Upper Cretaceous stratigraphy and rudist-bearing facies of the Simbruini Mts. (Central Apennines, Italy). New field data and a review

The rudist-bearing carbonate platform succession of Marsia, in the northern Simbruini Mts. (Central Apennines), is described for the first time through the analysis of two stratigraphic sections, and better characterized by the study of three single significant outcrops located outside the sections. The identification of the rudist assemblages, related facies and micropaleontological analyses of the collected samples allowed to determine the age of this Upper Cretaceous succession, and the definition of a biostratigraphic frame for the of the entire study area. The Marsia composite stratigraphic section encompasses the late Turonian-early/middle Campanian interval, and records the evolution from inner platform-low hydrodynamic setting in the late Turonian, to an open platform setting characterized by high hydrodynamism in the late Santonian-early/middle Campanian. This succession has been compared to the already described Trevi, Santa Maria dei Bisognosi and Subiaco carbonate platform successions, and to regional bioevent schemes, in order to constrain the evolution of these carbonate facies in a wider sedimentological and stratigraphic context. Since the late Turonian, a spreading of rudist facies occurred throughout the central-southern Apennines, representing the first Upper Cretaceous rudist bioevent. In the Simbruini area inner platform environments, characterized by soft fine-grained sediment, are widespread. The successions of Marsia and Trevi, which are marked by upper Turonian inner platform facies with a thriving oligospecific rradiolitid association characterized by semi-infaunal lifestyle, record this bioevent. During the Santonian and the early Campanian a gradual increase in hydrodynamic conditions is recorded by rudist assemblages with hippuritids and robust radiolitids, associated with rare corals and echinoids which mark the second and third Upper Cretaceous rudist bievent, recorded at Marsia, Trevi and Santa Maria dei Bisognosi. The middle Campanian-Maastrichtian bioevents are only represented at Santa Maria dei Bisognosi and Subiaco, where high energy bioclastic facies, dominated by the peculiar radiolitid Sabinia sp., occur

Landscape genetics structure of European sweet chestnut (Castanea sativa Mill): indications for conservation priorities

Sweet chestnut is a tree of great economic (fruit and wood production), ecological and cultural importance in Europe. A large-scale landscape genetic analysis of natural populations of sweet chestnut across Europe is applied to 1) evaluate the geographic patterns of genetic diversity 2) identify spatial coincidences between genetic discontinuities and geographic barriers 3) propose certain chestnut populations as reservoirs of genetic diversity for conservation and breeding programmes. Six polymorphic microsatellite markers were used for genotyping 1608 wild trees sampled in 73 European sites. The Geostatistical IDW technique (ArcGIS 9.3) was used to produce maps of genetic diversity parameters (He, Ar, PAr) and a synthetic map of the population membership (Q value) to the different gene pools. Genetic barriers were investigated using BARRIER 2.2 software and their locations were overlaid on a Digital Elevation Model (GTOPO30). The DIVA-GIS software was used to propose priority areas for conservation. High values of genetic diversity (He) and allelic richness (Ar) were observed in the central area of C. sativa's European distribution range. The highest values of private allelic richness (PAr) were found in the eastern area. Three main gene pools and a significant genetic barrier separating the eastern from the central and western populations were identified. Areas with high priority for genetic conservation were indicated in Georgia, eastern Turkey and Italy. Our results increase knowledge of the biogeographic history of C. sativa in Europe, indicate the geographic location of different gene pools and identify potential priority reservoirs of genetic diversity

Combining demographic and land-use dynamics with local communities perceptions for analyzing socio-ecological systems: a case study in a mountain area of Italy

Rural communities are facing increasing social heterogeneity and organization complexity consequently to land use changes, demographic dynamics and globalization processes. Members of the communities should have a direct perception of their own territories, recognizing any positive or negative change that may occur. A better knowledge of these processes may be achieved by investigating local community awareness and perspectives. A research was carried out in a rural and mountainous area of Central Italy with the following aims: (i) to highlight demographic dynamics and land use changes that affected the area during the last decades; (ii) to assess local communities’ perceptions and awareness of their own territories; (iii) to verify and validate a research methodology by evaluating the resilience of socio-ecological systems. The study area involved four municipalities that were analyzed considering the historical changes of demographic data and land-use system. A questionnaire was submitted to a sample of local population. The questionnaire was aimed to investigate the following issues: (i) level and quality of participation and communication within the community life; (ii) awareness of environmental resources of the territories; (iii) socio-cultural opportunities and expectations of future changes within the communities. In each municipality, different behaviors and needs emerged according to the age of the inhabitants. In spite of that, awareness of social, cultural and environmental constraints/potentialities emerged in all the communities. Communication capability seems a key factor to reinforce both the social capital and the resilience of the territories. Thus, sharing of experience and knowledge could play a major role in developing an efficient governance of the occurring territorial changes. Finally, the study highlights that serious efforts should be spent especially to satisfy expectations of young people concerning the territorial development. This latter seems a prerequisite for the maintenance of the system resilience

The Jurassic succession of Ras Sharwayn, South-eastern Yemen

Four Jurassic stratigraphic units have been recognised at Ras Sharwayn, about 300 km east of Al-Mukalla along coast of the Gulf of Aden. The Kohlan Formation (60 m) unconformably overlies the crystalline basement. Its lower and middle part consist of fluviatile sandstone and conglomerate. The upper part is made up of transitional coarse- and fine-grained sandstones and siltstones. The sequence ends with shallow marine fine-grained sandstones. The Shuqra Formation (71 m) can be divided into two members. The lower Calcareous-marly Member (45 m) consists of grey bioclastic limestone and subordinate nodular marl (inner to mid ramp). Its age is Late Oxfordian. The upper Carbonate Member (26 m) changes from basal reddish marly limestones (mid ramp) to thick beds of red-brown, coarsely crystalline limestones and dolomites (inner ramp). The topmost beds contain fossils of colonial organisms, essentially stromatoporoids. Its age is Late Oxfordian, and possibly earliest Kimmeridgian. The Madbi Formation (>30 m) consists of yellowish marl alternating with marly limestone and bioclastic limestone (coquinas) corresponding to storm layers (mid to outer ramp). With regard to its age, a specimen of Orthosphinctes sp., collected a few metres from the base, possibly refers to the Early Kimmeridgian. The Madbi Formation ends with an unconformity surface. The informal elastic unit (56 m) (including the Naifa Formation) consists, from bottom upwards, of: red-brown dolomite; grey detrital limestone with quartz grains; massive, white conglomerate with well rounded limestone clasts, quartz and bioclasts (e.g. colonial organisms). The last lithotypes are gravity flow deposits, accumulated at the base of a scarp possibly tectonic in origin, approximately at the Jurassic-Cretaceous boundary. This detailed lithological, sedimentological and biostratigraphical study has provided revised litostratigraphical subdivision and nomenclature and improved the stratigraphic control