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Microbial Mat-Related Structures: Laboratory Experiments and Observations from the Mesoproterozoic Belt Supergroup, Southwestern Montana, U.S.A.
DownloadSpring 2017
Siliciclastic sediments become biostabilized when benthic bacteria penetrate into the pore spaces and secure grains with filaments and extracellular polymeric substances, forming a microbial mat. The cohesive microbial cover changes typical sedimentary dynamics and leads to formation of diverse...
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