We studied the flood tolerance of five tree species growing in the flooded
forest adjacent to the Mapire river, in SW Venezuela, Mean photosynthetic r
ate and leaf conductance were 11 mu mol m(-2) s(-1) and 700 mmol m-2 s(-1),
respectively. Xylem water potential ranged from -0.08 to -1.15 MPa, Based
on leaf gas exchange as a criterion of tolerance to flooding, two response
patterns were identified: (1) decreasing photosynthetic rate with increasin
g flooding and leaf conductance (Psidium ovatifolium Berg. ex Desc., Campsi
andra laurifolia Benth., Symmeria paniculata Benth. and Acosmium nitens (Vo
g.) Benth); and (2) independence of photosynthesis and leaf conductance fro
m flooding (Eschweilera tenuifolia (Berg.) Miers,). In the first response p
attern, declining photosynthetic rate with flooding may be interpreted as a
sign of reduced flood tolerance, whereas the second response pattern may i
ndicate increased flood tolerance. An increase in xylem water potential wit
h depth of water column was found for all species (with the possible except
ion of P. ovatifolium), indicating that flooding does not cause water stres
s in these trees. Submerged leaves that had been under water for between fo
ur days and four months generally had photosynthetic rates and leaf conduct
ances similar to those of aerial leaves, indicating maintenance of photosyn
thetic capacity under water. Daily positive oscillations in glucan content
in submerged leaves of P. ovatifolium and C. laurifolia suggest that submer
ged leaves do not represent a sink for photosynthates produced by aerial le
aves.