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1,140 results for “colonial”
Fig. 1 in A Unique Colony Of The Bobak Marmot, Marmota Bobak (Rodentia, Sciuridae), In Steppes Of The Right-Bank Ukraine
Fig. 1. Bobak marmot, the vicinity of Syrovo Village, Vradiivo District, Mykolaiv Region, 29.07.2013 (photo's author: S. K Semeniuk).
Fig. 4 in Spatio-Temporal Structure And Reproductive Success In A Rook (Corvus Frugilegus) Colony
Fig. 4. Distance of the newly built nests from the centre of the colony, from the edge of the colony (metres) and number of neighbouring nests within 6 metres (medians, full circles) and those of the randomly selected points (medians, empty squares) at each sampling date. 100 random points were selected for each date, sample sizes of the observed nests are shown above the medians. In the marked (*) cases the values of the observed nests dif- fered significantly from the values of the ran- dom points (Mann-Whitney test, P <0.05)
Data and code for "Changing allometric relationships among fossil and Recent populations in two colonial species"
<p>MEPS.plus.xlsx (dataset from Di Martino & Liow 2021)</p> <p>Microporella_allometry_22.03.2022.xlsx (Sheet 1: Measurement data; Sheet 2: Fossil sample metadata; Sheet 3: Recent samples metadata)</p> <p>allo.10.R (code)</p>
Plant phenology, aphid colony growth, and honeydew deposition data
<p>Changing phenological cues can lead to trophic mismatch for plants and herbivores, and this often shifts herbivore feeding to plant stages of lower quality. Temperature can also mediate how herbivores respond to plant quality, leading to temperature-by-phenology interactions. We examined how both temperature and host plant phenology impact aphid abundance and their mutualism with ants. Our study system was composed of aphids (<em>Aphis asclepiadis</em>) that colonize flowering stalks of the host plant, <em>Ligusticum porteri</em>. Abundance of this aphid species is dependent on mutualism with several ant species. To understand how host plant phenology and temperature affect aphid abundance, we experimentally accelerated snow melt date by two weeks, which correspondingly advanced flowering phenology. Then, we factorially combined this phenology treatment with open top warming chambers surrounding aphid colonies. We tracked aphid colony growth and interactions with ants, and results showed the greatest colony growth at cooler, ambient temperatures on host plants without accelerated phenology. These colonies also showed the highest levels of honeydew deposition relative to their overall size. Our findings show that trophic mismatch decreases aphid abundance, and changes to the ant-aphid mutualism exacerbate this effect.</p>
Fig. 2 in . Study of Nosema spp. in the Tomsk region, Siberia: co-infection is widespread in honeybee colonies
Fig. 2. Distribution of Nosema species in bee colonies (Apis mellifera) throughout the Tomsk region (dots A–I). Bee colonies not infected by Nosema are indicated in yellow; bee
Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile. in Evidence For Wildfires During Deposition Of The Late Miocene Diatomites Of The Konservat-Lagerstätte Lake Saint-Bauzile (Ardèche, France) - Preliminary Results
Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile.
Fig. 16 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 16. Rugose coral Stelechophyllum cf. banffense (Warren, 1927), C-52434 = GSC-142476, locality 12 (Fig. 2), from Meilleur Member, Flett Formation Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada. Thin sections. A1, transverse section of fragment of colony, note different state of preservation in middle of picture and area around it (arrows); A2, A3, longitudinal sections; A4–A7, offsets in ascending growth stages.
Fig. 15 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 15. Rugose corals Cordilleria sp. A. IG-82 = UAM-Tc.Can./8, locality 3 (Fig. 2), from Meilleur Member, Flett Formation (Mississipian), Rundle Group, Liard Basin, Northwest Territories, Northwest Territories, Canada; transverse thin section (A1); longitudinal thin sections (A2, A3), weakly accentuated down sloping of peripheral part of tabulae (arrow). B. C-47942 = GSC-142475, locality 14 (Fig. 2), from Flett Formation undivided, Rundle Group, Liard Basin, Northwest Territories, British Columbia, Canada; transverse section (B1, B2), longitudinal section, peel (B3). C. IG-18 = UAM-Tc.Can./10, locality 3 (Fig. 2), from Tlogotsho Member, Flett Formation (Mississipian), Rundle Group, Liard Basin, Northwest Territories, British Columbia, Canada; longitudinal thin sections (C1, C2), transverse thin section (C3). D. IG-83 = UAM-Tc.Can./9, locality 3 (Fig. 2), from Meilleur Member, Flett Formation Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada; transverse thin section.
Fig. 13 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 13. Rugose coral Cordilleria aff. oculinum (Sando, 1963), from Meilleur Member, Flett Formation (Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada (A, C, F), Tlogotsho Member, Tlett Formation (Mississippian), Rundle Group, Liard Basin, Northwest Territories, Canada B, D), and upper Prophet Formation (Mississippian), Roundle Group, Northwest Territories, Canada (E). A. C-52268 = GSC-142473, locality 2 (Fig. 2); transverse thin section (A1), longitudinal thin section (A2). B. IG-16 = UAM-Tc.Can./5 B-D, locality 3 (Fig. 2); longitudinal section, peel (B1), transverse thin section (B2). C. IG-85 = UAM-Tc.Can./6, locality 3 (Fig. 2); longitudinal section (peel). D. IG-30 = UAM-Tc.Can./7, locality 3 (Fig. 2); longitudinal section, peel (D1), transverse thin section (D2). E. C-52205 = GSC-142472, locality 2 (Fig. 2); transverse thin section. F. C-52361 = GSC-142474, locality 13 (Fig. 2); transverse thin section.
Fig. 12 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 12. Variation in septal number and corallite diameters in colonies of rugose coral Cordilleria aff. oculinum (Sando, 1963) and holotypes of Cordilleria oculina (Sando, 1963) and Cordilleria warreni (Nelson, 1960) added for comparison. Data for C. oculina after Sando (1963: part of fig. 1); for C. warreni after Nelson (1960: pl. 24: 11).
Fig. 10 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 10. Variation in septal number and corallite diameters of rugose coral Cordilleria aff. mutabile (Kelly, 1942) and the holotype colony of Cordilleria mutabile (Kelly, 1942) added for comparison. Large differences in that character between colonies comparable to that noted by Sando (1963: fig. 1) in "Lithostrotion (Siphonodendron) oculinum" (Sando, 1963) = Cordilleria oculina (Sando, 1963) (see Fig. 12).
Fig. 9 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 9. Rugose corals Cordilleria aff. mutabile (Kelly, 1942), from Flett Formation (Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada. A. C-52124 = GSC142471, locality 3 (Fig. 2); longitudinal thin sections (A1, A2), transverse thin section (A3). B. C-47930 = GSC-142469, locality 14 (Fig. 2), Flett Formation undivided; longitudinal sections, peels (B1–B3), transverse thin section (B4). Note in B1 steeply arranged tabulae when pseudocolumella present (black arrow), flat tabulae when pseudocolumella absent (white arrow).
Fig. 8. Tabulate corals Michelinia expansa White, 1883, from locality 3 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 8. Tabulate corals Michelinia expansa White, 1883, from locality 3 (Fig. 2), Meilleur Member, Flett Formation (Viséan, Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada. Transverse thin sections unless stated otherwise. A. IG-91-2 = UAM-Tc.Can./3; A1, fragment of colony; A2, longitudinal section (peel) of offsetting corallite; showing pores (arrows). B. IG-17 = UAM-Tc.Can./1; B1, drawing on peel image of longitudinal section of corallites in different growth stage; showing pores (grey arrows) and apparent absence of pore resulting from eccentric section (black arrow); B2, fragment of a colony. C. IG-91-1 = UAM-Tc.Can./2, different growth stages; C1, very early growth stage of offset surrounded by thick, solid wall; C2, very early growth stage of offset; showing P2 pores (black arrows) and overgrown pores? (white arrows); note differentiated thickness of partitions; C3, two offsets adjacent to one another with first dissepiments developed; C4, very early growth stage of offset with two P1 pores open to two adjacent mature corallites; C5, partitions differentiated in thickness, showing P2 pores (arrow).
Fig. 1 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 1. Map showing location of study area, Carboniferous lithofacies assemblages subcropping beneath Permian and Mesozoic deposits in the Western Canada Sedimentary Basin, principal sub-basins, uplifts, and shelves. In the Liard Basin western occurrences of the Rundle and Matson lithofacies assemblages overlie and pass westwards into the Besa River lithofacies assemblage. See Fig. 3 for the formational composition of the Banff, Rundle, and Mattson lithofacies assemblages. Modified from Richards et al. (1994).
Fig. 7. Tabulate coral Michelinia expansa White, 1883 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 7. Tabulate coral Michelinia expansa White, 1883. IG-91-1 = UAM-Tc.Can./2, from locality 3 (Fig. 2), Meilleur Member, Fleet Formation (middle Viséan, Mississipian), Rundle Group, Liard Basin, Northwest Territories, Canada. A1, thin section of colony, transverse in most part and longitudinal at colony edge; A2, immature corallite, note remnants of wall microstructure, arrow points to P1 pore; A3, septal spines attached to tabula; A4, pores P1 and P 2 situated close to each other (arrows).
Fig. 6 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 6. Stratigraphic column of type section of Viséan Flett Formation at Jackfish Gap on Yohin Ridge, eastern Cordillera, southwest corner of Northwest Territories. Shows lithostratigraphic positions of coral collections discussed in this paper. Abbreviations: Fm., Formation. Stratigraphic column modified from Richards et al. (1989: fig. 24).
Fig. 3. A in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 3. A. Partly schematic, palinspastic stratigraphic cross-section A–A' showing stratigraphic relationships of Flett Formation in eastern Cordillera of northern part of project area in southwest corner of Northwest Territories and southeast Yukon. B. Environments of deposition. See Fig. 2 for line of cross-section A–A'. Abbreviations: Fm., Formation (formal unit); fm., formation (informal unit); Mbr., Member (formal unit). Modified from Richards et al. (1989).
Fig. 2 in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 2. Simplified geological map of study region showing distribution of outcrops of Carboniferous Prophet, Flett, and Mattson formations in southwest corner of Northwest Territories and southeast Yukon Territory and lines of cross-section A–A' and B–B' (see Figs. 4, 5 for details). Surface and subsurface sections (coral localities are in orange): 1, Twisted Mountain; 2, north end Mattson anticline; 3, Jackfish Gap (main coral locality); 4, Tlogotsho Plateau; 5, Etanda Lakes; 6, Tika Creek; 7, Pan American Home Signal C.S.P. Celibeta Number 7; 8, Texaco N.F.A. Bovie Lake J-72; 9, Pan American A-1 Pointed Mountain P-53; 10, Canada Southern et al. North Beaver River YT 1-27; 11, Pan American Beaver YT G-01; 12, West Flett anticline; 13, Southern Liard Range; 14, Sheaf Cree. Abbreviations: Fm., Formation (formal unit); fm., formation (informal unit); fms., formations; S., south; W., west; YT, Yukon Territory; C.S.P., Canada Southern Petroleum. Modified from Harker (1963) and an unpublished map by Andrew Okulitch from 2005 (reproduced with permission).
Fig. 4. A in Mississippian colonial tabulate and rugose corals from the Flett Formation, Liard Basin, northwest Canada
Fig. 4. A. Partly schematic, palinspastic stratigraphic cross-section showing stratigraphic relationships of Flett Formation in southern part of project area. B. Environments of deposition. See Fig. 2 for line of cross-section B–B'. Abbreviations: Fm., Formation (formal unit); fm., formation (informal unit); Mbr., Member (formal unit); mbr., member (informal unit); YT, Yukon Territory; C.S.P., Canada Southern Petroleum. Modified from Richards et al. (1994).
Figures 20A–D. Symplectoscyphus paulensis, stn 120. A, colony. B, distal monosiphonic branches. C in Deep-water hydroids (Hydrozoa: Leptolida) from Macquarie Island
Figures 20A–D. Symplectoscyphus paulensis, stn 120. A, colony. B, distal monosiphonic branches. C, part of distal branch. D, rim of hydrotheca showing obtuse cusps. Scale bar: A, 50 mm; B, 10 mm; C, 1 mm; D, 0.5 mm.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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DANDI Archive for NWB datasets
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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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