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Relevant bibliographies by topics / Geology Paleoclimatology Paleoclimatology Geology

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Academic literature on the topic 'Geology Paleoclimatology Paleoclimatology Geology'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "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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Dissertations / Theses on the topic "Geology Paleoclimatology Paleoclimatology Geology"

1

Heine, Jan T. "Glacier advances at the Pleistocene/Holocene transition near Mount Rainier volcano, Cascade Range, USA /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/6748.

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Shunk, Aaron Driese Steven G. "Late Tertiary paleoclimate and stratigraphy of the Gray Fossil Site (eastern TN) and Pipe Creek Sinkhole (northcentral IN)." Waco, Tex. : Baylor University, 2009. http://hdl.handle.net/2104/5303.

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Smith, Alexander Ryan. "Sedimentology and Stratigraphy of Miocene-Age Glacial Deposits, Friis Hills, Antarctica." Thesis, North Dakota State University, 2011. https://hdl.handle.net/10365/29316.

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The Friis Hills is an isolated plateau standing as much as 600 m above surrounding topography in the McMurdo Dry Valleys region or Antarctica.Preserved on the plateau surface is a sequence of early to middle Miocene-aged dritis. At the eastern edge of the plateau, these drifts fill a shallow paleovalley to a depth of at least 35 m. The drills are exposed in a natural cross-section where modern topography crosscuts the paleovalley. Establishing an age and an environmental interpretation for these deposits is important because Antarctic paleoclimate records are lacking from the Mid-Miocene Climate Optimum. Two drifts fill the ancient paleovalley in the eastern Friis Hills. The upper drift is here named Cavendish drift: the lower is here named Friis drift. Cavendish can be subdivided into three units, whereas Friis drift can be subdivided into two units. Each of these units is a horizontal bed that laps on paleovalley sidewalls. The lowest, Friis II, is a compact diamicton that is overlain by a nearly in-situ bedded volvanic ash. Based on [20]Ar/[39]Ar dating, the ash is 19.76 [plus/minus] 0.07 Ma old. A second diamicton, Friis I, conformably blankets Friis II and was discovered to hold fossileferous interbeds. Both Friis I and II contain erratic clasts and both are lodgemont tills deposited from small, locally derived, alpine glaciers. Bedrock striations show ice flow to the northeast at azimuths between 025? to 032?, parallel to the trend of the paleovalley axis. Above these, Cavendish I. II. and III were deposited when thick ice covered the Friis Hills. Where the Cavendish drift laps onto paleovalley sidewalls, bedrock striations show ice flow from 077? to 150?. Cavendish drift was deposited sometime alter 19.8 Ma but before 14 Ma. when the Dry Valleys glacial records show that regional glaciers became cold-based. Downcutting eventually isolated the Friis Hills plateau, resulting in the preservation of the drift sequence. This event was most likely associated with growth or the East Antarctic Ice Sheet 14 Ma ago. This age constraint means that the tills preserved in the Friis Hills date from a time just before the East Antarctic Ice Sheet expanded and became a permanent feature. Based on the age-dated stratigraphy presented in this thesis, future work focusing on fossiliferious interbeds could provide unique and important constraints on Miocene climate change.
North Dakota State University. Department of Geosciences

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Hartmann, Kerstin. "Jungquartäre Reliefentwicklung, Substratgenese, Klimageschichte und aktuelle Morphodynamik am Ostrand der Namib in der Region Hartmannstal-Marienflusstal (NW-Namibia) /." Köln : Geograph. Inst. der Univ. zu Köln, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016293693&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA.

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Kahmann-Robinson, Julia A. Driese Steven G. "Late Mississippian (Chesterian) high-frequency climate change in the Pennington Formation at Pound Gap, KY USA." Waco, Tex. : Baylor University, 2008. http://hdl.handle.net/2104/5293.

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Cleveland, David M. Atchley Stacy C. Nordt Lee C. "Fluvial sequence stratigraphy and paleoclimate of the Upper Triassic (Norian-Rhaetian) Chinle Strata, northern New Mexico." Waco, Tex. : Baylor University, 2007. http://hdl.handle.net/2104/5118.

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Thesis (Ph.D.)--Baylor University, 2007.
In the abstract "[delta]13C" the "13" and "[delta]18O" the "18" are superscript; "pCO2" the "2" is subscript. Includes bibliographical references (p. 107-118).

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Holmes, Jonathan Anthony. "Pliocene and Quaternary environmental change in Kashmir, north-west Himalaya." Thesis, University of Oxford, 1989. http://ora.ox.ac.uk/objects/uuid:e9bb6cf8-93a8-4471-9c55-7ed84044dc3c.

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Late Cainozoic environmental changes in Kashmir (33°30' to 34°30' N: 74°10' to 75°30' E) have been reconstructed using a range of techniques. The sedimentary record in Kashmir consists of a thick (>1000m) basin-fill sequence known as the Karewa group, together with glacial and related sediments in the surrounding mountain flanks. The Karewa sediments are fluviolacustrine in origin and comprise alternations of conglomerates, sands and clayey silts. Work on the lower Karewa formation, which has previously been dated palaeomagnetically to between 4 and 0.4 MaBP, involved the semi- quantitative analysis of clay-mineral assemblages by X-ray diffraction.The clay minerals in the lower Karewa mudstones are interpreted as detrital clays which reflect weathering within Kashmir basin. The analyses showed a change in clay mineralogy between about 2.5 and 2.3MaBP, from abundant kaolinite to abundant smectite. Work on the upper Karewa formation involved field description and mapping of facies, sedimentological analysis, dating using thermoluminescence (TL) and amino-acid racemization, and analysis of ostracod assemblages from lacustrine sediments. Areal restriction of the lake in Kashmir occurred about 0.4MaBP with the rapid uplift of the Pir Panjal Range. Sedimentological data show that aeolian dust formed a major input into the lake. Ostracod assemblages show that the lake itself was cool, shallow, alkaline and had abundant plant macrophytes, The lake drained between 120 and SOkaBP. Stratigraphical, sedimentological and faunal evidence suggests that this was a result of tectonically-induced drainage rather than climatically-induced desiccation. The glacial history of the surrounding mountain flanks was reconstructed by field mapping of glacial sediments and dated using TL and radiocarbon methods. Present and past patterns of glaciation wore assessed by the determination of equilibrium-line altitudes (ELAs), glaciation thresholds (GTs) and cirque aJtitudes. Glaciers extended to 2150 m a.s.l in the Great Himalayan flank and 2600 m a.s.l. in the Pir Panjal. There is evidence for only 2 pre-Holucene advances in Kashmir, the older of which predates 35kaBP. Present patterns of glacierization indicate a SW to NE rise in the height of ELAs and GTs suggesting topographic and precipitation control. An apparent reversal of trends during the past is explained by Quaternary uplift of the Pir Panjal Range.

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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 the north to more marine deposits in the south. Although variable in character, the facies composing the sequence are described by four principal environments of deposition: alluvial, estuarine, lagoonal and marine. In an attempt to achieve a more accurate stratigraphic control on the succession, sequence-stratigraphic concepts are applied to outcrop exposures and subsurface cores. The identification of 'key surfaces' in the sequence resolves a series of lithological cycles which reflect relative sea-level fluctuations. Using this approach the Aalenian-Bathonian sequence can be subdivided into two large-scale (second-order) transgressive-regressive cycles onto which six medium-scale (thirdorder) cycles of transgression and regression are superimposed. The potential for correlating these lithological cycles regionally has been assessed by comparing coeval sections from southern Scandinavia. Plant-bearing fluvio-deltaic sequences from Bornholm and Scania were chosen as a means for appraising the lateral continuity of the cycles, and assessing what factors might have controlled their development. Study of floral remains from the Ravenscar Group within the context of this stratigraphic framework yields valuable palaeoclimatic information. Growth-ring analysis of fossil wood of Late Pliensbachian to Late Bathonian age indicates a distinctly seasonal climate with low to moderate interseasonal variation in tree growth. Significant intraseasonal influences on wood production are implicit in the abundance of false rings. Consideration of these results within a stratigraphic context suggests that conditions during the Bathonian were comparatively hostile: a finding which is interpreted to be due to more frequent and extended water shortages associated with a drier climate. These palaeoclimatic inferences are substantiated by evidence obtained from the examination of the flora using Correspondence Analysis (CA). This approach verifies the presence of a temporal fluctuation in the flora found by previous investigations and, furthermore, highlights physiognomic trends in the flora with time. The results from CA also indicate adverse growing conditions during the Bathonian, emphasized by the prevalence of xeromorphic taxa.

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Morse, David L. "Glacier geophysics at Taylor Dome, Antarctica /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/6801.

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Hawley, Robert L. "Borehole investigations of firn processes /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/6796.

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Books on the topic "Geology Paleoclimatology Paleoclimatology Geology"

1

Paleoclimatology: Reconstructing climates of the quaternary. 2nd ed. San Diego, CA: Academic Press, 1999.

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Quaternary paleoclimatology: Methods of paleoclimatic reconstruction. Boston: Allen & Unwin, 1985.

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Fazzini, Paolo. La geologia nella storia dell'uomo. Modena: Mucchi, 2001.

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America, Geological Society of, ed. Geology and geoarchaeology of the Black Sea Region: Beyond the flood hypothesis. Boulder, Colo: Geological Society of America, 2011.

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Onoprienko, I︠U︡ I., and A. V. Lozhkin. Klimaticheskie letopisi v chetvertichnykh osadkakh Beringii: Climate records from quaternary sediments of Beringia. Magadan: Severo-Vostochnyĭ kompleksnyĭ NII DVO RAN, 2004.

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Yang, In Che. Climatic changes inferred from analyses of lake-sediment cores, Walker Lake, Nevada ; prepared in cooperation with the U.S. Department of Energy. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1989.

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Balobanov, Oleg Maksimovich. Globalʹnye klimaticheskie sobytii︠a︡ neogena. Leningrad: Gidrometeoizdat, 1990.

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Zhang, Mingshu. Zhongguo hai an dai wan di si ji shi jian di zhi xue. Beijing: Di zhi chu ban she, 2000.

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Group, IGCP Project 218 Chinese Working. Quaternary processes in eastern China and their international correlation: A report. Beijing, China: Geological Pub. House, 1991.

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Arkhipov, Stanislav Anatolʹevich. Geologicheskai︠a︡ istorii︠a︡, landshafty i klimaty pleĭstot︠s︡ena Zapadnoĭ Sibiri. Novosibirsk: OIGGM SO RAN, 1994.

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Book chapters on the topic "Geology Paleoclimatology Paleoclimatology Geology"

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Bowen, R. "Isotopic Paleoclimatology." In Nuclear Methods in Mineralogy and Geology, 453–93. Boston, MA: Springer US, 1998. http://dx.doi.org/10.1007/978-1-4615-5363-2_10.

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Rea, David K. "Geologic Record of Atmospheric Circulation on Tectonic Time Scales." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 841–57. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_35.

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Parrish, Judith Totman, and Eric J. Barron. "Brief History of Paleoclimatology and the Importance of Continental Drift." In Paleoclimates and Economic Geology, 12–15. SEPM (Society for Sedimentary Geology), 1986. http://dx.doi.org/10.2110/scn.86.18.0012.

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Bradley, Raymond S. "Nonmarine Geologic Evidence." In Paleoclimatology, 345–75. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-386913-5.00010-7.

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Reports on the topic "Geology Paleoclimatology Paleoclimatology Geology"

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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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