{"title":"巴登尼亚海-中中新世古环境的古生态学研究","authors":"Monika Milošević , Vlasta Ćosović , Valentina Hajek-Tadesse , Ines Galović , Mirjana Miknić , Viktória Baranyi","doi":"10.1016/j.geobios.2025.05.005","DOIUrl":null,"url":null,"abstract":"<div><div><span><span><span>During the Badenian (Langhian–early Serravallian), a high diversity marine biocenosis inhabited the warm, normal-salinity environments spanning the </span>epicontinental sea<span> of the Alpine-Carpathian-Dinarides region known as Central Paratethys<span>. The 95 m thick sedimentary succession of the Striježevica core, located in the southwestern part of the Pannonian Basin (North Croatian Basin), provides a unique insight into the palaeoenvironmental evolution from this part of the Paratethys, including changes in water depth, salinity, oxygen, and nutrient levels. An integrated analysis, including calcareous </span></span></span>nannoplankton<span><span>, dinoflagellate cysts, benthic and planktonic foraminifera, </span>ostracods, and diversity proxies, revealed three phases of palaeoenvironmental evolution. The stratigraphic position of the studied succession in the NN4/5 Zone is indicated by the nannoplankton assemblage with </span></span><em>Helicosphaera waltrans</em>, along with the presence of the planktonic foraminifera <em>Orbulina suturalis,</em> and the dinoflagellate cyst <em>Unipontidinium aquaeductus</em><span><span>, correlated to the Middle Miocene Badenian stage. Micropalaeontological proxies indicated shelf to upper slope environments under the influence of shallow-water conditions. At the base of the Striježevica core, the composition of small benthic foraminiferal assemblages and their diversity indices indicated a eutrophic-mesotrophic environment with constant nutrient input. A “transitional environment” in the middle part of the Striježevica core was characterized by </span>eutrophication<span> related to the fertilization effect of enhanced volcanic activity in the surrounding area. A shallowing upward trend is suggested by an increase in oxygen content at the sea bed, a decrease in species richness, and a diversity drop in the benthic foraminiferal assemblage. The upper part of the section depicted a shallow, oligotrophic environment<span> with seagrass meadows evidenced by the predominance of </span></span></span><em>Biasterigerina planorbis</em> and cibicidoids.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"92 ","pages":"Pages 45-64"},"PeriodicalIF":1.6000,"publicationDate":"2025-05-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Palaeoecological insight into the Badenian Sea – Middle Miocene palaeoenvironments from the North Croatian Basin, Central Paratethys\",\"authors\":\"Monika Milošević , Vlasta Ćosović , Valentina Hajek-Tadesse , Ines Galović , Mirjana Miknić , Viktória Baranyi\",\"doi\":\"10.1016/j.geobios.2025.05.005\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div><span><span><span>During the Badenian (Langhian–early Serravallian), a high diversity marine biocenosis inhabited the warm, normal-salinity environments spanning the </span>epicontinental sea<span> of the Alpine-Carpathian-Dinarides region known as Central Paratethys<span>. The 95 m thick sedimentary succession of the Striježevica core, located in the southwestern part of the Pannonian Basin (North Croatian Basin), provides a unique insight into the palaeoenvironmental evolution from this part of the Paratethys, including changes in water depth, salinity, oxygen, and nutrient levels. An integrated analysis, including calcareous </span></span></span>nannoplankton<span><span>, dinoflagellate cysts, benthic and planktonic foraminifera, </span>ostracods, and diversity proxies, revealed three phases of palaeoenvironmental evolution. The stratigraphic position of the studied succession in the NN4/5 Zone is indicated by the nannoplankton assemblage with </span></span><em>Helicosphaera waltrans</em>, along with the presence of the planktonic foraminifera <em>Orbulina suturalis,</em> and the dinoflagellate cyst <em>Unipontidinium aquaeductus</em><span><span>, correlated to the Middle Miocene Badenian stage. Micropalaeontological proxies indicated shelf to upper slope environments under the influence of shallow-water conditions. At the base of the Striježevica core, the composition of small benthic foraminiferal assemblages and their diversity indices indicated a eutrophic-mesotrophic environment with constant nutrient input. A “transitional environment” in the middle part of the Striježevica core was characterized by </span>eutrophication<span> related to the fertilization effect of enhanced volcanic activity in the surrounding area. A shallowing upward trend is suggested by an increase in oxygen content at the sea bed, a decrease in species richness, and a diversity drop in the benthic foraminiferal assemblage. The upper part of the section depicted a shallow, oligotrophic environment<span> with seagrass meadows evidenced by the predominance of </span></span></span><em>Biasterigerina planorbis</em> and cibicidoids.</div></div>\",\"PeriodicalId\":55116,\"journal\":{\"name\":\"Geobios\",\"volume\":\"92 \",\"pages\":\"Pages 45-64\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2025-05-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geobios\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0016699525000440\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geobios","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016699525000440","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
Palaeoecological insight into the Badenian Sea – Middle Miocene palaeoenvironments from the North Croatian Basin, Central Paratethys
During the Badenian (Langhian–early Serravallian), a high diversity marine biocenosis inhabited the warm, normal-salinity environments spanning the epicontinental sea of the Alpine-Carpathian-Dinarides region known as Central Paratethys. The 95 m thick sedimentary succession of the Striježevica core, located in the southwestern part of the Pannonian Basin (North Croatian Basin), provides a unique insight into the palaeoenvironmental evolution from this part of the Paratethys, including changes in water depth, salinity, oxygen, and nutrient levels. An integrated analysis, including calcareous nannoplankton, dinoflagellate cysts, benthic and planktonic foraminifera, ostracods, and diversity proxies, revealed three phases of palaeoenvironmental evolution. The stratigraphic position of the studied succession in the NN4/5 Zone is indicated by the nannoplankton assemblage with Helicosphaera waltrans, along with the presence of the planktonic foraminifera Orbulina suturalis, and the dinoflagellate cyst Unipontidinium aquaeductus, correlated to the Middle Miocene Badenian stage. Micropalaeontological proxies indicated shelf to upper slope environments under the influence of shallow-water conditions. At the base of the Striježevica core, the composition of small benthic foraminiferal assemblages and their diversity indices indicated a eutrophic-mesotrophic environment with constant nutrient input. A “transitional environment” in the middle part of the Striježevica core was characterized by eutrophication related to the fertilization effect of enhanced volcanic activity in the surrounding area. A shallowing upward trend is suggested by an increase in oxygen content at the sea bed, a decrease in species richness, and a diversity drop in the benthic foraminiferal assemblage. The upper part of the section depicted a shallow, oligotrophic environment with seagrass meadows evidenced by the predominance of Biasterigerina planorbis and cibicidoids.
期刊介绍:
Geobios publishes bimonthly in English original peer-reviewed articles of international interest in any area of paleontology, paleobiology, paleoecology, paleobiogeography, (bio)stratigraphy and biogeochemistry. All taxonomic groups are treated, including microfossils, invertebrates, plants, vertebrates and ichnofossils.
Geobios welcomes descriptive papers based on original material (e.g. large Systematic Paleontology works), as well as more analytically and/or methodologically oriented papers, provided they offer strong and significant biochronological/biostratigraphical, paleobiogeographical, paleobiological and/or phylogenetic new insights and perspectices. A high priority level is given to synchronic and/or diachronic studies based on multi- or inter-disciplinary approaches mixing various fields of Earth and Life Sciences. Works based on extant data are also considered, provided they offer significant insights into geological-time studies.