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339 results for “Utah”
Figure 13 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 13. Right vomer of Gryposaurus monumentensis gen. et sp. nov. in lateral view: A, RAM 6797; B, UMNH VP 13970. The broken line marks the estimated position of the dorsal margin of the anteroventral excavation. ave, anteroventral excavation; mxa, maxillary articulation; pma, premaxillary articulation; pvl, posteroventral lobe. Scale bar, 5 cm.
Figure 14 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 14. Predentary of RAM 6797 in left anterolateral view. D, dentary; nf, nutrient foramen; pdd, predentary denticles; pdlp, predentary lateral process; pdvp, predentary ventral process. Scale bar, 5 cm.
Figure 12 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 12. Gryposaurus monumentensis gen. et sp. nov. (RAM 6797) right quadrate: A, lateral view; B, medial view. mc, mandibular condyle; ptw, pterygoid wing; qb, quadrate buttress; qh, quadrate head; qjn, quadratojugal notch; qs, quadrate shaft. Scale bar, 5 cm.
Figure 6 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 6. Dorsal view of frontal–nasal suture in Gryposaurus incurvimanus (ROM 764). F, frontal; Na, nasal; nfs, nasofrontal suture; Pa, parietal; Pf, prefrontal; Po, postorbital. Scale bar, 5 cm.
Figure 3 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 3. Lateral view of Gryposaurus monumentensis gen. et sp. nov. left premaxilla, RAM 6797. en, external nares; MX, maxilla; or, oral margin rugosities; pmd, dorsal process; pmf, premaxillary foramen; pml, lateral process; pmlf, premaxilla lateral process flare; pmlp, premaxillary lip; pms, premaxillary shelf. Scale bar, 5 cm.
Figure 7 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 7. Maxillae from Gryposaurus monumentensis gen. et sp. nov., specimens RAM 6797 and UMNH VP 13970: A, left maxilla in lateral view with surrounding elements from RAM 6797; B, posterior region of right maxilla from UMNH VP 13970; C, right maxilla from RAM 6797 in lateral view; D, anterior region of left maxilla from UMNH VP 13970. D, dentary; ecr, ectopterygoid ridge; ecs, ectopterygoid shelf; J, jugal; jp, jugal process; La, lacrimal; madp, anterodorsal process; mavp, anteroventral process; mdp, maxilla dorsal process; mf, maxillary foramen; Mx, maxilla; nf, nutrient foramen; palp, palatine process; Pm, premaxilla; ptp, pterygoid process. Scale bar, 5 cm.
Figure 5 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 5. Line drawings of the four Gryposaurus species in lateral view, showing synapomorphies of the genus and other comparative features: A, G. monumentensis gen. et sp. nov. (RAM 6797); B, G. notabilis (ROM 873); C, G. incurvimanus (TMP 80.22.1); D, G. latidens (after Horner, 1992; no scale included). itf, infratemporal fenestra; mf, mandibular foramen; na, nasal arch; pmlf, lateral process flare. Scale bar, 10 cm.
Figure 4 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 4. Lateral view of Gryposaurus monumentensis gen. et sp. nov. left nasal, UMNH VP 13970. en, external naris; na, nasal arch; nap, nasal anterior process; nfs, nasofrontal suture. Scale bar, 5 cm.
Figure 10 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 10. Left squamosal from Gryposaurus sp. UMNH VP 16669 in lateral view. poc, postcotyloid process; pog, postorbital groove; prc, precotyloid process; prf, precotyloid fossa; qc, quadrate cotylus. Scale bar, 5 cm.
Figure 9 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 9. Posterior view of left lacrimal–jugal contact in Gryposaurus monumentensis gen. et sp. nov. (RAM 6797). The left side of the figure is lateral and the right side is medial. Note the interlocking relationship between these elements. J, jugal; La, lacrimal; lf, lacrimal foramen.
Figure 8 in A new species of Gryposaurus (Dinosauria: Hadrosauridae) from the late Campanian Kaiparowits Formation, southern Utah, USA
Figure 8. Lateral view of juvenile right jugal from UMNH VP 13970. jap, jugal anterior process; jpp, jugal posterior process; pop, postorbital process; pvf, posteroventral flange. Scale bar, 5 cm.
Radiometric dating of sediment cores from three alpine lakes in Utah, United States, with stable isotope data
<p>We collected sediment cores from three alpine lakes in Utah, United States, to isolate dormant <em>Daphnia </em>eggs for a resurrection ecology experiment. Our question was whether radioactive fallout from above-ground nuclear weapons testing at the Nevada Test Site in the 1950s and 1960s caused increased mutation rates and population evolution in <em>Daphnia</em>. That work is ongoing. Here, we publish radioisotope dating profiles from our sediment cores.</p>
GPR data collected near the Chepeta Weather Station and the DUST-1 sampler, Uinta Mountains, Utah
Ground penetrating radar data collected on September 9, 2021 in the Uinta Mountains at the Chepeta Remote Automated Weather Station (RAWS) and the DUST-1 passive dust sampler. Data were collected with a GSSI SIR-4000 control unit and a 350HS antenna connected to an Emlid Reach RS2 GPS receiver. Data files have been distance normalized and field-applied range gains have been removed before being exported in .sgy format. Files were also exported in .kml format for viewing the transect locations in Google Earth. Two long transects (780 feet each) were collected. The "West" transect passed to the west of the Chepta RAWS; the "East" transect passed to the east. The transects started at different points along the northern lip of the summit upland and came together at a common point at their southern ends. Marks were made in the data file every 60 feet while surveying; these marks were used to distance normalize the results. The system collected 334 scans/second with 512 samples/scan while surveying. Two 30-foot perpendicular transects were also surveyed (north to south, and west to east) with their intersection adjacent to a soil pit excavated to a depth of 92 cm. The location of the soil pit was noted in each transect with a mark near 16 feet. Data were used to evaluate spatial variations in the thickness of regolith overlying the bedrock beneath this gently sloping summit flat.
Radiometric dating of sediment cores from three alpine lakes in Utah, United States, with stable isotope data
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Evaluation of IDEAL-CT test in Utah for Balanced Mix Design
<p>The data contained herein are the results of asphalt mixtures tested at 25 C using the indirect tensile configuration based on the IDEAL tests developed by Zhou et al. (Zhou, F., Newcomb, D., Gurganus, C., Banihashemrad, S., Park, E., Sakheeifar, M., and Lytton, R.: Experimental Design for Field Validation of Laboratory Tests to Assess Cracking Resistance of Asphalt Mixtures. Final Project Report, NCHRP project 9-57. April 2016)</p> <p>The work was performed in the State of Utah as part of a research contract between the Department of Transportation and the University of Utah. PEPG, LLC., a consulting lab was also involved. The complete report can be found at the Utah Department of Transportation website (<a href="http://www.udot.utah.edu">www.udot.utah.edu</a>), Research and Innovation Division.</p>
Insect herbivory for Catula gettyi, a late Cretaceous laurel from Utah, USA
<p class="Body">The Upper Cretaceous (Campanian Stage) Kaiparowits Formation of southern Utah, USA, preserves abundant plant, invertebrate, and vertebrate fossil taxa. Taken together, these fossils indicate that the ecosystems preserved in the Kaiparowits Formation were characterized by high biodiversity. Hundreds of vertebrate and invertebrate species and over 80 plant morphotypes are recognized from the formation, but insects and their associations with plants are largely undocumented. Here, we describe a new fossil leaf taxon, <i>Catula gettyi </i>gen et. sp. nov. in the family Lauraceae from the Kaiparowits Formation. <i>Catula gettyi</i> occurs at numerous localities in this deposit that represent ponded and distal floodplain environments. The type locality for <i>C. gettyi</i> has yielded 1,564 fossil leaf specimens of this species, which provides the opportunity to circumscribe this new plant species. By erecting this new genus and species, we are able to describe ecological associations on <i>C. gettyi </i>and place these interactions within a taxonomic context<i>. </i>We describe an extensive archive of feeding damage on <i>C</i>.<i> gettyi</i> caused by herbivorous insects, including more than 800 occurrences of insect damage belonging to five functional feeding groups indicating that insect-mediated damage on this taxon is both rich and abundant. <i>Catula gettyi</i> is one of the best-sampled host plant taxa from the Mesozoic Era, a poorly sampled time interval, and its insect damage is comparable to other Lauraceae taxa from the younger Late Cretaceous Hell Creek Flora of North Dakota, USA.</p>
American Beaver: GPS and VHF tag data from resident and translocated beavers on the Price and San Rafael Rivers, Utah
<p>Wildlife translocations can dramatically alter animal movement behavior. Thus, identifying common movement patterns post-translocation can aid in setting expectations and anticipating animal behavior in subsequent efforts. American and Eurasian beavers (Castor canadensis; C. fiber) are frequently translocated for reintroduction efforts, to mitigate human-wildlife conflict, and for use as an ecosystem restoration tool. However, little is known about movement behavior of translocated beavers post-release, especially in desert rivers where resources are patchy and dynamic. We identified space-use patterns to develop an expectation framework of beaver movement behavior for future beaver-assisted restoration efforts. We captured, tagged, translocated, and monitored 41 nuisance American beavers in desert river restoration sites on the Price and San Rafael Rivers, Utah, USA, and compared their space use to 16 resident beavers. We tracked beavers 2-7 times per week from May through October in 2019 and 2020 via GPS locations and radio-telemetry, and from May 2019 through March 2021 via passive integrated antennae installed in the rivers. Resident adult beavers were detected at a mean maximum distance of 0.86 ± 0.21 river kilometers (km; ±1 SE), while resident subadult (11.00 ± 4.24 km), translocated adult (19.69 ± 3.76 km), and translocated subadult (21.09 ± 5.54 km) beavers were detected at substantially greater maximum distances. Based on coarse-scale movement models, translocated and resident subadult beavers moved substantially farther from release sites and faster than resident adult beavers up to six months post-release. In contrast, based on fine-scale, short-term movement models over 5-minute intervals, we observed similar median distance traveled between resident adult and translocated beavers. Our findings suggest day-to-day activities such as foraging and resting were largely unaltered by translocation, but translocated beavers exhibited coarse-scale movement behavior most similar to dispersal by resident subadults. Coarse-scale movement rates decreased with time since release, suggesting that translocated beavers adjusted to the novel environment over time and eventually settled into a home range similar to resident adult beavers. This is the first study comparing resident and translocated beaver movement behavior in the same system. Understanding translocated beaver movement behavior in response to a novel desert system can help future beaver-assisted restoration efforts to identify appropriate release sites and strategies.</p>
FIGURE 14 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 14. Detailed comparison of model versions.
FIGURE 13 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 13. Refined model results.
FIGURE 9 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 9. Revised weighted suitability analysis results.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
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