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We quantified changes in BMP-Smad signaling following perturbations of Ddr, Intβ1, and Vegfr functions to test if adhesion to the ECM regulates polarity.
We also quantified changes in overstory and understory cover, supply of downed woody debris, and disturbance to the forest floor.
We also quantified changes in biomass composition and confirmed turnover of macromolecules by applying [U-13C]glucose and [U-13C]xylose tracers.
We quantified changes in bird assemblages at the rainforest margin of Lore Lindu National Park, Central Sulawesi, over an interval of 6 years.
We quantified changes in their swimming activity and in the kinematics and geometrical properties of their motion, three important descriptors of the motility patterns of zooplankters.
We quantified changes in soil nutrient stocks, foliar nutrient concentrations, and the chemical forms of soil P along the Cooloola chronosequence, a series of coastal dunes spanning ca. 500,000 years of pedogenesis in subtropical Queensland.
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Hegerl, G. et al. Challenges in quantifying changes in the global water cycle.
DeVries et al. used a new ocean inverse-modelling approach to quantify changes in circulation.
They should also quantify changes in river run-off and water quality.
Libraries can then be analyzed by deep sequencing to quantify changes in sgRNA/shRNA abundance.
In this study, we used fractal-scaling measures to quantify changes in brain dynamics and their relation to effort.
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