The structural basis for membrane binding and pore formation by lymphocyte perforin
The structural basis for membrane binding and pore formation by lymphocyte perforin Nature 468, 7322 (2010).
The structural basis for membrane binding and pore formation by lymphocyte perforin Nature 468, 7322 (2010).
Bottom-up effects of plant diversity on multitrophic interactions in a biodiversity experiment Nature 468, 7323 (2010). doi:10.1038/nature09492 Authors: Christoph Scherber, Nico Eisenhauer, Wolfgang W.
Climate-driven population divergence in sex-determining systems Nature 468, 7322 (2010). doi:10.1038/nature09512 Authors: Ido Pen, Tobias Uller, Barbara Feldmeyer, Anna Harts, Geoffrey M. While & Erik Wapstra Sex determination is a fundamental biological process, yet its mechanisms are remarkably diverse
Quantum tunnelling of the magnetization in a monolayer of oriented single-molecule magnets Nature 468, 7322 (2010). doi:10.1038/nature09478 Authors: M
Distant metastasis occurs late during the genetic evolution of pancreatic cancer Nature 467, 7319 (2010). doi:10.1038/nature09515 Authors: Shinichi Yachida, Si
The patterns and dynamics of genomic instability in metastatic pancreatic cancer Nature 467, 7319 (2010).
On-line, voluntary control of human temporal lobe neurons Nature 467, 7319 (2010). doi:10.1038/nature09510 Authors: Moran Cerf, Nikhil Thiruvengadam, Florian Mormann, Alexander Kraskov, Rodrigo Quian Quiroga, Christof Koch & Itzhak Fried Daily life continually confronts us with an exuberance of external, sensory stimuli competing with a rich stream of internal deliberations, plans and ruminations. The brain must select one or more of these for further processing.
Fine-scale recombination rate differences between sexes, populations and individuals Nature 467, 7319 (2010).
Late middle Eocene epoch of Libya yields earliest known radiation of African anthropoids Nature 467, 7319 (2010).
Deformation of the lowermost mantle from seismic anisotropy Nature 467, 7319 (2010). doi:10.1038/nature09507 Authors: Andy Nowacki, James Wookey & J-Michael Kendall The lowermost part of the Earth’s mantle—known as D″—shows significant seismic anisotropy, the variation of seismic wave speed with direction. This is probably due to deformation-induced alignment of MgSiO3-post-perovskite (ppv), which is believed to be the main mineral phase present in the region.