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FIG. 7 in The role of birds as grave gifts in richly furnished Roman Iron Age inhumation graves c. 1-375 AD, eastern Denmark

FIG. 7. — Tarsometatarsal SC plotted against GL of domestic chicken of Danish Roman Age finds compared with measurements of red jungle fowl (Gallus gallus). Measurements of the Smedegård specimen and red jungle fowl from Raahauge (2002). SMG: Smedegård; MUG; Munkehøjgård; VRÅ:Vråby; KAER:Kaerup Nord. Measurements are according to von den Driesch (1976).

FIG. 2 in The role of birds as grave gifts in richly furnished Roman Iron Age inhumation graves c. 1-375 AD, eastern Denmark

FIG. 2. — Calvarium, trunk and wing elements of a robust goose from a princely grave at Varpelev Vest. Photograph: Marcus Krag. Scale bar: 50 mm.

FIG. 6 in The role of birds as grave gifts in richly furnished Roman Iron Age inhumation graves c. 1-375 AD, eastern Denmark

FIG. 6. – The entire cock skeleton of Kaerup Nord, Grave A3663 a richly furnished woman's grave. The cock was retrieved from a pottery vessel at the foot end of the grave.A fragmented furculum, sternum and a total of 11 phalanges are not shown. Scale bar 10 cm. Photograph: Geert Brovad.

FIG. 4. — A in The role of birds as grave gifts in richly furnished Roman Iron Age inhumation graves c. 1-375 AD, eastern Denmark

FIG. 4. — A, Coracoid with cut marks cranially mid-shaft; B, Furcula with cut marks peripherally below pneumatic foramina; C, Humerus with numerous faint long cut marks proximally, indicated by arrows. Photograph: Marcus Krag. Scale bars: 10 mm.

Figure 2 in Population dynamics, age structure and sex ratio of the bromeliad-dwelling jumping spider, Psecas chapoda (Salticidae)

Figure 2. Mean number (¡SE) of Psecas chapoda per Bromelia balansae with no inflorescence, from May 1998 to April 2000 (N53516 spiders).

Figure 1 in Population dynamics, age structure and sex ratio of the bromeliad-dwelling jumping spider, Psecas chapoda (Salticidae)

Figure 1. Fluctuations in the number of Psecas chapoda and egg sacs (log) on bromeliads with and without inflorescence, and the frequency (%) of bromeliads in bloom (with inflorescence or infrutescence) between May 1998 and April 2000 (N53516 spiders and 314 egg sacs).

Figure 5 in Population dynamics, age structure and sex ratio of the bromeliad-dwelling jumping spider, Psecas chapoda (Salticidae)

Figure 5. Mean number (¡SE) of spiders Psecas chapoda on bromeliads that produced inflorescence between August and December and on bromeliads that did not produce inflorescence until December, in 1998 (A) and 1999 (B). The frequency (%) of bromeliads that bloomed up to December is also shown.

Figure 4 in Population dynamics, age structure and sex ratio of the bromeliad-dwelling jumping spider, Psecas chapoda (Salticidae)

Figure 4. Phenogram of the Psecas chapoda population on plants of Bromelia balansae without inflorescence, from May 1998 to April 2000 (N53516 spiders).

opencc-by-4.0Dec 2018View details →

Fig. 1 in Dependence of the sperm number on the adult age of the male black field cricket Teleogryllus commodus W ALKER (Insecta: Orthoptera)

Fig. 1: Shape and morphology of the spermatophore (total length: ca. 5 mm) separated from males of the black field cricket Teleogryllus commodus.

opencc-by-4.0Dec 2018View details →

Fig. 2 in Dependence of the sperm number on the adult age of the male black field cricket Teleogryllus commodus W ALKER (Insecta: Orthoptera)

Fig. 2: Results of sperm quantification of male crickets belonging to different age categories: (a) Age-dependence of the percentage of filled/unfilled spermatophores (N = 80); (b) Age-dependence of the number of sperm per spermatophore (N = 80). The asterisk indicates a significant difference (p <0.05) between adjacent mean values.

opencc-by-4.0Aug 2021View details →

Source data for "Glacial isostatic adjustment directed incision of the Channeled Scabland by ice-age megafloods"

The data provided in this repository is the source data for "Glacial isostatic adjustment directed incision of the Channeled Scabland by ice-age megafloods". This repository contains three directories for ANUGA simulations on (1) present-day topography, (2) glacial isostatic adjustment-corrected topography at 18 ka, and (3) glacial isostatic adjustment-corrected topography at 15.5 ka. Each directory includes hydrodynamic modeling data and topographic reconstruction data. This repository also contains MATLAB scripts for analyzing simulated discharge and shear stress values for replicating plots. Cite as: Pico. T., David, S.R., Larsen, I.J, Mix, A., Lehnigk, K., Lamb, M.P., Glacial isostatic adjustment directed incision of the Channeled Scabland by ice-age megafloods, PNAS, 2022.

FIG. 10 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 10. Looking south from the base of the Zos Canyon section. The arrow indicates the Red Rum sublocality.

FIG. 9. B in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 9. B. Shared diagnostic character (6) a shallow depression along the midline nasal suture anterior to the orbits on the dorsal surface of the skull.

FIG. 9. A in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 9. A. Comparison of IGM 100/3181 (top) with the holotype of Haya griva (IGM 100/2017, bottom). Shared diagnostic characters (Makovicky et al., 2011) are: (1) homodont unserrated premaxillary teeth, (2) the lack of a rugose rhamphothecal pad on the anterior surface of the premaxilla, (3) the presence of a triangular maxillary fenestra, (4) a jugal with a bifurcated (forklike) posterior ramus where it abuts the quadratojugal, (5) the presence of a quadratojugal foramen.

FIG. 4. A in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 4. A. Premaxillary tooth of IGM 100/3181 in mesial and distal views. Its precise orientation cannot be determined as it was found as float during preparation. B. Cheek tooth of IGM 100/3181. Its precise orientation cannot be determined as it was found as float during preparation, and is compatible with the morphology of both upper and lower teeth of referred Haya specimens.

FIG. 3 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 3. The left side of the cranium of IGM 100/3181, with interpretive drawing. Abbreviations are listed in appendix 1.

FIG. 1 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 1. Map of Mongolia showing the relative positions of the Javkhlant Formation exposures and Zos Canyon beds (near Ukhaa Tolgod). Zos Canyon is 7 km northwest of the Ukhaa Tolgod locality. See Pol and Norell (2004a: fig. 1) for detail.

opencc-by-4.0Oct 2013View details →

FIG, 1. John William Daly (1933–2008) on the upper Río San Juan. This paper is dedicated to John Daly, our late friend and colleague, who helped collect three of the new species here described. In addition to his globally acclaimed discoveries in chemistry and pharmacology, John was an accomplished field herpetologist who contributed importantly to the systematics and natural history of dendrobatoid frogs (see Grant et al., 2006; Myers, 2009). This photograph shows John at age 37, with the upper Río San Juan behind him and branches overhead of a madroño tree (probably Garcinia magnifolia, syn. Rheedia chocoensis, Clusiaceae). When in South America, John was never far from a dendrobatid frog—this time, in the tree above his head, a tiny, undescribed semiarboreal species (also collected and later named "Dendrobates fuguritus" by our colleague Philip Silverstone). Other dendrobatids found nearby included Phyllobates aurotaenia (Boulenger, 1913), which was then being used for poisoning blowgun darts, and also the nontoxic species that we name Silverstoneia dalyi herein. (Photograph by C. W. Myers, 2 km above Playa de Oro, Chocó, February 16, 1971.) in Review of the Frog Genus Silverstoneia, with Descriptions of Five New Species from the Colombian Chocó (Dendrobatidae: Colostethinae)

FIG, 1. John William Daly (1933–2008) on the upper Río San Juan. This paper is dedicated to John Daly, our late friend and colleague, who helped collect three of the new species here described. In addition to his globally acclaimed discoveries in chemistry and pharmacology, John was an accomplished field herpetologist who contributed importantly to the systematics and natural history of dendrobatoid frogs (see Grant et al., 2006; Myers, 2009). This photograph shows John at age 37, with the upper Río San Juan behind him and branches overhead of a madroño tree (probably Garcinia magnifolia, syn. Rheedia chocoensis, Clusiaceae). When in South America, John was never far from a dendrobatid frog—this time, in the tree above his head, a tiny, undescribed semiarboreal species (also collected and later named "Dendrobates fuguritus" by our colleague Philip Silverstone). Other dendrobatids found nearby included Phyllobates aurotaenia (Boulenger, 1913), which was then being used for poisoning blowgun darts, and also the nontoxic species that we name Silverstoneia dalyi herein. (Photograph by C. W. Myers, 2 km above Playa de Oro, Chocó, February 16, 1971.)

opencc-by-4.0Oct 2005View details →

Fig. 19 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. 19. Right mandible (UNSM 44813) and maxilla (UNSM 44814) of the oreodont Merycochoerus magnus from the Carpenter Ranch Formation, Merycochoerus Butte, Goshen County, Wyoming.