cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.25406218
title: Elsafty_RBCs_Slide_20

description: Each one of (Elsafty_RBCs_Slide_1-25) contains the field images/patches of a specific slide/patient. The names of the patches start with the respective slide/patient number, followed by the unique patch/field number. There is a total of 47,363 patches with 1076x535 pixels size from the 25 slides/patients, the counts of patches per slide/patient are as follows: 1690, 1709, 2697, 2400, 1905, 1803, 2964, 3049, 2464, 2080, 1894, 1852, 2590, 2263, 3328, 983, 1066, 935, 1131, 1237, 1874, 1393, 1277, 1199, and 1580.
DOI: 10.6084/m9.figshare.25403698.v1
title: The source data for graphs of Pre of Pre-Failure Operational Anomalies of the Kakhovka Dam Revealed by Satellite Data

description: Graph data for Figure 2 is from PlanetScope. Other raw data source are also concluded as follows:The Sentinel-2 and Landsat images used in this study are accessible at https://www.sentinel-hub.com/index.html. The PlanetScope images are obtained through https://www.planet.com/. The Sentinel-1 images were acquired from https://asf.alaska.edu/. The reservoir water levels can be found at https://ipad.fas.usda.gov/cropexplorer/global_reservoir/. The GloFAS-ERA5 river discharge reanalysis data are available at https://cds.climate.copernicus.eu/cdsapp#!/dataset/cems-glofas-historical?tab=overview.
DOI: 10.5281/zenodo.10823338
title: NCT05930912 Individual Participant Data

description: The data is composed of MRI & MRA results of the participant, data monitoring, and hematology result.
DOI: 10.5281/zenodo.10823339
title: NCT05930912 Individual Participant Data

description: The data is composed of MRI & MRA results of the participant, data monitoring, and hematology result.
DOI: 10.34622/datarepositorium/zt1uxk
title: Média Alternativos Digitais relacionados às Migrações e/ou pessoas racializadas - Mapeamento

description: Mapeamento dos média alternativos em Portugal associados a ativismos decoloniais. Desenvolvido no âmbito do projeto de investigação “Migrações, média e ativismos em língua portuguesa: descolonizar paisagens mediáticas e imaginar futuros alternativos” (PTDC/COM-CSS/3121/2021), acolhido pelo Centro de Estudos de Comunicação e Sociedade (CECS) da Universidade do Minho, em Portugal.
DOI: 10.34622/datarepositorium/rk4s4y
title: Base de Dados de Filmes de Moçambique e Portugal

description: O projeto “Memórias, culturas e identidades: o passado e o presente das relações interculturais em Moçambique e Portugal” (Cultures Past Present), teve como um de seus objetivos a análise de filmes portugueses e moçambicanos. Nesse contexto, foi elaborada a compilação dos dados dos filmes produzidos desde o início do cinema por ambos países, que abordam as relações entre Moçambique e Portugal ou que olham o passado colonial a partir de diversas perspetivas. Esta base de dados de filmes moçambicanos e portugueses está organizada cronologicamente, por filmes produzidos entre 1929 e 2019, incluindo informações sobre a realização, produção, duração, género e local onde decorre a ação de 165 filmes, longas e curtas-metragens.
DOI: 10.34622/datarepositorium/t49tkx
title: Ficheiro resultante do alinhamento de partes de vocabulários - Ciência da Computação

description: Ficheiro resultante do alinhamento de partes de vocabulários - Ciência da Computação.
DOI: 10.5281/zenodo.10823523
title: Skillful Seasonal Prediction of Wind Energy Resources in the contiguous United States

description: This dataset contains data files used to replicate figures in a paper published in communications earth & environment. These datasets are in .mat format, which can be readable by Matlab software.
DOI: 10.5281/zenodo.10823524
title: Skillful Seasonal Prediction of Wind Energy Resources in the contiguous United States

description: This dataset contains data files used to replicate figures in a paper published in communications earth & environment. These datasets are in .mat format, which can be readable by Matlab software.
DOI: 10.1594/pangaea.438932
title: Immobilisation dose rates for Weddell seals during expedition NEU2005
DOI: 10.1594/pangaea.718250
title: Seawater carbonate chemistry during a Ishigaki Island (Japan) coral reef seasonal observations, 2005

description: Monitoring seawater CO2 for a full year with seasonal observations of community metabolism in Ishigaki Island, Japan, revealed seasonal variation and anomalous values owing to the bleaching event in 1998. The daily average pCO2 showed a seasonal pattern on an annual scale, 280 to 320 ?atm in winter and 360 to 400 ?atm in summer, which was determined primarily by the seasonal change in seawater temperature. By contrast, the range in the diel variation in pCO2, 400 to 500 ?atm in summer 200 to 300 ?atm in winter, was attributed to the seasonal variation in community metabolism: Gross primary production (P g ) and respiration (R) were high in summer and low in winter. During the 1998 bleaching event, although P g and R increased, community excess organic production (E) decreased by three quarters compared with the same month in 1999, when the coral community showed high recovery. This change in metabolism led to large diel range and increased average value of pCO2 levels in the seawater on the reef flat. The decrease in the range and increase in the average value of pCO2 were observed by monitoring the Palau barrier reef flat, where overall mortality of corals occurred after the bleaching. All the metabolic parameters, P g , R, E and calcification (G) were reduced by half after the bleaching, which increased the average pCO2 value by 10 ?atm and decreased its diel range from 200-400 ?atm to 100-200 ?atm. Bleaching and resultant mortality of coral reefs led to degradation of their metabolic performance, and thus resulted in the loss of their active interaction with the carbon cycle.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI).
description: Supplement to: Kayanne, Hajime; Hata, Hiroshi; Kudo, Setsuko; Yamano, Hiroya; Watanabe, Atsushi; Ikeda, Yutaka; Nozaki, Ken; Kato, Ken; Negishi, Akira; Saito, Hiroshi (2005): Seasonal and bleaching-induced changes in coral reef metabolism and CO2 flux. Global Biogeochemical Cycles, 19, GB3015
DOI: 10.1594/pangaea.721997
title: Seawater carbonate chemistry and community calcification during a Molokai reef (Hawaii) study 2006

description: The severity of the impact of elevated atmospheric pCO2 to coral reef ecosystems depends, in part, on how seawater pCO2 affects the balance between calcification and dissolution of carbonate sediments. Presently, there are insufficient published data that relate concentrations of pCO2 and CO3 to in situ rates of reef calcification in natural settings to accurately predict the impact of elevated atmospheric pCO2 on calcification and dissolution processes. Rates of net calcification and dissolution, CO3 concentrations, and pCO2 were measured, in situ, on patch reefs, bare sand, and coral rubble on the Molokai reef flat in Hawaii. Rates of calcification ranged from 0.03 to 2.30 mmol CaCO3 m**-2 h**-1 and dissolution ranged from -0.05 to -3.3 mmol CaCO3 m**-2 h**-1. Calcification and dissolution varied diurnally with net calcification primarily occurring during the day and net dissolution occurring at night. These data were used to calculate threshold values for pCO2 and CO3 at which rates of calcification and dissolution are equivalent. Results indicate that calcification and dissolution are linearly correlated with both CO3 and pCO2. Threshold pCO2 and CO3 values for individual substrate types showed considerable variation. The average pCO2 threshold value for all substrate types was 654±195 µatm and ranged from 467 to 1003 µatm. The average CO3 threshold value was 152±24 µmol/kg, ranging from 113 to 184 µmol/kg. Ambient seawater measurements of pCO2 and CO3 indicate that CO3 and pCO2 threshold values for all substrate types were both exceeded, simultaneously, 13% of the time at present day atmospheric pCO2 concentrations. It is predicted that atmospheric pCO2 will exceed the average pCO2 threshold value for calcification and dissolution on the Molokai reef flat by the year 2100.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI).
DOI: 10.1594/pangaea.721761
title: Seawater carbonate chemistry and calcification during experiments with maerl beds, 2007

description: Maerl community respiration, photosynthesis and calcification were measured seasonally in the Bay of Brest (France). The dynamics of oxygen, carbon and carbonate fluxes at the water-sediment interface were assessed using benthic chambers. Community respiration (CR) fluctuated in accordance with the seasonal changes in water temperature, from 1.5 mmol C m**-2 h**-1 in winter to 8.7 mmol C m**-2 h**-1 in summer. Mean gross community production (GCP) varied significantly among seasons, according to incident irradiance and temperature, from 3.4 mmol C m**-2 h**-1 in winter to 12.7 mmol C m-2 h-1 in summer. Mean annual Pmax for the P-E curve was estimated to 13.3 mmol C m-2 h-1. Carbonate precipitation only occurred during light incubations and varied seasonally from 0.7 mmol CaCO3 m-2 h-1 in winter to 4.2 mmol CaCO3 m-2 h-1 in summer. Mean annual Pmax was 3.2 mmol CaCO3 m-2 h-1. Annual CR was estimated to 407.4 g C m**-2 yr**-1, and GCP, to 240.9 g C m**-2 yr**-1. Maerl communities are, therefore, heterotrophic systems (GCP:CR = 0.6), and are a source of CO2 for surrounding environments. In addition, CO2 released by calcification averaged 39.2 g C m**-2 yr**-1. Maerl community annual carbonate production was estimated to 486.7 g CaCO3 m**-2 yr**-1; they are therefore one of the most important carbonate producers in shallow coastal waters.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI).
description: Supplement to: Martin, Sophie; Clavier, Jacques; Chauvaud, Laurent; Thouzeau, Gérard (2007): Community metabolism in temperate maerl beds. I. Carbon and carbonate fluxes. Marine Ecology Progress Series, 335, 19-29
DOI: 10.1594/pangaea.739273
title: Pollen profile GOSCI187, Lake Gosciaz, Polen

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.741353
title: Lithology of sediment core GOSCI187, Lake Gosciaz, Polen

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.756649
title: Seawater carbonate chemistry in Hog reef, Bermuda reef community, 2010

description: Despite the potential impact of ocean acidification on ecosystems such as coral reefs, surprisingly, there is very limited field data on the relationships between calcification and seawater carbonate chemistry. In this study, contemporaneous in situ datasets of seawater carbonate chemistry and calcification rates from the high-latitude coral reef of Bermuda over annual timescales provide a framework for investigating the present and future potential impact of rising carbon dioxide (CO2) levels and ocean acidification on coral reef ecosystems in their natural environment. A strong correlation was found between the in situ rates of calcification for the major framework building coral species Diploria labyrinthiformis and the seasonal variability of [CO32-] and aragonite saturation state omega aragonite, rather than other environmental factors such as light and temperature. These field observations provide sufficient data to hypothesize that there is a seasonal "Carbonate Chemistry Coral Reef Ecosystem Feedback" (CREF hypothesis) between the primary components of the reef ecosystem (i.e., scleractinian hard corals and macroalgae) and seawater carbonate chemistry. In early summer, strong net autotrophy from benthic components of the reef system enhance [CO32-] and omega aragonite conditions, and rates of coral calcification due to the photosynthetic uptake of CO2. In late summer, rates of coral calcification are suppressed by release of CO2 from reef metabolism during a period of strong net heterotrophy. It is likely that this seasonal CREF mechanism is present in other tropical reefs although attenuated compared to high-latitude reefs such as Bermuda. Due to lower annual mean surface seawater [CO32-] and omega aragonite in Bermuda compared to tropical regions, we anticipate that Bermuda corals will experience seasonal periods of zero net calcification within the next decade at [CO32-] and omega aragonite thresholds of ~184 micro moles kg-1 and 2.65. However, net autotrophy of the reef during winter and spring (as part of the CREF hypothesis) may delay the onset of zero NEC or decalcification going forward by enhancing [CO32-] and omega aragonite. The Bermuda coral reef is one of the first responders to the negative impacts of ocean acidification, and we estimate that calcification rates for D. labyrinthiformis have declined by &gt;50% compared to pre-industrial times.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI).
DOI: 10.1594/pangaea.773608
title: Acoustic records of the underwater soundscape at PALAOA in 2007 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.770297
title: Acoustic records of the underwater soundscape at PALAOA in 2005 with links to audio stream files

description: See further details for setup of audio files. See doi:10.1594/PANGAEA.770298 for physical oceanography. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.772897
title: Acoustic records of the underwater soundscape at PALAOA in 2006 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.775743
title: Acoustic records of the underwater soundscape at PALAOA in 2010 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.774878
title: Acoustic records of the underwater soundscape at PALAOA in 2009 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.774290
title: Acoustic records of the underwater soundscape at PALAOA in 2008 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.807962
title: Acoustic records of the underwater soundscape at PALAOA in 2011 with links to audio stream files

description: See further details for setup of audio files. Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.821644
title: Metabolic costs of larval settlement and metamorphosis in the coral Seriatopora caliendrum under ambient and elevated pCO2

description: We tested the effects of pCO2 on Seriatopora caliendrum recruits over the first 5.3 d of post-settlement existence. In March 2011, 11-20 larvae were settled in glass vials (3.2 mL) and incubated at 24.0 °C and ~250 µmol quanta/m**2/s while supplied with seawater (at 1.4 mL/s) equilibrated with 51.6 Pa pCO2 (ambient) or 86.4 Pa pCO2. At 51.6 Pa pCO2, mean respiration 7 h post-settlement was 0.056 ± 0.007 nmol O2/recruit/min, but rose quickly to 0.095 ± 0.007 nmol O2/recruit/min at 3.3 d post-settlement, and thereafter declined to 0.075 ± 0.002 nmol O2/recruit/min at 5.3 d post-settlement (all ± SE). Elevated pCO2 depressed respiration of recruits by 19% after 3.3 d and 12% overall (i.e., integrated over 5.3 d), and while it had no effect on corallite area, elevated pCO2 was associated with weaker adhesion to the glass settlement surface and lower protein biomass. The unique costs of settlement and metamorphosis for S. caliendrum over 5.3 d are estimated to be 257 mJ/recruit at 51.6 Pa pCO2, which is less than the energy content of the larvae and recruits.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2013-10-10.
description: Supplement to: Edmunds, Peter J; Cumbo, Vivian R; Fan, Tung-Yung (2013): Metabolic costs of larval settlement and metamorphosis in the coral Seriatopora caliendrum under ambient and elevated pCO2. Journal of Experimental Marine Biology and Ecology, 443, 33-38
DOI: 10.1594/pangaea.833023
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE417
DOI: 10.1594/pangaea.844106
title: Acoustic records of the underwater soundscape at PALAOA in 2013 with links to audio stream files

description: Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.845083
title: Acoustic records of the underwater soundscape at PALAOA in 2012 with links to audio stream files

description: Warning! All files are very big (up to 2 GB). Do not open with your browser, use right click to save file to disk.
DOI: 10.1594/pangaea.914886
title: Seawater carbonate chemistry and resistance of corals and coralline algae to ocean acidification

description: Ocean acidification is a threat to the continued accretion of coral reefs, though some undergo daily fluctuations in pH exceeding declines predicted by 2100. We test whether exposure to greater pH variability enhances resistance to ocean acidification for the coral Goniopora sp. and coralline alga Hydrolithon reinboldii from two sites: one with low pH variability (less than 0.15 units daily; Shell Island) and a site with high pH variability (up to 1.4 pH units daily; Tallon Island). We grew populations of both species for more than 100 days under a combination of differing pH variability (high/low) and means (ambient pH 8.05/ocean acidification pH 7.65). Calcification rates of Goniopora sp. were unaffected by the examined variables. Calcification rates of H. reinboldii were significantly faster in Tallon than in Shell Island individuals, and Tallon Island individuals calcified faster in the high variability pH 8.05 treatment compared with all others. Geochemical proxies for carbonate chemistry within the calcifying fluid (cf) of both species indicated that only mean seawater pH influenced pHcf. pH treatments had no effect on proxies for Omega cf. These limited responses to extreme pH treatments demonstrate that some calcifying taxa may be capable of maintaining constant rates of calcification under ocean acidification by actively modifying Omega cf.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-04-16.
DOI: 10.1594/pangaea.917705
title: Seawater carbonate chemistry and respiration of blue crab Callinectes sapidus

description: Quantifying the physiological impact of environmental stressors on living organisms is critical to predicting the response of any given species to future climate scenarios. Oxygen consumption rates (μmol/g/min) were measured to examine the physiological response of the juvenile blue crab Callinectes sapidus from the Chesapeake Bay (Patuxent River, Maryland) to elevated temperature and dissolved carbon dioxide in water (pCO2) reflective of projected future climate scenarios. Treatment levels were selected to represent current conditions in the Chesapeake Bay (26°C and 800 μatm) and conditions predicted to occur by the year 2100 (31°C and 8,000 μatm). Crabs were exposed in a factorial design to these conditions throughout two successive molts (approximately 30 days). At the end of the exposure, the oxygen consumption rates of individual crabs were determined over at least a 10-h period using a flow-through respiration chamber equipped with optical oxygen electrodes. No significant effect of temperature or pCO2 on oxygen consumption was observed, suggesting the absence of a respiratory impact of these two climate stressors on juvenile blue crabs. Oxygen consumption rates were also determined for crabs that experienced a rapid increase in temperature without prior acclimation. The oxygen consumption rate of crabs may have acclimated to increased temperature during the 30-day exposure period before respiratory measurement. This potential acclimation, combined with high individual variability, and a relatively small difference in temperature treatments are likely the cause for the lack of a statistically significant difference in mean oxygen consumption rates by temperature in the core experiment. The results of this study suggest that the blue crab may be quite resilient to future climate stressors and underscore the need for species-specific studies to quantify the effects of climate change on estuarine crustaceans.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-05-6.