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

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Abstract

Highlights.
► 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
Volume315
Issue numberNA
DOIs
Publication statusPublished - 1 Jan 2012

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