Il lascito di Agostino Mitelli ai quadraturisti e ai decoratori del secondo Seicento bolognese attraverso le testimonianze grafiche

Agostino Mitelli (1609-1660) è una figura centrale nella vicenda artistica bolognese. Rinnova profondamente la quadratura, genere in cui opera maggiormente, e diventa il principale riferimento per le generazioni successive. Infatti ha un grande numero di allievi che si fanno interpreti del suo stile e le sue opere continuano ad essere studiate fino a Settecento inoltrato. Nel suo lavoro accorda una grande importanza al mezzo grafico, in cui eccelle e che considera strumento di verifica ed esercizio. Questa predilezione influenza anche i suoi seguaci: dopo la sua morte i suoi disegni diventano molto ricercati e vengono impiegati come repertori di soluzioni di quadratura ed elementi decorativi. Sono essi stessi strumento di studio e infatti ci è pervenuto un grande numero di copie ed esercizi in stile mitelliano. L'analisi sistematica di questo materiale anonimo e poco studiato mi ha permesso di individuare alcune delle personalità di maggiore spicco tra i suoi seguaci, quali Domenico Santi, Giacomo Antonio Mannini e Marc'Antonio Chiarini. Per valutare l'influenza dell'opera di Agostino presso le generazioni successive è centrale anche la produzione calcografica che analizzo a partire dalle quattro serie di elementi di ornato che egli stesso dà alle stampe e che riscuotono molto successo, come provano le numerose ristampe, anche francesi. Dopo la sua morte vengono incise diverse imprese che si riallacciano al suo operato: la prima è quella del figlio Giuseppe Maria Mitelli che pubblica alcuni suoi disegni. Seguono le serie di Santi, Buffagnotti, Mannini, Chiarini e diversi altri che comprendono anche quadratura e veduta e che spesso sono state riassemblate da editori e collezionisti. Anche le fonti affrontano la questione della dipendenza delle successive generazioni dagli stilemi di Agostino Mitelli, oltre a quelle a stampa ho studiato approfonditamente i manoscritti inediti dell'altro figlio di Agostino, Giovanni Mitelli, che forniscono molte nuove notizie.

Abitati rupestri e citta' fortificate nella Sicilia occidentale dai bizantini ai normanni

La ricerca effettuata, analizza in modo razionale ma contestualmente divulgativo, le dinamiche insediative che hanno caratterizzato il paesaggio della Sicilia occidentale dall'occupazione bizantina al dominio da parte dei Normanni ( 535-1194 d.C. circa ). Il volume presenta una chiara raccolta dei documenti e delle fonti letterarie che riguarda gli abitati rurali ed i borghi incastellati della Sicilia occidentale e pone l’interesse sia per la cultura materiale che per la gestione ed organizzazione del territorio. Attraverso i risultati delle attestazioni documentarie, unite alle ricerche archeologiche ( effettuate nel territorio preso in esame sia in passato che nel corso degli ultimi anni ) viene redatto un elenco dei siti archeologici e dei resti monumentali ( aggiornato fino al 2013-14 ) in funzione della tutela, conservazione e valorizzazione del paesaggio. Sulla base dei documenti rinvenuti e delle varie fonti prese in esame ( letterarie, archeologiche, monumentali, toponomastiche ) vengono effettuate alcune considerazioni sull’insediamento sparso, sull’incastellamento, sulle istituzioni e sulla formazione delle civitates. L’indagine svolta, attraverso cui sono stati individuati i documenti e le fonti, comprende anche una parziale ricostruzione topografica dei principali centri abitativi indagati. Per alcune sporadiche strutture medievali, talvolta raffigurate in fortuite stampe del XVI-XVII secolo, è stato possibile, in aggiunta, eseguire un rilievo architettonico. La descrizione degli abitati rurali e dei siti fortificati, infine, è arricchita da una serie di schede in cui vengono evidenziati i siti archeologici, i resti monumentali ed i reperti più interessanti del periodo bizantino, arabo e normanno-svevo della Sicilia occidentale.

Palaeotsunami imprints in the near-coast sedimentary records of the Gulfs of Lakonia and Argolis (Peloponnese, Greece)

From historical accounts it is well-known that the coasts of the Gulfs of Lakonia and Argolis (southern and eastern Peloponnese, Greece) have been repeatedly affected by tsunamis during historical times. It is assumed that these palaeotsunamis left sedimentological and geomorphological traces in the geological record which are still detectable these days. As both gulfs are located within one of the seismically most active regions in whole western Eurasia in particular the nearby Hellenic Trench is regarded as the main trigger for tsunami generation. Against this background, selected near-coast sedimentary archives were studied by means of sedimentological, geomorphological, geophysical, geochemical and microfaunal investigations in order to detect signatures of Holocene palaeotsunamigenic activity. The investigations revealed allochthonous sediment layers featuring distinctive sedimentary characteristics of marine high-energy event deposits in most of the investigated study areas. In order to differentiate between the geomorphodynamic driving mechanisms for the deposition of the associated marine high-energy event layers, a multi-method approach was used. The detected high-energy marine deposits are suggested to be of tsunamigenic origin. Radiocarbon dating results allowed establishing local event geo-chronostratigraphies and correlations on a local and regional scale as well as correlations with already described palaeotsunami findings on a supra-regional scale. The geochronological dataset attests repeated tsunamigenic activity at least since the 5th millennium BC up to the 17th century AD. For the studied areas in southeastern Lakonia up to four palaeotsunami event generations were identified, for central Lakonia three and for the investigated areas around the Argolis Gulf also up to four. Comparing the findings with literature data, chronological correlations were found with palaeotsunami deposits detected in near-coast geological archives of Akarnania, of the southwestern, the western and northwestern Peloponnese, with event deposits found on Crete and on the Ionian Islands of Cefalonia and Lefkada as well as with findings from southeastern Sicily (Italy) and Cesarea (Israel). By the identification of multiple palaeotsunami event layers, disturbing autochthonous near-coast sedimentary records of the Gulfs of Lakonia and Argolis during the last seven millennia, a significant tsunami frequency is attested for these regions.

Causes and consequences of past and projected Scandinavian summer temperatures, 500-2100 AD

Tree rings dominate millennium-long temperature reconstructions and many records originate from Scandinavia, an area for which the relative roles of external forcing and internal variation on climatic changes are, however, not yet fully understood. Here we compile 1,179 series of maximum latewood density measurements from 25 conifer sites in northern Scandinavia, establish a suite of 36 subset chronologies, and analyse their climate signal. A new reconstruction for the 1483–2006 period correlates at 0.80 with June–August temperatures back to 1860. Summer cooling during the early 17th century and peak warming in the 1930s translate into a decadal amplitude of 2.9°C, which agrees with existing Scandinavian tree-ring proxies. Climate model simulations reveal similar amounts of mid to low frequency variability, suggesting that internal ocean-atmosphere feedbacks likely influenced Scandinavian temperatures more than external forcing. Projected 21st century warming under the SRES A2 scenario would, however, exceed the reconstructed temperature envelope of the past 1,500 years.

Climate and human impact during the past 2000 years as recorded in the Lagunas de Yala, Jujuy, northwestern Argentina

210Pb, 137Cs and 14C dated sediments of two late Holocene landslide lakes in the Provincial Park Lagunas de Yala (Laguna Rodeo, Laguna Comedero, 24°06′S, 65°30′W, 2100 m asl, northwestern Argentina) reveal a high-resolution multi-proxy data set of climate change and human impact for the past ca. 2000 years. Comparison of the lake sediment data set for the 20th century (sediment mass accumulation rates MARs, pollen spectra, nutrient and charcoal fluxes) with independent dendroecological data from the catchment (fire scars, tree growth) and long regional precipitation series (from 1934 onwards) show that (1) the lake sediment data set is internally highly consistent and compares well with independent data sets, (2) the chronology of the sediment is reliable, (3) large fires (1940s, 1983/1984–1989) as documented in the local fire scar frequency are recorded in the charcoal flux to the lake sediments and coincide with low wet-season precipitation rates (e.g., 1940s, 1983/1984) and/or high interannual precipitation variability (late 1940s), and (4) the regional increase in precipitation after 1970 is recorded in an increase in the MARs (L. Rodeo from 100 to 390 mg cm−2 yr−1) and in an increase in fern spores reflecting wet vegetation. The most significant change in MARs and nutrient fluxes (Corg and P) of the past 2000 years is observed with the transition from the Inca Empire to the Spanish Conquest around 1600 AD. Compared with the pre-17th century conditions, MARs increased by a factor of ca. 5 to >8 (to 800 +130, −280 mg cm−2 yr−1), PO4 fluxes increased by a factor of 7, and Corg fluxes by a factor of 10.5 for the time between 1640 and 1930 AD. 17th to 19th century MARs and nutrient fluxes also exceed 20th century values. Excess Pb deposition as indicated by a significant increase in Pb/Zr and Pb/Rb ratios in the sediments after the 1950s coincides with a rapid expansion of the regional mining industry. Excess Pb is interpreted as atmospheric deposition and direct human impact due to Pb smelting.

Signatures of slope failures and river-delta collapses in a perialpine lake (Lake Lucerne, Switzerland)

Historical reports from the 17th Century document two destructive tsunamis with runups exceeding 5 m, affecting proximal basins of Lake Lucerne (Switzerland). One event in AD 1601 is coeval with a strong nearby earthquake (MW ca 5.9), which caused extensive slope failures in many parts of the lake. The second event in AD 1687 is associated with an apparently spontaneous partial collapse of the Muota river delta. This study combines high-resolution bathymetry, reflection seismic and lithological data in order to document the sedimentary and morphological signatures of the two subaqueous mass movements that probably generated the observed tsunamis. Such mass movements are significant as a common sedimentation process and as natural hazard in fjord-type lakes and similar environments. The deposits, covering large parts of the basins with thicknesses reaching >10 m, consist of two subunits: A lower ‘massflow deposit’ contains variably deformed sediments from the source areas. Its emplacement affected pre-existing sediments, incorporating thin sediment slices into the deposit and increasing its volume. Deep-reaching deformation near This is an Accepted Article that has been peer-reviewed and approved for publication in the Sedimentology, but has yet to undergo copy-editing and proof correction.

Filling the Eastern European gap in millennium-long temperature reconstructions

Tree ring–based temperature reconstructions form the scientific backbone of the current global change debate. Although some European records extend into medieval times, high-resolution, long-term, regional-scale paleoclimatic evidence is missing for the eastern part of the continent. Here we compile 545 samples of living trees and historical timbers from the greater Tatra region to reconstruct interannual to centennial-long variations in Eastern European May–June temperature back to 1040 AD. Recent anthropogenic warming exceeds the range of past natural climate variability. Increased plague outbreaks and political conflicts, as well as decreased settlement activities, coincided with temperature depressions. The Black Death in the mid-14th century, the Thirty Years War in the early 17th century, and the French Invasion of Russia in the early 19th century all occurred during the coldest episodes of the last millennium. A comparison with summer temperature reconstructions from Scandinavia, the Alps, and the Pyrenees emphasizes the seasonal and spatial specificity of our results, questioning those large-scale reconstructions that simply average individual sites.