Thematische Bibliographien / Biostratigrapy

Auswahl der wissenschaftlichen Literatur zum Thema „Biostratigrapy“

Autor: Grafiati
Veröffentlicht am 22. Juni 2024

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Zeitschriftenartikel zum Thema "Biostratigrapy"

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Al-Hahidi, Abdullah. „Planktonic Foraminiferal Biostratigrapy of Shiranish Formation in Makhmur Well No. (1), Makhmur Area, Northern Iraq“. Iraqi National Journal of Earth Sciences 10, Nr. 2 (28.12.2010): 19–28. http://dx.doi.org/10.33899/earth.2010.5516.

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Karmini, Mimin, und H. Yuniarto. „BIOSTRATIGRAFI FORAMINIFERA KUARTER PADA BOR INTI MD 982152 DAN 982155 DARI SAMUDRA HINDIA“. JURNAL GEOLOGI KELAUTAN 11, Nr. 2 (16.02.2016): 55. http://dx.doi.org/10.32693/jgk.11.2.2013.231.

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Dari bor inti pada EKSPEDISI IMAGES, di Samudra Hindia, telah diteliti sebanyak 21 percontoh sedimen dari lokasi MD 982152, dan 29 buah dari lokasi MD 982155 untuk kepentingan biostratigrafi berdasarkan analisis foraminifera plankton dalam interval 1,5 meter. Pada kedua penampang bor inti tersebut hanya dijumpai satu zona foraminifera plankton Kuarter, yaitu Zona Globorotalia truncatulinoides. Untuk MD 982152, zona ini bisa dibagi ke dalam dua subzona, yakni Subzona-subzona Globorotalia crassaformis hessi dan Globigerinella calida, sedangkan untuk MD 982155, zona tersebut bisa dibagi lagi ke dalam tiga subzona, yakni Subzona-subzona Globorotalia crassaformis hessi Globigerinella calida, dan Beella digitata. Kejadian yang signifikan di kedua penampang itu adalah Datum Pemunculan Pertama dari Globigerinella calida dan Pemunculan Akhir dari Globorotalia crassaformis hessi. Pada MD 982155, dijumpai Pemunculan Pertama dari Beella digitata. Kata kunci: foraminifera plankton, Kuarter, biostratigrafi, Samudra Hindia. From IMAGES Expedition in Indian Ocean, 21 samples from MD 982152, and 29 samples from MD 982155 had been studied for the purpose of biostratigraphy based on planktonic foraminifera within 1,5 meter interval. In both sections, only one Quaternary zone is found, namely Globorotalia truncatulinoides Zone. For MD 982152, that zone can be subdivided into two interval subzones e.g. Globorotalia crassaformis hessi and Globigerinella calida calida. However, in MD 982155 Globorotalia truncatulinoides Zone can be subdivided into three subzones namely, Globorotalia crassaformis hessi, Globigerinella calida calida, and Beella digitata Subzones. The planktonic foraminifera event revealed in both sections are the First Appearance Datum (FAD) of Globigerinella calida calida and the Last Appearance (LAD) of Globorotalia crassaformis hessi. In MD 982155 the FAD of Beella digitata is found. Keywords: planktonic foraminifera, Quaternary, biostratigraphy, Indian Ocean.
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Rizky, Aga, Ignatius Didi Setyawan und Sugeng Widada. „Analisis Fasies dan Lingkungan Pengendapan pada Formasi Pulau Balang Cekungan Kutai“. Jurnal Ilmiah Geologi PANGEA 9, Nr. 1sp (03.04.2023): 20. http://dx.doi.org/10.31315/jigp.v9i1sp.9405.

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Abstrak - Formasi Pulau Balang merupakan salah satu formasi penghasil hidrokarbon yang terdapat pada Cekungan Kutai. Penelitian ini dilakukan pada beberapa sumur pemboran yang mempunyai data Formasi Pulau Balang. Data yang digunakan dalam penelitian ini adalah data cutting dan data biostratigrafi pada Sumur X. Analisis yang dilakukan untuk menetukan lingkungan pengendapan pada penelitian ini adalah dengan melakukan interpretasi fasies menggunakan data biostratigrafi dan sifat fisik batuan menggunakan data cutting. Sampel yang digunakan pada Sumur X terdapat pada kedalaman 420 m - 2700 m, yang terdiri dari 251 sampel. Berdasarkan hasil interpretasi, didapatkan litologi berupa packstone pada kedalaman 420 m - 520 m dengan komposisi berupa fragmen koral dan fragmen bryozoan, dan beberapa foraminifera besar yang merupakan marga Operculina serta mempunyai pola kurva log gamma ray berupa funnel shape diinterpretasikan masuk dalam fasies distributary mouth bar dengan lingkungan pengendapan adalah delta front. Data biostratigrafi yang ditemukan pada kedalaman 520 m – 950 m yang mempunyai litologi berupa batupasir halus adalah pelecypod, gastropods dan bentik kecil foraminifera seperti cellanthus sp., amonia sp., dan pseudorotalia catilliformis, serta pola log berupa serrated dan bell shape diinterpretasikan termasuk dalam fasies distributary mouth bar dengan lingkungan pengendapan delta front. Interval kedalaman 960 m – 1635 m sedikit ditemukan Nannofossil pada litologi batupasir sedang brupa Cyclicargolithus abisectus dan C. Floridanus, Helicosphaera perchnielseniae, Discoaster exilis, Coronocyclus nitescens, C. Cf. Nitescens, Rhabdosphaera poculi dengan pola serrated, bell shape dan funnel shape diintepretasikan termasuk dalam fasies distributary channel dengan lingkunan pengendapan lower delta plain. Interval kedalaman 2071 m – 2210 m pada litologi batulanau ditemukan fosil foraminifera besar seperti Miogypsina sp., dan Lepidocyclina sp. dengan pola serrated, diinterpretasikan termasuk dalam fasies crevasse play yang terendapkan pada lingkungan upper delta plain. Interval kedalaman 2500 m – 2700 m ditemukan Nannoplankton yang terdiri dari Cyclicargelithus abisectus, C. Floridanus, Helicosphaera carteri, H. Esuphratis, Sphenolithus abies, Sphenolithus belemnos, dan Sphenolithus heteromorphus dengan pola funnel shape, diinterpretasikan masuk dalam fasies interdelta bay yang terendapkan pada lingkungan lower delta plain.Kata kunci: Formasi Pulau Balang, Cekungan Kutai, distributary mouth bar, distributary channel, crevasse play, interdelta bay, delta front, lower delta plain, upper delta plain.Abstract - The Pulau Balang Formation is one of the hydrocarbon-producing formations found in the Kutai Basin. This study was conducted on several drilling wells with data on the Pulau Balang Formation. The data used in this study are cutting data and biostratigraphy data from Well X. The analysis conducted to determine the depositional environment in this study is by interpreting the facies using biostratigraphy data and the physical properties of rocks using cutting data. The samples used in Well X are located at depths of 420 m - 2700 m, consisting of 251 samples. Based on the interpretation results, the lithology in the depth of 420 m - 520 m is packstone with a composition of coral fragments and bryozoan fragments, and some large foraminifera of the Operculina genus with a log gamma ray curve pattern of funnel shape interpreted as belonging to the distributary mouth bar facies with the depositional environment being a delta front. The biostratigraphy data found at a depth of 520 m - 950 m, which has a lithology of fine sandstone, is pelecypod, gastropods, and small benthic foraminifera such as Cellanthus sp., Ammonia sp., and Pseudorotalia catilliformis, as well as log patterns of serrated and bell shape interpreted as belonging to the distributary mouth bar facies with the depositional environment being a delta front. The depth interval of 960 m - 1635 m is slightly found Nannofossil in the lithology of medium sandstone in the form of Cyclicargolithus abisectus and C. Floridanus, Helicosphaera perchnielseniae, Discoaster exilis, Coronocyclus nitescens, C. Cf. Nitescens, and Rhabdosphaera poculi with serrated, bell shape, and funnel shape patterns are interpreted as belonging to the distributary channel facies with the depositional environment being a lower delta plain. The depth interval of 2071 m - 2210 m in the limestone lithology found large foraminifera fossils such as Miogypsina sp., and Lepidocyclina sp. with a serrated pattern, interpreted as belonging to the crevasse play facies deposited in the upper delta plain environment. The depth interval of 2500 m - 2700 m found Nannoplankton consisting of Cyclicargelithus abisectus, C. Floridanus, Helicosphaera carteri, H. Esuphratis, Sphenolithus abies, Sphenolithus belemnos, and Sphenolithus heteromorphus with a funnel shape pattern, interpreted as belonging to the interdelta bay facies deposited in the lower delta plain environment.Keywords: Pulau Balang Formation, Kutai Basin, distributary mouth bar, distributary channel, crevasse play, interdelta bay, delta front, lower delta plain, upper delta plain.
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Edwards, Lucy E. „Quantitative Biostratigraphy“. Short Courses in Paleontology 4 (1991): 39–58. http://dx.doi.org/10.1017/s2475263000002117.

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I find myself in the position of discussing a rather unfortunate misnomer. In the first place, topics that traditionally have been called “quantitative biostratigraphy” seldom deal with quantities of anything. In the second place, much of “quantitative biostratigraphy” deals more with chronostratigraphy and geochronology than with biostratigraphy. The operational concept is time, not fossil content, although, of course, the fossil content is the starting point. Nonetheless, the phrase “quantitative biostratigraphy” is quite firmly entrenched in the working vocabulary and I will use it here. I will focus on three very different techniques that all involve stratigraphic correlation based on the ranges of fossils.
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Mann, Keith Olin. „Teaching Biostratigraphy“. Journal of Geoscience Education 48, Nr. 2 (März 2000): 184–98. http://dx.doi.org/10.5408/1089-9995-48.2.184.

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Martinotti, Guido Menahem, und Shoshana Boehm. „Computerized biostratigraphy“. Newsletters on Stratigraphy 20, Nr. 1 (20.12.1988): 7–19. http://dx.doi.org/10.1127/nos/20/1988/7.

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Hadi, Mehdi, Lorenzo Consorti, Mohammad Vahidinia, Mohammad Parandavar und Marziyeh Zoraghi. „Ypresian Alveolina and calcareous nannofossils from the south Sabzevar area (Central Iran): biostratigraphic, taxonomic and paleobiogeographic implications“. Micropaleontology 67, Nr. 1 (2021): 31–52. http://dx.doi.org/10.47894/mpal.67.1.04.

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The Eocene carbonates of the south Sabzevar region in central Iran hold a rich Alveolina assemblage.Nine species including A. globula, Alveolina sp. 1, Alveolina aff. globula, A. regularis, A. globosa, A. pasticillata, A. laxa, A. pisiformis and A. cf. decipiens are identified through detailed analysis in thin section. The biostratigraphy obtained points to the early Ypresian Shallow Benthic Zones SBZ6 and partly SBZ7, indicating the occurrence of a lower Eocene carbonate system. The Alveolina biostratigraphy is correlated to the calcareous nannofossil biostratigraphy, and is assignable to the middle part of the NP10 Zone and especially with the CNE2 biozones. The evolutionary trends of A. globula and its dispersal through thewestern and central Neo-Tethys Ocean during theYpresian is here considered in relation with the occurrence of Alveolina sp. 1.
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Grahn, Y., und H. Nøhr-Hansen. „Chitinozoans from Ordovician and Silurian shelf and slope sequences in North Greenland“. Rapport Grønlands Geologiske Undersøgelse 144 (31.12.1989): 35–41. http://dx.doi.org/10.34194/rapggu.v144.8060.

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This first study on chitinozoans from Greenland has revealed representatives of twenty-two chitinozoan species recovered from Ordovician and Silurian beds in North Greenland. The Ordovician faunas are sirnilar to those described from North Arnerica, while the Silurian faunas are more sirnilar to those of Baltoscandia. Four distinct assemblages can be separated between Maysvillian - early Garnachian and Ludlow. The chitinozoan biostratigraphy is in agreement with that of the graptolites but differs from the conodont biostratigraphy.
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Simmons, Mike. „Biostratigraphy: Surviving Extinction“. PALAIOS 13, Nr. 3 (Juni 1998): 215. http://dx.doi.org/10.2307/3515446.

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Aitchison, Jonathan C., Noritoshi Suzuki, Martial Caridroit, Taniel Danelian und Paula Noble. „Paleozoic radiolarian biostratigraphy“. Geodiversitas 39, Nr. 3 (September 2017): 503–31. http://dx.doi.org/10.5252/g2017n3a5.

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Dissertationen zum Thema "Biostratigrapy"

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Shafique, Naseer Ahmed. „Spatial Biostratigraphy of NW Pakistan“. Miami University / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=miami991186162.

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Luo, Hui, und 羅煇. „Devonian radiolarian biostratigraphy of Southwest China“. Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2000. http://hub.hku.hk/bib/B3124211X.

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Doherty, Stephen James. „Wenlock graptolite biostratigraphy of North Wales“. Thesis, University of Portsmouth, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.424217.

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Robinson, Paul David. „Tertiary radiolarian biostratigraphy of coastal Ecuador“. Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261097.

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Luo, Hui. „Devonian radiolarian biostratigraphy of Southwest China“. Hong Kong : University of Hong Kong, 2000. http://sunzi.lib.hku.hk/hkuto/record.jsp?B22718862.

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Saunders, Kate Marie. „Silurian dendroid graptolites : taxonomy, palaeoecology and biostratigraphy“. Thesis, University of Portsmouth, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.343388.

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Roelofs, Brett Peter Ashworth. „Utilisation of microvertebrates in biostratigraphy and chemostratigraphy“. Thesis, Curtin University, 2016. http://hdl.handle.net/20.500.11937/48487.

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The utility of marine microvertebrate fossils for bio- and chemostratigraphy and subsequent correlation were tested on the exceptionally preserved Devonian reef complexes of the Canning Basin, Western Australia. Microvertebrates provided refined age ranges for restricted depositional environments unable to be dated using conodonts or ammonoids. In addition, the O-isotope signatures recovered from hypermineralised tissues within microvertebrate fossils enabled the reconstruction of palaeoenvironmental conditions, in addition to providing the basis for chemical stratigraphy.
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Leith, Thomas Leslie. „The role of coals and carbonaceous shale facies in the petroleum reservoir system : a case study from the Gullfaks Field, Norwegian North Sea“. Thesis, Heriot-Watt University, 2000. http://hdl.handle.net/10399/545.

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Smith, Giles A. „Palynology of the Jurassic/Cretaceous boundary interval in the Volga Basin, Russia“. Thesis, University of Bristol, 1999. http://hdl.handle.net/1983/a981fc30-fa69-4cf5-aae5-7290d2a489df.

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Hybertsen, Frida. „Distribution of Sabellidites (Annelida?) in the Basal Cambrian of the Digermulen Peninsula, Arctic Norway“. Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-325148.

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The Digermulen Peninsula, Arctic Norway, offers a unique section of late Ediacaran to Cambrian sediments in an almost complete succession within the Vestertana Group. The proposed annelidan fossil Sabellidites cambriensis is found here, within the Lower Breidvika Member and is believed to exist also in the underlying Manndrapselva Member of the Stáhpogieddi Formation. Three cycles are recognized from the Manndrapselva Member, the uppermost being the third cycle, and the sediment interval of interest for this study ranges from the third cycle of the Manndrapselva Member to the Lower Breidvika Member where the Ediacaran–Cambrian boundary is situated. The distribution of Sabellidites has been investigated in three different localities on the Digermulen Peninsula, and from two of these stratigraphical logs were made and the sections were documented with photographs. The logs were created over sediments from Locality 1: Bárdeluovttjohka and Locality 3: Manndrapselva in the interval of the top of the Manndrapselva Member and Lower Breidvika Member. Previous studies have shown that the stratigraphical distribution of Sabellidites is within the Lower Breidvika Member. New results presented in this study extended the temporal distribution downwards in the third cycle of the Manndrapselva Member and closer to the Ediacaran–Cambrian boundary. The boundary is indicated by the trace fossil Treptichnus pedum. A few samples, collected from the logged sections, were found below the T. pedum level, indicating late Ediacaran origin. Three samples were collected even further down, close to the base of the Manndrapselva log, but these could only loosely be identified as Sabellidites and further analysis is required on these specimens. The Sabellidites distribution range from the Digermulen Peninsula was briefly compared to other locations and a global correlation is possible. The results here indicate that Sabellidites is an excellent reference taxon for the terminal Ediacaran and early Cambrian and that the succession on the Digermulen Peninsula may be one of the most important for global correlation across the Ediacaran-Cambrian boundary.
På Digermulenhalvön i arktiska Norge finns en nästan helt oavbruten sektion av sediment från sen ediacara och tidig kambrium. Fossilet Sabellidites cambriensis, som tros tillhöra phylat Annelida, går att hitta här inuti sediment från det undre Breidvikaledet och det underliggande Manndrapselvaledet. De här två leden ingår i Vestertanagruppen. Tre cykler är identifierade från Manndrapselvaledet och den översta är den tredje cykeln. Distributionen av Sabellidites i de här sedimenten har undersökts i tre olika lokaler på Digermulenhalvön, och två biostratigrafiska loggar ritades och dokumenterades med foton. Tidigare har studier påvisat Sabellidites i det undre Breidvikaledet, men resultaten från den här studien visar att det går att hitta Sabellidites även i den tredje cykeln av Manndrapselvaledet vilket är längre ned i sedimentföljden, och således också äldre sediment som ligger nära gränsen mellan ediacara och kambrium, som är ett mycket intressant och omdiskuterat geologiskt tidsavsnitt. Gränsen indikeras av ett spårfossil vid namn Treptichnus pedum och resultat ifrån den här studien påvisar Sabellidites nedanför nivån för T. pedum. Det här förlänger spannet inom vilket man kan hitta Sabellidites och resultaten från Digermulenhalvön har jämförts med områden runt om i världen i ett försök att korrelera dem med varandra. Studien visar att en global korrelation är möjlig vilket gör Sabellidites till ett utmärkt referensfossil för undre kambrium och sektionen på Digermulenhalvön är exceptionellt bra för att undersöka förhållandena kring gränsen mellan ediacara och kambrium.
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Bücher zum Thema "Biostratigrapy"

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Rickards, Barrie. Bendigonian graptolites (Hemichordata) of Victoria. Melbourne: Museum ofAustralia, 1991.

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Bown, Paul R., Hrsg. Calcareous Nannofossil Biostratigraphy. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4902-0.

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R, Bown P., Hrsg. Calcareous nannofossil biostratigraphy. London: Chapman & Hall, 1998.

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Cao, Rui-ji, Zhang Wen-tang, Pei-ji Chen und Palmer Allison R, Hrsg. Biostratigraphy of China. Beijing, China: Science Press, 2003.

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R, Bown P., Hrsg. Calcareous nannofossil biostratigraphy. Dordrecht: Kluwer Academic, 1999.

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1940-, Wright Raymond M., und Robinson Edward 1934-, Hrsg. Biostratigraphy of Jamaica. Boulder, Colo: Geological Society of America, 1993.

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1957-, Long John A., Hrsg. Palaeozoic vertebrate biostratigraphy and biogeography. Baltimore: Johns Hopkins University Press, 1994.

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1957-, Long John A., Hrsg. Palaeozoic vertebrate biostratigraphy and biogeography. London: Belhaven, 1993.

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1956-, Powell A. J., Riding J. B, Geological Society of London und British Micropalaeontological Society, Hrsg. Recent developments in applied biostratigraphy. London: The Geological Society, 2005.

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G, Lucas Spencer, Cassinis Giuseppe, Schneider Joerg W und Geological Society of London, Hrsg. Non-marine permian biostratigraphy and biochronology. London: The Geological Society, 2006.

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Buchteile zum Thema "Biostratigrapy"

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Gygi, Reinhart A. „Biostratigraphy“. In Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany, 69–103. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7_4.

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Saraswati, Pratul Kumar, und M. S. Srinivasan. „Biostratigraphy“. In Micropaleontology, 157–69. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-14574-7_10.

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Aubry, Marie-Pierre. „Biostratigraphy“. In Encyclopedia of Scientific Dating Methods, 83–107. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_192.

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Aubry, Marie-Pierre. „Biostratigraphy“. In Encyclopedia of Scientific Dating Methods, 1–35. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6326-5_192-1.

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Denne, Richard A. „Biostratigraphy“. In Selective Neck Dissection for Oral Cancer, 1–20. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-02330-4_6-1.

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Berggren, William A., und Richard D. Norris. „Biostratigraphy“. In Smithsonian Contributions to Paleobiology, 8–10. Washington, D.C.: Smithsonian Institution Press, 1999. http://dx.doi.org/10.5479/si.00810266.85.8.

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Saraswati, Pratul Kumar. „Biostratigraphy“. In Larger Benthic Foraminifera Through Space and Time, 167–80. Cham: Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-57631-7_8.

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Gradstein, F. M. „Biochronology, Biostratigraphy“. In Encyclopedia of Marine Geosciences, 1–2. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6644-0_41-1.

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Gradstein, Felix. „Biochronology, Biostratigraphy“. In Encyclopedia of Marine Geosciences, 1–2. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_41-2.

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Gradstein, Felix M. „Biochronology, Biostratigraphy“. In Encyclopedia of Marine Geosciences, 55–56. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_41.

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Konferenzberichte zum Thema "Biostratigrapy"

1

Keller, Gerta. „BIOSTRATIGRAPHY AND IMPACT STRATIGRAPHY“. In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283457.

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2

W. Bailey, H., L. T. Gallagher und F. J. Gregory. „Sequence biostratigraphy of European chalks“. In EAPG/AAPG Special Conference on Chalk. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201407529.

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3

M. Gradstein, F. „Crunching Bugs' - Quantitative biostratigraphy for explorations“. In 55th EAEG Meeting. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609.201411727.

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4

Politova, N. V. „Geology of seas and oceans: Proceedings of XXIV International Conference on Marine Geology. Vol. I.“ In XXIV International Conference on Marine Geology. Shirshov Institute of Oceanology Publishing House, Russian Academy of Sciences, 2021. http://dx.doi.org/10.29006/978-5-6045110-4-6.

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The reports of marine geologists, geophysics, geochemists and other specialists of marine science at XXIV International Conference on Marine Geology in Moscow are published in four volumes. Volume I includes reports devoted to the problems of paleooceanology, paleoecology, biostratigraphy, cross correlation of deposits and of geoecology, pollution of the World Ocean.
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5

W. Hughes, Geraint, Osman Varol und Nigel P. Hooker and Raymond Enay. „New aspects of Saudi Arabian Jurassic biostratigraphy“. In GEO 2008. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.246.180.

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6

„Devonian Conodont Biostratigraphy of the Norilsk Area“. In Interexpo GEO-Siberia. Siberian State University of Geosystems and Technologies, 2018. http://dx.doi.org/10.18303/2618-981x-2018-1-224-227.

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7

Efremenko, Vsevolod D. „BELEMNITES AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS IN THE ANABAR REGION OF SIBERIA“. In All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Trofimuk Readings - 2021. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1251-2-23-26.

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This work contains the conclusions obtained during the study of new collections and generalization of previously published works on the Lower Cretaceous belemnites of the Anabar region. Particular attention is paid to the discussion of imperfection of the subdivision of the Lower Cretaceous by belemnites; it is necessary to clarify both the boundaries of biostratigraphic units and the choice of index species matching the objectives of biostratigraphy.
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8

Henderson, Charles M. „PERMIAN BIOSTRATIGRAPHY OF THE SHALLOW-WATER TAXON SWEETOGNATHUS“. In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281245.

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9

Crouch*, Erica M., Pi S. Willumsen und Denise Kulhanek. „Paleocene Dinoflagellate Cyst Biostratigraphy in Eastern New Zealand“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2202257.

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10

Vinnikovskaya, O. S., und M. Ivantsiv. „Application of Biostratigraphy to Improve the Geological Section“. In First Workshop on Far East Hydrocarbons 2011. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144336.

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Berichte der Organisationen zum Thema "Biostratigrapy"

1

McNeil, D. H. Phanerozoic Biostratigraphy. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/126951.

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2

Jennings, A. E., G. Vilks, B. Deonarine, A. Silis und N. Weiner. Foraminiferal biostratigraphy and paleoceanography. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212201.

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3

Jakobs, G., J. Palfy und P. L. Smith. L. Jurassic Ammonite Biostratigraphy, Q.c.i. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131212.

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4

Pohler, S. M. L., und M. J. Orchard. Ordovician conodont biostratigraphy, western Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131452.

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5

Williams, G. L., P. Ascoli, M. S. Barss, J. P. Bujak, E H Davies, R. A. Fensome und M A Williamson. Chapter 3: biostratigraphy and related studies. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/132698.

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6

White, J. M. Tertiary biostratigraphy, Queen Charlotte Basin, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122712.

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7

Silis, A. B. Late Quaternary foraminiferal biostratigraphy of Hudson Strait. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/208321.

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8

Ascoli, P., M. P. Avery, M. S. Barss, J. P. Bujak, E H Davies, P. A. Fensome, J K Hacquebard et al. Biostratigraphy and maturation data 6: selected wells. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210618.

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9

Ascoli, P., M. P. Avery, M. S. Barss, J. P. Bujak, E H Davies, P. A. Fensome, J K Hacquebard et al. Biostratigraphy and maturation data 5: selected wells. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210620.

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10

Ascoli, P., M. P. Avery, M. S. Barss, J. P. Bujak, E H Davies, P. A. Fensome, J K Hacquebard et al. Biostratigraphy and maturation data 7: selected wells. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210621.

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