Sediment accumulation rates are an essential tool for the understanding of processes related to the deposition of organic and inorganic materials in marine and lacustrine environments. Sediment accumulation rates are not only a measure of the speed of deposition, but also represent a very useful tool for further paleoenvironmental reconstructions of climate history or biotic evolution as seen in the fossil record.
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Age-Depth Models Alaskan Shelves and Lakes Arctic Ocean Bioturbation Brownian Motion Coccolithophore Continental Margin Holocene IRD Luminescence Manganese Nodules Mass Accumulation Rate ODSN Okhotsk Sea Persistence