Structural biology: Spliceosome subunit revealed.


are living in a time that is not ‘typical’ of the fluxes averaged over a longer timescale. This is the explanation explored by Vance and colleagues: they propose that much of the world’s land surface is suffering from a glacial hangover, and that geochemical fluxes have not yet recovered from the major perturbation of the last glacial–interglacial… (More)
DOI: 10.1038/458418a


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