Yosef Steinberger

The failure of nitrogen and lignin control of decomposition in a North American desert

We measured mass losses of both buried and surface litter of six litter types: leaves of the perennial evergreen shrub, Larrea tridentata, leaves of the winter deciduous perennials Fluorensia cernua, Prosopis glandulosa and Chilopsis linearis (a desert riparian species), an evergreen monocot, Yucca elata, and a mixture of annual plants. These species differed in lignin content and carbon-nitrogen ratios. There was no correlation between rates of mass loss and percent lignin, carbon-nitrogen ratio, or lignin-nitrogen ratio. The leaves of F. cernua and the mixed annuals exhibited the highest rates of mass loss. Surface litter of Y. elata, the mixed annuals and C. linearis exhibited higher mass loss than buried litter of the same species. The patterns of mass loss of buried and surface litter differed with buried litter mass loss occurring as a negative exponential and surface litter exhibiting low rates in winter and spring and high rates in summer. There was no correlation between mass loss in surface bags that were field exposed for 1 month and actual evapotranspiration (AET) but there was a correlation between AET and mass losses in buried litter. A model relating mass loss to AET and initial lignin content underestimated mass losses in all species examined.

Microbial biomass response to seasonal fluctuation in soil salinity under the canopy of desert halophytes

The relationships between seasonal changes in soil salinity and the microbial biomass and activity (represented by the quotient for basal respiration—qCO2) were monitored year-round under the canopy of two halophytes; Zygophyllum dumosum and Reaumuria negevensis, typical of the hot, dry Negev Desert. Fluctuations in soil salinity were assumed to be the result of different ecophysiological strategies employed by the halophytes in order to survive in saline environments. The amount of the microbial biomass was not directly affected by the degree of soil salinity, especially in the R. negevensis microhabitat where the highest biomass (245 μg g−1) was observed in high salty soil (12.8 dS m−1) during the summer. A negative relationship was found between the microbial biomass and qCO2 values, indicating the possibility of channeling organic substrates to metabolic activity aimed at overcoming conditions of temporary stress.

Decomposition of genetically engineered tobacco under field conditions : persistence of the proteinase inhibitor I product and effects on soil microbial respiration and protozoa, nematode and microarthropod populations

To evaluate the potential effects of genetically engineered (transgenic) plants on soil ecosystems, litterbags containing leaves of non-engineered (parental) and transgenic tobacco plants were buried in field plots. The transgenic tobacco plants were genetically engineered to constitutively produce proteinase inhibitor I, a protein with insecticidal activity. The litterbag contents and surrounding soil, as well as soil from control plots without litterbags, were sampled over a 5-month period at 2- to 4-week intervals and assayed for proteinase inhibitor concentration, litter decomposition rates, carbon and nitrogen content, microbial respiration rates and population levels of nematodes, protozoa and microarthropods. The proteinase inhibitor concentration in the transgenic plant litter after 57 days was 0.05% of the sample day 0-value and was not detectable on subsequent sample days. Although the carbon content of the transgenic plant litter was comparable to that of the parental plant litter on sample day 0, it became significantly lower over the course of the experiment. Nematode populations in the soil surrounding the transgenic plant litterbags were greater than those in the soil surrounding parental plant litterbags and had a different trophic group composition, including a significantly higher ratio of fungal feeding nematodes to bacterial feeding nematodes on sample day 57. In contrast, Collembola populations in the soil surrounding the transgenic plant litterbags were significantly lower than in the soil surrounding parental plant litterbags. Our results demonstrated that under field conditions proteinase inhibitor remained immunologically active in buried transgenic plant litter for at least 57 days and that decomposing parental and transgenic plant litter differed in quality (carbon content) and in the response of exposed soil organisms (Collembola and nematodes).

Soil respiration in a chihuahuan desert rangeland

Abstract Soil respiration of a desert soil was measured at the New Mexico State University Ranch in Southern New Mexico. Respiration rates were highest during late July and August after summer rains. Soil respiration data were used to estimate soil organic matter turnover which was 54 yr using summer data and 20 yr using both summer and winter data. The long turnover estimate for summer measurements resulted from temperatures above optimum in June and July. Diurnal soil respiration was also measured after a simulated 2.54 cm rain event. For both wetted and dry soils, temperature controlled the patterns of soil respiration with an optimum of near 41°C. Activation energy values decreased from 84.91 to 39.5 kJ mol −1 when the soil was wetted. A light-dark container method was tested as a possible means of estimating algal uptake of CO 2 , however, the method was not feasible for desert soils.

Phospholipid fatty acid profiles as indicators for the microbial community structure in soils along a climatic transect in the Judean Desert

Abstract Analyses of phospholipid fatty acids (PLFAs) were used to assess variations in soil microbial biodiversity, community structure and biomass, and consequently, the soil microbial successions in time along the climate gradient of the Judean Desert. Principal component analysis of the PLFA data revealed that the degree of time- and space-related variations in PLFA composition and microbial community structure was high among the desert habitats. Significant shifts of specific groups of fatty acids caused by climatic variations were observed. The biomass represented by the total amounts of PLFAs indicated that the greater the average amount of precipitation, the higher the biomass. The results indicate that at least three different microorganism strategies were probably followed: (1) in soils with a high biomass during the rainy period, a significant biomass decrease occurred during the dry period, mainly due to an extraordinary decrease of Gram-negative bacteria as indicated by the decrease of typical monounsaturated fatty acids and hydroxy-substituted phospholipid fatty acids in semi-arid climates; (2) in soils with low biomass content during the rainy period, a significant increase of biomass during the dry period occurred, due mainly to the increase of eukaryotes, Gram-positive, and Gram-negative bacteria characterized by polyunsaturated, branched chain and some of the monounsaturated fatty acids, respectively; and (3) relatively low and constant biomass during the entire observation period in the more arid zones of the Judean Desert.

Effect of irrigation on nematode population dynamics and activity in desert soils

SummaryThe nematode community in litter and soil was examined for a year in the Chihuahuan desert, before and after supplemental rainfall application. Proportions of nematode-active or anhydrobiotic forms and population densities were determined for 3 treatments: control (natural rainfall), a single, large (25-mm) monthly irrigation pulse, and 4 smaller (6-mm) irrigations spaced at weekly intervals. In litter the greatest nematode abundance was in the 6 mm week−1 treatment (48 nematodes 20 g−1 litter). Bacteriovores and fungivores accounted for approximately 95% of the numbers and biomass in all treatments. In soil, water amendments had no significant effect (P < 0.05) on annual mean densities of total nematodes, fungivores, bacterivores, or omnivore predators. Phytophage densities were greater on both irrigation treatments, with highest densities (9268 m−2) in the 6 mm week−1 soils, which was 5.9% of the total soil nematode density. Total densities of individual trophic groups were not significantly different before or after rainfall. Soil nematode densities fluctuated independently with trophic group, month, and season. Bacterial feeders and omnivore predators were the largest contributor to total soil nematode density and biomass. Prior to irrigation, there were no differences in the percentage of anhydrobiotes on the three treatments. Anhydrobiotes decreased after irrigation in all treatments, and were significantly lower in soils of the larger, monthly irrigation. Nematodes were inactive (anhydrobiotic) and decoupled from decomposition processes when soil water matric potentials reached −0.4 MPa.

Contributions of subterranean termites to the “economy” of Chihuahuan desert ecosystems

SummaryWe examined the role of subterranean termites in decomposition of cattle dung, various herbaceous plant species and wood in a Chihuahuan desert ecosystem. From July–September, termites removed dung at a rate of 0.63 g day-1 accounting for a percent mass loss of 19.5–100%. During the autumn subterranean termites consumed more than 50% of the leaves of the shrub Larrea tridentata, the grass Erioneuron pulchellum and annual plant Lepidium lasiocarpum and Baileya multiradiata but used very little of two other annuals Eriastrum diffusum and Eriogonum trichopes. Yucca inflorescence stalks on plots with termites lost 23% of their original mass in 30 months while those on termite free soils lost 11%. Elimination of termites resulted in reduction of fluff grass, Erioneuron pulchellum biomass, thereby affecting the structure of the ecosystem.

Response by soil nematode populations and the soil microbial biomass to a rain episode in the hot, dry Negev Desert

Since the amount, intensity, and frequency of rainfall in desert regions vary strongly over space and time, the response by soil biota to this variability is of great importance. We conducted a study in the Negev desert in order to examine the immediate response by the soil nematode populations and the microbial biomass to varying amounts of water applied in a single pulse. Soil samples from the 0–10-cm depth were collected from areas undergoing four different wetting treatments, comprising 5, 10, 15, and 20 mm of water, and from a non-irrigated control soil. There was a correlation between diurnal variations in nematode populations and the diurnal fluctuations in soil moisture. The greatest abundance of nematodes was found in the soil treated with 20 mm water (970 individuals 100 g-1 dry soil) which was 2, 4, 5, and 14 times larger than that found in the soil treated with 15, 10, 5, and 0 mm of water, respectively. Bacterialfeeding and fungal-feeding nematodes accounted for approximately 95% of the total nematode population found in all treatments. The microbial biomass examined in the current study exhibited an immediate response to the wetting which was greater in soil treated with, 10, 15, and 20 mm of water compared with 0 and 5 mm. However, after 4 days (96 hours) the microbial biomass stabilized again at the basic level of the 0-mm control. However, our results indicated that the major trigger for changes in the nematode populations, and in the microbial biomass, was diurnal fluctuations in soil moisture, since peaks in nematode populations and in the microbial biomass were observed at various times of the day.

A Comparison of Surface and Buried Larrea Tridentata Leaf Litter Decomposition in North American Hot Deserts

We conducted studies of mass losses from surface and buried litter bags in four North American hot desert areas to test the following hypotheses: (1) leaf litter disappearance in hot deserts is independent of actual evapotranspiration, (2) buried litter disappearance is a function of actual evapotransporation, (3) the pattern of microarthropod colonization of buried leaf litter is a function of the stage of decomposition, and (4) elimination of microarthropods results in reduced rates of decomposition and increased numbers of free—living nematodes. Mass losses from surface Larrea tridentata leaf litter bags ranked highest to lowest: Chihuahuan desert, Sonoran desert, Mojave desert, Coloradan desert. Mass losses from buried litter bags were essentially equal. °40%, in each of the deserts for bags buried from March to October. There was low correlation between rainfall and mass loss of buried litter and surface litter in the North American hot deserts. Mass losses from insecticide—treated buried bags were lower than from untreated bags. There was a greater abundance of nematodes in insecticide—treated bags than in untreated bags. Tarsonemid mites were found only in litter bags from the Chihuahuan desert. The most abundant microarthropods in buried leaf litter in the other deserts were predatory raphignathids, tydeids, and arctacarids. Decomposition (litter disappearance) in North American hot deserts was highly correlated with long—term rainfall patterns, which we hypothesize have served as the selective agents for the soil biota active in the decomposition process. Thus litter disappearance does not respond to annual fluctuations in rainfall amounts.

Decomposition along a rainfall gradient in the Judean desert, Israel.

SummaryThe effect of a rainfall gradient, from a semiarid to extremely arid, on decomposition, were studied in the Judean desert, Israel. During the study period, the rainfall gradient obtained ranged from 308 mm to 24.4 mm. There was a annual mass loss of approximately 20% and 16% in the semi-arid and extremely arid regions, respectively. No significant correlation was found between the total rainfall and total mass losses. The data suggest that in an area where the conditions are not suitable for biological activity, the decomposition processes result from abiotic conditions, like temperature and radiation.