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Tesi sul tema "Paleobotany"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 25 luglio 2025

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1

Emerson, Lisa Francis. "The early Miocene Cape Blanco flora of coastal Oregon /." Connect to title online (Scholars' Bank) Connect to title online (ProQuest), 2009. http://hdl.handle.net/1794/10343.

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2

Blinnikov, Mikhail S. "Late-Pleistocene history of the Columbia Basin grassland based on phytolith records in loess /." view abstract or download file of text, 1999. http://wwwlib.umi.com/cr/uoregon/fullcit?p9948017.

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Thesis (Ph. D.)--University of Oregon, 1999.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 202-211). Also available for download from the Internet; free to University of Oregon users. Address: http://wwwlib.umi.com/cr/uoregon/fullcit?p9948017.

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3

Carlson, Lisa Jo. "Describing the postglacial pattern and rate of Picea expansion in Alaska using paleoecological records /." Thesis, Connect to this title online; UW restricted, 2003. http://hdl.handle.net/1773/5452.

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4

Tomescu, Alexandru Mihail Florian. "Late Ordovician - Early Silurian terrestrial biotas of Virginia, Ohio, and Pennsylvania : an investigation into the early colonization of land /." Ohio University / OhioLINK, 2004. http://www.ohiolink.edu/etd/view.cgi?ohiou1108479418.

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5

Hill, Robert S. "Evolution of the Australian flora in response to Cenozoic climate change /." Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09S.D/09s.dh6469.pdf.

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6

Currano, Ellen Diane. "Variations in insect herbivory on angiosperm leaves through the late Paleocene and early Eocene in the Bighorn Basin, Wyoming, USA /." View online, 2008. http://etda.libraries.psu.edu/theses/approved/WorldWideFiles/ETD-2863/Thesis_Currano_final.pdf.

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7

Blake, Bascombe Mitchel. "Carboniferous paleobotany and paleoclimatology of the central Appalachian Basin, West Virginia, U.S.A." Morgantown, W. Va. : [West Virginia University Libraries], 2009. http://hdl.handle.net/10450/10655.

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Thesis (Ph. D.)--West Virginia University, 2009.<br>Title from document title page. Document formatted into pages; contains xi, 240 p. : ill. (some col.), maps (some col.). Vita. Includes abstract. Includes bibliographical references.

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8

Sweet, Natalie L. "Paleoecology and sedimentology of late Silurian biogenic structures in the Duoro and Devon Island Formations on western Devon and southwestern Ellesmere Islands, Arctic Canada." Thesis, University of Ottawa (Canada), 1995. http://hdl.handle.net/10393/10385.

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Carbonate buildups of late-Ludlow-Pridoli age occur within an extensive Silurian reef 'belt' in the Canadian Arctic Islands. Two phases of mound development were documented. The buildups include mudmounds in the uppermost Douro Formation on western Devon Island, and skeletal mounds in the Devon Island Formation on southwestern Ellesmere, North Kent, and Seal islands and Colin Archer Peninsula on Devon Island. The mudmounds average 50m in diameter and 15m in height, and are composed predominantly of sparsely fossiliferous lime mudstone containing sponge spicules and micrite fabrics of probable

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9

Wymer, Dee Anne. "The paleoethnobotanical record of central Ohio - 100 B.C. to A.D. 800 : subsistence continuity amid cultural change." Connect to resource, 1987. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1219945114.

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10

Hoyt, Cathryn A. "Grassland to desert : Holocene vegetation and climate change in the northern Chihuahuan Desert /." Digital version:, 2000. http://wwwlib.umi.com/cr/utexas/fullcit?p9992819.

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11

Nelson, Nathan Alfred. "Holocene fire and climate in rangeland ecosystems of Southwestern Idaho." [Boise, Idaho] : Boise State University, 2009. http://scholarworks.boisestate.edu/td/24/.

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12

Oswald, William Wyatt. "Holocene vegetational history of the central Arctic foothills, northern Alaska : pollen representation of tundra and edaphic controls on the response of tundra to climate change /." Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/5578.

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13

Brunelle-Daines, Andrea. "Holocene changes in fire, climate and vegetation in the northern Rocky Mountains of Idaho and western Montana /." view abstract or download file of text, 2002. http://wwwlib.umi.com/cr/uoregon/fullcit?p3061935.

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Thesis (Ph. D.)--University of Oregon, 2002.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 170-178). Also available for download via the World Wide Web; free to University of Oregon users.

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14

Rowett, A. "The megafossil and microfossil floras of the Curlew Formation, Queensland /." Title page, contents and abstract only, 1986. http://web4.library.adelaide.edu.au/theses/09PH/09phr8812.pdf.

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15

Ingram, Steven. "Palynology of the Cape's top ten richest families and its taxonomic implications." Bachelor's thesis, University of Cape Town, 2011. http://hdl.handle.net/11427/23943.

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Principal pollen characters, of the Cape floristic Regions ten richest families, which are phylogenetically useful at higher taxonomic levels (including aperture type, exine structure, pollen-unit, polarity, symmetry, shape), and their evolutionary trends are examined. Monocotyledons differ from eu-dicotyledons (and eu-dicots from basal-dicots) in their aperture number and form, and exine structure and are discussed in relation to their pollination syndrome aswell as their evolutionary trends. We also discuss the possibilities of creating a taxonomic key at species level, if not only for use a

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16

Baghai, Nina Lucille. "An analysis of palynomorphs from upper Cretaceous sedimentary rocks with emphasis in the Aguja Formation, Big Bend National Park, Brewster County, Texas /." Digital version, 1996. http://wwwlib.umi.com/cr/utexas/fullcit?p9719292.

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17

Madigosky, Stephen R. "Palynological and paleoecological assessment of a Pennsylvanian shale overlying the Danville coal member (VII) in Sullivan County, Indiana." Virtual Press, 1987. http://liblink.bsu.edu/uhtbin/catkey/536305.

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Shale samples from three Upper Pennsylvanian assemblages overlying the Danville (No. 7) Coal Member in Sullivan County, Indiana were compared with respect to miospore content. Eight samples from each of the Hawthorn, Dugger and Minnehaha mines were chemically macerated and analyzed for pollen/spore content. A total of 108 species assigned to 40 genera were recovered. A comparison of the palynoflora from the three assemblages reveals 17 genera and 32 species found in common. The palynoflora is dominated by the following four genera: Lycospora, Laevigatosporites. Punctatisporites and Punctatospo

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18

Anshari, Gusti Zakaria. "Late quaternary vegetation and environments in the Lake Sentarum Wildlife Reserve, West Kalimantan, Indonesia." Monash University, School of Geography and Environmental Science, 2000. http://arrow.monash.edu.au/hdl/1959.1/9252.

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19

Woolfenden, Wallace Bird 1941. "Late Quaternary vegetation history of the southern Owens Valley region, Inyo County, California." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/282184.

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This study analyzes the pollen, spores, and algae in the upper 90 m section of a mostly continuous, well dated, 323 m core (OL-92) from Owens Lake, southeastern California. The entire core has produced a paleoclimatic record for the past ∼800 ka. The 90 m interval dates from ∼9 ka to ∼151 ka beginning with the penultimate glaciation and ending during the termination of the last glaciation. The record shows high amplitude fluctuations in the abundances of pine, juniper, saltbush, sagebrush, chenopods/amaranths, and Ambrosia-type pollen. High percentages of juniper pollen with low percentages of

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20

Shafer, David Scott. "The timing of late Quaternary monsoon precipitation maxima in the southwest United States." Diss., The University of Arizona, 1989. http://hdl.handle.net/10150/184766.

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The southwest monsoon is responsible for a summer precipitation maximum for much of the southwest U.S. Biostratigraphies of pollen, plant macrofossils, and aquatic fossils in lakes from near modern monsoon boundaries in conjunction with climate modelling suggests variations in strength of the monsoon system during the late Quaternary. At Montezuma Well, Arizona, high percentages of Pinus and Juniperus pollen as well as maximum influxes of Quercus and Gramineae pollen suggest a shift from dominantly winter to summer precipitation between ca. 12,000 and 9000 yr BP. Maximum aridity occurred 7000-

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21

Milburn, Paula. "Palaeoenvironmental investigation into aspects of the vegetation history of north Fife and south Perthshire, Scotland." Thesis, University of Edinburgh, 1997. http://hdl.handle.net/1842/10541.

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Results from the palaeoenvironmental investigations into the Holocene vegetation history of three sites in eastern lowland Scotland are presented. Two of the sites, Cruvie and Pitbladdo, are located in north Fife; the third site, Methvern is situated in south Perthshire. Cruvie is located in a kettle-hole and provides data extending from the Late-glacial to ea. 3900 BP. Pitbladdo is a former bog and cores from this site provide data on the period from ca. 8000 to 3900 BP. Methvern is a well-maintained raised bog and provides data that spans the entire Holocene. Relative, concentration and poll

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22

Sandau, Stephen D. "The Paleoclimate and Paleoecology of a Uintan (Late Middle Eocene) flora and fauna from the Uinta Basin, Utah /." Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd719.pdf.

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23

Scharf, Elizabeth Ann. "Long-term interactions of climate, vegetation, humans, and fire in eastern Washington /." Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/6444.

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24

Scholtz, Anton. "Palynological and palaeobotanical studies in the Southern Cape." Thesis, [S.l. : s.n.], 1986. http://hdl.handle.net/10019/877.

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25

Valentina, Corti. "Palynology and Paleobotany of Permo-Triassic Beacon Supergroup at Allan Hills, South Victoria Land, Antarctica: stratigraphical and paleoenvironmental change implications." Doctoral thesis, Università di Siena, 2021. http://hdl.handle.net/11365/1133988.

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Nowadays the Antarctic continent is almost entirely covered by ice (around 98% of the total land surface) and the conditions are inhospitable for vegetation, apart from very few species such as mosses and lichens. During the geological time however, conditions were very different and the Phanerozoic fossil record documents several occurrences of vegetation remains also indicating the presence of wide high latitude forests. The life of plants in the continent was obviously strictly influenced by the evolving paleogeography and paleoenvironmental conditions and their mutual interactions during

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26

Capretz, Robson Louiz [UNESP]. "Paleoecologia e tafonomia da floresta petrificada do Tocantins setentrional (Bacia do Parnaíba, Permiano)." Universidade Estadual Paulista (UNESP), 2010. http://hdl.handle.net/11449/103007.

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Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2010-08-16Bitstream added on 2014-06-13T21:04:03Z : No. of bitstreams: 1 capretz_rl_dr_rcla.pdf: 3353928 bytes, checksum: 7e9219802799c05db6d9550923870f72 (MD5)<br>Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>No presente estudo é descrita uma floresta do Eopermiano do Norte do Gondwana, dominada por pteridófitas arborescentes, gimnospermas, licófitas e esfenófitas. Esta rica assembléia fossilífera localiz

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27

Stranks, Lena. "Physiognomic and taphonomic studies in New Zealand and Australia : implications for the use of palaeobotany as a tool for palaeoclimate estimation." Thesis, University of Oxford, 1996. http://ora.ox.ac.uk/objects/uuid:478a83e2-5954-4c4f-b1ce-a8f7b6933011.

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Measurements of surface uplift rate potentially hold the key to understanding the tectonics of mountain belts and areas of uplift. Wolfe (1993) compiled a multicharacter data set (CLAMP) of the physiognomy of woody dicotyledon leaves with a view to using it to extract climatic information from fossil floras. The limited extent of this data set, along with the anomalous behaviour of some outliers cause me to question the global relationship between physiognomy and climate which has been implicitly assumed in all analyses of the data conducted to date. Additional data collected from native veget

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28

Huerta, Mariana Angelica. "Postglacial vegetation, fire, and climate history of Blacktail Pond, Northern Yellowstone National Park, WY." Thesis, Montana State University, 2008. http://etd.lib.montana.edu/etd/2008/huerta/HuertaM0508.pdf.

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Previous studies in Yellowstone National Park (YNP) suggest intensification of the summer-dry and summer-wet patterns in Yellowstone during the early Holocene when increased summer insolation caused atmospheric circulation patterns to strengthen. To examine this hypothesis further, pollen and high-resolution charcoal records were analyzed from Blacktail Pond to reconstruct fire and vegetation histories near the present transition between summer-wet and summer-dry conditions. The site currently lies in Pseudotsuga parkland with Artemisia steppe at lower elevations around the pond. The site supp

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29

Morgans, Helen Sarah. "Early to middle Jurassic stratigraphic development, vegetation and climate change in north-western Europe." Thesis, University of Oxford, 1997. http://ora.ox.ac.uk/objects/uuid:4b5cae3c-7562-45b9-b2a2-543b2649b24f.

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The aim of work presented in this thesis was to explore the inter-relationships of cyclic sedimentation, relative sea-level change, and palaeoclimate as inferred from plant megafossils. To this end, the investigation focused on the classic plant-bearing Middle Jurassic succession of Yorkshire. The Middle Jurassic (Aalenian-Bathonian) Ravenscar Group of the Cleveland Basin (Yorkshire) comprises a predominantly fluvio-deltaic succession intercalated between thinner, laterally persistent marine units. There is a pronounced lateral facies change across the basin, from mainly alluvial sediments in

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30

Davies, Katherine Siân. "Early Palaeocene vegetation and climate of North America." Thesis, University of Oxford, 1993. http://ora.ox.ac.uk/objects/uuid:4e48bfd5-f749-4d84-a132-c45fd8429fdc.

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Early Palaeocene floras from twenty seven sites within the Raton, southern Powder River and south-western Williston Basins of the western interior of North America were collected, and their leaf physiognomy, ecological character and depositional setting compared. Such a spread of samples enabled the study of spatial and temporal vegetational and climatic variations in the region, following the Cretaceous-Tertiary boundary event. Climatic changes are observed across the Cretaceous-Tertiary boundary. Precipitation increased dramatically, and remained relatively high throughout the earliest Palae

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31

Biedenbender, Sharon Helen 1950. "Landscape-scale vegetation change indicated by carbon isotopes in soil organic matter for a semidesert grassland in southeastern Arizona." Diss., The University of Arizona, 1999. http://hdl.handle.net/10150/284017.

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Vegetation change, particularly from the grass to shrub lifeform, is a critical issue on the world's rangelands. The plant community present on a site is the primary determinant of the land's value for watershed protection, wildlife habitat, livestock production, and recreation. Studying past vegetation composition can help separate natural from anthropogenic sources of change and guide natural resource conservation and management decisions. Stable carbon isotope (δ¹³C) values and associated radiocarbon ages from soil organic matter (SOM) were used to evaluate vegetation change across five lan

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32

Calentine, Leighann. "The Spoon Toe Site (11MG179) Middle Woodland gardening in the lower Illinois River Valley /." Diss., Columbia, Mo. : University of Missouri-Columbia, 2005. http://hdl.handle.net/10355/4256.

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Thesis (M.A.)--University of Missouri-Columbia, 2005.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (November 27, 2006) Vita. Includes bibliographical references.

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33

Scrivan, Leonie Jane. "Diversity of the mid-Eocene Maslin Bay flora, South Australia /." Title page, contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09PH/09phs434.pdf.

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34

Kauffmann, Marjorie 1982. "Mapeamento geológico e levantamento paleontológico do Monumento Natural das Árvores Fossilizadas, Bacia do Parnaíba, Estado do Tocantins." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287749.

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Orientadores: Frésia Soledad Ricardi Torres Branco, André Jasper<br>Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-27T04:59:02Z (GMT). No. of bitstreams: 1 Kauffmann_Marjorie_D.pdf: 10896204 bytes, checksum: e87c18b3f56ed15a1ab698a2c00261cf (MD5) Previous issue date: 2014<br>Resumo: O presente trabalho foi desenvolvido no Monumento Natural das Árvores Fossilizadas do Tocantins (MNAF), um rico sítio paleobotânico depositado na Bacia Sedimentar do Parnaíba onde os fósseis afloram nas Formações Pedra de Fogo e Motuca. Pela i

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35

Crawford, Laura J. Dr. "The Role of Selectivity on Alaskan Fuel Management Strategies." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1600964489257755.

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36

Greenwood, David Robert. "The foliar physiognomic analysis and taphonomy of leaf beds derived from modern Australia rainforest." Title page, contents and abstract only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phg8165.pdf.

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37

Duncan, Faith Louise, and Faith Louise Duncan. "Botanical reflections of the encuentro and the Contact Period in southern Marin County, California." Diss., The University of Arizona, 1992. http://hdl.handle.net/10150/185977.

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Plant indicator species and longitudinal paleobotanical data were used as independent measures to document the human ecological record of the contact period in southern Marin County, California. These data suggest that archaeological and documentary records are insufficient for examining changes in land management and use during the contact period. Prior to A.D. 1579, Western Miwok peoples had not encountered Europeans face to face. This early phase of the contact period is marked the possible introduction of New World species through passive cultural vectors. Two brief encounters occurred bet

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38

Capretz, Robson Louiz. "Paleoecologia e tafonomia da floresta petrificada do Tocantins setentrional (Bacia do Parnaíba, Permiano) /." Rio Claro : [s.n.], 2010. http://hdl.handle.net/11449/103007.

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Orientador: Rosemarie Rohn Davies<br>Banca: Fresia Soledad Ricardi Torres Branco<br>Banca: Roberto Ianuzzi<br>Banca: Joel Carneiro de Castro<br>Banca: Luis Gustavo Ferreira de Oliveira<br>Resumo: No presente estudo é descrita uma floresta do Eopermiano do Norte do Gondwana, dominada por pteridófitas arborescentes, gimnospermas, licófitas e esfenófitas. Esta rica assembléia fossilífera localiza-se no Monumento Natural das Árvores Fossilizadas do Tocantins (MNAFTO), na Bacia do Parnaíba, Norte do Brasil. Dois aspectos se destacam: a abundância dos fitofósseis e seu excepcional nível de preservaç

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39

Moraweck, Karolin. "Potential and significance of leaf trait changes of long lived species during the Paleogene." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-227800.

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Fossil plants are regard to be excellent proxies to trace paleoclimatic and paleoatmospheric changes. The vegetational response to changing paleoclimate and paleoatmospheric conditions has already been known for a long time and is well documented for the Paleogene of central Europe. Methods such as the Coexistence Approach (CA) and the Climate Leaf Analyses Multivariate Program (CLAMP) analyze the composition of fossil plant assemblages. Changes in paleoclimate and CO2 through time can be tracked also via changes in morphometric parameters such as leaf area, leaf size and leaf shape or epiderm

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40

Watanasak, Manas. "Mid-tertiary palynology of onshore and offshore Thailand /." Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09PH/09phm267.pdf.

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41

Grigg, Laurie Davis. "Millennial-scale vegetation and climate variations in the Pacific Northwest during the last glacial period (60,000-16,000 cal yr B.P.) /." view abstract or download file of text, 2000. http://wwwlib.umi.com/cr/uoregon/fullcit?p9998032.

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Thesis (Ph. D.)--University of Oregon, 2000.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 237-250). Also available for download via the World Wide Web; free to University of Oregon users.

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42

Sandau, Stephen Dee. "A Uintan (Late Middle Eocene) Flora and Fauna from the Uinta Basin, Utah." BYU ScholarsArchive, 2005. https://scholarsarchive.byu.edu/etd/247.

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Late Middle Eocene time marks one of the most dynamic periods of the Paleogene in the western interior of North America. Analysis of an extensive, new collection of plant, invertebrate, and vertebrae fossils from the Uinta Formation in the Uinta Basin, south of Myton, Utah, USA, provides evidence of environmental change. Paleobotanical specimens are preserved in late stage Uinta Lake sediments and coarse-grained fluvial sediments which are stratigraphically 650 to 660 m above the Green River Formation. Deposition rates estimates of 18 to 55 cm/kyr, for Uinta Lake sediments in the Uinta Basin s

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43

Meyer, Laura (Laura B. ). "High precision U/Pb geochronology on the Cenomanian Dakota Formation, Utah : implications for paleobotany and the transgression of the Western Interior Seaway preceding Oceanic Anoxic Event 2." Thesis, Massachusetts Institute of Technology, 2010. http://hdl.handle.net/1721.1/114377.

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Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2010.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (pages 31-35).<br>The Dakota Formation was deposited during the Cenomanian, a time when the Western Interior Seaway spanned much of North America. The Dakota Formation contains a rich record of plant and animal fossils. Key to understanding their importance, it is imperative to precisely place the Dakota Formation within the geological time scale. Volcanic ash samples interlayed with fossil bearing s

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44

Souza, Isabel Cortez Christiano de 1983. "Nova abordagem para os estudos paleobotânicos neopaleozóicos da borda leste na porção brasileira da bacia do Paraná utilizando sistemas de informação geográfica." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287395.

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Orientador: Frésia Soledad Ricardi Torres Branco<br>Acompanha 1 mapa acondicionado em bolso no [anexo IV]<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-19T16:09:15Z (GMT). No. of bitstreams: 1 Souza_IsabelCortezChristianode_M.pdf: 9651668 bytes, checksum: 4da84ef5f4b99b65a558d352d48494b0 (MD5) Previous issue date: 2011<br>Resumo: A presente dissertação buscou revisar as publicações acerca dos fitofósseis da Bacia do Paraná, permitindo visualizar a distribuição espacial das ocorrências fossilíferas. Para tanto fo

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45

Neregato, Rodrigo [UNESP]. "Esfenóitas do monumento natural das árvores fossilizadas do Tocantins, Bacia do Parnaíba (Permiano, Brasil)." Universidade Estadual Paulista (UNESP), 2012. http://hdl.handle.net/11449/102860.

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Made available in DSpace on 2014-06-11T19:32:17Z (GMT). No. of bitstreams: 0 Previous issue date: 2012-10-08Bitstream added on 2014-06-13T21:03:55Z : No. of bitstreams: 1 neregato_r_dr_rcla.pdf: 6620889 bytes, checksum: 7be6212f3d43bf983cee3190210e2efb (MD5)<br>Pela primeira vez são descritos, em detalhe, caules de esfenófitas permianos da Bacia do Parnaíba, atribuídos ao gênero Arthropitys, anteriormente conhecidos nas Províncias Florísticas Euramericana e Cataísica. Apresentam-se permineralizados por sílica, com preservação celular, em depósitos fluviais que provavelmente foram controlados

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Tavares, Tatiane Marinho Vieira [UNESP]. "Estudo de marattiales da Floresta Petrificada do Tocantins Setentrional (Permiano, Bacia do Parnaíba)." Universidade Estadual Paulista (UNESP), 2011. http://hdl.handle.net/11449/102995.

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Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-10-11Bitstream added on 2014-06-13T19:21:54Z : No. of bitstreams: 1 tavares_tmv_dr_rcla.pdf: 22064000 bytes, checksum: c51a1bd0310cf6dd42d21d4038317172 (MD5)<br>Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)<br>O trabalho apresenta descrições morfo-anatômicas de samambaias arborescentes permianas (Marattiales) permineralizadas por sílica da Formação Motuca, Bacia do Parnaíba, no Monumento Natural das Árvores Fossilizadas do Tocantins, Norte do Brasil. Os fósseis compre

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Faria, Rafael Souza de 1985. "Licofitas Guadalupianas da Bacia do Parana : Novos dados morfo-anatomicos." [s.n.], 2009. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287313.

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Orientador: Fresia Soledad Ricardi-Branco<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociencias<br>Made available in DSpace on 2018-08-12T21:47:49Z (GMT). No. of bitstreams: 1 Faria_RafaelSouzade_M.pdf: 4846121 bytes, checksum: 06fbb408dd12015c7f8b819ab250dae9 (MD5) Previous issue date: 2009<br>Resumo: Lycopodiopsis derbyi é a espécie à qual mais comumente se relacionam os fragmentos caulinares licofíticos encontrados em estratos guadalupianos da Bacia do Paraná. Tipicamente caracteriza-se por um cilindro vascular sifonostélico com o anel descontínuo cortado

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Tavares, Tatiane Marinho Vieira. "Estudo de marattiales da "Floresta Petrificada do Tocantins Setentrional" (Permiano, Bacia do Parnaíba) /." Rio Claro : [s.n.], 2011. http://hdl.handle.net/11449/102995.

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Orientador: Rosemarie Rohn Davies<br>Banca: Jefferson Prado<br>Banca: Fresia Soledad Ricardi Torres Branco<br>Banca: Roberto Iannuzzi<br>Banca: Joel Carneiro de Castro<br>Resumo: O trabalho apresenta descrições morfo-anatômicas de samambaias arborescentes permianas (Marattiales) permineralizadas por sílica da Formação Motuca, Bacia do Parnaíba, no Monumento Natural das Árvores Fossilizadas do Tocantins, Norte do Brasil. Os fósseis compreendem caules, folhas férteis, estéreis e raques. Os caules classificam-se em Tietea ou Psaronius. Os primeiros são muito abundantes e, mesmo sem ápice preserva

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Neregato, Rodrigo. "Esfenóitas do monumento natural das árvores fossilizadas do Tocantins, Bacia do Parnaíba (Permiano, Brasil) /." Rio Claro, 2012. http://hdl.handle.net/11449/102860.

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Orientador: Rosemaire Rohn Davies<br>Banca: Joel Carneiro de Castro<br>Banca: Roberto Iannuzzi<br>Banca: Fresia Soledad Ricardi-Branco<br>Banca: Jefferson Prado<br>Resumo: Pela primeira vez são descritos, em detalhe, caules de esfenófitas permianos da Bacia do Parnaíba, atribuídos ao gênero Arthropitys, anteriormente conhecidos nas Províncias Florísticas Euramericana e Cataísica. Apresentam-se permineralizados por sílica, com preservação celular, em depósitos fluviais que provavelmente foram controlados por estações secas e úmidas bem definidas. Diversos exemplares possuem ramos conectados ou

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Crifo, Camilla. "VARIATIONS IN ANGIOSPERM LEAF VEIN DENSITY HAVE IMPLICATIONS FOR INTERPRETING LIFE FORM IN THE FOSSIL RECORD." Miami University / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=miami1375987428.

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