foraminiferal biozonation, which concurs with the nannoplankton results. The Tethyan Middle and Upper Maastrichtian are probably equivalent to the Upper Maastrichtian in the Boreal sense. The bases of the Maastrichtian substages are thus diachronous between the Boreal and Tethyan realms. Palaeotemperatures (which were estimated using the oxygen isotopic composition of the Goban Spur chalks) indicate, in combination with palaeowind directions, that the faunal and floral distribution pattern recorded is the result of a stable, warm water outflow from the northwest European epicontinental seas through the Channel area to the Celtic Shelf sea and Goban Spur. This mechanism appears to have been a dominant separating factor of the Boreal and Tethyan bioprovinces on the western European Shelf.
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Dissertations / Theses on the topic "Biozonation"

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Afghah, Massih [Verfasser], and Heinrich [Akademischer Betreuer] Bahlburg. "Biozonation and biostratigraphic limits of the Tarbur formation around Shiraz (SW of Iran) / Massih Afghah. Betreuer: Heinrich Bahlburg." Münster : Universitäts- und Landesbibliothek der Westfälischen Wilhelms-Universität, 2011. http://d-nb.info/1017896364/34.

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Coiffant-Martin, Brigitte. "Contribution des rongeurs du néogène d'Algérie à la biochronologie mammalienne d'Afrique nord-occidentale." Nancy 1, 1991. http://www.theses.fr/1991NAN10165.

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Ce travail repose sur l'étude de vingt-deux nouveaux gisements de micromammifères du miocène et du pliocène d'Algérie orientale ayant livre dix-sept espèces nouvelles. Il aboutit à la révision des zramys et des paraethomys en Afrique du nord, permet de préciser l'origine du genre zramys et met en évidence l'existence de deux espèces de zramys dans un même site. Pour la première fois, les genres progonomys et paraethomys sont rencontrés dans le même gisement. Golunda et protolophiomys sont découverts au Maghreb, représentés par de nouvelles espèces. Le seul site attribuable au messénien en Afrique du nord fournit, avec ses formes d'origine essentiellement européenne (stephanomys, ruscinomys, apodemus gudrunae et castillomys), de nouvelles indications quant aux échanges fauniques du miocène terminal entre l'Europe et l'Afrique; de plus, la faune espagnole de salobrena semble devoir être considérée comme d'origine maghrébine. La connaissance des faunes du miocène moyen du nord de l'Afrique est désormais plus précise, et un nouveau genre de myocricetodontinae a pu y être décrit. Les principales périodes de renouvellement faunique sont mises en évidence, et la durée de vie des taxons miocènes est étudiée. Des précisions nouvelles sont données sur l'âge de divers gisements déjà connus dans le nord de l'Afrique. L'ensemble de ces résultats permet de distinguer de nouveaux niveaux repères, et de proposer pour l'Afrique nord-occidentale une biozonation fondée sur les micromammifères, ainsi que des corrélations avec les échelles bio chronologiques établies en Europe
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Le, Hérissé Alain. "Acritarches et kystes d'algues prasinophycees de l'ordovicien supérieur et du silurien de Gotland, Suède." Brest, 1988. http://www.theses.fr/1988BRES2012.

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Description des microfossiles a paroi organique, acritarches et kystes d'algues prasinophycees, recueillis dans l'ordovicien superieur et le silurien du gotland. Discussion sur les caracteristiques morphologiques, leur signification biologiques et affinites. Etablissement d'une biozonation pour la suede et correlation avec celles du domaine nord europeen. L'integration de l'evolution morphologique et des contraintes paleoecologiques et paleogeographiques devrait amener une plus grande precision stratigraphique pour les acritarches. Interpretation paleoecologique mettant entre autre en evidence le controle de la latitude sur la distribution des acritarches
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Books on the topic "Biozonation"

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Zhang, Shunxin. A new llandovery (early Silurian) conodont biozonation and conodonts from the Becscie, Merrimack, and Gun River formations, Anticosti Island, Québec. Lawrence, Kan: Allen Press, 2002.

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Book chapters on the topic "Biozonation"

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Rigo, Manuel, Michele Mazza, Viktor Karádi, and Alda Nicora. "New Upper Triassic Conodont Biozonation of the Tethyan Realm." In Topics in Geobiology, 189–235. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-68009-5_6.

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Kucenjak, Morana Hernitz, and Vlasta Premec Fucek. "Planktonic Foraminiferal Biozonation of the Oligocene in the Northern Adriatic Sea." In Springer Geology, 1115–18. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_213.

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Raffi, Isabella, Claudia Agnini, Jan Backman, Eliana Fornaciari, Domenico Rio, and Heiko Pälike. "A New Low- to Middle-Latitude Biozonation and Revised Biochronology of Palaeogene Calcareous Nannofossils." In Springer Geology, 137–41. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_28.

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Pérez Panera, Juan P., Francisco J. Parra, Rosa E. Navarrete, Christian Sánchez, Diana Daza, Manuel Rodriguez, and Mario Prince. "Turonian–Santonian Calcareous Nannofossil Biozonation for La Luna Formation, Middle Magdalena Valley Basin, Northern Colombia." In Advances in South American Micropaleontology, 46–66. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-02119-1_3.

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Saha, Sandip, Shiladri S. Das, and Subhronil Mondal. "Gastropod Biozonation for the Jurassic Sediments of Kutch and Jaisalmer Basins and Its Application in Interbasinal Correlation." In Mesozoic Stratigraphy of India, 333–72. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71370-6_12.

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Ben Nsir, Sana, Mabrouk Boughdiri, Ichrak Cherif, Néjib Bahrouni, Rafika Ferchichi, and Asma Zrelli. "Berriasian Ammonite and Calpionellid Associations from the North-South Range of Central Tunisia: Updated Biozonation, Regional Geodynamic Context and Paleobiogeography." In Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas, 83–86. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_20.

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Ferchichi, Rafika, Ichrak Cherif, Mabrouk Boughdiri, Sana Ben Nsir, Néjib Bahrouni, and Mohamed Faouzi Zagrarni. "First Calpionellid Biozonation of the Berriasian Reference Section of Jebel Ben Younes (Gafsa Basin, South Central Tunisia): Updated Age Attribution and Geodynamic Consequences." In Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas, 79–82. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_19.

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Masse, Jean Pierre, Consuelo Arias, and Lorenzo Vilas. "Stratigraphy and biozonation of a reference Aptian — Albian p.p. Tethyan carbonate platform succession: The Sierra del Carche series (oriental Prebetic zone — Murcia, Spain)." In New Aspects on Tethyan Cretaceous Fossil Assemblages, 201–21. Vienna: Springer Vienna, 1992. http://dx.doi.org/10.1007/978-3-7091-5644-5_12.

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"Calcareous Nannofossil Biozonation." In Cenozoic Foraminifera and Calcareous Nannofossil Biostratigraphy of the Niger Delta, 395–416. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-812161-0.00008-9.

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BOWMAN, ANDREW R., GARRY D. JONES (deceased), ROGER J. WITMER, and ANTHONY C. GARY. "Application of a Statistically Derived, Integrated Biozonation to a Deepwater Miocene Gulf of Mexico Field." In Geologic Problem Solving with Microfossils, 337–42. SEPM (Society for Sedimentary Geology), 2009. http://dx.doi.org/10.2110/sepmsp.093.337.

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Conference papers on the topic "Biozonation"

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Stolfus, Brittany M., Nicholas Jay Hogancamp, Bradley D. Cramer, James Day, Ryan J. Clark, and Stephanie A. Tassier-Surine. "A REVISED CONODONT BIOZONATION FOR THE KINDERHOOKIAN (LOWER MISSISSIPPIAN)." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338906.

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Laursen, G. V., S. Monibi, T. L. Allan, N. A. H. Pickard, A. Hosseiney, B. Vincent, Y. Hamon, F. S. P. van Buchem, A. Moallemi, and G. Druillion. "The Asmari Formation Revisited: Changed Stratigraphic Allocation and New Biozonation." In 1st International Petroleum Conference and Exhibition Shiraz 2009. Netherlands: EAGE Publications BV, 2009. http://dx.doi.org/10.3997/2214-4609.20145919.

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Beiranvand, Bijan, and Ebrahim Ghasemi Nejad. "Late Campanian to Paleocene Planktic Foraminiferal Biozonation for Izeh, the Zagros Basin, Iran." In GEO 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609-pdb.248.374.

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Reports on the topic "Biozonation"

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Gradstein, F. M., and M. Fearon. Stratcor, a new method for biozonation and correlation with application to exploration micropaleontology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128120.

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