cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.d7xb2z
title: Occurrence Download

description: A dataset listing the 5 species recorded in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Chrysolophus"
 ]
}

 The dataset's 5 records were derived from 128 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021273-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.26180/31343776
title: OZARADH Cleaned Dataset

description: Complete dataset that has been cleaned and de-identified from the OZARADH Trial in Melbourne, Australia from November 2024.
DOI: 10.26180/31343776.v1
title: OZARADH Cleaned Dataset

description: Complete dataset that has been cleaned and de-identified from the OZARADH Trial in Melbourne, Australia from November 2024.
DOI: 10.6084/m9.figshare.31314891
title: Dataset from Fish locomotor variation: connecting energetics and kinematic modulation

description: DataDepository_PTSR-ModulatedDynamicLocomotionGait .xlsx
DOI: 10.6084/m9.figshare.31314891.v1
title: Dataset from Fish locomotor variation: connecting energetics and kinematic modulation

description: DataDepository_PTSR-ModulatedDynamicLocomotionGait .xlsx
DOI: 10.1594/pangaea.985525
title: Benthic foraminiferal trace element ratios at IODP Site 383-U1540 during Marine Isotope Stage 11

description: This dataset presents benthic foraminiferal trace element ratios (i.e., B/Ca, U/Ca, Mn/Ca, U/Mn, Al/Ca, Fe/Ca) measured on the epibenthic foraminifera Cibicides kullenbergi at sediments from International Ocean Discovery Program Site 383-U1540 (55° 8.47ʹ S, 114° 50.52ʹ W, 3580 m) during Marine Isotope Stage 11. The samples were reductively cleaned and to determine the uncertainty of the analyses, two full replicates were analyzed. For all except one sample the C. kullenbergi Al/Ca ratios were below the limit of detection (LOD), at 0.5 µmol/mol. The element ratios were measured at the Institute of Geosciences at Kiel University (Kiel, Germany) using an Agilent 7900 inductively coupled plasma-mass spectrometer (ICP-MS). The degree of carbonate ion saturation (Δ[CO₃²⁻]) in bottom waters was calculated using the calibration of Yu and Elderfield (2007, doi:10.1016/j.epsl.2007.03.025).
DOI: 10.15468/dl.9zqmgf
title: Occurrence Download

description: A dataset containing 29 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Qualea hannekesaskiarum",
 "HasCoordinate is true",
 "BasisOfRecord is one of (Specimen)"
 ]
}

 The dataset includes 29 records from 18 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021289-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.j49jwx
title: Occurrence Download

description: A dataset containing 435 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is Asia",
 "DatasetKey is Australian Microbiome 16S (Bacteria) Dataset of Terrestrial Samples",
 "Month is March",
 "TaxonKey is Desulfobacterota"
 ]
}

 The dataset includes 435 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021288-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.988355
title: Age-depth model from ODP Hole 177-1090D
DOI: 10.1594/pangaea.988369
title: Alkenone concentration of ODP Site 177-1090
DOI: 10.1594/pangaea.984105
title: Benthic foraminifera faunal total relative abundance data for the Marine Isotope Stage (MIS) 19 to MIS 28 interval of IODP Site 339-U1387, Gulf of Cadiz
DOI: 10.1594/pangaea.988390
title: Depth integration of ODP Hole 177-1090D
DOI: 10.1594/pangaea.984107
title: Bottom current strength indicators for the Marine Isotope Stage (MIS) 19 to MIS 28 interval of IODP Site 339-U1387, Gulf of Cadiz
DOI: 10.1594/pangaea.984108
title: Benthic foraminifera C. pachyderma and P. ariminensis oxygen and carbon isotope records for the Marine Isotope Stage (MIS) 19 to MIS 28 interval of IODP Site 339-U1387, Gulf of Cadiz
DOI: 10.1594/pangaea.900889
title: Bacterial data from the coast of Ghana
DOI: 10.1594/pangaea.931096
title: Cobalt concentrations in the water column during LOHAFEX
DOI: 10.1594/pangaea.931098
title: Cobalt fluxes during LOHAFEX
DOI: 10.1594/pangaea.931099
title: Cobalt standing stocks during LOHAFEX
DOI: 10.1594/pangaea.937461
title: Zooplankton abundances Huinay
DOI: 10.1594/pangaea.937462
title: Zooplankton biomasses of Huinay
DOI: 10.1594/pangaea.937483
title: Zooplankton biovolume of Huinay
DOI: 10.15468/dl.u2hxpn
title: Occurrence Download

description: A dataset containing 2 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Ruizterania belemnensis",
 "HasCoordinate is true",
 "BasisOfRecord is one of (Specimen)"
 ]
}

 The dataset includes 2 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021290-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.929441
title: Oxygen isotope composition of diatoms from Lake Kotokel (southern Siberia, Russia)

description: This is a diatom oxygen isotope record from Lake Kotokel (southern Siberia, Russia), with implications for responses of the lake system and its environment to global change over the past 46 cal. ka BP. The δ¹⁸O diatom values vary between +23.7 and +31.2‰ over the record. The results present mainly diatom assemblages of summer blooming periods, except for the time span between 36 and 32 cal. ka BP, when the isotopic signal records mainly a shift from summer to spring blooming conditions. Possible water temperature changes only partly explain the changes in the isotopic record. The observed isotopic patterns are mainly produced by isotope changes in lake water in response to variations in air temperature, hydrology, and atmospheric circulation in the region. During Marine Isotope Stage (MIS) 2 (Last Glacial maximum), high δ¹⁸O diatom resulted from rapid evaporation and low fluvial inputs. The relatively high δ¹⁸O diatom values during the first half of MIS 1 (Holocene interglacial) suggest an increased portion of summer precipitation associated with southern/southeastern moisture transport. The decrease in δ¹⁸O diatom values during the second half of MIS 1 is due to the overall hemispheric cooling and increased moisture supply to the area by the Atlantic air masses. The Lake Kotokel record provides an example of complex interplay among several climatic/environmental controls of δ¹⁸O diatom during the Late Pleistocene and the Holocene.
DOI: 10.6084/m9.figshare.31343839
title: Code from Dipole and pairwise models for the motion of bubbles in a Hele-Shaw cell

description: The code used to generate the figures in this paper.
DOI: 10.6084/m9.figshare.31343839.v1
title: Code from Dipole and pairwise models for the motion of bubbles in a Hele-Shaw cell

description: The code used to generate the figures in this paper.
DOI: 10.5281/zenodo.15817156
title: /b β v/ in Romance: Frequency-Based Mapping Using Multiple Regional Atlases and Google Earth

description: The article is available at: https://authors.elsevier.com/sd/article/S0024384126000136This dataset provides a Google Earth Pro (.kml) file visualising the distribution of /b β v/ variants across Romance dialects, based on frequency-based analysis from multiple linguistic atlases.

Keywords:



Romance languages, phonetics, /b β v/, Google Earth Pro, linguistic atlas, phonological variation, betacism
DOI: 10.5281/zenodo.15817155
title: /b β v/ in Romance: Frequency-Based Mapping Using Multiple Regional Atlases and Google Earth

description: The article is available at: https://authors.elsevier.com/sd/article/S0024384126000136This dataset provides a Google Earth Pro (.kml) file visualising the distribution of /b β v/ variants across Romance dialects, based on frequency-based analysis from multiple linguistic atlases.

Keywords:



Romance languages, phonetics, /b β v/, Google Earth Pro, linguistic atlas, phonological variation, betacism
DOI: 10.1594/pangaea.974729
title: Margalefidium polykrikoides cell concentration time series

description: M.polykrikoides is a cosmopolitan harmful dinoflagellate that blooms in coastal waters worldwide. Despite genomic evidence that it is in Group III and so closely related to isolates from Puerto Rico, Malaysia, North America, and Central America, M. polykrikoides group III VA, isolated from the lower Chesapeake Bay, bloom at warmer temperatures and lower salinities than in coastal ecosystems occupied by its closest relatives. In contrast, M. polykrikoides blooms in other regions initiate when salinities are higher (e.g., 30) and water temperatures are cooler, leading to the question of whether there are differences in salinity and temperature preferences for different groups and strains of *M. polykrikoides*, or whether the realized niche of M. polykrikoides varies based on local conditions and competitive interactions . In this study, the effect of temperature and salinity on the exponential growth rate and total cell yield of an M. polykrikoides VA culture isolate were examined. A clonal culture of *M. polykrikoides *(MP-LRCB-082419) was established by isolating a cell from the Lafayette River, a sub-tributary of the lower Chesapeake Bay, on August 24, 2019. Lafayette River water of 20 salinity was filtered through Thermo ScientificTM NalgeneTM Rapid-FlowTM sterile, 1,000 mL disposable filter units containing a 90 mm diameter and 0.1 µm pore size PES membrane. Filtered river water was augmented with L1 medium (Guillard & Hargraves, 1993) nutrient concentrations excluding silicate) that was then used as the culture medium. The M. polykrikoides cell was isolated in Dr. Margaret Mulholland's lab via serial transfer into fresh medium using a 100-1000 µL Eppendorf® Research® pipette, Costar® 12-well clear TC-treated sterile well plates, and an OLYMPUS CKX41 inverted microscope. Then, the cell was inoculated into VWR® tissue culture flasks (25mL, non-treated, plug seal cap, and sterilized) containing L1 medium and incubated at 28 ̊ C, under 140µmol photons m-2 s-1 lights on a 14 h:10h light:dark cycle. M. polykrikoides cultures were acclimated to multiple temperature (16, 18, 20, 24, 28, 30, 32, and 34 ̊ C) and salinity (10, 15, 20, 25, and 30) treatments for 7 to 38 days by stepwise transferring (Yamaguchi & Honjo, 1989). Light was maintained under constant conditions at 140 µmol photons m-2 s-1 supplied over a 14h:10h light:dark cycle. Cultures in exponential growth phase were used to inoculate cells into tissue culture flasks containing L1 medium (total of 10 mL after inoculating cells) and exposed to the different temperature and salinity treatments in triplicate. The initial cell concentration for all the experiments was 1,200 cells mL-1. The experiments duration was 7, 14, 28, or 35 days. Samples (1mL each) were collected during seven timepoints every 1, 2, 4, or 5 days and alkaline Lugol's solution was added to preserve *M. polykrikoides* cells. M. polykrikoides cells were quantified from these preserved samples under bright field using an OLYMPUS BX51 microscope and a Palmer-Maloney counting chamber.
DOI: 10.1594/pangaea.974730
title: Margalefidium polykrikoides growth rates, carrying capacity, and coefficient of determination data

description: The growth rate was calculated by finding the best fit to the classic logistic growth model with the MATLAB curve fitting toolbox: N_t=K/(1+(e^(-r(-b+t) ))), where "N_t" is the cell concentration at time "t", K is the total cell yield, "r" is the exponential growth rate coefficient, and "b" the time of inflection of the curve (Garnier & Quetelet, 1838). However, when the classic logistic growth model did not fit the data because the asymptote was reached within one or two time intervals or was never reached, the following model was used to calculate the growth rate: N_t = N_0 e^rt, where "N_t " is the cell concentration at time "t", "N_0" was the initial cell concentration, and "r" is the growth rate coefficient (Andersen, 2005).
DOI: 10.1594/pangaea.974064
title: Trophic ecology of squids in the Benguela Upwelling System assessed through stomach content, fatty acid and stable isotopes analyses in austral spring 2021 - Fatty acid contents of squids

description: Squids were collected during the research cruise SO285 on RV Sonne in the northern (nBUS) and southern (sBUS) Benguela Upwelling System between September 13 and October 9, 2021 in order to determine their trophic position and nutritional ecology. The cruise was part of the TRAFFIC (Trophic tRAnsfer eFFICiency in the Benguela Current) project. Samples were retrieved from rectangular midwater trawl (RMT) net hauls at 10 stations in the nBUS (sampling ranged from surface down to 230–600 m) and 7 stations in the sBUS (sampling ranged from surface down to 500–750 m). Furthermore, some squids were caught using hook and line in the upper two meters of the water column at 2 stations in the nBUS (ranging from 20 to 115 min per station, 4–5 rods) and 4 stations in the sBUS (ranging from 45 to 105 min per station, 4–6 rods). At 1 station in sBUS one squid was retrieved from a neuston catamaran haul (NCAT) used to sample the surface layer (0­–20 cm sampling depth). Dorsal mantle length (DML) of each specimen was measured to the nearest mm below. This data set contains the results of the fatty acid trophic marker analyses of squid mantle muscle and midgut gland (MGG) tissue of 84 specimens. A modified carnivory index after Bode et al. (2015) was determined and ranged from 0.55 to 0.92. Differences in fatty acid compositions displayed distinct clusters separating squid families and different prey taxa through principal component analyses.
DOI: 10.1594/pangaea.974072
title: Trophic ecology of squids in the Benguela Upwelling System assessed through stomach content, fatty acid and stable isotopes analyses in austral spring 2021 - Stable isotope measurements of squids

description: Squids were collected during the research cruise SO285 on RV Sonne in the northern (nBUS) and southern (sBUS) Benguela Upwelling System between September 13 and October 9, 2021 in order to determine their trophic position and nutritional ecology. The cruise was part of the TRAFFIC (Trophic tRAnsfer eFFICiency in the Benguela Current) project. Samples were retrieved from rectangular midwater trawl (RMT) net hauls at 10 stations in the nBUS (sampling ranged from surface down to 230–600 m) and 6 stations in the sBUS (sampling ranged from surface down to 500–555 m). Furthermore, some squids were caught using hook and line in the upper two meters of the water column at 2 stations in the nBUS (ranging from 20 to 115 min per station, 4–5 rods) and 4 stations in the sBUS (ranging from 45 to 105 min per station, 4–6 rods). At 1 station in sBUS one squid was retrieved from a neuston catamaran haul (NCAT) used to sample the surface layer (0­–20 cm sampling depth). Dorsal mantle length (DML) of each specimen was measured to the nearest mm below. Mantle muscle tissue sample was taken from 82 squid specimens for stable isotope analyses (SIA). SIA revealed significant differences in δ15N values of small squids (dorsal mantle length &lt;10 cm) between the two subsystems, but none in those of large squids (dorsal mantle length &gt;10 cm). Trophic position estimates based on Post (2002) ranged from 2.2 to 5.0. Isotopic niche width was widest in the families Ommastrephidae and Cranchiidae.
DOI: 10.1594/pangaea.974073
title: Trophic ecology of squids in the Benguela Upwelling System assessed through stomach content, fatty acid and stable isotopes analyses in austral spring 2021 - Stable isotope baseline measurements

description: For stable isotope baseline measurements, the primarily herbivorous copepod Nannocalanus minor was collected during the research cruise SO285 on RV Sonne in the northern (nBUS) and southern (sBUS) Benguela Upwelling System between September 15 and October 7, 2021. The cruise was part of the TRAFFIC (Trophic tRAnsfer eFFICiency in the Benguela Current) project. Samples were retrieved from vertical multinet "Midi" hauls (200 µm mesh size) at 1 station in the nBUS (0–50 m depth) and 2 stations in the sBUS (50–100 m and 0–50 m depth respectively). In total, 3 samples were obtained from the nBUS and 6 from the sBUS. Stable isotope measurements of the copepod were then used as baseline values for further analyses in the study.
DOI: 10.15468/dl.e6faxb
title: Occurrence Download

description: A dataset containing 147 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Ruizterania esmeraldae",
 "HasCoordinate is true",
 "BasisOfRecord is one of (Specimen)"
 ]
}

 The dataset includes 147 records from 19 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021291-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.18653783
title: Dengue infection elicits skin tissue-resident and circulating CD8+ T-cells associated with protection from hospitalization
DOI: 10.5281/zenodo.18653782
title: Dengue infection elicits skin tissue-resident and circulating CD8+ T-cells associated with protection from hospitalization
DOI: 10.1594/pangaea.982930
title: Reproduction results of Folsomia candida depending on the Break-Thru® S 301 soil concentration

description: The reproduction data set contains the results on the reproduction of F. candida depending on the Break-Thru® S 301 soil concentration in mg/kg dry soil, test soil and extraction method, respectively. Reproductive endpoints are the absolute number of counted juveniles and adults as well as the counted number of juveniles relative to the control. As multiple tests were conducted, each test is assigned to a test number.
DOI: 10.1594/pangaea.983359
title: Grain size of sediment cores from the Western Irish Sea Mud Belt, June 2022

description: Particle size distributions were determined using a Malvern Mastersizer 3000 laser microgranulometer. Every other sample depth was analysed down to 40–45 cm (e.g. 0–2 cm, 4–6 cm, etc.). Samples were dispersed in a 1% Calgon solution (sodium hexametaphosphate) and sonicated for 10 minutes prior to analysis. Samples with particle diameters &gt;2000 µm were sieved using a 1000 µm mesh prior to analysis, and the results from laser diffraction (volumetric) were scaled to the overall sample (mass) by assuming constant sediment density. Particle size classes were grouped as: clay (&lt;3.9 μm), silt (3.9–62.5 μm), mud (&lt;62.5 μm), and sand (62.5–2000 μm).
DOI: 10.1594/pangaea.983327
title: Electromagnetic induction measurements with the vertically oriented dipole of the CMD Mini Explorer (32 cm transmitter-receiver spacing) taken in June 2023 in the Lower Havel Inner Delta near Lake Gülpe, Brandenburg (Germany)

description: Electromagnetic induction (EMI) was measured with a CMD-Mini Explorer (GF Instruments s.r.o., Brno, Czech Republic) in June 2023. We used the vertical dipole (VDP) at coil spacings of 0.32 m (VDP1), 0.71 m (VDP2) and 1.18 m (VDP3), archieving effective penetration depths of 0.5 m (VDP1), 1.0 m (VDP2) and 1.8 m (VDP3). According to the manufacturer, 70% of the signal originate from above these depths. The EMI sensors measure the apparent electrical conductivity (ECa, in mS/m). Measurements were taken by carrying the instrument about 0.2 m above ground while being directly connected to D-GPS (Leica GPS1200) for positioning. The acquisition rate was five measurements per second. Data quality was checked by measuring a reference line before and after each measurement. The area investigated by EMI in June 2023 is located to the north and northeast of the Gülpe research station. It has a total area of 12.3 ha. The reference line was located in the southern part of the study area. No drift correction had to be applied due to good data quality. Reference lines and single outliers were removed.The data set contains the EMI data with an intercoil spacing of 0.32 m.
DOI: 10.1594/pangaea.983332
title: Electromagnetic induction measurements with the vertically oriented dipole of the CMD Mini Explorer (71 cm transmitter-receiver spacing) taken in June 2023 in the Lower Havel Inner Delta near Lake Gülpe, Brandenburg (Germany)

description: Electromagnetic induction (EMI) was measured with a CMD-Mini Explorer (GF Instruments s.r.o., Brno, Czech Republic) in June 2023. We used the vertical dipole (VDP) at coil spacings of 0.32 m (VDP1), 0.71 m (VDP2) and 1.18 m (VDP3), archieving effective penetration depths of 0.5 m (VDP1), 1.0 m (VDP2) and 1.8 m (VDP3). According to the manufacturer, 70% of the signal originate from above these depths. The EMI sensors measure the apparent electrical conductivity (ECa, in mS/m). Measurements were taken by carrying the instrument about 0.2 m above ground while being directly connected to D-GPS (Leica GPS1200) for positioning. The acquisition rate was five measurements per second. Data quality was checked by measuring a reference line before and after each measurement. The area investigated by EMI in June 2023 is located to the north and northeast of the Gülpe research station. It has a total area of 12.3 ha. The reference line was located in the southern part of the study area. No drift correction had to be applied due to good data quality. Reference lines and single outliers were removed.The data set contains the EMI data with an intercoil spacing of 0.71 m.
DOI: 10.1594/pangaea.983461
title: Electromagnetic induction measurements with the vertically oriented dipole of the CMD Mini Explorer (118 cm transmitter-receiver spacing) taken in June 2023 in the Lower Havel Inner Delta near Lake Gülpe, Brandenburg (Germany)

description: Electromagnetic induction (EMI) was measured with a CMD-Mini Explorer (GF Instruments s.r.o., Brno, Czech Republic) in June 2023. We used the vertical dipole (VDP) at coil spacings of 0.32 m (VDP1), 0.71 m (VDP2) and 1.18 m (VDP3), archieving effective penetration depths of 0.5 m (VDP1), 1.0 m (VDP2) and 1.8 m (VDP3). According to the manufacturer, 70% of the signal originate from above these depths. The EMI sensors measure the apparent electrical conductivity (ECa, in mS/m). Measurements were taken by carrying the instrument about 0.2 m above ground while being directly connected to D-GPS (Leica GPS1200) for positioning. The acquisition rate was five measurements per second. Data quality was checked by measuring a reference line before and after each measurement. The area investigated by EMI in June 2023 is located to the north and northeast of the Gülpe research station. It has a total area of 12.3 ha. The reference line was located in the southern part of the study area. No drift correction had to be applied due to good data quality. Reference lines and single outliers were removed.The data set contains the EMI data with an intercoil spacing of 1.18 m.