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The dominant sediments type switches between carbonate and siliciclastic over a sea-level cycle.
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Both are clearly different in geomorphology, sediments, types of salts, and ecology.
SM2: This seamount is characterized by cobbles and fine sediments types of substratum, with medium faunal abundance and diversity.
Neither sedimentation depth nor sediment type influenced biomass allocation.
Besides thickness, seismic reflection data can often reveal sediment type and the processes of sedimentation.
It images the first 10 to 50 meters of sediment beneath the seafloor, depending on bottom type, roughness and sediment type.
In addition to all these temperature-controlled provinces, Ordovician faunas are known to change with water depth, nutrient levels, and sediment type.
In order to understand this behaviour we need to know in detail: sediment concentrations, sediment type (mineralogy and grain size), organic content, current velocities, shear velocities, turbulence, wave height and period, diatom concentrations and growth rates, invertebrate types and densities, and important vertebrates such as fish and birds that have major effects on benthic invertebrates.
This sediment type extends down to a 15-m water depth (Fig. 2).
The lake sediment type was controlled by the source rocks (Gebhardt et al. 2000).
The fringing reef offshore Pakarang Cape is covered with boulders (sediment type G, Fig. 2).
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