The genome sequence of the Bordered Straw, Heliothis peltigera (Denis & Schiffermüller) 1775 by Wawman, D, Crowley, L, University of Oxford and Wytham Woods Genome Acquisition Lab, Darwin Tree of Life Barcoding collective, Wellcome Sanger Institute Tree of Life Management, Samples and Laboratory team, Wellcome Sanger Institute Scientific Operations: Sequencing Operations, Wellcome Sanger Institute Tree of Life Core Informatics team, Tree of Life Core Informatics collective, Darwin Tree of Life Consortium

The genome sequence of the Green Pug moth, Pasiphila rectangulata (Linnaeus, 1758) by Wawman, DC

The genome sequence of the Blue-bordered Carpet moth Plemyria rubiginata (Denis & Schiffermüller) 1775 by Boyes, D, Lees, DC, Wawman, DC

The formation and evolution of Earth’s inner core by Wilson, AJ, Davies, CJ, Walker, A, Pozzo, M, Alfé, D, Deuss, A

“…Mineral physics calculations suggest that a supercooling of at least 450 K is needed to nucleate the inner core, while inferences from geophysical observations constrain the maximum available supercooling to 420 K, and more likely <100 K when satisfying constraints on long-term core-mantle evolution. Supercooling requires that the inner core initially grew rapidly, comparable to the timescale of outer core dynamics, followed by a slower phase of classical equilibrium growth. …”