Particle-in-cell simulations are used to investigate collisionless magnetic
reconnection in thin current sheets, based on the configuration chosen for
the Geospace Environment Modeling (GEM) magnetic reconnection challenge [B
irn et al., this issue]. The emphasis is on the overall evolution, as well
as details of the particle dynamics in the diffusion region. Here electron
distributions show clear signatures of nongyrotropy, whereas ion distributi
ons are simpler in structure. The investigations are extended to current sh
eets of different widths. Here we derive a scaling law for the evolution de
pendence on current sheet width. Finally, we perform a detailed comparison
between a kinetic and Hall-magnetohydrodynamic model of the same system. Th
e comparison shows that although electric fields appear to be quite similar
, details of the evolution appear to be considerably different, indicative
of the role of further anisotropies in the ion pressures.