Xylem cavitation in winter and recovery from cavitation in the spring were visualized in two species of diffuse-porous trees, Betula platyphylla var. japonica Hara and Salix sachalinensis Fr. Schm., by cryo-scanning electron microscopy after freeze-fixation of living twigs. Water in the vessel lumina of the outer three annual rings of twigs of B. platyphylla var. japonica and of S. sachalinensis gradually disappeared during the period from January to March, an indication that cavitation occurs gradually in these species during the winter. In April, when no leaves had yet expanded, the lumina of most of the vessels of both species were filled with water. Many vessel lumina in twigs of both species were filled with water during the period from the subsequent growth season to the beginning of the next winter. These observations indicate that recovery in spring occurs before the onset of transpiration and that water transport through twigs occurs during the subsequent growing season. We found, moreover, that vessels repeat an annual cycle of winter cavitation and spring recovery from cavitation for several years until irreversible cavitation occurs.In plants "cavitation" refers to the formation of a cavity within a body of water, usually in the xylem watertransport system (Milburn, 1991). All conduits for the transport of water in plants are potentially vulnerable to cavitation. Cavitation disrupts water transport and longterm consequences can include reduced growth and dieback of the plant. Cavitation occurs mainly in response to water stress or freezing (Tyree and Sperry, 1989), and cavitation caused by water stress has been explained in terms of air-seeding, as follows. When the tension inside xylem conduits exceeds a certain critical value, air is sucked into the lumina of water-filled conduits from adjacent gas-filled conduits through the pores of intervascular pit membranes (Zimmermann, 1983;Sperry and Tyree, 1988). By contrast, the cavitation that is caused by freezing seems to occur as a result of the low solubility of gases in ice. When frozen sap containing air bubbles thaws under tension, air bubbles expand in the xylem conduits and cavitation occurs (Zimmermann, 1983; Sperry, 1993).In dicotyledonous trees the region of the xylem that functions in water transport varies among species. In ringporous trees it is the earlywood vessels of the current-year xylem that are mainly involved in water transport (Chaney and Kozlowski, 1977; Ellmore and Ewers, 1986). The earlywood vessels lose the capacity to function in the transport of water by the end of each winter, and no refilling with water occurs in these vessels during the following spring (Zimmermann, 1983). Consequently, earlywood vessels play a role in water transport during a single growth season. The cavitation that occurs in earlywood vessels of ring-porous trees is believed to be irreversible.In diffuse-porous trees, by contrast to ring-porous trees, water transport generally occurs in a larger part of the sapwood (Greenidge, 1958; Chaney and Kozlowsk...