Contents

20 March 2020
Vol 367, Issue 6484
  • Special Issue

  • Contents

    • This Week in Science

    • Editorial

    • Editors' Choice

    • Products & Materials

      • New Products

        A weekly roundup of information on newly offered instrumentation, apparatus, and laboratory materials of potential interest to researchers.

    • In Brief

    • In Depth

    • Feature

      • Sick time

        Dozens of diseases wax and wane with the seasons. Will COVID-19?

    • Working Life

    • Letters

    • Books et al.

    • Policy Forum

      • Time for NIH to lead on data sharing

        A draft policy is generally supportive but should start mandating data sharing

    • Perspectives

    • Research Articles

      • Insights into human genetic variation and population history from 929 diverse genomes

        Genomes from diverse human populations record human genetic diversity and illuminate the history of our species.

      • The genetic architecture of the human cerebral cortex

        Common genetic variation is associated with interindividual variation in the structure of the cortex of the human brain.

      • Structural basis of Gs and Gi recognition by the human glucagon receptor

        Structures of a G protein–coupled receptor bound to two different G proteins reveal molecular details that govern G protein selectivity.

      • Resolving spatial and energetic distributions of trap states in metal halide perovskite solar cells

        The distributions of trap states in metal halide perovskite solar cells were measured with drive-level capacitance profiling.

    • Reports

    • From the AAAS Office of Publishing

    • Technical Comments

      • Response to Comment on “Amphibian fungal panzootic causes catastrophic and ongoing loss of biodiversity”

About The Cover

Cover image expansion

COVER An iceberg from Antarctica drifts in the Southern Ocean. Mass loss from the Antarctic Ice Sheet, whether by iceberg calving or melting, will help determine the future of sea level in our warming climate. How the ice sheet changes over the coming decades to centuries will depend on its structure, dynamics, and interactions with the atmosphere and surrounding ocean. See page 1316.
Photo: Michel Roggo