Effects of Infant Pneumococcal Conjugate Vaccination on Serotype Distribution in Invasive Pneumococcal Disease among Children and Adults in Germany by Mark van der Linden (109670)

“…After the switch from PCV7 to PVC10/PCV13 for infant vaccination in 2010, serotypes 1, 6A and 7F significantly decreased. A decrease in serotype 19A was only observed in 2013–2014, as compared to 2010–2011 (children p = 4.16E-04, adults p = 6.98E-06). …”

Tau knockout prevents sensitivity to Kainic acid–mediated stress in AICD-Tg mice. by Kaushik Ghosal (244754)

“…C. Mean seizure severity scores showed a significant rescue of seizure severity by Tau-/- in AICD animals. n = 4–5 mice per group (A-C). …”

Differential expression across salinity gradients of the CRCM compared to seasonal tidal freshwater baselines. by Maria W. Smith (239878)

“…Expression data are colored according to fold changes in the mRNA levels (displayed using a logarithmic scale). …”

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 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)

Preparation of high concentration coal water slurry with good fluidity based on preferentially modified ultrafine particle under three-peak grading by Dingsong Yao (14007582)

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)