Source water used by plants of several species in a semi-evergreen low
land tropical forest on Barro Colorado Island, Panama, was assessed by
comparing the relative abundance of deuterium, D, versus hydrogen, H
(stable hydrogen isotope composition, delta D) in xylem sap and in soi
l water at different depths, during the dry season of 1992. Ecological
correlates of source water were examined by comparing xylem water del
ta D values with leaf phenology, leaf water status determined with a p
ressure chamber, and rates of water use determined as mass flow of sap
using the stem heat balance method. Soil water delta D values decreas
ed sharply to 30 cm, then remained relatively constant with increasing
depth. Average delta D values were -13 parts per thousand, for 0-30 c
m depth and -36.7 parts per thousand for 30-100 cm depth. Soil water 6
D values were negatively associated with soil water content and soil w
ater potential. Concurrent analyses of xylem water revealed a high deg
ree of partitioning of water resources among species of this tropical
forest. Xylem water delta D of deciduous trees (average = - 25.3 +/- 1
.4 parts per thousand) was higher than that of evergreen trees (averag
e = - 36.3 +/- 3.5 parts per thousand), indicating that evergreen spec
ies had access to the more abundant soil water at greater depth than d
eciduous species. In evergreen shade-tolerant and high-light requiring
shrubs and small trees, delta D of xylem water was negatively correla
ted with transpiration rate and leaf water potential indicating that s
pecies using deeper, more abundant water resources had both higher rat
es of water use and more favorable leaf water status.