Sedimentacijsko okolje srednjetriasne Strelovške formacije na Raduhi v Kamniško–Savinjskih Alpah, severna Slovenija

The Raduha section represents a continuation of the research of the Anisian Strelovec Formation in the Kamnik-Savinja Alps. The Strelovec Formation was deposited during the Anisian on a drowned section of the Serla Dolomite carbonate platform in a restricted probably outer ramp environment associated with an intraplatform basin. The base of the section is represented by dolostone breccia containing angular carbonate lithoclasts of shallow-marine origin. This is followed by alternations of laminated and homogenous hemipelagic limestones deposited in a restricted and anoxic environment. Hemipelagic sedimentation was occasionally interrupted by clay input and deposition of sediments from gravity mass flows. Slow filling of the basin lead to a gradual cessation of anoxic conditions and sedimentation of bedded shallow-marine limestones. After shallow water conditions were established, bioclastic dolostone of the Contrin Formation was deposited.Profil Raduha predstavlja nadaljevanje raziskav anizijske Strelovške formacije v Kamniško-Savinjskih Alpah. V aniziju se je na potopljenem delu karbonatne platforme formiral intraplatformni bazen, v katerem je prišlo do sedimentacije Strelovške formacije na verjetno zunanjem delu karbonatne rampe. Profil se prične z dolomitno brečo s klasti spodaj ležeče anizijske karbonatne platforme. Sledi sedimentacija hemipelagičnih plastnatih laminiranih ter homogenih apnencev v hidrodinamično mirnem in anoksičnem okolju. Umirjene pogoje sedimentacije so občasno prekinili gravitacijski tokovi (sinsedimentni zdrsi in turbiditi), ki so vnesli droben klastični material s kopnega. S počasnim zasipavanjem bazenskega okolja pride do postopne prekinitve anoksičnih pogojev ter sedimentacije plastnatih plitvovodnih apnencev, kar nakazuje na popolno zapolnitev intraplatformnega bazena. Sledi sedimentacija bioklastičnega dolomita zgornjeanizijske Contrinske formacije

Harbours and shipwrecks between prehistory and antiquity in Istria

Diplomsko delo obravnava arheološka spoznanja o pristaniščih in brodolomih ob obalah Istrskega polotoka od prazgodovine do pozne antike. Naloga je razdeljena na dva dela, in sicer na uvodni del, v katerem so predstavljene geografske in geomorfološke značilnosti obravnavanega območja, oris zgodovine prostora od prazgodovine do konca antike ter trgovina na območju Jadrana. Drugi del naloge vsebuje predstavitve izbranih pristanišč ter brodolomov.The thesis deals with the archaeological knowledge about the harbours and shipwrecks along the coasts of the Istrian peninsula from prehistoric times to the Late Antiquity. The thesis is divided into two parts, namely the introductory part, which presents the geographical and geomorphological characteristics of the area, an outline of the history of the area from prehistoric times to the end of antiquity, and the trade in the Adriatic area. The second part of the thesis presents selected ports and shipwrecks

Anisian Strelovec Formation in the Robanov kot, Savinja Alps (Northern Slovenia)

A detailed sedimentological features of the Slatinski plaz section with a transition from the deep-water Anisian (Illyrian) Strelovec Formation to the Ladinian shallow-water Contrin Formation have been presented. The Strelovec Formation is divided into fie different lithostratigraphic units that are characterised by dark hemipelagic and pelagic thin-bedded limestones and dolomitic mudstones that are frequently intercalated with deposits of gravitymass flws, slump and slide to fie-grained low-density turbidity origin. The Strelovec Formation was deposited in a hydrodynamically quiet, pelagic deeper-water anoxic environment, most probably on a gentle platform slope. In the upper part of the formation, the presence of olistolith blocks of shallow-water limestones indicates the closing of the prograding shallow-water platform wedge. Massive dolostones of Unit 6 mark the complete filing of the basin and the beginning of the shallow-water sedimentation of the Contrin Formation in the Early Ladinian

Obvladovanje hruševega ožiga (Erwinia amylovora (Burrill) Winslow et al.)

Prvi pojav hruševega ožiga pri nas je uradno zabeležen leta 2001. Prvi večji izbruh bolezni v Sloveniji je bil v letu 2003, ko se je hrušev ožig razširil po celotni Gorenjski in v okolici Maribora. Ob drugem večjem izbruhu, ki se je zgodil leta 2007, se je bolezen razširila tudi proti jugu in vzhodu države. Hrušev ožig se je ustalil na Gorenjskem, Koroškem, na območju Maribora in na Notranjskem. Kasneje sta bili iz varovanega (neokuženega) območja izločeni še občini Lendava ter Renče-Vogrsko (južno od avtoceste H4)