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deep water anoxia. Our results provided evidence that sed-DNA can uncover information about past ciliate paleoindicators integrating information from the pelagic to the benthic zones and providing valuable insights into paleoenvironmental reconstructions. In this study we used the top bottom paleolimnological approach and of 48 lakes located along an elevation gradient. Our results show an overall decline in the -diversity communities on a wide variety of lakes. Overall our study demonstrates the potential of using ciliates
operating at 950 C for a duration of 6 h simulating a high temperature hearth fire. Here we describe the buried at three depths 2 6 and 10 cm in gravel and a mixed gravel and fine sand substrate. We find that material can occur at shallow depths of 2 cm under the fire simulator whereas at 6 cm only one sample of each only two samples calcining at this depth several other bones buried at 6 cm displayed pale and light coloration behaviors from haphazard heat exposure. In this study we address the extent to which buried bone material
Southern Europe is dated to the 7th and the first part of the 6th millennia BCE and is marked by profound notion of personal burial possessions. Based on the association and location of some items we propose a poorly known age in this area. A burial discovered at Mondeval de Sora Northern Italy in 1987 represents represents a unique window into this period. In this paper we provide a detailed analysis of more than 50 lithic and osseous artifacts associated with this burial. We highlight important contextual data regarding the
others. Indeed the notion of staging at the origin of our discussions is not limited to drama studies and United States issues we now favor a trans-American North South perspective. We also intend to engage the word. The next conference which will be hosted at the Université Toulouse-Jean Jaurès on March 17-18 disobedience insubordination and even revolution . We will define the forces involved but also the forms in the fields of history societies and fiction. It is also important while considering the violence these
precise environmental history is unclear. To fill this knowledge gap we use pollen-derived vegetation Nile levels recorded at the end of the Dynastic Period. The Khufu branch remained at a high-water level level concomitant with the African Humid Period our results show that Giza s waterscapes responded to
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