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236 results for “Eurasia”
The Neanderthal Niche Space of Western Eurasia - Supplemental Material
<p>The data provided here are the supplemental information accompanying the journal article <strong>The Neanderthal Niche Space of Western Eurasia 145ka to 30ka ago</strong> by Yaworsky, Nielsen, & Nielsen. All analyses were performed in R v4.5.0 and are documented in the HTML document, <strong>Supplemental 9</strong>.</p> <p>List of Supplemental Files:</p> <ol> <li><strong>ROCEEH Archaeological Observations - File name: </strong><em><strong>FaunalData_52923_NOANIMALS.csv</strong></em> <ol> <li>Retrieved from <em>Role of Culture in Early Expansions of Humans Out-of Africa Database (</em>http://www.roceeh.net)</li> <li>Original PHP query is found in Supplemental 9. The zooarchaeological observations have been removed from the original PHP query.</li> </ol> </li> <li><strong>ROCEEH Dates Data - File name: </strong><em><strong>Dates_Geog.csv</strong></em> <ol> <li>Retrieved from <em>Role of Culture in Early Expansions of Humans Out-of Africa Database (</em>http://www.roceeh.net)</li> <li>Original PHP query is found in Supplemental 9. These are the Geolayer dates.</li> </ol> </li> <li><strong>ROCEEH Dates Data - File name: </strong><em><strong>Dates_Assem.csv</strong></em> <ol> <li>Retrieved from <em>Role of Culture in Early Expansions of Humans Out-of Africa Database (</em>http://www.roceeh.net)</li> <li>Original PHP query is found in Supplemental 9. These are the ArchLayer dates.</li> </ol> </li> <li><strong>ROCEEH Dates Data - File name: </strong><em><strong>Dates_ArchLayer.csv</strong></em> <ol> <li>Retrieved from <em>Role of Culture in Early Expansions of Humans Out-of Africa Database (</em>http://www.roceeh.net)</li> <li>Original PHP query is found in Supplemental 9. These are the Assemblage dates.</li> </ol> </li> <li><strong>Spatiotemporal Archaeological Observations - File name: </strong><em><strong>ArchaeologicalData_V1.csv</strong></em> <ol> <li>Derived from Supplemental 1 after removing observations that dated outside of the 145ka to 50ka year range, all NA values, and observations duplicated in time and space (1000-year range).</li> </ol> </li> <li><strong>Spatiotemporal Background Points - File name: </strong><em><strong>AbsencePointData.csv</strong></em> <ol> <li>Randomly generated background points. 100 random points were generated in each millennium.</li> </ol> </li> <li><strong>High-Resolution Spatiotemporal Predictions - File name: </strong><em><strong>SDM_MainGIF.mp4</strong></em> <ol> <li>High-resolution mp4 file showing the predictions of the Neanderthal niche space from 145ka to 30ka ago.</li> </ol> </li> <li><strong>Neanderthal Niche Space 145ka to 30ka ago- File name: </strong><em><strong>Human_Niche_Size.csv</strong></em> <ol> <li>Quantification of the Neanderthal niche space for each millennium.</li> </ol> </li> <li><strong>Analysis Markdown Document - File Name: </strong><em><strong>NeanderEdgeMD_v5.html</strong></em> <ol> <li>Markdown illustrating step-by-step the methods used to organize and analyze the data.</li> </ol> </li> <li><strong>Delta O18 Record - File name: </strong><em><strong>LisieckiRaymod18O.csv</strong></em> <ol> <li>Delta O18 Record from Lisiecki & Raymo, 2005.</li> <li>Used in Figure 1 of the publication to illustrate the relationship between Neanderthal niche size and Delta O18 values.</li> </ol> </li> <li><strong>Neanderthal Niche Space 350ka ago to Present - File name: </strong><em><strong>Human_Niche_Size_350k.csv</strong></em> <ol> <li>Neanderthal niche space estimates from 350ka to the present based on the model constructed around the 145ka to 50ka ago archaeological observations.</li> <li>Not discussed in the main publication.</li> </ol> </li> </ol> <p>The NeanderEDGE Project is funded by the Independent Research Fund Denmark (Danmarks Frie Forskningsfond) case number 9062-00027B.</p>
A tectonic model reconciling evidence for the collisions between India, Eurasia and intra-oceanic arcs of the central-eastern Tethys
<p>2 February 2014<br>Version 1.2</p> <p>Supplement and plate model accompanying: <br>Gibbons, A., Zahirovic, S., Müller, R., Whittaker, J., and Yatheesh, V., 2015, A tectonic model reconciling evidence for the collisions between India, Eurasia and intra-oceanic arcs of the central-eastern Tethys: Gondwana Research FOCUS.</p> <p><strong>Gibbons_etal_2015_GR_PlateModel.zip</strong></p> <p>This directory contains four files:</p> <p>TPW_CK95G94_Rigid_Gibbons.rot - the Gibbons et al. global rotation model TPW_CK95G94_PP_Rigid_Gibbons.gpml - the Gibbons et al. global evolving topologies <br>CK95G94_Coastlines.gpmlz - Present-day coastlines with Plate ID assignments<br>CK95G94_StaticPolygons_Gibbons.gpmlz - Present-day block outlines </p> <p>To load these datasets in GPlates do the following:</p> <p>1. Open GPlates<br>2. Pull down the GPlates File menu and select the operation Open Feature Collection<br>3. Click all the files while holding down the shift key to select all files. All the files should be highlighted.<br>4. Click Open </p> <p>Alternatively, drag and drop the files onto the globe.<br> <br>Play around with the GPlates buttons to make an animation, select features, draw features, etc. For more information, read the GPlates manual which can be downloaded from <a href="https://www.gplates.org">www.gplates.org</a></p> <p><strong>Zahirovic_etal_2014_SE</strong></p> <p>This file provides a detailed description of all of the files that make up the data collection associated with the publication: Zahirovic, S., Seton, M., & Müller, R. D. (2014). The Cretaceous and Cenozoic tectonic evolution of Southeast Asia. Solid Earth, 5(1), 227-273. doi:<a href="https://doi.org/10.5194/se-5-227-2014" target="_blank" rel="noopener">10.5194/se-5-227-2014</a></p> <p>Any questions, please email: <br>Ana Gibbons <angi@statoil.com><br>Sabin Zahirovic <sabin.zahirovic@sydney.edu.au></p>
Stress regimes in the Himalaya-Karakoram-Tibet, the western part of India-Eurasia collision: stress field implications based on focal mechanism solution data
<p>This dataset contains valuable information on earthquake events, including their location, magnitude, depth, and focal mechanism solutions. This README file provides detailed explanations of each header in the dataset, as well as information about the files included in the repository.<br><br><em>"Stress regimes in the Himalaya-Karakoram-Tibet, the western part of India-Eurasia collision: stress field implications based on focal mechanism solution data"</em> <strong>(Under Review)</strong><br> </p>
Fig. 20 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 20. Distribution of the studied species of the genus Rhagasostoma Koschinsky, 1885 in the Late Cretaceous of Eurasia.
Fig. 19 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 19. Rhagasostoma mimosa (Brydone, 1930). A–B. Lectotype, SM B36696, early Maastrichtian (Ostrea lunata Zone), Porosphaera Beds of Trimingham, Norfolk, England, UK. A. Part of erect bifoliate colony showing ovicellate (some ooecia arrowed) and non-ovicellate autozooids and aviacularia. B. Detail of autozooids with opesiules and some with vestigial ooecia (arrowed), and avicularia. C. SMF 29923, early Maastrichtian, Island of Møn, Denmark, bifurcating colony showing autozooids some opesiules and avicularia. D–F. Early Maastrichtian of an unknown locality on the Mangyshlak Peninsula, Mangystau Region, Kazakhstan. D–E. PIN 5502/3057. D. Part of erect bifoliate colony showing autozooids and aviacularia. E. Detail of autozooids with opesiules and avicularia. F. PIN 5502/3056, autozooids with opesiules and avicularia. Scale bars: A = 200 µm; B = 100 µm; C = 1 mm; D = 2 mm; E–F = 500 µm.
Fig. 18 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 18. Rhagasostoma rowei (Brydone, 1906). A. SMF 29932, early Maastrichtian, Rügen, Germany, overview of erect bifoliate stem-like then dichotomously branching colony. B–C. SMF 29925, early Maastrichtian, Island of Møn, Denmark. B. Overview of erect bifoliate stem-like then dichotomously branching colony. C. Opesia and opesiules of avicularium. D. SMF 29933, late Maastrichtian, former brick factory, Hamburg-Hummelsbüttel, Germany, showing the parallel-sided base of erect bifoliate colony with rare avicularia. E. TsNIGR Museum 36/9757, late Maastrichtian, Turkmenistan, Tuarkyr, showing the parallel-sided base of erect bifoliate colony with rare avicularia. F–H. Maastrichtian, Kazakhstan, Mangyshlak Peninsula. F–G. PIN 3421/1009. F. Erect bifoliate colony, almost parallelsided but widening distally. G. The widest part of the colony showing autozooids and numerous avicularia. H. PIN 3421/1008, showing autozooids with long cryptocystal tongues, and avicularia. I. TsNIGR Museum 32/9757, late Maastrichtian, Turkmenistan, western Kopetdag, showing ovicellate (arrows) and non-ovicellate autozooids with long cryptocystal tongues, and avicularia. J. PIN 5502/3050, Maastrichtian, Kazakhstan, northern Aral Sea Region, showing autozooids and avicularia. Scale bars: A–B, D, H, J = 1 mm; C = 100 µm; E–G = 2 mm; I = 500 µm.
Fig. 13 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 13. Rhagasostoma gibbosum (Marsson, 1887). A–C. Erratic block of?late Campanian age, quarry near Hrodna/Grodno (Гродна/Гродно), Grodno Region, Belarus. A. PIN 2922/218, overview of erect bifoliate colony showing autozooids, avicularia and kenozooids. B. PIN 2922/216, autozooids with proximal peripheral caverns (Cv) and broken ooecium (arrowed), avicularia. C. PIN 2922/275, nonovicellate autozooids with proximal caverns and avicularia. D–E. Late Campanian (Belemnitella lanceolata Zone), Emba River, Kazakhstan. D. PIN 5502/3058, overview of erect bifoliate colony showing autozooids (some ovicellate), avicularia and kenozooids. E. PIN 5502/3059, non-ovicellate and ovicellate autozooids, some with gymnocyst (arrowed), and avicularia. Scale bars: A, D–E = 1 mm; B–C = 500 µm.
Fig. 11 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 11. Rhagasostoma operculatum sp. nov. A–C. Holotype, TsNIGR Museum 27/12582, western Kopetdag, Turkmenistan, boundary between the early and late Campanian (Cibicidoides temirensis/ Bolivinoides decoratus decoratus Zone, LS13). A. Overview of erect bifoliate colony. B. Autozooids with putative opercula and avicularia. C. Autozooids with putative opercula and avicularium. Scale bars: A = 1 mm; B = 500 µm; C = 200 µm.
Fig. 9. Rhagasostoma angliae Brydone, 1936. A–C in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 9. Rhagasostoma angliae Brydone, 1936. A–C. SM B36671, Middle Campanian (Belemnitella mucronata Zone), Weybourne, Norfolk, England, UK. A. Overview of erect bifoliate colony. B. Nonovicellate autozooids and avicularia. C. Opesiae of non-ovicellate autozooids with distal shelf and avicularium. D–E. SMF 29914, Late Campanian of Vigny, Île-de-France, France. D. Overview of erect bifoliate colony. E. Non-ovicellate and one ovicellate (with partially broken ooecium, arrowed) autozooids and avicularia. F–G. SMF 26288, early Maastrichtian of Hemmor, Germany. F. Overview of erect bifoliate colony. G. Non-ovicellate autozooids and avicularia. Scale bars: A, D = 1 mm; B, G = 200 µm; C = 100 µm; E = 300 µm; F = 2 mm.
Fig. 10 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 10. Rhagasostoma aralense sp. nov., southern Aral Sea Region, Uzbekistan. A–F. Holotype, TsNIGR Museum 26/12582, early Campanian, Cibicidoides temirensis/Bolivinoides decoratus decoratus Zone. A. Overview of erect bifoliate colony. B. Autozooids with proximolateral peripheral caverns and avicularia. C. Opesia of non-ovicellate autozooid with crenulated proximal edge. D. Edge of the colony with autozooids, avicularia, and kenozooids. E. Non-ovicellate autozooids with proximal peripheral caverns and avicularium. F. Non-ovicellate autozooids and avicularia. G. Paratype, TsNIGR Museum 28/12582, middle Campanian, Brotzenella monterelensis Zone, ovicellate autozooid and avicularium. Scale bars: A = 1 mm; B = 500 µm; C = 100 µm; D–G = 200 µm.
Fig. 7. Rhagasostoma minuens Brydone, 1936. A–C in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 7. Rhagasostoma minuens Brydone, 1936. A–C. Coniacian, Chatham, Kent, England, UK. A–B. SMF 29921. A. Overview of erect bifoliate colony. B. Autozooids with proximolateral peripheral caverns (Cv) and broken ooecia, avicularia, and intramural avicularia within host avicularia (arrowed). C. SMF 29922, autozooids with proximolateral peripheral caverns (arrowed) and broken ooecia (some with reparative sutures). D. SMF 29920, early Campanian, Harnham, SW of Salisbury, Wiltshire, England, UK; non-ovicellate autozooids, some with proximal peripheral caverns, and avicularia; intramural kenozooids observed within host autozooid and avicularia (arrowed). E–F. Early Campanian, Meeching Quarry, Newhaven, East Sussex, England, UK. E. SMF 29943, ovicellate (with broken ooecia) and non-ovicellate autozooids, some with proximal peripheral caverns, avicularia, and intramural kenozooid within a host avicularium (arrowed). F. SMF 29944, ovicellate (with broken ooecia) and non-ovicellate autozooids with proximal peripheral caverns and avicularia. G. SMF 29918, Campanian, Hanches, France, overview of bifoliate colony showing autozooids and avicularia. H. SM B36678, specimen (a), late Campanian to early Maastrichtian (Ostrea lunata Zone) [middle Campanian (Belemnitella mucronata Zone), Weybourne, Norfolk, in SM database], Trimingham, Norfolk, England, UK; autozooids with peripheral caverns surrounding the cryptocyst and avicularia. Scale bars: A = 2 mm; B, E–G = 1 mm; C = 500 µm; D = 300 µm; H = 200 µm.
Fig. 4 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 4. Rhagasostoma inelegans (Lonsdale, 1850). A–C. Early Campanian, Alemannia quarry, Sehnde-Höver, Lower Saxony, Germany. A–B. SMF 24564. A. Distal part of erect bifoliate colony. B. Autozooids and avicularia (ooecia of endozooidal ovicells are clearly visible). C. SMF 29915, fragment of erect bifoliate colony with rare ovicellate autozooids, intramural non-ovicellate autozooid within autozooid and intramural avicularia within avicularia (arrowed). D–F. Erratic block of Campanian age, quarry near Hrodna/Grodno (Гродна/Гродно), Grodno Region, Belarus. D. PIN 2922/219, overview of erect bifoliate colony with row of three ovicellate autozooids, one with a broken ooecium, and avicularia. E–F. PIN 2922/273. E. Autozooid with broken ooecium, avicularia and non-ovicellate autozooids. F. Intramural non-ovicellate autozooid within autozooid and intramural avicularium within avicularium, and normal avicularium. Scale bars: A, C–D = 1 mm; B = 300 µm; E = 500 µm; F = 200 µm.
Fig. 5 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 5. Rhagasostoma brydonei sp. nov. A–D. Latest Turonian (Sternotaxis plana Zone), Kings Lane, Froxfield, south of Alton, Hampshire, England, UK. A–B. Holotype, SM B36666. A. Overview of erect bifoliate colony. B. Autozooids (Az) and kenozooids (Kz) with peripheral caverns (arrowed) and avicularia. C–D. Paratype SM B36667. C. Overview of erect bifoliate colony. D. Autozooids with peripheral cavern surrounding the cryptocyst (arrowed) and avicularia. E–H. Coniacian, Chatham, Kent, England, UK. E. Paratype, SMF 29940, autozooids with proximal peripheral caverns (arrowed) and avicularia. F. Paratype, SMF 29939, autozooids with peripheral cavern surrounding the cryptocyst and avicularia. G–H. Paratype, SMF 29941. G. Autozooids with peripheral cavern surrounding the cryptocyst and avicularia. H. Autozooids with peripheral cavern surrounding the cryptocyst and ooecia of immersed ovicells (arrowed) and avicularia. Scale bars: A, D, H = 200 µm; B = 100 µm; C, F = 1 mm; E, G = 500 µm.
Fig. 2 in Rhagasostoma (Bryozoa) from the Late Cretaceous of Eurasia: taxonomic revision, stratigraphy and palaeobiogeography
Fig. 2. Map of the Caspian and Aral seas region showing localities of bryozoan material examined or mentioned in this study. Abbreviations: Emb = Emba River, Aqtöbe Region, Kazakhstan; Kop = western Kopetdag, Balkan Region, Turkmenistan; Man = Mangyshlak Peninsula, Mangystau Region, Kazakhstan; NAS = northern Aral Sea region, Kyzylorda Region, Kazakhstan; SAS = southern Aral Sea region north of Chimboy/Shımbay, Republic of Karakalpakstan, Uzbekistan; Tua = Tuarkyr, Balkan Region, Turkmenistan.
Data of LAI-L20C in Vegetation masking effect on future warming and snow albedo feedback in a boreal forest region of northern Eurasia according to MIROC-ESM
<p>Data of LAI-L20C experiment in the research paper: Vegetation masking effect on future warming and snow albedo feedback in a boreal forest region of northern Eurasia according to MIROC-ESM.</p> <p>The paper was submitted to JGR-Atmosphere.</p> <p>Variables are limited to those used in the paper.</p> <ul> <li>snow water equivalent (swe)</li> <li>snow cover fraction (snc)</li> <li>clear-sky downward shortwave radiation at surface (rsdscs)</li> <li>clear-sky upward shortwave radiation at surface (rsuscs)</li> <li>surface air temperature (tas)</li> </ul> <p>See the paper for the detail.</p>
Fig. 4 in New Data On Phylogeography Of The Boreal Owl, Aegolius Funereus (Strigiformes, Strigidae), In Eurasia
Fig. 4. Boreal Owl mtDNA CR1 haplotype distribution across it's Eurasian range. Colored dots indicate approximate regions of sampling for individuals possessing the corresponding haplotype. White dots with numbers reflect the total number of unique haplotypes for this region.
Fig. 2 in New Data On Phylogeography Of The Boreal Owl, Aegolius Funereus (Strigiformes, Strigidae), In Eurasia
Fig. 2. Mismatch distribution graph for the pairwise comparison of mtDNA CR1 sequences of Eurasian Boreal Owl population. X axis reflects pairwise difference, Y axis reflects frequency of the difference across sequences; Freq. Obs. is the studied sample's observed mismatch frequency graph, Freq. Exp. is the expected frequency for the sudden expansion model.
Fig. 3 in New Data On Phylogeography Of The Boreal Owl, Aegolius Funereus (Strigiformes, Strigidae), In Eurasia
Fig. 3. Median joining network of mtDNA CR1 haplotypes for the studied Boreal Owl sample. Each circle reflects a mtDNA CR1 haplotype. Circle sizes reflect the number of studied individuals possessing the haplotype; circle colors reflect geographic origin of individuals possessing the haplotype. Bars connect related haplotypes, with notches on bars reflecting the number of nucleotide differences between them. Black dots indicate implied haplotypes not present in the sample.
Fig. 1 in New Data On Phylogeography Of The Boreal Owl, Aegolius Funereus (Strigiformes, Strigidae), In Eurasia
Fig. 1. The source regions of Boreal Owl mtDNA CR1 sequences used in the present study. Numbered yellow circles indicate sampling regions for utilized Boreal Owl mtDNA CR1 sequences, as well as the number of sequences per each region. Green coloration indicates boreal owl's range.
Extreme Erosion Events database for Eurasia
<p>Climate changes lead to an increase of extreme events frequency and intensity (hurricanes, floods, extreme<br> rainfall), and as a consequence to the intensification of erosion processes both in the<br> mountainous and plain regions. Database of extreme erosion events (EEEs) was created on the basis of literature review.</p> <p><em>This work was supported by the Russian Foundation for Basic Research under grant 16-05-00815.</em></p> <p>Изменение климата приводит к увеличение частоты и интенсивности экстремальных событий (ураганы, наводнения, экстремальные осадки), в результате происходит интенсификация эрозионных процессов как в горных так и в равнинных регионах. На основе анализа литературы была создана база данных Экстремальных эрозионных событий (ЭЭЭ) в Евразии.</p> <p><em>Работа выполнена при финансовой поддержке Российского фонда фундаментальных исследований, грант 16-05-00815.</em></p>
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