Bibliographies thématiques / Early Middle Pleistocene

Littérature scientifique sur le sujet « Early Middle Pleistocene »

Auteur : Grafiati
Publié le 10 mars 2023

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Articles de revues sur le sujet "Early Middle Pleistocene"

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Rodríguez-Gómez, Guillermo, Jesús Rodríguez, Jesús A. Martín-González et Ana Mateos. « Evaluating the impact of Homo-carnivore competition in European human settlements during the early to middle Pleistocene ». Quaternary Research 88, no 1 (24 mai 2017) : 129–51. http://dx.doi.org/10.1017/qua.2017.20.

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AbstractFossil remains and the technological complexes recorded in archaeological sites suggest that the human presence in Europe late in the early and middle Pleistocene was discontinuous. Moreover, competition for meat with other secondary consumers could have delayed the human dispersal through Europe. However, evaluation of the extent competition intensity among secondary consumers suggests this influenced the discontinuity of the human settlement of Europe between 1.1 and 0.2 Ma. Using a mathematical model, we estimate the amount of biomass available in a community for secondary consumers. The amount of available biomass is subsequently distributed among the guild of secondary consumers according to their requirements and prey preferences. Indexes that quantify the competition intensity among secondary consumers to compare the conditions in different paleoecosystems show that the competition intensity late in the early Pleistocene, early in the middle Pleistocene, and late in the middle Pleistocene does not support the view that an increase in competition intensity constrained the expansion of human populations early in the middle Pleistocene. Somewhat paradoxically, the lowest competition intensity is estimated to have occurred early in the middle Pleistocene, most likely because of an increase in the number of large herbivore species and a decrease in the number of secondary consumers. The early Pleistocene paleoecosystems supported higher competition intensity than the middle Pleistocene ecosystems, likely because of the different configuration in the food webs of these two periods (the early and middle Pleistocene).
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Pečnerová, Patrícia, David Díez-del-Molino, Tom van der Valk, Marianne Dehasque, Anders Götherström et Love Dalén. « Mammuthus sp. (Early and Middle Pleistocene Mammoths) ». Trends in Genetics 37, no 7 (juillet 2021) : 682–83. http://dx.doi.org/10.1016/j.tig.2021.04.006.

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Tchernov, Eitan, et Evangelia Tsoukala. « Middle Pleistocene (Early Toringian) Carnivore Remains from Northern Israel ». Quaternary Research 48, no 1 (juillet 1997) : 122–36. http://dx.doi.org/10.1006/qres.1997.1901.

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Seventy well-preserved fossil remains from deposits of an eroded karstic cave in the Upper Galilee of northern Israel includeUrsus deningeri(Ursidae),Canis lupus cf.mosbachensis (Canidae),Crocuta crocuta cf. praespelaea (Hyaenidae), Panthera leo cf. spelaea (Felidae), and Dama sp. (Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus–Zagros mountain chain this far to the south. Due to the relative scarcity of Middle Pleistocene assemblages, especially carnivores, in the southern Levant, the biogeographic connection between the southern Levant and the Near East is still not well known. This faunule elucidates Pleistocene biotic exchanges between Europe and the Levant during this period.
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HALL, Adrian M., Jon W. MERRITT, E. Rodger CONNELL et Alun HUBBARD. « Early and Middle Pleistocene environments, landforms and sediments in Scotland ». Earth and Environmental Science Transactions of the Royal Society of Edinburgh 110, no 1-2 (4 octobre 2018) : 5–37. http://dx.doi.org/10.1017/s1755691018000713.

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ABSTRACTThis paper reviews the changing environments, developing landforms and terrestrial stratigraphy during the Early and Middle Pleistocene stages in Scotland. Cold stages after 2.7 Ma brought mountain ice caps and lowland permafrost, but larger ice sheets were short-lived. The late Early and Middle Pleistocene sedimentary record found offshore indicates more than 10 advances of ice sheets from Scotland into the North Sea but only 4–5 advances have been identified from the terrestrial stratigraphy. Two primary modes of glaciation, mountain ice cap and full ice sheet modes, can be recognised. Different zones of glacial erosion in Scotland reflect this bimodal glaciation and the spatially and temporally variable dynamics at glacier beds. Depths of glacial erosion vary from almost zero in Buchan to hundreds of metres in glens in the western Highlands and in basins both onshore and offshore. The presence of tors and blockfields indicates repeated development of patches of cold-based, non-erosive glacier ice on summits and plateaux. In lowlands, chemical weathering continued to operate during interglacials, but gruss-type saprolites are mainly of Pliocene to Early Pleistocene age. The Middle Pleistocene terrestrial stratigraphic record in Scotland, whilst fragmentary and poorly dated, provides important and accessible evidence of changing glacial, periglacial and interglacial environments over at least three stadial–interstadial–interglacial cycles. The distributions of blockfields and tors and the erratic contents of glacial sediments indicate that the configuration, thermal regime and pattern of ice flow during MIS 6 were broadly comparable to those of the last ice sheet. Improved control over the ages of Early and Middle Pleistocene sediments, soils and saprolites and on long-term rates of weathering and erosion, combined with information on palaeoenvironments, ice extent and sea level, will in future allow development and testing of new models of Pleistocene tectonics, isostasy, sea-level change and ice sheet dynamics in Scotland.
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Whiteman, Colin A., et James Rose. « Early-Middle Pleistocene Beheading of the River Thames ». Paléoréseaux hydrographiques quaternaires : centenaire W.M. Davis 51, no 3 (30 novembre 2007) : 327–36. http://dx.doi.org/10.7202/033131ar.

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ABSTRACT This paper marks the centenary of the first of three articles by W.M. Davis on the beheading of the Thames, beginning with a statement of his capture hypothesis in 1895 and concluding with attempts to explain anomalous misfit streams in 1899 and 1909. It discusses Davis's classic thesis of river capture by slow, long-term landscape evolution and his apparent reluctance to accept the fact of rapid Quaternary climate change. In contrast, recent work based on lithostratigraphy, biostratigraphy and morphostratigraphy emphasises the dynamism of the Quaternary Period and its influence on river capture. Possible mechanisms for the beheading of the Thames, tectonism, glacial erosion and conventional Davisian river capture, and the timing of the event, are discussed. In conclusion, the paper summarises known and unknown components of the problem of the beheading of the Thames, and discusses the extent of Davis's influence on later Thames studies.
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Belshaw, R. K., P. L. Gibbard, J. B. Murton et D. K. Murton. « Early Middle Pleistocene drainage in southern central England ». Netherlands Journal of Geosciences - Geologie en Mijnbouw 93, no 4 (12 septembre 2014) : 135–45. http://dx.doi.org/10.1017/njg.2014.25.

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AbstractThe fluvial sequences of the Milton and the Letchworth formations in the south Midlands of England and neighbouring regions represent at least two pre-existing rivers, the Milton and Brigstock streams, underlying Middle Pleistocene glacial sediments. The Milton Formation includes sand sourced from the Midlands bedrock. This implies that both streams were aligned in a northwest to southeast direction. This direction parallels the contemporaneous courses of the rivers Thames and Trent, the former turning towards the east and northeast to enter the North Sea. Their alignments indicate that the Milton and Letchworth streams formed left-bank tributaries of the Thames, joining the river in Hertfordshire and Essex, as illustrated in the article. This reconstruction has important implications for the interpretation of the proto-Soar river of the south Midlands, represented by the Baginton Formation. Although originally thought to represent a late Middle Pleistocene line, this southwest to northeast aligned system was reinterpreted as the headwaters of a pre-Anglian ‘Bytham river’, a1ligned towards East Anglia. However, recent work has shown that this river could not have existed in the pre-Anglian since there is no link between the Midlands and East Anglian spreads. Recent re-recognition that the Baginton Formation deposits do represent a later, post-Anglian drainage line is reinforced by the identification of the Milton and Letchworth streams, whose catchments occupied the area later drained by the proto-Soar. Overall, the main drainage alignment in southern England during the pre-Anglian period was dominated by northwest–southeast-draining consequent rivers adjusted to the regional geological dip. After widespread drainage disruption caused by the Anglian glaciation, northeast–southwest-orientated subsequent streams eroded frost-susceptible clay bedrock under periglacial and permafrost conditions, and beheaded the courses of some of the older consequent streams.
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Rose, James. « Early and Middle Pleistocene landscapes of eastern England ». Proceedings of the Geologists' Association 120, no 1 (janvier 2009) : 3–33. http://dx.doi.org/10.1016/j.pgeola.2009.05.003.

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Jianhua, Jin, et Liao Wenbo. « Palaeovegetation and palaeoclimate during middle Late Palaeolithic age of Lingnan area, China ». Journal of Palaeosciences 57, no (1-3) (31 décembre 2008) : 511–14. http://dx.doi.org/10.54991/jop.2008.269.

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The fossil spore-pollen recovered from middle Late Palaeolithic age (i.e. late Middle Pleistocene to Late Pleistocene) of Lingnan area of China are mainly distributed in the Pearl River Mouth Basin, Pearl River Delta, Shenzhen, Zhanjiang, Leizhou Peninsula and Hainan Island. As revealed by the fossil spore-pollen, the vegetation of Lingnan area during the late Middle Pleistocene to Late Pleistocene comprised mainly of subtropical evergreen broad-leaved forest, evergreen and deciduous broad-leaved mixed forest, and coniferous forest. During the early Late Pleistocene, the area experienced transgression of sea, and climate became hot leading to the development, of mangrove vegetation in the littoral area. On recession of sea, near the end of Late Pleistocene, climate became cooler and drier and the mangrove forest diminished significantly. Thus, the above mentioned luxuriant vegetation and subtropical climate in middle Late palaeolithic age suggests existence of favourable conditions for early Homo sapiens activities in the Lingnan area.
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Schick, Kathy, et Nicholas Toth. « Acheulean Industries of the Early and Middle Pleistocene, Middle Awash, Ethiopia ». L'Anthropologie 121, no 5 (novembre 2017) : 451–91. http://dx.doi.org/10.1016/j.anthro.2017.10.009.

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Liu, Chao, Qiyun Lei, Peng Du, Zhiqun Wu, Zeshan Li, Sihan Yu, Shun Yang et Yin Wang. « Activity Characteristic of the Two Buried Faults in Zhongwei Basin along the Northeastern Margins of Tibetan Plateau, China, by Means of Shallow Seismic and Composite Drilling Section Exploration ». Applied Sciences 12, no 23 (25 novembre 2022) : 12074. http://dx.doi.org/10.3390/app122312074.

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By using shallow seismic exploration, composite drilling section exploration and sample dating test, we have obtained precise positions, burial depths of uppermost point and activity characteristics of Hetan-Guotan buried fault and Zhenjing-Zhenbei buried fault in Zhongwei Basin. The results show that the latest active period of Hetan-Guotan buried fault is the middle-late Middle Pleistocene, and the latest active period of Zhenjing-Zhenbei buried fault is the Early and Middle Pleistocene. The two buried faults became inactive at the end of the Middle Pleistocene and have been inactive since the Late Pleistocene.
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Thèses sur le sujet "Early Middle Pleistocene"

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Rowney, Francis. « Ecology and climates of early Middle Pleistocene interglacials in Britain ». Thesis, University of Plymouth, 2018. http://hdl.handle.net/10026.1/11836.

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This thesis refines and develops understanding of the ecological and climatic characteristics of early Middle Pleistocene (MIS 19-13, c. 780-430 ka) interglacial environments in Britain. This period is characterised by globally muted (i.e. low amplitude) glacial-interglacial cycles, which increased in amplitude c. 430 ka with the Mid-Brunhes Transition (MBT). However, the influence of these global climatic characteristics on climates and ecology at regional and local scales is yet to be fully understood. Local ecological processes, particularly disturbance processes, have also received limited attention in pre-Holocene interglacial settings, despite their likely importance for vegetation and habitat structure. Chapters 4, 5 and 6 present in-depth multi-proxy palaeoenvironmental studies from three early Middle Pleistocene sites: West Runton, Pakefield and Brooksby. A combination of Coleoptera, pollen, coprophilous fungal spores, microcharcoal and sedimentology is used to reconstruct local ecological attributes for each site. Multivariate analyses of these datasets indicate the importance of disturbance processes (herbivore activity, wildfire, hydrogeomorphic processes) in driving and maintaining local vegetation structure and habitat heterogeneity. This is explored further (in Chapter 8), emphasising the apparent importance of site-specific factors, rather than those shared between sites, in determining the relative influence of each disturbance factor. In Chapter 7, new approaches to the coleopteran Mutual Climatic Range (MCR) method are applied to a suite of coleopteran records from interglacial sites spanning the Middle and Late Pleistocene (c.712-126 ka, MIS 17-5e). Summer temperatures, winter temperatures and temperature seasonality are reconstructed, to test whether there is evidence for MBT expression in Northwest European thermoclimates. No evidence for this is found, and it is suggested (in Chapter 8) that MBT expression in this region may instead be reflected in hydroclimatic variables (e.g. enhanced annual precipitation). Finally, it is suggested that disturbance processes and potentially wetter climates were beneficial to contemporary Lower Palaeolithic populations in Northwest Europe.
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Lee, Jonathan Robin. « Early and Middle Pleistocene lithostratigraphy and palaeo-environments in northern East Anglia ». Thesis, Royal Holloway, University of London, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.409122.

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Hallam, David Frank. « Palaeomagnetic investigations of Early and Middle Pleistocene sediments in East Anglia, UK ». Thesis, University of East Anglia, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.282974.

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Machin, Anna Jane. « The Acheulean handaxe : symmetry, function and Early and Middle Pleistocene hominin behaviour ». Thesis, University of Reading, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.434309.

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Marlow, Lisa. « The hominid dispersal into Early and Middle Pleistocene Europe : an approach from biogeography ». Thesis, University of Cambridge, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.612794.

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Asperen, Eline Naomi Van. « An outline of late Middle Pleistocene horse biostratigraphy a contribution to the chronology and ecology of the European early and Middle Palaeolithic ». Thesis, University of York, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.533542.

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Killick, Laura Elizabeth. « Geometric morphometric analysis of the Microtus M1 and its application to Early Middle Pleistocene in the UK ». Thesis, Durham University, 2012. http://etheses.dur.ac.uk/3550/.

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Species of the genus Microtus are known to be some of the most rapidly evolving taxa during the Quaternary. Their remains are common in archaeological and palaeontological contexts and are frequently used in palaeoclimatic and habitat reconstructions as well as providing a key component of biostratigraphic dating models. This study focused on the dental morphology of the lower M1 in 6 species of Microtus found in the British early Middle Pleistocene. The study examined the potential for a new approach to gaining better resolution in biostratigraphic and palaeoclimatic reconstructions in this period, using Geometric Morphometric (GMM) analyses. GMM analyses of modern samples of known origin found that it was possible to identify M1 teeth to species level with a high degree of statistical significance ( <0.0001). The application of protocols developed on modern samples to those from the early Middle Pleistocene sites at Westbury sub-Mendip and Boxgrove suggested species identification on ancient material was also possible. Taxonomic revision of the extinct species Microtus arvalinus was suggested by their morphological similarity to both modern and ancient M. agrestis samples, not M. arvalis as has previously been suggested. Identification of a large morphological disparity between modern and early Middle Pleistocene examples of M. subterraneus also suggest a complex genetic history, which previously had not been identified. Additionally, evidence for morphological differences linked to climate was found. Variation in morphology between stratigraphic levels was found to be relatively low in most cases, even when samples were thought to be separated by a significant period of time. These findings strongly support the use of GMM methods in determining Microtus remains to species level and suggest a strong potential for their use as palaeoclimatic and relative-dating proxies, requiring further research.
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Keates, S. G. « The significance of the older palaeolithic occurrences in the Nihewan Basin, northern China : in the context of important Early and Middle Pleistocene northern Chinese localities ». Thesis, University of Oxford, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.260637.

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Proborukmi, Maria Sekar [Verfasser], et Brigitte [Akademischer Betreuer] Urban. « Climate and environmental evolution in Late Pliocene and Quaternary sediments of coastal northwest Germany and Early-Middle Pleistocene of the Upper Jordan Valley, Israel / Maria Sekar Proborukmi ; Betreuer : Brigitte Urban ». Lüneburg : Universitätsbibliothek der Leuphana Universität Lüneburg, 2018. http://d-nb.info/1169395740/34.

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Proborukmi, Maria Sekar Verfasser], et Brigitte [Akademischer Betreuer] [Urban. « Climate and environmental evolution in Late Pliocene and Quaternary sediments of coastal northwest Germany and Early-Middle Pleistocene of the Upper Jordan Valley, Israel / Maria Sekar Proborukmi ; Betreuer : Brigitte Urban ». Lüneburg : Universitätsbibliothek der Leuphana Universität Lüneburg, 2018. http://d-nb.info/1169395740/34.

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Livres sur le sujet "Early Middle Pleistocene"

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Charles, Turner, et INQUA-Subcommission on European Quaternary Stratigraphy., dir. The Early middle Pleistocene in Europe : Proceedings of the SEQS Cromer Symposium, Norwich, United Kingdom, 3-7 September 1990. Rotterdam : A.A. Balkema, 1996.

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The early and middle Pleistocene archaeological record of Greece : Current status and future prospects. [Leiden], the Netherlands : Leiden University Press, 2010.

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Early Middle Pleistocene in Europe. Taylor & Francis, 1996.

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Turner, Charles. Early Middle Pleistocene in Europe. Taylor & Francis Group, 2020.

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Turner, Charles. Early Middle Pleistocene in Europe. Taylor & Francis Group, 2020.

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Turner, Charles. Early Middle Pleistocene in Europe. Taylor & Francis Group, 2020.

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Turner, Charles. Early Middle Pleistocene in Europe. Taylor & Francis Group, 2020.

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Early and Middle Pleistocene Hominid Behaviour in Northern China. British Archaeological Reports, 2000.

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(Editor), M. J. Head, et P. L. Gibbard (Editor), dir. Early Middle Pleistocene Transitions : The Land-Ocean Evidence (Special Publication, No. 247). Geological Society of London, 2005.

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Tourloukis, Vangelis. Early and Middle Pleistocene Archaeological Record of Greece : Current Status and Future Prospects. Amsterdam University Press, 2010.

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Chapitres de livres sur le sujet "Early Middle Pleistocene"

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Markova, Anastasia K. « A New Early Middle Pleistocene Locality of Small Mammals (Lower Dniester River) and its Position in the Early Middle Pleistocene Sequence ». Dans Springer Geology, 1017–18. Cham : Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_193.

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Trinkaus, Erik, Tea Jashashvili et Biren A. Patel. « Perspectives on Pliocene and Pleistocene Pedal Patterns and Protection ». Dans Reading Prehistoric Human Tracks, 121–32. Cham : Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60406-6_7.

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AbstractAs a framework for interpreting Pliocene and Pleistocene hominin footprints, the functional implications of australopith and Homo pedal remains are reviewed. Despite minor variations in pedal proportions and articular morphology, all of these remains exhibit tarsometatarsal skeletons fully commensurate with an efficient (human) striding bipedal gait. The Middle and Late Pleistocene Homo pedal phalanges exhibit robust and distally flattened metatarsal 1 heads, hallux valgus, relatively short lateral digits with largely straight proximal phalanges with dorsally oriented metatarsal facets, all similar to those of recent humans. The Pliocene and Early Pleistocene halluces lack hallux valgus and have bulbous metatarsal 1 heads. The australopith pedal remains have lateral proximal phalanges that are relatively long and dorsally curved and have more proximally oriented metatarsal facets. In addition, pre-Upper Paleolithic Homo lateral phalanges have robust diaphysis implying the habitual absence of protective footwear, whereas the Upper Paleolithic ones are variably gracile, especially at higher latitudes, indicating more consistent use of footwear. These paleontological considerations provide a framework for interpreting the distal portions of earlier hominin footprints (especially with respect to hallucal orientation and digital length) and suggest that many of the Late Pleistocene footprints may be unrecognized given the use of footwear.
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Belmaker, Miriam. « Hominin Adaptability and Patterns of Faunal Turnover in the Early to Middle Pleistocene Transition in the Levant ». Dans Sourcebook of Paleolithic Transitions, 211–27. New York, NY : Springer New York, 2009. http://dx.doi.org/10.1007/978-0-387-76487-0_12.

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Piperno, D. R. « Prehistoric human occupation and impacts on Neotropical forest landscapes during the Late Pleistocene and Early/Middle Holocene ». Dans Tropical Rainforest Responses to Climatic Change, 185–212. Berlin, Heidelberg : Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-05383-2_6.

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Karrow, P. F., G. S. Morgan, R. W. Portell, E. Simons et K. Auffenberg. « Middle Pleistocene (early Rancholabrean) vertebrates and associated marine and non-marine invertebrates from Oldsmar, Pinellas County, Florida ». Dans Palaeoecology and Palaeoenvironments of Late Cenozoic Mammals, 97–133. Toronto : University of Toronto Press, 1996. http://dx.doi.org/10.3138/9781487574154-009.

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Moncel, Marie-Hélène. « Technological Behavior and Mobility of Human Groups Deduced from Lithic Assemblages in the Late Middle and Early Late Pleistocene of the Middle Rhône Valley (France) ». Dans Neanderthal Lifeways, Subsistence and Technology, 261–87. Dordrecht : Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0415-2_22.

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Koenigswald, Wighart von. « Discontinuities in the Faunal Assemblages and Early Human Populations of Central and Western Europe During the Middle and Late Pleistocene ». Dans Vertebrate Paleobiology and Paleoanthropology, 101–12. Dordrecht : Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0492-3_9.

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Richmond, G. M. « The INQUA-approved provisional Lower-Middle Pleistocene boundary ». Dans The Early Middle Pleistocene in Europe, 319–27. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077879-22.

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West, R. G. « Outline of the stratigraphy and vegetational history of the Cromer Forest-bed Formation ». Dans The Early Middle Pleistocene in Europe, 1–8. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077879-1.

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Grüger, Eberhard. « Palynostratigraphy of the Middle Pleistocene sequence from Göttingen, Otto-Strasse ». Dans The Early Middle Pleistocene in Europe, 173–80. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077879-10.

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Actes de conférences sur le sujet "Early Middle Pleistocene"

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Kartoziia, Andrei A., Olga B. Kuzmina, Irina V. Khazina, Leonid B. Khazin et Anastassiya V. Mishina. « Lithology and palynology of neogene-quaternary sediments of Sardakh island (the Lena river delta) ». Dans Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-011.

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Results of the study of Neogene-Quaternary deposits of Sardakh Island (the Lena Delta) are described here. Taxonomic composition and spore-pollen spectra structure analysis indicated that sandstones, which are located in the section bottom have middle-late Miocene age. The middle part of the studied section has a Pliocene - early Pleistocene age. The upper part has a late Pleistocene age. We assume that sediments were deposited in the river environments.
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Kulakov, S. « К ВОПРОСУ О СТРАТИГРАФИИ И ГЕОЛОГИЧЕСКОМ ПОЛОЖЕНИИ КОСТЕНОСНОЙ ЛИНЗЫ В КУЛЬТУРОСОДЕРЖАЩИХ ОТЛОЖЕНИЯХ СТОЯНКИ БОГАТЫРИ/СИНЯЯ БАЛКА : ВЗГЛЯД АРХЕОЛОГА ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-65-90.

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Belyaeva, E. « ДИНАМИКА ПРИРОДНОЙ СРЕДЫ И УСЛОВИЯ ОБИТАНИЯ РАННЕПАЛЕОЛИТИЧЕСКИХ ЛЮДЕЙ НА ЗАКАВКАЗСКОМ НАГОРЬЕ В РАННЕМ И СРЕДНЕМ ПЛЕЙСТОЦЕНЕ ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-25-40.

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Shchelinsky, V., et E. Kuznetcov. « МЕСТОНАХОЖДЕНИЯ СОРОКИН И ИГНАТЕНКОВ КУТОК НА ТЕРРАСАХ р. ПСЕКУПС (ЗАКУБАНЬЕ) В КОНТЕКСТЕ РАННЕГО И СРЕДНЕГО ПАЛЕОЛИТА СЕВЕРО-ЗАПАДНОГО КАВКАЗА ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-91-142.

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Belyaeva, E. « PREFACE ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-5-6.

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Belyaeva, E. « РАННЕАШЕЛЬСКИЕ ИНДУСТРИИ ЗАКАВКАЗСКОГО НАГОРЬЯ И СОПРЕДЕЛЬНЫХ ТЕРРИТОРИЙ КАВКАЗА И БЛИЖНЕГО ВОСТОКА ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-41-64.

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Tesakov, A., V. Trifonov, A. Simakova, S. Sokolov, Ya Trikhunkov, H. Çelik, P. Frolov et al. « ГЕОДИНАМИЧЕСКИЕ И БИОЦЕНОТИЧЕСКИЕ УСЛОВИЯ РАННЕГО-СРЕДНЕГО ПЛЕЙСТОЦЕНА В КОНТЕКСТЕ ЗАСЕЛЕНИЯ ДРЕВНИМ ЧЕЛОВЕКОМ КРЫМСКО-КАВКАЗСКО-АРАВИЙСКОГО РЕГИОНА ». Dans The Early Paleolithic sites and environments of the Caucasus and adjacent areas in the Early-Middle Pleistocene. Institute for the History of Material Culture of the Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-85803-549-7-7-24.

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Rovey, Charles W., et Greg Balco. « STRATIGRAPHIC COMPLEXITY WITHIN THE EARLY AND MIDDLE PLEISTOCENE TILL SEQUENCE IN NEBRASKA AND WESTERN IOWA ». Dans 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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Jonsson, Carl H. W., Richard Hebda, Richard Hebda, René W. Barendregt et René W. Barendregt. « THE HIGHLAND VALLEY FORMATION : CONTINUOUS EARLY TO MIDDLE PLEISTOCENE DEPOSITS IN SOUTH CENTRAL BRITISH COLUMBIA, CANADA ». Dans GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285112.

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Makshaev, Radik, Alexander Svitoch, N. Tkach et Daria Lobacheva. « THE LATE PLEISTOCENE PALEOESTUARY LITHOFACIES OF THE EARLY KHVALYNIAN BASIN (THE MIDDLE VOLGA RIVER VALLEY, RUSSIA) ». Dans GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-365405.

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Rapports d'organisations sur le sujet "Early Middle Pleistocene"

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Dafoe, L. T., K. Dickie, G. L. Williams et 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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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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Hodnett, John, Ralph Eshelman, Nicholas Gardner et Vincent Santucci. Geology, Pleistocene paleontology, and research history of the Cumberland Bone Cave : Potomac Heritage National Scenic Trail. National Park Service, janvier 2023. http://dx.doi.org/10.36967/2296839.

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The Cumberland Bone Cave is a public visitation stop along the Potomac Heritage National Scenic Trail renowned for its unique fossil resources that help reconstruct Appalachian middle Pleistocene life in the mid-Atlantic region of North America. This site is gated for safety and to prevent unwanted exploration and damage. Approximately 163 taxa of fossil plant and animals have been collected from Cumberland Bone Cave since 1912. Most of the fossils that have been published pertain to mammals, including many extinct or locally extirpated genera and species. Though the early excavations made by the Smithsonian Institution between 1912 and 1915 are the best known of the work at Cumberland Bone Cave, over many decades multiple institutions and paleontologists have collected and studied the fossil resources from this site up until 2012. Today, fossils from Cumberland Bone Cave are housed at various museum collections, including public displays at the National Museum of Natural History in Washington D.C. and the Allegany Museum in Cumberland, Maryland. This report summarizes the geology, fossil resources, and the history of excavation and research for Potomac Heritage Trail’s Cumberland Bone Cave.
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