Stream hydraulics as a major determinant of benthic invertebrate zonation patterns

SUMMARY. 1. Studies on the zonation of benthic fauna in fourteen streams situated in a variety of latitudes from Alaska to New Zealand have been evaluated.
2. We suggest that physical characteristics of flow ('stream hydraulics') are the most important environmental factor governing the zonation of stream benthos on a world-wide scale.
3. From the source to the mouth of a stream, zones of transition in stream hydraulics' occur, to which the general pattern of stream invertebrate assemblages can be related. In these zones benthic community stability and resilience must be different from those upstream and downstream of the hydraulic transition zones.     

Disturbance, rainfall and contrasting species responses mediated aboveground biomass response to 11 years of CO2 enrichment in a Florida scrub-oak ecosystem

This study reports the aboveground biomass response of a fire-regenerated Florida scrub-oak ecosystem exposed to elevated CO₂ (1996–2007), from emergence after fire through canopy closure. Eleven years exposure to elevated CO₂ caused a 67% increase in aboveground shoot biomass. Growth stimulation was sustained throughout the experiment; although there was significant variability between years. The absolute stimulation of aboveground biomass generally declined over time, reflecting increasing environmental limitations to long-term growth response. Extensive defoliation caused by hurricanes in September 2004 was followed by a strong increase in shoot density in 2005 that may have resulted from reopening the canopy and relocating nitrogen from leaves to the nutrient-poor soil. Biomass response to elevated CO₂ was driven primarily by stimulation of growth of the dominant species, Quercus myrtifolia , while Quercus geminata , the other co-dominant oak, displayed no significant CO₂ response. Aboveground growth also displayed interannual variation, which was correlated with total annual rainfall. The rainfall × CO₂ interaction was partially masked at the community level by species-specific responses: elevated CO₂ had an ameliorating effect on Q. myrtifolia growth under water stress. The results of this long-term study not only show that atmospheric CO₂ concentration had a consistent stimulating effect on aboveground biomass production, but also showed that available water is the primary driver of interannual variation in shoot growth and that the long-term response to elevated CO₂ may have been caused by other factors such as nutrient limitation and disturbance.     

Biogeography and contemporary climatic differentiation among Moroccan Salamandra algira

The opening of the Gibraltar land bridge occurred at the end of the Messinian Salinity Crisis approximately 5.3 Mya, and was one of the main causes of vicariance between European and north‐west African amphibians, resulting in the origin of several new species. However, little is currently known about the causes for post‐Messinian amphibian differentiation in the Maghreb, although it is acknowledged that the Pleistocene glaciations probably had considerable influence on several species. The current study uses both species distribution modelling (MAXENT) and information from a total of 694 bp of mitochondrial data (351 from cytochrome b and 342 from 12S rRNA) from 36 representatives of all three recognized subspecies of Moroccan Salamandra to infer the phylogeny and biogeography of Salamandra algira tingitana, which is characterized by both viviparous and ovoviviparous populations. According to the results, the split between S. a. tingitana and S. a. algira from the Rif and Middle Atlas mountains took place approximately 1.6 Mya, and could have been caused by a shift towards a colder and drier climate that occurred during the upper Pliocene, which may have resulted in the isolation of Salamandra at increasingly higher altitudes, or in other climatically favourable areas. Several lineages within S. a. tingitana originated during the Pleistocene climatic oscillations, one of which gave rise to the viviparous populations north of the Oued Martil. It is suggested that the origin of viviparity in S. a. tingitana occurred during the last 600 000 years. In order to further understand the origin of the unique viviparous population of S. algira from North Africa, predictive distribution models of the viviparous and ovoviviparous populations of S. a. tingitana were created using MAXENT to assess environmental differences. Niche divergence was subsequently determined using Schoener's D and Warren et al.'s I niche similarity metrics. Predictive modelling and niche divergence analyses revealed significant environmental differences between the two reproductive types, which could have influenced the transition from ovoviviparity to viviparity. © 2010 The Linnean Society of London, Biological Journal of the Linnean Society, 2010, 101 , 626–641.     

Elevated CO2 increases the long-term decomposition rate of Quercus myrtifolia leaf litter

Decomposition of Quercus myrtifolia leaf litter in a Florida scrub oak community was followed for 3 years in two separate experiments. In the first experiment, we examined the effects CO₂ and herbivore damage on litter quality and subsequent decomposition. Undamaged, chewed and mined litter generated under ambient and elevated (ambient+350 ppm V) CO₂ was allowed to decompose under ambient conditions for 3 years. Initial litter chemistry indicated that CO₂ levels had minor effects on litter quality. Litter damaged by leaf miners had higher initial concentrations of condensed tannins and nitrogen (N) and lower concentrations of hemicellulose and C : N ratios compared with undamaged and chewed litter. Despite variation in litter quality associated with CO₂, herbivory, and their interaction, there was no subsequent effect on rates of decomposition under ambient atmospheric conditions. In the second experiment, we examined the effects of source (ambient and elevated) of litter and decomposition site (ambient and elevated) on litter decomposition and N dynamics. Litter was not separated by damage type. The litter from both elevated and ambient CO₂ was then decomposed in both elevated and ambient CO₂ chambers. Initial litter chemistry indicated that concentrations of carbon (C), hemicellulose, and lignin were higher in litter from elevated than ambient CO₂ chambers. Despite differences in C and fiber concentrations, litter from ambient and elevated CO₂ decomposed at comparable rates. However, the atmosphere in which the decomposition took place resulted in significant differences in rates of decomposition. Litter decomposing under elevated CO₂ decomposed more rapidly than litter under ambient CO₂, and exhibited higher rates of mineral N accumulation. The results suggest that the atmospheric conditions during the decomposition process have a greater impact on rates of decomposition and N cycling than do the atmospheric conditions under which the foliage was produced.     

Short-term decomposition of litter produced by plants grown in ambient and elevated atmospheric CO2 concentrations

The effects of elevated atmospheric CO₂ (ambient + 340 μmol mol^–1) on above-ground litter decomposition were investigated over a 6-week period using a field-based mesocosm system. Soil respiratory activity in mesocosms incubated in ambient and elevated atmospheric CO₂ concentrations were not significantly different (t-test, P > 0.05) indicating that there were no direct effects of elevated atmospheric CO₂ on litter decomposition. A study of the indirect effects of CO₂ on soil respiration showed that soil mesocosms to which naturally senescent plant litter had been added (0.5% w/w) from the C₃ sedge Scirpus olneyi grown in elevated atmospheric CO₂ was reduced by an average of 17% throughout the study when compared to soil mesocosms to which litter from Scirpus olneyi grown in ambient conditions had been added. In contrast, similar experiments using senescent material from the C₄ grass Spartina patens showed no difference in soil respiration rates between mesocosms to which litter from plants grown in elevated or ambient CO₂ conditions had been added. Analysis of the C:N ratio and lignin content of the senescent material showed that, while the C:N ratio and lignin content of the Spartina patens litter did not vary with atmospheric CO₂ conditions, the C:N ratio (but not the lignin content) of the litter from Scirpus olneyi was significantly greater (t-test;P < 0.05) when derived from plants grown under elevated CO₂ (105:1 compared to 86:1 for litter derived from Scirpus olneyi grown under ambient conditions). The results suggest that the increased C:N ratio of the litter from the C₃ plant Scirpus olneyi grown under elevated CO₂ led to the lower rates of biodegradation observed as reduced soil respiration in the mesocosms. Further long-term experiments are now required to determine the effects of elevated CO₂ on C partitioning in terrestrial ecosystems.     

Differential Response of B and T Cells to ALS revealed by Electrophoretic Mobility Determinations

SINCE their discovery anti-lymphocyte antisera (ALS) have been widely investigated in order to clarify their mode of action and to determine their usefulness in clinical practice. Briefly, it seems that the efficacy of a particular ALS depends on its mode of production and on the method adopted for testing its immunosuppressive effect. It also seems likely that many ALS have a harmful effect on a population of thymus-dependent (T) lymphocytes¹. It is the intention of this paper to confirm this notion and to indicate that other lymphocytes (B cells) are likely to be less affected by ALS.