Continental and global effects of different Δ<em>T</em>_g levels by Dieter Gerten (557088)

“…Projections are based on a new, consistent set of 152 climate scenarios (eight Δ<em>T</em>_g trajectories reaching 1.5–5 ° C above pre-industrial levels by 2100, each scaled with spatial patterns from 19 general circulation models). …”

Presentation1.ppt by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Table1.xlsx by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Image1.JPEG by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Table4.XLSX by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Table2.xlsx by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Table3.XLSX by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Presentation1.pptx by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Image4.jpg by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Image2.JPEG by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

Image3.jpg by Julien Leuthold (4921660)

“…We show that partial resorption textures and geochemical zoning result from partial melting of REE-poor lower oceanic crust gabbroic cumulate (protolith) following intrusion by hot primitive mantle-derived melt, and subsequent overgrowth crystallization (refertilization) from a hybrid melt. In addition, toward the outer rims of crystals, Ti, Zr, Y and the REE strongly increase and Al, Cr, Mg#, Eu/Eu^*, and Sr/Sr^* decrease, suggesting crystallization either from late-stage percolating relatively differentiated melt or from in situ trapped melt. …”

DataSheet1_Glycine Ameliorates Endoplasmic Reticulum Stress Induced by Thapsigargin in Porcine Oocytes.pdf by Sicong Yu (10732777)

“…<p>The endoplasmic reticulum (ER) is a multifunctional organelle in the cytoplasm that plays important roles in female mammalian reproduction. …”

The effect of <i>PNPLA4</i> variant on mitochondrial function. by Masakazu Kohda (206767)

“…(<b>F</b>) mito-TurboRFP-V5 and PNPLA-V5 proteins in the mitochondria of patient cells with stable expression of <i>mito-TurboRFP-V5 or PNPLA4-V5</i> cDNA were detected by SDS-PAGE/Western blotting. …”

Phacoemulsification with Kahook Dual Blade goniotomy in eyes with medically treated glaucoma: analysis of surgical outcomes and success predictors by Larissa Fouad Ibrahim (10367102)

“…Results: A total of 47 patients (57 eyes) were included (mean age, 70.5 ± 7 years). …”

Comparisons of the DEGs between microarray and the mRNA-Seq. by Nupur Dasgupta (180790)

“…<p>DEGs were identified in 9V/null vs. WT spleen by Mixed Model ANOVA (microarray) and DESeq and edgeR (mRNA-Seq). …”

The benefit of Silybum marianum in ethanol-induced reprotoxicity of male Wistar rat by Amina Talbi (12653676)

Cephalometric changes during aging in subjects with normal occlusion by Daniela GARIB (12682165)

Minor temperature shifts do not affect chromosomal ploidy but cause transcriptomic changes in Leishmania braziliensis promastigotes in vitro by Nathalia Ballesteros (8776682)

Participation of hepatic α/β-adrenoceptors and AT1 receptors in glucose release and portal hypertensive response induced by adrenaline or angiotensin II by L.J.T. de Araújo (5994071)

Effect of CCN6 inhibition on the phenotype of mammary epithelial cells by Yanhong Zhang (15518)