Submarine depositional terraces at Salina Island (Southern Tyrrhenian Sea) and implications on the Late-Quaternary evolution of the insular shelf

The integrated analysis of high-resolution multibeam bathymetry and single-channel seismic profiles around Salina Island allowed us to characterize the stratigraphic architecture of the insular shelf. The shelf is formed by a gently-sloping erosive surface carved on the volcanic bedrock, mostly covered by sediments organized in a suite of terraced bodies, i.e. submarine depositional terraces. Based on their position on the shelf, depth range of their edge and inner geometry, different orders of terraces can be distinguished. The shallowest terrace (near-shore terrace) is a sedimentary prograding wedge, whose formation can be associated to the downward transport of sediments from the surf zone and shoreface during stormy conditions. According to the range depth of the terrace edge (i.e., 10–25 m, compatible with the estimated present-day, local storm-wave base level in the central and western Mediterranean), the formation of this wedge can be attributed to the present-day highstand. By assuming a similar genesis for the deeper terraces, mid-shelf terraces having the edge at depths of 40–50 m and 70–80 m can be attributed to the late and early stages of the Post-LGM transgression, respectively. Finally, the deepest terrace (shelf-edge terrace) has the edge at depths of 130–160 m, being thus referable to the lowstand occurred at ca. 20 ka. Based on the variability of edge depth in the different sectors, we also show how lowstand terraces can be used to provide insights on the recent vertical movements that affected Salina edifice in the last 20 ka, highlighting more generally their possible use for neo-tectonic studies elsewhere. Moreover, being these terraces associated to different paleo-sea levels, they can be used to constrain the relative age of the different erosive stages affecting shallow-water sectors

Insular shelves as a tool for reconstructing the evolution of volcanic islands

The erosion by waves, accomplished at different elevations due to glacio-eustatic sea-level fluctuations and islands’ vertical movements, carves the flanks of volcanic islands resulting in the formation of insular shelves, features long known in literature since the early paper of Menard (1983). However, a systematic study of their morphometric parameters and evolution has seldom been carried out. This Ph.D project, based on high-resolution multibeam bathymetric data and seismic reflection profiles collected in the last decades by the University of Bologna, University of Rome “La Sapienza”, CNR-IGAG Rome and by the Hydrographic Institute of the Portuguese Navy, explores the geomorphologic and structural features of the shelves surrounding the volcanic islands of Salina, Lipari and Vulcano in the Central Aeolian Archipelago and Santa Maria in the Azores Archipelago, respectively. The main aim is to increment our knowledge regarding the processes that influence the formation and the evolution of insular shelves and how these features might help us to better constraint the volcanic history of such islands. The study of insular shelves helps to improve the evolutionary models of the studied volcanic islands, which were previously developed only from the knowledge of the onshore geology. The information derived from the measured morphometric parameters (mainly the shelf width and the erosive edge depth) were integrated with field studies, allowing to infer, in some cases, the possible location of their earlier evolutionary stages, as well as to improve the overall geological evolution of studied volcanic islands.In the Central Aeolian sector, we thus document the occurrence of presently submerged and largely dismantled volcanic edifices predating the oldest complexes located onshore. At Santa Maria we adopted the same integrated approach to relate the morphologic characteristics of the shelf with the geology onshore

Active surveillance of paratuberculosis in Alpine-dwelling red deer (Cervus elaphus)

Paratuberculosis (Johne’s disease) is a globally widespread infectious disease affecting domestic and wild ruminants, caused by Mycobacterium avium subsp. paratuberculosis (MAP). The bacterium is excreted in the feces and is characterized by high environmental resistance. The new Animal Health Law (Regulation EU 2016/429) on transmissible animal diseases, recently in force throughout the European Union, includes paratuberculosis within the diseases requiring surveillance in the EU, listing some domestic and wild Bovidae, Cervidae, and Camelidae as potential reservoirs. Taking advantage of a culling activity conducted in the Stelvio National Park (Italy), this study investigated MAP infection status of red deer (Cervus elaphus) between 2018 and 2022, and evaluated the probability of being MAP-positive with respect to individual and sampling-level variables. A total of 390 subjects were examined macroscopically and tested for MAP, using different diagnostic tools: IS900 qPCR, culture, histopathology, and serology. Twenty-three of them were found positive for MAP by at least one test, with an overall prevalence of 5.9% (95% CI 4.0–8.7), that, respectively, ranged from 12.4% in the first culling season to 2.0 and 2.1% in the 2019–2020 and 2021–2022 culling seasons. Quantitative PCR assay on ileocecal valve and mesenteric lymph nodes detected the highest number of MAP positive animals. The results of the study showed the increased probability of being MAP-positive with increasing age and that red deer with lower body mass values were more likely to be infected with MAP. Overall, the absence of signs of clinical paratuberculosis and gross lesions together with the low level of shedding witness early phases of the disease among the positive red deer and support an improvement of the paratuberculosis status of this population, as shown by the decreased prevalence of the disease over the years

Marine terrace development on reefless volcanic islands:New insights from high-resolution marine geophysical data offshore Santa Maria Island (Azores Archipelago)

Submerged marine terraces are relict coastal erosional landforms now underwater due to rising sea level and/or land subsidence. Using as case study the shelf around Santa Maria Island (North Atlantic Ocean), we intend to advance our knowledge on the formation and preservation of these features on reefless volcanic islands. Santa Maria is an ideal place to study their combined generation, since it displays a sequence of subaerial and submerged marine terraces (the latter not studied before), distributed between 7/230 m in elevation, and 1240/ 12140 m in depth, respectively. Based on some geological constraints, we investigated a possible correlation between the formation of the different terraces with known sea-level changes. Our results suggest that the spatial distribution of marine terraces at Santa Maria depends on the complex interplay between glacio-eustatic sea-level fluctuations, the island's vertical motion trends, the morphology of the shelf, and the intensity of marine erosion. Subaerial terraces probably developed from ~3.5 Ma to ~1 Ma following a fortuitous conjugation of optimal exposure to energetic waves and a suitable arrangement/lithology of the stratigraphic units promoting easier erosion. Their preservation was likely promoted by the uplift trend the island experienced in the last 3.5 Ma, which was rapid enough to prevent their destruction by subsequent highstands. The submerged terraces, presumably all younger than ~1 Ma, were largely influenced by shelf gradient, leading to more developed and preserved terraces in wider and low-gradient sectors. Displacement by active faults also conditioned the formation and further development of both subaerial and submerged terraces, with tectonic activity documented for the 0.693 Ma\u20132.7 Ma period

Analisi di facies e stratigrafia dei depositi tardo-quaternari della Pianura Padana centrale

La ricostruzione dettagliata dell’architettura stratigrafica e delle facies delle successioni tardo-quaternarie sepolte al di sotto delle pianure alluvionali moderne sta assumendo un’importanza crescente come strumento per le ricostruzioni paleoambientali e paleoclimatiche e per la correlazione dei sistemi deposizionali continentali e costieri, finalizzata alla caratterizzazione geometrica di corpi sedimentari che rappresentano potenziali serbatoi. Un impulso significativo verso la caratterizzazione dell’architettura stratigrafica dei depositi tardo-quaternari del Bacino Padano è stato fornito, negli ultimi quindici anni, da un’intensa campagna di perforazioni operata dal Servizio Geologico, Sismico e dei Suoli di Regione Emilia-Romagna, nell’ambito della realizzazione della Carta geologica d’Italia in scala 1:50.000. Tuttavia, per ottenere un numero sufficiente di informazioni stratigrafiche è necessario un dataset molto esteso e le perforazioni (sondaggi a carotaggio continuo) presentano costi estremamente elevati. I limiti operativi delle descrizioni dei sondaggi a carotaggio continuo possono essere superati utilizzando metodi indiretti che si basano sullo sfruttamento delle proprietà geotecniche dei depositi tardo-quaternari. In questo lavoro di tesi l’analisi delle caratteristiche geotecniche delle prove CPTU è stata sfruttata per caratterizzare le associazioni di facies della Pianura Padana centrale. Una dettagliata analisi dei log stratigrafici e, in particolare, delle curve di resistenza delle prove CPTU inserite nelle sezioni, la costruzione di sezioni stratigrafiche e un meticoloso lavoro di correlazione basato su 19 datazioni radiometriche, ha rivelato una serie di paleosuoli (inceptisuoli) impilati nei 50-60 m più superficiali della successione tardo-quaternaria della Pianura Padana centrale; questi paleosuoli rappresentano l’unico marker stratigrafico all’interno di una successione costituita prevalentemente da depositi argillosi uniformi. L’analisi delle caratteristiche geotecniche di alcuni paleosuoli e dei loro rapporti con la channel belt del Fiume Po risulta fondamentale per comprendere l’evoluzione recente del Bacino Padano e le caratteristiche geometriche dei corpi sedimentari finalizzata allo sfruttamento di potenziali risorse fluide sotterranee

Bad Oeynhausen (Rehme), Westfalen

dargest. vom Oberbergrath Freyta