Find research datasets worth reusing

Text-fig. 4. Stratigraphic correlation of the five major fossil-bearing localities in the Mikhailovka quarry near Zheleznogorsk. 1 – loesses and soils, 2 – unlaminated loams, 3 – laminated loams, 4 – clays, 5 – sands, 6 – gravels, 7 – carbonate concretions, 8 – mollusk shells, 9 – small mammal remains, 10 – insect remains, 11 – plant macroremains. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)

Text-fig. 4. Stratigraphic correlation of the five major fossil-bearing localities in the Mikhailovka quarry near Zheleznogorsk. 1 – loesses and soils, 2 – unlaminated loams, 3 – laminated loams, 4 – clays, 5 – sands, 6 – gravels, 7 – carbonate concretions, 8 – mollusk shells, 9 – small mammal remains, 10 – insect remains, 11 – plant macroremains.

Text-fig. 8. Upper molars of Arvicola ex gr. sapidus MILLER, 1908 from Mikhailovka-5. a–d: M1, e–h: M2, i–q: M3. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)

Text-fig. 8. Upper molars of Arvicola ex gr. sapidus MILLER, 1908 from Mikhailovka-5. a–d: M1, e–h: M2, i–q: M3.

Text-fig. 3. Correlation of geological sections with Pleistocene deposits of the Mikhailovka quarry near Zheleznogorsk. 1 – modern and fossil soils, 2 – loess-like loam, 3 – sandy clay, 4 – aleurites, 5 – horizontally laminated clays, 6 – brown loams, 7 – blue clays and loams, 8 – sands, 9 – gravels, 10 – mollusk shells, 11 – small mammal remains. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)

Text-fig. 3. Correlation of geological sections with Pleistocene deposits of the Mikhailovka quarry near Zheleznogorsk. 1 – modern and fossil soils, 2 – loess-like loam, 3 – sandy clay, 4 – aleurites, 5 – horizontally laminated clays, 6 – brown loams, 7 – blue clays and loams, 8 – sands, 9 – gravels, 10 – mollusk shells, 11 – small mammal remains.

Text-fig. 7. Lower molars of Arvicola ex gr. sapidus MILLER, 1908 from Mikhailovka-5. a–g: m1, h–j: m2, k–m: m3. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)

Text-fig. 7. Lower molars of Arvicola ex gr. sapidus MILLER, 1908 from Mikhailovka-5. a–g: m1, h–j: m2, k–m: m3.

Text-fig. 9. Enamel differentiation index (SDQ) of Likhvinian (1, 2) and Mikulinian (3, 4) samples of Arvicola from the Russian Plain. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)

Text-fig. 9. Enamel differentiation index (SDQ) of Likhvinian (1, 2) and Mikulinian (3, 4) samples of Arvicola from the Russian Plain.

FIG. 7 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 7. — Logarithmic ratio diagram comparing the skulls of Hipparion dietrichi (Wehrli, 1941) from localities: Strumyani-2 (STR-2); Samos (S); Nikiti-2 (NIK-2); Vathilakkos (VTK); Perivolaki (PER). Standard Hippotherium primigenium, HÖwenegg. Measurements: 1, muzzle length, prostion-middle of the line connecting the anterior borders of P2; 2, palatal length, middle of the line connecting the anterior borders of P2 to anterior border of choane; 3, vomerine length; 4, post-vomerine length; 6, basilar length: basion-prostion; 7, premolar length; 8, molar length; 9, upper cheek teeth length; 14, minimal muzzle breadth; 15, muzzle breadth at I1-I1; 30, length of the naso-incisival notch; 31, cheek length, posterior end of the narial opening-anterior border of the orbit; 32, distance orbit-preorbital fossa (POF); 33, length of PF; 35, height of POF (perpendicular to 33); 36, distance ventral border of POF-crista facialis; 37, distance infraorbital foramen-alveoles of the tooth series; 38, distance posterior end of PF-alveoli of the cheek teeth.

FIG. 13 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 13. — Fossil mammals from the Miocene of Strumyani (SW Bulgaria): A-C, F, G, Palaeoreas lindermayeri Wagner, 1848; A, skull FM-2738, front view; B, mandible FM-2744; C, mandible FM-2783; F, frontlet FM-2740; G, frontlet FM-2780; D, I, J, Prostrepsiceros rotundicornis (Weithofer, 1888); D, mandible FM-2331; I, frontlet FM-2779; J, frontlet FM-2739; E, Palaeoryx sp., tooth row p2-m2 FM-2251; H, Tragoportax sp., skull FM-2094. Scale bar: A, G-J, 20 cm; B-E, 5 cm.

FIG. 6 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 6. — Fossil mammals from the Miocene of Strumyani (SW Bulgaria): A, Hippotherium cf. brachypus (Hensel, 1862), lateral view of skull FM-2326; B, Cremohipparion mediterraneum (Roth & Wagner, 1855), lateral view of skull FM-2028; C, Hipparion dietrichi (Wehrli, 1941), lateral view of skull FM-2029. Scale bar: 20 cm.

FIG. 4 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 4. — Bivariate plots (L × W) of DP2 in tetralophodont elephantoids from Strumyani and other Late Miocene sites. Data: GM (own measurements MNHN, NHM, NHMW, NMNHAs) and sources quoted in the text. Abbreviation: T., Tetralophodon.

FIG. 9 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 9. — Logarithmic ratio diagram comparing the skulls of Cremohipparion mediterraneum (Roth & Wagner,1855) and Cremohipparion moldavicum Gromova, 1952 from localities: Strumyani-2 (STR-2); Taraklia (TAR); Novaya Emetovka-2 (NE); Novoelizavetovka (Ne); Cherevichnoe (CHER); Akkasdağı (AK). Measurements and standard as for Figure 7.

FIG. 14 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 14. — Plot of premolar vs molar length (in mm) in Palaeoreas lindermayeri Wagner, 1848 from Strumyani, Hadjidimovo and Pikermi.

FIG. 8 in Upper Miocene mammals from Strumyani, South-Western Bulgaria

FIG. 8. — Logarithmic ratio diagram comparing the skulls of Cremohipparion mediterraneum (Roth & Wagner, 1855) and "Hipparion" verae Gabunia, 1959 from localities: Strumyani-2 (STR-2); Hadjidimovo-1 (HD); Pikermi (PIK); Perivolaki (PER); Grebeniki (GREB). Measurements and standard as for Figure 7.

FIG. 3 in Louis de Bonis: 50 years of paleontological research on mammals

FIG. 3. — Excavating the locality Xirochori-1 of the Axios Valley (Macedonia, Greece) in 1989, just after the discovery of the partial skull of the hominoid primate Ouranopithecus macedoniensis; from left to right: D. Geraads, G. D. Koufos and L. de Bonis.

FIG. 1 in Louis de Bonis: 50 years of paleontological research on mammals

FIG. 1. — Louis de Bonis excavating at Pech Crabit (Quercy, France) in 1972; from left to right: L. de Bonis, M. Vianey-Liaud, J.-P. Aguilar and D. Helmer.

FIG. 4 in Louis de Bonis: 50 years of paleontological research on mammals

FIG. 4. — Louis is acclaimed Honorary Doctor in the School of Geology in the Aristotle University of Thessaloniki in 2001; from left to right: G. D. Koufos, L. de Bonis and E. Vavliakis, who gives to L. de Bonis the insignia of the School.

FIG. 2 in Louis de Bonis: 50 years of paleontological research on mammals

FIG. 2. — Louis de Bonis excavating at the locality "Ravin des Zouaves-5" of the Axios Valley (Macedonia, Greece) in 1978.

Fig. 97 in The Mammals Of Paracou, French Guiana: A Neotropical Lowland Rainforest Fauna Part 2. Nonvolant Species

Fig. 97. Results of biogeographic analyses of 12 nonvolant rainforest mammal faunas (see table 55 for geographic coordinates and other locality information). Solid and broken contours enclosing various groups were drawn following the same conventions explained in the caption to figure 96. The raw (presence/absence) data on which both clustering and PAE were based are tabulated in appendix 2.

Fig. 95 in The Mammals Of Paracou, French Guiana: A Neotropical Lowland Rainforest Fauna Part 2. Nonvolant Species

Fig. 95. Distribution of lowland rainforest on the Central and South American mainland (see Voss and Emmons, 1996, for references). Major habitat discontinuities delimit four distinct regions: (1) the Andes and the Serranía de Perijá separate transAndean rainforests to the west from Venezuelan coastal rainforests and Amazonian rainforests to the east; (2) the Llanos and the lower Orinoco separate Venezuelan coastal rainforests to the north and west from Amazonia to the south and east; (3) an arid diagonal of xeromorphic biomes (Caatinga, Cerrado, Chaco) separates Amazonia to the northwest from the Atlantic rainforests (Mata Atlantica) to the southeast. The location of our inventory site at Paracou is indicated by the arrow.

Fig. 94 in The Mammals Of Paracou, French Guiana: A Neotropical Lowland Rainforest Fauna Part 2. Nonvolant Species

Fig. 94. Percent faunal similarity (Jaccard's coefficient of faunal similarity Χ 100) plotted against airline distance for all 45 pairwise comparisons among ten nonvolant rainforest mammal inventories (tables 62, 63).

Fig. 89 in The Mammals Of Paracou, French Guiana: A Neotropical Lowland Rainforest Fauna Part 2. Nonvolant Species

Fig. 89. Analysis of faunal similarity among nonvolant mammal inventories from 12 Neotropical rainforest localities. Faunal similarity was quantified between each pair of localities (i, j) by Jaccard's coefficient, Jij = Cij/Tij, where Cij is the number of species common to both faunas and Tij is the total number of species in both faunas combined (Tij = Ni + Nj — Cij). Localities were clustered by the unweighted pairgroup method using arithmetic averages (Sneath and Sokal, 1973) for comparability with other recent biogeographic analyses of Neotropical vertebrates (e.g., da Silva and Sites, 1995). The bottom scale shows the clustering level in units of percent faunal similarity (J Χ 100). No historical or other causal interpretation is implied by these results, nor do we assume that a hierarchical model is necessarily appropriate except as a convenient summary graphic.