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FIGURE 2 in A new species, Cricotopus cataractaenostocicola, living in a cyanobacterial colony on vertical rocky substrates with trickling water film in Japan (Diptera: Chironomidae)
FIGURE 2. Landscapes of the habitats of the Nostoc colonies symbiotic with chironomids. Information on the sites is listed in Table 1.
FIGURE 4 in A new species, Cricotopus cataractaenostocicola, living in a cyanobacterial colony on vertical rocky substrates with trickling water film in Japan (Diptera: Chironomidae)
FIGURE 4. Cricotopus cataractaenostocicola sp. nov. Adult male (A–G'), A: general appearance, B: antenna, C: thorax, D: hypopygium, E: eye, F: thorax and head, G, G', and G": right wing. Adult female (H–L), H and H': general appearance, I: head, J and J': genitalia, K: antenna. Abbreviations (adult). Al: alula; An: anal vein; Ap: anal point; Ce: cercus; Clw: craw, Cp: cibarial pump; Dc: dorsocentrals; Gc: gonocoxite; Gs: gonostylus; Hl: halter; Ivo: inferior volsella; La: labrum; Pm: palpal segments; Po: Postnotum; Sct: scutelium; Scu: scutum; Sq: squama.
FIGURE 3 in A new species, Cricotopus cataractaenostocicola, living in a cyanobacterial colony on vertical rocky substrates with trickling water film in Japan (Diptera: Chironomidae)
FIGURE 3. Phylogeny based on the COI dataset. Information on the sequences used for this analysis is shown in Table 2.
FIGURE. Dothiorella viticola on dead branch of Morus sp. (MFLU 19-0621). a, b. Conidiomata on host substrate. c. Vertical section through conidioma. d. Ostiole. e. Peridium of conidioma. f–j. Conidia attached to conidiogenous cells. k–m. Conidia. n. Germinating conidium. o, p. Colony on PDA (o upper, p lower). Scale bars: a = 1 mm, b = 100 μm, c = 50 μm, d = 20 μm, e–n = 10 μm. in Two new species of Botryosphaeriaceae (Botryosphaeriales) and new host/ geographical records
FIGURE. Dothiorella viticola on dead branch of Morus sp. (MFLU 19-0621). a, b. Conidiomata on host substrate. c. Vertical section through conidioma. d. Ostiole. e. Peridium of conidioma. f–j. Conidia attached to conidiogenous cells. k–m. Conidia. n. Germinating conidium. o, p. Colony on PDA (o upper, p lower). Scale bars: a = 1 mm, b = 100 μm, c = 50 μm, d = 20 μm, e–n = 10 μm.
Figure 5 in Vertical distribution of brown and red macroalgae along the central Western Antarctic Peninsula
Figure 5: Vertical distribution of seven additional red macroalgal species by the number of transects in which they were present in the diver by-hand collections. Other details as in Figure 4.
Figure 4 in Vertical distribution of brown and red macroalgae along the central Western Antarctic Peninsula
Figure 4: Vertical distribution of seven red macroalgal species by the number of transects in which they were present in the diver byhand collections. Sites are ordered by National Ice Center average sea ice concentrations from 2014 to 2019. No fleshy red macroalgae were present at site K, and none of the species included in this report were present at site N. Only two transects were sampled at site I, so the abscissa only extends to two for that site. Single blue asterisks indicate one less transect collection at that depth at that site; "(present)" indicates that the species was found in general collections at the site but was not present in the transect collections.
Figure 3 in Vertical distribution of brown and red macroalgae along the central Western Antarctic Peninsula
Figure 3: Vertical distribution of Desmarestia menziesii and Desmarestia anceps combined and of Himantothallus grandifolius at horizontal depth intervals from video transect analyses. Means + standard error of mean. Sample size was two at sites H, I, and K and three at all other sites. Sites are ordered by National Ice Center average sea ice concentrations from 2014 to 2019. No fleshy macroalgae were present at site K so it is not included. "(present)" indicates that the species was found in general collections at the site but was not present under a random dot in the video analyses.
Figure 2 in Vertical distribution of brown and red macroalgae along the central Western Antarctic Peninsula
Figure 2: Vertical distribution of brown macroalgal species by the number of transects in which they were present in the diver byhand collections. Sites are ordered by National Ice Center average sea ice concentrations from 2014 to 2019. No fleshy macroalgae were present at site K so it is not included. Only two transects were sampled at site I, so the abscissa only extends to two for that site. Single blue asterisks indicate one less transect collection at that depth at that site, two asterisks indicate two less; "(present)" indicates that the species was found in general collections at the site but was not present in the transect collections.
Figure 1 in Vertical distribution of brown and red macroalgae along the central Western Antarctic Peninsula
Figure 1: Study sites along the central Western Antarctic Peninsula. Inset shows the entire northern and central portions of the Antarctic Peninsula. The 14 research sites, designated north to south as A through N, were surveyed between April 23 and May 18, 2019. Their locations spanned the range of annual sea ice coverage (color scale bar). Modified from Amsler et al. (2023).
Supplementary Data from manuscript entitled: Cloud processing dominates the vertical aerosol profiles in marine air masses over the Great Barrier Reef
<p>The data used in the manuscript "Cloud processing dominates the vertical aerosol profiles in marine air masses over the Great Barrier Reef" is available. It contains information from different instruments on board the research aircraft. The manuscript describes the instrumentation details. There is a read_me file in each folder with further information.</p>
Temporal variation in counterclockwise vertical-axis block rotations across a rift overlap zone, southwestern Ethiopia, East Africa
Open the record for dataset details and reuse information.
Solutal convection in 3D porous media - Horizontal and vertical concentration distributions over time at Rayleigh number 10000.
<p>Solutal convection in 3D porous media - Horizontal and vertical concentration distributions over time at Rayleigh number 10000. </p> <p> </p>
MOM6 Model Output from "Improved Upper Ocean Vertical Mixing in the Equatorial Oceans in NOAA/GFDL's OM4 Model"
<p>Datasets produced during the MOM6 experiments described by "Improved Upper Ocean Vertical Mixing in the Equatorial Oceans in NOAA/GFDL's OM4 Model".</p> <p>These datasets are needed to reproduce the figures in the version of this manuscript as submitted to ESS.</p> <p>The location of the notebooks for creating figures from these datasets is indicated in the manuscript.</p>
Data for "Identifying and quantifying unexpected deep zooplankton diel vertical migration in a large deep lake (Lake Geneva)"
<p>The repository contains the data for the paper "Identifying and quantifying unexpected deep zooplankton diel vertical migration in a large deep lake (Lake Geneva)", submitted to Limnology & Oceanography. </p>
Dataset microbial counts and sequencing of BSF larvae to assess vertical transmission of E. coli
<p>Sequencing data available from <a href="https://www.ncbi.nlm.nih.gov/bioproject/?term=PRJNA1068952" target="_blank" rel="noopener">BioProject PRJNA1068952</a></p>
Supplementary material 1 from: de Oliveira Dias C, de Araujo AV, Bonecker SLC (2018) Vertical distribution and structure of copepod (Arthropoda: Copepoda) assemblages in two different seasons down to 1,200 m in the tropical Southwestern Atlantic. Zoologia 35: 1-11. https://doi.org/10.3897/zoologia.35.e13886
Table S1. Vertical distributions of the mean, standard deviation (SD), relative abundance (RA), and occurrence frequency (OF) of the copepod species found in Campos Basin, during the rainy season. :
Supplementary material 2 from: de Oliveira Dias C, de Araujo AV, Bonecker SLC (2018) Vertical distribution and structure of copepod (Arthropoda: Copepoda) assemblages in two different seasons down to 1,200 m in the tropical Southwestern Atlantic. Zoologia 35: 1-11. https://doi.org/10.3897/zoologia.35.e13886
Table S2. Vertical distributions of the mean, standard deviation (SD), relative abundance (RA), and occurrence frequency (OF) of the copepod species found in Campos Basin, during the dry season. :
The role of ground type, moisture and temperature on the vertical growth of lichens: A test of hypotheses with paramo lichens
<p>There is little reliable information about determinants of vertical growth in terricolous lichens, traditionally divided into short "crustose", intermediate "foliose" and tall "fruticose" growth forms, a practice that artificially hides a growth continuum. Substrate, temperature and especially water are thought to affect, but such factors are hard to measure, because, for example, the water actually available to lichens does not match rainfall patterns or even over ground levels. To reliably assess the effect of those factors, I recorded the temperature, moisture and substrate in and under individual lichen colonies in 415 fixed PVC frame quadrats (Cerro de la Muerte, Costa Rica, 9°33'N; 83°45'W), on April, August, October and December of 2015. The measurements are more reliable because they were taken inside the colonies themselves (rather than on the general environment), because they covered hundreds of cases during a year, and because they are from the relatively simple paramo habitat, where animals or vegetation have less impact on lichens than in lower ecosystems. The hypotheses were that lichens would grow taller on softer, warmer and moister ground, on the moister Caribbean versant and on the moister part of the year. Results matched the hypotheses, with one exception: lichens on soft ground were not taller than those on rock. Caribbean colonies were, on the average, 7 cm taller than those on the drier Pacific versant. Foliose, fruticose and crustose lichens were equally frequent as dominant in the quadrats. Crustose species, together with their bacterial and microinvertebrate communities, with suffer the most with global warming.</p>
The role of ground type, moisture and temperature on the vertical growth of lichens: A test of hypotheses with paramo lichens
<p>There is little reliable information about determinants of vertical growth in terricolous lichens, traditionally divided into short "crustose", intermediate "foliose" and tall "fruticose" growth forms, a practice that artificially hides a growth continuum. Substrate, temperature and especially water are thought to affect, but such factors are hard to measure, because, for example, the water actually available to lichens does not match rainfall patterns or even over ground levels. To reliably assess the effect of those factors, I recorded the temperature, moisture and substrate in and under individual lichen colonies in 415 fixed PVC frame quadrats (Cerro de la Muerte, Costa Rica, 9°33'N; 83°45'W), on April, August, October and December of 2015. The measurements are more reliable because they were taken inside the colonies themselves (rather than on the general environment), because they covered hundreds of cases during a year, and because they are from the relatively simple paramo habitat, where animals or vegetation have less impact on lichens than in lower ecosystems. The hypotheses were that lichens would grow taller on softer, warmer and moister ground, on the moister Caribbean versant and on the moister part of the year. Results matched the hypotheses, with one exception: lichens on soft ground were not taller than those on rock. Caribbean colonies were, on the average, 7 cm taller than those on the drier Pacific versant. Foliose, fruticose and crustose lichens were equally frequent as dominant in the quadrats. Crustose species, together with their bacterial and microinvertebrate communities, with suffer the most with global warming.</p>
Mediterranean Sea Climatic Indices - T/S Vertical Averages
<p>Climatic indices for the Mediterranean Sea (6.25W-36.5E, 30N-46N) from 1950 to 2015. The file<br> "Med_Climatic_Indices_VerticalAverages.tar.gz" contains : a) an ascii file named "inventory_VerticalAverages.txt" which lists all the available indices, and b) a directory named "VerticalAverages" with the indices under the following structure:</p> <ul> <li>VerticalAverages/Annual_Decadal/Variable_decade_allmonths_z1z2.nc</li> <li>VerticalAverages/Seasonal_Decadal/ Variable_decade_season_z1z2.nc</li> </ul> <p>The Variable naming is:</p> <ul> <li>Tanomvavg: Vertically averaged temperature anomaly</li> <li>Sanomvavg: Vertically averaged salinity anomaly</li> </ul> <p>Other naming:</p> <ul> <li>allmonths: 0112 (all months from January to December)</li> <li>season: 0103 for winter, 0406 for spring, 0709for summer, 1012 for autumn</li> <li>decade: 19501959 to 20062015</li> <li>z1z2: vertical layer between z1 and z2 depths</li> </ul> <p>Example:</p> <ul> <li>Tanomvavg_20062015_1012_6004000.nc, is the autumn vertically averaged temperature anomaly, for the decade 2006-2015, between 600 and 4000 m</li> </ul>
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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.