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212 results for “Fossil localities”
FIGURE 2 in Novel analysis of locality data can inform better inventory and monitoring practices for paleontological resources at John Day Fossil Beds National Monument Oregon, USA
FIGURE 2. Map of Oregon showing the three park units (purple) and the extent of the majority of non-NPS sites worked by JODA paleontologists (green). There are museum collections at JODA from many sites in area highlighted in green. However, many of these sites have not been visited recently. Many of the sites with paleontological resources in the green area are found on lands administered or owned by partners and are scattered across the full area.
FIGURE 3 in Novel analysis of locality data can inform better inventory and monitoring practices for paleontological resources at John Day Fossil Beds National Monument Oregon, USA
FIGURE 3. Map of locality data for cataloged specimens by year collected in one of the five main collection areas. Years correspond to cyclic prospecting schedule outlined in Table 1. Note the overlap between 1993 and 1994 and 1997 and 1998 contrary to the schedule shown in Table 1. Precise locality information is available to qualified researchers upon request from JODA's museum program.
FIGURE 1 in Novel analysis of locality data can inform better inventory and monitoring practices for paleontological resources at John Day Fossil Beds National Monument Oregon, USA
FIGURE 1. Composite stratigraphic column of the John Day Formation with the Columbia River Basalt Group capping the section. Stratigraphic relationships and radiometric dates are based on Hunt and Stepleton (2004), Albright et al. (2008), and Fremd (2010). The black box encompasses the subunits that are considered lower Turtle Cove for the purposes of this study. Figure provided by the National Park Service.
Text-fig. 1. Neogene fossil suid localities of Europe. Mahmutgazi is in southwest Anatolia, Turkey. in Hippopotamodon erymanthius (Suidae, Mammalia) from Mahmutgazi, Denizli-Çal basin, Turkey
Text-fig. 1. Neogene fossil suid localities of Europe. Mahmutgazi is in southwest Anatolia, Turkey.
Figures 1-6 from: Fikácek M, Hajek J, Schmied H (2011) On the identity of the fossil hydrophilid beetles from the Tertiary localities in the southern part of the Upper Rhine Graben (Coleoptera: Hydrophilidae, Dytiscidae). ZooKeys 78: 15-25. https://doi.org/10.3897/zookeys.78.800
Figures 1-6 - Copelatus convexus (Förster, 1891). 1–4 neotype (1, 3 NHMB R91; 2, 4 NHMB R74) 5 original illustrations of the holotype by Förster (1891) 6 drawing of the specimen NHMB R91 by Théobald (1937).
Figures 7-12 from: Fikácek M, Hajek J, Schmied H (2011) On the identity of the fossil hydrophilid beetles from the Tertiary localities in the southern part of the Upper Rhine Graben (Coleoptera: Hydrophilidae, Dytiscidae). ZooKeys 78: 15-25. https://doi.org/10.3897/zookeys.78.800
Figures 7-12 - 7 Escheria crassipunctata Förster, 1891, original illustration of the holotype 8 Escheria dimidiata Förster, 1891, original illustration of the holotype 9 Escheria punctulata Förster, 1891, original illustration of the holotype 10–12 specimen NHMB R707 (10 photograph 11 drawing 12 original drawing by Théobald (1937)).
Figure 1 from: (2011) Sub-fossil beetle assemblages associated with the "mammoth fauna" in the Late Pleistocene localities of the Ural Mountains and West Siberia. ZooKeys 100: 149-169. https://doi.org/10.3897/zookeys.100.1524
Figure 1 - Geographical location of the study sites in the Ural Mountains and Western Siberia. Numbers of sites: 1 Syoyakha-Mutnaya 2 430 km from Ob 3 Aganskiy uval-1290/2 4 Mega 5 Lokosovo 6 Kul'egan-2247 Point I 7 Kul'egan -2247 Point II 8 Skorodum 9 Andriyshino 10 Nizhnyaya Tavda 11 Mal'kovo 12 Nikitino 13 Shurala. Bold line - Borders of vegetation types, reconstructed for the beginning of MIS 2 on the basis of palynological data: I periglacial tundra II periglacial steppe and forest-steppe III boreal forest and parklands (after Grichuk and Borisova 2009)
Fig. 1. Stratigraphy and locality map. A in Hyoliths and small shelly fossils from the Lower Cambrian of North-East Greenland
Fig. 1. Stratigraphy and locality map. A. Map of Greenland with area of study marked. B. Generalised map of study area with outcrops of Lower Palaeozoic rocks in black. The position of hyolith localities indicated. C. Generalised stratigraphy of the Bastion Formation of Hudson Land with position of samples yielding hyoliths in acid resistant residues. Modified from Skovsted and Holmer (in press).
Cladistic matrix targeted at resolving relationships between fossil birds from the Changma locality of the Lower Cretaceous Xiagou Formation
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Text-fig. 1—Index map of Tornillo outcrop pattern and fossil locality (F). in Tyrannosaurus and Torosaurus, Maestrichtian Dinosaurs From Trans-Pecos, Texas
Text-fig. 1—Index map of Tornillo outcrop pattern and fossil locality (F).
FIGURE 1. Fossil locality information. A in A new clam shrimp (Branchiopoda: Diplostraca: Spinicaudata) from the Upper Jurassic in the Jiyuan Basin, China and its biostratigraphic significance
FIGURE 1. Fossil locality information. A, Map of the fossil locality and column of the Upper Jurassic Maao Formation. B, Horizon (red arrow) from which the clam shrimps were collected in the present study. Lithology: 1. conglomerate; 2. sandstone; 3. siltstone; 4. muddy siltstone; 5. mudstone; 6. shale; 7. clam shrimp.
FIGURE 1 in A new species of the fossil genus Electrotrichia (Insecta: Trichoptera: Hydroptilidae) from Rovno amber (Zhytomyr region, Olevsk locality)
FIGURE 1. General view of male paratype. A, Male type, dorsal view. B, Ventral view and male type genital structures on ventrolateral view. C, Electrotrichia rasnitsyni sp. nov. Scale bars = 0.5 mm in A; 0.25 mm in B; 0.1 mm in C.
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International Brain Laboratory public data
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