Many insects exchange respiratory gases cyclically and discontinuously
. A typical discontinuous gas exchange cycle (DGC) starts with a close
d-spiracle (C) phase, during which little external gas exchange takes
place, followed by a fluttering-spiracle (F) phase, which is usually d
ominated by diffusive oxygen uptake. The DGC is terminated by an open-
spiracle (O) phase, during which accumulated CO2 escapes. This review
critically examines the applicability of the DGC to insect gas exchang
e in general, discusses the primary mechanisms of gas exchange in the
F and O phases, evaluates the widespread hypothesis that the DGC lower
s respiratory water loss rates adaptively, and proposes new hypotheses
concerning the evolutionary genesis of the DGC in insects and other t
racheate arthropods.