Induction of Nano-lantern-positive cells from <i>hSOX10</i>^{<i>2A-NL/+</i>} hiPS cells. by Tomoko Horikiri (3686857)

“…<p>(A-D) Morphology of cultured cells from <i>hSOX10</i>^{<i>2A-NL/+</i>} hiPS cells during 3 days (Day3) to 9 days (Day9). …”

Bcl3 deficient bone marrow-derived cDCs fail to differentiate into potent antigen-presenting cells. by June Guha (14041154)

Drebrin phosphorylation on S142 regulates neuroblast morphology and orientation <i>in vivo</i>. by Martina Sonego (481270)

“…(B) Quantitative morphological analysis also shows a decrease in leading process length for wt, S142A and S142D compared to the control (mean ± SEM; n = 8 brains for empty vector; n = 5 brains for wt, S142A, and S142D drebrin; *<i>P</i><0.05, **<i>P</i><0.01, ***<i>P</i><0.001). …”

Bcl3 expression in classical dendritic cells is critical for protection against. <i>T</i>. <i>gondii</i>. by June Guha (14041154)

DC distribution is significantly influenced by Bcl3 deficiency in the context of <i>T</i>. <i>gondii</i> infection. by June Guha (14041154)

Bcl3 in classical dendritic cells promotes T cell activation after <i>T</i>. <i>gondii</i> infection. by June Guha (14041154)

Condition 2 of the connecting tube. by Xiaolei Zhang (316541)

Parasite control and histopathology (lung) are similarly impaired in complete and cDC-specific <i>Bcl3</i>-deficient mice infected with <i>T</i>. <i>gondii</i>. by June Guha (14041154)

Western blot analysis of p-AMPK expression levels in the left ventricle of each group examined. by Hossein Azizian (17696750)

Impact of Dsg2 on invasion. by Wiebke K. Peitsch (173727)

“…(C) TEER assay, showing no alteration of invasive properties upon Dsg2 depletion. A marked decrease in TEER was seen in cocultures of Dsg2 Ko, nt Ko or untreated MeWo and C32 with a MDCK-C7 monolayer after 48 and 72 h. …”

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. …”

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. …”