Biosedimentary disturbances in shallow-water carbonate environments: An example from the Upper Hauterivian in the Lusitanian Basin

Research output: Contribution to journalArticlepeer-review

4 Citations (Scopus)


► Paleoenvironmental significance of biological, chemical, magnetic markers in a lagoon.
► Detrital input modifies benthic foraminifera associations and mode of life.
► Activity of boring and micritizing organisms varies according to detrital input.
► δ13C variations are explained by variation of photosynthesis activity and turbidity.
► Detrital input is controlled by variations of rainfall on the continent.
Original languageUnknown
Pages (from-to)24-37
JournalPalaeogeography Palaeoclimatology Palaeoecology
Issue numberNA
Publication statusPublished - 1 Jan 2012

Cite this