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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.
Text-fig. 8. Line drawings of third molars from the upper part of the Nagri Formation; 8a–b and 8e–g are referred to Karnimata fejfari, 8c and 8h are referred to Progonomys hussaini, and 8d represents Progonomys morganae. a) left m3 YGSP 34573, b) right m3 YGSP 34568, c) right m3 YGSP 34574, d) left M3 YGSP 34033 from Y 259, e) right M3 YGSP 34595, f) right M3 YGSP 34596, g) right M3 YGSP 33197 from Y 450, h) right M3 YGSP 34597. All teeth drawn to same scale, anterior is upward; black shading represents dentine exposed by wear; hatching on 8d represents breakage. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 8. Line drawings of third molars from the upper part of the Nagri Formation; 8a–b and 8e–g are referred to Karnimata fejfari, 8c and 8h are referred to Progonomys hussaini, and 8d represents Progonomys morganae. a) left m3 YGSP 34573, b) right m3 YGSP 34568, c) right m3 YGSP 34574, d) left M3 YGSP 34033 from Y 259, e) right M3 YGSP 34595, f) right M3 YGSP 34596, g) right M3 YGSP 33197 from Y 450, h) right M3 YGSP 34597. All teeth drawn to same scale, anterior is upward; black shading represents dentine exposed by wear; hatching on 8d represents breakage.
Text-fig. 7. Molars referred to Karnimata fejfari sp. nov. from type locality Y 311. Right M2, a) YGSP 34588 and b) 54187, buccal upward. Lower teeth c) YGSP 34528 and d) 36166 both left m1, and e) 36170 and f) 54176, left and right m2; c–f figured lingual side upward. All teeth same scale. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 7. Molars referred to Karnimata fejfari sp. nov. from type locality Y 311. Right M2, a) YGSP 34588 and b) 54187, buccal upward. Lower teeth c) YGSP 34528 and d) 36166 both left m1, and e) 36170 and f) 54176, left and right m2; c–f figured lingual side upward. All teeth same scale.
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1.
Text-fig. 10. List of Siwalik murine rodents. a) Stratigraphic occurrence of fossil localities of the Potwar Plateau, Pakistan. b) Murine species recovered from the Siwaliks, updated from Kimura et al. (2015). All localities but DP 13 have Y as prefix. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 10. List of Siwalik murine rodents. a) Stratigraphic occurrence of fossil localities of the Potwar Plateau, Pakistan. b) Murine species recovered from the Siwaliks, updated from Kimura et al. (2015). All localities but DP 13 have Y as prefix.
Text-fig. 1. Line drawings of idealized murine left first molars, M1 above (a) and m1 below (b). Standard Cope-Osborn terminology is used for the cusps, with equivalent t1 to t12 terminology and specialized cingulum cusp names for m1. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 1. Line drawings of idealized murine left first molars, M1 above (a) and m1 below (b). Standard Cope-Osborn terminology is used for the cusps, with equivalent t1 to t12 terminology and specialized cingulum cusp names for m1.
Text-fig. 9. First upper molars of Parapodemus badgleyae sp. nov. (a–d) and Muridae, gen. et sp. indet. (e). a) YGSP 33936, holotype, locality Y 259, b) 33939 from Y 259, c) 34542 from Y 311, d) 34543 from Y 311, e) 34559 from Y 311. All molars but c are left molars, all figured with buccal side upward and at the same scale. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 9. First upper molars of Parapodemus badgleyae sp. nov. (a–d) and Muridae, gen. et sp. indet. (e). a) YGSP 33936, holotype, locality Y 259, b) 33939 from Y 259, c) 34542 from Y 311, d) 34543 from Y 311, e) 34559 from Y 311. All molars but c are left molars, all figured with buccal side upward and at the same scale.
Text-fig. 4. First upper molars of Karnimata fejfari sp. nov. from type locality Y 311, all figured with buccal side upward. a) YGSP 34551, b) 34544, c) 34546 holotype, d) 34548, e) 34540, f) 34547, g) 34554, h) 36162, i) 54126, j) 54127, k) 54147, l) 54153. All at same 1 mm scale, all left M1 except for right h and l. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 4. First upper molars of Karnimata fejfari sp. nov. from type locality Y 311, all figured with buccal side upward. a) YGSP 34551, b) 34544, c) 34546 holotype, d) 34548, e) 34540, f) 34547, g) 34554, h) 36162, i) 54126, j) 54127, k) 54147, l) 54153. All at same 1 mm scale, all left M1 except for right h and l.
Text-fig. 5. First upper molars of Karnimata fejfari sp. nov. from localities Y 450 (a–d) and Y 259 (e–l). a) YGSP 33181, b) 33182, c) 33185, d) 33186, e) 33945, f) 33940, g) 33948, h) 33958, i) 33960, j) 33946, k) 33967, l) 33973. Figured at same scale, buccal upward, all right M1 except for left f, g, j, l. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 5. First upper molars of Karnimata fejfari sp. nov. from localities Y 450 (a–d) and Y 259 (e–l). a) YGSP 33181, b) 33182, c) 33185, d) 33186, e) 33945, f) 33940, g) 33948, h) 33958, i) 33960, j) 33946, k) 33967, l) 33973. Figured at same scale, buccal upward, all right M1 except for left f, g, j, l.
Text-fig. 6. Scatter diagram of length and width of M1 specimens in Progonomys hussaini and Karnimata fejfari from localities Y 259, 450, 311. The solid line ellipse is a 55% concentration ellipse for P. hussaini, and the dashed ellipse is a 55% concentration ellipse for Karnimata fejfari, all specimens combined. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 6. Scatter diagram of length and width of M1 specimens in Progonomys hussaini and Karnimata fejfari from localities Y 259, 450, 311. The solid line ellipse is a 55% concentration ellipse for P. hussaini, and the dashed ellipse is a 55% concentration ellipse for Karnimata fejfari, all specimens combined.
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.
Characterizing the automatic radon flux Transfer Standard system Autoflux: laboratory calibration and field experiments
<p>Data from the manuscript: Characterizing the automatic radon flux Transfer Standard system Autoflux: laboratory calibration and field experiments.</p> <p>The present folder contains:</p> <ol> <li>Exhalation Bed data (data and plots from the characterization of the exhalation bed of the Cantabria University)</li> <li>ANSTO Autoflux (data and plots of the calibration of the Autoflux radon flux system)</li> <li>INTE_UPC (data and plots of the calibration of the INTE_UPC radon flux system)</li> </ol>
Portable two-filter dual-flow-loop 222Rn detector: stand-alone monitor and calibration transfer device
<p>Little overlap exists in the required capabilities of <sup>222</sup>Rn (radon) monitors for public health and atmospheric research. The former requires robust, compact, easily transportable instruments to characterise daily to yearly variability >100 Bq m<sup>−3</sup>, whereas the latter requires static instruments capable of characterising sub-hourly variability between 0.1 and 100 Bq m<sup>−3</sup>. Consequently, detector development has evolved independently for the two research communities, and while many radon measurements are being made world-wide, the full potential of this measurement network can't be realised because not all results are comparable. Development of a monitor that satisfies the primary needs of both measurement communities, including a calibration traceable to the International System of Units (SI), would constitute an important step toward (i) increasing the availability of radon measurements to both research communities, and (ii) providing a means to harmonize and compare radon measurements across the existing eclectic global network of radon detectors. To this end, we describe a prototype detector built by the Australian Nuclear Science and Technology Organisation (ANSTO), in collaboration with the EMPIR 19ENV01 <em>traceRadon</em> Project and Physikalisch-Technische Bundesanstalt (PTB). This two-filter dual-flow-loop radon monitor can be transported in a standard vehicle, fits in a 19<sup>′′</sup> instrument rack, has a 30 min temporal resolution, and a detection limit of ∼0.14 Bq m<sup>−3</sup>. It is capable of continuous, long-term, low-maintenance, low-power, indoor or outdoor monitoring with a high sensitivity and an uncertainty of ∼15 % at 1 Bq m<sup>−3</sup>. Furthermore, we demonstrate the successful transfer of an SI traceable calibration from this portable monitor to a 1500 L two-filter radon monitor under field conditions.</p>
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