Gotowe bibliografie tematyczne / Biochronology

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Gotowa bibliografia na temat „Biochronology”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 9 marca 2023

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Artykuły w czasopismach na temat "Biochronology"

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McRoberts, Christopher A. "Biochronology of Triassic bivalves". Geological Society, London, Special Publications 334, nr 1 (2010): 201–19. http://dx.doi.org/10.1144/sp334.9.

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Cirilli, Omar, Helena Machado, Joaquin Arroyo-Cabrales, Christina I. Barrón-Ortiz, Edward Davis, Christopher N. Jass, Advait M. Jukar i in. "Evolution of the Family Equidae, Subfamily Equinae, in North, Central and South America, Eurasia and Africa during the Plio-Pleistocene". Biology 11, nr 9 (24.08.2022): 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 taxonomic records with their chronologic and geographic ranges recognizing regional biochronologic frameworks. The paleoecology section provides insights into paleobotany and diet utilizing both the mesowear and light microscopic methods, along with calculation of body masses. We provide a temporal sequence of maps that render paleoclimatic conditions across these continents integrated with Equinae occurrences. These records reveal a succession of extinctions of primitive lineages and the rise and diversification of more modern taxa. Two recent morphological-based cladistic analyses are presented here as competing hypotheses, with reference to molecular-based phylogenies. Our contribution represents a state-of-the art understanding of Plio-Pleistocene Equus evolution, their biochronologic and biogeographic background and paleoecological and paleoclimatic contexts.
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Fara, Emmanuel. "Estimates of phylogeny and biochronology". Revista Brasileira de Paleontologia 7, nr 3 (30.12.2004): 301–10. http://dx.doi.org/10.4072/rbp.2004.3.01.

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Lucas, Spencer G. "Tetrapod Footprint Biostratigraphy and Biochronology". Ichnos 14, nr 1-2 (styczeń 2007): 5–38. http://dx.doi.org/10.1080/10420940601006792.

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Lindsay, Everett. "Eurasian mammal biochronology: an overview". Palaeogeography, Palaeoclimatology, Palaeoecology 133, nr 3-4 (październik 1997): 117–28. http://dx.doi.org/10.1016/s0031-0182(97)00083-7.

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Hills, Scott J., i Hans R. Thierstein. "Plio-Pleistocene calcareous plankton biochronology". Marine Micropaleontology 14, nr 1-3 (maj 1989): 67–96. http://dx.doi.org/10.1016/0377-8398(89)90032-7.

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Jorissen, F. J., A. Asioli, A. M. Borsetti, L. Capotondi, J. P. de Visser, F. J. Hilgen, E. J. Rohling, K. van der Borg, C. Vergnaud Grazzini i W. J. Zachariasse. "Late Quaternary central Mediterranean biochronology". Marine Micropaleontology 21, nr 1-3 (kwiecień 1993): 169–89. http://dx.doi.org/10.1016/0377-8398(93)90014-o.

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Fernández López, Sixto. "Taphonomic concepts for a theoretical biochronology". Spanish Journal of Palaeontology 6, nr 1 (11.08.2022): 37. http://dx.doi.org/10.7203/sjp.25035.

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Lucas, Spencer G. "Global Triassic tetrapod biostratigraphy and biochronology". Palaeogeography, Palaeoclimatology, Palaeoecology 143, nr 4 (listopad 1998): 347–84. http://dx.doi.org/10.1016/s0031-0182(98)00117-5.

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Lucas, Spencer G. "Global Permian tetrapod biostratigraphy and biochronology". Geological Society, London, Special Publications 265, nr 1 (2006): 65–93. http://dx.doi.org/10.1144/gsl.sp.2006.265.01.04.

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Rozprawy doktorskie na temat "Biochronology"

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Peleo-Alampay, Alyssa M. "Miocene and oligocene calcareous nannofossils : biochronology and paleoceanography /". Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1997. http://wwwlib.umi.com/cr/ucsd/fullcit?p9823695.

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Mou, Yun. "Biochronology and magnetostratigraphy of the Pliocene Panaca Formation, southeast Nevada". Diss., The University of Arizona, 1999. http://hdl.handle.net/10150/284594.

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About 2,500 specimens of small mammal fossils were collected from 10 localities in the Pliocene Panaca Formation in Meadow Valley, southeast Nevada. The most common taxa are cricetid and heteromyid rodents, and lagomorphs. Twenty-seven species, including five new species, were recognized from the fauna. A new genus of microtine rodent, Nevadomys, including three new species, N. fejfari, N. lindsayi, and N. downsi, is recognized. Nevadomys was probably derived from the Hemphillian Paramicrotoscoptes. Repomys minor n. sp. is another new species of high-crowned cricetid that was detected in the Panaca local fauna. With abundant upper and lower third molars of Repomys, it was possible to amend the diagnoses of genus Repomys. The fifth new species recognized from the fauna is a shrew, Paranotiosorex panacaensis n. gen. and sp. Enamel microstructure of molars of the microtine rodents Mimomys panacaensis and Nevadomys n. gen. from the fauna were examined under the scanning electronic microscope. Mimomys panacaensis shows the same schmelzmuster among different populations. Nevadomys has a more primitive schmelzmuster compared to Mimomys panacaensis. Both its leading and trailing edges are entirely composed of radial enamel. The assemblage of small mammal fossils suggests that the Panaca local fauna represents the early Blancan land mammal age. The first appearance datum of Mimomys panacaensis is suggested as the beginning of Blancan land mammal age, and the absolute age of the lowest stratigraphic datum of M. panacaensis in the Panaca Formation is interpolated from magnetostratigraphy and is considered as the age of the Hemphillian-Blancan boundary. The magnetostratigraphy of the Panaca Formation in Meadow Valley is established based on four sections in the basin. The ash in the Rodent Hill section was dated at 4.64 +/- 0.03 Ma, which constrains the correlation of the reversed polarity magnetozone in the Rodent Hill section to the C3n.2r in the Geomagnetic Polarity Time Scale (GPTS). The other three sections are correlated to the Rodent Hill section based on the ashes. The Panaca Formation in Meadow Valley was deposited from 4.50--5.30 Ma, and the Hemphillian-Blancan boundary is around 4.95 Ma, close to the termination of Thvera Subchron in the GPTS.
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Boudadi-Maligne, Myriam. "Les canis pléistocènes du sud de la France : approche biosystématique, évolutive et biochronologique". Thesis, Bordeaux 1, 2010. http://www.theses.fr/2010BOR14126/document.

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L’étude des faunes du Quaternaire s’inscrit dans une dynamique de connaissance des paléoenvironnements et est de ce fait nécessaire pour mieux cerner les contraintes environnementales qui ont rythmé la dispersion des hominidés sur l’ensemble des continents. Le genre Canis, autour duquel nous avons axé ce travail de recherche, présente la particularité d’être resté constamment présent en Europe occidentale depuis son apparition, il y a plus de trois millions d’années, jusqu’à aujourd’hui. Cette constance fait de lui, malgré son caractère ubiquiste, un excellent témoin de l’évolution des paléoenvironnements.A travers l’analyse de la variabilité des populations actuelles et l’étude de dix séries fossiles du Sud de la France couvrant le Pléistocène, de nouveaux éléments de discussion sont avancés sur l’évolution des représentants du genre. Nos résultats, couplés à l’analyse critique des données bibliographiques nous ont dès lors permis de proposer une nouvelle phylogénie. Cette dernière permet non seulement de mieux cerner les phases d’apparition et de dispersion des différentes espèces du genre Canis, mais également de démontrer son potentiel biochronologique. Ainsi, trois grandes phases dans l’évolution du genre ont pu être mises en évidence. La transition de ces espèces est corrélée à de grands événements de l’histoire des faunes quaternaires (bioevent) et autorise de ce fait l’utilisation de cette phylogénie à des fins biochronologiques ainsi qu’une discussion autour des relations entre ces espèces et les paléocommunautés animales et humaines
Quaternary mammals form an important part of the material available for researchers focusing on paleoenvironmental reconstructions. Their study is thus often used to infer the environmental constraints that set the pace of human dispersal through the world. The genus Canis, main subject of this thesis, is present in Western Europe since its origin three million years ago. This continuous presence makes it a good candidate as a paleoenvironmental proxy, even when considering its ecological plasticity.The study of ten fossil sequences from Southern France spanning the Pleistocene, coupled with the analysis of the variability of modern populations, bring new insights on the evolution of the members of this lineage. Our results, once confronted to previous studies, allowed us to propose a new phylogeny. This new framework permits a better understanding of the apparition and disappearance of the different species, but also demonstrates the biochronological potential of the Canis genus. Three major phases have been identified in its evolutionary history. The transition between the different Canids is correlated with major events in the history of quaternary mammals (bioevent). Thus, its phylogeny can be used for biochronological purposes and has to be considered in the bigger debates that focus on the interactions between animal communities and human groups
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Warr, Ginette Louise. "Chronology of the Western Limeworks australopithecine site, Makapansgat, South Africa : Magnetostratigraphy, biochronology and implications for hominin evolution". Thesis, University of Liverpool, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.507590.

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Travouillon, Kenny James Biological Earth &amp Environmental Sciences Faculty of Science UNSW. "Palaeoecological and biochronological studies of Riversleigh, world heritage property, Oligo-Miocene fossil localities, north-western Queensland, Australia". Publisher:University of New South Wales. Biological, Earth & Environmental Sciences, 2008. http://handle.unsw.edu.au/1959.4/41305.

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Riversleigh, World Heritage Property, located in North-western Queensland, Australia, contains over 200 fossil bearing localities from the Oligo-Miocene. The study presented here aims at finding new methods to improve the accuracy of palaeoecological and biochronological studies and describe the palaeoenvironmental and chronological settings of the Riversleigh fossil deposits. One of the methods developed in this thesis, Minimum Sample Richness (MSR), determines the minimum number of species that must be present in a fauna to allow meaningful comparisons using multivariate analyses. Using MSR, several Riversleigh localities were selected for a palaeoecological study using the cenogram method to determine the palaeoenvironment during the Oligo-Miocene. Finally, the Numerical ages method was used to refine the relative ages of the Riversleigh localities and a re-diagnosis of the Riversleigh Systems is proposed.
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Blaj, Teodora. "Late Eocene through Oligocene calcareous nannofossils from the paleo-equatorial Pacific Ocean – taxonomy, preservation history, biochronology and evolution". Doctoral thesis, Stockholm : Department of geology and geochemistry, Stockholm university, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-27600.

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Chandler, Robert Baron. "High resolution ammonite biostratigraphy and biochronology of the Aalenian and Bajocian stages (Middle Jurassic) of Dorset and Somerset, UK". Thesis, University of Portsmouth, 2018. https://researchportal.port.ac.uk/portal/en/theses/high-resolution-ammonite-biostratigraphy-and-biochronology-of-the-aalenian-and-bajocian-stages-middle-jurassic-of-dorset-and-somerset-uk(ac6722c9-0bbc-44a5-a9d8-2f99fb46b75f).html.

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The Inferior Oolite Formation of southern England is one of the foundations and testing grounds for the biostratigraphy of the Aalenian, Bajocian and lowermost Bathonian stages of the Middle Jurassic. The successions are highly discontinuous both vertically and laterally, comprising thin, lenticular deposits initially seemingly of limited use for standard chronostratigraphy. The beds are highly fossiliferous and are the source of many nominal genera and species of the classical literature introduced by S.S. Buckman. Publications herein represent a lifetime's work and incorporate research that focuses on the re-exposure, collecting and recording of the stratigraphical succession of many historical locations. This thesis reexamines, refines and advances the understanding of the biostratigraphy of the Inferior Oolite ammonite assemblages of Dorset and Somerset and is an important resource for comparison with many areas worldwide and for which this author provides commentary. Critical assessment is made of new, large, in situ, collections of well-preserved specimens made by the author, supported by data and evaluation against types in several museums. New taxa are erected accordingly. Specimens have been prepared using state of the art methods that allow evaluation of the complete shells, stages of growth and sexual dimorphism. The precise levels from which almost all of Buckman's Inferior Oolite specimens came is now known and this has enabled the variability of the fauna at discrete levels to be assessed, and has eliminated many ambiguities in the literature, to select those names that are useful and to decide which must be abandoned. Interpretation is made of patterns of ammonite migration, provincialism and Middle Jurassic biogeography. Distinguishable biohorizon lists present the biostratigraphy of the ammonites alongside correlation charts. Presently (2017), in the British Aalenian, there are 18. In the Lower Bajocian, there are 30 and the Upper Bajocian has 11 with 3 faunal horizons identified that require further study. Only the earliest Bathonian strata are considered and 3 horizons are recognised to date. It is therefore possible to discriminate 62 biohorizons in Dorset and Somerset for strata of the Aalenian-lowest Bathonian.
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TOMIDA, YUKIMITSU. "SMALL MAMMAL FOSSILS AND CORRELATION OF CONTINENTAL DEPOSITS, SAFFORD AND DUNCAN BASINS, ARIZONA (GILA CONGLOMERATE, MAGNETOSTRATIGRAPHY, BIOCHRONOLOGY, BLANCAN AGE, TAXONOMY)". Diss., The University of Arizona, 1985. http://hdl.handle.net/10150/188105.

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Fossil bearing continental deposits, the Gila Conglomerate, of the Safford and Duncan Basins, Arizona were correlated with the magnetic polarity time scale by means of magnetostratigraphy and biochronology of mammalian fossils. Within the Safford Basin, the Bear Springs section with a middle Blancan fauna is correlated with the lower or upper Gauss chron; the 111 Ranch section with a middle to late Blancan fauna is correlated with the upper Gauss to early Matuyama chrons; and the San Simon Power Line section with probably a latest Blancan fauna is correlated with the early Matuyama chron. In the Duncan Basin, the Duncan section with a middle Blancan fauna is correlated with the middle Gauss chron; the Pearson Mesa section with a middle Blancan fauna is correlated with the Upper Gauss chron; and the Country Club section with a middle Blancan fauna is correlated with the latest Gilbert to early Gauss chrons or from the middle Gauss to the earliest Matuyama chrons. A late Blancan fauna is not recognized in the Duncan Basin at least within the study area, whereas the Gila Conglomerate in the Safford Basin includes deposits and fauna of the latest Blancan (latest Pliocene) age. A minimum of 37 taxa of small mammals are recognized among the approximately 1,600 specimens from the Gila Conglomerate of the Safford and Duncan Basins. Three new rodent species are described; they are Pappogeomys (Cratogeomys) sansimonensis, new species; Reithrodontomys galushai, new species; and Repomys arizonensis, new species. One new combination of genus and species, Hypolague virginiae, is described. In the Safford Basin, a minimum of 26 small mammal taxa are now recognized in the 111 Ranch fauna, of which three genera (Dipodomys, Peromyscus, and Repomys) are new records to the fauna; a minimum of 6 taxa of small mammals are recognized and described for the first time in the San Simon Power Line fauna. In the Duncan Basin, a minimum of 15 small mammal taxa are recognized and described for the first time.
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Mahboubi, Salamet. "Les rongeurs du miocène supérieur et terminal d'Afrique nord-occidentale : biochronologie, magnétostratigraphie, biogéographie et paléoenvironnements". Thesis, Poitiers, 2014. http://www.theses.fr/2014POIT2323/document.

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L'Afrique nord-occidentale, ou le Maghreb, occupe une position géographique toute particulière car bien que partie intégrante du continent africain, elle possède une façade septentrionale intégrée au domaine méditerranéen et un domaine méridional semi-désertique ou désertique. Dans un premier lieu, des études paléomagnétiques et biostratigraphiques basées sur la faune de rongeurs ont été effectuées sur des dépôts continentaux de deux bassins algériens (Tafna et El Eulma). L'étude magnétostratigraphique réalisée dans ce travail a permis de dater avec précision les différents gisements fossilifères et de les corréler avec les autres bassins néogènes d'Afrique du Nord.Dans la seconde partie, les nouvelles prospections paléontologiques dans le bassin d'Aït Kandoula au Maroc méridional ont amené à découvrir trois gisements fossilifères datés du Miocène terminal. Ces gisements ont livré une riche faune de micromammifères associés à des restes de grands mammifères. L'étude systématique des micromammifères et plus particulièrement des rongeurs des deux gisements AF12-1 et AF12-2 a permis d'identifier des taxons qui ont des affinités avec ceux d'Europe sud-occidentale. Ces deux nouveaux sites ont fourni de nouvelles indications quant aux échanges de faunes entre l'Afrique et l'Europe. Le genre Stephanomys est notamment signalé pour la première fois au Maroc. L'étude biochronologique couplée avec l'étude magnétostratigraphique a permis de bien dater ces gisements, apportant ainsi des indications fiables quant à la chronologie de différentes phases d'échanges fauniques entre l'Afrique nord-occidentale et l'Europe sud-occidentale. Les premiers échanges fauniques ont eu lieu 0,25 Ma avant la crise de salinité messinienne. En outre, certains taxons identifiés dans AF12-2 (Myocricetodon, Protatera, Atlantoxerus) se révèlent utiles comme indicateurs paléoenvironnementaux, attestant des conditions climatiques chaudes et sèches
North-western Africa, or the Maghreb, occupies a special geographic position, being an integral part of the African continent, but also consisting of an integrated northern Mediterranean area and of a semi-desert or desertic southern area. In the first part, paleomagnetic and biostratigraphic studies based on rodent faunas were carried on continental deposits of two Algerian basins (Tafna and El Eulma). The magnetostratigraphic study realized in this work allowed to estimate the age of various fossiliferous deposits, and to correlate them with various other Neogene basins of North Africa.In the second part, new paleontological prospections in the Aït Kandoula basin (Morocco) led to the discovery of three fossiliferous deposits dated back to late Miocene. These deposits delivered a rich micromammalian fauna associated with large mammal remains. The systematic study of small mammals and especially rodents of deposits from both AF12-1 and AF12-2 allowed identifying taxa which have affinities with those of south-western Europe. These two new localities provide new information on the exchanges of faunas between Africa and Europe. The genus Stephanomys is reported here for the first time in Morocco. The biochronologic and magnetostratigraphic studies provide reliable information for the chronology of various phases of faunal exchanges between north-western Africa and south-western Europe. Faunal exchanges took place 0.25 Ma before the Messinian Salinity Crisis. In addition, some of the taxa identified in AF12-2 (Myocricetodon, Protatera, Atlantoxerus), are useful as paleoenvironmental indicators, attesting warm and dry climatic conditions
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Suraprasit, Kantapon. "Paléoenvironnements et reconstitutions paléoclimatiques du Pléistocène moyen de Thaïlande et leur impact sur la biodiversité et la distribution des espèces : la contribution de la faune de vertébrés du gisement de Khok Sung (Province du Khorat)". Thesis, Poitiers, 2015. http://www.theses.fr/2015POIT2285/document.

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La sablière de Khok Sung, dans la province de Nakhon Ratchasima, qui a livré plus d'un millier de fossiles de mammifères et de reptiles (cranes, dents isolées et restes post-craniens), abrite la faune de vertébrés du Pléistocène la plus riche de Thaïlande. La faune mammalienne qui est décrite ici en détail, se compose d'au moins 18 espèces identifiées (12 genres), y compris un primate et des proboscidiens, rhinocéros, suidés, bovidés, cervidés et carnivores. Elle compte principalement des taxons encore représentés de nos jours, ainsi que quelques taxons globalement ou localement éteints. A partir des données paléomagnétiques et des comparaisons fauniques, l'âge de la faune de Khok Sung est estimé au Pléistocène Moyen tardif, vers 188000 ou 213000 ans. Par rapport aux autres faunes diversifiées du Pléistocène d'Asie du Sud Est, l'assemblage de Khok Sung est caractérisé par une association des taxons Stegodon-Ailuropoda, comparable en cela au site de Thum Wiman Nakin, ce qui supporte l'hypothèse selon laquelle le Nord Est de la Thaïlande était un corridor biogéographique appartenant à la route migratoire Sino-Malaise, entre la Chine du Sud et l'île de Java. L'analyse des isotopes stables du carbone à partir de l'émail des ongulés fossiles révèle la présence d'une partition de niches entre les méga-herbivores et au sein des cervidés. Les valeurs du d13C de l'émail suggèrent également que les ruminants ont consommé une grande quantité de plantes en C4, ce qui indique que les prairies à graminées étaient particulièrement répandues en Thaïlande à cette époque où les écosystèmes n'étaient pas encore soumis à l'influence anthropique. La mesure des isotopes stables de l'oxygène, obtenue par échantillonnage sérié de l'émail des dents de grands mammifères, et l'analyse du cénogramme de la localité de Khok Sung reflètent une importante variation saisonnière des précipitations et de la température, associée à des conditions climatiques relativement humides
The Khok Sung sand pit, Nakhon Ratchasima province, has yielded the richest Pleistocene vertebrate fauna of Thailand, where more than a thousand fossil mammals and reptiles (skulls, isolated teeth, and postcranial remains) were recovered. The mammalian fauna, which is described in details hereby, consists of at least 18 identified species (12 genera), including a primate, proboscideans, rhinoceroses, suids, bovids, cervids, and carnivores, which are characterized by mostly extant elements associated to some completely and locally extinct taxa. The age of the Khok Sung fauna is tentatively attributed to the late Middle Pleistocene as either 188 or 213 ka, based on the paleomagnetic data and on the faunal comparisons. The Khok Sung mammal assemblage yields the Stegodon-Ailuropoda faunal association, most similar in composition to that of Thum Wiman Nakin, supporting the hypothesis that northeastern Thailand was a biogeographic gateway of the Sino-Malayan migration route from South China to Java. An analysis of stable carbon isotopes extracted from the tooth enamel of fossil ungulates reveals evidence of niche partitioning among megaherbivores and within cervids. The enamel carbonate d13C values also suggest a considerable amount of C4 plants in the dietary use of ruminants, indicating that grasslands had significantly expanded in Thailand at that time during which anthropic impacts on the ecosystems were absent. The stable oxygen isotope results, obtained from the serial sampling of large mammal enamel, combined with the cenogram analysis reflect significant seasonal variation in precipitations and temperature for Khok Sung, associated to a relatively humid climate
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Książki na temat "Biochronology"

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U, Haq Bilal, red. Plankton biochronology. Oxford: Elsevier, 1989.

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

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Moczydłowska, Małgorzata. Cambrian acritarchs from Upper Silesia, Poland: Biochronology and tectonic implications. Oslo: Scandinavian University Press, 1998.

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E, Taylor Michael, Sweet Walter C i Sheehan Peter M, red. Early Paleozoic biochronology of the Great Basin, western United States. Washington: U.S. G.P.O., 1997.

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O, Baumgartner Peter, INTERRAD Jurassic-Cretaceous Working Group i International Association of Radiolarian Paleontologists., red. Middle Jurassic to Lower Cretaceous radiolaria of Tethys: Occurences, systematics, biochronology. Lausanne, Suisse: Section des Sciences de la Terre, Université de Lausanne, 1995.

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Carter, Elizabeth S. Biochronology and paleontology of Lower Jurassic (Hettangian and Sinemurian) Radiolarians, Queen Charlotte Islands, British Columbia. Ottawa: Geological Survey of Canada, 1998.

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Alain, Blieck, Turner Susan i IGCP Project 328, red. Palaeozoic vertebrate biochronology and global marine/non-marine correlation: Final report of IGCP 328 (1991-1996). Frankfurt am Main: Senckenbergische Naturforschende Gesellschaft, 2000.

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Geological Survey (U.S.), red. Early Paleozoic Biochronology of the Great Basin, Western United States, U.S. Geological Survey Professional Paper 1579, 1997. [S.l: s.n., 1997.

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Dumont, Michael P. Diatom biochronology of the Sisquoc Formation in the Santa Maria basin, California, and its paleoceanographic and tectonic implications. [Washington: U.S. Govt. Print. Off., 1995.

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Tiffin, Sarah Heather. Dinocyst biochronology and palynofacies: Inferred systems tract character of Miocene sequences from New Jersey mid-Atlantic transect (ODP legs 174A and 174AX). St. Catharines, Ont: Brock University, Dept. of Earth Sciences, 2001.

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Części książek na temat "Biochronology"

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Gradstein, F. M. "Biochronology, Biostratigraphy". W 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". W 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". W 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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Bell, Christopher J. "Biochronology of North American Microtine Rodents". W AGU Reference Shelf, 379–406. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/rf004p0379.

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Guex, Jean, Federico Galster i Øyvind Hammer. "Lower Jurassic Radiolarian Biochronology and Evolutionary Rates". W Discrete Biochronological Time Scales, 79–86. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-21326-2_7.

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Monnet, Claude, Arnaud Brayard i Hugo Bucher. "Ammonoids and Quantitative Biochronology—A Unitary Association Perspective". W Topics in Geobiology, 277–98. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9633-0_11.

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Lucas, Spencer G., i Lawrence H. Tanner. "Triassic Timescale Based on Tetrapod Biostratigraphy and Biochronology". W Springer Geology, 1013–16. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_192.

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Guérin, Claude. "Biozones or Mammal Units? Methods and Limits in Biochronology". W European Neogene Mammal Chronology, 119–30. Boston, MA: Springer US, 1990. http://dx.doi.org/10.1007/978-1-4899-2513-8_8.

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Trevarthen, Colwyn. "Human biochronology: on the source and functions of ‘musicality’". W Music that works, 221–65. Vienna: Springer Vienna, 2009. http://dx.doi.org/10.1007/978-3-211-75121-3_16.

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Lucas, Spencer G. "Late Triassic Terrestrial Tetrapods: Biostratigraphy, Biochronology and Biotic Events". W Topics in Geobiology, 351–405. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-68009-5_10.

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Streszczenia konferencji na temat "Biochronology"

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Huttenlocker, Adam. "PROGRESS TOWARD CONSTRAINING CARBONIFEROUS-PERMIAN VERTEBRATE BIOCHRONOLOGY IN WESTERNMOST PANGEA". W 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343851.

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Lucas, Spencer G., i Robert M. Sullivan. "VERTEBRATE BIOCHRONOLOGY OF THE CRETACEOUS-PALEOCENE TRANSITION, SAN JUAN BASIN, NEW MEXICO". W 2009 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2009. http://dx.doi.org/10.56577/sm-2009.839.

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Jattiot, Romain, Hugo Bucher, Hugo Bucher, Arnaud Brayard, Arnaud Brayard, Morgane Brosse, Morgane Brosse i in. "A NEW KEY SMITHIAN (EARLY TRIASSIC) QUANTITATIVE AMMONOID BIOCHRONOLOGY FROM THE WESTERN USA BASIN". W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-277288.

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Kdýr, Šimon, Ján Soták, Ján Soták, Tiiu Elbra i Tiiu Elbra. "THE MERCURY CONCENTRATIONS AND BIOCHRONOLOGY OF BOUNDARY EVENTS ACROSS THE CRETACEOUS-PALEOGENE TRANSITION IN SLOVAKIA". W GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369688.

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Moretti, John A., i Eileen Johnson. "LATE BLANCAN GAZELLE-HORSE NANNIPPUS PENINSULATUS (MAMMALIA, EQUIDAE) FROM SCURRY COUNTY, TEXAS, WITH IMPLICATIONS FOR BIOCHRONOLOGY". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303999.

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Ikejiri, Takehito. "Distribution and biochronology of Camarasaurus (Dinosaria, Sauropoda) from the Jurassic Morrison Formation of the Rocky Mountain Region". W 56th Annual Fall Field Conference. New Mexico Geological Society, 2005. http://dx.doi.org/10.56577/ffc-56.367.

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Lucas, Spencer G. "NEW MEXICO’S FOSSIL RECORD: DETERMINATION OF GEOLOGICAL AGES FOR CAMBRIAN-PLEISTOCENE ROCKS USING BIOCHRONOLOGY". W 2009 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2009. http://dx.doi.org/10.56577/sm-2009.836.

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Hunt, Adrian P., i Spencer G. Lucas. "Vertebrate paleontology and biochronology of the lower Chinle Group (Upper Triassic), Sante Fe County, north-central New Mexico". W 46th Annual Fall Field Conference. New Mexico Geological Society, 1995. http://dx.doi.org/10.56577/ffc-46.243.

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Hunt, Adrian P., i Spencer G. Lucas. "BIOCHRONOLOGY OF TRIASSIC VERTEBRATE COPROLITES AND THE LACK OF A SIGNIFICANT TURNOVER IN COPROLITE ICHNOFAUNAS AT THE TRIASSIC/JURASSIC BOUNDARY". W Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314409.

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Fassett, James E., i Matthew T. Heizler. "A <sup>40</sup>AR/<sup>39</sup>AR SINGLE-CRYSTAL SANIDINE AGE FOR AN ALTERED VOLCANIC ASH BED FROM THE PALEOCENE NACIMIENTO FORMATION IN THE SOUTHERN SAN JUAN BASIN SHEDS NEW LIGHT ON THIS FORMATION&rsquo;S SRATIGRAPHIC AND BIOCHRONOLOGIC ESSENCE". W 2008 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2008. http://dx.doi.org/10.56577/sm-2008.875.

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Raporty organizacyjne na temat "Biochronology"

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Haggart, J. W. Turonian (Upper Cretaceous) strata and biochronology of southern Gulf Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193634.

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Orchard, M. J. Upper Triassic conodont biochronology and new index species from the Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132442.

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Nadaraju, G., i P. L. Smith. Jurassic biochronology in the Iskut River map area, British Columbia: a progress report. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132822.

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Haggart, J. W. Reconnaissance lithostratigraphy and biochronology of the Lower Cretaceous Longarm Formation, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127399.

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Carter, E. S., P. A. Whalen i J. Guex. Biochronology and paleontology of Lower Jurassic (Hettangian and Sinemurian) radiolarians, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209778.

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Orchard, M. J. Late Triassic Conodont Biochronology and Biostratigraphy of the Kunga Group, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131971.

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Anderson, R. G. Phanerozoic Time Scale, Biochronology, Geochronometry, and Some Mineral Deposits in the Canadian Cordillera and Adjacent parts of Alaska. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132639.

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Johannson, G. G. Preliminary report on the stratigraphy, sedimentology, and biochronology of the Inklin Formation in the Atlin Lake area, northern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134188.

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Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications. US Geological Survey, 1995. http://dx.doi.org/10.3133/b1995jk.

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