Development, regeneration and cancer involve drastic transitions in
tissue morphology. In analogy with the behavior of inert fluids, some of these
transitions have been interpreted as wetting transitions. The validity and scope
of this analogy are unclear, however, because the active cellular forces that
drive tissue wetting have been neither measured nor theoretically accounted for.
Here we show that the transition between two-dimensional epithelial monolayers
and three-dimensional spheroidal aggregates can be understood as an active
wetting transition whose physics differs fundamentally from that of passive
wetting phenomena. By combining an active polar fluid model with measurements of
physical forces as a function of tissue size, contractility, cell-cell and
cell-substrate adhesion, and substrate stiffness, we show that the wetting
transition results from the competition between traction forces and contractile
intercellular stresses. This competition defines a new intrinsic lengthscale
that gives rise to a critical size for the wetting transition in tissues, a
striking feature that has no counterpart in classical wetting. Finally, we show
that active shape fluctuations are dynamically amplified during tissue
dewetting. Overall, we conclude that tissue spreading constitutes a prominent
example of active wetting — a novel physical scenario that may explain
morphological transitions during tissue morphogenesis and tumor progression.