Bibliografías temáticas / Early-Middle Pleistocene Transition

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Literatura académica sobre el tema "Early-Middle Pleistocene Transition"

Autor: Grafiati
Publicado: 10 de marzo de 2023
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Early-Middle Pleistocene Transition"

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Peng, Xianzhe, Hong Ao, Guoqiao Xiao, Xiaoke Qiang, and Qiang Sun. "The Early-Middle Pleistocene transition of Asian summer monsoon." Palaeogeography, Palaeoclimatology, Palaeoecology 545 (May 2020): 109636. http://dx.doi.org/10.1016/j.palaeo.2020.109636.

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Madurell-Malapeira, Joan, Maria Prat-Vericat, Saverio Bartolini-Lucenti, et al. "A Review on the Latest Early Pleistocene Carnivoran Guild from the Vallparadís Section (NE Iberia)." Quaternary 7, no. 3 (2024): 40. http://dx.doi.org/10.3390/quat7030040.

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The Vallparadís Section encompasses various geological layers that span a significant chronological range, extending from the latest Early Pleistocene to the early Middle Pleistocene, covering a timeframe from approximately 1.2 to 0.6 Ma. This period holds particular importance, as it coincides with a significant climatic transition known as the Early–Middle Pleistocene Transition, a pivotal phase in Quaternary climatic history. This transition, marked by the shift from a 41,000-year obliquity-driven climatic cycle to a 100,000-year precession-forced cyclicity, had profound effects on the Cala
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Merh, S. S. "Neogene-Quaternary Sequence in Gujarat: A Review." Journal Geological Society of India 41, no. 3 (1993): 259–76. http://dx.doi.org/10.17491/jgsi/1993/410306.

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Abstract The constituent rocks of Neogene are conglomerates, grits, silty sandstones, marls and argillaceous limestones. Marine Quaternaries are represented by the miliolite rocks of Saurashtra (Middle Pleistocene) and younger Holocene Rann sediments, mudflats and beach rocks. The transition of Neogene to Quaternary is not fully understood. Perhaps regressive conditions prevailed during the close of Pliocene and in the early Pleistocene. Evidences point to a bw strandline during the Lower Pleistocene. The Quaternary period is marked by two major transgressions-one in Ihe Middle Pleistocene and
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Maslin, Mark A., and Christopher M. Brierley. "The role of orbital forcing in the Early Middle Pleistocene Transition." Quaternary International 389 (December 2015): 47–55. http://dx.doi.org/10.1016/j.quaint.2015.01.047.

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Markova, Anastasia K., Svetlana A. Sycheva, and Tatiana M. Gorbacheva. "Early Middle Pleistocene Fauna Of Fossil Rodents And LoessPaleosol Series Of The Pekla Key Section (Taman Peninsula, Russia)." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 16, no. 2 (2023): 31–39. http://dx.doi.org/10.24057/2071-9388-2022-169.

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The history of the early Middle Pleistocene small mammal faunas of Eastern Europe is very complicated. The early Middle Pleistocene which spanned from the Brunhes-Matuyama transition (772.9 ka BP, within MIS 19) till the beginning of the Likhvin Interglacial (424 ka BP, MIS 11) includes a number of interglacials and glaciations. Rodent species of the Tiraspolian faunal assemblage were found in the Chaudian fluvial deposits of the Cape Pekla section (northern coast of the Taman Peninsula). The evolutional level of the Pekla rodents are similar to those from the stratotype section of the Tiraspo
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Zieliński, Tomasz. "Prospects and limitations of heavy mineral analyses to discriminate preglacial/glacial transitions in Pleistocene sedimentary successions." Geologos 24, no. 2 (2018): 151–62. http://dx.doi.org/10.2478/logos-2018-0014.

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Abstract The present study revolves around the identification of the stratigraphical boundary between Pleistocene formations that formed prior to the first advance of the Scandinavian ice sheet (Early Pleistocene, i.e., the so-called preglacial) and the overlying, glacially derived deposits (Middle Pleistocene). In particular, it focuses on variation in heavy mineral assemblages, which are an important tool for stratigraphers. The Neogene basement, described here, was most often the source of material that was redeposited by Early Pleistocene rivers. The geological structure and Early Pleistoc
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Johnson, Kenneth G. "Middle Miocene recovery of Caribbean reef corals: New data from the Tamana Formation, Trinidad." Journal of Paleontology 75, no. 3 (2001): 513–26. http://dx.doi.org/10.1017/s0022336000039639.

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Caribbean coral reef communities were restructured by episodes of accelerated biotic change during the late Oligocene/early Miocene and the late Pliocene/early Pleistocene. However, rigorous description of the effects of rapid biotic change is problematic because preservation and exposure of coral-bearing deposits is not consistent in all stratigraphic intervals. In the Caribbean, early and middle Miocene exposures are more rare than late Miocene and Pliocene exposures. One exception is the late early to early middle Miocene Tamana Formation of Trinidad, and old and new collections from this u
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8

Marković, S. B., U. Hambach, T. Stevens, 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 (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 ra
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Markova, Anastasia K. "Eastern European rodent (Rodentia, mammalia) faunas from the Early–Middle Pleistocene transition." Quaternary International 131, no. 1 (2005): 71–77. http://dx.doi.org/10.1016/j.quaint.2004.07.020.

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Huuse, Mads. "Late Cenozoic palaeogeography of the eastern North Sea Basin: climatic vs tectonic forcing of basin margin uplift and deltaic progradation." Bulletin of the Geological Society of Denmark 49 (December 2, 2002): 145–70. http://dx.doi.org/10.37570/bgsd-2003-49-12.

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The late Eocene to middle Pleistocene development of the eastern North Sea Basin is described by a series of palaeogeographic maps. The maps are based on published information integrated with recent investigations of seismic and well data from the eastern North Sea. The maps provide overviews of the basin geometry at late Eocene, late Oligocene, middle Miocene, late Miocene, late Pliocene and middle Pleistocene time. In post-Eocene time, the eastern and central North Sea Basin was progressively filled by large deltas, which built out from the eastern basin margin. These deltas were fed by anci
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Tesis sobre el tema "Early-Middle Pleistocene Transition"

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Jonsson, Carl H. W. "Late-early to middle pleistocene vegetation and climate history of the Highland Valley, British Columbia, Canada." Thesis, 2017. https://dspace.library.uvic.ca//handle/1828/8922.

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The climate and vegetation history of the Middle Pleistocene transition in the interior of British Columbia (BC) is poorly understood due largely to the lack of records. Sediments from the overburden of the Teck Highland Valley Copper mine (HVC) of British Columbia straddle the Brunhes-Matuyama paleomagnetic transition, providing a opportunity to study this critical Pleistocene interval. The stratigraphy was described and sampled for paleomagnetic and pollen/spore analysis at reconnaissance scale. The HVC sediments consist mainly of (from bottom to top) a lower glacial drift, >50 m of lakebed
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Toti, Francesco. "A Mediterranean perspective on the Early-Middle Pleistocene transition with emphasis on marine isotope stage 19." Doctoral thesis, 2018. http://hdl.handle.net/2158/1124617.

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In this thesis, we discuss pollen and dinocysts data from the western and central Mediterranean to reconstruct vegetation and climate during the Early-Middle Pleistocene transition, with emphasis on MIS 19, i.e. the best analogue of the present interglacial.
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Libros sobre el tema "Early-Middle Pleistocene Transition"

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

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Capítulos de libros sobre el tema "Early-Middle Pleistocene Transition"

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Belmaker, Miriam. "Hominin Adaptability and Patterns of Faunal Turnover in the Early to Middle Pleistocene Transition in the Levant." In Sourcebook of Paleolithic Transitions. Springer New York, 2009. http://dx.doi.org/10.1007/978-0-387-76487-0_12.

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Mihailović, Dušan. "Lower Palaeolithic Settlement of the Balkans: Evidence from Caves and Open-air Sites." In The Prehistoric Hunter-Gatherers of South-Eastern Europe. Oxford University PressNew York, 2023. http://dx.doi.org/10.1093/9780197267509.003.0002.

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Abstract It is assumed that the Balkan Peninsula may have represented a major migratory corridor and the area where hominin groups initially adapted to the ecological conditions of the temperate climate during the Early and Middle Pleistocene. Until recently, these ideas could only be assessed hypothetically, due to the very small number of identified archaeological sites. This situation changed with discoveries of sites in the Lower Danube (Kozarnika, Dealul Guran), Aegean (Kokkinopilos, Marathousa 1, Rodafnidia) and Central Balkan (Balanica Cave Complex) regions, which presented artefacts in
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3

Mihailović, Dušan. "Lower Palaeolithic Settlement of the Balkans: Evidence from Caves and Open-air Sites." In The Prehistoric Hunter-Gatherers of South-Eastern Europe. British Academy, 2023. http://dx.doi.org/10.5871/bacad/9780197267509.003.0002.

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Abstract It is assumed that the Balkan Peninsula may have represented a major migratory corridor and the area where hominin groups initially adapted to the ecological conditions of the temperate climate during the Early and Middle Pleistocene. Until recently, these ideas could only be assessed hypothetically, due to the very small number of identified archaeological sites. This situation changed with discoveries of sites in the Lower Danube (Kozarnika, Dealul Guran), Aegean (Kokkinopilos, Marathousa 1, Rodafnidia) and Central Balkan (Balanica Cave Complex) regions, which presented artefacts in
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4

Munsterman, Dirk K., Timme H. Donders, Alexander J. P. Houben, Johan H. ten Veen, and Frank P. Wesselingh. "Paleogene – Neogene." In Geology of the Netherlands. Amsterdam University Press, 2025. https://doi.org/10.5117/9789463728362_ch09.

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Abstract During the late Danian-Selandian Laramide phase, open-marine carbonate deposition of the Late Cretaceous and earliest Paleocene was replaced by clastic sediment infill of the Southern North Sea Basin. The Laramide phase, associated with domal uplift and subsidence of Mesozoic grabens, led to a break in sedimentation and reworking of Upper Cretaceous carbonates into marls. Consequently, Paleogene marine deposits are condensed in most areas. Late Paleocene to earliest Eocene uplift of basin margins caused major sand influxes into marginal marine environments with restricted circulation.
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