Relevant bibliographies by topics / Paleoecology

Academic literature on the topic 'Paleoecology'

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Published: 4 June 2021
Last updated: 29 July 2024

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Journal articles on the topic "Paleoecology"

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Ausich, William I. "Paleoecology Workshop." PALAIOS 7, no. 2 (April 1992): 239. http://dx.doi.org/10.2307/3514935.

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Gavin, Daniel. "PALEOECOLOGY SECTION." Bulletin of the Ecological Society of America 84, no. 4 (October 2003): 186. http://dx.doi.org/10.1890/0012-9623(2003)84[186b:ps]2.0.co;2.

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Shuman, Bryan. "PALEOECOLOGY SECTION." Bulletin of the Ecological Society of America 85, no. 4 (October 2004): 186–87. http://dx.doi.org/10.1890/0012-9623(2004)85[186b:ps]2.0.co;2.

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Booth, Robert. "PALEOECOLOGY SECTION." Bulletin of the Ecological Society of America 86, no. 4 (October 2005): 263. http://dx.doi.org/10.1890/0012-9623(2005)86[263a:ps]2.0.co;2.

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Brugam, Richard. "Paleoecology Section." Bulletin of the Ecological Society of America 89, no. 4 (October 2008): 368. http://dx.doi.org/10.1890/0012-9623(2008)89[368a:ps]2.0.co;2.

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Bottjer, David J. "Bivalve Paleoecology." Notes for a Short Course: Studies in Geology 13 (1985): 122–37. http://dx.doi.org/10.1017/s0271164800001135.

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Bivalves are one of the major macroinvertebrate fossil groups of the Phanerozoic. Bivalves have occupied many aqueous habitats, and in doing this have undergone a steady, relatively unchecked increase in diversity (Figure 1). Thus, bivalves are one of the most useful fossil groups in paleoecology, both for environmental reconstruction as well as for deciphering patterns and processes of evolutionary paleoecology.
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Kohn, Alan J. "Gastropod Paleoecology." Notes for a Short Course: Studies in Geology 13 (1985): 174–89. http://dx.doi.org/10.1017/s0271164800001160.

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Paleoecology concerns the life processes and patterns of environmental relationships of groups of ancient organisms during their lifetimes. Two assumptions are fundamental to paleoecological theory: observed patterns in populations, associations, communities and ecosystems represented in the fossil record were imposed by contemporaneous physical and biological environmental factors and their interactions, and at least some past environmental conditions can be discerned from fossil assemblages and their rock matrices.
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Ward, Peter D., and Gerd E. G. Westermann. "Cephalopod Paleoecology." Notes for a Short Course: Studies in Geology 13 (1985): 215–29. http://dx.doi.org/10.1017/s0271164800001196.

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Studying the paleoecology of the extinct chambered cephalopods is somewhat analogous to studying a distant landscape through the wrong end of a powerful telescope: we can see very small views of what must have been great panoramic vistas. Two factors have lead to this situation. First, the extant cephalopods still utilizing the phragmocone system of density reduction are at very low standing diversity, while most of the more interesting taxa, such as ammonites and belemnites, are completely extinct. Our functional interpretations of various shell morphologies thus depend heavily on generalizations based on a small number of sometimes distantly related taxa, such as Nautilus and Sepia. Secondly, studies of fossil associations and their relationships to various facies are clouded by the possibility of extensive post-mortal drift of the cephalopod shells. Because of this, we cannot ever be sure that we are studying cephalopod biocoenoses. In spite of these constraints, however, the past two decades have witnessed a great research effort into the study of cephalopod paleoecology. Debate over various issues has been sometimes clamorous, a sign of a healthy and vigorous utilization of the scientific method by many interested students of the fossil record.
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Miller, Ranall F. "Chitin paleoecology." Biochemical Systematics and Ecology 19, no. 5 (August 1991): 401–11. http://dx.doi.org/10.1016/0305-1978(91)90057-7.

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Webb, Robert H. "Spatial and Temporal Distribution of Radiocarbon Ages on Rodent Middens from the Southwestern United States." Radiocarbon 28, no. 1 (1986): 1–8. http://dx.doi.org/10.1017/s0033822200059981.

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The analysis of rodent middens, principally deposited by packrats (Neotoma sp), has rapidly become the most important paleoecologic and paleoclimatologic tool in the southwestern United States. The recent discovery of rodent middens created by stick-nest rats (Leporillus sp) and rock wallabies (Petrogale sp) in Australia (Green et al, 1983; P S Martin, oral commun, 1984) and by dassie rats (Petromus typicus) in South Africa (L Scott, oral commun, 1984) portends the use of midden analysis in arid regions worldwide. Several recent reviews of southwestern paleoecology (eg, Spaulding et al, 1983) rely heavily on rodent middens for ecologic and climatic reconstructions.
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Dissertations / Theses on the topic "Paleoecology"

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Mattos, Nathália Helena Secol 1988. "Geoquímica e proveniência do Grupo Bauru no Oeste de Minas Gerais." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/286616.

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Orientador: Alessandro Batezelli
Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências
Made available in DSpace on 2018-08-25T21:40:30Z (GMT). No. of bitstreams: 1 Mattos_NathaliaHelenaSecol_M.pdf: 5195246 bytes, checksum: 2551186b0e4a53abcac203b4227922a3 (MD5) Previous issue date: 2014
Resumo: Estudos geoquímicos e mineralógicos de arenitos e argilitos da Bacia Bauru (Cretáceo Superior), localizada na região do Triângulo Mineiro (Minas Gerais) foram realizados visando à determinação da proveniência, tectônica da rocha fonte, o papel de processos como intemperismo e reciclagem sedimentar na assinatura geoquímica da rocha fonte e à proposição de um modelo de evolução paleoambiental para a área de estudo. As amostras tem sua mineralogia principal composta por quartzo, microclínio, calcita, albita, dolomita e hematita. Illita, montmorillonita e paligorsquita são os argilominerais identificados. Elementos maiores, traços e terras raras e as razões elementares entre eles foram utilizadas para determinar a composição da rocha fonte. Valores do Índice Químico de Alteração e do Índice de Intemperismo Químico variando de 64 a 92 e de 84 a 98, respectivamente, e a ocorrência de feldspatos nas rochas sedimentares indicam intemperismo químico moderado na área fonte. Gráficos de elementos maiores e traços e valores para razões como La/Sc (1,47-4,86), (La/Yb)c (3,86-20,44) e a anomalia de Eu (Eu/Eu* = 0,62-0,92) comparados com dados da literatura sugerem que os sedimentos da Bacia Bauru na área de estudo tenham sido originados de rochas de composição quartzítica a granítico-gnáissica, derivadas de áreas continentais estáveis e depositados em ambientes de bacias intracratônica. A possível área-fonte para as rochas estudadas localiza-se a NE da Bacia Bauru, consistindo em rochas graníticas e metassedimentares do embasamento pré-cambriano. A deposição sedimentar na Bacia Bauru reflete a interação de processos aluviais e lacustres
Abstract: Geochemical and mineralogical studies of sandstones and mudstones from the Late Cretaceous Bauru Basin of Triângulo Mineiro region (Minas Gerais State) were undertaken to determine the provenance, tectonic setting, the role of weathering, sorting and recycling on the source rock geochemical signature and to propose a palaeoenvironmental evolution model to the study area. The analysed samples are mainly composed by quartz, microcline, calcite, albite, dolomite and hematite. Illite, montmorillonite and palygorskite are the identified clay minerals. Major elements were used to determine the source rock composition, as well as trace and rare earth elements and the ratios among them. Chemical Index of Alteration and Chemical Index of Weathering ranging from 64.83 to 92.3 and from 84 to 98.2, respectively, along with the feldspar occurrence on sedimentary rocks indicate a moderate weathering in the source area. Plots of major and trace elements and values for the ratios such as La/Sc (1.47-4.86), (La/Yb)c (3.86-20.44) and the Eu anomaly (Eu/Eu*= 0.62-0.92), compared to data from the literature indicate source rock was located into a continental passive margin tectonic setting and sediments were derived from quartzitic to granitic-gneissic rocks of stable continental areas and deposited in an intracratonic basin. Probable source area to the studied rocks is located at NE of Bauru Basin and consists in granitic and metassedimentary rocks from the Precambrian basement. Sedimentary deposition in Bauru Basin reflects an interaction of alluvial and processes
Mestrado
Geologia e Recursos Naturais
Mestra em Geociências
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Voltani, Cibele Gasparelo. "Redescrição osteológica comentada e aspectos paleoecológicos dos gêneros Notelops e Rhacolepis (Pachyrhizodontoidei) /." Rio Claro, 2016. http://hdl.handle.net/11449/141899.

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Orientador: Reinaldo José Bertini
Banca: Roberto Goitein
Banca: Marise Sardenberg Salgado de Carvalho
Banca: Alcina Magnólia da Silva Franca
Banca: Maria Helena Ribeiro Hessel
Resumo: A Bacia do Araripe situa-se no Nordeste brasileiro, e sua área estende-se sobre os estados de Ceará, Pernambuco e Piauí. Esta bacia sedimentar apresenta formações geológicas de idade paleozoica e mesozoica em cujos estratos estão fossilizados diversos tipos de organismos. A Formação Santana, eocretácica, possui destaque em termos de diversidade e qualidade dos organismos fossilizados. O Membro Romualdo é o mais superior desta formação e representa o contexto no qual ocorrem os ictiólitos ou concreções calcárias portadoras de peixes fósseis, sendo fonte de cerca de 30 gêneros formalmente descritos. Destes gêneros, dois foram selecionados para redescrição osteológica, Notelops e Rhacolepis, mediante preparação mecânica e/ou química para a remoção de sedimento de modo a evidenciar estruturas ósseas. Além da osteologia dos gêneros mencionados, outros organismos associados também foram evidenciados, permitindo a observação de um passado "congelado" nas imediações da gênese dos ictiólitos viabilizando, assim, breves abordagens de aspectos paleoecológicos para os para os peixes fósseis redescritos nesta tese
Abstract: Araripe Basin is located in Brazilian northeast, and its area extends over Ceará, Pernambuco and Piauí states. This watershed presents geologic formations from the Paleozoic and Mesozoic ages in which strata are fossilized several kinds of organisms. The Santana Formation, Early Cretaceous, is highlighted in terms of diversity and quantity of fossilized organisms. Romualdo Member is the most superior of this formation and it is the context in which ichthyoliths or calcareous concretions bearing fossilized fish occurs, being the source of about 30 formally described genres. Of these genres, two have been selected for osteological redescriptions, Notelops and Rhacolepis, by mechanical and/or chemical preparation for sediment removal to evidence bone structures. Besides the osteology of these mentioned genres, other organisms in association with them were also evidenced, allowing the observation of a "frozen" past near the genesis of ichthyoliths, enabling thus brief observations of the paleoecological aspects for the fish redescribed in these Ph D Thesis
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Silveira, Rosemery Rocha da. "Bioestratigrafia e paleoecologia de depósitos neógenos e pleistocenos aflorantes na porção central e ocidental da Bacia do Solimões, Estado do Amazonas, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/132294.

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As 93 amostras palinológicas obtidas deste estudo são oriundas de 12 afloramentos relacionados às formações Solimões e Içá, na região de Coari (5 afloramentos) e Alto Solimões (7 afloramentos), Bacia do Solimões, no estado do Amazonas. Este trabalho apresenta os palinomorfos reconhecidos nestes depósitos (incluindo descrições quando necessárias), com registro fotomicrográfico, relativos a 11 taxons de esporos de fungos, 7 algas, 1 escolecodonte, 1 cisto de dinoflagelado, 31 esporos de pteridófitas, 2 grãos de pólen de gimnospermas e 48 grãos de pólens de angiospermas. Perfis compostos foram construídos para os depósitos aflorantes das regiões de Alto Solimões e Coari, com interpretação estratigráfica. A composição da palinoflora em ambas as áreas apresenta contrastes, sendo aquela de Alto Solimões a de menor diversidade, mas com maior abundância, em comparação com a de Coari. Na região do Alto Solimões há documentação de formas como Crassoretitriletes vanraadshooveni, Foveotriletes ornatos, Magnastriatites grandiosus e a ocorrência de um cisto de dinoflagelado, que confirma influência marinha local para a Formação Solimões. Na região de Coari foi verificado predomínio de esporomorfos, evidenciando contexto continental para as formações Solimões e Içá. Palinofósseis guias de zoneamentos palinológicos foram reconhecidos para a região do Alto Solimões, tais como Crassoretitriletes vanraadshooveni, Grimsdalea magnaclavata, Multimarginites vanderhammeni, Diphyes latiusculus, entre outros. A associação dessas formas permitiu posicionar os depósitos da Formação Solimões na região de Tabatinga e Atalaia do Norte entre o Serravaliano e o Tortoniano (Mioceno Médio/ Superior), com correspondência com a Zona Grimsdalea, pré-estabelecida para intervalo coevo da unidade. Para Coari as amostras foram posicionadas no Neomioceno/Plioceno, a partir do reconhecimento da Subzona de Intervalo de Fenestrites longispinisus, ainda que na área este apresente baixa frequência. Ainda na região de Coari são identificados depósitos mais jovens, a partir da presença de Alnipollenites verus, que indica idade Pleistocena.
The 93 pollen samples obtained in this study were the result of research 12 outcrops related to Solimões and Içá formations in the region of Coari (5 outcrops) and Alto Solimões (7 outcrops) in the state of Amazonas. This paper presents the recognized palinomorphs (including descriptions when necessary) and photomicrographs of 11 fungal spores, 7 algae, 1 escolecodont, 1 dinoflagellate cyst, 31 fern spores and 48 pollen grains of angiosperms. The composition of palinoflora in both areas shows contrasts with that of the Alto Solimões less diverse, but more abundantly in comparison with the Coari. In the Alto Solimões is no documentation of ways Crassoretitriletes vanraadshooveni, Foveotriletes ornamentos, Magnastriatites grandiosus and the occurrence of a dinoflagellate cyst, confirming local marine influence to the Solimões Formation. In Coari region was verified predominance of esporomorphs, showing the continental context for the Solimões and Içá formations. Guides species of zonal schemes previously proposed were recognized for the Alto Solimões, such as Crassoretitriletes vanraadshooveni, Grimsdalea magnaclavata, Multimarginites vanderhammeni, Diphyes latiusculus, among others. The association of these forms allowed positioning of the deposits of the Solimões Formation in the region of Tabatinga and Atalaia do Norte on the edge of Serravaliano-Tortonian intervals (Miocene Middle and Upper), with correspondence with the Grimsdalea Zone, preset to coeval range of the unit. To Coari samples were placed in Neomioceno / Pliocene, from the recognition Interval Subdivision of Fenestrites longispinisus, although in this area has a low frequency. Still in the region Coari younger deposits are identified from the presence of Alnipollenites verus, which indicates age Pleistocene.
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Sudhaus, Dirk. "Paläoökologische Untersuchungen zur spätglazialen und holozänen Landschaftsgenese des Ostschwarzwaldes im Vergleich mit den Buntsandsteinvogesen /." Freiburg i. Br. : Institut für Physische Geographie der Albert-Ludwigs-Universität, 2005. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=014181535&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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Glenwright, T. Lane. "Diatom-based palaeoecology of Kowloon Bay, Hong Kong /." Hong Kong : University of Hong Kong, 2000. http://sunzi.lib.hku.hk/hkuto/record.jsp?B22032423.

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Liu, Liping. "Chinese fossil Suoidea : systematics, evolution and paleoecology." Helsinki : University of Helsinki, 2003. http://ethesis.helsinki.fi/julkaisut/mat/geolo/vk/liping/.

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Tosal, Alcobé Aixa. "Modelització paleoclimàtica del límit Eocè–Oligocè a Catalunya a partir de l’anàlisi CLAMP." Doctoral thesis, Universitat de Barcelona, 2019. http://hdl.handle.net/10803/668462.

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Aquesta tesi té com a objectiu modelitzar el paleoclima del trànsit Eocè−Oligocè de la Conca de l’Ebre i conèixer com aquest canvi afectà a la flora local. Aquesta caracterització paleoclimàtica s’ha obtingut a partir de l’estudi de les fulles de dicotiledònies de les localitats de Sarral (Priabonià terminal) i Cervera (Rupelià inferior) mitjançant CLAMP (Climate Leaf Analysis Multivariate Program). Per altra banda, per tal de poder caracteritzar els canvis florístics entre ambdues localitats, s’ha estudiat la seva taxonomia, tafonomia i paleoecologia així com la sedimentologia dels dipòsits que inclouen les associacions fòssils. S’han descrit setanta-cinc espècies de magnoliòpsides una de les quals, Rhus asymmetrica, és nova. La descripció s’ha basat en criteris moderns prenent en consideració caràcters com la nervadura terciària i detalls del marge foliar, fet que ha permès definir el polimorfisme intraespecífic d’algunes espècies. Tot i així en el futur caldrà revisar la taxonomia d’aquestes espècies comparant-les amb especies similars d’altres localitats europees contemporànies i amb les fulles d’espècies actuals afins. Des del punt de vista paleoambiental les flores de les dues localitats estudiades s’estructuraven en biomes similars encara que de composició força diferent. Aquestes diferències han permès caracteritzar els canvis en la distribució de la vegetació, que van tenir lloc entre el Priabonià i el Rupelià a la Conca de l’Ebre. L’exemple més evident fa referència a la vegetació que ocupava la zona adjacent a la comunitat del bosc de ribera amb un accés indirecte de les seves restes als rius i al llac. En el Priabonià de Sarral aquest bioma estava dominat per Tetraclinis, formant una bosquina oberta de cupressàcies. En canvi, al Rupelià de Cervera les plantes que creixien darrera del bosc de ribera eren principalment Daphnogene, Laurophyllum, Myrica faya i M. oligocenica i formaven petites laurisilves. Un altre bioma que mostra diferències notables entre les dues localitats estudiades fa referència a la part més allunyada dels llacs que estaria caracteritzada per una vegetació de tipus sabana. Aquest bioma mostrà una biodiversitat relativament baixa durant el Priabonià de Sarral, on estaria dominat per vuit espècies de fabals, Zizyphus zizyphoides i Pinus. Pel contrari, la comunitat equivalent en el Rupelià de Cervera estaria dominada per catorze espècies de fabals i set espècies d’altres grups taxonòmics tals com Rhamnus aizoon, Rhus asymmetrica i espècies afins com Toxicodendron. L’anàlisi CLAMP de les flores estudiades a la Conca de l’Ebre mostra una tendència climàtica cap a un refredament i un augment de l’estacionalitat entre l’Eocè superior i l’Oligocè inferior, que concorda amb la tendència global observada a l’hemisferi nord. Tanmateix, també assenyala que la pluviometria era més elevada a l’Oligocè de Cervera que al Priabonià de Sarral, fet que seria l’oposat de la tendència generalment acceptada vers un augment de l’aridesa al sud d’Europa durant aquest període. Aquests resultats reflectirien un canvi climàtic més complex del què s’havia documenatat fins ara. L’anàlisi de fàcies aporta dades clau per interpretar els resultats de la modelització mitjançant CLAMP. En aquest sentit, la flora de Sarral es trobaria en els períodes secs d’una seqüència de somització lacustre interpretada com a moments de màxima precessió. Per altra banda, la flora rupeliana de Cervera reflectiria els estadis humits dels cicles sedimentaris de somització lacustre, que correspondrien als cicles orbitals de precessió mínima. Aquestes condicions climàtiques específiques de cada localitat permeten comprendre els canvis en la composició i la distribució de la vegetació detectats per l’estudi paleoecològic. Per exemple, la temperatura elevada i la pluviometria baixa del Priabonià de Sarral haurien afavorit les plantes adaptades a bosquines obertes i de tipus sabana dominades per les fabals o Tetraclinis. Alhora, aquelles espècies amb un requeriment hídric més elevat, com les lauràcies, s’haurien vist obligades a créixer en zones relativament més humides, concretament al bosc de ribera. En canvi, les condicions ambientals amb una temperatura més moderada i una pluviometria més alta en el Rupelià de Cervera haurien permès el desenvolupament de moltes altres famílies de plantes al costat de les fabals, especialment les anacardiàcies. L’increment de la pluviometria a l’Oligocè de Cervera hauria beneficiat que els llorers s’expandissin fora del bosc de ribera formant petites comunitats de laurisilva. La combinació dels estudis sedimentològics, tafonòmics, paleoecològics i paleoclimàtics ha permès comprendre les interaccions entre el clima i la vegetació durant el trànsit Eocè−Oligocè a la Conca de l’Ebre. La sobreimposició de cicles climàtics d’ordre menor (cicles orbitals de precessió) en els cicles d’ordre major (cicles d’excentricitat) produiria un canvi climàtic no lineal. Els paràmetres pluviomètrics fluctuants van condicionar enormement l’evolució de les comunitats vegetals i probablement es trobarien en l’origen d’una vegetació resistent a aquestes variacions, com és la flora Mediterrània.
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Briles, Christy Elaine. "Holocene vegetation and fire history of the floristically diverse Klamath Mountains, northern California, USA /." Connect to title online (Scholars' Bank) Connect to title online (ProQuest), 2008. http://hdl.handle.net/1794/7486.

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Thesis (Ph. D.)--University of Oregon, 2008.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 217-227). Also available online in Scholars' Bank; and in ProQuest, free to University of Oregon users.
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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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Minckley, Thomas A. "Holocene environmental history of the northwestern Great Basin and the analysis of modern pollen analogues in western North America /." view abstract or download file of text, 2003. http://wwwlib.umi.com/cr/uoregon/fullcit?p3113019.

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Thesis (Ph. D.)--University of Oregon, 2003.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 294-310). Also available for download via the World Wide Web; free to University of Oregon users.
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Books on the topic "Paleoecology"

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Bottjer, David J. Paleoecology. Chichester, UK: John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781118455838.

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Croft, Darin A., Denise F. Su, and Scott W. Simpson, eds. Methods in Paleoecology. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-94265-0.

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Smykatz-Kloss, Werner, and Peter Felix-Henningsen, eds. Paleoecology of Quaternary Drylands. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/b92353.

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DeWitt, Norris Richard, Corfield R. M, and Geological Society of America. Meeting, eds. Isotope paleobiology and paleoecology. [Fayetteville, AR]: Paleontological Society, 1998.

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1938-, Smykatz-Kloss Werner, and Felix-Henningsen Peter, eds. Paleoecology of quaternary drylands. New York: Springer, 2004.

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1931-, Stanton Robert J., ed. Paleoecology, concepts and applications. 2nd ed. New York: Wiley, 1990.

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K, Behrensmeyer Anna, ed. Terrestrial ecosystems through time: Evolutionary paleoecology of terrestrial plants and animals. Chicago: University of Chicago Press, 1992.

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A, DiMichele William, Wing Scott L, and Botanical Society of America. Paleobotanical Section., eds. Methods and applications of plant paleoecology. Knoxville, TN: Published for the Paleontological Society at the Dept. of Geological Sciences, University of Tennessee-Knoxville, 1988.

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N, Goren-Inbar, and Speth John D, eds. Human paleoecology in the Levantine Corridor. Oxford: Oxbow Books, 2004.

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Frederiksen, Norman O. Review of Early Tertiary sporomorph paleoecology. [Texas?]: American Association of Stratigraphic Palynologists Foundation, 1985.

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Book chapters on the topic "Paleoecology"

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Gordillo, Sandra, María Sol Bayer, Gabriella Boretto, and Melisa Charó. "Paleoecology." In Mollusk shells as bio-geo-archives, 23–33. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-03476-8_4.

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Wilson, Chris C., and Nicholas E. Mandrak. "Paleoecology." In The Lake Charr Salvelinus namaycush: Biology, Ecology, Distribution, and Management, 41–67. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-62259-6_3.

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Reed, Kaye E. "Multiproxy Paleoecology." In A Companion to Paleoanthropology, 203–25. Oxford: Blackwell Publishing Ltd, 2013. http://dx.doi.org/10.1002/9781118332344.ch11.

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McCann, Tom. "Fossils and Paleoecology." In Pocket Guide Geology in the Field, 147–60. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63082-2_6.

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Saraswati, Pratul Kumar. "Ecology and Paleoecology." In Larger Benthic Foraminifera Through Space and Time, 103–23. Cham: Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-57631-7_5.

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Andrews, Peter, Sylvia Hixson Andrews, Tania King, Yolanda Fernández-Jalvo, and Manuel Nieto-Díaz. "Paleoecology of Azokh 1." In Azokh Cave and the Transcaucasian Corridor, 305–20. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-24924-7_15.

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Maletz, Jörg, and Denis E. B. Bates. "Paleoecology of the Pterobranchia." In Graptolite Paleobiology, 50–75. Chichester, UK: John Wiley & Sons, Ltd, 2017. http://dx.doi.org/10.1002/9781118515624.ch4.

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Caldwell, Michael Wayne. "Ancient Snake Lizard Paleoecology." In The Origin of Snakes, 165–91. Boca Raton : Taylor & Francis, 2019.: CRC Press, 2019. http://dx.doi.org/10.1201/9781315118819-4.

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Smykatz-Kloss, W., and P. Felix-Henningsen. "The Importance of Desert Margins as Indicators for Global Climatic Fluctuations (Introduction)." In Paleoecology of Quaternary Drylands, 1–3. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_1.

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Eitel, Bernhard, Wolf Dieter Blümel, and Klaus Hüser. "Palaeoenvironmental Transitions Between 22 ka and 8 ka in Monsoonally Influenced Namibia." In Paleoecology of Quaternary Drylands, 167–94. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_10.

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Conference papers on the topic "Paleoecology"

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Politova, N. V. "Geology of seas and oceans: Proceedings of XXIV International Conference on Marine Geology. Vol. I." In XXIV International Conference on Marine Geology. Shirshov Institute of Oceanology Publishing House, Russian Academy of Sciences, 2021. http://dx.doi.org/10.29006/978-5-6045110-4-6.

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Abstract:
The reports of marine geologists, geophysics, geochemists and other specialists of marine science at XXIV International Conference on Marine Geology in Moscow are published in four volumes. Volume I includes reports devoted to the problems of paleooceanology, paleoecology, biostratigraphy, cross correlation of deposits and of geoecology, pollution of the World Ocean.
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Laflamme, Marc, Seyed Hamid Vaziri, Mahmoud Reza Majidifard, and Simon Darroch. "LATE EDIACARAN DIVERSITY AND PALEOECOLOGY FROM CENTRAL IRAN." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357475.

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Wierenga, Matthew Wayne, and Ralph Stearley. "PALEOECOLOGY AND TAPHONOMY OF THE GRASSY MOUNTAIN FORMATION." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-312282.

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Lamsdell, James C. "EXPLORING DRIVERS OF MORPHOLOGICAL SHIFTS THROUGH PHYLOGENETIC PALEOECOLOGY." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312489.

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Foster, William J., Silvia Danise, Gregory D. Price, and Richard J. Twitchett. "PALEOECOLOGY OF THE LOWER TRIASSIC SERVINO FORMATION, ITALY." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289084.

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Chipman, Melissa, and Joseph Napier. "THE POWER OF PALEOECOLOGY FOR UNDERSTANDING DISTURBANCE REGIMES." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-381604.

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Ditmar, Jolene M., Maree Kutcher, Bryan Rue, and Nicole Bonuso. "THE PALEOECOLOGY OF PLEISTOCENE OYSTER BEDS, SAN PEDRO, CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274644.

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Pilaar Birch, Suzanne E. "MOBILIZING FAUNAL ISOTOPE DATA WITHIN THE NEOTOMA PALEOECOLOGY DATABASE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356829.

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Paradis, Michael J. "RECONSTRUCTION OF LATE-GLACIAL MARINE PALEOECOLOGY IN NORRIDGEWOCK, MAINE." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311232.

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Ditmar, Jolene M., and Nicole Bonuso. "A PALEOECOLOGY OF PLEISTOCENE OYSTER BEDS, SAN PEDRO, CALIFORNIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284257.

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Reports on the topic "Paleoecology"

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Clague, J. J., and G. M. Macdonald. Paleoecology and paleoclimatology [Chapter 1: Quaternary geology of the Canadian Cordillera]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127943.

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Stevens, D. S. P. Late Pleistocene paleoecology of Dalton Gulch, Tofty mining district, central Alaska. Alaska Division of Geological & Geophysical Surveys, July 2024. http://dx.doi.org/10.14509/31093.

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Sanchez, T. M., J. L. Benedetto, and E. Brussa. Late Ordovician Stratigraphy, Paleoecology, and Sea Level Changes in the Argentine Precordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132193.

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Higgins, A. C., B. C. Richards, and C. M. Henderson. Conodont biostratigraphy and paleoecology of the uppermost Devonian and Carboniferous of the Western Canada Sedimentary Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132439.

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Grigelis, A., and P. Ascoli. Middle Jurassic-Early Cretaceous foraminiferal zonation and paleoecology of offshore eastern Canada and the East European Platform. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/203755.

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Schweger, C. E. Paleoecology of the western Canadian Ice - Free Corridor [Chapter 7: Quaternary Environments in Canada As Documented By Paleobotanical Case Histories]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131561.

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Jackson, L. E., D. G. Froese, A. M. Telka, J. A. Westgate, S J Preece, J. E. Storer, and C A Huscroft. Late Cenozoic geology, Ancient Pacific Margin NATMAP Project, report 5: paleoecology and proxy climatic change records, south Klondike placer region, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213068.

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Pinney, D. S., and D. M. Hopkins. Late Pleistocene paleoecology of Dalton Gulch, Tofty mining district, central Alaska (poster): Canadian Quaternary Association Meeting, Whitehorse, Yukon Territory, Canada, August 20-29, 2001. Alaska Division of Geological & Geophysical Surveys, August 2001. http://dx.doi.org/10.14509/21841.

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Marcot, Bruce G., L. K. Croft, J. F. Lehmkuhl, R. H. Naney, C. G. Niwa, W. R. Owen, and R. E. Sandquist. Macroecology, paleoecology, and ecological integrity of terrestrial species and communities of the interior Columbia basin and northern portions of the Klamath and Great Basins. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 1998. http://dx.doi.org/10.2737/pnw-gtr-410.

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Heckel, Philip H., and John W. Swade. Conodont distribution, paleoecology, and preliminary biostratigraphy of the Upper Cherokee and Marmaton groups (Upper Desmoinesian, Middle Pennsylvanian) from two cores in south-central Iowa. Iowa City, Iowa: Iowa Geological Survey, January 1985. http://dx.doi.org/10.17077/rep.006529.

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