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U znanstvenom \u010dasopisu Palaeogeography, Palaeoclimatology, Palaeoecology<\/em><\/strong> objavljen je znanstveni rad pod naslovom Holocene paleoclimate reconstruction on the eastern Adriatic based on ostracods and stable isotopes from a coastal Lake Velo Blato (Croatia)<\/em><\/strong>. Ovaj rad rezultat je suradnje znanstvenika Hrvatskog geolo\u0161kog instituta sa znanstvenicima iz Hrvatskog prirodoslovnog muzeja i Britanske geolo\u0161ke slu\u017ebe, a financiran je od strane javne ustanove Natura Jadera i Zavoda za mineralne sirovine i marinsku geologiju Hrvatskog geolo\u0161kog instituta. Rad je proiza\u0161ao iz znanstvenog usavr\u0161avanja doktorandice Hrvatskog geolo\u0161kog instituta i Rudarsko-geolo\u0161ko-naftnog fakulteta, Ivone Ivki\u0107 Filipovi\u0107, u laboratorijima za stabilne izotope Britanske geolo\u0161ke slu\u017ebe, koji je ostvaren uz potporu stipendije zaklade British Scholarship Trust. \u00a0\u00a0\u00a0<\/p>\n U radu je prikazana detaljna paleookoli\u0161na i paleoklimatska rekonstrukcija razvoja kr\u0161kog jezera Velog Blata na otoku Pagu tijekom holocena na temelju analiza stabilnih izotopa kisika i ugljika u jezerskom karbonatu i lju\u0161turicama ostrakoda, ugljika u organskoj tvari te multivarijatnoj statisti\u010dkoj analizi ostrakoda primjenom metode CoDA (Compositional Data Analysis). Interpretacije su potkrijepljene i hidrokemijskim analizama jezerske vode.<\/p>\n Paleoklimatska i paleookoli\u0161na rekonstrukcija jezera za posljednjih 8100 cal yr BP pokazuje dinami\u010dne promjene od otvorenog slatkovodnog i bo\u010datog jezera do postupnog ispunjavanja sedimentom i razvoja mo\u010dvare. Podaci stabilnih izotopa i ostrakodne faune upu\u0107uju da su promjene prvenstveno bile posljedica regionalnih klimatskih varijacija i promjena razine mora, uz mogu\u0107e antropogene utjecaje u rimskom i srednjovjekovnom razdoblju. Rezultati tako\u0111er isti\u010du izazove u interpretaciji stabilnih izotopa u kr\u0161kim jezerima poput kontaminacije uzoraka detritalnim karbonatom (prvenstveno iz fli\u0161kih naslaga) tijekom vla\u017enih perioda te intruzije morske vode kroz okr\u0161enu podlogu, koji zna\u010dajno utje\u010du na interpretaciju zapisa u sli\u010dnim okoli\u0161ima.<\/p>\n