Relevant bibliographies by topics / Stratigraphic Pleistocene

Academic literature on the topic 'Stratigraphic Pleistocene'

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Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "Stratigraphic Pleistocene"

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Šeirienė, Vaida, Tatjana Rylova, Alexander Karabanov, Valentinas Baltrūnas, Irina Savchenko, Bronislavas Karmaza, Svetlana Demidova, and Dalia Kisielienė. "The Pleistocene stratigraphy of the south-eastern sector of the Scandinavian glaciation (Belarus and Lithuania) in the light of new data." Baltica 28, no. 1 (June 1, 2015): 51–60. http://dx.doi.org/10.5200/baltica.2015.28.06.

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The paper summarises geological and palaeobotanical investigation data on Pleistocene sediments of recent decades in Lithuania and Belarus. The main problems in Pleistocene stratigraphy and correlation of sections are discussed. As a result the chronostratigraphical correlation chart of Lithuania and Belarus is presented and some changes in local stratigraphic schemes proposed. The majority of the stratigraphical units is comparable and correlates well however some unsolved stratigraphical problems still exist. To solve these problems additional very detail investigations are needed by applying the new modern methods. The lack of the absolute dates of the Pleistocene sediments is the main problem in both countries.
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Gaudenji, Tivadar, and Mladjen Jovanovic. "Quaternary stratigraphy: Recent changes." Glasnik Srpskog geografskog drustva 92, no. 4 (2012): 1–16. http://dx.doi.org/10.2298/gsgd1204001g.

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Corrections to the Quaternary stratigraphic division of Serbia was updated/renewed by lowering limit of the Pleistocene / Quaternary to the beginning of the Gelasian that is at approximately 2.588 million years. Rather than the officially rejected Penck & Br?ckner Alpine stratigraphic model, the use of oxygen isotope stages (OIS / MIS) is recommended. Climatostratigraphic terms glacial and interglacial have a regional applicability and their use is recommended only in areas where there are traces of glaciation, while the terms cold and warm stage (or moderate) stages should be used within the global context. Eopleistocene is a regional term for the former Soviet Union and due to its uniqueness it can hardly be applied in the stratigraphical scheme of the Quaternary depostis in Serbia. With the latest extension of the Lower Pleistocene, further use of Eopleistocene would lead to further confusion in stratigraphic correlation as such the use of the Lower / Early Pleistocene or other appropriate stratigraphic units is recommended.
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Marković, S. B., U. Hambach, T. Stevens, M. Jovanović, K. O'Hara-Dhand, B. Basarin, H. Lu, et al. "Loess in the Vojvodina region (Northern Serbia): an essential link between European and Asian Pleistocene environments." Netherlands Journal of Geosciences - Geologie en Mijnbouw 91, no. 1-2 (September 2013): 173–88. http://dx.doi.org/10.1017/s0016774600001578.

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AbstractLoess deposits in the Vojvodina region, northern Serbia, are among the oldest and most complete loess-paleosol sequences in Europe to date. These thick sequences contain a detailed paleoclimatic record from the late Early Pleistocene. Based on the correlation of detailed magnetic susceptibility (MS) records from Vojvodina with the Chinese loess record and deep-sea isotope stratigraphy we here reconfirm and expand on a stratigraphic model of the Vojvodinian loess-paleosol chronostratigraphic sequence following the Chinese loess stratigraphic system.Variations in MS, dust accumulation rates, and the intensity of pedogenesis demonstrate evidence for a Middle Pleistocene climatic and environmental transition. The onset of loess deposition in Vojvodina also indicates a direct link between dust generation in Europe and that in the interior of Eurasia since the Early Pleistocene. The youngest part of the Early Pleistocene and oldest part of the Middle Pleistocene is characterised by relatively uniform dust accumulation and soil formation rates as well as relatively high magnetic susceptibility values. In contrast, the last five interglacial-glacial cycles are characterised by sharp environmental differences between high dust accumulation rates during the glacials and low rates observed during soil development. The data presented in this study demonstrate the great potential of Vovjodina's loess archives for accurate reconstruction of continental Eurasian Pleistocene climatic and environmental evolution.
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Gaudenyi, Tivadar, Drazenko Nenadic, Mladjen Jovanovic, and Petar Stejic. "The revision of quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia)." Annales g?ologiques de la Peninsule balkanique, no. 00 (2022): 7. http://dx.doi.org/10.2298/gabp210306007g.

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The geological analysis of artesian borehole material from Sombor, Subotica, and Zrenjanin, was in the first campaign of detailed stratigraphic studies of Vojvodina in 1892-1895. The results of Quaternary stratigraphy from Zrenjanin were published by HalavAts m ore than a decade later (1914). The significance of the Zrenjanin, Sombor, and Subotica artesian well profiles for more than a century is considered the representative local profiles for the Quaternary stratigraphy of Vojvodina recognized by Serbian (Yugoslavian) and Hungarian geologists. Significant changes were after the taxonomical revision of molluscan material and its stratigraphic context, which was done through the excellent work of Krolopp in the 1970-ies. Unfortunately, the mentioned changes were not applied in the studies during the geological surveying of former Yugoslavia. The developments in Quaternary geology, changes in the Quater nary chronostratigraphic scale, and the results shown by this paper enable the Lower Pleistocene fluvial deposits to be defined as the Pleistocene Corbicula beds, the Viviparus boeckhi Horizon. The Lower Pleistocene at Zrenjanin was documented from 234.54 to 58.36 m depth. The interval between 234.54 and 208.50 m comprises the Upper Paludina - Viviparus vucotinovici zone, while the Viviparus boeckhi Horizons were identified between 135.18 m and 58.36 m. The interval between 58.36 m and 37.75 m is defined as Pleistocene (Lower- and Middle Pleistocene) based on sedimentological and the molluscan record. The interval from 37.75 m to 21.67 m depth was identified as Middle Pleistocene, according to its lithology and the paleontological material. The fluvial sediments? 21.69 m and 7.31 m depths cannot be determined according to the faunistic data; we can only consider them as Pleistocene age. The Holocene sediment and soil horizons ascend to a 2.90 m depth.
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Konradi, P. "Cenozoic stratigraphy in the Danish North Sea Basin." Netherlands Journal of Geosciences 84, no. 2 (July 2005): 109–11. http://dx.doi.org/10.1017/s001677460002299x.

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AbstractThis paper provides a concise review of investigations into the Cenozoic stratigraphy of the Danish North Sea Basin. In the Danish North Sea, mainly Pliocene and Pleistocene strata are found. Results of published seismic and sequence stratigraphic analyses are combined with biostratigraphic analyses and correlated to marine formations found onshore.
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Boreham, S. "The Geology of the Wicken Vision Area, lower Cam valley, Cambridgeshire, UK." Netherlands Journal of Geosciences - Geologie en Mijnbouw 92, no. 1 (April 2013): 47–59. http://dx.doi.org/10.1017/s0016774600000275.

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AbstractThe geology of the Wicken Vision Area in the lower Cam valley is described with reference to a stacked series of ten cross-sections through Holocene and Pleistocene deposits, and Cretaceous/Jurassic bedrock across the region. A detailed cross-section through a Holocene palaeochannel, with radiocarbon dating and pollen analyses is also presented. The structural geology of the bedrock and the stratigraphic arrangement of the Pleistocene and Holocene deposits are used to describe landscape development for the area. This study offers a new understanding of the stratigraphy and context of the Holocene, Weichselian and earlier Pleistocene deposits of the lower Cam valley, and provides a unique view of sediment architecture in valley-fill sediments at the fen edge.
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Aiello, Gemma. "Quaternary Lowstand Prograding Wedges of the Salento Continental Shelf (Southern Adriatic Sea, Italy): Architectural Stacking Patterns and the Control of Glacio-Eustatic Sea Level Fluctuations and Foreland Tectonic Uplift." Geosciences 13, no. 1 (December 22, 2022): 4. http://dx.doi.org/10.3390/geosciences13010004.

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The performance of both the tectonic uplift and of the 4th-order glacial eustatic sea level fluctuations in controlling the stratigraphic architecture of Quaternary lowstand prograding wedges of the Salento continental shelf (Southern Adriatic sea, Italy) during a time interval spanning from the Middle Pleistocene to the Holocene has been pointed out through the interpretation of high-resolution seismic reflection profiles and their correlation to the curves of the isotopic stratigraphy. Three main transgressive surfaces of erosion (RS1, RS2 and RS3) punctuate the stratigraphic architecture of the Salento continental shelf, separating Quaternary lowstand prograding wedges between them. All along the Middle Pleistocene, increasing the tectonic uplift of the Puglia offshore, combining with 4th-order glacio-eustatic variations, have dealt with the pattern of a broad forced regression prograding wedge, favoring a platform progradation of approximately 15 km. The architectural stacking patterns of the overlying Late Pleistocene and Holocene prograding wedges are controlled by 4th-order glacio-eustatic sea level changes, allowing for the formation of incomplete depositional sequences. In this period, the eustatic signature overcomes the tectonic mark, implying a decline in the uplift of the Apulian foreland in the course of the final 250 ky.
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Adamenko, Oleg, Yaroslav Adamenko, and Kateryna Radlovska. "GEOLOGICAL MEMORY OF STARUNJA – AS THE COURSE OF PROTECTION OF THE WORLD NATURAL HERITAGE IN CARPATHIAN REGION OF UKRAINE." Scientific Bulletin Series D : Mining, Mineral Processing, Non-Ferrous Metallurgy, Geology and Environmental Engineering 32, no. 2 (2018): 15–25. http://dx.doi.org/10.37193/sbsd.2018.2.02.

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Paleontological location of the Pleistocene fauna of hairy rhinos and mammoths near the village. Starunya Bogorodchany district of Ivano-Frankivsk region (Prykarpathian, Ukraine) is considered as a paleoclimatic rapper of global changes and a stratigraphic "bridge" linking stratigraphic patterns of the Upper Pleistocene of Western Europe and the plain territory of Ukraine. This is important for the reconstruction of global climate change and the transformation of natural and man-made geosystems.
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Boreham, Steve, and Karolina Leszczynska. "The Geology of the Middle Cam Valley, Cambridgeshire, UK." Quaternary 2, no. 3 (July 12, 2019): 24. http://dx.doi.org/10.3390/quat2030024.

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This study offers a new understanding of the stratigraphy and context of the Pleistocene (including Elsterian and Weichselian) and Holocene deposits of the Middle Cam valley, Cambridgeshire, United Kingdom, and provides a unique and detailed view of the sediment architecture of these valley-fill and interfluve sediments. The new insights into the geology of the area, including dating, pollen analyses, and sediment architecture, are presented with reference to a series of nine cross-sections through Holocene and Pleistocene deposits, as well as Cretaceous bedrock across the region. The structural geology of the bedrock and the stratigraphic arrangement of younger deposits are used to explain the landscape evolution of the area.
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Gruhn, Ruth, and Alan L. Bryan. "A Review of Lynch's Descriptions of South American Pleistocene Sites." American Antiquity 56, no. 2 (April 1991): 342–48. http://dx.doi.org/10.2307/281423.

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The description of major South American Pleistocene sites by Lynch (1990) contains significant errors and omissions. The artifact assemblage at the Colombian site of Tibitó, dated at 11,740 ± 140 B.P., is much larger than indicated by Lynch and well represents the Abriense industry, which features small unifacially retouched flake tools and core tools, with no stone projectile points. Lynch did not describe the 1976 stratigraphic profile at the Venezuelan site of Taima-Taima, and he failed to refer to the evidence for butchering of the juvenile mastodon with which an El Jobo projectile point fragment and a utilized flake were associated directly. The descriptions of Brazilian sites also feature serious mistakes. For the site of Alice Boër, Lynch overlooked a thick sterile stratigraphic unit (Bed IV) that intervenes between Bed III, with its thermoluminescence dates as early as 10,970 ± 1020 B.P. and radiocarbon dates as early as 14,200 ± 1150 B.P., and the artifact-bearing surface of Bed V. For Lapa Vermelha, Lynch failed to indicate that several artifacts were recovered from an older cemented cave fill that yielded radiocarbon dates of 22,410 B.P. and > 25,000 B.P. Lynch’s description of the site of Toca do Boqueirào da Pedra Furada does not correspond to eyewitness reports, and his description of the nearby Toca do Sitio do Meio was incomplete and confused. Finally, in his description of the stratigraphy of the Patagonian site of Los Toldos, Cueva 3 Lynch misquoted and misconstrued the original reports, which indicate clearly the stratigraphic priority and integrity of the Level 11 industry. For accurate descriptions of early South American archaeological sites, readers are urged to examine the original sources.
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Dissertations / Theses on the topic "Stratigraphic Pleistocene"

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Queen, Sandra June. "Petrologic characterization and differentiation of Neogene and Pleistocene sediments in the Verdi-Reno Truckee River corridor." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1460773.

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Lacy, Stephen L. "The stratigraphy and sedimentation of the pleistocene section of the May Stone and Sand Company, Inc., Ardmore Avenue Quarry, Fort Wayne, Allen County, Indiana." Virtual Press, 1986. http://liblink.bsu.edu/uhtbin/catkey/459230.

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The Pleistocene section exposed in the May Stone and Sand Company, Inc., Ardmore Avenue quarry rests in the upper reaches of the Wabash-Erie Channel. The section consists of two distinct till units which are covered by a thick outwash deposit. Analysis of the tills has led to the assignment of the lower till to the Trafalgar Formation, while the upper till is assigned to the Lagro Formation. The 13- to 16-foot outwash unit shows evidence of rapid drainage which may be related to the catastrophic drainage of glacial Lake Maumee. Isolated mud to muck inclusions in the top eight feet of the section show the final depositional environment of the channel. These deposits were produced near the end of late Wisconsinan time. The last major event in the area was the stream piracy of the St. Joseph and Ste. Mary's Rivers by the Maumee River, in Late Wisconsinan or Recent time.
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Campo, Bruno <1984&gt. "The Pleistocene-Holocene Transition in the Po Plain (Italy): Stratigraphic Architecture and Sequence Stratigraphy from a Highly-Subsiding Basin." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7540/.

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This work focuses on the Late Pleistocene-Holocene transition in the southern Po Basin. Five areas were investigated, with the aim of unraveling the role of different allogenic factors (climate, eustacy, sediment supply) on stratigraphic architecture in the last 45 ky. The study starts from the distal portion of the basin (the coastal plain deposits) and then moves towards increasingly internal areas: the alluvial sector characterized by the Po channel belt deposits, and the mud-prone interfluvial succession between the Apenninic margin and the Po channel belt. In the coastal sector, high-resolution facies analysis, along with a well-constrained chronostratigraphic framework, led to the accurate paleoenvironmental reconstruction of the last 45 ky BP depositional history along the 93 km-long transect. It is also provided a sequence stratigraphic interpretation for the whole sedimentary succession. In the Po channel belt sector, based on 28 radiocarbon dates, facies interpretation from high-quality core descriptions and freshly-drilled continuous cores, the contrasting stratigraphic architecture of Late Pleistocene and Holocene deposits was highlighted. Changes in lithofacies and channel stacking patterns reveal the vertical superposition of amalgamated fluvial-channel sands (Late Pleistocene) and mud-dominated deposits (Holocene), with isolated fluvial-channel bodies. We also attempted to establish the link between facies architecture, sea-level fluctuations and climate changes. The 3rd study area (interfuvial succession) was selected to test a new method for paleosol identification, on the basis of geotechnical properties generated from pocket penetrometer values. Through the reconstruction of the Biferno coastal deposits (4th study area, located ca. 300 km south of the Po Plain) we had the opportunity to document two coeval (Late Pleistocene - Holocene) coastal sedimentary successions, diverging in terms of shelf gradient and proximity to the LGM-lowstand Po Delta. The 5th study area, broadly coincides with Ferrara, was selected to show how high-resolution stratigraphic studies can be used for aquifer protection.
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Korotkikh, Elena. "A High Resolution Record of the Eemian Interglacial and Transition to the Next Glacial Period from Mount Moulton (West Antarctica)." Fogler Library, University of Maine, 2009. http://www.library.umaine.edu/theses/pdf/KorotkikhE2009.pdf.

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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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Andrews, William M. "Geologic controls on plio-pleistocene draining evolution of the Kentucky river in central Kentucky." Lexington, Ky. : [University of Kentucky Libraries], 2004. http://lib.uky.edu/ETD/ukygeol2004d00169/wmandrews.pdf.

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Thesis (Ph. D.)--University of Kentucky, 2004.
Title from document title page (October 12, 2004). Document formatted into pages; contains xi, 216 p. : ill., maps. Includes abstract and vita. Includes bibliographical references (p. 202-212).
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Rathburn, Sara L. "Pleistocene glacial outburst flooding along the Big Lost River, east-central Idaho." Thesis, The University of Arizona, 1989. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0127_sip1_w.pdf&type=application/pdf.

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Kushner, Vaughn A. "STRATIGRAPHIC CORRELATION OF LATE PLEISTOCENE SEDIMENTS OF A BURIED VALLEY IN NORTHFIELD CENTER TOWNSHIP, SUMMIT COUNTY, OHIO." University of Akron / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=akron1158259597.

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Ryter, Derek. "Late Pleistocene kinematics of the central San Jacinto fault zone, southern California /." view abstract or download file of text, 2002. http://wwwlib.umi.com/cr/uoregon/fullcit?p3072605.

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Thesis (Ph. D.)--University of Oregon, 2002.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 131-137). Also available for download via the World Wide Web; free to University of Oregon users.
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Meldahl, Keith Heyer. "Paleoenvironmental and stratigraphic implications of taphonomic processes: Case studies from Recent and Pleistocene shallow marine environments." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185114.

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Taphonomic data can be applied to problems in paleoenvironmental analysis, stratigraphy and paleobiology. Ecologic and taphonomic data from molluscan assemblages in Recent clastic shallow marine environments (northern Gulf of California, Mexico, and Cape Cod, Massachusetts, U.S.A.) furnish different and complementary types of environmental information. Ecological data (species composition, trophic and life habit data) are regulated principally by substrate variation. In contrast, taphonomic data (abrasion, fragmentation, corrosion, bioerosion and encrustation) variously track shifts in surface residence time of shells, water energy, and tidal submergence time. Taphonomic contrasts between sedimentary environment arise because shells in different environments are altered along distinct "taphonomic pathways". Variation in residence time, water energy and tidal submergence time elicit responses in unique suites of taphonomic attributes. Taphonomic processes affect the distribution of fossils in strata, and this has important stratigraphic and paleobiologic ramifications. Shell concentrations in Pleistocene shallow marine strata in the northern Gulf of California formed either as beach ridge accumulations, tidal channel lags, autochthonous communities, or "unconformity beds". The latter are significant stratigraphic markers, capping angular unconformities. The "unconformity beds" are identified taphonomically as transgressive lags derived from beach face reworking during erosion of structural bulges that formed by periodic deformation along the Pleistocene shoreline. These shell beds are products of sedimentary processes along tectonically active continental margins. Preservational incompleteness of fossils hampers reconstruction of patterns of mass extinction, because biostratigraphic last occurrences nearly always underestimate times of lineage extinction. The distribution of biostratigraphic last occurrences of mollusc species in sediment cores from a Recent tidal flat indicates that sudden extinction can appear gradual, due to error in biostratigraphic range endpoints (Signor-Lipps effect). Extinction is typically not accurately recorded for species with less than 15% stratigraphic abundance (i.e. occurring in less than 15% of the sample intervals). Extinction simulations demonstrate that stratigraphic abundance and last occurrence data (readily available in the fossil record) can be used together to distinguish between sudden, stepwise and gradual patterns of mass extinction.
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Books on the topic "Stratigraphic Pleistocene"

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William, Dawson John. Canadian pleistocene. London: Trubner, 1987.

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World Archaeological Congress (1st 1986 Southampton, England). The pleistocene perspective. [London]: Allen & Unwin, 1986.

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Attig, John W. Pleistocene geology of Taylor County, Wisconsin. Madison, Wis: Wisconsin Geological and Natural History Survey, University of Wisconsin-Extension, 1993.

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Ham, Nelson R. Pleistocene geology of Lincoln County, Wisconsin. Madison, Wis: University of Wisconsin-Extension, Wisconsin Geological and Natural History Survey, 1997.

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Syverson, Kent M. Pleistocene geology of Chippewa County, Wisconsin. Madison, Wis: Wisconsin Geological and Natural History Survey, 2007.

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Attig, John W. Pleistocene geology of Marathon County, Wisconsin. Madison, Wis: University of Wisconsin-Extension, Geological and Natural History Survey, 1989.

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W, Attig John, Mickelson David M, and Clayton Lee 1938-, eds. Pleistocene stratigraphic units of Wisconsin, 1984-87. Madison, WI: University of Wisconsin, 1988.

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Jánossy, D. Pleistocene vertebrate faunas of Hungary. Amsterdam: Elsevier, 1986.

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Clayton, Lee. Pleistocene geology of Dane County, Wisconsin. Madison, Wis: University of Wisconsin-Extension, Wisconsin Geological and Natural History Survey, 1997.

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Clayton, Lee. Pleistocene geology of Wood County, Wisconsin. Madison, Wis. (3817 Mineral Point Rd., Madison 53705): Wisconsin Geological and Natural History Survey, 1991.

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Book chapters on the topic "Stratigraphic Pleistocene"

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Al-Helal, Anwar, Yaqoub AlRefai, Abdullah AlKandari, and Mohammad Abdullah. "Subsurface Stratigraphy of Kuwait." In The Geology of Kuwait, 27–50. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16727-0_2.

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AbstractThis chapter reviews the subsurface stratigraphy of Kuwait targeting geosciences educators. The lithostratigraphy and chronostratigraphy of the reviewed formations (association of rocks whose components are paragenetically related to each other, both vertically and laterally) followed the formal stratigraphic nomenclature in Kuwait. The exposed stratigraphic formations of the Miocene–Pleistocene epochs represented by the Dibdibba, Lower Fars, and Ghar clastic sediments (Kuwait Group) were reviewed in the previous chapter as part of near-surface geology. In this chapter, the description of these formations is based mainly on their subsurface presence. The description of the subsurface stratigraphic formations in Kuwait followed published academic papers and technical reports related to Kuwait’s geology or analog (GCC countries, Iraq and Iran) either from the oil and gas industry or from different research institutions in Kuwait and abroad. It is also true that studies related to groundwater aquifer systems also contribute to our understanding of the subsurface stratigraphy of Kuwait for the shallower formations. The majority of the published data were covered the onshore section of Kuwait. The subsurface stratigraphic nomenclature description is based on thickness, depositional environment, sequence stratigraphy, the nature of the sequence boundaries, biostratigraphy, and age. The sedimentary strata reflect the depositional environment in which the rocks were formed. Understanding the characteristics of the sedimentary rocks will help understand many geologic events in the past, such as sea-level fluctuation, global climatic changes, tectonic processes, geochemical cycles, and more, depending on the research question. The succession of changing lithological sequences is controlled by three main factors; sea-level change (eustatic sea level), sediment supply, and accommodation space controlled by regional and local tectonics influences. Several authors have developed theoretical methods, established conceptual models, and produced several paleofacies maps to interpret Kuwait’s stratigraphic sequence based on the data collected over time intervals from the Late Permian to Quaternary to reconstruct the depositional history of the Arabian Plate in general and of Kuwait to understand the characteristics of oil and gas reservoirs.
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Graf, Hans Rudolf, and Reto Burkhalter. "Pleistocene Deposits of the Swiss Northern Alpine Foreland: Stratigraphic Concept and Nomenclature." In Springer Geology, 515–19. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_99.

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Duveau, Jérémy, Gilles Berillon, and Christine Verna. "On the Tracks of Neandertals: The Ichnological Assemblage from Le Rozel (Normandy, France)." In Reading Prehistoric Human Tracks, 183–200. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60406-6_11.

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AbstractHominin tracks represent a unique window into moments in the life of extinct individuals. They can provide biological and locomotor data that are not accessible from skeletal remains. However, these tracks are relatively scarce in the fossil record, particularly those attributed to Neandertals. They are also most often devoid of associated archaeological material, which limits their interpretation. The Palaeolithic site of Le Rozel (Normandy, France) located in a dune complex formed during the Upper Pleistocene has yielded between 2012 and 2017 several hundred tracks (257 hominin footprints, 8 handprints as well as 6 animal tracks). This ichnological assemblage is distributed within five stratigraphic subunits dated to 80,000 years. These subunits are rich in archaeological material that attests to brief occupations by Neandertal groups and provides information about the activities that they carried out. The ichnological assemblage discovered at Le Rozel is the largest attributed to Neandertals to date and more generally the most important for hominin taxa other than Homo sapiens. The particularly large number of footprints can provide major information for our understanding of the Palaeolithic occupations at Le Rozel and for our knowledge of the composition of Neandertal groups.
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Agatova, A. R., R. K. Nepop, and H. Rodnight. "On the Problems of Correlating the Pleistocene Glacial Deposits in the Russian Altai with Siberian Stratigraphic Scales." In Springer Geology, 903–7. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_170.

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Taldenkova, Ekaterina, Sergei Nikolaev, Pavel Rekant, and Nataliya Chistyakova. "Pleistocene Sediment Sequence of the Southern Lomonosov Ridge, Arctic Ocean: Preliminary Stratigraphic Subdivision Based on Iceberg-Rafted Debris and Benthic Foraminiferal Records." In Springer Geology, 1321–25. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_252.

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Pino, Mario, Alejandra Martel-Cea, Rodrigo M. Vega, Daniel Fritte, and Karin Soto-Bollmann. "Geology, Stratigraphy, and Chronology of the Pilauco Site." In Pilauco: A Late Pleistocene Archaeo-paleontological Site, 33–53. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-23918-3_3.

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Tesson, M., G. P. Allen, and C. Ravenne. "Late Pleistocene Shelf-Perched Lowstand Wedges on the Rhône Continental Shelf." In Sequence Stratigraphy and Facies Associations, 181–96. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304015.ch10.

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Muto, T. "Incised Valleys in the Pleistocene Tenryugawa and Oigawa Coastal-Fan Systems, Central Japan: The Concept of the Fan-Valley Interval." In Sequence Stratigraphy and Facies Associations, 69–92. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304015.ch5.

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Carew, James L., and John E. Mylroie. "Stratigraphy, depositional history, and karst of San Salvador Island, Bahamas." In Pleistocene and Holocene Carbonate Environments on San Salvador Island, Bahamas: San Salvador Island, Bahamas, July 2–7, 1989, 7–15. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft175p0007.

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Weimer, P. "Sequence stratigraphy of the Mississippi Fan (Late Miocene-Pleistocene), northern deep Gulf of Mexico." In Atlas of Deep Water Environments, 94–99. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_17.

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Conference papers on the topic "Stratigraphic Pleistocene"

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Pacht, Jory A., John H. Beard, Gordon Weisser, Arnold H. Bouma, Bruce E. Bowen, and Peter R. Vail. "Seismic‐stratigraphic analysis of plio‐pleistocene depositional facies, East and West Cameron, offshore Louisiana." In SEG Technical Program Expanded Abstracts 1989. Society of Exploration Geophysicists, 1989. http://dx.doi.org/10.1190/1.1889775.

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Lipparini, L., and R. Tinterri. "Seismo-stratigraphic Study of the Plio-pleistocene Deposits of the Central Adriatic Sea, Italy." In 72nd EAGE Conference and Exhibition incorporating SPE EUROPEC 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609.201401050.

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Larsen, Daniel, and Kristian Olson. "STRATIGRAPHIC EVIDENCE FOR SUBTLE TECTONIC ACTIVITY DURING PLEISTOCENE DEPOSITION IN THE TECOPA BASIN, SOUTHEASTERN CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274350.

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Rovey, Charles W., and Greg Balco. "STRATIGRAPHIC COMPLEXITY WITHIN THE EARLY AND MIDDLE PLEISTOCENE TILL SEQUENCE IN NEBRASKA AND WESTERN IOWA." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327603.

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Jochems, Andy, Dan Koning, and Colin Cikoski. "Updated Stratigraphic Nomenclature of the Plio-Pleistocene Palomas Formation (upper Santa Fe Group), South-Central New Mexico." In 2018 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2018. http://dx.doi.org/10.56577/sm-2018.790.

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Albarbary, Z., V. Spiess, E. Bassiouni, M. El-Boukhary, and H. Farouk Ewida. "3D sequence stratigraphic framework for assessing hydrocarbon potential of Plio-Pleistocene successions in offshore North Sinai, Egypt." In Third EAGE Eastern Mediterranean Workshop. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202137028.

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Sycheva, S. A., M. Frechen, E. V. Ponomarenko, and A. N. Simakova. "DETAILED STRATIGRAPHIC SCHEME OF THE LATE PLEISTOCENE OF THE EAST EUROPEAN PLAIN AND ITS CORRELATION WITH OTHER REGIONAL SCHEMES." In PALEONTOLOGY, STRATIGRAPHY AND PALEOGEOGRAPHY OF THE MESOZOIC AND CENOZOIC IN BOREAL REGIONS. Trofimuk Institute of Petroleum Geology and Geophysics (SB RAS), 2021. http://dx.doi.org/10.18303/b978-5-4262-0104-0-396.

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Collins, Joe D., Trinity A. Miller, Thomas E. Gill, and Richard P. Langford. "STRATIGRAPHIC RELATIONSHIP AND HISTORY OF TWO LATE PLEISTOCENE AND HOLOCENE PLAYAS IN THE HARNEY BASIN, EASTERN OREGON, USA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306198.

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Feibel, Craig, and Catherine Beck. "THE NATOO TUFF AT KAITIO, WEST TURKANA, KENYA: A STRATIGRAPHIC KEY FOR EARLY PLEISTOCENE FOSSIL AND ARCHAEOLOGICAL RECORDS." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-367228.

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Thornton, Erik, and Kathleen M. Farrell. "CROSS SECTION CONSTRUCTION FOR THE STRATIGRAPHIC CHARACTERIZATION OF PLIOCENE-PLEISTOCENE DEPOSITS OF THE NORTH CAROLINA COASTAL PLAIN, FALKLAND 7.5 MINUTE QUADRANGLE." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-326615.

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Reports on the topic "Stratigraphic Pleistocene"

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Russell, H. A. J., and R. W. C. Arnott. Stratigraphic evidence for supercritical flow and hydraulic jump conditions in a subaqueous fan succession, Oak Ridges Moraine (Pleistocene), southern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/216707.

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Klassen, R. W. The Tertiary-Pleistocene stratigraphy of the Liard Plain, southeastern Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122373.

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Armstrong, R., D. J. W. Piper, and C. G. P. Pereira. Pleistocene Stratigraphy and Sedimentology of western Flemish Pass: a Seismic Interpretation. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130439.

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Lamothe, M. Pleistocene stratigraphy and till geochemistry of the Miramichi Zone, New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/183878.

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Ryane, C., B. R. Edwards, and J. K. Russell. The volcanic stratigraphy of Kima'Kho Mountain: a Pleistocene tuya, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289196.

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Mountain, Gregory, and Peter Buhl. Pleistocene Margin Stratigraphy, New Jersey vs. Northern California: A STRATAFORM Study of Contrasts. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630278.

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Dafoe, L. T., K. Dickie, G. L. Williams, and T. McCartney. Stratigraphy of the Labrador margin: a synthesis and new perspectives. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321829.

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Abstract:
The Labrador Sea formed during rifting between North America and Greenland beginning in the Early Cretaceous, with subsequent seafloor spreading from the Maastrichtian (chron C31) to Early Paleocene (chron C27n) that ended by chron C13 (earliest Oligocene). Early Cretaceous rifting resulted in accumulation of Alexis Formation basalt units and Bjarni Formation nonmarine and marginal marine clastic rocks. In the Late Cretaceous, extension focused further offshore as sag basin conditions formed across the shelf, with a basinwide transgression of Markland Formation shale and localized Freydis Member sandstone development. A Middle Paleocene to Early Eocene regression formed Gudrid Formation shoreline sandstone units, with correlative Cartwright Formation marine shale units. This was followed by an Early Eocene transgression of the Kenamu Formation and Middle Eocene Leif Member shoreline development. During the Late Eocene through Pleistocene, transgression took place once again at the base of the Mokami Formation, with subsequent development of the partly correlative shallow-marine sandstone units of the Saglek Formation.
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Bednarski, J. M. Surficial geology and Pleistocene stratigraphy from Deep Bay to Nanoose Harbour, Vancouver Island, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/295609.

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Morris, T. H., D. L. Clark, and S. M. Blasco. Sediments of the Lomonosov Ridge and Makarov Basin: a Pleistocene Stratigraphy For the North Pole. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126767.

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Dixon, J., J. R. Dietrich, and D. H. McNeil. Upper Cretaceous to Pleistocene sequence stratigraphy of the Beaufort-Mackenzie and Banks Island areas, Northwest Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133237.

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