I. Historischer AbrißDas seit dem 2. Jh. v. Chr. römische Tergeste wurde 52 v. Chr. zur Colonia erhoben und von Augustus befestigt. Nach ostgotischer Herrschaft (bis 539) kam die Stadt, inszwischen ...Bi...
U članku se analiziraju prostorna obilježja upravne zgrade šećerane u Rijeci – palače Tršćansko-riječke privilegirane kompanije, s obzirom na dvije ključne faze njezina građevnog razvoja, razdoblje ...izgradnje 1752. i obnovu nakon požara 1785. – 1786. godine. Razmatra se funkcija pojedinih etaža i prostorija u zgradi, te utvrđuju namjenski prostori za stanovanje, poslovne sadržaje i skladišta. Palača se dovodi u vezu s korpusom arhitekture reprezentativnih poslovnostambenih palača izgrađenih u Trstu u drugoj polovini 18. stoljeća, koje nose vrlo slične prostorne karakteristike, a one se mogu iščitati iz arhivskih nacrta, jer same palače uglavnom nisu sačuvane. Navedene usporedbe upućuju, nadalje, na postojanje konkretnog tipskog obrasca za prostorno rješenje zgrada poslovno stambene namjene, bilo da ih podižu imućni trgovci za vlastito stanovanje i djelatnost, ili pak velike privilegirane kompanije koje su imale sjedišta u Trstu tijekom 18. stoljeća.
A specimen of common thresher shark
(Bonnaterre 1788) was caught in a fishing net in the waters off Piran (Gulf of Trieste, northern Adriatic Sea). It was a juvenile male with a total length of 2841 ...mm. In recent decades, other cases of juvenile specimens of common thresher shark have been recorded in Slovenian coastal waters. Despite the drastic decline in the population of this species, thresher shark continues to be caught in local Adriatic fisheries.
The analysis of multichannel seismic profiles and their correlation with well data in the northern Adriatic Sea (Northern Italy) has allowed to document Plio-Quaternary episodes of tectonic ...subsidence and uplift. They affected the sedimentation above the Mesozoic to lower Eocene Friuli-Dinaric Carbonate Platform (FDCP) and the unit composed of the Eocene Trieste Flysch and the Miocene Molassa (TFM), as well as the sedimentary succession lying SW of the FDCP. In particular, the early Zanclean reflooding that postdated the Messinian Salinity Crisis, was followed by the SW-ward progradation of a highstand to forced regressive shelf-slope system (Sequence 1). Forced regression was controlled by a main episode of tectonic uplift that occurred at the end of the Zanclean. This tectonic event also led to the formation of the sequence boundary separating the two main sequences that compose the Plio-Quaternary succession. The lower part of Sequence 2 (Piacenzian to late Pleistocene) recorded a two-step subsidence phase, which led to drowning episodes during Piacenzian and in particular late Gelasian (transgressive systems tract of Sequence 2). They were associated with the partial flooding of the TFM and the Miocene deposits overlying the FDPC, and with a downward bending of the pre-Calabrian succession toward the Apennine chain. The accommodation created during the late Gelasian drowning event was filled in part by an Alpine-sourced, SW-ward prograding system, and in part by the NE-ward paleo-Po prograding system (highstand systems tract of Sequence 2). The most recent part of Sequence 2 documents the last glacio-eustatic cycles in a physiographic context characterized by a very low gradient.
•A reconstruction of the Plio-Quaternary geologic evolution of the northern Adriatic Sea is provided.•A sequence stratigraphic approach is adopted.•The relationships between tectonics and sedimentation are highlighted.•The present results help to better understand the geodynamic evolution of the study area.
The integration of high-resolution seismic profiles, core data and radiocarbon plus U-Th datings, allows to document the late Quaternary succession of the Trieste Gulf, which represents the ...easternmost part of the northern Adriatic Sea. This succession consists of an alternation of shallow-marine and continental deposits organized to compose four transgressive-regressive sequences down to ca. 90 m below present sea level. The sequences terminate landwards against a stepped surface bounding the Eocene Trieste Flysch and produced by alternating episodes of wave erosion during transgressions and subaerial exposure during stages of relative sea-level fall and lowstand. Two shallow-marine wedges, in addition to the Holocene one, have been recognized; they are associated with the Marine Isotopic Stage (MIS) 5.5 (Tyrrhenian) and probably at least one of the peaks of MIS 7. The recognized shallow-marine wedges typically prograde just seaward of a buried wave-cut platform lying in front of a receding paleo-coastal cliff. A previously unrecognized stratigraphic hiatus of ca. 25 ka duration, containing the whole Last Glacial Maximum (LGM) phase, was found at the top of palustrine deposits that accumulated on the MIS 5.5 marine sediments until ca. 40 cal ka B.P. and a post-LGM peat bed accumulated during the Younger Dryas stadial. The beginning of the Holocene was characterized by marked fluvial aggradation preceding the marine transgression at ca. 11-10 cal ka B.P. This new evidence is invaluable for better understanding late Quaternary sedimentary and erosional episodes that characterized the easternmost part of the norther Adriatic Sea, in the frame of the well-known glacio-eustatic sea-level changes.
Mercury (Hg) is one of the primary health concerns in natural and urbanised environments due to past and present natural and anthropogenic emissions. Its environmental cycle is driven by redox ...reactions, microbial metabolism and organic matter (OM) interactions, which may all lead to formation of bioaccumulative organic Hg species; methylmercury (MeHg), with damaging consequences for human and ecosystem health. Hence, Hg lability and bioavailability has been the focus of many investigations and assessed with a variety of chemical proxies in order to improve understanding of the conditions that lead to enhanced bioavailability of Hg and its species. We investigated Hg labile species with Diffusive Gradient in Thin-film technique (DGT) in the water column and sediment of Zenne River (Brussels, Belgium) and Gulf of Trieste (North Adriatic). They represent two contemporary important Hg-impacted areas; the former by anthropogenic urban pollution, and the latter by historic pollution from Hg mining. Hg speciation of labile inorganic and methylmercury in these two environments was not yet investigated using DGT technique. The results show labile Hg species changing with season in the water column of Zenne River, while the sediments are the source of bioavailable MeHg to the water column that is transported further creating a halo effect in the region. Values of labile Hg species for water column and sediments in Gulf of Trieste differ from previous research, highlighting the need for more investigation into Hg bioavailability. MeHg/THg ratios were compared to other sampling methods for labile Hg species.
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•Labile Hg species were measured using a Diffusive Gradient in Thin-film technique.•DGTs were used in the Zenne River Brussels and Gulf of Trieste (North Adriatic).•Winter-time THg in Zenne is highly labile and mobilized far from its source.•MeHg/THg% in Gulf showed higher labile Hg bioavailability than previously thought.•Labile MeHg in the sediment of the Gulf represents up to 75% of total labile Hg.
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