cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.20452910
title: Additional file 2 of Nutrient-limited subarctic caves harbour more diverse and complex bacterial communities than their surface soil

description: Additional file 2. ASV table with all the samples (including triplicates) from four cave zones of the six subarctic caves. GenBank accession numbers are given above each column (Table S2).
DOI: 10.6084/m9.figshare.20452916.v1
title: Additional file 4 of Nutrient-limited subarctic caves harbour more diverse and complex bacterial communities than their surface soil

description: Additional file 4. Multiple properties of soil samples measured from different cave zones in the six sampled caves (Table S4).
DOI: 10.6084/m9.figshare.20452913
title: Additional file 3 of Nutrient-limited subarctic caves harbour more diverse and complex bacterial communities than their surface soil

description: Additional file 3. ASV table with averaged microbiomes for each zone within each cave (averages of triplicates). Only the ASVs with more than 20 sequences are given within the table (Table S3).
DOI: 10.6084/m9.figshare.20452916
title: Additional file 4 of Nutrient-limited subarctic caves harbour more diverse and complex bacterial communities than their surface soil

description: Additional file 4. Multiple properties of soil samples measured from different cave zones in the six sampled caves (Table S4).
DOI: 10.6084/m9.figshare.20399175
title: Data by figure

description: data in the paper title <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em><br> <br>
DOI: 10.6084/m9.figshare.20399175.v1
title: Data by figure

description: data in the paper title <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em><br> <br>
DOI: 10.6084/m9.figshare.20399181
title: Pure solution dataset

description: raw sensor data from the integrated chip with 3ISMs tested in pure ion solution. Data for the paper titled <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em> <br>
DOI: 10.6084/m9.figshare.20399181.v1
title: Pure solution dataset

description: raw sensor data from the integrated chip with 3ISMs tested in pure ion solution. Data for the paper titled <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em> <br>
DOI: 10.6084/m9.figshare.20399217
title: Mixed solution dataset

description: Raw sensor data from the integrated chip with 3ISMs tested in mixed ion solution. Data for the paper titled <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em>
DOI: 10.6084/m9.figshare.20399217.v1
title: Mixed solution dataset

description: Raw sensor data from the integrated chip with 3ISMs tested in mixed ion solution. Data for the paper titled <em>Integrated biosensor platform based on graphene transistor arrays for real-time high-accuracy ion sensing</em>
DOI: 10.21985/n2-8c5z-qd12
title: Additional Datasets
DOI: 10.21985/n2-e8p0-wh39
title: Supplemental Figures - Reference
DOI: 10.6084/m9.figshare.20410704.v2
title: Observational Study: Determinants for Vegetable Consumption Among Elementary School Students in Indonesia

description: Respondent Characteristics, Food Recall data, Knowledge Score and Attitude score<strong> Observational Study: Determinants for Vegetable Consumption Among Elementary School Students in Indonesia</strong>
DOI: 10.21985/n2-77ts-qc71
title: Supplemental Figures - Set 1
DOI: 10.21985/n2-c7gv-bw50
title: Supplemental Figures - Set 2
DOI: 10.21985/n2-fvff-3607
title: Supplemental Figures - Set 3
DOI: 10.5281/zenodo.6975765
title: DCIP_DNAPL_Imaging

description: This is the dataset for the journal paper "Characterization of DNAPL source zones in clay-sand media via joint inversion of DC resistivity, induced polarization and borehole data"
DOI: 10.5281/zenodo.6975764
title: DCIP_DNAPL_Imaging

description: This is the dataset for the journal paper "Characterization of DNAPL source zones in clay-sand media via joint inversion of DC resistivity, induced polarization and borehole data"
DOI: 10.21985/n2-w4fs-sh32
title: Supplemental Figures - Set 4
DOI: 10.6084/m9.figshare.20453175
title: Dated Huon Peninsula coral samples

description: <strong>Revised submission to Communications Earth and Environment (09/08/22): </strong>High interstadial sea levels over the past 420ka from the Huon Peninsula (Papua New Guinea) <strong>Supplementary Data 2. Dated Huon Peninsula coral samples from the compilation of Hibbert et al. (2016), with the updated uplift rates as proposed in this study.</strong> We also updated our estimates of the latitude and longitude of the samples, based on the descriptions and maps in the original studies. Uplift rate calculations are descibed in the method section. The uncertainty given here is based on the average uncertainty of T16 (MIS 5e) shoreline angle elevations, Huon RSL during MIS 5e, reference water level, seismic cycle influence, DSM elevation and time of terrace formation (see Methods). Additionally we note that there is unknown uncertainty in the location of the samples here. There are no lattitude/longitude values given for the samples in any of the references, and only reference 22 (Stein et al., 1993) presents sample locations in a detailed map. We did not determine accurate uplift rates for the Bobongora section as it is not clearly connected, and deformed differently than the terraces at the other sample sites, so we use the same rough estimate as in Supplementary Fig. 2.
DOI: 10.6084/m9.figshare.20155097
title: Data Deposition for "Measuring anion binding at biomembrane interfaces"

description: Contains raw data for figures in the main text and the supporting information.
DOI: 10.6084/m9.figshare.20453310
title: Data-1

description: GIS, Data
DOI: 10.6084/m9.figshare.20453310.v1
title: Data-1

description: GIS, Data
DOI: 10.6084/m9.figshare.20452887
title: Lattice-SIM Immunofluorescence Imaris Files

description: Immunofluorescence data acquired from fixed HaCaT keratinocytes with lattice-SIM microscopy, identifying the membrane co-localisaiton of Orai1 and TRPC1.
DOI: 10.6084/m9.figshare.20452887.v1
title: Lattice-SIM Immunofluorescence Co-localisation

description: Immunofluorescence data acquired from fixed HaCaT keratinocytes with lattice-SIM microscopy, identifying the membrane co-localisaiton of Orai1 and TRPC1.
DOI: 10.21227/xps8-wv71
title: Supplementary video files

description: Astrictive-type grippers, which generate gripping forces from adhesive forces at the contact surface such as suction cup, are popular end-effectors as picking solutions because of their simplicity and small working space. However, the adhesive force of the astrictive gripper decreases with increasing complexity of the object surface; thus, its application has been restricted to simple picking of objects with a flat surface. Here, we present an all-round honeycomb astrictive gripper that has an orthotropic surface tension for grasping highly irregular shaped objects with an uneven surface. The design is inspired by mimicking the two-level (macro- and meso-scale) shape adaptation of the octopus’s leg. The stiffness-variable structure is also consisted to change its stiffness similar to the function of octopus’s leg, and owing to the combination of these structures makes possible to perform various tasks including hammering, breakfast serving, and vaccination which were not possible for previous astrictive gripper.
DOI: 10.6084/m9.figshare.20453499
title: Lattice-SIM Immunofluorescence Analysis Files

description: Analysis data files for the lattice-SIM colocalisation data pool
DOI: 10.6084/m9.figshare.20453499.v2
title: Lattice-SIM Immunofluorescence Analysis Files

description: Analysis data files for the lattice-SIM colocalisation data pool
DOI: 10.6084/m9.figshare.20453499.v1
title: Lattice-SIM Immunofluorescence Analysis Files

description: Analysis data files for the lattice-SIM colocalisation data pool
DOI: 10.6084/m9.figshare.20453631.v1
title: Supplementary Material for: Evaluating the Effectiveness of a Telehealth Cancer Genetics Program: A <b><i>BRCA</i></b> Pilot Study

description: <b><i>Introduction:</i></b> Ashkenazi Jewish (AJ) individuals face a 1 in 40 (2.5%) risk of having a <i>BRCA</i> mutation, which is 10 times the general population risk. JScreen launched the PEACH <i>BRCA</i> Study, a telehealth-based platform for <i>BRCA</i> education and testing, with the goal of creating an effective model for <i>BRCA</i> testing in low-risk AJ individuals who do not meet national testing criteria. Other goals were to determine the rate of <i>BRCA</i> mutations in this group, to assess the adequacy of screening for the 3 common AJ founder mutations only, and to assess satisfaction with the telehealth model to help inform a national launch of a broader cancer genetic testing program. <b><i>Methods:</i></b> Criteria for participation included those who were AJ, resided in the metro-Atlanta area, were aged 25 and older, and had no personal or close family history of <i>BRCA</i>-related cancers. Pre-test education was provided through a video and written summary, followed by complimentary <i>BRCA1/2</i> sequencing and post-test genetic counseling. Participants responded to pre- and post-test surveys, which assessed knowledge and satisfaction. Those who were not eligible to participate were sent genetic counseling resources and later surveyed. <b><i>Results:</i></b> Five hundred one participants were tested and the results included 4 positives (0.8% positivity rate), 494 negatives, and 3 variants of uncertain significance. Overall satisfaction with the study process was high (96.9/100), knowledge about <i>BRCA</i> was high (97.5% of participants passed a pre-test knowledge quiz), and satisfaction with pre- and post-test education was high (97.9% of participants were satisfied with the pre-test video and written summary, and 99.5% felt that their post-test genetic counseling session was valuable). Many participants expressed interest in receiving broader cancer testing. <b><i>Conclusions:</i></b> The <i>BRCA</i> founder mutation rate in a low-risk AJ population was significantly lower than the previously established AJ rate of 1 in 40. It was also determined that a telehealth model for a cancer genetics program is effective and acceptable to the population tested. This study established interest in broader cancer genetic testing through a telehealth platform and suggested that testing may be successful in the Jewish community at a national level and potentially in other populations, provided that patient education and genetic counseling are adequately incorporated.
DOI: 10.6084/m9.figshare.20453622
title: economic indicators

description: The main economic indicators of labor in the People's Republic of China and the Russian Federation
DOI: 10.6084/m9.figshare.20453619
title: TRPC1 at membrane

description: Data for TRPC1 signal restricted to the plasma membrane
DOI: 10.6084/m9.figshare.20453619.v1
title: TRPC1 at membrane

description: Data for TRPC1 signal restricted to the plasma membrane
DOI: 10.6084/m9.figshare.20453646
title: Total Orai1

description: Data for total Orai1 signal
DOI: 10.6084/m9.figshare.20453646.v1
title: Total Orai1

description: Data for total Orai1 signal
DOI: 10.6084/m9.figshare.20453655.v1
title: Lineage statistics

description: Результаты генотипирования (pangolin 4.1.1) Pangolin lineage report (pangolin 4.1.1)
DOI: 10.6084/m9.figshare.19776187.v1
title: Zircon U–Pb age, whole-rock geochemistry and Nd–Sr–Pb isotope constraints on petrogenesis of the Eocene Zajkan gabbro–monzogranite intrusion, Tarom-Hashtjin magmatic belt, NW Iran

description: The late Eocene high-K to shoshonitic Zajkan intrusion, situated in the Tarom-Hashtjin magmatic belt (THMB), NW Iran, ranges in composition from gabbro to pyroxene quartz monzodiorite, pyroxene quartz monzonite and monzogranite, and is classified as an I-type metaluminous granitoid. On the primitive mantle-normalised spider diagram, these rocks demonstrate negative high field strength element (HFSE) anomalies, large-ion lithophile element (LILE) enrichment, and positive Pb anomaly, indicating a subduction-related signature. Furthermore, the granitoids are characterised by coherent chondrite-normalised rare earth element patterns with high light rare earth elements/heavy rare earth elements (LREE/HREE) and moderate to weakly negative Eu anomalies (Eu/Eu* = 0.6–0.86). LA-ICP-MS zircon U–Pb dating demonstrates that the Zajkan intrusion crystallised at <i>ca</i> 36.5 Ma. Relatively low to moderate <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.7046–0.7061) and positive εNd<sub>(t)</sub> values (1.52–1.88) of the Zajkan samples are consistent with an enriched lithospheric mantle source that was metasomatised by an earlier subducted slab. Geochemical features show that the parental magma of the Zajkan intrusion likely resulted from a partial melting of metasomatised amphibole-bearing mantle source. Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of a mantle-derived magma and ∼20% of a juvenile lower crustal-derived magma. Partial melting of the metasomatised mantle may have resulted from late Eocene lithospheric thinning and hot asthenospheric upwelling through slab roll-back or lithospheric delamination. KEY POINTSThe late Eocene high-K to shoshonitic Zajkan intrusion is located within the Tarom-Hashtjin magmatic belt, NW Iran.U–Pb zircon dating revealed an age of <i>ca</i> 36.5 Ma for emplacement of the Zajkan intrusion.Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of mantle-derived magma and ∼20% of juvenile lower crustal-derived magma. The late Eocene high-K to shoshonitic Zajkan intrusion is located within the Tarom-Hashtjin magmatic belt, NW Iran. U–Pb zircon dating revealed an age of <i>ca</i> 36.5 Ma for emplacement of the Zajkan intrusion. Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of mantle-derived magma and ∼20% of juvenile lower crustal-derived magma.
DOI: 10.6084/m9.figshare.20103534
title: Geochemistry of seafloor surface sediment and submarine hydrothermal signature of Tomini Bay, Indonesia

description: During the Indonesia–Australia Submarine Survey of Hydrothermal Activity (IASSHA) 2001 cruise, several seafloor surface sediment samples were collected from Tomini Bay. The samples were geochemically examined for major and trace-element geochemistry to study the hydrothermal signature fingerprint. The Tomini Bay seafloor surface sediment sampled by gravity coring is relatively enriched in Na, P, S, Ca, Ni, Sr, and Ba mainly from a terrigenous source. The elevated concentrations of Mg, S, Cr, Co and Ni at one site suggest a contribution from a mafic terrigenous source. A manganese-rich sediment layer was detected on the sediment surface with Mn up to 9474.43 ppm. A hydrothermal signature was successfully distinguished from the manganese-rich sediment layer. Despite the lack of hydrothermal precipitates, the geochemistry of the Tomini Bay seafloor surface sediments provides evidence for submarine hydrothermal activity. KEY POINTSSeafloor surface sediment is an alternative proxy for investigating submarine hydrothermal activity.Hydrothermal signature is well recorded in the Fe/Mn-rich sediment layer and can be distinguished from measured concentrations and elemental ratios of Fe, Mn, HFSE (Zr), trace elements (Cu, Ni, Zn, Co, Zr) and REY (Y, Ce).The Mn-rich sediment layer in Tomini Bay seafloor surface sediment preserved hydrothermal fingerprint and confirmed the evidence of an active hydrothermal system in the studied area. Seafloor surface sediment is an alternative proxy for investigating submarine hydrothermal activity. Hydrothermal signature is well recorded in the Fe/Mn-rich sediment layer and can be distinguished from measured concentrations and elemental ratios of Fe, Mn, HFSE (Zr), trace elements (Cu, Ni, Zn, Co, Zr) and REY (Y, Ce). The Mn-rich sediment layer in Tomini Bay seafloor surface sediment preserved hydrothermal fingerprint and confirmed the evidence of an active hydrothermal system in the studied area.
DOI: 10.6084/m9.figshare.20103534.v1
title: Geochemistry of seafloor surface sediment and submarine hydrothermal signature of Tomini Bay, Indonesia

description: During the Indonesia–Australia Submarine Survey of Hydrothermal Activity (IASSHA) 2001 cruise, several seafloor surface sediment samples were collected from Tomini Bay. The samples were geochemically examined for major and trace-element geochemistry to study the hydrothermal signature fingerprint. The Tomini Bay seafloor surface sediment sampled by gravity coring is relatively enriched in Na, P, S, Ca, Ni, Sr, and Ba mainly from a terrigenous source. The elevated concentrations of Mg, S, Cr, Co and Ni at one site suggest a contribution from a mafic terrigenous source. A manganese-rich sediment layer was detected on the sediment surface with Mn up to 9474.43 ppm. A hydrothermal signature was successfully distinguished from the manganese-rich sediment layer. Despite the lack of hydrothermal precipitates, the geochemistry of the Tomini Bay seafloor surface sediments provides evidence for submarine hydrothermal activity. KEY POINTSSeafloor surface sediment is an alternative proxy for investigating submarine hydrothermal activity.Hydrothermal signature is well recorded in the Fe/Mn-rich sediment layer and can be distinguished from measured concentrations and elemental ratios of Fe, Mn, HFSE (Zr), trace elements (Cu, Ni, Zn, Co, Zr) and REY (Y, Ce).The Mn-rich sediment layer in Tomini Bay seafloor surface sediment preserved hydrothermal fingerprint and confirmed the evidence of an active hydrothermal system in the studied area. Seafloor surface sediment is an alternative proxy for investigating submarine hydrothermal activity. Hydrothermal signature is well recorded in the Fe/Mn-rich sediment layer and can be distinguished from measured concentrations and elemental ratios of Fe, Mn, HFSE (Zr), trace elements (Cu, Ni, Zn, Co, Zr) and REY (Y, Ce). The Mn-rich sediment layer in Tomini Bay seafloor surface sediment preserved hydrothermal fingerprint and confirmed the evidence of an active hydrothermal system in the studied area.
DOI: 10.6084/m9.figshare.19776187
title: Zircon U–Pb age, whole-rock geochemistry and Nd–Sr–Pb isotope constraints on petrogenesis of the Eocene Zajkan gabbro–monzogranite intrusion, Tarom-Hashtjin magmatic belt, NW Iran

description: The late Eocene high-K to shoshonitic Zajkan intrusion, situated in the Tarom-Hashtjin magmatic belt (THMB), NW Iran, ranges in composition from gabbro to pyroxene quartz monzodiorite, pyroxene quartz monzonite and monzogranite, and is classified as an I-type metaluminous granitoid. On the primitive mantle-normalised spider diagram, these rocks demonstrate negative high field strength element (HFSE) anomalies, large-ion lithophile element (LILE) enrichment, and positive Pb anomaly, indicating a subduction-related signature. Furthermore, the granitoids are characterised by coherent chondrite-normalised rare earth element patterns with high light rare earth elements/heavy rare earth elements (LREE/HREE) and moderate to weakly negative Eu anomalies (Eu/Eu* = 0.6–0.86). LA-ICP-MS zircon U–Pb dating demonstrates that the Zajkan intrusion crystallised at <i>ca</i> 36.5 Ma. Relatively low to moderate <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.7046–0.7061) and positive εNd<sub>(t)</sub> values (1.52–1.88) of the Zajkan samples are consistent with an enriched lithospheric mantle source that was metasomatised by an earlier subducted slab. Geochemical features show that the parental magma of the Zajkan intrusion likely resulted from a partial melting of metasomatised amphibole-bearing mantle source. Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of a mantle-derived magma and ∼20% of a juvenile lower crustal-derived magma. Partial melting of the metasomatised mantle may have resulted from late Eocene lithospheric thinning and hot asthenospheric upwelling through slab roll-back or lithospheric delamination. KEY POINTSThe late Eocene high-K to shoshonitic Zajkan intrusion is located within the Tarom-Hashtjin magmatic belt, NW Iran.U–Pb zircon dating revealed an age of <i>ca</i> 36.5 Ma for emplacement of the Zajkan intrusion.Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of mantle-derived magma and ∼20% of juvenile lower crustal-derived magma. The late Eocene high-K to shoshonitic Zajkan intrusion is located within the Tarom-Hashtjin magmatic belt, NW Iran. U–Pb zircon dating revealed an age of <i>ca</i> 36.5 Ma for emplacement of the Zajkan intrusion. Sr–Nd isotope modelling is consistent with the Zajkan intrusion formed from a mix of ∼80% of mantle-derived magma and ∼20% of juvenile lower crustal-derived magma.
DOI: 10.6084/m9.figshare.20453577
title: Orai1 at Membrane

description: Data for Orai1 signal restricted to the plasma membrane
DOI: 10.6084/m9.figshare.20453577.v2
title: Orai1 at Membrane

description: Data for Orai1 signal restricted to the plasma membrane
DOI: 10.6084/m9.figshare.20453577.v1
title: Orai1 at Membrane

description: Data for Orai1 signal restricted to the plasma membrane
DOI: 10.34740/kaggle/dsv/4046791
title: WallStreetBets 2022
DOI: 10.6084/m9.figshare.20422494
title: The enzymatic activities and physicochemical properties

description: The enzymatic activities and physicochemical properties
DOI: 10.6084/m9.figshare.20422494.v2
title: The enzymatic activities and physicochemical properties

description: The enzymatic activities and physicochemical properties
DOI: 10.6084/m9.figshare.20443377
title: Data used for the publication "Large contribution of fossil-derived components to aqueous secondary organic aerosols in China "

description: We report new radiocarbon measurements of individual dicarboxylic acids in aerosols collected from a regional receptor site in South China. The compound-specific radiocarbon isotopic evidences show that fossil anthropogenic precursors contribute to the formation of aqueous-phase secondary organic aerosol to a much higher extent than expected. The dataset includes chemical composition and dual-carbon (stable carbon and radiocarbon) isotope composition of aerosols used in the study.
DOI: 10.6084/m9.figshare.20443377.v2
title: Data used for the publication "Large contribution of fossil-derived components to aqueous secondary organic aerosols in China "

description: We report new radiocarbon measurements of individual dicarboxylic acids in aerosols collected from a regional receptor site in South China. The compound-specific radiocarbon isotopic evidences show that fossil anthropogenic precursors contribute to the formation of aqueous-phase secondary organic aerosol to a much higher extent than expected. The dataset includes chemical composition and dual-carbon (stable carbon and radiocarbon) isotope composition of aerosols used in the study.
DOI: 10.6084/m9.figshare.20443377.v1
title: Data used for the publication "Large contribution of fossil-derived components to aqueous secondary organic aerosols in China "

description: We report new radiocarbon measurements of individual dicarboxylic acids in aerosols collected from a regional receptor site in South China. The compound-specific radiocarbon isotopic evidences show that fossil anthropogenic precursors contribute to the formation of aqueous-phase secondary organic aerosol to a much higher extent than expected. The dataset includes chemical composition and dual-carbon (stable carbon and radiocarbon) isotope composition of aerosols used in the study.
DOI: 10.6084/m9.figshare.20453772
title: Total TRPC1

description: Data for total TRPC1 signal
DOI: 10.6084/m9.figshare.20453772.v1
title: Total TRPC1

description: Data for total TRPC1 signal