Field experiments and observations were used to define the functional roles and relationships of species in the rocky mid-intertidal community at Pelican Point in the northern Gulf of California. This approach provided resolution of the influences of grazing, predation, competition, and abiotic factors on community structure, and of the direct and indirect effects involved in species interactions. Competition for space, apparently via space pre-emption, between the barnacle Chthamalus anisopoma and encrusting algae of the genus Ralfsia was consistently evident. Grazing by the limpet Collisella strongiana was shown to limit algal abundance and bring about the replacement of Ralfsia by Chthamalus. Chthamalus also excluded Collisella from the rock surface. Predation on Chthamalus by the thaidid gastropod Acanthina angelica increased the abundances of both Ralfsia and Collisella. Some of the temporal variations in community structure observed during this study were clearly linked to variations in the abundances of Acanthina and Collisella and the above interactions. This relatively simple community, existing in what seems a rigorous physical environment, was characterized by strong, highly interdependent biological interactions. Indirect effects were consistently important in species interactions. An intriguing result of this study was the emergence of indirect mutualism between Acanthina and Collisella; this interaction appears to contribute to the persistence and continuing influences of both consumer species, and hence may be of major importance in the organization of this community. The zonation of the barnacles Chthamalus anisopoma and Tetraclita stalactifera at Pelican Point and elsewhere in the Gulf was examined in a test of recent ideas relating ecological and evolutionary patterns in barnacles to morphology and competition for space. Experiments and observations indicated the restriction of Tetraclita to the upper part of the shore by competition from Chthamalus, with Tetraclita able to survive above Chthamalus by virtue of greater tolerance to exposure. These results were in direct opposition to the presumed competitive dominance of large, rapidly-growing, tubiferous barnacles like Tetraclita. Comparisons with results from other shores suggested that numerical dominance goes hand-in-hand with competitive dominance in acorn barnacles. Morphological differences appear to be of minor importance.

Evapotranspiration rates of plots with vegetative cover and evaporation rates from bare soil differed during the active growing season of desert hackberry (Celtis pallida) plants but total water losses from both plots for the year were the same. Thermally induced vapor flux appeared to contribute insignificantly to moisture movement under the desert hackberry plant. The difference in measured available soil moisture was independent of location from the plant center during the growing season. During the winter months, when the plants were semidormant, soil moisture measurements had more variability and measurement locations appeared to be important due to differential rainfall input. The determined soil moisture release curve and soil water conductivity values (using an in situ technique) appeared to be representative of the conditions at the study site. A model using soil and plant parameters predicted evapotranspiration rates during the active growing season of the plants when water was not a limiting factor. Calculated results using the model were unreliable when plants were under stress -- very low soil water content. Monitoring of climatic parameters delineated only major differences in surface albedo and net radiation between plant cover and bare ground. Potential evapotranspiration estimations were high but within acceptable bounds for desert conditions. Plant diffusion resistance for the desert hackberry plant, determined from a climatological model and measured soil moisture changes, appeared to increase linearly with decreasing soil moisture until it reached a critical value, below which it rose sharply.

Arid and semi-arid ecosystems of the southwestern U.S. are experiencing major changes that have profound impacts for community structure and ecosystem function. First, these ecosystems are experiencing dramatic shifts in vegetation composition as a result of the invasion of non-native species. Second these ecosystems are predicted to undergo substantial shifts in climate regime, which include increases in the variability and frequency of extreme temperature and precipitation events. It is not well understood how these current and predicted changes will affect the physiological performance of different plant types in arid and semi-arid ecosystems. To address the effect of these changes, this dissertation focused on the photosynthetic response of a native and non-native grass species, and dominant shrub species to precipitation across contrasting soil surfaces in southeastern Arizona. The native and non-native grasses were exposed to wet and dry seasonal precipitation and responses to precipitation events ('pulses') were measured over the course of a summer growing season. To gain a mechanistic understanding of these patterns, the biochemical and diffusion limitations to photosynthetic function were measured over the course of a pulse period. Building on this foundation, natural stands of the non-native grass species were exposed to sequences of different sized pulse events. The physiological performance of a dominant shrub species, Larrea tridentata, was measured in order to determine the biochemical and diffusional constraints to photosynthetic function across seasons and contrasting soil surfaces. The results showed that leaf area development of these grass species affects water availability and time lags in photosynthetic response. Initial soil moisture conditions across contrasting soil surfaces influence the magnitude of photosynthetic response in grasses. Large photosynthetic responses of the non-native grass require large and consecutive precipitation pulses. Co-limitation of photosynthesis of Larrea tridentata by diffusion and biochemistry does not illustrate typical trends across seasons and soil surfaces. Overall results demonstrate the importance of determining the mechanisms responsible for observed leaf-level photosynthetic patterns across individual pulse events, seasons, and contrasting soil surfaces. This is especially important for predicting the magnitude of the response of plant communities in arid and semi-arid ecosystems to species invasions and changes in climate.

Awarded second place in Biological Sciences for GPSC Student Showcase

See also: Jojoba: An Annotated Bibliographic Update (1978), in the Additional Links field

From the 1840s to 1950s, interpretations of nature played a central role in the defining and enculturating the Sonoran Desert into the American nation. Written works and physical nature like plants became an archive for cultural interpretations of the region. Scientific descriptions of nature became stories of place as they were consumed. Proxy landscapes like national monuments became the spaces for demonstrating these stories. Throughout the period of this study, a constant give and take between regional nature and global arid lands shaped the national interpretations used to describe regional nature within the American nation-state. This work follows the production and consumption of meaning and the definition of a desert region.

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The rate at which volatile organic compounds (VOCs) are removed from the vadose zone by forced ventilation may be reduced by slow micro-scale processes such as diffusion through intra-aggregate and pore water and slow reactions at sorption sites located at the soil-water interface. Column experiments using benzene and p-xylene were performed in order to simulate cleanup of VOC's in the vadose zone by forced ventilation. Analytical solutions of the one-dimensional advection-dispersion equation coupled to mass transfer equations were fitted to the data. Parameter estimates were used in order to determine time scales of diffusion through water, desorption from, and sorption to, soil organic matter. Lower limits for the time scales for these processes were calculated to be on the order of minutes. Results indicate that these micro-scale processes reduce the rate of removal on the laboratory scale but may have no effect on the field scale.

No description available.