The filter-feeders signal: response of ostracods to marine environmental changes in the Devonian F–F event

The percentage of filter-feeder species in benthic ostracod assemblages shows evident changes during the Late Devonian Frasnian–Famennian (F–F) transition with two sharp rises in the event stratal interval based on materials collected from the Yangdi section, South China. Neither anoxia nor oligotrophy, eustasy should have been the only primary cause of filter-feeders signal in the F–F event. The sea level fall and rise would create...