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FIGURE 2 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test
FIGURE 2. Classical (A) and coverage-based (B) rarefaction of the Bermont Formation samples. In each panel, the red curve marks the lithified sample, and the blue curve marks the corresponding unlithified replicate sample. The gray curves mark other unlithified samples taken from different horizons of the same formation at the same outcrop. The red and blue bands mark 95% confidence intervals.
FIGURE 14 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 14. Distribution maps of benthic foraminifera occurring in Namibian and western South African outer shelf (blue shading = Lowry, 1987; black dots = Compton et al., 2002, 2004 and this study), lower to middle upper Quaternary sediments (green-yellow dots = McMillan, 1987) and inner shelf surface grab sediments (red-yellow dots = Schmidt-Sinns, 2008). Samples from McMillan (1987), Compton et al. (2002, 2004) and this study represent Pleistocene-aged foraminifera and samples from Lowry (1987) and Schmidt-Sinns (2008) are from surface grab sediments.
FIGURE 15 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 15. Mid to late Pleistocene/Holocene environmental interpretation of the southwestern margin of Africa based on foraminifera and mollusc species found in outer shelf sediments. Slope data and occurrences are based on reports from ODP Leg 175 (Wefer et al., 1998) and results from cores GeoB 20601-4, 8342-6 and 8336-6 (Meteor Cruises M123 and M57/1) in Chapter 7 of Bergh (2019).
FIGURE 10 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 10. Whole and fragmented shells (top) (core 2658, 10-15 cm sampling interval), Nuculana bicuspidata (bottom left) shells including articulated valves (core 2634, 78-85 cm) and Pecten spp. fragments (bottom right) (core 2658, 88-90 cm) from the northern Namibian cores.
FIGURE 11. Planktic foraminifera from the Namibian outer shelf with primary apertural views visible. 1 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 11. Planktic foraminifera from the Namibian outer shelf with primary apertural views visible. 1. Globorotalia (Globoconella) inflata (d'Orbigny, 1839b) (core 2670, 98 cm); 2. Globorotalia menardii (Parker, Jones and Brady, 1865) (core 2670, 23 cm); 3. Globorotalia truncatulinoides (d'Orbigny, 1839b) (core 2670, 23 cm); 4. Neogloboquadrina dutertrei (d'Orbigny, 1839a) (core 2670, 43 cm); 5. Neogloboquadrina incompta (Cifelli, 1961) (core 2670, 85 cm); 6 Globigerina bulloides d'Orbigny, 1826 (core 2670, 85 cm); 7. Globigerinella siphonifera (d'Orbigny, 1839b) (core 2670, 33 cm); 8. Globigerinoides ruber white (d'Orbigny, 1839a) (core 2670, 13 cm); 9. Trilobatus sacculifer (Brady, 1877) (core 2670, 63 cm); 10. Orbulina bilobata (d'Orbigny, 1846) (core 2670, 3 cm); 11. Orbulina universa d'Orbigny, 1839a (core 2670, 33 cm).
FIGURE 8 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 8. Mollusc shells from the gravel fraction of the uppermost 2 units of the Walvis Bay-Lüderitz cores. 1. Dosinia lupinus (Linnaeus, 1758) (core 1407, 0-4 cm sampling interval); 2. Lucinoma capensis (Jaeckel and Thiele, 1931) (core 1397, 0-4 cm); 3. Tellina (Moerella) analogica Sowerby III, 1904 (core 1478, 8-12 cm); 4. Ostrea sp. (core 1657, 0-4 cm); 5. Nassarius vinctus (Marrat, 1877) (core 1407, 0-4 cm); 6. Turritella declivis Adams and Reeve, 1850 (core 1657, 20-24 cm); 7. Comitas saldanhae (Barnard, 1958) (core 1307, 0-4 cm).
FIGURE 8 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test
FIGURE 8. Hypothetical rarefaction curves illustrating the potential effects of lithification or other diagenetic processes on the observed biodiversity of a fossil assemblage. The rarefaction curves are shown in blue for unlithified, unaltered assemblages and in red for the lithified, altered assemblages. A-C, Total species richness is the same in the pristine and altered samples. D-F, Total species richness is lower in the altered samples. A,D, Evenness is lower in the altered samples. B,E Evenness is the same. C,F, Evenness is higher in the altered samples.
FIGURE 12 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 12. Distribution maps of benthic foraminifera occurring in Namibian and western South African outer shelf (blue shading = Lowry, 1987; black dots = Compton et al., 2002, 2004 and this study), lower to middle upper Quaternary sediments (green-yellow dots = McMillan, 1987) and inner shelf surface grab sediments (red-yellow dots = Schmidt-Sinns, 2008). Samples from McMillan (1987), Compton et al. (2002, 2004) and this study represent Pleistocene-aged foraminifera and samples from Lowry (1987) and Schmidt-Sinns (2008) are from surface grab sediments.
FIGURE 1 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test
FIGURE 1. Photographs of the outcrop and fossil samples. A. Outcrop at Caloosa Shell Quarry, Hillsborough County, Florida, USA. B. Close-up of outcrop showing sampling scheme. Pairs of replicate samples were taken immediately adjacent to each other at 30 cm vertical increments. C. Fossil sample prior to either sieving or cementation. D. Artificially cemented sample.
FIGURE 13 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 13. Distribution maps of benthic foraminifera occurring in Namibian and western South African outer shelf (blue shading = Lowry, 1987; black dots = Compton et al., 2002, 2004 and this study), lower to middle upper Quaternary sediments (green-yellow dots = McMillan, 1987) and inner shelf surface grab sediments (red-yellow dots = Schmidt-Sinns, 2008). Samples from McMillan (1987), Compton et al. (2002, 2004) and this study represent Pleistocene-aged foraminifera and samples from Lowry (1987) and Schmidt-Sinns (2008) are from surface grab sediments.
FIGURE 4 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 4. Mean relative abundance of planktic species preserved across the three units of the Walvis BayLüderitz cores.
FIGURE 3 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 3. Mean relative abundance, represented by column charts, of the major components within the complete sand fractions of core 1479.
FIGURE 2 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 2. Stratigraphy of the Conception and Meob Bay cores. The depositional ages and units are defined by Compton and Bergh (2016). Unit 6 = reworked foram layer; unit 5 = brown to olive-green mud unit; unit 4 = pelletal phosphorite sandy layer; unit 3 = slightly shelly layer; unit 2 = shelly sandy layer; unit 1 = shelly gravel layer (Compton and Bergh, 2016).
FIGURE 5 in When roads cross streams: fish assemblage responses to fluvial fragmentation in lowland Amazonian streams
FIGURE 5 | ANOVA results for assemblage structure in northeastern Amazonian streams among stream reach groups. A. Taxonomic structure; B. Functional structure. D: Downstream reaches from impoundments; I: Impounded reaches; U: Upstream reaches from impoundments.
FIGURE 4 in When roads cross streams: fish assemblage responses to fluvial fragmentation in lowland Amazonian streams
FIGURE 4 | Relative contribution of turnover and nestedness component to total beta diversity obtained after averaging pairwise dissimilarities (Sørensen index) between stream reaches at each stream. D: Downstream reaches from impoundments; I: Impounded reaches; U: Upstream reaches from impoundments.
FIGURE 3 in Short-term response of fish assemblages to instream habitat restoration in heavily impacted streams
FIGURE 3 | Physical changes in stream reaches: A. Picture of the buried structure in P2; B. P3 stream reach at the beginning of the experiment; C. P3 stream reach at the end of the experiment, illustrating organic matter retention by the woody structure; D. macrophytes retention by wire in P8; E. growth of periphyton on the wood; F. growth of algae on the wood.
FIGURE 2 in Short-term response of fish assemblages to instream habitat restoration in heavily impacted streams
FIGURE 2 | Details of the structure used in the experiment. A. top view; B. side view; C. representation of the placement of the leaf-packs; D. cross section of the stream channel showing details of how the structure was placed in the stream; E. top view of the structure showing the points where the iron rods were installed.
Fig. 4 in Fish assemblages along a morphodynamic continuum on three tropical beaches
Fig. 4. Ordination diagram (tripolot) from Canonical Correspondence Analysis for the numerical abundance of fish species and environmental variables. (TEMP= Temperature; SAL= Salinity; TRANSP= Transparency and RTR= Relative Tide Range). (Acli = Achirus lineatus; Ancl = Anchovia clupeoides; Anja = Anchoa januaria; Anle = Anchoviella lepidentostole; Atbl = Atherinella blackburni; Atbr = Atherinella brasiliensis; Baso = Bathygobius soporator; Cala = Caranx latus; Ciar = Citharichthys arenaceus; Cima = Citharichthys macrops; Cisp = Citharichthys spilopterus; Ctbo = Ctenogobius boleosoma; Ctsm = Ctenogobius smaragdus; Ctst = Ctenogobius stigmaticus; Ersm = Erotelis smaragdus; Euar = Eucinostomus argentus; Eubr = Eugerres brasilianus; Eume = Eucinostomus melanopterus; Gost = Gobionellus stomatus; Hacl = Harengula clupeola; Hyun = Hyporhamphus unifasciatus; Lipi = Lile piquitinga; Lusy = Lutjanus synagris; Lygr = Lycengraulis grossidens; Meli = Menticirrhus littoralis; Mucu = Mugil curema; Muho = Mugil hospes; Muli = Mugil liza; Olsa = Oligoplites saurus; Poco = Pomadasys corvinaeformis; Povi = Polydactylus virginicus; Rhba = Rhinosardinia bahiensis; Spgr = Sphoeroides greeleyi; Spsp = Sphoeroides spengleri; Spte = Sphoeroides testudineus; Sypl = Symphurus plagusia; Syte = Symphurus tesselatus; Trca = Trachinotus carolinus; Trfa = Trachinotus falcatus; Trgo = Trachinotus goodei).
Figure 11 in Effects of temperature patterns on the spawining phenology and niche overlap of fish assemblages in the water bodies of the Dnipro River basin
Figure 11. Temporal trend of the Pianka mean niche overlap indexes deviation from random alternatives (1998–2018). The abscissa axis – years, the ordinate axis – the Pianka mean niche overlap indexes deviation from random alternatives, line – the linear approximation of the temporal trend (R2 = 0.32, p <0.001).
Figure 9 in Effects of temperature patterns on the spawining phenology and niche overlap of fish assemblages in the water bodies of the Dnipro River basin
Figure 9. Dynamics of the spawning start and end of fish in the "Dnipro-Orilskiy" nature reserve. The abscissa axis – years; the ordinate axis – spawning start and end, days of the year (black dot – spawning start time, red dot – spawning end time); lines – linear trend approximation
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
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
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.