{"id":43200,"date":"2024-03-06T10:26:42","date_gmt":"2024-03-06T10:26:42","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=43200"},"modified":"2025-04-01T09:09:00","modified_gmt":"2025-04-01T09:09:00","slug":"razvoj-miocenskih-paleookolisa-na-prostoru-hrvatske-i-njihova-povezanost-s-globalnim-dogadajima-rampa","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/razvoj-miocenskih-paleookolisa-na-prostoru-hrvatske-i-njihova-povezanost-s-globalnim-dogadajima-rampa\/","title":{"rendered":"Razvoj miocenskih paleookoli\u0161a na prostoru Hrvatske i njihova povezanost s globalnim doga\u0111ajima (RAMPA)"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}”][et_pb_fullwidth_slider _builder_version=”4.16″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off” global_colors_info=”{}”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”||7px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.24.0″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}”]<\/p>\n

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INTERNI ISTRA\u017dIVA\u010cKI PROJEKTI
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[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”5px||41px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ custom_margin=”||20px” custom_padding=”||50px” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.24.0″ text_font=”|300|||||||” ul_font=”||||||||” header_font=”||||||||” header_text_align=”center” header_2_font=”|800|||||||” header_2_text_align=”center” header_2_text_color=”#1e5096″ header_2_font_size=”54px” header_3_font=”|300|||||||” header_3_line_height=”1.3em” text_orientation=”center” custom_margin=”-4px||18px|||” custom_padding=”||22px|||” animation_direction=”bottom” header_2_font_size_tablet=”” header_2_font_size_phone=”30px” header_2_font_size_last_edited=”on|phone” header_2_text_shadow_style=”preset1″ header_2_text_shadow_horizontal_length=”0.03em” header_2_text_shadow_vertical_length=”0.03em” header_2_text_shadow_blur_strength=”0.05em” header_2_text_shadow_color=”rgba(0,0,0,0.3)” global_colors_info=”{}”]<\/p>\n

Razvoj miocenskih paleookoli\u0161a na prostoru Hrvatske i njihova povezanost s globalnim doga\u0111ajima (<\/strong>RAMPA)<\/strong><\/h3>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2024\/03\/rampa.png” title_text=”rampa” align=”center” _builder_version=”4.24.0″ _module_preset=”default” custom_margin=”||65px|||” global_colors_info=”{}”][\/et_pb_image][et_pb_tabs _builder_version=”4.27.4″ custom_margin=”-15px||||false|false” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″][et_pb_tab title=”O projektu” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n

U relativno kratkom geolo\u0161kom razdoblju tijekom donjeg miocena globalni i lokalni doga\u0111aji utjecali su na razvoj dva bazenska prostora s razli\u010ditom povije\u0161\u0107u talo\u017eenja: Hrvatsko zagorje (HZB) i Sjevernohrvatski bazen (SHB). Uvrije\u017eeno je mi\u0161ljenje da su donjomiocenske marinske naslage na prostoru Hrvatske jedino istalo\u017eene na malom prostoru u HZB, koji je bio dio Centralnog Paratethysa od po\u010detka miocena,\u00a0 dok\u00a0 u SHB, razvoj bazena zapo\u010dinje u otnangu s formiranjem kontinentalnih sredina nakon dugotrajne emerzije, a marinska sedimentacija zapo\u010dela je u donjem badenu. Najnovija istra\u017eivanja dokumentiraju raniju transgresiju na prostoru SHB krajem donjeg miocena te ukazuju na potrebu redefiniranja po\u010detka transgresije i rekonstrukciju paleookoli\u0161a. Promjene smjera cirkulacije i razli\u010diti karakteri prihranjivanja miocenskih bazena Hrvatske rezultirali su promjenama abioti\u010dkih i bioti\u010dkih \u010dimbenika koji odre\u0111uju razli\u010dite tipove paleookoli\u0161a. Povezivanjem sedimentolo\u0161kih, mineralo\u0161kih, geokemijskih i fosilnih podataka definirat \u0107emo paleookoli\u0161e kroz prostor i vrijeme. Koncentrirat \u0107emo se\u00a0 na prepoznavanje globalnih doga\u0111aja koji su obilje\u017eili vrijeme miocena, a posebna pa\u017enja bit \u0107e usmjerena na temperature vode u dugovje\u010dnim jezerima i moru kao i prosje\u010dne godi\u0161nje temperature\u00a0 koje su bile u skladu s promjenama globalne temperature uzrokovane fluktuacijama u sadr\u017eaju uglji\u010dnog dioksida u atmosferi. Istra\u017eivanja \u0107e se provoditi unutar dva radna paketa. Istra\u017eivanjem mineralo\u0161kih, geokemijskih i sedimentolo\u0161kih podataka te razli\u010ditih skupina fosila\u00a0 (vapnena\u010dki nanoplankton, palinomorfe, foraminifere, ostrakodi, otoliti riba i meku\u0161ci) \u00a0definirat \u0107emo tipove paleookoli\u0161a i njihov me\u0111usobni prostorni i vremenski odnos; napraviti paleoklimatsku rekonstrukciju naslaga miocena; utvrditi paleobiogeografska kretanja najzna\u010dajnijih fosilnih grupa; utvrditi glavne zonalne fosile i marker vrste pojedinih fosilnih skupina te razmotriti korelaciju s op\u0107e prihva\u0107enom zonacijom u Paratethysu i Mediteranu. Glavni cilj projekta je povezivanje\u00a0 dobivenih rezultata istra\u017eivanja s poznatim globalnim i regionalnim miocenskim doga\u0111ajima: kao \u0161to su miocenski klimatski optimum, srednjomiocenska klimatska tranzicija, badenska kriza saliniteta, doga\u0111aje izumiranja faune na granicama badena i sarmata te sarmata i panona, \u201ewashhouse\u201c doga\u0111aj u gornjem miocenu, pomak izotopa ugljika u kasnom miocenu, zahla\u0111enje u gornjem miocenu i mesinsku krizu saliniteta.<\/p>\n

RAMPA – Novosti i obavijesti<\/strong><\/em><\/a><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Voditelj” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Glavni istra\u017eiva\u010d \/ voditelj projekta:<\/strong><\/em>\u00a0D<\/em>r. sc. Valentina Hajek-Tadesse<\/em><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Suradnici” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Hrvatski geolo\u0161ki institut, Zagreb:<\/strong><\/p>\n

Bakra\u010d Koraljka,<\/p>\n

Grizelj Anita,<\/p>\n

Galovi\u0107 Ines,<\/p>\n

Kure\u010di\u0107 Tomislav,<\/p>\n

Wacha Lara,<\/p>\n

\u010cai\u0107 Jankovi\u0107 Ana,<\/p>\n

Feri\u0107 Pavle,<\/p>\n

Filjak Radovan,<\/p>\n

Milo\u0161evi\u0107 Monika (doktorandica),<\/p>\n

Mu\u017eek Katja (doktorandica)<\/p>\n

Vanjski suradnici:<\/strong><\/p>\n

Oleg Mandic, Prirodoslovni muzej Be\u010d<\/em>;<\/p>\n

Bettina Richenbacher, Ludwig-Maximilian –<\/em> Sveu\u010dili\u0161te, M\u00fcnchen, Njema\u010dka; <\/em><\/p>\n

Maud Meijers, Earth Sciences Sveu\u010dili\u0161te u Grazu; <\/em><\/p>\n

Elsa Gliozzi, ROMA TRE Sveu\u010dili\u0161te; <\/em><\/p>\n

Ljupko Rundi\u0107, Rudarsko geolo\u0161ki fakultet, Univerzitet u Beogradu; <\/em><\/p>\n

Miha Marin\u0161ek, Geolo\u0161ki zavod Slovenije; <\/em><\/p>\n

Marianna Kov\u00e1\u010dov\u00e1, Sveu\u010dili\u0161te Comenius u Bratislavi, Slova\u010dka;<\/em><\/p>\n

Marijan Kova\u010di\u0107, Prirodoslovno-matemati\u010dki fakultet Sveu\u010dili\u0161ta u Zagrebu.<\/em><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Trajanje projekta” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Trajanje projekta:<\/strong> 01.01.2024.\u201331.12.2027.<\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Kategorija” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Kategorija projekta: <\/strong><\/span>istra\u017eiva\u010dki projekt pra\u0107en od strane Ministarstva znanosti i obrazovanja Republike Hrvatske; sredstva iz Nacionalnog plana oporavka i otpornosti 2021.\u20132026. \u2013 NextGenerationEU<\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Iznos financiranja” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Financiranje:\u00a0 <\/strong><\/em>60.800,00 \u20ac<\/p>\n

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    Status:<\/strong> Aktivan<\/em><\/span><\/p>\n

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    \u00a0 INTERNI ISTRA\u017dIVA\u010cKI PROJEKTIRazvoj miocenskih paleookoli\u0161a na prostoru Hrvatske i njihova povezanost s globalnim doga\u0111ajima (RAMPA)U relativno kratkom geolo\u0161kom razdoblju tijekom donjeg miocena globalni i lokalni doga\u0111aji utjecali su na razvoj dva bazenska prostora s razli\u010ditom povije\u0161\u0107u talo\u017eenja: Hrvatsko zagorje (HZB) i Sjevernohrvatski bazen (SHB). Uvrije\u017eeno je mi\u0161ljenje da su donjomiocenske marinske naslage na prostoru […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-43200","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t