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Fig. 9 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 9. Measured section of the Carpenter Ranch Formation at Deahl Butte at the locality yielding the partial cranial dome (UNSM 44801) and mandible (UNSM 44800) of the chalicothere Tylocephalonyx (table 3). The dome, mandible, and diaphysis of a femur (UNSM 44802) were found in proximity within a crystalline gravel lens. Here Arikaree gray sands intervene between the incised Carpenter Ranch paleovalley and Brule Formation. Lithic symbols apply to figures 7–9.
Fig. 5 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 5. Redrafted version of N.H. Darton's crosssection (1899: fig. 213) from Spoon Butte to Sturdivant's Ranch, showing the silicacemented sandstone caprocks descending in elevation to the south. Darton regarded all the caprocks as ''Arikaree'' conglomerates, ''consisting in large part of crystalline rocks and apparently lying on a steeply sloping surface''. The letters AE were not explained in his caption. Note correspondence to figure 3.
Fig. 4 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 4. Principal fossil mammal localities (indicated by arrows) in the capping sandstones of the Patrick Buttes. Cow Trail Notch at East Sturdivant Butte and sites at Merycochoerus Butte have yielded most of the agediagnostic specimens in the early Hemingfordian Carpenter Ranch Formation. Deahl Butte produced the partial dome and mandible of the chalicothere (UNSM 44800, 44801). Barstovian sites in the Spoon Butte Beds include South Rim, GF Butte, North Point and Box Canyon. The Oberg Quarries are gravel pits containing waterworn mid and late Miocene mammals and Pleistocene Equus.
Fig. 1 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 1. Geographic map of the Patrick Buttes, WyomingNebraska. The areal extent of each butte is indicated by solid and/or dashed lines marking the limits of the butte caprocks, formed by silicacemented sandstone. Names for individual buttes are derived from historical usage, local practice, and UNSM field terms.
Fig. 11 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 11. Partial right mandible of the chalicothere Tylocephalonyx (UNSM 44800) with m3 and partial m2, lingual view, Carpenter Ranch Formation, from the south escarpment of Deahl Butte, Goshen County, Wyoming. Note distinct m3 metastylid.
Fig. 18 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 18. Chalicothere left distal humerus (UNSM 44826) scavenged by a large entelodont, showing bite marks on both (A) anterior and (B) posterior surfaces of the bone, Lay Ranch beds (a paleovalley fill within the Anderson Ranch Formation, latest Arikareean), east side of Spoon Butte, 500 ft west of the WyomingNebraska state boundary, Goshen County, Wyoming. Arrows mark the principal percussion fractures.
Fig. 14 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 14. Distal chalicothere femur (UNSM 44806) in posterior view, referred to Tylocephalonyx, Carpenter Ranch Formation, Childers Butte, Goshen County, Wyoming. A circular percussion fracture (at the arrow) produced by the premolar of a large entelodont suggests postmortem scavenging of the chalicothere carcass. No other mammal identified in early Hemingfordian faunas can have made these circular bite marks.
Fig. 13 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 13. Cranial dome of the chalicothere Tylocephalonyx (UNSM 44801), internal surface of the dome showing the welldeveloped compartmentalized architecture, Carpenter Ranch Formation, Deahl Butte, Goshen County, Wyoming (presumed anterior face to right, dorsal upward).
Fig. 17 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 17. Detail of the internal compartmentalized architecture of the cranial dome of Tylocephalonyx (UNSM 44801), Deahl Butte, Carpenter Ranch Formation, Goshen County, Wyoming. A, Enlarged view of the sinus compartments showing the smooth unbroken edges of septa in the central part of the dome; B, Stereopair of the dome interior shown in A. Finest divisions of scale in B in mm.
Fig. 21 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 21. Right maxilla of the moschid Pseudoblastomeryx (UNSM 44821) with M1–3, Cow Trail Notch local fauna, Carpenter Ranch Formation, East Sturdivant Butte, Sioux County, Nebraska. Stereopair. Scale bar, 1 cm.
Fig. 22 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 22. Left mandible of the amphicyonid Daphoenodon (UNSM 44815) with m1–3, partial p4, Merycochoerus Butte, Carpenter Ranch Formation, Goshen County, Wyoming. Scale bar, 1 cm.
Fig. 8 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 8. Measured reference section of the Carpenter Ranch Formation at Merycochoerus Butte, Goshen County, Wyoming. The large oreodont Merycochoerus magnus was found at both low and high stratigraphic levels in Carpenter Ranch sediments filling a deeply incised early Hemingfordian paleovalley cut into the Brule Formation. Lithic symbols as in fig. 9.
Fig. 20 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 20. Right mandible of a juvenile dromomerycid Aletomeryx gracilis (UNSM 44820) with dp4 and m1, Cow Trail Notch local fauna, Carpenter Ranch Formation, East Sturdivant Butte, Sioux County, Nebraska. Stereopair. Scale bar, 1 cm.
Fig. 24 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 24. Interpretive restoration of sinuous westtoeast trend of the Carpenter Ranch paleochannel axis incised into rocks of the White River Group, Goshen County, Wyoming, and Sioux County, Nebraska. Inset illustrates a typical northwesttosoutheast crosssection of the paleochannel from Duncan Buttes to Merycochoerus Butte.
Fig. 26 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 26. Trend of early Miocene paleovalleys of early Hemingfordian age east of the Rocky Mountain Front Range and Laramie Mountains in Colorado, Wyoming, and Nebraska. Oldest mammal faunas in the valley fills document the initiation of regional uplift at;18.2–18.8 Ma. 1, Carpenter Ranch Runningwater paleovalley; 2, Martin Canyon paleovalley; 3, Troublesome Formation basinfill, Middle Park, Colorado.
Fig. 25 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism
Fig. 25. Alignment of the Carpenter Ranch and Runningwater paleovalley systems in southeastern Wyoming and western Nebraska. Fossil mammals in these early Miocene fluvial sediments indicate an early Hemingfordian age.
Text-fig. 1. Locality map and Keshin Formation section at Cape Tsvetkov, East Taimyr (after Kazakov et al. 2002). 1 – tuff conglomerate, 2 – sandstone, 3 – grained siltstone, 4 – siltstone, 5 – mudstone, 6 – foraminifers, 7 – conchostracans, 8 – plant megafossils, 9 – locality of described plants, 10 – Tsvetkov Cape (East Taimyr). in Taimyria Gen. Nov., A New Genus Of Evolutionary Advanced Gymnosperms From Triassic Of The Taimyr Peninsula, Siberia, Russia
Text-fig. 1. Locality map and Keshin Formation section at Cape Tsvetkov, East Taimyr (after Kazakov et al. 2002). 1 – tuff conglomerate, 2 – sandstone, 3 – grained siltstone, 4 – siltstone, 5 – mudstone, 6 – foraminifers, 7 – conchostracans, 8 – plant megafossils, 9 – locality of described plants, 10 – Tsvetkov Cape (East Taimyr).
Рис. 26. Сравнение среΑних значений частоты изменчивости эΛементов рисунка и инΑекса пигментации Mesobuthus eupeus в посеΛениях из разнотипных (А) и оΑнотипных (В) биотопов в кажΑой из выборок: I – Северо-ЗапаΑный Гобустан; II – Северо-Восточный Гобустан; III – ЦентраΛьный Гобустан; IV – Юго-Восточный Гобустан; V – Юго-Восточный Ширван. ИнΑекс корреΛяции r в преΑеΛах 0.744–0.989; p <0.05. Fig. 26. Comparison of the average values of the frequency of variability of pattern elements and the pigmentation index of Mesobuthus eupeus in conglomerations from habitats of different types (A) and of the same type (B) in each sample: I – northwestern Gobustan; II – northeastern Gobustan; III – central Gobustan; IV – southeastern Gobustan; V – southeastern Shirvan. Correlation index r = 0.744–0.989; p <0.05. in Materials on the colour pattern variability of Mesobuthus eupeus (C.L. Koch, 1839) (Arachnida: Scorpiones) in southeastern Shirvan and Gobustan (Eastern Azerbaijan)
Рис. 26. Сравнение среΑних значений частоты изменчивости эΛементов рисунка и инΑекса пигментации Mesobuthus eupeus в посеΛениях из разнотипных (А) и оΑнотипных (В) биотопов в кажΑой из выборок: I – Северо-ЗапаΑный Гобустан; II – Северо-Восточный Гобустан; III – ЦентраΛьный Гобустан; IV – Юго-Восточный Гобустан; V – Юго-Восточный Ширван. ИнΑекс корреΛяции r в преΑеΛах 0.744–0.989; p <0.05. Fig. 26. Comparison of the average values of the frequency of variability of pattern elements and the pigmentation index of Mesobuthus eupeus in conglomerations from habitats of different types (A) and of the same type (B) in each sample: I – northwestern Gobustan; II – northeastern Gobustan; III – central Gobustan; IV – southeastern Gobustan; V – southeastern Shirvan. Correlation index r = 0.744–0.989; p <0.05.
Рис. 21–25. Частота изменчивости основных эΛементов рисунка (меΑиаΛьной, парамеΑиаΛьных и маргинаΛьных поΛос) ΑорсаΛьной поверхности мезосомы Mesobuthus eupeus в посеΛениях кажΑой из выборок. 21 – Северо-ЗапаΑный Гобустан (n = 57); 22 – Северо-Восточный Гобустан (n = 40); 23 – ЦентраΛьный Гобустан (n = 81); 24 – Юго-Восточный Гобустан (n = 103); 25 – Юго-Восточный Ширван (n = 86). По оси абсцисс указаны посеΛения, по оси орΑинат – частота изменчивости. Figs 21–25. Frequency of variability of the main elements of pattern (medial, paramedical and marginal stripes) of dorsal surface of mesosome of Mesobuthus eupeus in conglomerations of each sample. 21 – northwestern Gobustan (n = 57); 22 – northeastern Gobustan (n = 40); 23 – central Gobustan (n = 81); 24 – southeastern Gobustan (n = 103); 25 – southeastern Shirvan (n = 86). Abscissas show conglomerations, ordinates – the frequency of variability. in Materials on the colour pattern variability of Mesobuthus eupeus (C.L. Koch, 1839) (Arachnida: Scorpiones) in southeastern Shirvan and Gobustan (Eastern Azerbaijan)
Рис. 21–25. Частота изменчивости основных эΛементов рисунка (меΑиаΛьной, парамеΑиаΛьных и маргинаΛьных поΛос) ΑорсаΛьной поверхности мезосомы Mesobuthus eupeus в посеΛениях кажΑой из выборок. 21 – Северо-ЗапаΑный Гобустан (n = 57); 22 – Северо-Восточный Гобустан (n = 40); 23 – ЦентраΛьный Гобустан (n = 81); 24 – Юго-Восточный Гобустан (n = 103); 25 – Юго-Восточный Ширван (n = 86). По оси абсцисс указаны посеΛения, по оси орΑинат – частота изменчивости. Figs 21–25. Frequency of variability of the main elements of pattern (medial, paramedical and marginal stripes) of dorsal surface of mesosome of Mesobuthus eupeus in conglomerations of each sample. 21 – northwestern Gobustan (n = 57); 22 – northeastern Gobustan (n = 40); 23 – central Gobustan (n = 81); 24 – southeastern Gobustan (n = 103); 25 – southeastern Shirvan (n = 86). Abscissas show conglomerations, ordinates – the frequency of variability.
low Cerro Gordo; StL 2, Cerro Gordo sandstone; StL 3, between Cerro Gordo and Chunchullo; StL 4, Chunchullo sandstone; StL 5, bed set between Chunchullo and Tatacoa; StL 6, Tatacoa sandstone; StL 7, bed set below Cerbatana conglomerate; StL 8, Cerbatana conglomerate; StL 9, Monkey beds; StL 10, bed set above Monkey beds; StL 12, bed set above Fish bed; StL 14, bed set below La Venta red beds; StL 15, La Venta red beds; StL 16, bed set between La Venta red beds and El Cardón red beds; StL 17, El Cardón red beds; StL 18, San Francisco sandstone; StL 19, Polonia red beds; D, reconstruction of the head of Neodolodus colombianus based on the 3D model of the almost complete skull of the specimen VPPLT 1696. Abbreviations: Fm, Formation; St m, Stratigraphic meter. Reconstruction of N. colombianus made by Tatsuya Shimura. in New remains of Neotropical bunodont litopterns and the systematics of Megadolodinae (Mammalia: Litopterna)
low Cerro Gordo; StL 2, Cerro Gordo sandstone; StL 3, between Cerro Gordo and Chunchullo; StL 4, Chunchullo sandstone; StL 5, bed set between Chunchullo and Tatacoa; StL 6, Tatacoa sandstone; StL 7, bed set below Cerbatana conglomerate; StL 8, Cerbatana conglomerate; StL 9, Monkey beds; StL 10, bed set above Monkey beds; StL 12, bed set above Fish bed; StL 14, bed set below La Venta red beds; StL 15, La Venta red beds; StL 16, bed set between La Venta red beds and El Cardón red beds; StL 17, El Cardón red beds; StL 18, San Francisco sandstone; StL 19, Polonia red beds; D, reconstruction of the head of Neodolodus colombianus based on the 3D model of the almost complete skull of the specimen VPPLT 1696. Abbreviations: Fm, Formation; St m, Stratigraphic meter. Reconstruction of N. colombianus made by Tatsuya Shimura.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
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.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
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