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October 3, 2011 - Volume 89, Number 40
- p. 35
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New results in total synthesis reinvigorate a 40-year-old field of research.
Disagreement on conservation course of action complicates a potential reopening.
Researchers zero in on the pathways that allow cancer to bounce back after treatment.
Making the iconic pants requires both color-addition and color-removal chemistry.
Materials Science: Chemists observe metal objects sloughing off ions to form nanoparticles.
Chemical Biology: Methylated bases in mRNA may have roles in gene regulation and obesity.
Microfluidics: Automated chip is designed to detect extraterrestrial amino acids.
Publishing: Jonathan Sweedler to take the helm.
Yale updates policies on machine shop use after student death.
Conservation scientists seek new ways to keep modern paintings looking their best.
Studies could lead to sensitive and selective analyses for tiny signaling agent.
Materials Science: Guidelines predict structures formed by nanoparticles and DNA linkers.
Molecular Biology: Technique tags and enriches cells genetically altered by nucleases.
Electronics: Metal-carbon bonds increase electrical conductance.
Stereochemistry: Enzymelike pocket that hosts chiral species controls catalyst's enantioselectivity.
For the first time, seasonal ozone loss in the stratosphere over the Arctic qualifies as a full-blown “ozone hole.” Although winter-spring ozone holes over the Antarctic, associated with extreme cold and chlorofluorocarbons and other ozone-depleting chemicals, have been documented since the 1980s, ozone loss over the milder Arctic had been far less dramatic. An international team led by Gloria L. Manney at NASA’s Jet Propulsion Laboratory now shows that in 2011 the amount of ozone loss in the Arctic was comparable to that in some early Antarctic ozone holes. (Nature, DOI: 10.1038/nature10556). The cause, they believe, stems from an unusually lengthy cold period—conditions that promote formation of stratospheric clouds, providing surfaces on which reactions that convert chlorine into ozone-destroying species such as ClO take place. The researchers comment that atmospheric behavior in the Arctic is still poorly understood, and thus scientists are unable to predict if or when another major ozone loss will occur there.
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