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235 results for “Western Europe”
FIG. 2 in New data about the diversity of Early Oligocene eomyids (Mammalia, Rodentia) in Western Europe
FIG. 2. — Eomys antiquus (Aymard, 1853) lower teeth, MÖhren 13: A, Rdp4, BSP 1972 XI 4261; B, Rdp4, BSP 1972 XI 4262; C, Rp4, BSP 1972 XI 4082; D, Rp4, BSP 1972 XI 4098; E, Lp4, BSP 1972 XI 4074; F, Lp4, BSP 1972 XI 4058; G, Lp4, BSP 1972 XI 4059; H, Lp4, BSP 1972 XI 4060; I, Lp4, BSP 1972 XI 4064; J, Rm1/2, BSP 1972 XI 4122;K, Rm1, BSP 1972 XI 4135; L, Rm1/2, BSP 1972 XI 4133;M, Rm1/2, BSP 1972 XI 4148; N, Lm2, BSP 1972 XI 4171; O, Lm2, BSP 1972 XI 4196; P, Lm1/2, BSP 1972 XI 4135; Q, Lm1, BSP 1972 XI 4118; R, Rm3, BSP 1972 XI 4210; S, Rm3, BSP 1972 XI 4245; T, Rm3, BSP 1972 XI 4251; U, Lm3, BSP 1972 XI 4232. Scale bar: 0.5 mm.
Fig. 6 in La Piquera in central Iberian Peninsula: A new key vertebrate locality for the Early Pliocene of western Europe
Fig. 6. ESEM images of insectivores from La Piquera site, Lower Pliocene, Duero Basin, Spain. A. Soricid Myosorex meini Jammot, 1977, UCM-LPQEUL-1, right M1 in occlusal view. B. Soricid Neomyini indet., UCM-LPQ-EUL-2, left mandibular fragment with p4–m2 in lateral view. C. Neomyini indet., UCM-LPQ-EUL-3, left mandibular fragment with m2 in lateral view. D. Erinaceid Parasorex ibericus (Mein and Martín-Suárez, 1993), UCM-LPQ-EUL-4, right M1 in occlusal view.
Fig. 7 in La Piquera in central Iberian Peninsula: A new key vertebrate locality for the Early Pliocene of western Europe
Fig. 7. ESEM images of rodents from La Piquera site, Lower Pliocene, Duero Basin, Spain, all in occlusal view. A. Cricetid Ruscinomys lasallei Adrover, 1969, UCM-LPQ-ROD-1, left M1. B. Cricetid Blancomys aff. sanzi Adrover, Mein, and Moissenet, 1993, UCM-LPQ-ROD-2, right M1. C. Cricetid Apocricetus cf. barrierei (Mein and Michaux, 1970), UCM-LPQ-ROD-3, left M1. D, E. Murid Stephanomys dubari Aguilar, Michaux, Bachelet, Calvet, and Faillat, 1991. D. UCM-LPQ-ROD-4, right M1. E. UCM-LPQ-ROD-5, right m1 and m2. F. Murid Occitanomys alcalai Adrover, Mein, and Moissenet, 1988, UCM-LPQ-ROD-6, left M1. G. Murid Apodemus gorafensis Ruiz Bustos, Sesé, Dabrio, Peña, and Padial, 1984, UCM-LPQ-ROD-7, right M1. H. Murid Castillomys gracilis van de Weerd, 1976, UCM-LPQ-ROD-8, left M1. I, J. Murid Paraethomys meini (Michaux, 1969). I. UCM-LPQ-ROD-9, right M2. J. UCM-LPQ-ROD-10, right m1, m2, and m3. K. Gerbillid Debruijnimys sp., UCM-LPQ-ROD-11, left m1. L. Glirid Eliomys truci Mein and Michaux, 1970, UCM-LPQ-ROD-12, left M1/2. M. Glirid Glis cf. minor, UCM-LPQ-ROD-13, left m1. N, O. Sciurid Atlantoxerus sp. N. UCM-LPQROD-14, left M1/2. O. UCM-LPQ-ROD-15, right m1/2.
Data and code for "Sustainable Human Population Density in Western Europe between 560.000 and 360.000 years ago"
<p>This dataset contains the modeling results GIS data (maps) of the study “Sustainable Human Population Density in Western Europe between 560.000 and 360.000 years ago” by Rodríguez et al. (2022).</p> <p>The NPP data (npp.zip) was computed using an empirical formula (the Miami model) from palaeo temperature and palaeo precipitation data aggregated for each timeslice from the Oscillayers dataset (Gamisch, 2019), as defined in Rodríguez et al. (2022, in review).</p> <p>The Population densities file (pop_densities.zip) contains the computed minimum and maximum population densities rasters for each of the defined MIS timeslices. With the population density value Dc in logarithmic form log(Dc).</p> <p>The Species Distribution Model (sdm.7z) includes input data (folder /data), intermediate results (folder /work) and results and figures (folder /results). All modelling steps are included as an R project in the folder /scripts. The R project is subdivided into individual scripts for data preparation (1.x), sampling procedure (2.x), and model computation (3.x).</p> <p>The habitat range estimation (habitat_ranges.zip) includes the potential spatial boundaries of the hominin habitat as binary raster files with 1=presence and 0=absence. The ranges rely on a dichotomic classification of the habitat suitability with a threshold value inferred from the 5% quantile of the presence data.</p> <p>The habitat suitability (habitat_suitability.zip) is the result of the Species Distribution Modelling and describes the environmental suitability for hominin presence based on the sites considered in this study. The values range between 0=low and 1=high suitability. The dataset includes the mean (pred_mean) and standard deviation (pred_std) of multiple model runs.</p>
Data for: Holocene history of the landscape at the biogeographical and cultural crossroads between Central and Eastern Europe (Western Podillia, Ukraine)
<p><strong>Here, we publish the working data sheets for individual proxies (pollen, plant macrofossils, mollusc and geochemical composition), which was used for paleoecological diagrams in the paper Hájková et al. in Quaternary Science Reviews. </strong></p>
Fig. 4 in Changing climate-changing pathogens: Toxoplasma gondii in North-Western Europe
Fig. 4 Expected increases in T. gondii prevalence in NorthWestern Europe towards 2069 based upon the combination of climatic conditions from Figs. 2 and 3. The dotted bright green areas indicate a small increase in T. gondii prevalence as a result of climatic change, pink areas a limited increase, and red areas a substantial increase
Fig. 2 in Changing climate-changing pathogens: Toxoplasma gondii in North-Western Europe
Fig. 2 Total precipitation in North-Western Europe as calculated by the CCSR (Center for Climate System Research, University of Tokyo) and NIES (National Institute for Environmental Studies) model under a SRES A1 scenario. Presented is the total mean precipitation in period from 1970 to 1999 (a), and the projected total mean precipitation from 2010 to 2039 (b) and 2040–2069 (c). Figures obtained from www.ipcc-data.org
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level.
Figure 1 in Rediscovery of Eunapius carteri (Bowerbank, 1863) in Western Europe
Figure 1. Images of body and gemmules of E. carteri (MNCN-1.01/212) from the sponge collection of the National Museum of Natural History of Madrid: A) Images of body shape fragments (scale = 1 cm); B) Slide of gemmules and spicules for light microscopy (scale = 1 cm); C) Detail of gemmules forming a carpet at the sponge base (scale = 50 µm); D–E) Microscopic details of gemmules (scale = 100 µm); F–G) Microscopic details of bi-layered gemmular theca (scale = 50 µm); H) Pneumatic layer with regular lines of polygonal chambers, with outlines evident at the gemmular surface (scale = 50 µm); I) Inner layer (scale = 50 µm).
Figure 2 in Rediscovery of Eunapius carteri (Bowerbank, 1863) in Western Europe
Figure 2. Microscopic details of spicules of E. carteri in slide MNCN-1.01/865 from the sponge collection of the National Museum of Natural History of Madrid. A) Gemmule surface covered by a dense matrix of gemmuloscleres; some megascleres can be observed externally (shown by arrows); B–C) Megascleres; D) Gemmulosclere matrix; E) An infrequent centrostyle gemmulosclere; F–I) Gemmuloscleres (scale = 50 µm).
Fig. 3 in Youngest agamid lizards from Western Europe (Sierra de Quibas, Spain, late Early Pleistocene)
Fig. 3. Chronological synthesis of the latest Miocene, Pliocene, and Pleistocene records of the family Agamidae in Western Europe (data mainly from Delfino et al. 2008). The grey strips represent the two periods of extinction of Western and Central European herpetofauna during the Pliocene and Pleistocene (Bailon 1991; Blain 2005, 2009; Bailon and Blain 2007; Ivanov 2007). MN, Mammal Neogene Biozonation.
Fig. 2 in Youngest agamid lizards from Western Europe (Sierra de Quibas, Spain, late Early Pleistocene)
Fig. 2. Agamidae indet. from the late early Pleistocene of Sierra de Quibas, Murcia, southeastern Spain. A. IPHES QB-06-EC-H/1, right maxilla in lateral (A 1) and medial (A 2) views. B. IPHES QB-06-EC-H/2, left dentary in lateral (B 1) and medial (B 2) views. C. IPHES QB-06-EC-H/3, right dentary in lateral (C 1) and medial (C 2) views. D. IPHES QB-06-EC-H/6, trunk vertebra in dorsal (D 1), ventral (D 2), and posterior (D 3) views. E. IPHES QB-06-EC-H/7, anterior caudal vertebra in dorsal (E ), ventral (E ), anterior (E ), posterior (E ), and left lateral (E ) views.
Fig. 1 in Youngest agamid lizards from Western Europe (Sierra de Quibas, Spain, late Early Pleistocene)
Fig. 1. Map of Western Europe (A), the location of Quibas paleontological site (B), geological map of the Quibas area (C) (modified from Montoya et al. 1999, 2001).
FIGURE 11 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 11. Body mass of caballine Equidae (Equus ferus and E. mosbachensis) in Middle and Late Pleistocene localities from Britain and Germany. For explanation of graph, see Figure 6.
FIGURE 10 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 10. Body mass of bovine Bovidae (Bison priscus and Bos primigenius) from Middle and Late Pleistocene localities of Britain and Germany. For explanation of graph, see Figure 6.
FIGURE 8 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 8. Body mass of Rhinocerotidae from Pleistocene localities of Britain and Germany. For explanation of graph, see Figure 6.
FIGURE 9 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 9. Linear regressions of body mass (kg) of Bovidae and Equus ferus/mosbachensis from localities with pollen records, and minimum, maximum and mean NAP % in the pollen records of the localities. Each point represents an individual specimen. Numbers of specimens per each locality are given in brackets after the locality names.
FIGURE 7 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 7. Body mass of Megacerini, Rangifer tarandus and Alcini in Middle and Pleistocene localities from Britain and Germany. For explanation of graph, see Figure 6.
FIGURE 3 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 3. Linear regressions of mean mesowear values of deer (Cervidae) from localities with pollen records, and minimum, maximum and mean NAP % in the pollen records of the localities. Numbers of specimens per locality are given in brackets after the locality names. For Megacerini, the samples from Grays Thurrock and Ireland are Megaloceros giganteus; those from Boxgrove, West Runton and Voigstedt combine Praemegaceros verticornis, P. dawkinsi and Megaloceros savini. For Dama the specimens from Boxgrove are D. cf. roberti; others are D. dama.
FIGURE 6 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation
FIGURE 6. Body mass of Cervus elaphus, Dama spp. and Capreolus capreolus in Middle and Late Pleistocene localities from Britain and Germany. The localities are arranged from oldest (right) to youngest (left) estimated age. The middle line in the diamonds marks the mean body mass and the upper and lower lines mark the 95% confidence limits of the mean. Diamonds that do not overlap at the 95% lines indicate statistically significant difference between populations. The central line in the figures indicates the combined mean body mass of all the populations. The individual body mass estimates of each specimen are shown as data points. Sample sizes are given in brackets for each locality.
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