Generation of the benthic foraminiferal assemblage: Theory and preliminary data

Abstract

The production of benthic foraminiferal communities is filtered through taphonomic (mainly destructive) processes within the sediments to generate the fossil assemblage. Both the production and the taphonomy depend on bottom water oxygen content and flux of organic carbon to the seabed. An examination of the relationships of processes generating the fossil assemblage to oxygen and organic carbon supply is made using pore water geochemical measurements to estimate carbon flux for locations in the Gulf of Mexico and the central California margin. The locations are plotted in a three dimensional field with bottom water oxygen content, organic carbon flux, and sediment depth as the axes. Then the response of foraminiferal standing stock, taphonomic processes and the developing fossil assemblage to the field is investigated. Variation in the vertical stratification of foraminiferal standing stock and test production, species' stratification, taphonomic process intensity and stratification, and sediment bioturbation lead to marked differences in the way the fossil assemblage is generated across the oxygen content-organic carbon flux field. The result is that the oxygen-carbon flux field has a significant impact on the fossil assemblage through the interaction of biological and biogeochemical processes in the sediments. A model of this interaction is investigated to show how its elements change across the oxygen-carbon flux field and how these affect the generation of the fossil assemblage.