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opencc-by-4.0Nov 2020View details →

Figure 3 in Leishmaniasis and phlebotomine sand flies in Oman Sultanate

Figure 3. (A) Professor Rioux and the field team in the Dhofar; (B) Ouadi Herwouib in the Dhofar labelled Dh6 in accordance with Figure 1 where Ph. bergeroti, Ph. alexandri, Se. tiberiadis and Se. fallax are the most abundant species. (C) the Sharqiyah around the Ouadi.

opencc-by-4.0Nov 2020View details →

Figure 2 in Leishmaniasis and phlebotomine sand flies in Oman Sultanate

Figure 2. Map showing the sampling of phlebotomine sandflies, dogs, foxes and patients. Locations in the Sharqiyah are labelled Sh and those from the Dhofar are labelled Dh, in accordance with Figure 1.

opencc-zeroJun 2024View details →

Dataset: Smart Sand, Inc. (SND) Stock Performance

This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.

opencc-by-4.0Dec 2020View details →

Fig. S1 in A New Testate Amoeba, Matsakision ogawaraensis sp. nov. (Silicofilosea: Incertae sedis Euglyphida) from Lake Shore Sand of Northern Japan

Fig. S1. Light micrograph of Matsakision ogawaraensis sp. nov. (A) broad lateral view of paratype MO-004 (on TNS-AL-58972). (B) ventral view of paratype MO-005 (on TNS-AL-58972). Scare bar: 10 µm

opencc-by-4.0Dec 2020View details →

Fig. 2 in A New Testate Amoeba, Matsakision ogawaraensis sp. nov. (Silicofilosea: Incertae sedis Euglyphida) from Lake Shore Sand of Northern Japan

Fig. 2. Light micrographs of Matsakision ogawaraensis sp. nov. (A) broad ventral view of a living cell. (B) ventral view of a living cell. (C) back view with emphasis on the pseudopodia. Arrowheads indicate pseudopodia. (D) ventral view of holotype MO-001 (on TNS- AL-58972). (E) view of shell structure when the focal distance is adjusted to the test surface of MO-001. (F) view of MO-001 with emphasis on the apertural edge. Arrowheads indicate a chitinous lip. (G)–(H) lateral view of paratypes MO-002 (on TNS-AL-58972) and MO-003 (on TNS-AL-58972), respectively. Scale bars: 10 µm.

opencc-by-4.0Dec 2020View details →

Fig. 1 in A New Testate Amoeba, Matsakision ogawaraensis sp. nov. (Silicofilosea: Incertae sedis Euglyphida) from Lake Shore Sand of Northern Japan

Fig. 1. Outline of Matsakision ogawaraensis sp. nov.: ventral (A), lateral (B), apertural (C) view. SL – shell length, SW – shell width, SH – the longest shell height, AW – apertural width, AH – apertural height.

opencc-by-4.0Dec 2019View details →

Fig. 3 in Molecular Phylogeny of the Sand-dwelling Dinoflagellate Planodinium striatum and Chrysodinium gen. nov. for Plagiodinium ballux (Dinophyceae)

Fig. 3. Line drawings of the plate arrangement of Planodinium striatum (A–C), Plagiodinium belizeanum (D–F) and Chrysodinium ballux gen. nov. & comb. nov. (=Plagiodinium ballux) (G–I). Left lateral (A), right lateral (B), apical (C) views of Planodinium striatum redrawn from Hoppenrath et al. (2014). Left lateral (D), right lateral (E) and apical (F) views of Plagiodinium belizeanum redrawn from Wakeman et al. (2018). Left lateral (G), ventral (H) and apical (I) views of Chrysodinium ballux gen. & comb. nov. redrawn from Yamada et al. (2018) with a re-interpreted tabulation.

opencc-by-4.0Dec 2019View details →

Fig. 1 in Molecular Phylogeny of the Sand-dwelling Dinoflagellate Planodinium striatum and Chrysodinium gen. nov. for Plagiodinium ballux (Dinophyceae)

Fig. 1. Light (A–M) and scanning electron microscopy (N–O) images of Planodinium striatum isolated in June 2012 at Wimereux, France. (A–B) A cell in left lateral and dorsal views. Asterisk (*) indicates the pusule. (C–M) Different views of another cell. The arrows indicate hypothecal plates. (N) Cell in ventro-left lateral view. (O) Another cell in left lateral view. The arrowheads indicate the trichocysts. The inset shows a large pore surrounded by several small pores. Scale bar = 10 μm.

Fig. 3 in Cryptic subterranean diversity: regional phylogeography of the sand termite Psammotermes allocerus Silvestri, 1908 in the wider Namib region

Fig. 3 Median-joining network of the combined COI and COII P. allocerus sequences. Coloured circles represent the observed haplotypes, and the size is proportional to the number of collections. Black circles represent missing haplotypes. Marks show the number of mutation steps. Haplotype numbers are gained from DnaSP v6. Dotted lines and colours mark haplotypes according to the genetic group of the phylogeny

Fig. 4 in Cryptic subterranean diversity: regional phylogeography of the sand termite Psammotermes allocerus Silvestri, 1908 in the wider Namib region

Fig. 4 Differences in the tapetum colour of three P. allocerus colonies and the royal pair. A Whitish tapetum of a nest from the Springklipplain from the 'Succulent Karoo' group %South Africa, 26 September 2016). B First image of the king and queen of P. allocerus from Yellow Dune %'Succulent Karoo', South Africa, 08 March 2015). C Blackish tapetum of a nest from Dieprivier %'Southern Namib', Namibia, 05 April 2017). D Blackish tapetum and chambers filled with foraged grass from Iona %'Northern Namib', Angola, 26 September 2016). Images taken by Norbert Jürgens, Felicitas Gunter

Fig. 1 in Cryptic subterranean diversity: regional phylogeography of the sand termite Psammotermes allocerus Silvestri, 1908 in the wider Namib region

Fig. 1 Phylogeny of 65 P. allocerus collections inferred by the Bayesian analysis of COI and COII markers. Support values are given in posterior probability. Clades are coloured according to the genetic group. Dark blue: Succulent Karoo; Light Blue: Southern Namib; Dark green: East Gariep; Light Green: Southwestern Kalahari; Yellow: Nama; Ochre: Western Kalahari Basin; Red: Northern Namib. Abbreviations of study sites are shown in Fig. 2

Figure 6 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 6: Scorpion movement after being displaced from its burrow. The scorpion in this lured experiment grabbed the floss as it moved past its burrow and was dragged about 50 cm away from its burrow in the direction of 7 o'clock. The excursion began at 21:14:12 and lasted almost 32 minutes. The scorpion did not relocate its burrow and walked off the screen to the left as indicated by the arrowhead. The arrow is 10 cm long and points north; upslope is toward the top of the figure.

Figure 1 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 1: Cue clues. a. Major scorpion sensory organs and the modalities to which they respond. b. Different return routes suggest the use of different stimuli.

Figure 5 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 5: Lured excursions. Twenty-five tosses of a small lure were made across the span of about an hour; times of tosses are indicated at right and the movement of the lure after each toss is shown in the figures at left. The duration of the dragging of the lure is indicated in parentheses next to the time. The arrowhead at the end of each tracing indicates the point where the lure was lifted from the sand surface. The scorpion was coaxed from its burrow on four separate occasions. These excursions are depicted in parts a-e and indicated as E1-E4 in the time list at right. Part f shows all tosses that did not induce scorpion movement. Sometimes the animal reacted to subsequent tosses while away from its burrow; these tosses are indicated with an "x" next to its time and the interaction between the movement of the lure and the movement of the animal is indicated by fine dotted lines on figures c-e (the very small numbers indicate the time in seconds of the excursion at which the interaction occurred). The arrow is 10 cm long and points north; upslope is toward the top of the figures.

Figure 8 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 8: Scorpion at burrow threshold. A female P. utahensis near the Scamp trailer is photographed at the opening of her burrow under UV light on March 21, 2009.

Figure 2 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 2: In situ videotaping of scorpions. a. The relative positions of the Scamp base trailer and the two scorpion burrows. b. IR camera mounted on metal pole inserted in sand and positioned above burrow. c. Close-up of IR camera. d. Video receiver mounted on back of base trailer. e. Inside trailer showing video monitor and DVD recorder. f. Still frame of IR video of scorpion outside of its burrow.

Figure 3 in In situ infrared videography of sand scorpion nighttime surface activity

Figure 3: Scorpion emergence relative to traffic around the burrow. Shown are tracings of paths taken by all animals moving within 40 cm of scorpion 2's burrow during the 2 hr surveillance on night 1. The key shows the beginning time of each animal's path. The small numbers on the paths indicate time, in seconds, after the beginning of the movement into the region. Scorpion 2 emerged from its burrow twice (excursions C and K). The fine dotted lines indicate the time and location of other animals at the moment of scorpion emergence. The inset shows a composite photo of a kangaroo rat's movements near scorpion 2's burrow on the second night of filming; the top path occurred about 35 minutes into the filming, the lower path 82 minutes later. Each path took less than 2 seconds to complete. Both arrows are 10 cm long; the direction arrow points north. Upslope is toward the top of figure.

Fig. 2 in Cryptic subterranean diversity: regional phylogeography of the sand termite Psammotermes allocerus Silvestri, 1908 in the wider Namib region

Fig. 2 Distribution map of all Psammotermes allocerus collections and their assignment to the genetic groups found in the phylogenetic analyses %colours). Circles: Collections used for the phylogeny. Black lines: Country borders. Northern Namib: %AH) Aba Huab rivier, %GV) Giribesvlakte, %HD) Hartmann Dunes, %HO) Hoada, %IO) Iona, %MF) Marienfluss, %PR) Purros, %ROE) Rössing mountain, %SO) Sorris Sorris, %TM) Tomakas; Western Kalahari Basin: %AHV) Alt-Hartebeestvlei, %AM) Alex Muranda, %GU) Gariganus, %KM) Katima Mulilo, %RI) Rimini, %RS) Rundu South, %RV) Ravenna, %SA) Samehaling, %SK) Swartkop, %WF2) Warmfontein; Nama: %BY) Barby, %FRC) Fish river Canyon, %GO) Goageb, %SH) Seeheim, %WV) Witvley; Southwestern Kalahari: %GM) Goedmoed, %GR) Gurus, %KFE) Kalkfontein East, %NK) Neikop, %SKN) Swartkop North, %TT) Tranental, %UK) Ukamas, %WF1) Warmfontein; East Gariep: %AP) Akadispass, %BD) Belda, %BH) Bruinheuwel, %DH) De Hoop, %KFE) Kalfontein East, %KFW), %KV) Koeroegabvlakte, %NO) Norachas, %NU) Numees, %RB) Rooiberg, %TB) Tatasberg, %TBQ) Tatasberg Quarzfield; Southern Namib: %DV) Dieprivier, %GA) Garub, %KH) Keetmanshoop, %KW) Keerweder, %RO) Rostock, %SR) Sesriem; Succulent Karoo: %HN) Holhat North, %KTV) Kortdoornvlakte, %LUE) Lüderitz, %RDE) Red Dune East, %SP) Springklipplain, %YD) Yellow Dune, %YDRD) Yellow Dune Red Dune Transect

opencc-by-4.0Sep 2023View details →

Fig. 1 in A noteworthy locality of the javelin sand boa (Eryx jaculus Linnaeus, 1758) in Southern Bulgaria

Fig. 1. Javelin sand boas observed in the study area. 1, 8, and 10 - juveniles, 2 and 3 - half basking. 4 - the studied habitat, 5, 6, 7, and 9 - adult individuals.