In marine microbiology, the structural role of microbial mats in coastal sediment stabilization has been extensively documented. Microbial mats are multi-layered functional communities of microorganisms, predominantly cyanobacteria and microalgae, that form cohesive organic films over benthic surfaces in tidal environments. Early ecological surveys suggested that these microbial mats protected sediments against hydrodynamic erosion solely through mechanical binding, a physical mechanism wherein long filaments of cyanobacteria physically entangle with surrounding mineral grains. However, more recent biochemical analyses demonstrate that extracellular polymeric substances (EPS)—complex high-molecular-weight polymers secreted by cyanobacteria—play a far more pivotal stabilization role than mechanical binding alone.
Specifically, EPS acts as a sticky organic matrix that coats sediment particles and increases critical shear stress, thereby significantly elevating the threshold water flow velocity required for sediment mobilization during routine tidal cycles. Furthermore, research indicates that the chemical composition of EPS varies systematically according to seasonal shifts. During periods of peak summer photosynthetic activity, cyanobacterial production of acidic polysaccharides within the EPS matrix increases markedly. This chemical shift enhances ionic cross-linking with divalent cations, such as calcium and magnesium, which are abundantly present in surrounding seawater. Consequently, this seasonal biochemical modification strengthens the overall structural cohesion of the sediment bed, rendering coastal mudflats remarkably resilient to erosive storm surges during late summer and early autumn months.
According to the passage, which of the following describes how extracellular polymeric substances (EPS) elevate the threshold velocity required for sediment mobilization?
- By forming a cohesive matrix that coats mineral particles and elevates critical shear stressCevap
- BBy physically entangling mineral grains with long cellular filaments during low tide
- CBy decreasing the concentration of calcium and magnesium cations in surrounding seawater
- DBy replacing photosynthetic activity as the primary driver of microbial mat growth during summer
- EBy serving as the main structural support for coastal mudflats during early spring storm surges