Response of Mesquite (Prosopis velutina Woot.) Carbon-Water Relations to Variations in Soil Texture and Precipitation
Abstract (Summary)
Variability in climate and rainfall are commonly cited by aridland ecologists
to explain shifts in plant community structure and land-cover change in waterlimited
environments. While pulses of precipitation undoubtedly play an important
role in driving vegetation dynamics of arid and semiarid lands, the relationship
between precipitation and plant-water acquisition is not straightforward. The
amount of soil moisture that is effectively available to plants is ultimately
controlled by a complex combination of biotic and abiotic factors such as physical
soil attributes and plant developmental stage. This indirect relationship between
precipitation and plant water uptake can lead to profound differences in plant
distribution and ecosystem function across arid and semiarid landscapes, greatly
contributing to mesoscale physiognomic heterogeneity.
In this doctoral research I investigated the interaction between soil texture
and summer precipitation and its implications on the carbon-water acquisition of
a widespread woody legume: velvet mesquite (Prosopis velutina Wooten).
Specifically, the goal was to answer the following questions: how are precipitation
pulses translated into plant-available water across different soil types? Do
mesquite responses to different sized pulses vary across soils with different soil
textures? Does the response of mesquite to pulses of precipitation vary with
ontogeny?
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This research revealed that variations in soil texture across the landscape
led to differential utilization of seasonal precipitation by mesquite trees beginning
in the earliest stages of mesquite development. Specifically, we found that on
coarse-textured soils both adult and one year old mesquites are highly coupled to
and dependent on the occurrence of both large and small summer precipitation
pulses. In contrast, on fine textured soils, the response of mesquite to both large
and small summer precipitation pulses is limited by the presence in the soil of
antecedent winter water. Substantial differences in seasonal water balance
between mesquite occurring on different soil textures were also detected with
mesquite on fine-textured soils experiencing a smaller pre-monsoon water deficit
than mesquite on coarse-textured soils.
Differential utilization of seasonal water by mesquite across the landscape
coupled with predicted changes in seasonal precipitation may have important
consequences in future patterns of plant community structure and ecosystem
water balance of this semi-arid lands.
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Bibliographical Information:
Advisor:
School:The University of Arizona
School Location:USA - Arizona
Source Type:Master's Thesis
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