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com/site/guilleorti/classification-v-4 [accessed 17 Jul
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https://doi.org/10.5852%2Fejt.2018.466
, starting with the Agnatha up to the †Osteolepidiformes
https://doi.org/10.20341%2Fgb.2023.002
The “Mo Clay” (= Fur Formation, Denmark) and “Turkmenia” (Danata Formation, Turkmenistan) localities, thought by Patterson to date to the late Paleocene, are now known to be early Eocene in age, while the Nardò sites likely lie well within the Campanian
https://doi.org/10.1038%2Fs41586-024-07323-1
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https://dx.doi.org/10.1038/s41586-026-10976-9
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https://doi.org/10.1038%2Fsrep38939
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https://doi.org/10.1038%2Fnature13472
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https://doi.org/10.1038%2Fs41598-018-32468-1
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https://doi.org/10.1080%2F14623528.2018.1459160
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