[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.4.1″ custom_padding=”0px||0px|||”][et_pb_fullwidth_slider _builder_version=”4.7.7″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.7.7″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/04\/20191015_142016a-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.7.7″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/04\/20191014_133538-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″][et_pb_row _builder_version=”4.4.2″ custom_margin=”|auto|-14px|auto||” custom_padding=”||5px|||”][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.4.7″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.2em” header_4_line_height=”1.3em”]<\/p>\n
[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″ custom_padding=”0px||41px|||”][et_pb_row _builder_version=”3.25″ custom_padding=”15px|0px|28px|0px|false|false”][et_pb_column type=”4_4″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.6.5″]<\/p>\n
Paleolimnolo\u0161ka istra\u017eivanja provode se u sklopu geokemijske karakterizacije jezerskih sedimenata i njihovih slivnih podru\u010dja, u svrhu utvr\u0111ivanja antropogenog utjecaja na navedene ekosustave i rekonstrukcije paleookoli\u0161a s ciljem utvr\u0111ivanja klimatskih promjena i promjena uzrokovanih ljudskim utjecajem tijekom pleistocena i holocena. Cilj paleolimnolo\u0161kih istra\u017eivanja je utvrditi razvoj dinami\u010dnih teresti\u010dkih ekosustava kao \u0161to su kr\u0161ka slatkovodna jezera, treseti\u0161ta i kr\u0161ka polja i njihov odgovor na globalne promjene i pove\u0107an ljudski utjecaj, prvenstveno onih koji se nalaze pod direktnim utjecajem mora. Jezgre sedimenata omogu\u0107uju bolje razumijevanje prija\u0161njih promjena i dinamike jezera i te informacije slu\u017ee za jasnije sagledavanje budu\u0107ih promjena. Intergacija nekoliko posrednih pokazatelja (proxija) (fizi\u010dke karakteristike, sedimentni facijes, mineralo\u0161ki i geokemijski sastav, palinolo\u0161ke analize, analize ostrakoda, dijatomeja, kladocera i chironomida) mo\u017ee ukazivati na rekonstrukciju talo\u017eenja sedimenta u jezerima i njegove pro\u0161losti, uklju\u010duju\u0107i razinu jezera i hidrolo\u0161ke promjene. Tijekom dosada\u0161njih istra\u017eivanja provedena su znanstvena istra\u017eivanja sedimenata Vranskog jezera na Cresu (<\/a><\/strong>\u201cIstra\u017eivanja paleorazina Vranskog jezera na Cresu\u201c<\/a><\/em>), Vranskog jezera kod Biograda (<\/a>\u201ePaleolimnolo\u0161ka istra\u017eivanja Vranskog jezera kod Biograda\u201c<\/a>), Ba\u0107inskih jezera (\u201eHidrogeolo\u0161ka i paleolimnolo\u0161ka istra\u017eivanja Ba\u0107inska jezera\u201c<\/a><\/em>), Velikog jezera na otoku Mljetu, Visova\u010dkog jezera (<\/strong>\u201cPaleolimnolo\u0161ka istra\u017eivanja u NP Krka – Visova\u010dko jezero\u201c<\/em><\/a>).<\/p>\n [\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/05\/Vransko-jezero-na-Cresu.jpg” title_text=”Vransko jezero na Cresu” align=”center” _builder_version=”4.4.7″ width=”60%” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″][\/et_pb_image][et_pb_text _builder_version=”4.6.5″ text_font_size=”13px” custom_margin=”-30px||||false|false”]<\/p>\n Vransko jezero na Cresu i istra\u017eiva\u010dka platforma \u201eQ2\u201c za uzorkovanje jezerskih sedimenata.<\/p>\n [\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":" PALEOLIMNOLO\u0160KA ISTRA\u017dIVANJA Paleolimnolo\u0161ka istra\u017eivanja provode se u sklopu geokemijske karakterizacije jezerskih sedimenata i njihovih slivnih podru\u010dja, u svrhu utvr\u0111ivanja antropogenog utjecaja na navedene ekosustave i rekonstrukcije paleookoli\u0161a s ciljem utvr\u0111ivanja klimatskih promjena i promjena uzrokovanih ljudskim utjecajem tijekom pleistocena i holocena. Cilj paleolimnolo\u0161kih istra\u017eivanja je utvrditi razvoj dinami\u010dnih teresti\u010dkih ekosustava kao \u0161to su kr\u0161ka slatkovodna […]<\/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-31555","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