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<p>ocean waters above. Physically, seabed sediments often come from the <a href="page.php?w=erosion">erosion</a> of material on land and from other rarer sources, such as <a href="page.php?w=volcanic_ash">volcanic ash</a>. Sea currents transport sediments, especially in shallow waters where <a href="page.php?w=Tide">tidal energy</a> and <a href="page.php?w=wave">wave</a> energy cause resuspension of seabed sediments. Biologically, microorganisms living within the seabed sediments change seabed chemistry. Marine organisms create sediments, both within</p><p>
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