Marine Micropaleontology

Papers
(The TQCC of Marine Micropaleontology is 4. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-08-01 to 2026-08-01.)
ArticleCitations
An endemic conodont fauna of Darriwilian (Middle Ordovician) age from the Santa Gertrudis Formation, southwestern Gondwanan margin and its paleobiogeographic relationships21
Integrated statistical analysis of calcareous nannofossil and elemental geochemistry of an outcrop from of the eastern Cenomanian Western Interior Seaway: Novel insights of shallow marine paleoceanogr20
Corrigendum to <‘Evolution of Neogene fossil ceratoliths (Coccolithophores) by duplication title of article’> <[Marine Micropaleontology 201 (2025) Article 102530]>20
Biostratigraphy and Paleoenvironments of the Pirabas Formation (Neogene, Pará State-Brazil)17
Morphometric analysis of coccolithophore genus Reticulofenestra: Insights into taxonomy and evolution during late Eocene to early Oligocene15
Enhanced sedimentary ancient DNA (sedaDNA) retrieval from Antarctic diatoms15
The influence of submarine canyons-related processes on recent benthic foraminiferal distribution, Espírito Santo Basin, Southeastern Brazil14
The record of marine ingression in western Gondwana from Devonian conodonts in the Amazonas and Solimões basins, Brazil14
Extraction of calcareous dacryoconarid microfossils from limestones and mudrocks by surfactants paired with freeze-thaw processing12
Editorial Board12
Dinoflagellate cysts in sediment traps from the Nordic Seas: Implications for their use as proxies in paleoceanography11
Sudden disappearance of the foraminifer Calcarina gaudichaudii in the boundary between the Southern and Central Kuroshio ecoregions in the Ryukyu Archipelago, Japan11
Merging databases for CNN image recognition, increasing bias or improving results?10
Linkages between modern benthic foraminiferal assemblages and environmental conditions at continental slope depths: From Baffin Bay to the Labrador Sea10
Changes in calcareous nannofossil assemblages linked to dramatic climate change over the Paleocene–Eocene Thermal Maximum in the Taramsa Section, Central Nile Valley, Egypt10
Nutrients and hydrography explain the composition of recent Mediterranean planktonic foraminiferal assemblages9
Are there marine sedimentary losses and transgressions in the Southeast Bohai Sea during MIS 2-MIS 3?9
Holocene coastal sedimentary evolution of the southern Taihu Plain, East China9
Carbon isotope study of conodont elements: Applications and limitations9
Conodonts paleobiogeographic dynamic of the Pennsylvanian epicontinental sea Itaituba-Piauí, in the northern intracratonic Brazilian basins, Western Gondwana9
Lower Cretaceous calcareous nannofossils and their biostratigraphic and paleoceanographic implications in Southern Tibet8
Paleocene–Eocene boundary in the Gabal El-Gir, east Qena, Egypt: Paleoenvironment and sequence stratigraphy interpretations8
Foraminifera in temperate fjords strongly affected by glacial meltwater, Tierra del Fuego, South America8
Editorial Board8
Foraminiferal insights into the complexities of the turbidity currents triggered by the 2016 Kaikoura Earthquake, New Zealand8
Editorial Board8
Editorial Board8
Patterns of morphological variation in coiling forms of the planktic foraminifer Pulleniatina obliquiloculata across the Pleistocene L5 coiling event (Solomon Sea)8
Modern benthic foraminifera distribution in littoral environments of Bahía Samborombón8
Editorial Board7
Calcareous Nannofossil variability controlled by Milankovitch and sub-Milankovitch periodicity in the Monte San Nicola section (Gelasian GSSP / MIS 100–104)7
Editorial Board7
Santonian deep sea benthic foraminifera from IODP Site U1513, Mentelle Basin (SW Australia): Reactions of benthic foraminiferal assemblages to surface water cooling at southern high latitudes7
Comparison of sedimentary ancient DNA (sedaDNA) extraction and shotgun metagenomic library preparation techniques7
A 9000-year marine diatom assemblage reconstruction off Eastern Tasmania, Australia, using microfossil and molecular methods6
Corrigendum to “Microbial-dominated dendrolites in the Zhangxia Formation of the Cambrian Miaolingian: A case study of the Dongping section, Shandong Province, eastern China” [Marine Micropaleontology6
Conodont size in time and space: Beyond the temperature-size rule6
Editorial Board6
Paleoecological and paleobiogeographic implications of a seagrass-indicating foralgal skeletal assemblage: Retracing the Burdigalian Quilon Limestone (Kerala Basin, SW India)6
New paleocene calcareous nannofossils: Carlamuelleria, Davidbukrya, Mauriceblackia, Noelia and Senelia6
Radiolarian and Phaeodarian high-rank assemblage change through time in the Scotia Sea: A paleo-genomics approach (IODP Exp. 382)6
Complementarity of ancient DNA and microfossil records in a marine sedimentary archive from the Arctic6
Seasonal patterns of coccolithophores in the ultra-oligotrophic South-East Levantine Basin, Eastern Mediterranean Sea6
Foraminiferal biostratigraphy and correlation of the uppermost Cretaceous in the Paraíba and Potiguar onshore basins (northeastern Brazil) and their relationship with the Tethyan phosphogenesis event6
Implications of finding Peraclis spp. in the Holocene sediments of the northeastern Arabian Sea5
Relative abundance and biometry of Bolivina ordinaria on the northern continental slope of the Pelotas basin during the late Quaternary5
Editorial Board5
Machine Learning for identification and classification of Foraminifera: Testing on monothalamids5
Microfossil fragmentation across the Paleocene-Eocene transition at ODP Site 1209 (North Pacific): Implication for reconstructing nannofossil fluxes.5
Palynological approach to identifying the Pliocene-Pleistocene boundary and paleoenvironmental evolution in the southeastern continental shelf, East Sea5
Pseudofurnishius (Conodonta) from the Triassic Drežnica section, Bosnia and Herzegovina5
Distribution of modern benthic foraminiferal assemblages across the Northeast Greenland continental shelf5
Distribution of Miocene dinoflagellate cysts in the paralic basins of Tunisia: Paleogeographic and paleoecological reconstruction and eustatic movements5
Migration of oceanic fronts in the Pacific Southern Ocean during the Mid-Pleistocene transition5
Progress, challenges and future directions in marine organic-walled dinoflagellate cyst research: New insights from an international workshop5
Foraminifera community assemblages from the southern Maldivian Archipelago: A helpful baseline for future environmental assessments4
Editorial Board4
Paleoecological patterns and Panthalassic paleobiogeographic affinity of Pennsylvanian conodont faunas from the Chibcha Terrane (Colombia)4
Editorial Board4
Editorial Board4
Palaeoceanographic and palaeoenvironmental controls on late Quaternary benthic foraminifera of the western continental slope of South Africa4
The biphasic life cycle of the non-spinose planktonic foraminifera is characterised by an aberrant coiling signature4
Upper Ocean variations at IODP Hole U1505C in the northern South China Sea and their response to the East Asian Monsoon during the middle Miocene4
Benthic foraminifera biomass on the continental slope and São Paulo plateau of Santos Basin (SE Brazil): Comparison of different estimation methods4
Extant benthic foraminifera from the Indonesian seas: An update of what we know so far and implications for future studies4
Foram3D: A pipeline for 3D synthetic data generation and rendering of foraminifera for image analysis and reconstruction4
Synergic role of frontal migration and silicic acid concentration in driving diatom productivity in the Indian sector of the Southern Ocean over the past 350 ka4
Distribution of modern dinocysts and pollen in the western Mediterranean Sea (Algerian margin and Gulf of Lion)4
Using foraminifera to assess changes in marine coastal habitats of Caribbean Panama since the Middle Holocene4
Deep learning object detection for fossil diatom counting: assessing the impact of fossil preservation and intraspecific morphological variation4
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