Activity, work and employment: some reflections on a topic under debate

Since ten years ago, it is intensely thought of human work and employment in developed countries as a consequence of the deep changes on the productive system. In this chapter we analyze at first place the concept of work and its evolution, based on recent researches. In second place we review the notions of activity, work and employment and also the definition and measurement of unemployment, which is not a very old notion. The third part is about the work rol in human life and finally we study the different alternatives on activity and specific work contracts, proposals that nowadays replace the notion of "full employment" in France.

Activity, work and employment: some reflections on a topic under debate

Since ten years ago, it is intensely thought of human work and employment in developed countries as a consequence of the deep changes on the productive system. In this chapter we analyze at first place the concept of work and its evolution, based on recent researches. In second place we review the notions of activity, work and employment and also the definition and measurement of unemployment, which is not a very old notion. The third part is about the work rol in human life and finally we study the different alternatives on activity and specific work contracts, proposals that nowadays replace the notion of "full employment" in France.

Activity, work and employment: some reflections on a topic under debate

Since ten years ago, it is intensely thought of human work and employment in developed countries as a consequence of the deep changes on the productive system. In this chapter we analyze at first place the concept of work and its evolution, based on recent researches. In second place we review the notions of activity, work and employment and also the definition and measurement of unemployment, which is not a very old notion. The third part is about the work rol in human life and finally we study the different alternatives on activity and specific work contracts, proposals that nowadays replace the notion of "full employment" in France.

Biogeochemical characterization of pennate diatom and Melosira arctica ice algal aggregates in the Central Arctic Ocean collected in summer 2011 and 2012

Sea-ice diatoms are known to accumulate in large aggregates in and under the sea ice including melt ponds. In the Arctic, they can contribute substantially to particle export when sinking from the ice. The role and regulation of microbial aggregation in the highly seasonal, nutrient- and light-limited Arctic sea-ice ecosystem is not yet well understood, and may vary in relation to the fate of the Arctic sea-ice cover. To elucidate the mechanism controlling the formation and export of algal aggregates from sea ice, we investigated samples taken in late summer 2011 and 2012, during two cruises to the Eurasian Basin of the Central Arctic Ocean. Dense, spherical aggregates composed mainly of pennate diatoms, and filamentous aggregates formed by Melosira arctica were found in different degradation stages, with carbon to Chlorophyll a ratios ranging from 110 to 66700, and carbon to nitrogen molar ratios of 8-35 and 9-40, respectively. Fresh sub-ice algal aggregate densities ranged between 1 and 17 aggregates/m**2, corresponding to a net primary production of 0.4-40 mg C/m**2/d, contributing 3-80% of total biomass and up to 94% of total production at a local scale. A key factor controlling buoyancy of the aggregates was light intensity, regulating photosynthetic oxygen production and flotation by gas bubbles trapped within the mucous matrix, even at low ambient nutrient concentrations. Our data was used to evaluate the factors regulating the distribution and importance of the Arctic algal aggregates as carbon source for pelagic and benthic communities.

Phase-equilibrium data and liquidus for the system "MnO"-CaO-Al2O3-SiO2 at Al2O3/SiO2 of 0.55 and 0.65

Phase-equilibrium data and liquidus isotherms for the system MnO-CaO-(Al2O3 + SiO2) at silicomanganese alloy saturation have been determined in the temperature range of 1373 to 1723 K. The results are presented in the form of the pseudoternary sections MnO-CaO-(Al2O3 + SiO2) with Al2O3/SiO2 weight ratios of 0.55 and 0.65. The primary-phase fields have been identified in this range of conditions.

Oxygen isotope ratios of PO4: An inorganic indicator of enzymatic activity and P metabolism and a new biomarker in the search for life

The distinctive relations between biological activity and isotopic effect recorded in biomarkers (e.g., carbon and sulfur isotope ratios) have allowed scientists to suggest that life originated on this planet nearly 3.8 billion years ago. The existence of life on other planets may be similarly identified by geochemical biomarkers, including the oxygen isotope ratio of phosphate (δ18Op) presented here. At low near-surface temperatures, the exchange of oxygen isotopes between phosphate and water requires enzymatic catalysis. Because enzymes are indicative of cellular activity, the demonstration of enzyme-catalyzed PO4–H2O exchange is indicative of the presence of life. Results of laboratory experiments are presented that clearly show that δ18OP values of inorganic phosphate can be used to detect enzymatic activity and microbial metabolism of phosphate. Applications of δ18Op as a biomarker are presented for two Earth environments relevant to the search for extraterrestrial life: a shallow groundwater reservoir and a marine hydrothermal vent system. With the development of in situ analytical techniques and future planned sample return strategies, δ18Op may provide an important biosignature of the presence of life in extraterrestrial systems such as that on Mars.