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446 results for “Water body”
Fig. 1 in Water level influences on body condition of Geophagus brasiliensis (Perciformes: Cichlidae) in a Brazilian oligotrophic reservoir
Fig. 1. Means and standard errors (vertical lines) for condition (K) by sex and size classes for Geophagus brasiliensis in the Lajes Reservoir. Between-sex significant differences: * p <0.05; ** p <0.01.
Fig. 4 in Water level influences on body condition of Geophagus brasiliensis (Perciformes: Cichlidae) in a Brazilian oligotrophic reservoir
Fig. 4. Means and standard errors (vertical lines) for gonadosomatic index (GSI) by sex and water level periods for Geophagus brasiliensis in the Lajes Reservoir. Distinct letters (a, b, c) indicate significant differences at 95% level of confidence.
Body temperature, evaporative water loss and resting metabolic rate data for six southern African bats
<p><span>1. The microsites that animals occupy during the rest phase of their circadian activity cycle influence their physiology and behaviour, but relatively few studies have examined correlations between interspecific variation in thermal physiology and roost microclimate. Among bats, there is some evidence</span> that species exposed to high roost temperatures (<i>T<sub>roost</sub></i>) possess greater heat tolerance and evaporative cooling capacity, but<span> the small number of species for which both thermal physiology and roost microclimate data exist mean that the generality of this pattern remains unclear. </span></p> <p>2. Here, we test the hypothesis that bat heat tolerance and evaporative cooling capacity have co-evolved with roost preferences. We predicted that species occupying roosts poorly buffered from high outside environmental temperature exhibit higher heat tolerance and evaporative cooling capacity compared to species inhabiting buffered roosts in which <i>T<sub>roost</sub></i> remains well below outside conditions.</p> <p>3. We used flow-through respirometry to investigate thermoregulation at air temperatures (<i>T</i><sub>a</sub>) approaching and exceeding normothermic body temperature (<i>T</i><sub>b</sub>) among six <span>species with broadly similar body mass but differing in roost microclimate (hot <i>versus</i> cool roosts). We combined these data with empirical measurements of <i>T</i><sub>roost</sub> for each study population.</span></p> <p>4. Hot-roosting species tolerated <i>T</i><sub>a</sub> ~4 °C higher than cool-roosting bats before the onset of loss of coordinated locomotion and non-regulated hyperthermia. The evaporative scope [i.e., ratio of maximum evaporative water loss (EWL) to minimum thermoneutral EWL] of hot-roosting species (<span><span>16.1 </span></span>± 2.4) was substantially higher than that of cool-roosting species (<span><span>5.9 </span></span>± 2.4). Maximum evaporative cooling capacities (i.e., evaporative heat loss / metabolic heat production) of <span><span>hot-roosting species were > 2, while the corresponding values for cool-roosting species were ≤1. </span></span></p> <p>5. The greater heat tolerance and higher evaporative cooling capacity of hot-roosting species compared with those occupying cooler roosts reveal variation in bat evaporative cooling capacity correlated with roost microclimate, supporting the hypothesis that thermal physiology has co-evolved with roost preference.</p>
Fig. 2. The 13C in Structural investigation and comparative cytotoxic activity of water-soluble polysaccharides from fruit bodies of the medicinal fungus quinine conk
Fig. 2. The 13C NMR spectrum of β-glucan FoCA.
Using Electrical Bioimpedance Assessments to Estimate Perioperative Total Body Water and Postoperative Fluid Need
ClinicalTrials.gov study NCT02200055. IPD Sharing: NO. Countries: 1. Publications: 0.
Changes in Body Water During Surgery
ClinicalTrials.gov study NCT05272540. IPD Sharing: NO. Countries: 0. Publications: 1.
Body temperature, evaporative water loss and resting metabolic rate data for six southern African bats
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Is zooplankton body size an indicator of water quality in (sub)tropical reservoirs in China?
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Data from: Palaeoecological implications of the preservation potential of soft-bodied organisms in sediment-density flows: testing turbulent waters
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Data from: An experimental evolution study confirms that discontinuous gas exchange does not contribute to body water conservation in locusts
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High blood parasite infection rate and low fitness suggest ecological traps for pied flycatchers breeding near forest water-bodies
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Data from: Fruit consumption in migratory passerines is limited by water ingestion rather than by body water balance
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Non-biodegradable objects may boost microbial growth in water bodies by harnessing bubbles
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Assessing environmental DNA metabarcoding and camera trap surveys as complementary tools for biomonitoring of remote desert water bodies
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ASTER Global Water Bodies Database Attributes NetCDF V001
The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Water Bodies Database (ASTWBD) Version 1 data product provides global coverage of water bodies larger than 0.2 square kilometers at a spatial resolution of 1 arc second (approximately 30 meters) at the equator, along with associated elevation information. The ASTWBD data product was created in conjunction with the ASTER Global Digital Elevation Model (ASTER GDEM) Version 3 data product by the Sensor Information Laboratory Corporation (SILC) in Tokyo. The ASTER GDEM Version 3 data product was generated using [ASTER Level 1A](https://doi.org/10.5067/ASTER/AST_L1A.003) scenes acquired between March 1, 2000, and November 30, 2013. The ASTWBD data product was then generated to correct elevation values of water body surfaces.To generate the ASTWBD data product, water bodies were separated from land areas and then classified into three categories: ocean, river, or lake. Oceans and lakes have a flattened, constant elevation value. The effects of sea ice were manually removed from areas classified as oceans to better delineate ocean shorelines in high latitude areas. For lake water bodies, the elevation for each lake was calculated from the perimeter elevation data using the mosaic image that covers the entire area of the lake. Rivers presented a unique challenge given that their elevations gradually step down from upstream to downstream; therefore, visual inspection and other manual detection methods were required. The geographic coverage of the ASTWBD extends from 83°N to 83°S. Each tile is distributed in GeoTIFF format and referenced to the 1984 World Geodetic System (WGS84)/1996 Earth Gravitational Model (EGM96) geoid. Each data product is provided as a zipped file that contains an attribute file with the water body classification information and a DEM file, which provides elevation information in meters.
Location and Permanency of Water Bodies in the African Sahel Region from 2003-2011
This data set provides an estimate of the spatial and temporal extent of surface water at 250-m resolution over nine years (2003-2011) for the African Sahel region (10-20 degrees N) using imagery from the Moderate-resolution Imaging Spectroradiometer (MODIS). Water bodies were identified by a spectral analysis of MODIS vegetation indices with the aim to improve existing regional to global mapping products. This data set can be used to enhance the understanding of Earth system processes, and to support global change studies, agricultural planning, and disease prevention. These data provide a gridded (250-m) estimate of the number of years (during 2003-2011) that a pixel was covered by water. The data are presented in a single netCDF (*.nc) file.
ASTER Global Water Bodies Database V001
The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Water Bodies Database (ASTWBD) Version 1 data product provides global coverage of water bodies larger than 0.2 square kilometers at a spatial resolution of 1 arc second (approximately 30 meters) at the equator, along with associated elevation information. The ASTWBD data product was created in conjunction with the ASTER Global Digital Elevation Model (ASTER GDEM) Version 3 data product by the Sensor Information Laboratory Corporation (SILC) in Tokyo. The ASTER GDEM Version 3 data product was generated using [ASTER Level 1A](https://doi.org/10.5067/ASTER/AST_L1A.003) scenes acquired between March 1, 2000, and November 30, 2013. The ASTWBD data product was then generated to correct elevation values of water body surfaces.To generate the ASTWBD data product, water bodies were separated from land areas and then classified into three categories: ocean, river, or lake. Oceans and lakes have a flattened, constant elevation value. The effects of sea ice were manually removed from areas classified as oceans to better delineate ocean shorelines in high latitude areas. For lake water bodies, the elevation for each lake was calculated from the perimeter elevation data using the mosaic image that covers the entire area of the lake. Rivers presented a unique challenge given that their elevations gradually step down from upstream to downstream; therefore, visual inspection and other manual detection methods were required. The geographic coverage of the ASTWBD extends from 83°N to 83°S. Each tile is distributed in GeoTIFF format and referenced to the 1984 World Geodetic System (WGS84)/1996 Earth Gravitational Model (EGM96) geoid. Each data product is provided as a zipped file that contains an attribute file with the water body classification information and a DEM file, which provides elevation information in meters.
ASTER Global Water Bodies Database NetCDF V001
The Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Water Bodies Database (ASTWBD) Version 1 data product provides global coverage of water bodies larger than 0.2 square kilometers at a spatial resolution of 1 arc second (approximately 30 meters) at the equator, along with associated elevation information. The ASTWBD data product was created in conjunction with the ASTER Global Digital Elevation Model (ASTER GDEM) Version 3 data product by the Sensor Information Laboratory Corporation (SILC) in Tokyo. The ASTER GDEM Version 3 data product was generated using [ASTER Level 1A](https://doi.org/10.5067/ASTER/AST_L1A.003) scenes acquired between March 1, 2000, and November 30, 2013. The ASTWBD data product was then generated to correct elevation values of water body surfaces.To generate the ASTWBD data product, water bodies were separated from land areas and then classified into three categories: ocean, river, or lake. Oceans and lakes have a flattened, constant elevation value. The effects of sea ice were manually removed from areas classified as oceans to better delineate ocean shorelines in high latitude areas. For lake water bodies, the elevation for each lake was calculated from the perimeter elevation data using the mosaic image that covers the entire area of the lake. Rivers presented a unique challenge given that their elevations gradually step down from upstream to downstream; therefore, visual inspection and other manual detection methods were required. The geographic coverage of the ASTWBD extends from 83°N to 83°S. Each tile is distributed in GeoTIFF format and referenced to the 1984 World Geodetic System (WGS84)/1996 Earth Gravitational Model (EGM96) geoid. Each data product is provided as a zipped file that contains an attribute file with the water body classification information and a DEM file, which provides elevation information in meters.
Data files used in the paper " Multiple subglacial water bodies below the south pole of Mars unveiled by new MARSIS data "
<pre>Each file corresponds to a MARSIS radar acquisition on the Ultima Scopuli on Mars. The Data are in ASCII format and they organized as a follow: first row: operating frequency in MHz second row: longitude in degree third row: latitude in degree forth row: spacecraft height from fifth row to the end row: amplitude radar signal The name of the file corresponds to name of the MARSIS orbit</pre>
The drivers of anguillid eel movement in lentic water bodies: a systematic map - search engine results
<p>A total of 7 RIS files.</p> <p>Three RIS files from three web searches (Scholar, SCOPUS, and Web of Science) conducted for the review "The drivers of anguillid eel movement in lentic water bodies: a systematic map" currently submitted for publication at Reviews ins Fish Biology and Fisheries.</p> <p>RIS file of the combined search data conducted in Zotero</p> <p>RIS of the results from backward citation chasing.</p> <p>RIS file of the results from forward citation chasing.</p> <p>RIS file of the combined results from onward and backward citation chasing.</p>
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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.