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5 results for “Neolithic transition”

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zenodo48/100

PALEODEM/ What burned the forest? Wildfires, climate change and human activity during the Mesolithic – Neolithic transition in SE Iberian Peninsula

<p>This repository contains new XRD data from the Villena paleolake, archaeological radiocarbon evidence from the Villena area and the R code used to produce Summed Probability distribution analyses.&nbsp;&nbsp;</p> <p>They correspond to the following reference:&nbsp;&nbsp;</p> <p>S&aacute;nchez-Garc&iacute;a, C., Revelles, J., Burjachs, F., Euba, I., Exp&oacute;sito, I., Ib&aacute;&ntilde;ez, J., Schulte, L., Fern&aacute;ndez-L&oacute;pez de Pablo, J.&nbsp;What burned the forest? Wildfires, climate change and human activity during the Mesolithic &ndash; Neolithic transition in SE Iberian Peninsula (submitted to Catena).&nbsp;</p> <p>We specify the content of file further down:</p> <ul> <li>Vinalopo.csv: the list of radiocarbon dates from Villena spanning ca.9500-5500 cal BP from the following sites: Arenal de la Virgen, Cueva del Lagrimal and Casa Corona.&nbsp;</li> <li>ngrip.csv: NGRIP GICC05 paleotemperature record based on oxygen isotope series from Rasmussen SO&nbsp;<em>et al.</em>2006 A new Greenland ice core chronology for the last glacial termination.&nbsp;<em>J. Geophys. Res. Atmos.</em><strong>111</strong>. (doi:10.1029/2005JD006079) and&nbsp;Andersen KK&nbsp;<em>et al.</em>2006 The Greenland Ice Core Chronology 2005, 15&ndash;42ka.&nbsp;Part 1: constructing the time scale.&nbsp;<em>Quat. Sci. Rev.</em>25, 3246&ndash;3257.</li> <li>Char.csv:&nbsp;&nbsp;Sedimentary charcoal data set from the Villena Paleolake (VL3 core) published by Jones, S.E., Burjachs, F., Fern&aacute;ndez-L&oacute;pez de Pablo (2018)&nbsp;DOI/10.5281/zenodo.1244003, according to the new Bacon chronological model of the Villena paleolake (Fern&aacute;ndez-L&oacute;pez de Pablo et al., 2022&nbsp;. Impacts of Early Holocene environmental dynamics on open-air occupation patterns in the Western Mediterranean: insights from El Arenal de la Virgen (Alicante, Spain).&nbsp;<a href="https://doi.org/10.31235/osf.io/5yqsr">https://doi.org/10.31235/osf.io/5yqsr</a>)</li> <li>SPD_analysis.R: R script with the code to reproduce the SPD analysis presented in the manuscript.&nbsp;</li> <li>SupplMat1xlsl: an excel file&nbsp;This file is composed by 8 spreadsheets:</li> </ul> <ol> <li>&lsquo;Selected variables 12.6-5.5&rsquo;: all the data included in the time frame 12600-5500 cal BP, interpolated to 50 yr time windows. These data have been used for the Spearmans&rsquo;rs correlation analysis (see spreadsheet &lsquo;Spearmans&rsquo;rs 12.6-5.5&rsquo; to track the results), Detrended Correspondence Analysis (see spreadsheet &lsquo;Figure 5_DCA 12.6-5.5&rsquo; to track the results) and have been plotted in Figure 3 and 7.&nbsp;</li> <li>&#39;Selected variables 9.1-5.5&rsquo;: data included in the analysis focused on the time period 9.1-5.5 cal BP, interpolated to 50 yr time windows. These data have been used for the Spearmans&rsquo;rs correlation analysis (see spreadsheet &lsquo;Spearmans&rsquo;rs 9.1-5.5&rsquo; to track the results), Detrended Correspondence Analysis (see spreadsheet &lsquo;Figure 6_DCA 9.1-5.5&rsquo; to track the results) and have been plotted in Figure 8.</li> <li>&lsquo;Spearmans&rsquo;rs 12.6-5.5&rsquo;: Spearmans&rsquo;rs correlation analysis applied to the 12600-5500 cal BP dataset (data from &lsquo;Selected variables 12.6-5.5&rsquo;).</li> <li>&lsquo;Spearmans&rsquo;rs 9.1-5.5 cal BP&rsquo; Spearmans&rsquo;rs correlation analysis applied to the 9100-5500 cal BP dataset, including here high-resolution XRD data (data from &lsquo;Selected variables 9.1-5.5&rsquo;).</li> <li>&lsquo;Figure 2 charcoal results&rsquo;: original sedimentary charcoal results provided in this work. Data plotted in Figure 2.&nbsp;</li> <li>&lsquo;Figure 4 XRD results&rsquo;: original XRD results provided in this work. Data plotted in Figure 4.</li> <li>&lsquo;Figure 5 DCA 12.6-5.5&rsquo;: results of Detrended Correspondence analysis focused on the time period from 12600 to 5500 cal BP. Data plotted in Figure 5.</li> <li>&lsquo;Figure 6 DCA 9.1-5.5&rsquo; results of Detrended Correspondence analysis focused on the time period from 9100 to 5500 cal BP, including here high-resolution XRD data. Data plotted in Figure 6.</li> </ol>

opencc-by-4.0Nov 2022View details →
zenodo44/100

Radiocarbon dates for the Mesolithic-Neolithic transition in Iberia

<p>Radiocarbon dates to explore the chronology absolute of the Neolithic transition in the Iberian peninsula. A shapefile (GIS format has been upload too).</p>

opencc-by-4.0Apr 2018View details →
zenodo44/100

Genotype Data for "A genomic snapshot of demographic and cultural dynamism in Upper Mesopotamia during the Neolithic Transition"

<p>This repository contains genotype data from the article &quot;<a href="https://www.science.org/doi/10.1126/sciadv.abo3609">A genomic snapshot of demographic and cultural dynamism in Upper Mesopotamia during the Neolithic Transition</a>&quot;. Dataset preparation protocols are described in the article. Here, we only include the genotype files of 13 newly published &Ccedil;ay&ouml;n&uuml; samples in eigenstrat format.</p> <p>The 1KGYoruba suffix refers to the dataset prepared using variable positions in the Yoruba population (see the paper for details). Others are well known Human Origins and 1240K panels.&nbsp;</p> <p>Code and processed data related to the paper has been deposited <a href="http://doi.org/10.5281/zenodo.7086441">here</a>.</p> <p>* The first version has missing individuals.&nbsp;</p>

opencc-by-4.0Nov 2022View details →
dryad36/100

4500 years of morphological diversification in Western Europe wild boars (Sus scrofa) and the consequences of the Neolithic transition

<p>Evolutionary biologists have recently solicited archaeologists to help document and understand the morphological evolution of animals in response to human activities and, more globally, to help reconstruct the history and significance of the anthropogenic impact on worldwide ecosystems. Artificial selection associated with domestication is the best-known example of a major anthropogenic morphological evolution preserved in the archaeological record. However, the impact of the domestication process and dispersal on the morphological evolution of animals has been far less explored. To fill this gap, we focused on 5,000 years of Neolithic transition in Western Europe – a major anthropogenic ecological disturbance involving landscape modification and the translocation of domestic mammals. Using geometric morphometrics on key phenotypic markers preserved in the archaeological record associated with isotopic studies, we explored how and according to which cultural drivers the Neolithic niche construction has influenced the morphological evolution of wild boars (<em>Sus</em> <em>scrofa</em>). The decoupling of size and shape components from bone morphological variation has facilitated the identification of several processes of phenotypic diversification of <em>Sus</em> <em>scrofa</em> in response to human behaviour during the Neolithic transition in Western Europe.</p>

opencc-zeroDec 2022View details →
dryad36/100

4500 years of morphological diversification in Western Europe wild boars (Sus scrofa) and the consequences of the Neolithic transition

Open the record for dataset details and reuse information.

publicDec 2022View details →

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