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30,334 results for “Responsiveness”
Figure 2 in Response of Invasive Longhorn Beetles (Coleoptera: Lamiinae) to Known Cerambycid Aggregation-Sex Pheromones in the Puna District of Hawaii Island
Figure 2. Mean (± SE) numbers of QLB (Acalolepta aesthetica) caught in traps baited with solvent control, fuscumol, fuscumol acetate, geranylacetone, or a blend of the three compounds (experiment 2). There were no significant differences between the treatments and the solvent control (max-t test, p> 0.05).
Figure 1 in Response of Invasive Longhorn Beetles (Coleoptera: Lamiinae) to Known Cerambycid Aggregation-Sex Pheromones in the Puna District of Hawaii Island
Figure 1. Mean (± SE) numbers of QLB (Acalolepta aesthetica) caught in traps baited with solvent control, fuscumol acetate, or monochamol (experiment 1). There were no significant differences between the treatments and the solvent control (max-t test, p> 0.05).
Figure 4 in Response of Invasive Longhorn Beetles (Coleoptera: Lamiinae) to Known Cerambycid Aggregation-Sex Pheromones in the Puna District of Hawaii Island
Figure 4. Mean (± SE) numbers of PLB (Lagocheirus obsoletus) caught in traps baited with solvent control, fuscumol, fuscumol acetate, geranylacetone, or a blend of the three compounds (experiment 2). Means with an asterisk are significantly different than the solvent control (max-t test, p <0.05).
Conserved angio-immune subtypes of the cancer microenvironment predict response to immune checkpoint blockade therapy
<p>Immune checkpoint blockade (ICB) therapy has revolutionized cancer treatment. However, only a fraction of the patients respond to ICB therapy. Accurate prediction of patients to likely respond to ICB would maximize the efficacy of ICB therapy. The tumor microenvironment (TME) dictates tumor progression and therapy outcome. Here, we classify the TME by analyzing the transcriptome from 11,069 cancer patients based on angiogenesis and T-cell activity. We find three distinct angio-immune TME subtypes conserved across 30 non-hematological cancers. There is a clear inverse relationship between angiogenesis and anti-tumor immunity in TME. Remarkably, patients displaying TME with low angiogenesis with strong anti-tumor immunity show the most significant responses to ICB therapy in four cancers. Re-evaluation of the renal cell carcinoma clinical trials provides compelling evidence that the baseline angio-immune state is robustly predictive of ICB responses. This study offers a rationale for incorporating baseline angio-immune scores for future ICB treatment strategies.</p>
Fig. 13 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 13: The effect of hydrodynamics inside the Y-Cave, the location behind section B-B' (Fig. 2) at 5.5 m of depth, where the unusually coloured sediment sample was collected for analysis.
Fig. 12 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 12: Limestone tablets from the three representative sites after the 1-year exposure period: A) with bioaccumulation at site 1; B) corroded at site 3; C) abraded at site 6 (Fig. 3, Tab. 1).
Fig. 11 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 11: Cave features: A) stalactites in the chamber with the air pocket (section C-C'); B) submerged stalagmites and flowstones with a lack of marine cave biota (section C-C'); C) submerged scallops (asymmetrical, cuspate, oyster-shell-shaped dissolution depressions in the cave walls used as an indicator of flow direction; Murphy, 2012), (section D-D'); D) corroded cave walls (section F-F').
Fig. 5 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 5: The annual variation of temperature along the Y-Cave (from August 23–27, 2003 to July 4/October 8, 2004). Measurement positions are given in Fig. 3 and depths in Table 1.
Fig. 10 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 10: The mass (m.f.) and volume fractions (v.f.) of four sediment categories in the sediment sample collected behind section B-B' (Fig. 2), at 5.5 m of depth inside the Y-Cave; A) detrital terrigenous sediment>4 mm, B) mixed biogenic and terrigenous detritus, C) shells of gastropod Homalopoma sanguineum, D) other biogenic material – shells, tests and skeletons of other marine organisms.
Fig. 4 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 4: Living communities inside the Y-Cave: A) the entrance part of the cave, vertical wall, depth 9 m, biocenosis of semi-dark caves (GSO, see text for explanation of acronym) dominated by numerous sponge species; B) the entrance part of the cave, ceiling, depth 6 m, GSO dominated by scleractinian coral Leptopsammia pruvoti; C) the entrance part of the cave, overhang, depth 7 m, GSO dominated by scleractinian coral Madracis pharensis; D) the entrance part of the cave, vertical wall (near the bottom), depth 9 m, GSO, a large specimen of the orange sponge Agelas oroides dominates the photo; E) the middle part of the cave, in front of the section C-C', bottom, depth 10 m, a massive white specimen of the sponge Chondrosia reniformis; F) the middle part of the cave, between sections C-C' and D-D', vertical wall and overhang, depth 5 m, the transition from GSO to biocenosis of caves and ducts in total darkness (GO, see text for explanation of acronym), the community is dominated by serpulids; G) the middle part of the cave, between sections C-C' and D-D', vertical wall, depth 5 m, transition from GSO to GO, a dense population of brachiopod Novocrania anomala, encrusting sponge Placospongia decorticans and serpulids; H) the end part of the cave, near the section G-G', vertical wall with overhang and horizontal shelf, depth 6 m, GO with scarce calcareous sponges and serpulids (see Fig. 2 for position of the sections).
Fig. 1 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 1: The non-linear relationship between CO and Ca2+ con2 centrations in H 2O-CO2-CaCO3 solution. Each mixture (e.g. C) of the saturated solutions A and B lies on the straight line between them in the zone of undersaturation with respect to calcite, producing an aggressive solution that dissolves the surrounding carbonate (after Gabrovšek & Dreybrodt (2010)).
Fig. 8 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 8: Temperature, salinity and depth profiles recorded with the CTD probe during a dive inside the Y-Cave (August 27, 2003), 1 – vertical profile at the cave opening; 2 – vertical profile inside the cave entrance part; 3 – vertical profile at the turning point, section C-C'; 4 to 6 – vertical profiles in the inner part of the cave: 4 at approximately section E-E', 5 at approximately section G-G' and 6 at approximately section H-H'.
Fig. 3 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 3: The positions of temperature and light intensity data loggers inside the Y-Cave (dark circles - temperature data loggers; white circles - light intensity data loggers). Four loggers with their photosensitive cell facing upwards are marked with a black dot; the remaining cells were positioned to face the entrance of the cave.
Fig. 9 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 9: Variation of light intensity over a period of 11 days (June 19–30, 2006) at representative sites within the Y-Cave (Fig. 3): logger 1 – the entrance of the cave; logger 4 – the central part of the cave; logger 10 – the innermost part of the cave.
Fig. 6 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 6: The comparison of the tidal (solid line) and temperature (dashed line) fluctuation from February 2–8, 2004. Temperature records are from logger 4 (Fig. 3), and tides from the nearest tide gauge in Zadar port.
Fig. 7 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 7: Vertical temperature profiles inside and outside the YCave taken with the CTD probe (August 27, 2003); the profile labelled with a dotted line was taken at approximately section H-H', the profile labelled with a solid line at approximately section G-G'.
Fig. 2 in Biological response to geochemical and hydrological processes in a shallow submarine cave
Fig. 2: The location, cross-section and layout of the Y-Cave on Dugi Otok Island, Croatia, with characteristic profiles.
ChatGPT's responses to TUG-K 4.0 survey (October 2023)
<p>This dataset was created in October 2023, after the initial public release of ChatGPT vision. It contains 60 completed Test of Understanding Graphs in Kinematics 4.0 (TUG-K 4.0) surveys. The responses are sorted by item number. An analysis of the responses was published in <a href="https://doi.org/10.1103/PhysRevPhysEducRes.20.010109">https://doi.org/10.1103/PhysRevPhysEducRes.20.010109</a></p> <p>v2 of the dataset takes care of some accidentally duplicated responses present in v1. Because the analysis in the above cited paper used data directly out of the chatbot, the updates in no way impact the analysis or findings in the paper.</p>
Immunotherapy datasets associated with TimiGP-Response pan-cancer TIME landscape
<p>This version includes preprocessed single-cell RNA-seq data in the TimiGP-Response study.</p> <p>Please refer to https://github.com/CSkylarL/MSofTimiGP-Response for more information.</p> <p>Please cite our paper if you use this data: Li, C. et al. TimiGP-Response: the pan-cancer immune landscape associated with response to immunotherapy. bioRxiv, 2024.2006.2021.600089, doi:10.1101/2024.06.21.600089 (2024).</p> <p> </p> <p> </p>
FIG. 3 in Response of bryophytes to disturbances in managed forests. A case study from a Polish forest
FIG. 3. — Co-correspondence analysis biplot illustrating the ordination of most frequent bryophyte species colonizing ground in relation to the statistically significant environmental variables (n=75). Abbreviations: Age, forest age; DBH.max, maximal trees diameter at breast height; DW.vol, dead wood volume; L, Ellenberg indicator value (EIV) for light; T, EIV for temperature; F, EIV for moisture; R, EIV for pH; N, EIV for nitrogen; the first four letters of species indicate genus name, next four indicate species names and next four letters subspecies names.
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
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.