The axial and radial refilling with water of cut dry branches (up to 80 cm tall) of the resurrection plant
Myrothamnus flabellifolia was studied in both acro- and basipetal directions by using 1H-NMR imaging. NMR
measurements showed that the conducting elements were not filled simultaneously. Axial water ascent occurred
initially only in a cluster of a very few conducting elements. Refilling of the other conducting elements and of the
living cells was mainly achieved by radial extraction of water from these initial conducting elements. With time,
xylem elements in a few further regions were apparently refilled axially. Radial water spread through the
tissue occurred almost linearly with time, but much faster in the acropetal than in the basipetal direction.
Application of hydrostatic pressure (up to 16 kPa) produced similar temporal and spatial radial refilling patterns,
except that more conducting elements were refilled axially during the first phase of water rise. The addition of
raffinose to the water considerably reduced axial and radial spreading rates. The polarity of water climbing was
supported by measurements of the water rise in dry branches using the ‘light refraction’ (and, sometimes, the ‘leaf
recurving’) method. Basipetal refilling of the xylem conduit exhibited biphasic kinetics; the final rise height did
not exceed 20–30 cm. Three-cm-long branch pieces also showed a directionality of water climbing, ruling out the
possibility that changes in the conducting area from the base to the apex of the branches were responsible for this
effect. The polarity of water ascent was independent of gravity and also did not change when the ambient
temperature was raised to c. 40 °C. At external pressures of 50–100 kPa the polarity disappeared, with basipetal
and acropetal refill times of the xylem conduit of tall branches becoming comparable. Refilling of branches dried
horizontally (with a clinostat) or inverted (in the direction of gravity) showed a pronounced reduction of the
acropetal water rise to or below basipetal water climbing level (which was unaffected by this treatment). Unlike
water, benzene and acetone climbing showed no polarity. In the case of benzene, the rise kinetics (including the
final heights) were comparable with those measured acropetally for water, whereas with acetone the rise height was
less. Transmission electron microscopy of dry branches demonstrated that the inner surfaces of the conducting
tracheids and vessels were lined with a continuous osmiophilic (lipid) layer, as postulated by the kinetic analysis
and light microscopy studies. The thickness of the layer varied between 20 and 80 nm. The parenchymal and
intervessel pits as well as numerous tracheid corners contained opaque inclusions, presumably also consisting of
lipids. Electron microscopy of rehydrated plants showed that the lipid layer was either thinned or had
disintegrated and that numerous vesicle-like structures and lipid bodies were formed (together with various
intermediate structural elements). These, many other data and the physical–chemical literature imply that several
(radial) driving forces (such as capillary condensation, Marangoni forces, capillary, osmotic and turgor pressure
forces) operate when a few conducting elements become axially refilled with water. These forces apparently lead
to an avalanche-like radial refilling of most of the conducting elements and living cells, and thus to the removal
of the ‘internal cuticle’ and of the hydrophobic inclusions in the pits. The polarity of water movement presumably
results from high resistances in the basipetal direction, which are created by local gradients in the thickness of the
lipid film as a result of draining under gravity in response to drought. There are striking similarities in morphology
and function between the xylem-lining lipid film and the lung surfactant film lining the pulmonary air spaces of
mammals.