Marine Micropaleontology最新文献

{"title":"Orbital-scale biotic and paleoceanographic changes in Japan Sea during the late Miocene global cooling (LMGC)","authors":"Mizuki Tojima ,&nbsp;Masayuki Ikeda ,&nbsp;Kenji M. Matsuzaki","doi":"10.1016/j.marmicro.2025.102448","DOIUrl":"10.1016/j.marmicro.2025.102448","url":null,"abstract":"<div><div>The late Miocene global cooling (LMGC; ca. 7.9–5.8 Ma) was accompanied by global environmental changes including monsoon intensity, ocean circulation, and biotic turnover. Recent studies have revealed drastic environmental and biotic changes in the Japan Sea across the LMGC; the radiolarian fauna in the Japan Sea suggested decreased inflow of Pacific Central Water (PCW) species <em>Tricolocapsa papillosa,</em> increased subarctic species <em>Cycladophora sphaeris</em> and extinction of a dominant endemic radiolarian <em>Cycladophora nakasekoi</em>. These radiolarian fluxes showed ∼100-kyr eccentricity signals; however, the dominant paleoclimatic/paleoceanographic signal during the LMGC appeared to be ∼40-kyr obliquity cycle, which was not detected in the radiolarian fluxes possibly due to lower sampling resolution. Thus, orbital-scale variations of these radiolarian fluxes and their potential forcing mechanisms remain unclear.</div><div>In this study, we establish changes in the abundance of selected radiolarian species with a resolution that exceeds the 10-kyrs and suggest obliquity-paced changes in the paleoceanography in the Japan Sea during the LMGC. We detected ∼40-kyr cycles in abundance of <em>T</em><em>.</em> <em>papillosa</em>, suggesting that PCW inflow into the Japan Sea was controlled by a 40-kyr obliquity-paced glacial cycle. We also detected a ∼ 40-kyr signal in <em>C</em><em>.</em> <em>sphaeris</em> abundance, implying that the obliquity-paced winter monsoon probably promoted the inflow of subarctic water into the Japan Sea. Contrary, variation in <em>C</em><em>.</em> <em>nakasekoi</em> abundance lacks a ∼ 40-kyr signal. A 100-kyr cycle is also observed in a summer monsoon proxy from lacustrine sediment in China. Hence, it is possible that <em>C</em><em>.</em> <em>nakasekoi</em> decreased with weakened summer monsoon across the LMGC.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102448"},"PeriodicalIF":1.5,"publicationDate":"2025-01-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143148817","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The biostratigraphy and palaeobiogeography of the Late Jurassic dinoflagellate cysts from the Binalud Mountains, NE Iran","authors":"Behnaz Kalanat ,&nbsp;Elham Davtalab ,&nbsp;Ahmad Raoufian","doi":"10.1016/j.marmicro.2025.102446","DOIUrl":"10.1016/j.marmicro.2025.102446","url":null,"abstract":"<div><div>This study investigates the dinoflagellate cysts from the upper part of the Dalichai Formation in the Binalud Mountains (NE Iran, western Tethys), where the deposits are primarily consist of shale and marlstone layers. The analyzed section yielded common and diverse dinoflagellate cyst assemblages comprising 46 species belonging to 33 genera. These assemblages are correlated with the DSJ24–DSJ33 dinoflagellate cyst Zones of the Late Jurassic (late Oxfordian–Tithonian) in the Northern Hemisphere. Key bioevents identified in this interval included the last occurrences of <em>Compositosphaeridium polonicum</em> in the late Oxfordian, the last occurrence of <em>Ctenidodinium ornatum</em> at the Oxfordian–Kimmeridgian boundary, the last occurrences of <em>Tubotuberella eisenackii</em> and <em>Scriniodinium crystallinum</em> in the early Kimmeridgian, and the last occurrence <em>Endoscrinium luridum</em> around the Kimmeridgian–Tithonian boundary. The dinoflagellate cyst assemblages exhibit strong similarities to the flora of the western Tethys (the Middle East, Europe, eastern North America, and North Africa) and are marked differences from coeval assemblages of the eastern Tethys (Australasia, eastern Asia, and northeastern India), reflecting significant provincialism between the western and eastern Tethys during the Late Jurassic.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102446"},"PeriodicalIF":1.5,"publicationDate":"2025-01-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143098473","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Variations in the morphometric characteristics of Fragilariopsis kerguelensis in the Southwest Pacific sector of the Southern Ocean over the past 40,000 years","authors":"Xavier Crosta,&nbsp;Thibault Sutre","doi":"10.1016/j.marmicro.2025.102447","DOIUrl":"10.1016/j.marmicro.2025.102447","url":null,"abstract":"<div><div>High-throughput measurements demonstrated the presence of two morphotypes of <em>Fragilariopsis kerguelensis</em> in the Atlantic sector of the Southern Ocean, the proportions of which in downcore samples may be used to reconstruct past sea-surface temperatures quantitatively. We here measured the mean length, width, area, and rectangularity in core SO136–111 to assess variations in both morphotypes in the Polar Front Zone of the western Pacific sector of the Southern Ocean over the past 40,000 years. Mean length, width, and area increased rapidly at the end of the glacial period when the Polar Front migrated southward to reach the core site, ocean temperature increased, and sea ice was no longer present. In contrast, mean rectangularity decreased at the end of the glacial period, when the proportion of the cold-water, high-rectangularity morphotype declined as the ocean warmed at the core site. Downcore patterns and quantitative values of all morphometric characteristics in the southwest Pacific sector agree well with previous studies from the Atlantic sector, suggesting the presence of a similar population of <em>F. kerguelensis</em> in the open Southern Ocean. Nevertheless, rectangularity-based relationships can ultimately produce unrealistic estimates of sea-surface temperatures in core SO136–111 when the proportion of the high-rectangularity morphotype is too low, indicating that these approaches are now limited to temperatures below 3–4 °C.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102447"},"PeriodicalIF":1.5,"publicationDate":"2025-01-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143098474","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Distribution of Miocene dinoflagellate cysts in the paralic basins of Tunisia: Paleogeographic and paleoecological reconstruction and eustatic movements","authors":"Nadia Ben Moktar ,&nbsp;Amel Mahjoubi-Ghanmi ,&nbsp;Beya Mannai-Tayech","doi":"10.1016/j.marmicro.2025.102443","DOIUrl":"10.1016/j.marmicro.2025.102443","url":null,"abstract":"<div><div>The Miocene deposits of northeastern and central-eastern Tunisia are primarily of clastic, deltaic-type. These deposits are organized into complex sedimentary sequences shaped by tectonic activity, eustatic fluctuations, and changes in climatic conditions. This study presents the evolution of dinoflagellate cysts associations extracted from Miocene-age deposits. These deposits ranged from 16 million to 5.3 million years ago. They are taken from three boreholes and three sections in northeastern and central Tunisia. Dinocysts serve as valuable indicators of climatic variations and sea-level fluctuations. Their study supports the results obtained from the analysis of pollen grains. It sheds light on paleoecology, paleogeography, and eustatic conditions during that period.</div><div>Various associations (oceanic, neritic, climatic, etc.) were established based on the ecological preferences of these marine microorganisms. Oceanic conditions are characterized by the presence of <em>Impagidinium</em>. Shallow marine environments are defined by the presence of <em>Cordosphaeridium inodes minimus</em>. Meanwhile, <em>Nematosphaeropis</em> and <em>Tectatodinium</em> indicate a neritic to oceanic environment. It is confirmed by the abundance of <em>Lejeunecysta</em>, <em>Operculodinium</em>, <em>israelianum</em>, <em>Polysphardium zoharyi</em>, <em>Homotryblium</em>, <em>Spiniferites</em>, <em>Cleistosphaeridium</em>, and <em>Lingulodinium machaerophorum</em>. These results align with lithological and biostratigraphic data related to paleobathymetry and paleogeography.</div><div>Changes in dinocyst taxa relative abundances helped track the shoreline's evolution during the Miocene. Variations in the relative abundance of <em>Impagidinium</em> and <em>Cordosphaeridium inodes minimus</em>, or their absence, indicate environmental shifts. This shift reflects a transition from a neritic environment (Aïn Grab Formation) to an oceanic one (Mahmoud Formation). The Saouaf Formation is marked by a eustatic drop at its base (Unit I). However, Units II and III are defined by eustatic rises in pulsations. The Somaa sands were deposited in a neritic and/or epicontinental environment, followed by a return to an oceanic setting (Melquart Formation).</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102443"},"PeriodicalIF":1.5,"publicationDate":"2025-01-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143098429","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Machine Learning for identification and classification of Foraminifera: Testing on monothalamids","authors":"Anna Sabbatini ,&nbsp;Francesca Caridi ,&nbsp;Domenico Potena ,&nbsp;Alessandra Negri","doi":"10.1016/j.marmicro.2025.102442","DOIUrl":"10.1016/j.marmicro.2025.102442","url":null,"abstract":"<div><div>Here we propose an AI-based approach using machine learning (ML) to assist species identification and reduce morphotype redundancy in the study of monothalamous foraminifera. In fact, this group of protists, is often overlooked in taxonomic studies due to their morphological simplicity and diversity. These single-celled organisms with “soft” tests are poorly studied, with only a few species identified, while many morphotypes remain undescribed. Taxonomic research on monothalamids is limited by challenges in identification, lack of fossilization, and the time-intensive nature of the work. This gap may lead to underestimating biodiversity and hinder detecting ecosystem degradation. Despite these challenges, monothalamids play key roles in marine ecosystems, making their diversity crucial for conservation and resource management. With this in mind, we analyzed images from the scientific literature, extracting key morphological traits, such as chamber shape, shell type, composition, and aperture type, through objective human annotation to build a dataset processed by ML algorithms. Clustering techniques, such as K-Means, revealed that basic shape, followed by shell type and composition, were the primary features distinguishing clusters. This approach enabled more objective morphotype classification, improving consistency and reducing human bias.</div><div>These findings align with recent taxonomic revisions and demonstrate that applying unsupervised ML methods enhances species identification accuracy and streamlines the analysis of high-dimensional datasets.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102442"},"PeriodicalIF":1.5,"publicationDate":"2025-01-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143098472","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Morphometric analysis of coccolithophore genus Reticulofenestra: Insights into taxonomy and evolution during late Eocene to early Oligocene","authors":"Ruigang Ma ,&nbsp;David Bord ,&nbsp;Xiaobo Jin ,&nbsp;Chuanlian Liu","doi":"10.1016/j.marmicro.2024.102435","DOIUrl":"10.1016/j.marmicro.2024.102435","url":null,"abstract":"<div><div>The coccolithophore <em>Reticulofenestra</em> is key to understanding late Cenozoic climate change, but taxonomic identification remains challenging. This study uses morphometric and mixture analysis to evaluate taxonomic criteria for late Eocene to early Oligocene <em>Reticulofenestra</em>. The method enables a systematic comparison between the taxonomic morphotypes and the components recognized through Gaussian mixture modeling of parameters of distal shield length, circularity, and central opening ratio. At the species level, a total of nine morphotypes were studied from 6700 data points collected across three study sites in the mid–low latitude Atlantic–Indian Oceans. The results demonstrate that length and circularity effectively distinguish groups, validating their uses as primary taxonomic criteria. Nevertheless, central opening ratio exhibits high intra–group variability, limiting its standalone application. In addition, our integrated data reveal three evolutionary phases: (1) initial diversification during late Eocene cooling; (2) extinction following peak diversity after the Eocene–Oligocene Transition; and (3) early Oligocene stabilization reflecting adaptation in smaller species. This work provides statistical references for the validation of semi-quantitative morphologic descriptions, which may help establish a robust framework for identifying this ecologically vital lineage and enhance our understanding of phytoplankton responses to past environmental changes. Future genomic studies will be crucial for elucidating genotype-phenotype-environment relationships in <em>Reticulofenestra</em> evolution.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"195 ","pages":"Article 102435"},"PeriodicalIF":1.5,"publicationDate":"2025-01-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143098471","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"High-resolution Danian–Selandian benthic foraminifera-based paleoenvironmental reconstruction and response to sequence stratigraphy: Inferences from the Elles section, El Kef Basin, Tunisia","authors":"Sherif Farouk ,&nbsp;Islam El-Sheikh ,&nbsp;Sreepat Jain ,&nbsp;Fayez Ahmad ,&nbsp;Zaineb Elamri ,&nbsp;Jenö Nagy ,&nbsp;Khaled Al-Kahtany ,&nbsp;Youssef S. Bazeen","doi":"10.1016/j.marmicro.2024.102433","DOIUrl":"10.1016/j.marmicro.2024.102433","url":null,"abstract":"<div><div>High-resolution (123 samples) benthic foraminiferal distribution patterns were analyzed for paleoenvironmental reconstruction from a section located at the southern edge of the El Kef Basin (El Haria Formation; Tunisia) spanning the Danian–Selandian interval (planktic foraminifera P1a–P4b zones). Five distinct clusters were identified, each representing different paleoenvironments and depths ranging from inner neritic to upper bathyal, with significant variations in species diversity, paleoproductivity, and bottom water oxygenation. The Dan-C2 hypothermal event is characterized by moderately oxygenated bottom waters, high species diversity, and lowered paleoproductivity within an upper bathyal setting. The LDE is marked by high species diversity, higher paleoproductivity, moderately oxygenated bottom waters, abundance of epifaunal species, and shallowing to middle neritic depths. The Danian-Selandian boundary records (a) a sudden abundance of the inner neritic infaunal species <em>Bulimina strobila</em>, (b) an increase in species diversity, (c) moderately‑oxygenated bottom waters, (d) a positive δ¹³C excursion, and (e) deepening, from inner to middle neritic settings. Four transgressive-regressive (T-R) cycles based on benthic foraminiferal assemblage-derived bathymetry, P% and the transfer function-based estimate mirror each other, and distinctly mirror paleodepth changes, correlating with global eustatic cycles but also reflecting local tectonic influences.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"194 ","pages":"Article 102433"},"PeriodicalIF":1.5,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143095809","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Non-pollen palynomorphs as indicators of local environmental conditions in a Neotropical Estuary (Northeast Brazil)","authors":"Pietro Martins Barbosa Noga ,&nbsp;Anne de Vernal ,&nbsp;Daniela Mariano Lopes da Silva ,&nbsp;Doriedson Ferreira Gomes","doi":"10.1016/j.marmicro.2024.102424","DOIUrl":"10.1016/j.marmicro.2024.102424","url":null,"abstract":"<div><div>Non-pollen palynomorphs (NPPs) are organic-walled microfossils derived from diverse aquatic and terrestrial organisms, frequently observed in palynological studies. This study documents the distribution of NPPs in surface sediment samples from the two main rivers of Camamu Bay (Northeast Brazil), analyzed to explore their response to estuarine environmental and nutritional gradients. Using standard palynological techniques, 69 NPP taxa were identified, spanning 40 divisions, including dinoflagellates, foraminiferal linings, chlorophytes, cyanobacteria, ciliates, amoebozoans, scolecodonts, zoological fragments, and fungal spores. Assemblages were dominated by fungal spores across most stations. Distinct environmental gradients were reflected in NPP distribution, for instance upstream stations with low salinity (3 psu) and high nutrient ratios favored chlorophytes, while downstream stations with higher salinity (up to 35 psu) and lower N:P ratios (&lt;40 μM) were dominated by foraminiferal linings. Multivariate statistic analyses revealed that salinity and nutrient stoichiometry were significant drivers of assemblage composition. These findings highlight the utility of NPPs as indicators of environmental and biogeochemical conditions, particularly in low-latitude estuarine systems, and underscore their potential applications in paleoecological reconstruction.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"194 ","pages":"Article 102424"},"PeriodicalIF":1.5,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143095751","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Benthic foraminiferal population dynamics at the Goban Spur off Southwest Ireland reveal glacial-interglacial bottom water ventilation and organic flux variability over the last 420,000 years","authors":"Stanislaus Glenndy Fabian ,&nbsp;Stephen J. Gallagher ,&nbsp;David De Vleeschouwer","doi":"10.1016/j.marmicro.2024.102432","DOIUrl":"10.1016/j.marmicro.2024.102432","url":null,"abstract":"<div><div>Benthic foraminiferal assemblages from Deep Sea Drilling Project (DSDP) Site 548 on the Goban Spur off southwestern Ireland shed light on the changes in bottom water oxygenation and organic matter flux to the sea floor during the late Quaternary. Correlations of benthic foraminiferal δ¹⁸O values, the relative abundance of <em>Neogloboquadrina pachyderma</em> (%NP), and Ice Rafted Debris (IRD) concentration to global and regional and North Atlantic datasets suggest the upper 60 m of DSDP Site 548 extend to 420,000 years. Downcore variations of &gt;63 μm benthic foraminifera assemblages, abundance, and diversity reveal changes in dissolved oxygen concentration and organic fluxes to the seafloor related to glacial-interglacial cyclicity. <em>Cassidulina laevigata</em> and low dissolved oxygen indicator taxa such as <em>Bolivina</em> spp. and <em>Globobulimina</em> spp. characterised colder climates associated with lighter benthic δ¹³C values, suggesting minimal organic flux and/or weaker bottom water ventilation. In contrast, warmer interglacials are typified by heavier benthic δ¹³C, increased %CaCO₃, common high dissolved oxygen indicator taxa such as <em>Globocassidulina subglobosa</em> and phytodetritus sensitive taxa such as <em>Alabaminella weddellensis</em> and <em>Epistominella exigua</em>, suggest a more ventilated bottom water and increased organic fluxes to the seafloor, possibly associated with the invigoration of the Mediterranean Outflow Water (MOW).</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"194 ","pages":"Article 102432"},"PeriodicalIF":1.5,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143095810","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Paleoecological and paleoenvironmental insights from Ornatorotaliidae (larger foraminifera)","authors":"Andrea Benedetti ,&nbsp;Antonino Briguglio ,&nbsp;Lorenzo Consorti ,&nbsp;Cesare Andrea Papazzoni","doi":"10.1016/j.marmicro.2024.102423","DOIUrl":"10.1016/j.marmicro.2024.102423","url":null,"abstract":"<div><div>The present study deals with the ecology and phylogenetic relationships among species of the genera <em>Ornatorotalia</em>, <em>Granorotalia</em>, and <em>Risananeiza</em> belonging to the Family Ornatorotaliidae. The microfacies analyses allowed us to assign each taxon to its life paleoenvironment within the shallow-water carbonate setting, and to make a comparison with extant species belonging to the family Calcarinidae. While different species of <em>Ornatorotalia</em> and <em>Granorotalia</em> thrived only in the inner ramp, <em>Risananeiza</em> spp. possibly inhabited also deeper environments up to the middle ramp. The phylogenetic relationships among genera and species are here briefly discussed, nonetheless it's still impossible to identify any unambiguous ancestor of this group.</div></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"194 ","pages":"Article 102423"},"PeriodicalIF":1.5,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143095752","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}