Why don't the gas spaces of submerged organs of wetland
plants flood extensively when damaged? In addressing this
intriguing question, Soukup et al. (pp. 71–75 in this
issue) report on the role of rhizome diaphragms as barriers
to flooding in Phragmites australis. This should prompt
some reappraisal of the ways in which flooding resistance
can be realized, even perhaps in undamaged organs.
Most emergent wetland macrophytes have an abundance
of interconnected internal gas space, much of it in the form
of large voids transversely partitioned at intervals by
perforated cellular plates termed diaphragms. Functionally,
it provides a low-resistance pathway for internal
oxygen transport to support the respiratory needs of
submerged and buried organs (Armstrong, 1979; Armstrong et al.,
1988; Crawford, 1992) and facilitates carbon
dioxide removal. However, it does more than this, since it
enables oxygen to be released from the root to where it can
support aerobic microbial activity in otherwise anaerobic
sediments, and phytotoxin immobilization or destruction
(Armstrong et al., 1992; Begg et al., 1994; Gilbert &
Frenzel, 1998). This oxygen release is regarded by some as
a valuable aid to effluent purification by constructed
wetlands. Perhaps a less desirable property of this gas-space provision is its recently discovered role in enhancing
the emissions of greenhouse gases such as methane from
wetlands (Brix et al., 1992; Chanton & Whiting, 1996;
Crutzen, 1991; Dacey & Klug, 1979).