The pervasive role of biological cohesion in bedform development.

The pervasive role of biological cohesion in bedform development.
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DOI:
10.1038/ncomms7257
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发表时间:
2015-02-06
影响因子:
16.6
通讯作者:
Thorne, Peter D.
Thorne, Peter D.
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Malarkey, Jonathan;Baas, Jaco H.;Hope, Julie A.;Aspden, Rebecca J.;Parsons, Daniel R.;Peakall, Jeff;Paterson, David M.;Schindler, Robert J.;Ye, Leiping;Lichtman, Ian D.;Bass, Sarah J.;Davies, Alan G.;Manning, Andrew J.;Thorne, Peter D.

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Sediment fluxes in aquatic environments are crucially dependent on bedform dynamics. However, sediment-flux predictions rely almost completely on clean-sand studies, despite most environments being composed of mixtures of non-cohesive sands, physically cohesive muds and biologically cohesive extracellular polymeric substances (EPS) generated by microorganisms. EPS associated with surficial biofilms are known to stabilize sediment and increase erosion thresholds. Here we present experimental data showing that the pervasive distribution of low levels of EPS throughout the sediment, rather than the high surficial levels of EPS in biofilms, is the key control on bedform dynamics. The development time for bedforms increases by up to two orders of magnitude for extremely small quantities of pervasively distributed EPS. This effect is far stronger than for physical cohesion, because EPS inhibit sand grains from moving independently. The results highlight that present bedform predictors are overly simplistic, and the associated sediment transport processes require re-assessment for the influence of EPS. The role of cohesion is vital to our understanding of how sedimentary bedforms evolve. Here, the authors show that microorganisms within the sediment affect cohesion and demonstrate that ripples can take up to one hundred times as long to develop when extracellular polymeric substances are present.
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