{"id":47719,"date":"2026-03-16T09:59:37","date_gmt":"2026-03-16T09:59:37","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=47719"},"modified":"2026-03-16T10:03:49","modified_gmt":"2026-03-16T10:03:49","slug":"holocene-paleoclimate-reconstruction-on-the-eastern-adriatic-based-on-ostracods-and-stable-isotopes-from-a-coastal-lake-velo-blato-croatia","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/holocene-paleoclimate-reconstruction-on-the-eastern-adriatic-based-on-ostracods-and-stable-isotopes-from-a-coastal-lake-velo-blato-croatia\/","title":{"rendered":"Holocene paleoclimate reconstruction on the eastern Adriatic based on ostracods and stable isotopes from a coastal Lake Velo Blato (Croatia)"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][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=”{}” theme_builder_area=”post_content”][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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

NAJNOVIJI OBJAVLJENI RADOVI<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.6″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Holocene paleoclimate reconstruction on the eastern Adriatic based on ostracods and stable isotopes from a coastal Lake Velo Blato (Croatia)<\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2026\/03\/paleo.jpg” alt=”Geosciences logo” title_text=”paleo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.27.6″ width=”25%” max_width=”65%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.6″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

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

Rad je dostupan za besplatno preuzimanje na sljede\u0107oj poveznici u narednih 50 dana: https:\/\/authors.elsevier.com\/c\/1mlSk73N~LwRr<\/em><\/a><\/span><\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIHolocene paleoclimate reconstruction on the eastern Adriatic based on ostracods and stable isotopes from a coastal Lake Velo Blato (Croatia)U znanstvenom \u010dasopisu Palaeogeography, Palaeoclimatology, Palaeoecology 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). Ovaj rad […]<\/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-47719","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