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Emese Réka Bodor (Geological and Geophysical Institute of Hungary, Budapest) is thanked for her assistance in the field, and help with data analysis. Elżbieta Witkowska (Jagiellonian University, Kraków, Poland) and Jadwiga Ziaja (Władysław Szafer Institute of Botany, Kraków, Poland) are acknowledged for their help with taxonomy, and for obtaining literature. Emanuela Mattioli (Université Claude Bernard Lyon 1, France) kindly undertook calcareous nannofossil analyses during an earlier project on the section studied. We thank Wolfram M. Kürschner (University of Oslo, Norway) for his constructive comments on an early draft of the manuscript. Two anonymous reviewers provided constructive comments and help in improving this article. The research was financed by the Hungarian Scientific Research Fund (project K72633) and the Hantken Miksa Foundation. Viktória Baranyi was also supported by an AASP Student Scholarship in 2013. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). This is MTM–MTA–ELTE Palaeo contribution number 226.\nFunding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K72633]; Hantken Miksa Foundation; AASP Student Scholarship; Natural Environment Research CouncilUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [bgs05002, bgs05016] Funding Source: researchfish\n Funding text: We thank Maria Barbacka (Hungarian Natural History Museum, Budapest), and Andras Galacz and Istvan Szente (Elitvos Lorand University, Budapest), for their helpful advice. Emese Reka Bodor (Geological and Geophysical Institute of Hungary, Budapest) is thanked for her assistance in the field, and help with data analysis. Elzbieta Witkowska (Jagiellonian University, Krakow, Poland) and Jadwiga Ziaja (Wladyslaw Szafer Institute of Botany, Krakow, Poland) are acknowledged for their help with taxonomy, and for obtaining literature. Emanuela Mattioli (Universite Claude Bernard Lyon 1, France) kindly undertook calcareous nannofossil analyses during an earlier project on the section studied. We thank Wolfram M. Kurschner (University of Oslo, Norway) for his constructive comments on an early draft of the manuscript. Two anonymous reviewers provided constructive comments and help in improving this article. The research was financed by the Hungarian Scientific Research Fund (project K72633) and the Hantken Miksa Foundation. Viktoria Baranyi was also supported by an AASP Student Scholarship in 2013. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). 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The sequence of environmental change and regional differences during the T-OAE are not yet fully understood and organic-walled phytoplankton and other palynomorphs are well-suited, but under-utilised, in research into this event. Based on quantitative palynological analyses from a black shale-bearing succession at Réka Valley in the Mecsek Mountains of southwest Hungary, five sequential palynomorph assemblages are distinguished. These reveal major shifts in organic-walled phytoplankton communities, driven by palaeoenvironmental changes. In addition, palynofacies analysis helped to document changes in the composition of sedimentary organic matter, and to quantify the terrestrial input. Assemblage 1 is characterised by a moderately diverse phytoplankton community and high levels of terrestrial palynomorphs. Assemblage 2 records a significant peak of the euryhaline dinoflagellate cyst Nannoceratopsis. Assemblage 3 is distinguished by dominance of highly opportunistic prasinophytes and the temporary disappearance of all dinoflagellate cyst taxa. Assemblages 4 and 5 represent distinctive phases of a prolonged recovery phase with low diversity phytoplankton assemblages and intermittently high levels of terrestrially-derived palynomorphs. The successive disappearance of phytoplankton taxa and the gradual takeover by opportunistic euryhaline species at the onset of the T-OAE were related to several phenomena. These include reduced salinity in the surface waters, establishment of a stable pycnocline and deterioration of nutrient recycling, followed by oxygen deficiency throughout much of the water column. The high amount of terrestrially-derived palynodebris indicates intense runoff and freshwater input, driven by the early Toarcian warming and the enhanced hydrological cycle. Comparison with coeval European successions proves that the palaeoenvironmental changes during the T-OAE were not entirely synchronous, and local factors played a crucial role in influencing phytoplankton communities. 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