Latitudinal gradients in tree ring stable carbon and oxygen isotopes reveal differential climate influences of the North American Monsoon System
Paul Szejner
Université d'Arizona
Jeudi 12/01/2017, 11:00-12:00
Bât. 701, P. 17C, LSCE Orme des Merisiers
The arrival of the North American Monsoon System (NAMS) terminates a
presummer hyperarid period in the southwestern United States (U.S.),
providing summer moisture that is favorable for forest growth. Montane
forests in this region rely on winter snowpack to drive much of their
growth; the extent to which they use NAMS moisture is uncertain. We
addressed this by studying stable carbon and oxygen isotopes in
earlywood and latewood from 11 sites along a latitudinal gradient
extending from Arizona and
New Mexico to Utah. This study provides the first regional perspective
on the relative roles of winter versus summer precipitation as an
ecophysiological resource. Here we present evidence that Ponderosa pine
uses NAMS moisture differentially across this gradient. 13C/12C ratios
suggest that photosynthetic water use
efficiency during latewood formation is more sensitive to summer
precipitation at the northern than at the southern sites. This is likely
due to the fact that NAMS moisture provides sufficiently favorable
conditions for tree photosynthesis and growth during most years in the
southern sites, whereas the northern sites
experience larger summer moisture variability, which in some years is
limiting growth. Cellulose δ18O and δ13C values revealed that
photoassimilates in the southern sites were produced under higher vapor
pressure deficit conditions during spring compared to summer,
demonstrating a previously underappreciated effect
of seasonal differences in atmospheric humidity on tree ring isotope
ratios. Our findings suggest that future changes in NAMS will
potentially alter productivity and photosynthetic water use dynamics
differentially along latitudinal gradients in southwestern U.S. montane
forests.