Permian high-temperature metamorphism in the Western Alps (NW Italy)

During the late Palaeozoic, lithospheric thinning in part of the Alpine realm caused high-temperature low-to-medium pressure metamorphism and partial melting in the lower crust. Permian metamorphism and magmatism has extensively been recorded and dated in the Central, Eastern, and Southern Alps. However, Permian metamorphic ages in the Western Alps so far are constrained by very few and sparsely distributed data. The present study fills this gap. We present U/Pb ages of metamorphic zircon from several Adria-derived continental units now situated in the Western Alps, defining a range between 286 and 266 Ma. Trace element thermometry yields temperatures of 580-890°C from Ti-in-zircon and 630-850°C from Zr-in-rutile for Permian metamorphic rims. These temperature estimates, together with preserved mineral assemblages (garnet-prismatic sillimanite-biotite-plagioclase-quartz-K-feldspar-rutile), define pervasive upper-amphibolite to granulite facies conditions for Permian metamorphism. U/Pb ages from this study are similar to Permian ages reported for the Ivrea Zone in the Southern Alps and Austroalpine units in the Central and Eastern Alps. Regional comparison across the former Adriatic and European margin reveals a complex pattern of ages reported from late Palaeozoic magmatic and metamorphic rocks (and relics thereof): two late Variscan age groups (~330 and ~300 Ma) are followed seamlessly by a broad range of Permian ages (300-250 Ma). The former are associated with late-orogenic collapse; in samples from this study these are weakly represented. Clearly, dominant is the Permian group, which is related to crustal thinning, hinting to a possible initiation of continental rifting along a passive margin

Lay-up optimization of composite plates to delay mode-jump instabilities

All cyanobacterial mats that have been investigated have been proven to be diazotrophic, i.e., use atmospheric dinitrogen (N2) as the source of nitrogen. Many cyanobacteria possess the capacity to fix N2 and different species have evolved various ways to cope with the sensitivity of nitrogenase toward oxygen which is produced by these oxygenic phototrophs. These different strategies give rise to complex patterns of nitrogenase activity in microbial mats. Nitrogenase activity may exhibit complex variations over a day–night cycle but different types of microbial mats may also have their own characteristic patterns. Besides the cyanobacteria, numerous other members of the Bacteria as well as some Archaea are known to be diazotrophic. The complexity of the microbial community and of the observed patterns of nitrogenase activity makes it difficult to understand how the different groups of organisms contribute to N2 fixation in microbial mats. Cyanobacteria have ample access to energy (sunlight) and reducing equivalents (water) and therefore easily satisfy the demands of nitrogenase. As well, since they also fix CO2, they are able to synthesize the acceptor molecules for the fixed nitrogen. However, it is also feasible that other diazotrophs in a joint venture with cyanobacteria are responsible for the bulk of the fixed nitrogen. In this review we discuss the importance of cyanobacteria as diazotrophs in microbial mats, their interactions with other potential N2-fixing microorganisms, and the factors that control their activities.