Structure and composition of rhodoliths from the Amazon River mouth, Brazil

Rhodolith beds are one of the main habitats of the Brazilian Equatorial Margin continental shelf due to their wide extent and provision of ecosystem services. Northern, Central and Southern zones of the Amazon River mouth were sampled between water-depths of 23 and 120 m, covering a continental shelf area of 9500 km2, to characterize the structure and composition of rhodoliths along depth gradients and related river plume influence. The deepest rhodoliths consist of a thin algal/bryozoan/encrusting foraminifer cover around relatively large nuclei that determine the nodule size and shape. At 120-m depth in the Northern zone the nuclei are made of fragments of invertebrate boundstone or oolite rudstone, whereas at 100-m depth in the Central zone the nuclei consist of sandstone clasts. In both cases, the nuclei are fragments of sedimentary rocks that accumulated on the outer shelf during significantly lower sea level. Low-light levels prevent substantial growth of the algal cover around the nuclei. Reduced illumination an d high nutrient levels led to the composition of rhodoliths at 95-m depth in the Northern zone, predominantly built by bryozoans with subordinate coralline algae around small bioclastic nuclei. In the Central zone at 50–55 m depths, coralline algae are the main components of mostly sub-spheroidal rhodoliths. They have relatively recent ages of hundreds of years or show two phases of growth with the older phase beginning 1300 years ago and then being interrupted from about 1000 years BP to 600 years BP. All this suggests relatively high burial rates due to sediment flux, changing in time to favor exhumation after burial in some instances. The rhodoliths from 23 m in the Southern zone are growing under a low influence of the river plume and have the highest diversity of coralline algae and other builders. The rhodolith structure in the different sampling zones and depths reflects plume influence on light penetration, nutrient and organic matter levels, and sedimentation on the shelf, determining residence times of rhodoliths on the seafloor before burial.