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On the emergence mechanism of carrot sprites
<p>This dataset includes the input and output files for the paper: On the emergence mechanism of carrot sprites.</p> <p>Intput files:</p> <p># <strong>Plasma-chemistry, diffusion and mobility coefficients</strong></p> <p>sprite_chemistry_basic.txt</p> <p># <strong>Configuration files</strong></p> <p>sprite_3d_simp.cfg</p> <p>m_user.f90</p> <p>Output files:</p> <p>sprite_3d_*.silo</p>
Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass]. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass].
Fig. 1. Circular histogram rose plot showing Rhagoletis brncici and R in Differences in larval emergence chronotypes for sympatric Rhagoletis brncici Frías and Rhagoletis conversa (Bréthes) (Diptera, Tephritidae)
Fig. 1. Circular histogram rose plot showing Rhagoletis brncici and R. conversa larval emergence from fruit in a 24-h clock. For both graphs, the arrow shows the mean time of emergence. Main numbers in sections correspond to time in hours. Numbers accompanying circumferences refer to number of individual larvae replicates.
Figure 3 Drosophila suzukii collected emerging from a in Living fruits of Psychotria brachyceras Müll. Arg. (Rubiaceae) as the main larval host of Zygothrica orbitalis (Sturtevant, 1916) (Diptera, Drosophilidae)
Figure 3 Drosophila suzukii collected emerging from a fruit of Psychotria brachyceras. (A) Male in lateral view (arrow indicating the dark spot at wing apex, at the intersection of veins R2+3 and C, typical of males of the species); (B) Detail of sex combs in foretarsus (arrows); (C) Posteroventral view of male periphallic organs; (D) Lateral view of the apex of abdomen of a female, showing the serrated oviscapt. Abbreviations: cerc, cercus; epand, epandrium; ovscp, oviscapt; ph, phallus; sur, surstylus.
Fig. 1 in Impact of host plant resistance on emergence, body parameters, and supercooling point of Cylas formicarius elegantulus (Coleoptera: Brentidae)
Fig. 1. Daily (Mean ± SE) sweetpotato weevil emergence 30 d afer oviposition from individual storage roots of sweetpotato cultivars 'Beauregard,' 'Evangeline,' and 'Murasaki.'
Fig. 2. Adult spotted wing drosophila emergence from berries 2 in Efficacy of entomopathogenic fungal products for biological control of spotted wing drosophila (Diptera: Drosophilidae) under laboratory conditions
Fig. 2. Adult spotted wing drosophila emergence from berries 2 wk afer re- moval from the arenas. Bars with the same letter are not significantly different from each other (P> 0.05). Error bars represent standard error of the mean.
Fig. 1 in A bucket-type emergence trap for detecting overwintered Dasineura oxycoccana (Diptera: Cecidomyiidae) and its parasitoids in cranberry
Fig. 1. Bucket-type emergence trap seated into cranberry field. Inner bucket with mesh lid is descending into support bucket.
Figs. 1-18 in Emergent and possible invasive pest species of weevils in Mexico
Figs. 1-18. (1) Conotrachelus perseae Barber; (2) Conotrachelus aguacatae Barber; (3) Conotrachelus dimidiatus Champion; (4) Conotrachelus copalensis Salas and Romero; (5) Heilipus lauri (Boheman); (6) Heilipus albopictus (Champion); (7) Copturus aguacatae Kissinger; (8) Sphenophorus incurrens Gyllenhal; (9) Scyphophorus acupunctatus Gyllenhal; (10) Cactophagus spinolae (Gyllenhal); (11) Apinocis subnudus (Buchanan); (12) Rhyssomatus nigerrimus (Fåhraeus); (13) Epicaerus operculatus (Say); (14) Epicaerus cognatus Sharp; (15) Amphidees latifrons (Sharp); (16) Naupactus cervinus (Boheman); (17) Epicaerus aurifer Boheman; (18) Epicaerus mexicanus Boheman.
Fig. 2 in A bucket-type emergence trap for detecting overwintered Dasineura oxycoccana (Diptera: Cecidomyiidae) and its parasitoids in cranberry
Fig. 2. Number (mean + SEM) of overwintered cranberry tipworms and parasitoids detected per emergence trap per wk in 2015. Julian Date 124 = 4 May; 152 = 1 Jun; 187 = 6 Jul; 215 = 3 Aug. Number of traps per wk was 30, 50, 59, 60, 60, 46, 56, 57, 57, 57, 57, 57, 57, 57, 57, 51, 51, respectively, for the 17 wk.
Fig. 1 in Effect of the oviposition period and age of the females of Dalbulus maidis (Hemiptera: Cicadellidae) in the emergence of egg parasitoids
Fig. 1. Average (± SE) number of eggs laid per d by Dalbulus maidis in treatments (Young-3, Young-6, Mature-3, and Mature-6). The circles represent the mature (8-wk-old) leafoppers, whereas the squares represent the young (2-wk-old) leafoppers.
Fig. 52 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 52. Accumulations of goniatite conchs and other fossils in the latest Frasnian strata of the Holy Cross Mountais. A. Conchs of Archoceras varicosum (Drevermann, 1901) in a piece of the Upper Kellwasserkalk from Płucki (Pł−391). B. Conchs of Aulatornoceras belgicum (Matern, 1931) in association with Linguatornoceras sp. from the same bed. C. Acid etched sample Ko−142 from Kowala with similar but more homogenized association.
Fig. 43 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 43. Variability of P1 (sp) elements of the latest Frasnian palmatolepidids. Scattergrams show ontogenetic changes of the angle between the dorsal process and the posterior lobe of the platform in sample Pł−391 from the Upper Kellwasserkalk at Płucki (Fig. 42) overdominated by Lagovilepis bogartensis (with rare Manticolepis winchelli documented with its M elements), associated Klapperilepis triangularis and sample Wtr−18 from Wietrznia where only M elements of Manticolepis (probably a relic population of M. gigas) have been found (Fig. 38A–H). The Pł−391 population variability is separately shown for adult elements (longer than 1 mm) with contours of extreme and modal morphologies added. Note that there is no apparent difference in the course of ontogeny and morphologic variability of platform shape between L. bogartensis and M. winchelli or M. gigas (despite fundamental differences in the apparatus organisation) whereas K. triangularis is different in all these respects (plus the dorsal process bending).
Fig. 41 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 41. Palmatolepidid Lagovilepis bogartensis (Stauffer, 1938). A–J. Early population from the lower cephalopod limestone at Płucki, sample Pł−22; P1 (sp) elements ZPAL CXVI/656, 665, 1209, 657, 655, 1208 (A–F), P2 (oz) element ZPAL CXVI/658 (G), S0 (tr) element ZPAL CXVI/667 (H), S1 (lo) element ZPAL CXVI/668 (I), and M (ne) element ZPAL CXVI/663 (J). K–O. Late population from Kowala, samples Ko−149 (K, L, O) and Ko−151 (M, N); P1 (sp) elements ZPAL CXVI/491 and 492 (K, L), S3–4 (ke−hi) element ZPAL CXVI/1204 (M), and M (ne) elements ZPAL CXVI/1205 and 501 (N, O).
Fig. 37 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 37. Palmatolepidid Manticolepis gigas (Miller and Youngquist, 1947) from the midFrasnian of Wietrznia II quarry, sample Wtr−5; P1 (sp) elements ZPAL CXVI/752, 753, 754, 751, and 750 (A–E), S1 (lo) element ZPAL CXVI/758 (F), S0 (tr) elements ZPAL CXVI/761 and 760 (G, H), P2 (oz) element ZPAL CXVI/755 and 762 (I, L), S3–4 (ke−hi) element ZPAL CXVI/759 (J), S2 (pl) element ZPAL CXVI/757 (K), and M (ne) element ZPAL CXVI/756 (M).
Fig. 27 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 27. Late Ancyrodella from the late Frasnian of Płucki. A–F, K. Ancyrodella lobata Branson and Mehl, 1934 from the lower cephalopod limestone, sample Pł−22, P1 (sp) elements ZPAL CXVI/627, 625, 626, 624, 630, and 629 (A–F), and P2 (oz) element ZPAL CXVI/632 (K). G–J, L, M. Ancyrodella curvata Branson and Mehl, 1934 from the Upper Kellwasserkalk, sample Pł−391, P1 elements ZPAL CXVI/483, 1184, 484, 490, 632, 489, and 487 (G–I), M (ne) element ZPAL CXVI/490 (J), S3–4 (ke−hi) element ZPAL CXVI/489 (L), and S2 (pl) element ZPAL CXVI/487 (M). Magnifications shown by the bar scale in the upper left corner, except for G, J, L, M, and H with their own scales.
Fig. 33 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 33. Palmatolepidids from the mid−Frasnian of Wietrznia. A–H. Kielcelepis ljashenkoae (Ovnatanova, 1976) from Wietrznia, sample Wtr−15; P1 (sp) elements ZPAL CXVI/1108 and 1120 (A, B), P2 (oz) element ZPAL CXVI/1109 (C), S0 (tr) element ZPAL CXVI/1122 (D), S1 (lo) element ZPAL CXVI /1110 (F), S2 (pl) elements ZPAL CXVI/1123 and 1102 (E–G), and S3–4 (ke−hi) element ZPAL CXVI/1124 (N). I–S. Kielcelepis hassi (Müller and Müller, 1957) from sample Wtr−16 (M, O, S) and Wtr−30 (I–L, N, P–R); S0 element ZPAL CXVI/ 1125 (M), P1 (sp) elements ZPAL CXVI/ 1130, 1128, 1127, and 1129 (I–L), M (ne) element ZPAL CXVI/1133 (N), S3–4 elements ZPAL CXVI/1126 and 1132 (O, Q), and P2 elements ZPAL CXVI/1135, 1131, and 1103 (P, R, S).
Fig. 26 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 26. Variability and species distinctions of P1 (sp) elements in early Ancyrodella. Scattergrams of density of tuberculation quantified as a ratio of approximated platform area (platform length PL multiplied by its width W) to the number of denticles (except those of carina) and approximated area of the smooth surface on the ventral end of the platform (length of this area S multiplied by its lateral extend E) against element length which serves as an approximation of ontogenetic stage. Three successive samples from Wietrznia are represented by pairs of these scattergrams. That of sample Wtr−7 is A. rotundiloba (Bryant, 1921), sample Wtr−9 represents A. alata (Glenister and Klapper, 1966), and sample Wtr−13 A. rugosa Branson and Mehl, 1934.
Fig. 49 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 49. Succession of palmatolepidid species in sections of the Frasnian and earliest Famennian representing probably relatively deeper (Płucki, Włochy) and shallower (Wietrznia) areas in the Holy Cross Mountains. Approximate percent contribution to samples shown by horizontal bars; provisional Ancyrodella−based zonation used to correlate sections (each lower zonal boundary defined on the evolutionary origin of its nominal species – they remain to be documented biometrically). Note that Klapperilepis triangularis and Conditolepis? linguiformis first appear in offshore areas and then expand to shallower environments. Also Lagovilepis bogartensis may be an open−sea species. Only K. praetriangularis survives the Frasnian–Famennian boundary event, probably being a relatively cold−water species. The record is too incomplete and punctuated to allow precise evolutionary studies but a general pattern of the evolution is shown with diagrammatic presentation of apparatuses.
Fig. 15 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 15. Playfordia primitiva (Bischoff and Ziegler, 1957) from the early Frasnian of Wietrznia Iquarry, sample Wtr−9; elements ZPAL CXVI/1061 (A), 1062 (B), and 1060 (C).
Fig. 11 in Emergence and collapse of the Frasnian conodont and ammonoid communities in the Holy Cross Mountains, Poland
Fig. 11. The prioniodinid Pluckidina slupiensis sp. nov. from the early Frasnian of Włochy (sample Wł−R/A1) in the Holy Cross Mountains, P1 (sp) elements ZPAL CXVI/871 and 874 (A, B), P2 (oz) elements ZPAL CXVI/875 and 872 (C, D), S1 (lo) elements ZPAL CXVI/879 and 876 (E, F), S4 (hi) element ZPAL CXVI/880 (G), S2 (pl) elements ZPAL CXVI/877 and 878 (H, I; H holotype), S0 (tr) element ZPAL CXVI/873 (J), and M (ne) element ZPAL CXVI/881 (K).
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Allen Brain Atlas
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