Local ion temperature and flows are measured directly in the well-character
ized reconnection layer of a laboratory plasma. The measurements indicate s
trongly that ions are heated due to reconnection and that more than half of
the reconnected field energy is converted to ion thermal energy. Neither c
lassical viscous damping of the observed sub-Alfvenic ion flows nor classic
al energy exchange with electrons is sufficient to account for the ion heat
ing, suggesting the importance of nonclassical dissipation mechanisms in th
e reconnection layer.