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Artykuły w czasopismach na temat „Biochronology”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

McRoberts, Christopher A. "Biochronology of Triassic bivalves." Geological Society, London, Special Publications 334, no. 1 (2010): 201–19. http://dx.doi.org/10.1144/sp334.9.

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2

Cirilli, Omar, Helena Machado, Joaquin Arroyo-Cabrales, et al. "Evolution of the Family Equidae, Subfamily Equinae, in North, Central and South America, Eurasia and Africa during the Plio-Pleistocene." Biology 11, no. 9 (2022): 1258. http://dx.doi.org/10.3390/biology11091258.

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Studies of horse evolution arose during the middle of the 19th century, and several hypotheses have been proposed for their taxonomy, paleobiogeography, paleoecology and evolution. The present contribution represents a collaboration of 19 multinational experts with the goal of providing an updated summary of Pliocene and Pleistocene North, Central and South American, Eurasian and African horses. At the present time, we recognize 114 valid species across these continents, plus 4 North African species in need of further investigation. Our biochronology and biogeography sections integrate Equinae

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3

Forniaciari, Eliana, Claudia Agnini, Rita Catanzariti, Domenico Rio, Eleonora M. Bolla, and Elisabetta Valvasoni. "Mid-Latitude calcareous nannofossil biostratigraphy and biochronology across the middle to late Eocene transition." Stratigraphy 7, no. 4 (2010): 229–64. http://dx.doi.org/10.29041/strat.07.4.01.

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Calcareous nannofossil biostratigraphic studies are presented from 11 sedimentary sections, nine located in the Mediterranean area and one each from the middle latitude North and South Atlantic, respectively. The distribution patterns of middle to late Eocene calcareous nannofossils are studied by means of quantitative and semiquantitative methods. Our main goal was to test the biostratigraphic reproducibility of bioevents used in two classical standard biozonations, and to introduce new biostratigraphically useful biohorizons, resulting in a series of new middle latitude biostratigraphic even

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4

Fara, Emmanuel. "Estimates of phylogeny and biochronology." Revista Brasileira de Paleontologia 7, no. 3 (2004): 301–10. http://dx.doi.org/10.4072/rbp.2004.3.01.

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5

Lucas, Spencer G. "Tetrapod Footprint Biostratigraphy and Biochronology." Ichnos 14, no. 1-2 (2007): 5–38. http://dx.doi.org/10.1080/10420940601006792.

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6

Lindsay, Everett. "Eurasian mammal biochronology: an overview." Palaeogeography, Palaeoclimatology, Palaeoecology 133, no. 3-4 (1997): 117–28. http://dx.doi.org/10.1016/s0031-0182(97)00083-7.

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7

Hills, Scott J., and Hans R. Thierstein. "Plio-Pleistocene calcareous plankton biochronology." Marine Micropaleontology 14, no. 1-3 (1989): 67–96. http://dx.doi.org/10.1016/0377-8398(89)90032-7.

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8

Jorissen, F. J., A. Asioli, A. M. Borsetti, et al. "Late Quaternary central Mediterranean biochronology." Marine Micropaleontology 21, no. 1-3 (1993): 169–89. http://dx.doi.org/10.1016/0377-8398(93)90014-o.

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9

Di Stefano, Agata, Niccolo Baldassini, Isabella Raffi, et al. "Neogene-Quaternary Mediterranean calcareous nannofossil biozonation and biochronology: A review." Stratigraphy 20, no. 4 (2023): 259–302. http://dx.doi.org/10.29041/strat.20.4.02.

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The present study focuses on calcareous nannofossil biostratigraphy of the last 23 Myr in the Mediterranean region and is intended as a review paper in which an updated zonation is presented. This includes the improvements in biostratigraphic classification achieved in the last decades. The proposed biozonal scheme incorporates the biochronologic data derived from the integration of biostratigraphically useful events with radiometric datings, magnetostratigraphy and astronomically tuned cyclostratigraphy. This biochronology directly derives by previous compilations and includes improved data a

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10

Colombero, Simone, Giulio Pavia, and Giorgio Carnevale. "Messinian rodents from Moncucco Torinese, NW Italy: palaeobiodiversity and biochronology." Geodiversitas 36, no. 3 (2014): 421–75. https://doi.org/10.5252/g2014n3a4.

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Colombero, Simone, Pavia, Giulio, Carnevale, Giorgio (2014): Messinian rodents from Moncucco Torinese, NW Italy: palaeobiodiversity and biochronology. Geodiversitas 36 (3): 421-475, DOI: 10.5252/g2014n3a4, URL: http://dx.doi.org/10.5252/g2014n3a4

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11

Spassov, Nikolaï, Tzanko Tzankov, and Denis Geraads. "Late Neogene stratigraphy, biochronology, faunal diversity and environments of South-West Bulgaria (Struma River Valley)." Geodiversitas 28, no. 3 (2006): 477–98. https://doi.org/10.5281/zenodo.4665418.

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Spassov, Nikolaï, Tzankov, Tzanko, Geraads, Denis (2006): Late Neogene stratigraphy, biochronology, faunal diversity and environments of South-West Bulgaria (Struma River Valley). Geodiversitas 28 (3): 477-498, DOI: 10.5281/zenodo.4665418

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12

Fernández López, Sixto. "Taphonomic concepts for a theoretical biochronology." Spanish Journal of Palaeontology 6, no. 1 (2022): 37. http://dx.doi.org/10.7203/sjp.25035.

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13

Lucas, Spencer G. "Global Triassic tetrapod biostratigraphy and biochronology." Palaeogeography, Palaeoclimatology, Palaeoecology 143, no. 4 (1998): 347–84. http://dx.doi.org/10.1016/s0031-0182(98)00117-5.

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14

Lucas, Spencer G. "Global Permian tetrapod biostratigraphy and biochronology." Geological Society, London, Special Publications 265, no. 1 (2006): 65–93. http://dx.doi.org/10.1144/gsl.sp.2006.265.01.04.

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15

Lucas, Spencer G., and Adrian P. Hunt. "Permian tetrapod footprints: biostratigraphy and biochronology." Geological Society, London, Special Publications 265, no. 1 (2006): 179–200. http://dx.doi.org/10.1144/gsl.sp.2006.265.01.08.

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16

Hunt, Adrian P. "Non-marine Cretaceous biostratigraphy and biochronology." Episodes 36, no. 1 (2013): 73–74. http://dx.doi.org/10.18814/epiiugs/2013/v36i1/013.

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17

Lucas, Spencer G. "Fossil vertebrates, biostratigraphy, biochronology and chronostratigraphy." Palaeogeography, Palaeoclimatology, Palaeoecology 667 (June 2025): 112890. https://doi.org/10.1016/j.palaeo.2025.112890.

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18

Martin, Robert A., and Thomas S. Kelly. "Biostratigraphy and biochronology of late Cenozoic North American rodent assemblages." Palaeontologia Electronica 26, no. 2 (2023): 1–27. https://doi.org/10.26879/1303.

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Martin, Robert A., Kelly, Thomas S. (2023): Biostratigraphy and biochronology of late Cenozoic North American rodent assemblages. Palaeontologia Electronica (a29) 26 (2): 1-27, DOI: 10.26879/1303, URL: http://dx.doi.org/10.26879/1303

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19

Gradstein, Felix, Anna Waskowska, and Larisa Glinskikh. "The First 40 Million Years of Planktonic Foraminifera." Geosciences 11, no. 2 (2021): 85. http://dx.doi.org/10.3390/geosciences11020085.

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We provide a biochronology of Jurassic planktonic foramininfera, using first order linkage to ammonite and nannofossil stratigraphy and geochronology. This enigmatic and understudied group of microfossils occurred from middle Toarcian through Tithonian time, from ~180 to ~143 Ma; its origin is unknown. There are three genera: Globuligerina, Conoglobigerina and Petaloglobigerina. The genus Globuligerina, with a smooth to pustulose test surface texture appeared in Toarcian (late Early Jurassic) and Conoglobigerina, with a rough reticulate test surface texture in Oxfordian (early Late Jurassic) t

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20

Mecozzi, Beniamino, and Flavia Strani. "Equids from the late Middle Pleistocene to Early Holocene of the Apulia Peninsula (southern Italy): reassessment of their taxonomy and biochronology." Geodiversitas 44, no. 2 (2022): 17–45. https://doi.org/10.5252/geodiversitas2022v44a2.

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Mecozzi, Beniamino, Strani, Flavia (2022): Equids from the late Middle Pleistocene to Early Holocene of the Apulia Peninsula (southern Italy): reassessment of their taxonomy and biochronology. Geodiversitas 44 (2): 17-45, DOI: 10.5252/geodiversitas2022v44a2

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21

Tesakov, Alexey S., Pavel Frolov, Alexandra Simakova, et al. "Plio-Pleistocene Small Mammal-Based Biochronology of Eastern Anatolia and Transcaucasus." Quaternary 7, no. 4 (2024): 42. http://dx.doi.org/10.3390/quat7040042.

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The known Plio-Pleistocene mammalian record, mainly represented by small mammals, and its biotic and geological context in the vast region of Eastern Turkey and Transcaucasus provides a sound base for regional biochronology. Recently obtained faunal associations and the main evolutionary lineages found in the region support direct correlations to the European (ELMA/MN/MQ) and the Eastern European (faunal complexes/MQR-MNR) biochronological systems. Important data on palynology, aquatic and terrestrial mollusks, and magnetostratigraphy integrate the reviewed material into a robust local biochro

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22

Maridet, Olivier. "Postprint of : Maridet, O., 2002. Proposition of dating a Miocene Alpine tectonic event using mammal biochronology: example of the Four karst filling. Geodinamica Acta 15, 179–184. doi: 10.1080/09853111.2002.10510751." Geodinamica Acta 15 (April 14, 2002): 179–84. https://doi.org/10.1080/09853111.2002.10510751.

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Postprint of the manuscript published in Geodinamica acta: Maridet, O., 2002. Proposition of dating a Miocene Alpine tectonic event using mammal biochronology: example of the Four karst filling. Geodinamica Acta 15, 179–184. https://doi.org/10.1080/09853111.2002.10510751

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23

May, Steven R. "Proboscidea from Miocene strata of the Texas Coastal Plain with a reappraisal of the biochronology of the Fleming Group." Palaeontologia Electronica 27, no. 3 (2024): 1–46. https://doi.org/10.26879/1404.

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May, Steven R. (2024): Proboscidea from Miocene strata of the Texas Coastal Plain with a reappraisal of the biochronology of the Fleming Group. Palaeontologia Electronica (a55) 27 (3): 1-46, DOI: 10.26879/1404, URL: https://doi.org/10.26879/1404

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24

Petronio, Carmelo, Luca Bellucci, Edoardo Martiinetto, Luca Pandolfi, and Leonardo Salari. "Biochronology and palaeoenvironmental changes from the Middle Pliocene to the Late Pleistocene in Central Italy." Geodiversitas 33, no. 3 (2011): 485–517. https://doi.org/10.5252/g2011n3a4.

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Petronio, Carmelo, Bellucci, Luca, Martiinetto, Edoardo, Pandolfi, Luca, Salari, Leonardo (2011): Biochronology and palaeoenvironmental changes from the Middle Pliocene to the Late Pleistocene in Central Italy. Geodiversitas 33 (3): 485-517, DOI: 10.5252/g2011n3a4, URL: http://dx.doi.org/10.5252/g2011n3a4

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25

Bibi, Faysal. "Tragelaphus nakuae: evolutionary change, biochronology, and turnover in the African Plio-Pleistocene." Zoological Journal of the Linnean Society 162, no. 3 (2011): 699–711. https://doi.org/10.1111/j.1096-3642.2010.00691.x.

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Bibi, Faysal (2011): Tragelaphus nakuae: evolutionary change, biochronology, and turnover in the African Plio-Pleistocene. Zoological Journal of the Linnean Society 162 (3): 699-711, DOI: 10.1111/j.1096-3642.2010.00691.x, URL: http://dx.doi.org/10.1111/j.1096-3642.2010.00691.x

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26

Vucetich, María Guiomar, Cecilia M. Deschamps, Emma Carolina Vieytes, and Claudia I. Montalvo. "Late Miocene capybaras from Argentina: Skull anatomy, taxonomy, evolution, and biochronology." Acta Palaeontologica Polonica 59, no. 3 (2012): 517–35. https://doi.org/10.4202/app.2012.0063.

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Vucetich, María Guiomar, Deschamps, Cecilia M., Vieytes, Emma Carolina, Montalvo, Claudia I. (2014): Late Miocene capybaras from Argentina: Skull anatomy, taxonomy, evolution, and biochronology. Acta Palaeontologica Polonica 59 (3): 517-535, DOI: 10.4202/app.2012.0063, URL: http://dx.doi.org/10.4202/app.2012.0063

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27

Missiaen, Pieter, and Philip D. Gingerich. "New early Eocene tapiromorph perissodactyls from the Ghazij Formation of Pakistan, with implications for mammalian biochronology in Asia." Acta Palaeontologica Polonica 57, no. 1 (2011): 21–34. https://doi.org/10.4202/app.2010.0093.

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Missiaen, Pieter, Gingerich, Philip D. (2012): New early Eocene tapiromorph perissodactyls from the Ghazij Formation of Pakistan, with implications for mammalian biochronology in Asia. Acta Palaeontologica Polonica 57 (1): 21-34, DOI: 10.4202/app.2010.0093, URL: http://dx.doi.org/10.4202/app.2010.0093

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Alroy, John. "Appearance event ordination: a new biochronologic method." Paleobiology 20, no. 2 (1994): 191–207. http://dx.doi.org/10.1017/s0094837300012677.

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The fundamental goal of biochronology is ordering taxonomic first and last appearance events. The most useful biochronologic data are of the form “the first appearance event of one taxon predates the last appearance event of a second taxon” (FAE < LAE). FAE < LAE data sets are unusually reliable because they converge on a unique solution with greater sampling. The fact that the FAE of one taxoni< the LAE of another taxonjalways can be inferred either ifiis found lower thanjin a stratigraphic section, or ifiandjco-occur in at least one taxonomic list. Thus, FAE < LAE data accurately

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29

Yin, Jiarun. "Comment on Zhang et al. New Age Constraints of the Bilong Co Oil Shale in the Qiangtang Basin, Northern Tibet: Evidence from In Situ U–Pb Dating and Palaeontology. Minerals 2024, 14, 246." Minerals 14, no. 8 (2024): 777. http://dx.doi.org/10.3390/min14080777.

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Two species in question, Tiltoniceras sp. (Zhang et al., 2024, p. 6, Figure 5A,B,E) and “Hildoceratidae sp.”, belong to the misidentification of ammonites, the conclusion drawn by Zhang et al. (2024) lacks reliable evidence from ammonite biochronology to support the U–Pb Dating.

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30

Álvarez-Sierra, María Ángles, Israel García-Paredes, Verónica Hernández-Ballarín, et al. "Models of historical biogeography and continental biochronology." Spanish Journal of Palaeontology 28, no. 2 (2020): 129. http://dx.doi.org/10.7203/sjp.28.2.17847.

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31

Lucas, Spencer G. "Permian tetrapod biochronology, correlation and evolutionary events." Geological Society, London, Special Publications 450, no. 1 (2017): 405–44. http://dx.doi.org/10.1144/sp450.12.

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32

Cuenca-Bescós, Gloria, Juan Rofes, Juan Manuel López-García, et al. "Biochronology of Spanish Quaternary small vertebrate faunas." Quaternary International 212, no. 2 (2010): 109–19. http://dx.doi.org/10.1016/j.quaint.2009.06.007.

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33

Kučera, Michal. "Biochronology of the mid-Pliocene Sphaeroidinella event." Marine Micropaleontology 35, no. 1-2 (1998): 1–16. http://dx.doi.org/10.1016/s0377-8398(98)00016-4.

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Stoetzel, Emmanuelle. "Late Cenozoic micromammal biochronology of northwestern Africa." Palaeogeography, Palaeoclimatology, Palaeoecology 392 (December 2013): 359–81. http://dx.doi.org/10.1016/j.palaeo.2013.09.026.

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35

Bradbury, J. P., and W. N. Krebs. "Fossil Continental Diatoms: Paleolimnology, Evolution, and Biochronology." Short Courses in Paleontology 8 (1995): 119–38. http://dx.doi.org/10.1017/s2475263000001458.

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Diatoms are golden brown algae (class Bacillariophyceae) whose cellular contents are enclosed between two valves or shells of silica. They are classified into groups with radial symmetry (centric diatoms) and axial symmetry (pennate diatoms). The latter are subdivided as raphid and araphid diatoms according to the presence or absence of raphes (slit-like structures) that allow diatoms to move along firm surfaces. Many centric and some araphid diatoms are planktonic, maintained by turbulence in the limnetic region of a lake, whereas raphid diatoms live on the lake bottom or are attached to obje

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36

Lirer, Fabrizio, Luca Maria Foresi, Silvia Maria Iaccarino, et al. "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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KOIZUMI, ITARU. "Diatom biochronology for late Cenozoic northwest Pacific." Journal of the Geological Society of Japan 91, no. 3 (1985): 195–211. http://dx.doi.org/10.5575/geosoc.91.195.

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38

Sandberg, Charles A., and Willi Ziegler. "Devonian conodont biochronology in geologic time calibration." Senckenbergiana lethaea 76, no. 1-2 (1996): 259–65. http://dx.doi.org/10.1007/bf03042852.

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Tiwari, B. N. "Kanisamys Sivalensis, a Late Miocene Rhizomyid Rodent from Siwalik of Garhwal Himalaya, India." Journal Geological Society of India 37, no. 6 (1991): 595–98. http://dx.doi.org/10.17491/jgsi/1991/370608.

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Abstract Rodent molar recovered from the Kalagarh area has been identified as a 'rhizomyid Kanisamys sivalensis Wood, 1937. Utilizing the rhizomyid biochronology developed on the basis of large samples from Pakistan Siwalik, the Kalagarh faunal assemblage having K. sivalensis is assigned a Late Miocene age range of 9 to 7 Ma.

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40

Butler, Richard J., Oliver W. M. Rauhut, Michelle R. Stocker, and Robert Bronowicz. "Redescription of the phytosaurs Paleorhinus ('Francosuchus') angustifrons and Ebrachosuchus neukami from Germany, with implications for Late Triassic biochronology." Zoological Journal of the Linnean Society 170, no. 1 (2014): 155–208. https://doi.org/10.1111/zoj.12094.

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Butler, Richard J., Rauhut, Oliver W. M., Stocker, Michelle R., Bronowicz, Robert (2014): Redescription of the phytosaurs Paleorhinus ('Francosuchus') angustifrons and Ebrachosuchus neukami from Germany, with implications for Late Triassic biochronology. Zoological Journal of the Linnean Society 170 (1): 155-208, DOI: 10.1111/zoj.12094, URL: http://doi.wiley.com/10.1111/zoj.12094

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Boessenecker, Sarah J., Robert W. Boessenecker, and Jonathan H. Geisler. "Youngest record of the extinct walrus Ontocetus emmonsi from the Early Pleistocene of South Carolina and a review of North Atlantic walrus biochronology." Acta Palaeontologica Polonica 63, no. 2 (2018): 279–86. https://doi.org/10.4202/app.00454.2018.

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Boessenecker, Sarah J., Boessenecker, Robert W., Geisler, Jonathan H. (2018): Youngest record of the extinct walrus Ontocetus emmonsi from the Early Pleistocene of South Carolina and a review of North Atlantic walrus biochronology. Acta Palaeontologica Polonica 63 (2): 279-286, DOI: 10.4202/app.00454.2018, URL: http://dx.doi.org/10.4202/app.00454.2018

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42

Krebs, William N., J. Platt Bradbury, and Edward Theriot. "Neogene and Quaternary Lacustrine Diatom Biochronology, Western USA." PALAIOS 2, no. 5 (1987): 505. http://dx.doi.org/10.2307/3514621.

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Raia, Pasquale, and Lorenzo Rook. "The Evolution of Large Mammal Communities: Beyond Biochronology." Annales Zoologici Fennici 51, no. 1-2 (2014): 57–65. http://dx.doi.org/10.5735/086.051.0207.

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Callomon, John H. "Jurassic ammonite biochronology of Greenland and the Arctic." Bulletin of the Geological Society of Denmark 41 (November 30, 1994): 128–37. http://dx.doi.org/10.37570/bgsd-1995-41-12.

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􀀬e standard biochronological chronostratigraphy of the Phanerozoic and of its conjugate time-scale has been refined over a century and a half by a process of top-down subdivision in a hierarchy of successively smaller units. The finest units currently accepted, at the seventh level of the hierarchy, are the Subzones widely used in the Jurassic, thanks to that System's exceptional guide-fossils, its ammonites. But the time-resolution even at this level is not yet at the limits attainable through biostratigraphy. The ultimate observable is a characteristic fauna! horizon, defined as a fossilifer

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45

Alroy, John. "Diachrony of mammalian appearance events: Implications for biochronology." Geology 26, no. 1 (1998): 23. http://dx.doi.org/10.1130/0091-7613(1998)026<0023:domaei>2.3.co;2.

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46

Moffat, I. W., R. M. Bustin, and G. E. Rouse. "Biochronology of selected Bowser Basin strata; tectonic significance." Canadian Journal of Earth Sciences 25, no. 10 (1988): 1571–78. http://dx.doi.org/10.1139/e88-150.

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Recent evaluation and reinterpretation of fossil floral and faunal data more clearly define the ages of strata exposed in the Groundhog Coalfield and the surrounding Bowser Basin of north-central British Columbia. In the Groundhog Coalfield, Bowser Lake Group strata consist of an overall coarsening-upwards cycle divisible into four informal stratigraphic units, which are, from oldest to youngest, the Jackson, Currier, McEvoy, and Devils Claw units. The section has an unconformable relationship with underlying Bajocian Spatsizi marine shales, volcanics, and arenaceous sediments. Marine macrofos

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Erbajeva, Margarita A., Ursusla B. Göhlich, Lawrence J. Flynn, and Nadia V. Alexeeva. "Overview of Cenozoic Eurasian lagomorph biochronology and radiation." Fossil Imprint 80, no. 2 (2024): 312–18. https://doi.org/10.37520/fi.2024.023.

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Ochotonidae and Leporidae are two living families belonging to the Order Lagomorpha, an ancient group of mammals originating in the Paleogene of Asia. Those families diversified in the Oligocene and Miocene. More primitive stem lagomorphs inhabited Asia during a time of tropical environmental conditions. A Mid-Cenozoic change towards more continental and arid climate in parallel with Antarctic glaciation resulted in significant reorganisation of paleoenvironmental and climatic conditions in Asia and involved the opening of terrestrial connections between Asia, Europe, and North America, allowi

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Goričan, Špela, Luis O’Dogherty, Peter O. Baumgartner, Elizabeth S. Carter, and Atsushi Matsuoka. "Mesozoic radiolarian biochronology – current status and future directions." Revue de Micropaléontologie 61, no. 3-4 (2018): 165–89. http://dx.doi.org/10.1016/j.revmic.2018.08.001.

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Erbajeva, M. A. "The ochotonids of Eurasia: Biochronology and taxonomic diversity." Biology Bulletin 43, no. 7 (2016): 729–35. http://dx.doi.org/10.1134/s1062359016070062.

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Callomon, John H. "Palaeontological methods ofstratigraphy and biochronology: Some introductory remarks." Geobios 27 (December 1994): 16–30. http://dx.doi.org/10.1016/s0016-6995(94)80122-3.

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