Groundwater depletion threatens many riparian ecosystems in arid and semi‐arid regions of the world. The aquifer that sustains Arizona's San Pedro River riparian ecosystem, for example, is threatened by regional groundwater declines and localized pumping from the alluvial aquifer. This paper demonstrates the important role of shallow groundwater in structuring the San Pedro River plant community, portions of which function as reference areas that indicate site potential for a globally rare forest type (Sonoran riparian Populus‐Salix forests). Several ecological indicators varied with depth to groundwater, including a weighted average wetland indicator score calculated for herbaceous and woody plant species, cover of plants within wetland indicator groups, and frequency of indicator plant species. These relationships can be used in a space‐for‐time substitution to predict consequences of groundwater decline. For example, the wetland indicator score changed sharply as depth to groundwater ranged from 0 to 4 m, and abundance of obligate wetland herbs (the group most sensitive to groundwater changes) declined sharply at groundwater depths below ≈ 0.25 m. Such sequential desertification of the riparian flora (i.e., loss or reduction in cover of species based on their probability of occurrence in wetlands) is one predicted response to groundwater decline. Other predicted impacts of groundwater decline include reduced establishment of Populus fremontii‐Salix gooddingii forests, and reduced cover of herbaceous species associated with the fine‐textured soils and shady conditions of floodplain terraces stabilized by these early seral tree species. High floodplain terraces (depth to groundwater of 5‐8 m) had wetland indicator scores below those of upland sites and were vegetated by species (e.g., Prosopis velutina and Sporobolus wrightii) with low sensitivity to groundwater changes.

Summary 1We investigated resource limitations in a saltbrush scrub community along a salinityalkalinity gradient in the Mojave Desert of North America. Previous studies have shown that, as productivity declines with increasing soil stress, there are parallel declines in leaf Ca and Mg, suggesting availability of these resources may limit growth in addition to water, N and P limitations expected in deserts. 2 To determine which soil resources limited growth of the dominant shrub, Atriplex parryi , and whether this differed along the soil stress gradient or among life stages, water and nutrients were applied in combination at different rates to plants at high-and low-stress sites. We developed and applied a conceptual model to identify resource limitations from this experiment. We also investigated how those limitations interacted to influence A. parryi growth and physiological function at the high-stress site. 3 Availability of soil N and P limited growth at the low-stress site and N, P and Mg limited growth at the high-stress site for both adult and juvenile life stages. There was no evidence that availability of water alone or K, Ca or other nutrients, or increasing soil Na and B, limited growth along the soil stress gradient. 4 When N, P, Mg and water were supplied in combination, plant growth increased more than 16-fold. Supply of these resources interacted to influence both plant growth and function. Because of the high demand for N relative to other resources, N supply rate was the major driver of these interactions, influencing the magnitude by which P and Mg affected growth. The major mechanism behind these growth responses was an increase in allocation to leaves relative to fine roots, rather than nutrient or water effects on water relations, photosynthesis or water use efficiency. 5 Multiple, interacting resources limit the growth and distribution of A. parryi on a saline, alkaline Mojave Desert site. Similar interactions between multiple limiting resources are likely to be instrumental in shaping community and species distributions along other abiotic stress gradients.

Plant species and functionally related species groups from arid and semi-arid habitats vary in their capacity to take up summer precipitation, acquire nitrogen quickly after summer precipitation, and subsequently respond with ecophysiological changes (e.g. water and nitrogen relations, gas exchange). For species that respond ecophysiologically, the use of summer precipitation is generally assumed to affect long-term plant growth and thus alter competitive interactions that structure plant communities and determine potential responses to climate change. We assessed ecophysiological and growth responses to large short-term irrigation pulses over one to three growing seasons for several widespread Great Basin and northern Mojave Desert shrub species: Chrysothamnus nauseosus, Sarcobatus vermiculatus, Atriplex confertifolia, and A. parryi. We compared control and watered plants in nine case studies that encompassed adults of all four species, juveniles for three of the species, and two sites for two of the species. In every comparison, plants used summer water pulses to improve plant water status or increase rates of functioning as indicated by other ecophysiological characters. Species and life history stage responses of ecophysiological parameters (leaf N, delta15N, delta13C, gas exchange, sap flow) were consistent with several previous short-term studies. However, use of summer water pulses did not affect canopy growth in eight out of nine comparisons, despite the range of species, growth stages, and site conditions. Summer water pulses affected canopy growth only for C. nauseosus adults. The general lack of growth effects for these species might be due to close proximity of groundwater at these sites, co-limitation by nutrients, or inability to respond due to phenological canalization. An understanding of the connections between short-term ecophysiological responses and growth, for different habitats and species, is critical for determining the significance of summer precipitation for desert community dynamics.

No abstract

No abstract