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Organic and inorganic geochemistry of the petrification of woodSigleo, Anne Marguerite Colberg, 1944- January 1977 (has links)
No description available.
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302 |
Biostratigraphy and systematics of Siwalik Rhizomyidae (Rodentia)Flynn, Lawrence J. January 1981 (has links)
No description available.
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Pollen analysis of quaternary archaeological and lacustrine sediments from the Colorado PlateauHevly, Richard H. January 1964 (has links)
No description available.
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304 |
Small mammals of the Quiburis Formation, southeastern ArizonaJacobs, Louis L. January 1973 (has links)
No description available.
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Hard substrate communities across the K-Pg boundarySogot, Caroline Elizabeth January 2013 (has links)
No description available.
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306 |
Fossil pollen and its bearing on the archaeology of the Lehner Mammoth siteLindsay, Alexander J. January 1958 (has links)
No description available.
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307 |
Pollen analysis of sediments from Matty WashSchoenwetter, James January 1960 (has links)
No description available.
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308 |
A neoglacial pollen record from Osgood Swamp, CaliforniaZauderer, Jeffrey Norman, 1947- January 1973 (has links)
No description available.
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309 |
The Eocene cichlids (Perciformes:Labroidei) of Mahenge, Tanzania /Murray, Alison M. January 2000 (has links)
A new genus and five new species of fossil cichlid fishes (Perciformes: Labroidei) are described from Mahenge, Tanzania. These cichlids represent the oldest confirmed fossils of the family, dating from the middle of the Eocene. The specimens share many lepidological characters, and, from comparison with other members of the family, are identified as being a monophyletic group. Therefore, they are described as belonging to a single genus, Mahengechromis gen. nov., named for the type locality. Detailed anatomical study of the well-preserved specimens allows five species to be identified, M. plethos, M. rotundus, M. brachycranium , M. ellipticus, and M. curvifrons spp. nov. These species are distinguished on the basis of osteological characters, including the shape of the frontal bones, hyomandibulae and opercular bones. The species are believed to be endemic to the type locality, which, along with monophyly of the species, indicates that these fishes formed a species flock. This suggests that the capacity for cichlids to form species flocks arose early in the family's history. / Previously published phylogenetic analyses of the family Cichlidae have included few characters that can be used to incorporate fossil material. Osteological features that may be useful for determining relationships are identified and used in a phylogenetic analysis of the family. The results of this analysis are compared with the results of previous analyses to determine the usefulness of the characters. This comparison indicates that most osteological characters are homoplastic among cichlids, although some of the characters may prove to be phylogenetically useful. Although phylogenetic analysis of osteologic characters does not result in a well-resolved phylogeny, the most parsimonious placement of the fossil cichlids from Mahenge is in a relatively basal position among the African lineages, as the sister group to the hemichromine cichlids from West Africa. / The biogeographic relationships of members of the Cichlidae are examined based on information from the fossil record and the interrelationships of the lineages within the family. Two suggestions have been made for the age of the family; either the cichlids originated in the Early Cretaceous or they evolved near the end of the Mesozoic. The later time of origin would have required a trans-Atlantic dispersal. Based on the distribution of Recent and fossil cichlids, the latter hypothesis is accepted. A reconstruction of the dispersal patterns and possible means of dispersal are evaluated.
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Anatomy, functional morphology and phylogeny of Aistopoda (Tetrapoda, Lepospondyli)Anderson, Jason S., 1969- January 2000 (has links)
The importance of fossils to phylogenetic reconstruction is well established. However, analyses of fossil data sets are confounded by problems related to the incomplete nature of the specimens. Taxa that are incompletely known are problematic because of the uncertainty of their placement within a tree, leading to a proliferation of most parsimonious solutions because of wild card behavior. Problematic taxa are commonly deleted based on a priori criteria of completeness. Paradoxically, a taxon's problematic behavior is tree dependent, and levels of completeness are not necessarily associated with problematic behavior. Exclusion of taxa based on completeness eliminates real character conflict and, by not allowing incomplete taxa to determine tree topology, the phylogenetic hypothesis is diminished. / A method is proposed to allow optimization of taxonomic inclusion and tree stability. It identifies and removes taxa causing multiple most parsimonious solutions, producing a more stable topology, called the phylogenetic trunk. This method is used in an analysis of the Paleozoic Lepospondyli. A single most parsimonious tree, or trunk, was found after removal of one taxon identified as being problematic. The 38 trees found one additional step from this primary trunk are reduced to two by removal of one additional taxon. These trunks are compared to the trees found by excluding taxa with various degrees of completeness. Effects of incomplete taxa are explored by comparison with the stable tree. Correlated characters associated with limblessness are discussed regarding the assumption of character independence. Inclusion of intermediate taxa is found to be the single best method for breaking down long branches.
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