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60 results for “sound production”
Evolutionary novelties underlie sound production in baleen whales
<p>Experimental and modelling data from the paper "Evolutionary novelties underlie sound production in baleen whales." </p>
Fig. 3 in Sound production and pectoral spine locking in a Neotropical catfish (Iheringichthys labrosus, Pimelodidae)
Fig. 3. Sonogram (top) and oscillogram (below) swimbladder drumming sounds recorded underwater illustrating sound characteristics measured. TD = train durations; SD = sound duration; PP = pulse period; PD = pulse durations.
Fig. 1 in Sound production and pectoral spine locking in a Neotropical catfish (Iheringichthys labrosus, Pimelodidae)
Fig. 1. Sonogram (top) and oscillogram (below) of pectoral sounds illustrating sound characteristics measured. TD = train durations; SD = sound duration; PP = pulse period; PD = pulse durations.
Fig. 2 in Sound production and pectoral spine locking in a Neotropical catfish (Iheringichthys labrosus, Pimelodidae)
Fig. 2. Oscillogram of pectoral sound (all pulses in the oscillogram) emitted by Iheringichthys labrosus caught in the net in field.
DATASET Sound production mechanism in triggerfish (Balistidae): a synapomorphy
<p>Dataset corresponding to the article "Sound production mechanism in triggerfish (Balistidae): a synapomorphy". </p> <p>This dataset contains the sounds of three species of Balistidae : <em>Balistapus undulatus</em>, <em>Rhinecanthus aculeatus</em> and <em>Rhinecanthus rectangulus</em>.</p> <p>All the specimens are from Moorea Island (French Polynesia)<br> <em>B. undulatus</em> [standard length (SL) 10.59–15.35 cm]<br> <em>R. aculeatus</em> (SL: 12.7–17.4 cm) <br> <em>R. rectangulus</em> (SL: 8.1–15.3 cm) </p> <p>Specimens were recorded hand-held in a glass aquarium with a hydrophone HTI-96-MIN (sensitivity: −163.9dB V μPa−1; High Tech Inc., Long Beach, MS, USA) connected to a TASCAM DR-07 recorder (TEAC, Wiesbaden, Germany).<br> The sounds were digitized at 44.1 kHz (16-bit resolution).</p>
DATASET Unusual sound production mechanism in the triggerfish Rhinecanthus aculeatus (Balistidae)
<p>Dataset corresponding to the article "Unusual sound production mechanism in the triggerfish <em>Rhinecanthus aculeatus</em> (Balistidae) ". </p> <p>This dataset contains the sounds and results of morphological studies of <em>Rhinecanthus aculeatus</em></p> <p>Specimens were recorded hand-held in a glass aquarium with a hydrophone HTI-96-MIN (High Tech Inc., Long Beach, MS, USA) connected to a TASCAM DR-07 recorder (TEAC, Wiesbaden, Germany).<br> The sounds were digitized at 44.1 kHz (16-bit resolution).</p> <p>Contact: Xavier.Raick@uliege.be ; xavierraick@hotmail.com</p>
Figure 1 in Acoustic analysis of vocalization and the behavioral response associated to sound production of the nine banded armadillo Dasypus novemcinctus (Mammalia, Cingulata, Dasypodidae)
Figure 1. Oscillogram (top) and spectrogram (bottom) of the agonistic vocalizations of Dasypus novemcinctus, HCLP-S 1028, recorded from individual M1. (A) A single vocalization composed of the pattern A-I, A-I, B-I, B-II; (B) A single vocalization composed of the pattern A-I, A-II, B-I, A-II, B-I, B-II.
Figure 2. M1 in Acoustic analysis of vocalization and the behavioral response associated to sound production of the nine banded armadillo Dasypus novemcinctus (Mammalia, Cingulata, Dasypodidae)
Figure 2. M1 (marked with white tape at the middle of its moveable bands) Behavior (A) when cornered after being submitted to the presence of other male subject, (B) at a second moment, when the other animal approaches from its back, and then (C) M1 bends its body left to prevent the contact, with the other male scratching the basis of its tail. In (D) the other male bipedally projects its belly against M1's back, and the latter finally changes its position.
Apraxia of Speech: Comparison of EPG Treatment (Tx) and Sound Production Treatment (SPT)
ClinicalTrials.gov study NCT02554513. IPD Sharing: NO. Countries: 1. Publications: 1.
Crossett Experimental Forest site, station Unknown station at Crossett Experimental Forest, study of production of sound seeds by pines in units of numberPerHectare on a yearly timescale
The EcoTrends project was established in 2004 by Dr. Debra Peters (Jornada Basin LTER, USDA-ARS Jornada Experimental Range) and Dr. Ariel Lugo (Luquillo LTER, USDA-FS Luquillo Experimental Forest) to support the collection and analysis of long-term ecological datasets. The project is a large synthesis effort focused on improving the accessibility and use of long-term data. At present, there are ~50 state and federally funded research sites that are participating and contributing to the EcoTrends project, including all 26 Long-Term Ecological Research (LTER) sites and sites funded by the USDA Agriculture Research Service (ARS), USDA Forest Service, US Department of Energy, US Geological Survey (USGS) and numerous universities. Data from the EcoTrends project are available through an exploratory web portal (http://www.ecotrends.info). This web portal enables the continuation of data compilation and accessibility by users through an interactive web application. Ongoing data compilation is updated through both manual and automatic processing as part of the LTER Provenance Aware Synthesis Tracking Architecture (PASTA). The web portal is a collaboration between the Jornada LTER and the LTER Network Office. The following dataset from Crossett Experimental Forest (CRO) contains production of sound seeds by pines measurements in numberPerHectare units and were aggregated to a yearly timescale.
Crossett Experimental Forest site, station Unknown station at Crossett Experimental Forest, study of production of total seeds (sound and void) by pines in units of numberPerHectare on a yearly timescale
The EcoTrends project was established in 2004 by Dr. Debra Peters (Jornada Basin LTER, USDA-ARS Jornada Experimental Range) and Dr. Ariel Lugo (Luquillo LTER, USDA-FS Luquillo Experimental Forest) to support the collection and analysis of long-term ecological datasets. The project is a large synthesis effort focused on improving the accessibility and use of long-term data. At present, there are ~50 state and federally funded research sites that are participating and contributing to the EcoTrends project, including all 26 Long-Term Ecological Research (LTER) sites and sites funded by the USDA Agriculture Research Service (ARS), USDA Forest Service, US Department of Energy, US Geological Survey (USGS) and numerous universities. Data from the EcoTrends project are available through an exploratory web portal (http://www.ecotrends.info). This web portal enables the continuation of data compilation and accessibility by users through an interactive web application. Ongoing data compilation is updated through both manual and automatic processing as part of the LTER Provenance Aware Synthesis Tracking Architecture (PASTA). The web portal is a collaboration between the Jornada LTER and the LTER Network Office. The following dataset from Crossett Experimental Forest (CRO) contains production of total seeds (sound and void) by pines measurements in numberPerHectare units and were aggregated to a yearly timescale.
Fig. 4 in Audiospectrographical analysis of cicada sound production: a catalogue (Hemiptera, Cicadidae)
Fig. 4. Cumulative number of calling songs of different cicadas described through audiospectrographic analysis since 1948.
Figs 1 - 3. The three graphic representation s in Audiospectrographical analysis of cicada sound production: a catalogue (Hemiptera, Cicadidae)
Figs 1 - 3. The three graphic representation s of sound: the calling song of the PalaearcticspeciesCicadaon i Linnaeus 1758, 1: oscillogram (amplitude vs time). 2: spectrogram or sonagram (frequenc y vs time). 3: spectrum (amplitude vs frequency). Sound analysis software: SYNTANA T. Aubin CNRS U A 149 1 (Aubin 1994).
Data and derived products from airborne radar sounding survey over Devon Ice Cap, Canadian Arctic
<p>Data and derived products used in Rutishauser et al., “Radar sounding survey over Devon Ice Cap indicates the potential for a diverse hypersaline subglacial hydrological environment”, accepted for publication, The Cryosphere, <a href="https://doi.org/10.5194/tc-2021-220">https://doi.org/10.5194/tc-2021-220</a></p> <p>Corresponding author: <a href="mailto:rutishauser.anja@gmail.com">rutishauser.anja@gmail.com</a></p> <p> </p> <p><strong>Description of datasets:</strong></p> <p>------------------------------------------</p> <p><strong>2018_DIC_UTIG.IR2HI1B.kml</strong></p> <p>Geolocation of the SRH1 profile lines. Coordinates in EPSG: 4326 - WGS 84 (latitude, longitude)</p> <p>------------------------------------------</p> <p><strong>2018_DIC_UTIG.IR2HI1B.tgz</strong></p> <p>HiCARS 2 L1B echo strength profiles (radargrams) in NetCDF format. The naming of the files has the structure IR2HI1B_YYYYDOY_PST_x (e.g. IR2HI1B_2018153_DEV_JKB2t_Y87b_000.nc), where YYYY is the survey year (e.g. 2018), DOY is the survey day of the year (e.g. 153), PST is the profile name (e.g. DEV_JKB2t_Y87b), and x is the segment number if the profile was split in two (e.g. 000).</p> <p>For each profile, a PDF file showing the profile location and the radargram is included.</p> <p>------------------------------------------</p> <p><strong>2018_DIC_UTIG.Level2.tgz </strong></p> <p>Level 2 datasets for each profile, organized in the following folders:</p> <ul> <li><strong>2018_DIC_UTIG.ILUTP2:</strong> Laser altimeter geolocated surface elevation</li> <li><strong>2018_DIC_UTIG.IR2HI2:</strong> HiCARS 2 unfocused (pik1) geolocated ice thickness, ice surface elevation, bed elevation, surface- and bed reflection coefficients, and aircraft roll</li> <li><strong>2018_DIC_UTIG.IRHFOC2:</strong> HiCARS 2 focused (foc1) geolocated ice thickness, ice surface elevation, bed elevation, surface- and bed reflection coefficients, and aircraft roll</li> <li><strong>2018_DIC_UTIG.IRSPC2: </strong>HiCARS 2 derived basal interface specularity content</li> </ul> <p>------------------------------------------</p> <p><strong>Devon_basal_ice_temperature.tif: </strong>Modeled basal ice temperature [ºC] using a 1D advection diffusion model. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_bedrockDEM.tif: </strong>Digital elevation model (DEM) of the bedrock topography beneath Devon Ice Cap [m asl.]. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_gridded_RMSD_bedrock.tif</strong>: Root mean square deviation (RMDS) of the bedrock topography [m]. The RMSD was computed along each profile line, then interpolated on a 500x500m grid using the QGIS GDAL moving average grid interpolation. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_gridded_specularity.tif</strong>: Specularity content from along the profile lines interpolated on a 500x500m grid using the QGIS GDAL moving average grid interpolation. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_ice_thickness.tif</strong>: Gridded ice thickness [m] generated by subtracting the bedrock DEM from ice surface elevations derived from the ArcticDEM, Polar Geospatial Center from DigitalGlobe Inc. imagery. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_modeled_Geology.zip</strong></p> <ul> <li><strong>Devon_modeled_subglacial_geology.tif</strong>: Map of the projected geological units beneath Devon Ice Cap. The assigned numbers correspond to the following geological units: 1: pPe, 2: Cm-cf, 3: Oe, 4: Ocb, 5: Oct. Details on the geological units can be found in (Harrison et al., 2016; Mayr, 1980; Thorsteinsson & Mayr, 1987). 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> <li><strong>{pPe, Oe, Oct, Ocb,Cm_rb}_Model.stl</strong>: 3D geometry of the modeled geological units beneath Devon Ice Cap, originally published in (Rutishauser et al., 2018). Coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> <li><strong>Devon_load_geology_stl_files.py</strong><em>: </em>Python script to load and plot the 3D geology layers in the .stl files.</li> </ul> <p>------------------------------------------</p> <p><strong>Devon_subgl_hydraulic_head.tif</strong>: Subglacial hydraulic head [m] beneath Devon Ice Cap. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_subgl_hydraulic_slope.tif</strong></p> <p>Slope [º] of the subglacial hydraulic head beneath Devon Ice Cap. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</p> <p>------------------------------------------</p> <p><strong>Devon_subgl_lakes_brine_network.zip</strong></p> <ul> <li><strong>Devon_subgl_lake_outline.shp</strong>: Shoreline of the subglacial lakes beneath Devon Ice Cap (identified in this study). Coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> <li><strong>Devon_brine_network_outline.shp</strong>: Outlines of the mapped subglacial brine network beneath Devon Ice Cap. Coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> </ul> <p>------------------------------------------</p> <p><strong>Devon_subgl_water_routes.zip</strong></p> <ul> <li><strong>Devon_modeled_subgl_water_routes_{1, 2, 3}std.tif</strong>: Modeled subglacial water routes derived via application of a flow accumulation algorithm to the hydraulic head. The model is run 1000 times with normally distributed random errors of 1, 2 and 3 standard deviations of the hydraulic head uncertainty added to the hydraulic head (represented in the file name). Pixel values represent the model counts for which the cell has a minimum of 10 upstream cells draining into it. 500 m grid cell size, coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> <li><strong>Devon_extracted_subgl_water_routes.shp</strong>: Modeled subglacial water routes derived via the application of a flow accumulation algorithm to the hydraulic head. Coordinates in EPSG: 32617 - WGS 84 / UTM zone 17N.</li> </ul> <p>------------------------------------------</p> <p><strong>SpecularityJustification.zip</strong></p> <p>Jupyter notebook and example datafile to show the justification for the chosen specularity threshold of 0.4 for declaring a detection of possible subglacial water.</p> <p>------------------------------------------</p> <p> </p> <p><strong>Acknowledgments</strong></p> <p>The aerogeophysical survey and subsequent standard data processing were funded by the Weston Family Foundation. We also thank the G. Unger Vetlesen Foundation and the UTIG Postdoctoral Fellowship program who provided further funding for data analysis. M.L.S. was partially supported by NASA NNX16AJ64G and NASA 80NSSC20K1134. We thank PCSP and Kenn Borek Air Ltd. for logistical support, and the Nunavut Research Institute and the peoples of Grise Fjord and Resolute Bay for permission to conduct airborne surveys over Devon Ice Cap. Finally, we thank Scott Kempf for assistance with data processing, and Sam Christian and Miguel Liu-Schiaffini for help with radar reflection picking.</p> <p><strong>References</strong></p> <p>Harrison, J. C., Lynds, T., Ford, A., & Rainbird, R. H. (2016). Geology, simplified tectonic assemblage map of the Canadian Arctic Islands, Northwest Territories - Nunavut. <em>Geological Survey of Canada, Canadian Geoscience</em>, <em>Map 80</em>. https://doi.org/10.4095/297416</p> <p>Mayr, U. (1980). Stratigraphy and correlation of lower Paleozoic formations, subsurface of Bathurst Island and adjacent smaller islands, Canadian Arctic Archipelago. <em>Geological Survey of Canada, Bulletin</em>, <em>306</em>. https://doi.org/10.4095/102157</p> <p>Rutishauser, A., Blankenship, D. D., Sharp, M., Skidmore, M. L., Greenbaum, J. S., Grima, C., Schroeder, D. M., Dowdeswell, J. A., & Young, D. A. (2018). Discovery of a hypersaline subglacial lake complex beneath Devon Ice Cap, Canadian Arctic. <em>Science Advances</em>, <em>4</em>(4), eaar4353. https://doi.org/10.1126/sciadv.aar4353</p> <p>Thorsteinsson, R., & Mayr, U. (1987). <em>The sedimentary rocks of Devon island, canadian arctic archipelago</em>. https://doi.org/10.4095/122451</p>
FIGURE 14 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 14. Example of three syntopic Hetrodini species (Rau Forest, from left: Spalacomimus talpa, Enyaliopsis ephippiatus, Eugasteroides loricatus) and Spalacomimus stettinensis (second from right), occurring nearby (all 1 Nov 2021).
FIGURE 12 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 12. Examples of chromosome number and heterochromatin C-banding of mitotic male (A–C, G–K) and mitotic female complements (D), as well as diplotene/diakinesis (C, E, I on the right), and metaphase I (F) for the following Hetrodini taxa: A Cosmoderus femoralis, 2n = 24 + X0 (CH8626), B Enyaliopsis bloyeti, 2n = 28 + X0 (HE114), C Enyaliopsis carolinus, 2n =24 + neo-XY (CH8625), D Enyaliopsis ephippiatus, 2n = 26 + XX (female CH7849), E Enyaliopsis jennae, 2n = 26 + neo-XY (HE87), F Enyaliopsis spec. 2 Mpwapwa, 2n = 26 + X0 (CH8353), G Gymnoproctus rammei, 2n = 26 + X0 (CH8763), H Gymnoproctus spec., 2n = 26 + X0 (CH7953), I Spalacomimus magnus, 2n = 16 + X0 (CH7945), J Spalacomimus verruciferus, 2n = 22 + neo-XY (CH7897), K Spalacomimus spec. near verruciferus, 2n = 22 + neo-XY (CH7899). Bi-armed chromosomes (meta/submeta/subacrocentric) are marked with numbers (A, C, D, F–I); in the neo-XY system, sex chromosomes form association in diplotene (C) and metaphase I (I); arrowheads indicate interstitial C-bands in 1 (A, E, J, K) and 2 (I) pairs; asterisks (*) marked distal C-bands in 3, 4, 5 (C), 3, 4 (D), 2-heteromorphic (G, H) pair; X = neo-X and Y = neo-Y sex chromosomes. Scale bar = 10 µm.
FIGURE 9 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 9. Titillator and genitalic sclerites in Hetrodini, Enyaliopsina. First row A Cosmoderus femoralis (CH8627), B Enyaliopsis bloyeti (Kazimzumbwi), C Enyaliopsis carolinus (Minziro), D Enyaliopsis ephippiatus (Rau Forest); second row E Enyaliopsis spec. 1 near ephippiatus (Mwala), F Enyaliopsis jennae (Uluguru), G Enyaliopsis spec. 2 (Mpwapwa), H Enyaliopsis spec. 3 (East Chenene); third row I Gymnoproctus rammei (Puge Simbo), J Gymnoproctus spec. (East Chenene).
FIGURE 10 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 10. Oscillograms of the calling songs in the genera Eugaster, Eugasteroides and Spalacomimus (figures of S. liberianus based on figures and data from literature; see text). A Eugaster guyoni, B Eugaster spinulosa, C Eugasteroides loricatus, D Spalacomimus liberianus, E Spalacomimus magnus, F Spalacomimus stettinensis, G Spalacomimus talpa, H Spalacomimus verruciferus, I Spalacomimus spec. near verruciferus.
FIGURE 8 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 8. Oscillograms of the calling songs in the genera Cosmoderus and Enyaliopsis (figures of E. iaculator based on figures and data from literature; see text). A Cosmoderus femoratus, B Enyaliopsis bloyeti. C Enyaliopsis carolinus, D Enyaliopsis ephippiatus, song type A, E Enyaliopsis spec. 1 (near ephippiatus), song type B, F Enyaliopsis iaculator, G Enyaliopsis jennae, H Enyaliopsis spec. 2 Mpwapwa. Left column overview (5-s-section), right column detail (250-ms-section).
FIGURE 11 in Review of song patterns and sound production in armoured ground crickets (Orthoptera: Tettigoniidae: Hetrodini) with karyological data and taxonomic notes
FIGURE 11. Titillators in the genus Spalacomimus. A S. magnus (Gulwe), B S. stettinensis (Lambo Estate), C S. stettinensis (neotype), D S. talpa (Lembeni), E S. verruciferus (Lake Chala), F S. spec. near verruciferus (Lossogonoi).
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