{"id":49063,"date":"2026-10-06T08:20:33","date_gmt":"2026-10-06T08:20:33","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=49063"},"modified":"2026-10-06T08:22:55","modified_gmt":"2026-10-06T08:22:55","slug":"non-pollen-palynomorphs-npps-and-palynofacies-of-lake-sediments-from-the-bacina-lakes-croatia-as-indicators-of-holocene-paleoenvironmental-changes","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/non-pollen-palynomorphs-npps-and-palynofacies-of-lake-sediments-from-the-bacina-lakes-croatia-as-indicators-of-holocene-paleoenvironmental-changes\/","title":{"rendered":"Non-Pollen Palynomorphs (NPPs) and palynofacies of lake sediments from the Ba\u0107ina Lakes (Croatia) as indicators of Holocene paleoenvironmental changes"},"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=”4.27.8″ 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

Non-Pollen Palynomorphs (NPPs) and palynofacies of lake sediments from the Ba\u0107ina Lakes (Croatia) as indicators of Holocene paleoenvironmental changes<\/strong><\/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=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2026\/09\/clanak-1-logo.jpg” alt=”Quaternary science reviewes cover” title_text=”clanak 1 logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.27.8″ width=”25%” max_width=”65%” module_alignment=”center” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content”][\/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=”4.27.8″ 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 Review of Palaeobotany and Palynology<\/strong> objavljen je znanstveni rad \u201cNon-Pollen Palynomorphs (NPPs) and palynofacies of lake sediments from the Ba\u0107ina Lakes (Croatia) as indicators of Holocene paleoenvironmental changes\u201d.<\/p>\n

Rad je dio specijalnog izdanja \u201eNon-pollen palynomorphs in palaeoecological reconstructions: recent advances and future challenges\u201d a predstavlja prvo paleoekolo\u0161ko istra\u017eivanje, sa fokusom na zoolo\u0161ke Nepeludne palinomorfe (NPP-ove) kao komplementarne bioindikatore, na podru\u010dju Hrvatskih kr\u0161kih jezera.<\/p>\n

Tijekom istra\u017eivanja, dokumentiran\u00a0 je veliki broj raznolikih NPP-ova, uklju\u010duju\u0107i modrozelene (cijanobakterije) i zelene alge, Dinoflagellata (fitoplankton), spikule spu\u017evi, Chironomidae (trzalci), Cladocera (sitni rakovi), Turbellaria (jaja plosnatih crva), te raznoliki ostaci \u010dlankono\u017eaca. Rezultati su pokazali kako se brojnost fitoplanktona i zoobentosa (u obliku NPP-ova) mo\u017ee usporediti sa okoli\u0161nim faktorima kao \u0161to su organska tvar, ukupni organski ugljik (TOC), du\u0161ik (N) te raznim drugim faktorima. Untao\u010d tome, potreban je oprez kod interpretacije izoliranih ostataka zoobentosa kao \u0161to su chironomidi i cladocera, jer sami po sebi ne pru\u017eaju puno informacija o okoli\u0161u, te ih je potrebno interpretirati zajedno sa ostalim NPP-ovima i peludnim podacima. Ovo istra\u017eivanje pokazalo je kako je jezero Crni\u0161evo, u sklopu Ba\u0107inskih jezera, prolazilo nekoliko tranzicija od oligotrofnih do eutrofi\u010dnih uvjeta. Sli\u010dan pristup istra\u017eivanju NPP-ova mo\u017ee se primjeniti i na drugim jezerima na podru\u010dju Hrvatske, kako bi dobili potpuniju sliku okoli\u0161nih promjena i ljudskog utjecaja.<\/p>\n

Ovaj rad je rezultat istra\u017eivanja unutar projekta Non-Poll: Non-pollen palynomorphs and palynofacies in paleoenvironmental reconstruction <\/strong>(HRZZ IP-2024-05-1687) financiranog od strane Hrvatske Zaklade za Znanost (HRZZ)<\/p>\n

Poveznica na \u010dlanak: http:\/\/sciencedirect.com\/science\/article\/pii\/S0034666726002423?via%3Dihub<\/em><\/a> \u00a0<\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVINon-Pollen Palynomorphs (NPPs) and palynofacies of lake sediments from the Ba\u0107ina Lakes (Croatia) as indicators of Holocene paleoenvironmental changesU znanstvenom \u010dasopisu Review of Palaeobotany and Palynology objavljen je znanstveni rad \u201cNon-Pollen Palynomorphs (NPPs) and palynofacies of lake sediments from the Ba\u0107ina Lakes (Croatia) as indicators of Holocene paleoenvironmental changes\u201d. Rad je dio specijalnog […]<\/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-49063","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