Supplementary Material for: Cardiorenal Outcomes With Finerenone in Asian Patients With Chronic Kidney Disease and Type 2 Diabetes: A FIDELIO-DKD Post Hoc Analysis by Koya D. (16817664)

“…Efficacy outcomes included a primary kidney composite (time to kidney failure, sustained decrease of ≥40% in eGFR from baseline, and death from renal causes) and secondary cardiovascular (time to cardiovascular death, non-fatal myocardial infarction, non-fatal stroke, or hospitalization for heart failure) and kidney (time to kidney failure, sustained decrease of ≥57% in eGFR from baseline, and death from renal causes) composites. …”

Supplementary Material for: Cardiorenal Outcomes With Finerenone in Asian Patients With Chronic Kidney Disease and Type 2 Diabetes: A FIDELIO-DKD Post Hoc Analysis by Koya D. (16817664)

“…Efficacy outcomes included a primary kidney composite (time to kidney failure, sustained decrease of ≥40% in eGFR from baseline, and death from renal causes) and secondary cardiovascular (time to cardiovascular death, non-fatal myocardial infarction, non-fatal stroke, or hospitalization for heart failure) and kidney (time to kidney failure, sustained decrease of ≥57% in eGFR from baseline, and death from renal causes) composites. …”

Supplementary Material for: Cardiorenal Outcomes With Finerenone in Asian Patients With Chronic Kidney Disease and Type 2 Diabetes: A FIDELIO-DKD Post Hoc Analysis by Koya D. (16817664)

“…Efficacy outcomes included a primary kidney composite (time to kidney failure, sustained decrease of ≥40% in eGFR from baseline, and death from renal causes) and secondary cardiovascular (time to cardiovascular death, non-fatal myocardial infarction, non-fatal stroke, or hospitalization for heart failure) and kidney (time to kidney failure, sustained decrease of ≥57% in eGFR from baseline, and death from renal causes) composites. …”

Supplementary Material for: Mean Corpuscular Volume and Mortality in Incident Hemodialysis Patients by Dratch A. (6189002)

“…In the fully adjusted models, compared to a reference of MCV 92–< 94 fL, patients with a baseline MCV > 100+ fL had a 28% higher risk of all-cause mortality (hazard ratio [HR] 1.28, 95% CI 1.22–1.34), 27% higher risk of cardiovascular mortality (HR 1.27, 95% CI 1.18–1.36), and 18% higher risk of infectious mortality (HR 1.18, 95% CI 1.02–1.38). …”

30-year trends in incidence of acute STEMI and NSTEMI in the Belgian Province of Luxembourg. A long-term follow-up of the MONICA-BELLUX registry by Bernhard L. Gerber (10171583)

“…The overall AMI incidence decreased by 5.3 events per 100,000 inhabitants annually, from 314 per 100,000 in 1986 to 116 per 100,000 in 2014. …”

SD11 attenuates the progression of liver deterioration in STZ-treated mice. by Waraporn Ruathong (20308203)

Neural network classifiers can distinguish states which differ in either activity or correlations. by Nicholas A. Frost (10739821)

“…In this manner, half the neurons increased their activity in “State B” compared to “State A”; the other half decreased. The proportion of activity transferred was determined by randomly drawing a number with an upper bound ranging from 5% to 50%. …”

Combined epidural-general anesthesia was associated with lower risk of postoperative complications in patients undergoing open abdominal surgery for pheochromocytoma: A retrospecti... by Nan Li (155066)

“…</p><p>Methods</p><p>This was a retrospective cohort study. 146 patients who underwent open surgery for pheochromocytoma (100 received combined epidural-general anesthesia and 46 received general anesthesia) in Peking University First Hospital from January 1, 2002 to December 31, 2015 were enrolled. …”

ROS production by PBMC-derived monocytes and in the J774A.1 cell line (mouse macrophages) is also reduced by pre-incubation with iron-binding molecules. by Armand Paauw (255206)

“…<p>A) ROS production in PBMC-derived monocytes pre-incubated with yersiniabactin or iron-saturated yersiniabactin. …”

Image4_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image5_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image9_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image12_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image2_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image6_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image7_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image11_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image8_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image10_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”