cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.7467773.v1
title: Impact of dose capping in insulin glargine/lixisenatide fixed-ratio combination trials in patients with type 2 diabetes

description: <b>Objective</b>: The LixiLan clinical trials of insulin glargine (iGlar)/lixisenatide fixed-ratio combination (iGlarLixi) investigated the safety and efficacy of iGlarLixi versus iGlar: LixiLan-O (NCT02058147) in patients with type 2 diabetes (T2D) inadequately controlled on oral antidiabetes drugs (OADs), and LixiLan-L (NCT02058160) in patients with T2D inadequately controlled on basal insulin ± OADs. In these two trials, both iGlar and iGlarLixi were titrated to a maximum (capped) dose of 60 units. We evaluated whether this may have affected the reported glycemic efficacy of iGlar, and the glycemic differences observed between treatment with iGlarLixi and iGlar. <b>Methods</b>: The efficacy of iGlar under uncapped conditions was simulated in a 2-step approach. First, a model characterizing the relationship between iGlar dose and fasting self-measured plasma glucose (f-SMPG) was developed. Then, the relationship between glycated hemoglobin A1<sub>c</sub> (A1C) and f-SMPG was established to translate simulated f-SMPG responses to A1C responses. <b>Results</b>: Most patients achieved stable f-SMPG at ∼60 units/day, with no further reduction with increasing insulin dose. In comparisons of observed/capped and simulated/uncapped changes in mean A1C from baseline to Week 30, iGlarLixi consistently demonstrated treatment benefit compared with iGlar. Uncapping resulted in a slightly higher mean iGlar dose in both LixiLan-O (+0.72 units) and LixiLan-L (+2.1 units), without marked impact on f-SMPG or A1C change from baseline. <b>Conclusion</b>: Uncapping the iGlar dose in LixiLan-O and LixiLan-L would not have led to significant improvements in mean A1C reduction in the iGlar arm, supporting the conclusion that iGlarLixi provides additional, clinically-relevant glycemic control versus iGlar alone.
DOI: 10.7284/122371
title: Speedlog data collected during research cruise MGL1509 using a Furuno DS-50 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467677
title: Monthly Humidity

description: Update
DOI: 10.6084/m9.figshare.7467695
title: p = 1

description: Pressure = 1<br>
DOI: 10.6084/m9.figshare.7467722
title: Model storage of anthropogenic heat and carbon in the Southern Ocean

description: The dataset includes the final results for the heat and carbon storage budget in the Southern Ocean for two simulations performed with NOAA/GFDL model CM2.6. The first simulation is pre-industrial simulation, and the second is the climate change simulation with atmosphere CO2 in crease at 1% per year.
DOI: 10.6084/m9.figshare.7467695.v1
title: p = 1

description: Pressure = 1<br>
DOI: 10.6084/m9.figshare.7467722.v2
title: Model storage of anthropogenic heat and carbon in the Southern Ocean

description: The dataset includes the final results for the heat and carbon storage budget in the Southern Ocean for two simulations performed with NOAA/GFDL model CM2.6. The first simulation is pre-industrial simulation, and the second is the climate change simulation with atmosphere CO2 in crease at 1% per year.
DOI: 10.7284/118170
title: Expendable Probe data collected during research cruise MGL1510 using a Sippican MK21 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467722.v1
title: Model storage of anthropogenic heat and carbon in the Southern Ocean

description: The dataset includes the final results for the heat and carbon storage budget in the Southern Ocean for two simulations performed with NOAA/GFDL model CM2.6. The first simulation is pre-industrial simulation, and the second is the climate change simulation with atmosphere CO2 in crease at 1% per year.
DOI: 10.7284/118174
title: GNSS (Global Navigation Satellite System) data collected during research cruise MGL1510 using a C&C C-Nav 3050 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.7284/118178
title: GNSS (Global Navigation Satellite System) data collected during research cruise MGL1510 using a C&C C-Nav 2000 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.7284/118179
title: Gravimeter data collected during research cruise MGL1510 using a Bell BGM-3 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467446
title: Index Humidity

description: Update
DOI: 10.6084/m9.figshare.7467455
title: Countries and Number of Profiles that Gave Attention to Research Outputs with 'Comics' Keyword between 13/12/17 and 13/12/18 according to Altmetric

description: Data exported from the Altmetric Explorer. There were 4,588 tweets about research outputs with 'comics' as keyword between 13/12/17 and 13/12/18by 2,866 unique tweeters in 98 countries. <br>
DOI: 10.6084/m9.figshare.7467482
title: Figure 1_ PAR in EMT

description: PAR in EMT
DOI: 10.17028/rd.lboro.7467437
title: Supplementary information files for article: 'Single‐step fabrication of an anode supported planar single‐chamber solid oxide fuel cell'

description: Supplementary information files for article: 'Single‐step fabrication of an anode supported planar single‐chamber solid oxide fuel cell'.<br>Abstract: We present single‐step‐co‐sintering manufacture of a planar single‐chamber solid oxide fuel cell (SC‐SOFC) with porous multilayer structures consisting of NiO/CGO, CGO and CGO‐LSCF as anode, electrolyte, and cathode, respectively. Their green tapes were casted with 20 μm thickness and stacked into layers of anode, electrolyte, and cathode (10:2:2), then hot‐pressed at 2 MPa and 60°C for 5 minutes (deemed optimal). Subsequently, hot laminated layers were cut into 40 × 40 mm cells and co‐sintered up to 1200°C via different sintering profiles. Shrinkage behavior and curvature developments of cells were characterized, determining the best sintering profile. Hence, anode‐supported SC‐SOFCs were fabricated via a single‐step co‐sintering process, albeit with curvature formation at edges. Subsequently, anode thickness was increased to 800 μm and electrolyte reduced to 20 μm to obtain SOFCs with drastically reduced curvature with the help of a porous alumina cover plate.
DOI: 10.6084/m9.figshare.7467446.v1
title: Index Humidity

description: Update
DOI: 10.6084/m9.figshare.7467455.v1
title: Countries and Number of Profiles that Gave Attention to Research Outputs with 'Comics' Keyword between 13/12/17 and 13/12/18 according to Altmetric

description: Data exported from the Altmetric Explorer. There were 4,588 tweets about research outputs with 'comics' as keyword between 13/12/17 and 13/12/18by 2,866 unique tweeters in 98 countries. <br>
DOI: 10.6084/m9.figshare.7467482.v1
title: Figure 1_ PAR in EMT

description: PAR in EMT
DOI: 10.7284/118177
title: Gyrocompass data collected during research cruise MGL1510 using a Kongsberg Simrad GC80 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.17028/rd.lboro.7467437.v1
title: Supplementary information files for article: 'Single‐step fabrication of an anode supported planar single‐chamber solid oxide fuel cell'

description: Supplementary information files for article: 'Single‐step fabrication of an anode supported planar single‐chamber solid oxide fuel cell'.<br>Abstract: We present single‐step‐co‐sintering manufacture of a planar single‐chamber solid oxide fuel cell (SC‐SOFC) with porous multilayer structures consisting of NiO/CGO, CGO and CGO‐LSCF as anode, electrolyte, and cathode, respectively. Their green tapes were casted with 20 μm thickness and stacked into layers of anode, electrolyte, and cathode (10:2:2), then hot‐pressed at 2 MPa and 60°C for 5 minutes (deemed optimal). Subsequently, hot laminated layers were cut into 40 × 40 mm cells and co‐sintered up to 1200°C via different sintering profiles. Shrinkage behavior and curvature developments of cells were characterized, determining the best sintering profile. Hence, anode‐supported SC‐SOFCs were fabricated via a single‐step co‐sintering process, albeit with curvature formation at edges. Subsequently, anode thickness was increased to 800 μm and electrolyte reduced to 20 μm to obtain SOFCs with drastically reduced curvature with the help of a porous alumina cover plate.
DOI: 10.6084/m9.figshare.7467422
title: Monthly Temperature Night

description: Update
DOI: 10.6084/m9.figshare.7467422.v1
title: Monthly Temperature Night

description: Update
DOI: 10.7284/118175
title: INS (Inertial Navigation System) data collected during research cruise MGL1510 using a Kongsberg Seapath 200 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467383
title: Index Temperature Night

description: Update
DOI: 10.6084/m9.figshare.7467401
title: Triple Negative Breast Cancer Data

description: vcf data from whole exome sequencing of tumor from Thai patients with triple negative breast cancer between 2014 and 2017.<br>
DOI: 10.7284/118180
title: INS (Inertial Navigation System) data collected during research cruise MGL1510 using a Applanix POS/MV-320 V3 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467383.v1
title: Index Temperature Night

description: Update
DOI: 10.6084/m9.figshare.7467401.v1
title: Triple Negative Breast Cancer Data

description: vcf data from whole exome sequencing of tumor from Thai patients with triple negative breast cancer between 2014 and 2017.<br>
DOI: 10.7284/118182
title: Meteorological Station data collected during research cruise MGL1510 using a RM Young 26700 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467302
title: fast outflow

description: fast outflow<br>
DOI: 10.7284/118171
title: Multibeam Echosounder data collected during research cruise MGL1510 using a Kongsberg EM122 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467302.v1
title: fast outflow

description: fast outflow<br>
DOI: 10.6084/m9.figshare.7467287
title: GC-MS data

description: The GC–MS, and GC-FID runs were carried out on a two parallel GC-QP2010 and GC2010 instruments (Shimadzu, Kyoto, Japan). The GC column used was a 30 m × 0.25 mm i.d. × 0.25 μm df Supelcowax-10 column (MilliporeSigma). Helium was exploited as carrier gas, at a constant linear velocity of 30.0 cm/s which corresponding to an inlet pressure of 26.4 kPa for GC-MS and 97.4 kPa for GC-FID. The temperature program was the same in both analysis-type: 40°C at 3° C/min to 250°C, at 10°C/min to 280°C, held 10 min. GC-MS ion source temperature was set at 200°C; the interface temperature, 250°C. Scan range was set to m/z 40–360, with a scanning rate of 2000 amu/s. FFSNC 3.0 (Shimadzu) and NIST11 (Wiley) commercial libraries were used for identification, applying two filters, namely a spectrum similarity match over 85% and Linear Retention Index (LRI) (related to a C4-C24 FAMEs mixture) agreement in the ±15 range. The FID temperature was set at 280°C (sampling rate 40 ms) and gas flows were 40 mL/min for hydrogen and 400 mL/min for air, respectively. The data handling was supported by GCMSsolution ver.4.30 and GCsolution software (Shimadzu) for GC-MS and GC-FID analysis, respectively.
DOI: 10.7284/118181
title: pCO2 (Partial Pressure of Carbon Dioxide) data collected during research cruise MGL1510 using a LDEO pCO2 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.7284/118173
title: Singlebeam Echosounder data collected during research cruise MGL1510 using a Knudsen 3260 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467287.v3
title: GC-MS data

description: The GC–MS, and GC-FID runs were carried out on a two parallel GC-QP2010 and GC2010 instruments (Shimadzu, Kyoto, Japan). The GC column used was a 30 m × 0.25 mm i.d. × 0.25 μm df Supelcowax-10 column (MilliporeSigma). Helium was exploited as carrier gas, at a constant linear velocity of 30.0 cm/s which corresponding to an inlet pressure of 26.4 kPa for GC-MS and 97.4 kPa for GC-FID. The temperature program was the same in both analysis-type: 40°C at 3° C/min to 250°C, at 10°C/min to 280°C, held 10 min. GC-MS ion source temperature was set at 200°C; the interface temperature, 250°C. Scan range was set to m/z 40–360, with a scanning rate of 2000 amu/s. FFSNC 3.0 (Shimadzu) and NIST11 (Wiley) commercial libraries were used for identification, applying two filters, namely a spectrum similarity match over 85% and Linear Retention Index (LRI) (related to a C4-C24 FAMEs mixture) agreement in the ±15 range. The FID temperature was set at 280°C (sampling rate 40 ms) and gas flows were 40 mL/min for hydrogen and 400 mL/min for air, respectively. The data handling was supported by GCMSsolution ver.4.30 and GCsolution software (Shimadzu) for GC-MS and GC-FID analysis, respectively.
DOI: 10.7284/118172
title: Speedlog data collected during research cruise MGL1510 using a Furuno DS-50 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467224
title: Monthly Temperature Day

description: Update
DOI: 10.7284/118176
title: TSG (Thermosalinograph) data collected during research cruise MGL1510 using a Sea-Bird SBE-21 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467224.v1
title: Monthly Temperature Day

description: Update
DOI: 10.6084/m9.figshare.7467158
title: Index Temperature Day

description: Update
DOI: 10.7284/122383
title: GNSS (Global Navigation Satellite System) data collected during research cruise MGL1511 using a C&C C-Nav 3050 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467158.v1
title: Index Temperature Day

description: Update
DOI: 10.7284/122386
title: GNSS (Global Navigation Satellite System) data collected during research cruise MGL1511 using a C&C C-Nav 2000 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467143
title: CXDI_ESRF_Emili_huxleyi_RCC1212_NoCorr_figS7A_uint8_256_256_256_32_5

description: This file contains the tomographic slice images of the coccosphere from the <i>Emiliania huxleyi</i> RCC1212 species. The data is obtained from 3D Coherent X-ray Diffraction Imaging (3D-CXDI) at ESRF on ID10. After the reconstruction, no correction (no Gaussian subtraction) was applied. Each image has a size of 256 by 256. The intensity is coded in 8 bits (uint8). There are 256 images. The voxel size is 32.5 x 32.5 x 32.5 nm<sup>3</sup>. The data is used in the figure S7A of the article of T. Beuvier et al, Nat. Commun. (2019) (DOI: 10.1038/s41467-019-08635-x).
DOI: 10.6084/m9.figshare.7467143.v1
title: CXDI_ESRF_Emili_huxleyi_RCC1212_NoCorr_figS7A_uint8_256_256_256_32_5

description: This file contains the tomographic slice images of the coccosphere from the <i>Emiliania huxleyi</i> RCC1212 species. The data is obtained from 3D Coherent X-ray Diffraction Imaging (3D-CXDI) at ESRF on ID10. After the reconstruction, no correction (no Gaussian subtraction) was applied. Each image has a size of 256 by 256. The intensity is coded in 8 bits (uint8). There are 256 images. The voxel size is 32.5 x 32.5 x 32.5 nm<sup>3</sup>. The data is used in the figure S7A of the article of T. Beuvier et al, Nat. Commun. (2019) (DOI: 10.1038/s41467-019-08635-x).
DOI: 10.6084/m9.figshare.7467059
title: 1SC_INPUT

description: 1SC_INPUT
DOI: 10.6084/m9.figshare.7467116
title: Altmetric Top 100 Outputs with 'Comics' Keyword between 13/12/17 and 13/12/18

description: The top 100 outputs according to Altmetric, obtained by querying all articles with keyword "comics" between 13/12/17 and 13/12/18 in the Altmetric Explorer. Data was refined but character encoding errors might remain. Empty cells reflect unavailable data. <br>
DOI: 10.7284/122387
title: Gravimeter data collected during research cruise MGL1511 using a Bell BGM-3 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467059.v1
title: 1SC_INPUT

description: 1SC_INPUT
DOI: 10.6084/m9.figshare.7467116.v1
title: Altmetric Top 100 Outputs with 'Comics' Keyword between 13/12/17 and 13/12/18

description: The top 100 outputs according to Altmetric, obtained by querying all articles with keyword "comics" between 13/12/17 and 13/12/18 in the Altmetric Explorer. Data was refined but character encoding errors might remain. Empty cells reflect unavailable data. <br>
DOI: 10.7284/122385
title: Gyrocompass data collected during research cruise MGL1511 using a Kongsberg Simrad GC80 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7467005
title: 1SC_K4ME1

description: 1SC_K4ME1
DOI: 10.6084/m9.figshare.7467005.v1
title: 1SC_K4ME1

description: 1SC_K4ME1
DOI: 10.17028/rd.lboro.7466993
title: Supplementary information files for article: 'Regional variability in the atmospheric nitrogen deposition signal and its transfer to the sediment record in Greenland lakes'

description: Supplementary information files for article: 'Regional variability in the atmospheric nitrogen deposition signal and its transfer to the sediment record in Greenland lakes'.<br>Abstract: Disruption of the nitrogen cycle is a major component of global environmental change. δ15N in lake sediments is increasingly used as a measure of reactive nitrogen input but problematically, the characteristic depleted δ15N signal is not recorded at all sites. We used a regionally replicated sampling strategy along a precipitation and N‐deposition gradient in SW Greenland to assess the factors determining the strength of δ15N signal in lake sediment cores. Analyses of snowpack N and δ15N‐NO3 and water chemistry were coupled with bulk sediment δ15N. Study sites cover a gradient of snowpack δ15N (ice sheet: −6‰; coast urn:x-wiley:00243590:media:lno10936:lno10936-math-000110‰), atmospheric N deposition (ice sheet margin: ∼ 0.2 kg ha−1 yr−1; coast: 0.4 kg ha−1 yr−1) and limnology. Three 210Pb‐dated sediment cores from coastal lakes showed a decline in δ15N of ca. urn:x-wiley:00243590:media:lno10936:lno10936-math-00021‰ from ∼ 1860, reflecting the strongly depleted δ15N of snowpack N, lower in‐lake total N (TN) concentration (∼ 300 μg N L−1) and a higher TN‐load. Coastal lakes have 3.7–7.1× more snowpack input of nitrate than inland sites, while for total deposition the values are 1.7–3.6× greater for lake and whole catchment deposition. At inland sites and lakes close to the ice‐sheet margin, a lower atmospheric N deposition rate and larger in‐lake TN pool resulted in greater reliance on N‐fixation and recycling (mean sediment δ15N is 0.5–2.5‰ in most inland lakes; n = 6). The primary control of the transfer of the atmospheric δ15N deposition signal to lake sediments is the magnitude of external N inputs relative to the in‐lake N‐pool.
DOI: 10.7284/122384
title: INS (Inertial Navigation System) data collected during research cruise MGL1511 using a Kongsberg Seapath 200 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.17028/rd.lboro.7466993.v1
title: Supplementary information files for article: 'Regional variability in the atmospheric nitrogen deposition signal and its transfer to the sediment record in Greenland lakes'

description: Supplementary information files for article: 'Regional variability in the atmospheric nitrogen deposition signal and its transfer to the sediment record in Greenland lakes'.<br>Abstract: Disruption of the nitrogen cycle is a major component of global environmental change. δ15N in lake sediments is increasingly used as a measure of reactive nitrogen input but problematically, the characteristic depleted δ15N signal is not recorded at all sites. We used a regionally replicated sampling strategy along a precipitation and N‐deposition gradient in SW Greenland to assess the factors determining the strength of δ15N signal in lake sediment cores. Analyses of snowpack N and δ15N‐NO3 and water chemistry were coupled with bulk sediment δ15N. Study sites cover a gradient of snowpack δ15N (ice sheet: −6‰; coast urn:x-wiley:00243590:media:lno10936:lno10936-math-000110‰), atmospheric N deposition (ice sheet margin: ∼ 0.2 kg ha−1 yr−1; coast: 0.4 kg ha−1 yr−1) and limnology. Three 210Pb‐dated sediment cores from coastal lakes showed a decline in δ15N of ca. urn:x-wiley:00243590:media:lno10936:lno10936-math-00021‰ from ∼ 1860, reflecting the strongly depleted δ15N of snowpack N, lower in‐lake total N (TN) concentration (∼ 300 μg N L−1) and a higher TN‐load. Coastal lakes have 3.7–7.1× more snowpack input of nitrate than inland sites, while for total deposition the values are 1.7–3.6× greater for lake and whole catchment deposition. At inland sites and lakes close to the ice‐sheet margin, a lower atmospheric N deposition rate and larger in‐lake TN pool resulted in greater reliance on N‐fixation and recycling (mean sediment δ15N is 0.5–2.5‰ in most inland lakes; n = 6). The primary control of the transfer of the atmospheric δ15N deposition signal to lake sediments is the magnitude of external N inputs relative to the in‐lake N‐pool.
DOI: 10.6084/m9.figshare.7466912
title: 1SC_K27AC

description: 1SC_K27AC
DOI: 10.7284/122388
title: INS (Inertial Navigation System) data collected during research cruise MGL1511 using a Applanix POS/MV-320 V3 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7466909
title: 1SC_POL2

description: 1SC_POL2
DOI: 10.6084/m9.figshare.7466912.v1
title: 1SC_K27AC

description: 1SC_K27AC
DOI: 10.6084/m9.figshare.7466897
title: 1V_INPUT

description: 1V_INPUT
DOI: 10.6084/m9.figshare.7466909.v1
title: 1SC_POL2

description: 1SC_POL2
DOI: 10.7284/122389
title: Meteorological Station data collected during research cruise MGL1511 using a RM Young 26700 instrument system onboard the platform RV Marcus G. Langseth

description: Original (unprocessed) data collected during a Field_expedition
DOI: 10.6084/m9.figshare.7466897.v1
title: 1V_INPUT

description: 1V_INPUT
DOI: 10.6084/m9.figshare.7466882
title: 1V_K4ME1

description: 1V_K4ME1