Salinity tolerance of three ostracode species (Crustacea:Ostracoda) of Iberian saline lakes

Laboratory experiments and field data were used to determine salinity tolerance limits of three ostracode species (Prionocypris aragonica, Eucypris mareotica and Heterocypris barbara) from Iberian saline lakes. Salinity tolerance appeared related to ionic composition and temperature. Implications for ostracode ecology and geographical distribution are evaluated.     

Threshold response of Madagascar's littoral forest to sea-level rise

Aim Coastal biodiversity hotspots are globally threatened by sea‐level rise. As such it is important to understand how ecosystems resist, respond and adapt to sea‐level rise. Using pollen, geochemistry, charcoal and diatom records in conjunction with previously published palaeoclimatic records, we investigated the mechanism, interactions and ecosystem response and resilience of Madagascar's littoral forest to late Holocene sea‐level rise. Location Sediment sequences were collected along the south‐east coast of Madagascar in two adjacent habitats in Mandena; the highly diverse littoral forest fragment and species‐poor Erica‐matrix. Methods We used a multi‐proxy approach to investigate the relative influence of environmental changes on the littoral ecosystem. We reconstructed past vegetation and fire dynamics over the past 6500 years at two sites in the littoral forest using fossil pollen and macrofossil charcoal contained in sedimentary sequences. Alongside these records we reconstructed past marine transgressions from the same sedimentary sequences using geochemical analyses, and a salinity and drought index through the analysis of fossil diatoms. Results Our findings indicated that it was the synergistic effect of sea‐level rise coupled with rainfall deficits that triggered a threshold event with a switch from two types of littoral forest (an open Uapaca forest and a closed littoral forest fragment) to an Erica–Myrica heath/grassland occurring in approximately less than 100 years. Resilience to sea‐level rise differed in the two adjacent habitats, suggesting that the littoral forest fragment was more resilient to the impacts of sea‐level change and aridity than the open Uapaca woodland. Conclusions We demonstrated that the littoral ecosystem was influenced by late Holocene sea‐level rise and climatic desiccation. While climate change‐integrated conservation strategies address the effects of climate change on species distribution and dispersal, our work suggests that more attention should be paid to the impacts of interactive climatic variables that affect ecosystem thresholds.     

A Short Period of Mannitol Stress but Not LiCl Stress Led to Global Translational Repression in Plants

In plant cells, high salinity stress induces rapid inhibition of general protein synthesis. In this study, we found that treatment with mannitol, but not lithium stress, led to rapid global translational repression, suggesting that a rapid response at the level of translation might be induced by the osmotic but not the ionic components of salinity stress.     

Effect of a salt-osmotic upshock on the edaphic microalga Neochloris oleoabundans

Abstract. The edaphic microalga Neochloris oleoabundans (isolated from desert soil) was subjected to a salt-osmotic shock from 0 to 0·6 kmol m⁻³ NaCl. The effect of the osmotic upshock on the cell composition was determined. The cell dry weight and the lipid, glycerol and soluble amino acids contents remained unchanged during 5d of osmotic upshock. The protein content increased after 2d of initial osmotic shock, and it appears to be a long-term haloadaptation process of the cells. The most important short-term effects of salt osmotic upshock were a decrease in polysaccharide content and an increase in the soluble carbohydrate content of Neochloris oleoabundans cells. Within the first 4h after the initial shock, there was a transfer of carbon units from polysaccharides to sucrose which was independent of photosynthesis. The increase of intracellular concentration of sucrose contributed to cell osmoregulation.     

Mass Collaboration in Earthquake Risk Management

The mechanism of mass collaboration in risk management was studied during the Sichuan earthquake under a Web-based “PeopleFinder” project, where information is contributed and shared among mass contributors. The case study is provided by a great earthquake that happened in Wenchuan County, Sichuan Province, of southwestern China at 2:28 p.m. on May 12, 2008. We witnessed and experienced the rescue and relief efforts for the great earthquake. In this article, two fundamental frameworks are developed to study the mechanism of mass collaboration. Mass collaboration is proven to be effective in a big public crisis such as the Sichuan earthquake.     

Testing vicariance: melanopsid snails and Neogene tectonics in the Western Mediterranean

Abstract. Vicariance on a microplate dispersed by the formation of the Western Mediterranean is the probable origin of Melanopsis etrusca Villa in Brot, the only melanopsid (Gastopoda: Melanopsidae) living in the Italian Peninsula. It is distantly related to extant melanopsids in Iberia and Morocco, and is restricted to thermal springs in the Maremma of southern Tuscany. This area was an island throughout the Miocene, inferred to have become detached geographically from the Corso—Sardinian block. Alternative explanations conflict with geological, paleontological, ecological and systematic evidence. In the geologically young Italian Peninsula fossil freshwater melanopsids are known only from Lower Pleistocene sites located around the area occupied by living populations. Their similarity to extant specimens supports the hypothesis that they represent the same lineage, having expanded its range during a brief, favourable period. Introduction of M. etrusca by humans, birds or wind is most improbable given its distinctness, similarity to local fossils, and inability for passive dispersal. Long-distance dispersal along brackish lagoons during the late Messinian conflicts with the inferred inability of melanopsids living there to colonize freshwater habitats. Indeed, there are ecological, phylogenetic and geological reasons against invoking the Messinian salinity crisis in order to explain the distribution of most taxa. Other freshwater taxa show distribution patterns similar to that of living and fossil melanopsids. However, congruent area cladograms or generalized tracks may not constitute reliable evaluators of biogeographical hypotheses. The detection of vicariance, as that of any other cause, requires robust reconstructions of the past. By pointing at areas of endemism that deserve urgent action, biogeography can provide a contribution to conservation.     

Phosphorus uptake and translocation in salt-stressed melon plants

Melon seedlings (Cucumis melo L. cv.Galia) were grown hydroponically to study the effect of salinity (80 mmol/LNaCl) on phosphate (Pi) uptake and translocation at two levels of Pi (25 μmol/L and 1 mmol/L). Net uptake rates of Pi were determined by depletionof the medium and by plant content. Salinity decreased Pi uptake at low Pi (high affinity uptake mechanism), 25 μmol/L, although no specific competitive inhibition of Pi uptake by Cl⁻ was observed. When plants were grown with high Pi (1 mmol/L), the uptake of Pi through the low affinity system was increased by 80 mmol/L NaCl. Salinity also reduced the phosphorus flux, as Pi, through the xylem. It is hypothesised that high levels of NaCl decrease the mobility of Pi stored in vacuoles, and as a result, inhibit export from this storage compartment to other parts of the plant.