Climate-Induced Range Shifts and Possible Hybridisation Consequences in Insects by Rosa Ana Sánchez-Guillén (485512)

Wireless Battery-Free Broad-Band Sensor for Wearable Multiple Physiological Measurement by Yixin Liu (156717)

Model for active compensation by feedback and shared regulation. by Pétra Vande Zande (17628246)

Stratification to predict the response to antioxidant by Cristiane Ritter (296603)

Video_4_Pak1 Kinase Promotes Activated T Cell Trafficking by Regulating the Expression of L-Selectin and CCR7.AVI by Ana Dios-Esponera (6422411)

Video_5_Pak1 Kinase Promotes Activated T Cell Trafficking by Regulating the Expression of L-Selectin and CCR7.AVI by Ana Dios-Esponera (6422411)

Video_6_Pak1 Kinase Promotes Activated T Cell Trafficking by Regulating the Expression of L-Selectin and CCR7.AVI by Ana Dios-Esponera (6422411)

Evaluation of anionic surfactant removal by anaerobic degradation of commercial laundry wastewater and domestic sewage by Clara Vieira de Faria (4682032)

“…The reactor was operated in three stages, all under mesophilic conditions and with a hydraulic retention time of 36 h. At stage I, the laundry wastewater was diluted with tap water (influent: 15.3 ± 4.9 mg LAS/L); at stage II, 50% of the feed volume was domestic sewage and 50% was a mixture of tap water and laundry wastewater (influent: 15.8 ± 4.9 mg LAS/L); and at stage III, only domestic sewage was used as a diluent of the laundry wastewater (influent: 24.1 ± 4.1 mg LAS/L). …”

Description analysis of the main variables. by Li Siyao (18510148)

Oct4 actively enhances the proliferation of ATSC cells along with the overexpression of pluripotency related genes and telomerase activation. by Jung Hwan Kim (259298)

Anthropometric measures comparison of elderly residents in urban area in southern Brazil by sex and age group by Arethuza Sass (10421561)

Effect of drug interactions between carbapenems and valproate on serum valproate concentration: a systematic review and meta-analysis by Pony Yee-Chee Chai (9920787)

Caddisfly biodiversity in Pernambuco state, Brazil: overcoming the biodiversity knowledge shortfall and insights into the effects of climate change by Rafael Pereira (6635264)

“…Climate projections indicate a significant decrease in the temperature range, shifting from the current 13.2–33.6 °C to 17.9–33.6 °C, and precipitation range will decrease from 507 to 1948 mm³/year to 528–1428 mm³/year. …”

Presentation1.ppt by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Table1.xlsx by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Image1.JPEG by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Table4.XLSX by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Table2.xlsx by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Table3.XLSX by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”

Image4.jpg by Julien Leuthold (4921660)

“…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr^* ratios increase. …”