Upper Pleistocene oor Duits

Upper Pleistocene

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Upper Pleistocene [noun] [geol.]
enthält die Synonyme Vidua amauropteryx, Vidua centralis, Vidua neumanni, Vidua okavangoensis und Vidua ultramarinalangbot langbot
Upper Pleistocene
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The soil is of the Upper Pleistocene, comprising 10-30 m deep typical loess, sandy sloping loess, loessial sands and quicksand or fixed windblown sand.
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Mammuthus lamarmorai is a species of mammoth which lived during the late Middle and Upper Pleistocene (between 450,000 and perhaps 40,000 years) on the island of Sardinia.
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Finds from the Upper Pleistocene, which comprise a plurality of teeth are mainly from Tramariglio, near the city of Alghero, and came also from deposited sediments by wind, but above the Tyrrhenian conglomerate.
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The higher coast-lines are corresponding to the Tyrrhenian I (= upper part of the middle-Pleistocene), the lower ones are paralleled with the Monastirian I/II (= Tyrrhenian II = middle part of the upper-Pleistocene).
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The occurrence of this mammoth already in the late Middle Pleistocene makes that a descent from the classic woolly mammoth (M. primigenius) rather unlikely, since this latter species first appeared in Europe during the Upper Pleistocene.
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They range from Upper Eocene to Pleistocene time, i. e. about 40 mill, years.
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In Upper Pliocene/lowermost Pleistocene marine sediments of SE-Lakonia (Greece) shell fragments ofTestudo marginata have been found.
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The sponge-bearing strata correspond to the nannoplankton zone 21 (Emiliania huxleyi zone: Upper Pleistocene—Holocene). Various pathsways in the diagenetic alteration of the siliceous skeleton can be observed: In all cases the diagenetic history starts with sediment infill and lithification with high Mg-calcite (HMC) in the space between the spicules, where organic matter of the living sponge previously was present.
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Block tectonic movements with N-S and NNE-SSW directions from Upper Tertiary through Pleistocene affected the normal morphology of the fans.
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Volcanic ashes, resulting from Plinian type eruptions, are regularly interbedded with fluvio-lacustrine successions of the Plio-Pleistocene Upper Webi Shebele Basin in the southeastern uplands of Ethiopia.
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A wide range of relatively undifferentiated lavas, ranging in composition from quartz-tholeiites to ankaratrites, were erupted in the Iblean area (SE Sicily) during the Upper Miocene-Lower Pleistocene.
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These highly oblique faults with strike-slip movements, that affect the whole region, are probably ancient lineaments reactivated during Andean diastrophism in Upper Pliocene to Early Pleistocene time.
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In the whole area a Triassic to Middle Cretaceous ophiolite series and after an intervall of extremely intense tectonical movements — an Upper Cretaceous to Pleistocene granitoid, subsequent andesitic-rhyolitic magmatism and a final basaltic volcanism can be distinguished.
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Erosion, denudation and accumulation processes in the Upper Pliocene and during the Pleistocene laid the foundations for the morphology of the basin floor.
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Some other aspects as the permanent uplift trend of Scandinavia since the Cambrium or the rhythmic to and fro of magma in the upper mantle during the Pleistocene are mentioned.
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An investigation of the upper Kuwait Group clastic sequence (Mio-Pleistocene) exposed along the Jal Az-Zor escarpment in north Kuwait revealed several horizons of fossil calcrete.
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The emission occurred between the upper Miocene and the lower Pleistocene of systems of fissures running N/S and SE/NW, which were formed in connexion with deep faultings during the raise of the Andes.
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A sampling of Plio-Pleistocene and Upper Cretaceous basalts in SE Sicily yielded the following information Assuming that the Cretaceous direction is reversed, the confidence oval for the virtual pole overlaps that for the Cretaceous pole of Africa determined from the Mlanje Syenite byMcElhinny et al.
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This paper documents the discovery and study of an almost complete elephantid pelvis, found in Late Pleistocene deposits in the Upper Rhine valley in the administrative district ‚Im Binsfeld‘ north of Speyer.
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The increase in body size of Gulo gulo during the Upper Pleistocene is confirmed by data.
die Angabe des Prozentsatzes oder der Menge der von der Anlage erzeugten Elektrizität, der bzw. die als auf das nationale Ziel eines Mitgliedstaats anrechenbar zu betrachten ist, sowie die entsprechenden Finanzvereinbarungen, wobei Vertraulichkeitsanforderungen einzuhalten sindParaCrawl Corpus ParaCrawl Corpus
(1963): Contributions to the study of the upper pleistocene-holocene fauna of small mammals (Chiroptera, Insectivora, Glires).
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