The presence of an S-layer in a member of the Methanosarcinales was determined in the 1980s by electron microscope (EM) studies examining the cell morphology of Methanosarcina mazei.
Under conditions of low osmolarity the S-layer is extensively decorated with a polysaccharide, termed methanochondroitin, and the cells tend to grow in multicellular aggregates.
The high degree of primary amino acid sequence identity between the N- and C-terminal DUF1608 domains (79% identical and 87% similar) allowed the homology modeling of the N-terminal DUF1608 amino acid sequence onto one of the DUF1608 domains in the crystallographic DUF1608 CTR dimer thus providing the first high-resolution model of an Archaeal S-layer protein.
A model for the quaternary structure of the M. acetivorans S-layer was proposed based on packing of the MA0829 CTR in a hexagonal lattice in one of the two obtained crystal forms (Protein Data Bank accession number 3U2G).
Lateral translation of the trimeric unit creates a flat 2-dimensional sheet that has features consistent with the molecular properties of hexagonal archaeal S-layers.
Whereas the protein constituents of lipid-based barriers, such as bacterial outer membranes, can be rapidly modified in response to physiological or environmental stimuli, the large pore sizes of the S-layer composed of MSTP protein subunits are presumably required to allow passage of molecules across a protective barrier whose molecular features are difficult to modify.