Bibliografie tematiche / Paleobiogeography

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Letteratura scientifica selezionata sul tema "Paleobiogeography"

Autore: Grafiati
Pubblicato: 4 giugno 2021
Ultima modifica: 29 luglio 2024

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Articoli di riviste sul tema "Paleobiogeography"

1

Young, Gavin C. "Paleobiogeography of Devonian vertebrates". Paleontological Society Special Publications 6 (1992): 322. http://dx.doi.org/10.1017/s2475262200008820.

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Five distinctive vertebrate faunas characterised by endemic taxa can be recognised for the Early Devonian (Euramerica, Siberia, Tuva, China, and East Gondwana). By Late Devonian time these faunal provinces are obscured by widespread taxa which also inhabited nonmarine aquatic environments, but indicate faunal communication between Gondwana, Euramerica and China. This marked change in pattern between the Early and Late Devonian may be attributed to intrinsic (evolutionary) or extrinsic causal factors. Dispersal capabilities of aquatic vertebrates may have increased during the initial gnathostome radiation of the Devonian, but a predominantly extrinsic cause (e.g. global change in geography or climate) is suggested by the similar pattern for marine invertebrate faunas of Early Devonian endemism and Late Devonian cosmopolitanism. Outstanding problems of Devonian vertebrate biogeography include faunal differentiation on the largest landmass of the time (Gondwana), and the nature of barriers and connections between East and West Gondwana, East Gondwana and South and North China, and West Gondwana and Euramerica. A vertebrate equivalent of the cool-water Malvinokaffric invertebrate faunal realm of the Siluro-Devonian is not clearly identified, but vertebrate data from southern Africa and south America are sparse.Wide latitudinal distributions for some Late Devonian vertebrate taxa appear anomalous, and could indicate either reduced global climatic gradients, or erroneous paleogeographic base maps. There are difficulties in formulating a hypothesis of global warming and/or major paleogeographic change in a way which clearly distinguishes basic from interpreted data. Three major subdisciplines (paleomagnetism, paleoclimatology, paleobiogeography) contribute to Paleozoic paleogeographic reconstructions. Their data tend to be organised and represented in different ways, but each relies on the same principle of concordance with a general pattern (Young 1990). Degree of consilience of a hypothesis based on one data set (the extent to which it explains patterns within an unrelated set of data) is a primary criterion for accepting or rejecting the hypothesis. Apparent polar wander path representation facilitates testing of paleomagnetic data against those paleoclimatic or paleobiogeographic data which provide evidence of paleolatitude. However, as well as the simple indication of paleolatitude, biogeographic and some other qualitative data sets provide more complex evidence concerning connections or barriers between regions, for which APWP representation is not appropriate. Cladistic analysis of hierarchically organised data sets (Young, 1986, 1987) provides a means of integrating qualitative paleobiogeographic, paleoclimatic, and paleogeographic data such that inconsistencies in the evidence are emphasised, and the hypothesis is exposed to falsification. These ideas are illustrated using Devonian examples.
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2

HAYAMI, Itaru. "Modern Situation of Paleobiogeography". Journal of Geography (Chigaku Zasshi) 94, n. 7 (1986): 604–11. http://dx.doi.org/10.5026/jgeography.94.604.

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3

Waggoner, Ben. "Paleobiogeography. Bruce S. Lieberman". Quarterly Review of Biology 76, n. 3 (settembre 2001): 348. http://dx.doi.org/10.1086/394014.

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4

Croitor, Roman. "Paleobiogeography of Crown Deer". Earth 3, n. 4 (6 novembre 2022): 1138–60. http://dx.doi.org/10.3390/earth3040066.

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The article describes the paleobiogeographic history of the modern subfamilies so-called “crown deer” of the family Cervidae (Artiodactyla, Mammalia) in the world from the late Miocene to the late Pleistocene. The study overviews the taxonomic diversity and evolutionary radiation of Cervidae from all zoogeographic realms where this systematic group is present in the paleontological record. The evolutionary diversification of the fossil Cervidae is based on the estimations of species body masses that are regarded here as a proxy of occupied ecological niches. The study reveals two important evolutionary radiations of Cervidae during the late Miocene of Eurasia that gave the origin of the modern subfamilies Cervinae and Capreolinae. The evolutionary radiation of Capreolinae during the Pleistocene in South America shows a range of diversity comparable to the late Miocene radiations of Old World deer and provides multiple examples of evolutionary convergences with Eurasian Pleistocene cervids. The article discusses factors that shaped the modern biogeographic distribution of representatives of the subfamilies Cervinae and Capreolinae.
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Terras, Rafael, Mirian Carbonera, Guilherme Budke e Karla Janaísa Gonçalves Leite. "FAMÍLIA SPINOSAURIDAE (DINOSAURIA: THEROPODA): TAXONOMIA, PALEOBIOGEOGRAFIA E PALEOECOLOGIA (UMA REVISÃO)". PALEONTOLOGIA EM DESTAQUE - Boletim Informativo da Sociedade Brasileira de Paleontologia 37, n. 77 (10 luglio 2023): 14–54. http://dx.doi.org/10.4072/paleodest.2022.37.77.02.

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Spinosauridae family (Dinosauria: Theropoda): taxonomy, paleobiogeography and paleoecology (a revision). Spinosauridae is a family of Tetanuran theropod dinosaurs that was widely distributed during the Early Cretaceous. Here we revised the state of art of the family’s taxonomy, paleobiogeography and paleoecology. We compiled updated diagnosis for the holotypes of the 20 species attributed to the family since 1841, alongside with the different hypotheses related to the family’s paleobiogeography and paleoecology. We also compiled updated diagnosis for a series of indeterminate elements that are relevant in literature. We conclude that out of these 20 taxa six can be regarded as nomina dubia (Ostafrikasaurus crassiserratus, Suchosaurus girardi, Spinosaurus maroccanus, Siamosaurus suteethorni, Sinopliosaurus fusuiensis, Suchosaurus cultridens) due to the lack of diagnostic material and autapomorphies. Out of these, three were regarded as incertae sedis (Ostafrikasaurus crassiserratus, Suchosaurus girardi, Suchosaurus cultridens) for the same reasons and the possibility of belonging to previously already established taxa inside Spinosauridae and for one of these (Ostafrikasaurus crassiserratus) for possibly being a member of Ceratosauria. As for paleobiogeography, the fossil evidence suggests that the family might have originated in Laurasia (Western Europe), but the existence of a tooth older than the European taxa might indicate that the family might have originated in Gondwana (Brazil). Finally, regarding paleoecology, the most accepted hypothesis is that they were generalist predators of the margins of aquatic environments (i.e. riparian zone), and waders in shallow waters like modern herons and storks, and if necessary also resorting to terrestrial environments. They would be capable of alternating between resources and environments, in addition to sharing their habitats with theropods of the Abelisauridae and Carcharodontosauridae families and even with other spinosaurids, if the environmental conditions favored it. Keywords: Theropoda, Spinosauridae, Spinosaurinae, Baryonychinae, paleobiogeography, paleoecology.
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6

Smith, Paul L., e Gerd E. G. Westermann. "Paleobiogeography of the Ancient Pacific". Science 249, n. 4969 (10 agosto 1990): 680. http://dx.doi.org/10.1126/science.249.4969.680.a.

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Stanley, George D., e Thomas E. Yancey. "Paleobiogeography of the Ancient Pacific". Science 249, n. 4969 (10 agosto 1990): 680–81. http://dx.doi.org/10.1126/science.249.4969.680.b.

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8

Weishampel, David B., e Ralph E. Chapman. "The Quantitative Paleobiogeography of Dinosaurs". Paleontological Society Special Publications 8 (1996): 418. http://dx.doi.org/10.1017/s2475262200004202.

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9

Khan, Muhammad Akbar, e Muhammad Umer Farooq . "Paleobiogeography of the Siwalik Ruminants". International Journal of Zoological Research 2, n. 2 (15 marzo 2006): 100–109. http://dx.doi.org/10.3923/ijzr.2006.100.109.

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10

Smith, P. L., e G. E. G. Westermann. "Paleobiogeography of the Ancient Pacific". Science 249, n. 4969 (10 agosto 1990): 680. http://dx.doi.org/10.1126/science.249.4969.680.

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Tesi sul tema "Paleobiogeography"

1

Walls, Bradley J. "Quantitative Paleobiogeography of Maysvillian (Late Ordovician) Brachiopod Species of the Cincinnati Arch: a Test of Niche Modeling Methods for Paleobiogeographic Reconstruction". Ohio : Ohio University, 2009. http://www.ohiolink.edu/etd/view.cgi?ohiou1243010764.

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2

Frantescu, Ovidiu D. "Systematics, paleobiogeography, and paleoecology of cretaceous decapod faunas from northeast Texas". Thesis, Kent State University, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=3726727.

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Investigation of decapod fossils from the Pawpaw Shale, Albian, Texas, has yielded 17 new species, and seven new genera. In total, 14 brachyuran; 3 astacidean; 4 anomuran; 8 axiidean; 5 palinuridean, and one stomatopod species were described and classified according to the latest classification scheme. Shale samples from a single locality in Fort Worth were analyzed for their grain size, mineral and trace element content. The Pawpaw Shale consists of sediments derived from the Llanos uplift to the southwest of Fort Worth, and represents a fining upward sequence deposited in a restricted lagoonal environment. The decapod fauna of the Pawpaw Shale is one of the richest decapod faunas of Albian age known to date, composed of a population of adult and juvenile crabs and lobsters. The peculiar small size of the individual lobsters of this fauna is attributed to their representing an early ontogenetic stage. No trace elements known to affect the biology an physiology of extant decapods could be found in the shale samples analyzed to indicate an environmental cause for the reduced size of the Pawpaw lobsters.

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Frantescu, Ovidiu D. "SYSTEMATICS, PALEOBIOGEOGRAPHY, AND PALEOECOLOGY OF CRETACEOUS DECAPOD FAUNAS FROM NORTHEAST TEXAS". Kent State University / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=kent1368631876.

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4

Serobyan, Vahram. "Upper Devonian brachiopods and sedimentary sequences from Armenia : biodiversity, stratigraphy and paleobiogeography". Electronic Thesis or Diss., Université de Lille (2018-2021), 2021. http://www.theses.fr/2021LILUR033.

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Les séries sédimentaires carbonatées-terrigènes et les brachiopodes du Dévonien supérieur d’Arménie centrale ont été ici étudiées à partir de trois coupes distinctes (Ertych, Djravank et Noravank). Leur interprétation paléoenvironnementale a été réalisée à partir des bio- et lithofaciès afin de reconstituer leur milieux de dépôt. De plus, les coupes étudiées ont été corrélées lithostratigraphiquement, ainsi que biostratigraphiquement, en se basant sur leurs assemblages à brachiopodes. Vingt-six espèces de brachiopodes sont décrites sur la base d’un matériel récemment collecté. Quatre nouveaux genres de brachiopodes (Aramazdospirifer, Angustisulcispirifer, Pentagonospirifer et Tornatospirifer), ainsi que cinq nouvelles espèces (Crinisarina pseudoglobularis, Cyrtospirifer pseudoasiaticus, Pseudocyrtiopsis areniensis, Pentagonaspirifer abrahamyanae et Angustisulcispirifer arakelyani) sont introduits. Toutes les espèces de brachiopodes sont examinées selon des concepts taxonomiques modernes ; leurs caractéristiques internes et externes sont illustrées, à l’exception de quelques rares espèces. La variabilité morphologique intraspécifique des espèces décrites est documentée quantitativement. Le schéma biostratigraphique proposé auparavant pour l’intervalle Frasnien–Famennien du Petit Caucase (Arménie et Nakhichevan) est révisé. Plus particulièrement, la zone à Ripidiorhynchus gnishikensis–Angustisulcispirifer arakelyani, d’âge Frasnien, est proposée pour la faune trouvée dans les calcaires à péloïdes accumulés dans un cortège à haut niveau marin, alors que la zone à Aramazdospirifer orbelianus–Tornatospirifer armenicus, d’âge Fammenien inférieur, est caractérisée par des packstones/graistones de l’intervalle 4, déposés lors d’un événement transgressif. La présente étude documente également la diversité des brachiopodes signalée dans le Petit Caucase à travers l’intervalle Frasnien–Famennien inférieur et souligne un renouvellement majeur de faune parmi les rhynchonellides, les atrypides et les spiriférides. D’un point de vue paléobiogéographique, la faune étudiée a clairement des affinités avec celles connues dans d'autres régions de la marge nord-Gondwanienne, notamment celles qui s’étendent vers l’est du SAB (Bloc sud arménien) jusqu’en Afghanistan et le Pamir, bien qu’il existe également de nombreux éléments endémiques. De plus, la signification paléobiogéographique des quatre nouveaux genres est discutée, y compris de plusieurs autres espèces du Famennien qui leur sont réaffectés et qu’elles étaient connues auparavant du Nakhichevan, du Pamir (Tadjikistan), du Kazakhstan central et de la Plate-forme d’Europe de l’Est
The Upper Devonian carbonate-siliciclastic sedimentary sequences and brachiopods from three distinct sections (Ertych, Djravank and Noravank) of Central Armenia are here examined. Paleoenvironmental interpretation is performed based on bio- and lithofacies to reconstruct the depositional environments in which the sedimentary sequences were accumulated. Moreover, the studied sections are correlated lithostratigraphically, as well as biostratigraphically by focusing on their brachiopod assemblages. Twenty-six brachiopod species are described on the basis of recently collected material from the Frasnian–Famennian (F–F) succession. Four new brachiopod genera (Aramazdospirifer, Angustisulcispirifer, Pentagonospirifer and Tornatospirifer) and five new species (Crinisarina pseudoglobularis, Cyrtospirifer pseudoasiaticus, Pseudocyrtiopsis areniensis, Pentagonaspirifer abrahamyanae and Angustisulcispirifer arakelyani) are introduced. All brachiopod species are examined according to modern taxonomic concepts and illustrated both externally and internally, with the exception of some rare species. The intraspecific morphological variability of the described species is documented quantitatively. The previously suggested biostratigraphic scheme for brachiopods of the F–F interval of the Lesser Caucasus (Armenia and Nakhichevan) is revised. More particularly, the Ripidiorhynchus gnishikensis–Angustisulcispirifer arakelyani brachiopod zone, of Frasnian age, characterizes the peloidal grainstones of the Interval 1 that accumulated as a highstand system tract, while the Lower Famennian Aramazdospirifer orbelianus–Tornatospirifer armenicus Zone is found in the packstones/grainstones of the Interval 4, which was deposited during a transgressive event. The present study also documents the diversity of brachiopods reported from the Frasnian–lower Famennian sequences of the Lesser Caucasus (Armenia and Nakhichevan); the synthesis of all previous and current data suggests that a major change in diversity took place amongst rhynchonellides, atrypides and spiriferides. From a paleobiogeographic viewpoint, the studied fauna clearly shares affinities with contemporaneous brachiopods known from other parts of the north-Gondwanan margin, especially from those areas that extend eastwards of the South Armenian Block (SAB) into Afghanistan and Pamir, although there are also many endemic elements. Finally, the paleobiogeographic significance of the four newly defined genera is discussed, including the re-assignment to them of several other Famennian species known previously from Nakhichevan, Pamir (Tajikistan), Central Kazakhstan and the East European Platform
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Samathi, Adun [Verfasser]. "Theropod dinosaurs from Thailand and Southeast Asia : phylogeny, evolution, and paleobiogeography / Adun Samathi". Bonn : Universitäts- und Landesbibliothek Bonn, 2019. http://d-nb.info/120002012X/34.

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Wright, David F. "Macroevolution and Paleobiogeography of Middle to Late Ordovician Brachiopods: A Phylogenetic Biogeographic Approach". Ohio University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1338324936.

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7

Gorscak, Eric. "Descriptive and Comparative Morphology of African Titanosaurian Sauropods: New Information on the Evolution of Cretaceous African Continental Faunas". Ohio University / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1478778037108276.

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8

Pletka, Crystal. "Neogene Changes in Caribbean Paleoproductivity and the Diversity and Paleobiogeography of Deep-sea Benthic Foraminifera". FIU Digital Commons, 2016. http://digitalcommons.fiu.edu/etd/2468.

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The Neogene history of Caribbean deep-sea benthic foraminifera was investigated by calculating changes in paleoproductivity, diversity and paleobiogeography ~26 to 2 Ma, which includes the progressive closure of the Central American Seaway. Three hypotheses were tested: (1) Paleoproductivity values prior to closure of the Central American Seaway are similar in both the Caribbean and equatorial Pacific and then diverge by the time of early shoaling events; (2) Diversity values of benthic foraminifera prior to the closure of the Central American Seaway were similar in the Caribbean and EEP, and had changed by the time of early shoaling; and (3) during the Miocene and into the Pleistocene, the progressive constriction of the CAS affected deep-sea benthic foraminiferal assemblages by increasing their dissimilarity between the Caribbean and equatorial Eastern Pacific. These hypotheses were tested with 104 samples from five Caribbean and EEP deep-sea cores by calculating paleoproductivity with multiple proxies, determining diversity indices and calculating biogeographic similarity coefficients. The data supported the first two hypotheses: The greatest change in paleoproductivity occurred at ~8 Ma during seaway constriction, when values diverged between the Caribbean and EEP. After complete seaway closure at ~4 Ma, the Caribbean became oligotrophic, noted by a decrease in high-organic flux species, and an increase in Nuttalides umbonifera, an indicator species. The largest changes in species-level diversity occurred with the barrier to deep-water flow at ~12 Ma, and Caribbean diversity increased at ~8 Ma with seaway constriction. However, the third hypothesis was rejected: Increases in assemblage similarity actually occurred during most major paleoceanographic events, with the only decrease in Caribbean-EEP similarity occurring at ~12 Ma, coincident with a drop in diversity and emplacement of the Panama isthmian sill. Thus, the barrier to deep-water flow at ~12 Ma affected the composition of tropical American benthic foraminifera more than the largest change in paleoproductivity at ~8 Ma, or closure of the Central American Seaway at ~4 Ma.
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Chitnarin, Anisong. "Taxonomy of Permian ostracods from central northeastern, and western Thailand : implication for paleoenvironment and paleobiogeography". Paris 6, 2010. http://www.theses.fr/2010PA066123.

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Quinze coupes et deux localités de calcaires du Permien inférieur à moyen terminal appartenant au Groupe de Loei, Groupe de Saraburi et au Calcaire de Sai York (dans les régions de Loei, Petchabun, Nakhon Sawan-Lopburi et Kanchanaburi) ont été étudiées. Les calcaires qui ont été échantillonnés et traités par acétolyse à chaud, renferment de nombreux ostracodes. Ils appartiennent à 196 espèces et 41 genres. 29 espèces sont connues avec d'autres régions, 167 sont endémiques. Les assemblages d'ostracodes, comprenant des Bairdioidea, Kloedenellidae, Kirkbyidae, Hollinellidae, Paraparchitidea, Cytherideidae, Cavellinidae, Pachydomellidae, Aparchitidea, Coelonellidae et Polycopidae, sont typiquement des espèces marines peu profondes dans des environnements marins marginaux à de plate-forme externe. Les concentrations en oxygène dans l'eau, évaluées à partir des pourcentages d'ostracodes filtreurs vs détritivores, seraient approximativement de l'ordre de 5ml/l pour toutes les coupes. Vingt neuf espèces d'ostracodes sont reconnues dans d'autres régions de la Paléo-Téthys. Ces espèces sont benthiques et leurs larves ont le même mode de vie. L'indice de provincialisme suggère des relations étroites avec la Tunisie, la Chine du Sud, la Grèce, l'Oman, l'Italie, la Hongrie et Israël, en ordre décroissant. Les relations avec l'Amérique du Nord sont faibles. Les ostracodes peuvent avoir été transportés vers des régions éloignées par des courants de surfaces de l'est vers l'Ouest de la paléo-Téthys au cours du Permien. La présence d'espèces communes entre les régions de Loei, Phetchabun, et Nakhon Sawan-Lopburi suggèrent que les calcaires des groupes de Loei et de Saraburi se sont déposés dans des environnements marins peu profonds, peu éloignés les uns des autres, où les faunes d'ostracodes benthiques pouvaient se déplacer ou migrer
Belonged to Loei Group, Saraburi Group, and Sai Yok Limestone (in Loei, Phetchabun, Nakhon Sawan-Lopburi, and Kanchanaburi areas) were investigated. Limestones were collected and processed by the hot acetolysis which yielded many ostracods. They are belonged to 196 species and 41 genera of which 29 species are known from other places, 167 species are endemic. The ostracod assemblages including Bairdioidea, Kloedenellidae, Kirkbyidae, Hollinellidae, Paraparchitidea, Cytherideidae, Cavellinidae, Pachydomellidae, Aparchitidea, Coelonellidae, and Polycopidae are typical shallow marine species from marginal marine to exterior platform environments. Oxygen concentration is approximately 5ml/l at all sections according to percentage of filter-feeding and deposit-feeding ostracods. Twenty-nine ostracod species known from other Permian sites within Paleotethys region are benthic inhabitants and their larvae have the same way of life. Provincialism Index suggests close relationships with Tunisia, South China, Greece, Oman, Italy, Hungary, Israel, in decreasing order. The relationships with North American species are low. The ostracods could be carried to the remote sites by surface paleocurrents from east to west in Paleotethys realms during the Permian. Presence of common species between Loei, Phetchabun, and Nakhon Sawan-Lopburi areas suggest that limestones of Loei and Saraburi Groups were deposited in shallow marine environments not far from each other where benthic ostracod fauna was able to travel or migrate
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Randklev, Charles R. "The Ecology and Paleobiogeography of Freshwater Mussels (Family: Unionidae) from Selected River Basins in Texas". Thesis, University of North Texas, 2011. https://digital.library.unt.edu/ark:/67531/metadc68035/.

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This dissertation has two overall objectives: first, to demonstrate the utility of paleozoological data for ongoing and future mussel-conservation efforts in Texas and second, to evaluate whether simple measures of habitat (e.g., water depth, velocity and particle size) are important for demonstrating the within-habitat spatial separation of mussels. Although these topics may seem disparate, both are important for increasing our understanding of unionid ecology and biogeography. Chapters 1 through 3 examine the use of paleozoological data for mussel conservation. Although these types of data are not new they have rarely been used in mussel conservation efforts within Texas. This is unfortunate because paleozoological data can provide an excellent record of the mussel fauna prior to wide-scale modern impacts and in areas where historical survey data are lacking. Chapter 4 examines whether assessments of microhabitat for mussels using simple measures of habitat (e.g., water velocity, depth and particle size) are useful. Recent studies have suggested that these measures do not explain the mussel distribution in flowing streams. If this is correct, instream flow studies using this approach need to be revised. Results of Chapter 4 indicate that mussels in the lower Brazos River basin are constrained in distribution by the availability of heterogenous substrate. Appendix A, details the first account of a living population of Truncilla macrodon, which is a candidate species for the Endangered Species Act (ESA). The population was found while conducting mussel instream flow studies in the lower Brazos River basin.
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Più fonti

Libri sul tema "Paleobiogeography"

1

Lieberman, Bruce S. Paleobiogeography. Boston, MA: Springer US, 2000. http://dx.doi.org/10.1007/978-1-4615-4161-5.

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Puckett, T. Markham. Systematics and paleobiogeography of brachycytherine Ostracoda. New York: Micropaleontology Press, American Museum of Natural History, 2002.

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3

Ochsenius, Claudio. Relictia and refugia in geological history and panbiogeography: A contribution to the knowledge of the survival of geobiotas through time and space their conservation and change with a discussion of the refugia theory and its historical development. 3a ed. Singen am Hohentwiel: Carl-Christian Ochsenius-Stiftung, 1998.

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Petrovich, Tatarinov Leonid, Rozanov Alekseĭ I͡U︡rʹevich, Paleontologicheskiĭ institut (Akademii͡a︡ nauk SSSR) e Geologiĭn Khurėėlėn (BNMAU-yn Shinzhlėkh Ukhaany Akademi), a cura di. Problemy paleobiogeografii Azii. Moskva: Izd-vo "Nauka", 1986.

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5

Eric, Buffetaut, Jaeger Jean-Jacques, Rage Jean-Claude, Société géologique de France e Centre national de la recherche scientifique (France), a cura di. Paléogéographie de l'Inde, du Tibet et du sud-est asiatique: Confrontation des données paléontologiques avec les modèles géodynamiques : table ronde, Société géologique de France et Centre national de la recherche scientifique, Paris, les 17-20 octobre 1983. Paris: La Société géologique, 1985.

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Harper, D. A. T., e Thomas Servais. Early palaeozoic biogeography and palaeogeography. London: The Geological Society, 2013.

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A, Cherchi, a cura di. Autecology of selected fossil organisms: Achievements and problems. Modena: Mucchi, 1996.

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Urusov, V. M. Geografii͡a︡ i paleogeografii͡a︡ vidoobrazovanii͡a︡ v Vostochnoĭ Azii (sosudistye rastenii͡a︡) =: Geography and paleogeography speciation in East Asia. Vladivostok: TIG DVO RAN, 1998.

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9

Utah) Paleobiogeography (2005 Salt Lake City. Paleobiogeography: Generating new insights into the coevolution of the earth and its biota : presented as a Paleontological Society short course at the annual meeting of the Geological Society of America, Salt Lake City, Utah, October 15, 2005. A cura di Lieberman Bruce S, Stigall Rode Alycia L, White, Russell D. (Russell David), 1959-, Geological Society of America e Paleontological Society. New Haven, Conn: Printed by Yale University Reprographics & Imaging Service, 2005.

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Rieppel, Olivier. The genus Placodus: Systematics, morphology, paleobiogeography, and paleobiology. Chicago, Ill: Field Museum of Natural History, 1995.

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Capitoli di libri sul tema "Paleobiogeography"

1

Lieberman, Bruce S. "What Is Paleobiogeography?" In Topics in Geobiology, 1–3. Boston, MA: Springer US, 2000. http://dx.doi.org/10.1007/978-1-4615-4161-5_1.

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Prevosti, Francisco Juan, e Analia M. Forasiepi. "Paleoenvironment, Tectonics, and Paleobiogeography". In Springer Geology, 17–38. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-03701-1_2.

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Lieberman, Bruce S. "Defining Areas in Paleobiogeography". In Topics in Geobiology, 93–107. Boston, MA: Springer US, 2000. http://dx.doi.org/10.1007/978-1-4615-4161-5_7.

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Ifrim, Christina, Jens Lehmann e Peter Ward. "Paleobiogeography of Late Cretaceous Ammonoids". In Topics in Geobiology, 259–74. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9633-0_10.

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Lehmann, Jens, Christina Ifrim, Luc Bulot e Camille Frau. "Paleobiogeography of Early Cretaceous Ammonoids". In Topics in Geobiology, 229–57. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9633-0_9.

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Holroyd, Patricia A., e Mary C. Maas. "Paleogeography, Paleobiogeography, and Anthropoid Origins". In Anthropoid Origins, 297–334. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4757-9197-6_11.

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Lieberman, Bruce S. "The History of Biogeography and Paleobiogeography". In Topics in Geobiology, 37–62. Boston, MA: Springer US, 2000. http://dx.doi.org/10.1007/978-1-4615-4161-5_4.

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Waters, Johnny, e Gary D. Webster. "The Paleobiogeography of Pennsylvanian Crinoids and Blastoids". In Earth and Life, 831–47. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-90-481-3428-1_29.

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Yacobucci, Margaret M. "Macroevolution and Paleobiogeography of Jurassic-Cretaceous Ammonoids". In Topics in Geobiology, 189–228. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9633-0_8.

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Bibi, Faysal, Ferhat Kaya e Sara Varela. "Paleoecology and Paleobiogeography of the Baynunah Fauna". In Sands of Time, 333–50. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-83883-6_19.

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Atti di convegni sul tema "Paleobiogeography"

1

Angiolini, Lucia, Giovanni Muttoni, Gaia Crippa e Vincenzo Verna. "Paleobiogeography of the Permian Neo-Tethys Shores". In GEO 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609-pdb.248.173.

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Hunt, Gene, Huai-Hsuan May Huang, Moriaki Yasuhara, Thomas Cronin e Hisayo Okahashi. "PALEOBIOGEOGRAPHY OF THE GENUS POSEIDONAMICUS (OSTRACODA)". In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380150.

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Scotese, Christopher. "THE PERMIAN WORLD: PLATE TECTONICS, PALEOGEOGRAPHY, PALEOCLIMATE, & PALEOBIOGEOGRAPHY". In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343892.

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Scotese, Christopher. "THE TRIASSIC WORLD: PLATE TECTONICS, PALEOGEOGRAPHY, PALEOCLIMATE & PALEOBIOGEOGRAPHY". In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320140.

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Lam, Adriane R., Sarah L. Sheffield e Nicholas J. Matzke. "PALEOBIOGEOGRAPHY OF THE EARLY PALEOZOIC ECHINODERMS ACROSS THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT". In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344679.

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Phillipi, Daniel, Carrie E. Schweitzer e Rodney M. Feldmann. "UTILITY OF NODEXL IN INVESTIGATING PALEOECOLOGY AND PALEOBIOGEOGRAPHY OF FOSSIL DECAPOD CRUSTACEANS". In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301395.

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Quaglio, Fernanda, Rowan Whittle, Huw Griffiths, Silvio Shigueo Nihei, Katrin Linse e Marcello Simoes. "PALEOBIOGEOGRAPHY OF ANTARCTIC MOLLUSC BIVALVES AND THE ENVIRONMENTAL CHANGES AFTER THE CENOZOIC COOLING". In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356817.

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Beech, James. "WHERE THE HARPETIDS ARE: PALEOBIOGEOGRAPHY, DIVERSITY, AND MASS EXTINCTION IN AN ENIGMATIC TRILOBITE ORDER". In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-348653.

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Dorrell, Emma Louise, e Lance L. Lambert. "PALEOBIOGEOGRAPHY OF SWADELINA (PENNSYLVANIAN CONODONT) AT 20 YEARS--A REVIEW AND PROSPECTS". In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-394452.

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Oh, Yeongju, Sangmin Lee, Dong-Chan Lee, Paul S. Hong e Seung-Bae Lee. "PHYLOGENY AND PALEOBIOGEOGRAPHY OF THE FAMILY NISUSIIDAE (CAMBRIAN RHYNCHONELLIFORM BRACHIOPOD) WITH SYSTEMATIC REVISION OF NISUSIIDS FROM SOUTH KOREA". In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-332631.

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Rapporti di organizzazioni sul tema "Paleobiogeography"

1

Haggart, J. W., J. A. Burnett e P. R. Bown. Notes on Cretaceous calcareous nannofloral biostratigraphy and paleobiogeography, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194095.

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