1. Ženska v blejskem gospodstvu v poznem 17. stoletju : analiza zvezanih sodnih zapisnikovLucija Pečnik, 2025, original scientific article Abstract: Članek obravnava položaj in vlogo neprivilegiranih žensk na območju blejskega gospostva ob koncu 17. stoletja, ko so briksenski škofje gospostvo upravljali prek zakupnikov. Analizirani so zvezani sodni zapisniki iz fonda zemljiškega gospostva Bled, skoraj 1500 strani arhivskega gradiva iz let 1690 do vključno 1700, kot rezultat delovanja nižjega in le izjemoma višjega sodstva za neprivilegirane. Rezultati so predstavljeni v kontekstu literature, kar vodi do novih spoznanj o položaju žensk v vaški družbi in družinskem gospodarstvu ter o njihovi pravni in poslovni sposobnosti. Predstavljeni so nekateri tipični in posebni primeri žensk, ki so v proučevanem obdobju pred blejskim sodiščem nastopale v vlogi tožnic, toženk, prič, dolžnic, upnic, porokinj, zastopnic in varuhinj otrok. Obravnavani so civilnopravni postopki in z njimi povezani spori, ki v analiziranih sodnih zapisnikih znatno prevladujejo, pa tudi manj številni kazenskopravni procesi.
Keywords: zgodovina žensk, kmetica, sodni zapisniki, zemljiško gospodstvo, Bled, patrimonialno sodišče, deželno sodišče, 17.st.
Published in DiRROS: 09.02.2026; Views: 110; Downloads: 52
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2. Sedimentological and paleontological analysis of the Lower Jurassic part of the Zatrnik Formation on the Pokljuka plateau, SloveniaLuka Gale, Duje Kukoč, Boštjan Rožič, Anja Vidervol, 2021, original scientific article Abstract: The uppermost Ladinian to Lower Jurassic Zatrnik Formation is the lithostratigraphic unit of the Mesozoic deeper marine Bled Basin. The uppermost part of the Zatrnik Formation and the transition into the overlying Ribnica Breccia was logged at the Zajamniki mountain pasture on the Pokljuka mountain plateau in the Julian Alps. The lowermost part the section belongs to the “classical” Zatrnik Formation and is dominated by beige micritic limestone and fine-grained calcarenite. Foraminifers Siphovalvulina, ?Everticyclammina, ?Mesoendothyra and ?Pseudopfenderina are present, indicating Early Jurassic age. The beige limestone is followed by light pink limestone of the uppermost Zatrnik Formation. Slumps are common in this interval, and crinoids are abundant. Alongside some species already present in beds lower in the succession, Meandrovoluta asiagoensis Fugagnoli & Rettori, Trocholina sp., Valvulinidae, small Textulariidae, Lagenida, and small ?Ophthalmidium alsooccur in this interval. Resedimented limestone predominates through the studied part of the Zatrnik Formation, indicating deposition on the slope or at the foot of the slope of the basin. The switch to crinoid-rich facies within the slumped interval of the Zatrnik Formation may reflect accelerated subsidence of the margins of the Julian Carbonate Platform in the Pliensbachian. The Zatrnik Formation is followed by the formation of the Pliensbachian (?) Ribnica Breccia. Impregnations of ferromanganese oxides, violet colour, and an increase in clay content are characteristic. The foraminiferal assemblage consists of Lenticulina, small elongated Lagenida, and epistominids. Individual beds of the Ribnica Breccia were deposited via debris flows. Enrichments in ferromanganese oxides point to slower sedimentation.
Keywords: Lower Jurassic, Bled Basin, Pokljuka Nappe, stratigraphy, foraminifer, Hierlatz facies, Ribnica Breccia, Zajamniki
Published in DiRROS: 09.03.2022; Views: 1766; Downloads: 761
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