Journal articles: 'Geology Paleoclimatology Paleoclimatology Geology'

1

KANO, Akihiro. "Perspectives in carbonate paleoclimatology." Japanese Magazine of Mineralogical and Petrological Sciences 33, no. 3 (2004): 136–40. http://dx.doi.org/10.2465/gkk.33.136.

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Barnes, Christopher R. "Paleoceanography and paleoclimatology: an Earth system perspective." Chemical Geology 161, no. 1-3 (September 1999): 17–35. http://dx.doi.org/10.1016/s0009-2541(99)00079-0.

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Kohl, H. "Quaternary paleoclimatology. Methods of paleoclimatic reconstruction." Quaternary Science Reviews 4, no. 4 (1985): ix—x. http://dx.doi.org/10.1016/0277-3791(85)90010-1.

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Ruiz, Daniela P., M. Sol Raigemborn, Mariana Brea, and Roberto R. Pujana. "Paleocene Las Violetas Fossil Forest: Wood anatomy and paleoclimatology." Journal of South American Earth Sciences 98 (March 2020): 102414. http://dx.doi.org/10.1016/j.jsames.2019.102414.

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Formoso, Milton L. L. "Some topics on geochemistry of weathering: a review." Anais da Academia Brasileira de Ciências 78, no. 4 (December 2006): 809–20. http://dx.doi.org/10.1590/s0001-37652006000400014.

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Weathering is a complex process comprising physical disaggregation, chemical and biological decomposition of rocks and minerals transforming complex structure minerals in simpler ones. Hydrolysis of silicates is perhaps the most important process but associated certainly to biological weathering. It is discussed the role ofwaters: activities/concentrations of chemical species, pH, Eh, importance of complexes. Weathering is not only a destructive process. It can concentrate chemical species and form mineral deposits (kaolin, bauxite, Fe, Mn, P, Nb, Au). Weathering studies are important in pedology, engineering geology, hydrogeology, paleoclimatology and ecology. The use of stonemeal is based upon the study of rock weathering.

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Parrish, Judith Totman. "Paleoecology, Paleogeography, and Paleoclimatology: A Tribute to A. M. Ziegler on His Retirement." Journal of Geology 112, no. 6 (November 2004): 623–24. http://dx.doi.org/10.1086/424865.

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Jacobs, Louis L., Octávio Mateus, Michael J. Polcyn, Anne S. Schulp, Christopher R. Scotese, Argyha Goswami, Kurt M. Ferguson, John A. Robbins, Diana P. Vineyard, and André Buto Neto. "Cretaceous paleogeography, paleoclimatology, and amniote biogeography of the low and mid-latitude South Atlantic Ocean." Bulletin de la Société Géologique de France 180, no. 4 (July 1, 2009): 333–41. http://dx.doi.org/10.2113/gssgfbull.180.4.333.

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Abstract The Cretaceous tropical Atlantic Ocean was the setting for an initial tectonically controlled late Aptian shallow water (≤ 300 m) connection between the northern and southern portions of the Atlantic, followed by a deep-water connection by the Turonian. Ocean currents changed with deepening of the South Atlantic and progressive widening of the Equatorial Atlantic Gateway. Aptian evaporite deposition came to a halt. The Albian-Turonian interval includes a trend toward increasing sea level and was characterized by globally warm sea surface temperatures. Productive areas of coastal upwelling led to the deposition of organic-rich sediments varying in position along the African coast with time, culminating in the Benguela Upwelling that commenced in the Miocene. The drift of Africa in the Late Cretaceous indicates that throughout most of this period, the coastal area around the fossil locality of Iembe, north of Luanda, Angola, lay in arid latitudes (15o S to 30o S), which are generally characterized by sparse vegetation. This presumption is consistent with the utter lack of macroscopic terrestrial plant debris washed into near shore sedimentary environments and indicates that organic rich marine shales have a minimal terrestrial carbon component. The connection of the North and South Atlantic oceans severed a direct terrestrial dispersal route between South America and Africa, but opened a north-south dispersal route for marine amniotes. This seaway was used by late Turonian mosasaurs and sea turtles as evidenced by Angolasaurus and a new turtle taxon close to Sandownia, both found at Iembe and derived from northern clades. The presence of a sauropod in late Turonian sediments, also from Iembe, suggests that this animal was tolerant of warm, arid conditions as the desert elephants of Namibia are today. Further, it suggests that the waning terrestrial dispersal route between South America and Africa was situated in a region where high temperature, low rainfall, and sparse vegetation would be expected to restrict the movement of more mesic and ecologically sensitive species.

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Kooman, Jeroen P. "Geology, Paleoclimatology and the Evolution of the Kidney: Some Explorations into the Legacy of Homer Smith." Blood Purification 33, no. 4 (2012): 263–74. http://dx.doi.org/10.1159/000337095.

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Evans, M. N., S. E. Tolwinski-Ward, D. M. Thompson, and K. J. Anchukaitis. "Applications of proxy system modeling in high resolution paleoclimatology." Quaternary Science Reviews 76 (September 2013): 16–28. http://dx.doi.org/10.1016/j.quascirev.2013.05.024.

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Trouet, Valerie, and Geert Jan Van Oldenborgh. "KNMI Climate Explorer: A Web-Based Research Tool for High-Resolution Paleoclimatology." Tree-Ring Research 69, no. 1 (January 2013): 3–13. http://dx.doi.org/10.3959/1536-1098-69.1.3.

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Adetunji, J. R., and C. A. Kogbe. "Geology, paleoclimatology and laterite genesis in the Gada sector of the Trans-Saharan seaway in northwestern Nigeria." Journal of African Earth Sciences (1983) 6, no. 5 (January 1987): 643–53. http://dx.doi.org/10.1016/0899-5362(87)90003-0.

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Izart, A., R. F. Sachsenhofer, V. A. Privalov, M. Elie, E. A. Panova, V. A. Antsiferov, D. Alsaab, et al. "Stratigraphic distribution of macerals and biomarkers in the Donets Basin: Implications for paleoecology, paleoclimatology and eustacy." International Journal of Coal Geology 66, no. 1-2 (February 2006): 69–107. http://dx.doi.org/10.1016/j.coal.2005.07.002.

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Giral, Sylvie, Samuel M. Savin, Jean-Pierre Girard, and Daniel B. Nahon. "The oxygen isotope geochemistry of kaolinites from lateritic profiles: implications for pedology and paleoclimatology." Chemical Geology 107, no. 3-4 (July 1993): 237–40. http://dx.doi.org/10.1016/0009-2541(93)90182-i.

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Tewari, Rajni, Sankar Chatterjee, Deepa Agnihotri, and Sundeep K. Pandita. "Glossopteris flora in the Permian Weller Formation of Allan Hills, South Victoria Land, Antarctica: Implications for paleogeography, paleoclimatology, and biostratigraphic correlation." Gondwana Research 28, no. 3 (October 2015): 905–32. http://dx.doi.org/10.1016/j.gr.2015.02.003.

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Tamar-Agha, Mazin Y., Farhad A. Hakeem, and Ahmad M. Aqrawi. "The sedimentology and paleoclimatology of Early Triassic regional marine oxic event (Beduh Formation), Kurdistan region – Northern Iraq." Journal of African Earth Sciences 163 (March 2020): 103742. http://dx.doi.org/10.1016/j.jafrearsci.2019.103742.

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KELLOGG, THOMAS B. "Late Quaternary paleoclimatology and paleooceanography of the Labrador Sea and Baffin Bay: an alternative viewpoint." Boreas 15, no. 4 (January 16, 2008): 331–43. http://dx.doi.org/10.1111/j.1502-3885.1986.tb00940.x.

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Keinan, Jonathan, Miryam Bar-Matthews, Avner Ayalon, Tami Zilberman, Amotz Agnon, and Amos Frumkin. "Paleoclimatology of the Levant from Zalmon Cave speleothems, the northern Jordan Valley, Israel." Quaternary Science Reviews 220 (September 2019): 142–53. http://dx.doi.org/10.1016/j.quascirev.2019.07.018.

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Marret, Fabienne, and Jean-Louis Turon. "Paleohydrology and paleoclimatology off Northwest Africa during the last glacial-interglacial transition and the Holocene: Palynological evidences." Marine Geology 118, no. 1-2 (April 1994): 107–17. http://dx.doi.org/10.1016/0025-3227(94)90115-5.

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19

Condron, Alan, Anthony J. Joyce, and Raymond S. Bradley. "Arctic sea ice export as a driver of deglacial climate." Geology 48, no. 4 (January 31, 2020): 395–99. http://dx.doi.org/10.1130/g47016.1.

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Abstract A widespread theory in paleoclimatology suggests that changes in freshwater discharge to the Nordic (Greenland, Norwegian, and Icelandic) Seas from ice sheets and proglacial lakes over North America played a role in triggering episodes of abrupt climate change during deglaciation (21–8 ka) by slowing the strength of the Atlantic Meridional Overturning circulation (AMOC). Yet, proving this link has been problematic, as climate models are unable to produce centennial-to-millennial–length reductions in overturning from short-lived outburst floods, while periods of iceberg discharge during Heinrich Event 1 (ca. 16 ka) may have occurred after the climate had already begun to cool. Here, results from a series of numerical model experiments are presented to show that prior to deglaciation, sea ice could have become tens of meters thick over large parts of the Arctic Basin, forming an enormous reservoir of freshwater independent from terrestrial sources. Our model then shows that deglacial sea-level rise, changes in atmospheric circulation, and terrestrial outburst floods caused this ice to be exported through Fram Strait, where its subsequent melt freshened the Nordic Seas enough to weaken the AMOC. Given that both the volume of ice stored in the Arctic Basin and the magnitude of the simulated export events exceed estimates of the volumes and fluxes of meltwater periodically discharged from proglacial Lake Agassiz, our results show that non-terrestrial freshwater sources played an important role in causing past abrupt climate change.

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Chen, M. T., C. P. Chang, and Y. P. Chang. "Introduction to the special issue “New Global Perspectives on Paleontology, Stratigraphy, Paleoceanography, Paleoclimatology, and Tectonics in the East Asia and Western Pacific”." Journal of Asian Earth Sciences 69 (June 2013): 1–2. http://dx.doi.org/10.1016/j.jseaes.2013.04.013.

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21

Rinderknecht, Chanse J., Franek J. Hasiuk, and Stephan C. Oborny. "Mg zonation and heterogeneity in low-Mg calcite microcrystals of a depositional chalk." Journal of Sedimentary Research 91, no. 8 (August 3, 2021): 795–811. http://dx.doi.org/10.2110/jsr.2020.173.

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ABSTRACT Diagenetic low-magnesium calcite (LMC) microcrystals constitute the framework that hosts most micropores in limestone reservoirs and therefore create the storage capacity for hydrocarbons, water, and anthropogenic CO2. Limestones dominated by LMC microcrystals are also commonly used for paleoclimate reconstructions and chemostratigraphic correlations. LMC microcrystals are well known to exhibit a range of textures (e.g., granular, fitted, clustered), but there exists uncertainty with regard to how these textures form. One hypothesis is that during crystal growth, Mg is incorporated into diagenetic overgrowths (cement), where the chemical zonation and microtexture may reflect diagenetic processes. To evaluate small-scale geochemical zonation in LMC microcrystals, this study uses scanning electron microscopy (SEM) and energy-dispersive spectroscopy (EDS) to measure the Mg/Ca ratio across the interiors of LMC granular microcrystals from a Late Cretaceous marine chalk from the Tor Fm. (Norwegian North Sea). Mg/Ca zonation was identified in all LMC microcrystals with a diameter > 5 μm. Generally, the cores of large crystals have lower Mg/Ca (≈ 5.9 mmol/mol) and the rims have elevated Mg/Ca (≈ 13 mmol/mol). Smaller microcrystals (< 5 μm) show no resolvable zonation, but do exhibit a wide range in Mg/Ca content from 2.9 to 32.2 mmol/mol. Measured Mg/Ca values are arbitrarily divided into three populations: low Mg (average ≈ 5.9 mmol/mol), intermediate Mg (average ≈ 13.3 mmol/mol), and high Mg (average ≈ 20 mmol/mol). The observed zonation and Mg enrichment within LMC microcrystals is interpreted to reflect depositional as well as multiple diagenetic signals, such as constructive precipitation through recrystallization and pore-filling cementation. Although chalk from the Tor Fm. is dominated by granular euhedral LMC microcrystals, using SEM-EDS to find Mg/Ca heterogeneity in other LMC microcrystal textures may provide insight into the diagenetic processes that create textural variations in micropore-dominated limestones. The Mg data also more broadly suggest that there is useful, measurable diagenetic information in material that is otherwise considered homogeneous. Distinguishing between possible primary compositions and secondary cementation has implications for studies that rely on the primary chemistry of fine-grained carbonate deposits (e.g., micrite), such as paleoclimatology, Mg paleothermometry, and chemostratigraphy.

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Weedon, Graham P. "SALTZMAN, B. 2002. Dynamical Paleoclimatology. Generalized Theory of Global Climate Change. International Geophysics Series Volume 80. xxix + 354 pp. San Diego: Harcourt–Academic Press (Elsevier Science). Price £46.95 (hard covers). ISBN 0 12 617331 1." Geological Magazine 140, no. 6 (November 2003): 734–35. http://dx.doi.org/10.1017/s001675680333883x.

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Francis, Jane. "T. J. Crowley & G. R. North 1991. Paleoclimatology. Oxford Monographs on Geology and Geophysics no. 16. vii + 339 pp. New York, Oxford: Oxford University Press. Price £45.00 (hard covers). ISBN 0 19 503963 7." Geological Magazine 130, no. 2 (March 1993): 283. http://dx.doi.org/10.1017/s0016756800010062.

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Vasiliev, S. S., and V. A. Dergachev. "The ~ 2400-year cycle in atmospheric radiocarbon concentration: bispectrum of <sup>14</sup><i>C</i> data over the last 8000 years." Annales Geophysicae 20, no. 1 (January 31, 2002): 115–20. http://dx.doi.org/10.5194/angeo-20-115-2002.

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Abstract. We have carried out power spectrum, time-spectrum and bispectrum analyses of the long-term series of the radiocarbon concentrations deduced from measurements of the radiocarbon content in tree rings for the last 8000 years. Classical harmonic analysis of this time series shows a number of periods: 2400, 940, 710, 570, 500, 420, 360, 230, 210 and 190 years. A principle feature of the time series is the long period of ~ 2400 years, which is well known. The lines with periods of 710, 420 and 210 years are found to be the primary secular components of power spectrum. The complicated structure of the observed power spectrum is the result of ~ 2400-year modulation of primary secular components. The modulation induces the appearance of two side lines for every primary one, namely lines with periods of 940 and 570 years, of 500 and 360 years, and 230 and 190 years. The bispectral analysis shows that the parameters of carbon exchange system varied with the ~ 2400-year period during the last 8000 years. Variations of these parameters appear to be a climate effect on the rate of transfer of 14C between the atmosphere and the the ocean.Key words. Meteorology and atmospheric dynamics (climatology; ocean-atmosphere interaction; paleoclimatology)

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van Andel, Tj H. "CRONIN, T. M. 1999. Principles of Paleoclimatology. Perspectives in Paleobiology and Earth History Series. xv+560 pp. New York: Columbia University Press. Price £48.00, US $75.00 (hard covers), £20.50, US $32.00 (paperback). ISBN 0 231 10954 7; 0 231 10955 5 (pb)." Geological Magazine 137, no. 4 (July 2000): 463–79. http://dx.doi.org/10.1017/s0016756800214416.

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Mahaney, William C. "Book Review: Paleoclimatology by Th. J. Crowley and G.R. North. Oxford University Press, New York/Clarendon Press, Oxford. 1996. Oxford Monographs on Geology and Geophysics, Vol. 18 (349 pp.). £26.95. ISBN 0-510533-8 (paperback)." Journal of Quaternary Science 13, no. 1 (January 1998): 93–94. http://dx.doi.org/10.1002/(sici)1099-1417(199801/02)13:1<93::aid-jqs340>3.0.co;2-z.

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Conchon, G. "Paleogeographie et paleoclimatologie de la Corse au Quaternaire; chronologie des evenements." Bulletin de la Société Géologique de France IV, no. 4 (July 1, 1988): 587–94. http://dx.doi.org/10.2113/gssgfbull.iv.4.587.

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Cermak, Vladimir, Alan Beck, and Valiya Hamza. "International Heat Flow Commission: History and Accomplishments over the last fifty-five years." International Journal of Terrestrial Heat Flow and Applications 1, no. 1 (April 26, 2018): 1–5. http://dx.doi.org/10.31214/ijthfa.v1i1.17.

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The study of the earth's internal heat plays an important role in understanding the Earth's origin, internal constitution, and plate tectonics. The outflow of heat from the Earth's interior is, energy-wise, the most impressive terrestrial phenomenon. The present rate of heat loss is estimated to be about 1021 joules per year, which is orders of magnitude greater than the energy dissipation of earthquakes or heat loss from volcanic eruptions. Knowledge of terrestrial heat flow is essential in investigating the internal thermal field of the Earth. Initially focus has been on measurements of underground temperatures and thermal properties of geologic materials, assessment of sources and sinks of heat, institution of global data base, development of thermal models of crust and qualification of geothermal energy resources. During later stages, other implications of heat flow studies has also been recognized in fields such as paleoclimatology, global warming, exploration geophysics and hydrogeology. The International Heat Flow Commission – IHFC plays a guiding role in development of such investigations.

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Ruiz-Sánchez, Francisco J. "RECENSIÓN. Advances in Angiosperm Paleobotany and Paleoclimatic Reconstruction – Contributions Honouring David L. Dilcher and Jack A. Wolfe." Spanish Journal of Palaeontology 23, no. 2 (February 14, 2021): 314. http://dx.doi.org/10.7203/sjp.23.2.20414.

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La serie Courier Forschungsinstitut Senckenberg (Cfs) publica artículos de interés internacional en el ámbito de la geología y paleontología, con especial énfasis en la publicación de volúmenes especiales que resuman el conocimiento actual sobre alguna de las materias encuadradas en estas temáticas. El volumen 258 incluye parte de los trabajos presentados durante el encuentro de investigadores en Paleobotánica en Gainesville (Florida), auspiciado por el Museo de Historia Natural de Florida. Este volumen se estructura en dos partes bien definidas. La primera incluye las semblanzas personales y académicas de los homenajeados incluyendo un listado de sus publicaciones. La segunda parte recoge 14 contribuciones que abordan los últimos avances en el campo de la Paleobotánica del Cretácico y del Cenozoico y de la Paleoclimatología. Nos encontramos con una obra de gran interés para conocer la trayectoria científica de J. Wolfe y D. Dilcher. Los trabajos publicados en este volumen permiten conocer los avances más significativos alcanzados en los últimos años en el conocimiento del registro fósil de angiospermas y de las interpretaciones climáticas que a partir de estos datos pueden realizarse. Las cuestiones tratadas por los diferentes trabajos de este volumen no abarcan ni mucho menos el total de líneas de investigación que se desarrollan sobre el grupo de las angiospermas. No obstante, este volumen ofrece una magnífica oportunidad para conocer el estado actual de nuestro conocimiento sobre algunos aspectos del último de los grandes planes estructurales de plantas aparecido sobre la tierra.

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Soreghan, G. S., and A. S. Cohen. "Scientific drilling and the evolution of the earth system: climate, biota, biogeochemistry and extreme systems." Scientific Drilling 16 (November 5, 2013): 63–72. http://dx.doi.org/10.5194/sd-16-63-2013.

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Abstract. A US National Science Foundation-funded workshop occurred 17–19 May 2013 at the University of Oklahoma to stimulate research using continental scientific drilling to explore earth's sedimentary, paleobiological and biogeochemical record. Participants submitted 3-page "pre-proposals" to highlight projects that envisioned using drill-core studies to address scientific issues in paleobiology, paleoclimatology, stratigraphy and biogeochemistry, and to identify locations where key questions can best be addressed. The workshop was also intended to encourage US scientists to take advantage of the exceptional capacity of unweathered, continuous core records to answer important questions in the history of earth's sedimentary, biogeochemical and paleobiologic systems. Introductory talks on drilling and coring methods, plus best practices in core handling and curation, opened the workshop to enable all to understand the opportunities and challenges presented by scientific drilling. Participants worked in thematic breakout sessions to consider questions to be addressed using drill cores related to glacial–interglacial and icehouse–greenhouse transitions, records of evolutionary events and extinctions, records of major biogeochemical events in the oceans, reorganization of earth's atmosphere, Lagerstätte and exceptional fossil biota, records of vegetation–landscape change, and special sampling requirements, contamination, and coring tool concerns for paleobiology, geochemistry, geochronology, and stratigraphy–sedimentology studies. Closing discussions at the workshop focused on the role drilling can play in studying overarching science questions about the evolution of the earth system. The key theme, holding the most impact in terms of societal relevance, is understanding how climate transitions have driven biotic change, and the role of pristine, stratigraphically continuous cores in advancing our understanding of this linkage. Scientific drilling, and particularly drilling applied to continental targets, provides unique opportunities to obtain continuous and unaltered material for increasingly sophisticated analyses, tapping the entire geologic record (extending through the Archean), and probing the full dynamic range of climate change and its impact on biotic history.

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"An exciting textbook of Quaternary paleoclimatology." Boreas 15, no. 1 (January 16, 2008): 99. http://dx.doi.org/10.1111/j.1502-3885.1986.tb00748.x.

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Marita T. Bradshaw, Albert T. Brake. "Paleoclimatology of Australia During the Pangaean Interval: ABSTRACT." AAPG Bulletin 79 (1995). http://dx.doi.org/10.1306/7834e200-1721-11d7-8645000102c1865d.

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FLETCHER, CHARLES H., University of. "Warm to Cold Polar Climate Transitions Over the Last 15,000 Years: A Paleoclimatology Record from the Raised Beaches of Northern Norway." AAPG Bulletin 75 (1991). http://dx.doi.org/10.1306/20b241a0-170d-11d7-8645000102c1865d.

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Al ysa M. Keller. "Paleoclimatologic Analysis of an Upper Jurassic Petrified Forest, Ulgay Khid, Southeastern Mongolia: ABSTRACT." AAPG Bulletin 78 (1994). http://dx.doi.org/10.1306/a26004b7-171b-11d7-8645000102c1865d.

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Wood, Gordon D., Merrell A. Miller,. "Abstract: Paleoclimatologic, Paleoecologic and Biostratigraphic Significance of the Middle Cretaceous Elaterate Microfloral Province, Gondwana." AAPG Bulletin 82 (1998) (1998). http://dx.doi.org/10.1306/1d9bd489-172d-11d7-8645000102c1865d.

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Journal articles on the topic 'Geology Paleoclimatology Paleoclimatology Geology'

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