Literatura académica sobre el tema "Pleistocene Climate Changes"
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Artículos de revistas sobre el tema "Pleistocene Climate Changes"
Diester-Haass, Liselotte, Katharina Billups y Caroline Lear. "Productivity changes across the mid-Pleistocene climate transition". Earth-Science Reviews 179 (abril de 2018): 372–91. http://dx.doi.org/10.1016/j.earscirev.2018.02.016.
Texto completoVakulenko, N. V., V. M. Kotlyakov, F. Lambert y D. M. Sonechkin. "The role of the ocean in pleistocene climate changes". Doklady Earth Sciences 432, n.º 1 (mayo de 2010): 659–62. http://dx.doi.org/10.1134/s1028334x10050235.
Texto completoMäder, Geraldo, Priscilla M. Zamberlan, Ana Lucia A. Segatto, João R. Stehmann, Sandro L. Bonatto y Loreta B. Freitas. "When phylogeography meets niche suitability to unravel the evolutionary history of a shrub from the Brazilian Atlantic Forest". Botanical Journal of the Linnean Society 195, n.º 1 (3 de septiembre de 2020): 77–92. http://dx.doi.org/10.1093/botlinnean/boaa073.
Texto completoBender, Adrian M., Richard O. Lease, Lee B. Corbett, Paul R. Bierman, Marc W. Caffee, James V. Jones y Doug Kreiner. "Yukon River incision drove organic carbon burial in the Bering Sea during global climate changes at 2.6 and 1 Ma". Earth Surface Dynamics 10, n.º 5 (28 de octubre de 2022): 1041–53. http://dx.doi.org/10.5194/esurf-10-1041-2022.
Texto completoTimmermann, Axel, Kyung-Sook Yun, Pasquale Raia, Jiaoyang Ruan, Alessandro Mondanaro, Elke Zeller, Christoph Zollikofer et al. "Climate effects on archaic human habitats and species successions". Nature 604, n.º 7906 (13 de abril de 2022): 495–501. http://dx.doi.org/10.1038/s41586-022-04600-9.
Texto completoJiménez-Moreno, Gonzalo, Hülya Alçiçek, M. Cihat Alçiçek, Lars van den Hoek Ostende y Frank P. Wesselingh. "Vegetation and climate changes during the late Pliocene and early Pleistocene in SW Anatolia, Turkey". Quaternary Research 84, n.º 3 (noviembre de 2015): 448–56. http://dx.doi.org/10.1016/j.yqres.2015.09.005.
Texto completoMazza, Paul P. A. y Adele Bertini. "Were Pleistocene hippopotamuses exposed to climate-driven body size changes?" Boreas 42, n.º 1 (24 de octubre de 2012): 194–209. http://dx.doi.org/10.1111/j.1502-3885.2012.00285.x.
Texto completoTakakura, Jun. "Rethinking the Disappearance of Microblade Technology in the Terminal Pleistocene of Hokkaido, Northern Japan: Looking at Archaeological and Palaeoenvironmental Evidence". Quaternary 3, n.º 3 (20 de julio de 2020): 21. http://dx.doi.org/10.3390/quat3030021.
Texto completoSirenko, О. А. "CHANGES IN THE CLIMATE AND DENDROFLORA OF THE NORTHEASTERN PART OF UKRAINE IN THE LATE MIOCENE—EARLY PLEISTOCENE (ACCORDING TO PALYNOLOGICAL DATA)". Ukrainian geographical journal 2022, n.º 3 (noviembre de 2022): 21–28. http://dx.doi.org/10.15407/ugz2022.03.021.
Texto completoRousseau, Denis-Didier, Witold Bagniewski y Michael Ghil. "Abrupt climate changes and the astronomical theory: are they related?" Climate of the Past 18, n.º 2 (11 de febrero de 2022): 249–71. http://dx.doi.org/10.5194/cp-18-249-2022.
Texto completoTesis sobre el tema "Pleistocene Climate Changes"
Chalk, Thomas B. "Boron based insights into Plio-Pleistocene carbon cycle changes and global climate evolution". Thesis, University of Southampton, 2014. https://eprints.soton.ac.uk/374239/.
Texto completoWeirauch, Daniel R. "A high-resolution record of climate instability spanning ~1.0 million years across the mid-Pleistocene transition". Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 131 p, 2007. http://proquest.umi.com/pqdweb?did=1472642111&sid=21&Fmt=2&clientId=8331&RQT=309&VName=PQD.
Texto completoEastwood, Rodney Gordon y N/A. "Ant Association and Speciation in Lycaenidae (Lepidoptera): Consequences of Novel Adaptations and Pleistocene Climate Changes". Griffith University. Australian School of Environmental Studies, 2006. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20071130.134932.
Texto completoEastwood, Rodney Gordon. "Ant Association and Speciation in Lycaenidae (Lepidoptera): Consequences of Novel Adaptations and Pleistocene Climate Changes". Thesis, Griffith University, 2006. http://hdl.handle.net/10072/365668.
Texto completoThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Australian School of Environmental Studies
Full Text
Muteveri, Tinashe. "Effect of pleistocene climatic changes on the evolutionary history of South African intertidal gastropods". Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/79791.
Texto completoENGLISH ABSTRACT: Historical vicariant processes due to glaciations, resulting from the large-scale environmental changes during the Pleistocene (0.012-2.6 million years ago, Mya), have had significant impacts on the geographic distribution of species, especially also in marine systems. The motivation for this study was to provide novel information that would enhance ongoing efforts to understand the patterns of biodiversity on the South African coast and to infer the abiotic processes that played a role in shaping the evolution of taxa confined to this region. The principal objective of this study was to explore the effect of Pleistocene climate changes on South Africa′s marine biodiversity using five intertidal gastropods (comprising four rocky shore species Turbo sarmaticus, Oxystele sinensis, Oxystele tigrina, Oxystele variegata, and one sandy shore species Bullia rhodostoma) as indicator species. Sequence data obtained from partial segments of the mitochondrial cytochrome oxidase c subunit 1 (COI), and the nuclear ribosomal DNA (encompassing part of 5.8S, second Internal Transcribed Spacer and part of 28S, hereinafter called ITS2; or comprising part of the first Internal Transcribed Spacer, 5.8S, second Internal Transcribed Spacer and part of 28S, hereinafter called ITS), were used as genetic markers to construct phylogeographic patterns and to investigate demographic histories of the taxa. Population structure was investigated using haplotype network analyses, pairwise ΦST statistics, analysis of molecular variance (AMOVA), isolation by distance analyses, Bayesian analysis of population structure (BAPS) and coalescent analysis of gene flow. Demographic history was analysed through Fu′s Fs tests, mismatch distributions, and Bayesian skyline plots. Demographic analyses suggest that all five intertidal gastropods studied experienced demographic expansions dating to the late Pleistocene. The sandy shore direct developer B. rhodostoma began expansion after the LGM (c. 15 kya) whereas for the four rocky shore broadcast spawners (T. sarmaticus, O. sinensis, O. tigrina, and O. variegata) the onset of expansion coincided with or preceded the LGM (c. 25, 60, 50, 40 kya, respectively). Consistent with recent range expansions and gene flow patterns, the population genetic structure in all species was characterised by shallow or a lack of population differentiation. Oxystele variegata was an exception as it showed a deep disjunction, of late Pleistocene origin, between individuals in the west coast Namaqua Bioregion and those in the south coast Agulhas Bioregion. These results provide strong evidence of the vital role that Pleistocene climatic changes and current regimes played in shaping the nature and distribution of biodiversity on the South African coast. In addition, gene flow in all species, except O. tigrina, was remarkably asymmetrical with the regions around Cape Infanta and Port Elizabeth acting as source populations. Considering the generally weak population genetic structure and gene flow patterns detected for most gastropod species studied here, it is recommended that T. sarmaticus, O. sinensis, O. tigrina and B. rhodostoma be managed as panmictic populations, and that the region encompassing Cape Infanta, and Port Elizabeth should be prioritised for conservation as it appears to harbour source populations. Oxystele variegata was the only species showing distinct population structure and in this instance, species specific conservation efforts should recognize this divergence by treating the two genetic assemblages as distinct management units.
AFRIKAANSE OPSOMMING: Historiese vikariante prosesse kan toegeskryf word aan glasiasie, en het tot gevolg gehad dat grootskaalse veranderinge in die omgewing plaasgevind het tydens die Pleistoseen (,012 - 2.6 miljoen jaar gelede, Mjg). Dit het 'n beduidende impak gehad op die geografiese verspreiding van spesies, veral ook in die mariene stelsels. Die motivering vir hierdie studie was om nuwe data te voorsien wat sal bydrae tot die voortgesette pogings om die patrone van biodiversiteit langs die Suid-Afrikaanse kus te verstaan. Dit sou ook help om die abiotiese prosesse af te lei wat 'n rol gespeel het in die evolusie van taksa wat in hierdie streek voorkom. Die hoofdoel van hierdie studie was om die effek van die Pleistoseen klimaatsveranderinge op Suid-Afrika se mariene biodiversiteit te bepaal deur gebruik te maak van vyf intergety slak spesies as indikatore (vier wat in rotsagtige gebiede voorkom: Turbo sarmaticus, Oxystele sinensis, Oxystele tigrina, Oxystele variegata en 'n sanderige strand spesies: Bullia rhodostoma). Volgorde data verkry vanaf gedeeltelike segmente van die mitochondriale sitochroom oksidase c subeenheid 1 (COI), en die kern ribosomale DNA (bestaande uit 'n deel van 5.8S, tweede interne getranskribeerde spasieërders en 'n deel van 28S), hierna genoem ITS2 is gebruik as genetiese merkers om filogeografiese patrone te dokumenteer en ook om die demografiese geskiedenis van die spesies te ondersoek. Bevolking struktuur is ondersoek deur gebruik te maak van haplotipe netwerk analise, paarsgewyse ΦST statistiek, analise van molekulêre variansie (AMOVA), isolasie deur afstand analise, Bayesiaanse analise van die bevolking struktuur (BAPS) en analise van gene vloei. Demografiese geskiedenis is ontleed deur Fu se Fs toetse, misparing verdelings, en Bayesiaanse luglyn kurwes. Demografiese ontleding dui daarop dat al vyf die intergety slakke wat ondersoek is demografiese uitbreidings ervaar het wat terugdateer tot die einde van die Pleistoseen. Die sanderige strand direkte ontwikkelaar, B. rhodostoma, het die uitbreiding begin na die LGM (c. 15 Kya), terwyl vir die vier rotsagtige kusbewoners wat eiers oor 'n uitgebreide gebiede versprei (T. sarmaticus, O. sinensis, O. tigrina, en O. variegata) het die aanvang van die bevolkings uitbreiding saamgeval met die laaste galsiasie of dit voorafgegaan (c. 25, 60, 50, 40 Kya, onderskeidelik). In ooreenstemming met die onlangse reeks bevolkings uitbreidings, is die bevolking genetiese struktuur in alle spesies gekenmerk deur weinig differensiasie. Oxystele variegata was 'n uitsondering en het 'n ontwrigting van laat Pleistoceen oorsprong getoon tussen individue langs die weskus Namaqua Biostreek en dié in die suid kus Agulhas biostreek. Hierdie resultate voorsien sterk bewyse van die belangrike rol wat die Pleistoseen klimaatsveranderinge gespeel het in die vorming en verspreiding van biodiversiteit langs die Suid-Afrikaanse kus. Daarbenewens, geen vloei in alle spesies, behalwe O. tigrina, was merkwaardig asimmetries. Kaap Infanta en Port Elizabeth verteenwoordig moontlik die bron bevolkings. Met inagneming van die geringe bevolking genetiese struktuur en geenvloei patrone wat waargeneem is vir die meeste slak spesies wat bestudeer is, word dit aanbeveel dat T. sarmaticus, O. sinensis, O. tigrina en B. rhodostoma bestuur word as 'n panmiktiese bevolking, en dat die streek wat Kaap Infanta en Port Elizabeth insluit geprioritiseer moet word vir bewaring. Oxystele variegata was die enigste spesie wat duidelike bevolking struktuur getoon het en in hierdie geval, moet spesie spesifieke bewaringspogings aangewend word.
Heard, Joshua Andrews. "Late Pleistocene and Holocene Aged Glacial and Climatic Reconstructions in the Goat Rocks Wilderness, Washington, United States". PDXScholar, 2012. https://pdxscholar.library.pdx.edu/open_access_etds/557.
Texto completoRech, André Rodrigo 1985. "Walking through the flower fields = the role of time and space on the evolution of pollination strategies". [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/315723.
Texto completoTexto em português e inglês
Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Biologia
Made available in DSpace on 2018-08-24T19:39:30Z (GMT). No. of bitstreams: 1 Rech_AndreRodrigo_D.pdf: 2738650 bytes, checksum: 6bf617833a57ef7d0a29fdcd8d4cd53b (MD5) Previous issue date: 2014
Resumo: Os padrões encontrados em ecologia são resultado de processos contemporâneos interagindo com uma longa história de contingência. No entanto, poucos estudos têm buscado entender o papel relativo de fatores contemporâneos e pretéritos sobre padrões reprodutivos de plantas. No decorrer dessa tese foram consideradas essas duas dimensões (temporal e espacial) em estudos sobre polinização. A amplitude do estudo em relação ao tempo foi de horas até milênios, da mesma forma que para o espaço, para o qual se considerou desde metros até variações entre diferentes continentes na escala planetária. Os capítulos estão organizados em uma escala crescente de tempo e espaço. No primeiro capítulo foi considerada a variação fina de horas e metros no estudo sobre a polinização de algumas espécies de Davilla; nesse capítulo também são apresentados outros aspectos da história natural na família Dilleniaceae e uma abordagem filogenética para a evolução de algumas características florais. No capítulo 2, ao longo de vários anos, foi verificada a habilidade de visitantes florais depositar pólen, sua frequência e a importância de cada grupo de visitante nas flores de Knautia arvensis nesse período. O capítulo 3 demonstra variações no espaço tanto na morfologia floral e foliar como no crescimento do tubo polínico em diferentes testes de polinização, utilizando Curatella americana com populações distribuídas no Cerrado Brasileiro. No capítulo 4 é apresentada a variação espacial no sistema reprodutivo e a relação dos polinizadores com o nível de polinização cruzada e do passado climático com o nível de autopolinização espontânea, também tratando de C. americana. Para finalizar o capítulo 5 considera 50 inventários distribuidos ao redor do planeta categorizando as plantas em anemófilas ou zoófilas e demonstra o papel da precipitação (presente e passada) e da riqueza de espécies vegetais na prevalência de cada um dos modos de polinização. Como conclusão geral, fica clara a importância de se considerar as dimensões temporal e espacial nas interações entre plantas e polinizadores, a fim de entender como essas evoluem e como impactam na evolução da morfologia floral e nos sistemas de polinização
Abstract: Patterns in ecology are the products of current factors interacting with a longstanding history of contingency. Nevertheless, few studies have attempted to disentangle the contribution of past and current factors on plant reproduction patterns. Here we studied pollination considering both, spatial and temporal dimensions. Time variation goes from hours to millennia as well as space, whose importance was considered from meters to the whole planet. The chapter¿s sequence within the thesis is planned to go from the small to the large scale. We show the importance of fine grained variations such as hours and meters in the flower differentiation and pollination of two Davilla species in the chapter 1. In the chapter 2 we studied pollen deposition and visitation frequency in Knautia arvensis considering a year scale and showed the most important pollinator changing every year. In the Chapters 3 we used Curatella americana with populations studied across Brazilian Cerrado and show spatial variation in flower and leaf morphology and pollen tube growth. Chapter 4 also using C. americana shows the variation on the reproductive system across space, with cross-pollination related to pollinator availability and the level of autogamy underpinned by past climate. To finish, Chapter 5 deal with 50 community-based assessments of wind and animal pollination over the world and show the importance of precipitation (current and past) and plant species richness as major drivers of these proportion. As a general conclusion, it is clear that temporal and spatial factors cannot be ignored in spite to understand floral evolution and the interactions between plant and pollinators
Doutorado
Ecologia
Doutor em Ecologia
Lisiecki, Lorraine E. "Paleoclimate time series : new alignment and compositing techniques, a 5.3-MYR benthic [exponents] d18O stack, and analysis of Pliocene-Pleistocene climate transitions /". View online version; access limited to Brown University users, 2005. http://wwwlib.umi.com/dissertations/fullcit/3174639.
Texto completoFurini, Paulo Roberto. "Modelagem preditiva de distribuição passada e futura de Ficus adhatodifolia Schott., Ficus insipida Willd. e Ficus citrifolia Mil. (Moraceae)". Universidade de São Paulo, 2015. http://www.teses.usp.br/teses/disponiveis/59/59139/tde-26052015-143536/.
Texto completoThe Quaternary glaciations shaped the phylogeographic patterns of species in general. In some regions of South America (e.g.Cerrado and Caatinga) structural change was more pronounced and savannas predominated, whereas in other regions (e.g. Amazon and Atlantic Forest) changes were minor, forming areas of forest refuges. Species distribution Predictive Modeling uses associations between environmental variables and species occurrence records to estimate models that represent the environmental conditions favorable to the species. In the present study we chose three species of Neotropical Ficus with different ecological characteristics, representing two independent phylogenetic lineages, i.e., sections Americana (Ficus citrifolia) and Pharmacosycea (F.adhatodifolia and F.insipida). We generated models for the past (interglacial 140,000 years ago and Glacial 21,000 years ago), present and future scenarios (2050 and 2070 in optimistic and pessimistic scenarios) for the three study species using Maxent 3.3.3k program. Our results showed thatfor F. adhatodifolia the most important variables in the models were minimum temperature in the coldest month and precipitation in the driest month. For F.insipida the most important variables in the models were minimum temperature in the coldest month and annual precipitation. For F. citrifolia the most important variables in the models were minimum temperature in the coldest month and precipitation in the wettest month. The models designed for the interglacial stage showed areas of environmental suitability similar to the current scenario of the three species. During the glacial period F. adhatodifolia showed a considerable change in its range, occurring in regions considered refuges for some species. Ficus insipida had its environmental suitability decreased, but remained in the Amazon region, while F. citrifolia increased its area of suitability. In the future models (2050 and 2070) F.adhatodifolia showed a decrease in its range on both optimistic and pessimistic scenarios, F.insipida showed an increase in its area of environmental suitability and F.citrifolia has been decreasing and fragmentation in the Amazon region in the optimistic and pessimistic scenarios 2050 and optimistic 2070. The environmental requirements and the potential phylogeographic patterns of the study species are discussed in the context of the generated predictive models.
Tan, Ning. "Comprendre l’évolution de la cryosphère et du climat du Pliocène à la transition Plio-Pléistocène". Thesis, Université Paris-Saclay (ComUE), 2018. http://www.theses.fr/2018SACLV032/document.
Texto completoThis thesis is devoted tounderstanding the interaction betweencryosphere and climate from the mid Plioceneto the early Quaternary during the onset ofNorthern Hemisphere Glaciation (NHG).Firstly, we investigate the causes for thedevelopment and decay of the large but shortliving glaciation that occurred during MarineIsotope Stage 2 (M2, 3.264-¬3.312 Ma);Secondly, in the framework of the internationalPliocene Model Intercomparison Project(PLIOMIP2), we study the climate of Mid-Piacenzian Warm Period (MPWP, 3.3-3.0Ma).Thirdly, we explore the Plio-PleistoceneTransition (PPT, 3.0-2.5Ma) with anappropriate asynchronously coupled climatecryosphere model. Through these differentperiods, we provide a better understanding ofthe relationship between pCO2, tectonics andclimat during the transition from a warm andhigh-CO2 world to the cold and low-CO2Quaternary glaciations. This work also pointsout the necessity to further study the linkbetween ocean dynamics, carbon cycle andclimate
Libros sobre el tema "Pleistocene Climate Changes"
Avian community, climate, and sea-level changes in the Plio-Pleistocene of the Florida peninsula. Washington, DC: American Ornithologists' Union, 1998.
Buscar texto completoLittle, Martin Lewis. Pollen and grain size records in abyssal sediments of the northwest Pacific Ocean as proxies of Plio-Pleistocene climate change. St. Catharines, Ont: Brock University, Dept. of Earth Sciences, 2005.
Buscar texto completoMuller, R. Ice ages and astronomical causes: Data, spectral analysis, and mechanisms. London: Springer, 2000.
Buscar texto completo1929-, MacDonald Gordon J., ed. Ice ages and astronomical causes: Data, spectral analysis, and mechanisms. London: Springer, 2002.
Buscar texto completoLurcock, Pontus y Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.18.
Texto completoLurcock, Pontus y Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.18.
Texto completoLund, David Charles. Millennial-scale surface and deep water oscillations in the N.E. Pacific: Implications for late pleistocene climate change. 1997.
Buscar texto completoLund, David Charles. Millennial-scale surface and deep water oscillations in the N.E. Pacific: Implications for late pleistocene climate change. 1997.
Buscar texto completoBiodiversity response to climate change in the middle Pleistocene: The Porcupine Cave fauna from Colorado. Berkeley: University of California Press, 2004.
Buscar texto completoBarnosky, Anthony D. Biodiversity Response to Climate Change in the Middle Pleistocene: The Porcupine Cave Fauna from Colorado. University of California Press, 2004.
Buscar texto completoCapítulos de libros sobre el tema "Pleistocene Climate Changes"
Crucifix, Michel. "Pleistocene Glaciations". En Climate Changes in the Holocene, 77–106. Boca Raton : CRC Press, Taylor & Francis Group, 2018.: CRC Press, 2018. http://dx.doi.org/10.1201/9781351260244-3.
Texto completoDumont, Henri J. "Relict Distribution Patterns of Aquatic Animals: Another Tool in Evaluating Late Pleistocene Climate Changes in the Sahara and Sahel". En Palaeoecology of Africa and the Surrounding Islands, 1–24. London: Routledge, 2022. http://dx.doi.org/10.1201/9780203744529-1.
Texto completoFarmer, G. Thomas y John Cook. "Pleistocene Glaciations". En Climate Change Science: A Modern Synthesis, 407–27. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5757-8_21.
Texto completoBen-David, Ram. "Buildup and Breakdown of Sand Dune Barriers in the Drainage Basins of the NW Negev Desert, Israel, During Late Pleistocene to Holocene Climate Changes". En Engineering Geology for Society and Territory - Volume 3, 361–64. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09054-2_76.
Texto completoLeyden, Barbara W., Mark Brenner, David A. Hodell y Jason H. Curtis. "Late Pleistocene Climate in the Central American Lowlands". En Climate Change in Continental Isotopic Records, 165–78. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm078p0165.
Texto completoJouzel, Jean, Claude Lorius, Liliane Merlivat y Jean-Robert Petit. "Abrupt Climatic Changes: The Antarctic Ice Record during the Late Pleistocene". En Abrupt Climatic Change, 235–45. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3993-6_22.
Texto completoImbrie, John. "Abrupt Terminations of Late Pleistocene Ice Ages: A Simple Milankovitch Explanation". En Abrupt Climatic Change, 365–67. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3993-6_30.
Texto completoCowling, S. A. "Ecophysiological response of lowland tropical plants to Pleistocene climate". En Tropical Rainforest Responses to Climatic Change, 359–80. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-05383-2_13.
Texto completoMagaritz, Mordeckai y Glenn A. Goodfriend. "Movement of the Desert Boundary in the Levant from Latest Pleistocene to Early Holocene". En Abrupt Climatic Change, 173–83. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3993-6_17.
Texto completoPilaar Birch, Suzanne E. y Preston T. Miracle. "Human Response to Climate Change in the Northern Adriatic During the Late Pleistocene and Early Holocene". En Climate Change and Human Responses, 87–100. Dordrecht: Springer Netherlands, 2017. http://dx.doi.org/10.1007/978-94-024-1106-5_5.
Texto completoActas de conferencias sobre el tema "Pleistocene Climate Changes"
Fenton-samuels, Kelly y Suzanne OConnell. "ANTARCTIC CLIMATE CHANGES IN THE SCOTIA SEA AND THEIR UNDERLYING MECHANISMS DURING THE PLIO-PLEISTOCENE TRANSITION". En GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380531.
Texto completoZheltova, M., N. Zaretskaya y N. Burova. "ЗАЯЦ И ЧЕЛОВЕК НА ГЕОХРОНОЛОГИЧЕСКОЙ ШКАЛЕ ПАЛЕОЛИТА РУССКОЙ РАВНИНЫ". En Радиоуглерод в археологии и палеоэкологии: прошлое, настоящее, будущее. Материалы международной конференции, посвященной 80-летию старшего научного сотрудника ИИМК РАН, кандидата химических наук Ганны Ивановны Зайцевой. Samara State University of Social Sciences and Education, 2020. http://dx.doi.org/10.31600/978-5-91867-213-6-30-31.
Texto completoBenfield, Adam J., Sarah Ivory, Bailee N. Hodelka, Michael M. McGlue, Guleed A. H. Ali y Susan H. Zimmerman. "TERRESTRIAL ECOSYSTEM RESPONSE TO ABRUPT CLIMATE CHANGES DURING THE PLEISTOCENE-HOLOCENE TRANSITION AT MONO LAKE, CALIFORNIA, USA". En GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-354826.
Texto completoGutierrez, Evelin, Daniel F. Stockli, Jacob A. Covault y David Mohrig. "PLEISTOCENE TO HOLOCENE CLIMATE-MODULATED CHANGES IN FLUVIAL GEOMORPHOLOGY AND DETRITAL ZIRCON PROVENANCE IN CENTRAL TEXAS RIVERS". En GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355094.
Texto completoPustelnikovas, O. "Features of climate changes based on the chemical elements and palinological remnants distribution in the sediments and Late Pleistocene and Holocene deposits of the SE Baltic area". En 2012 IEEE/OES Baltic International Symposium (BALTIC). IEEE, 2012. http://dx.doi.org/10.1109/baltic.2012.6249162.
Texto completoPustelnikovas, O., M. Melesyte, E. Rudnickaite y D. Kaminskas. "The chemical elements and sedimentation types of deposits in the dug holes Dubičiai 1, 2 and Müšos Tyrelis as indicators of Late Pleistocene and Holocene climate changes". En 2012 IEEE/OES Baltic International Symposium (BALTIC). IEEE, 2012. http://dx.doi.org/10.1109/baltic.2012.6249161.
Texto completoBaxstrom, Kelli W. "APPALACHIAN ECOSYSTEM RESPONSE TO LATE PLEISTOCENE CLIMATE CHANGE". En GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316172.
Texto completoTripathi, Shubham. "Eastern Arabian Sea Climate Change during Mid-Pleistocene Transition". En Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.3284.
Texto completoSimpson, Andrew G. "DOES SEED DISPERSAL AFFECT RATE OF SPREAD DURING PLEISTOCENE CLIMATE CHANGE?" En GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320234.
Texto completoCerling, Thure, Tyler Huth, David Marchetti, David Bowling, Amy Ellwein, Benjamin Passey, Diego Fernandez, John Valley y Ian Orland. "Soil Pendant Carbonate Record of Climate Change in the Holocene and Late Pleistocene". En Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.346.
Texto completoInformes sobre el tema "Pleistocene Climate Changes"
Corbet, T. F. Evolution of patterns of regional groundwater flow in southeastern New Mexico: Response to post-Pleistocene changes in climate. Office of Scientific and Technical Information (OSTI), diciembre de 1994. http://dx.doi.org/10.2172/10114250.
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