
On the Determination of Sediment Accumulation Rates
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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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<sup>210</sup>Pb- and <sup>137</sup>Cs-Based Sediment Accumulation Rates in Inner Shelves and Coastal Lakes of Subarctic and Arctic Alaska: A Synthesis</li><li>Sedimentation Rates and Late Holocene Climate Change: A Case Study from the Skagerrak (NE North Sea)</li><li>Holocene Pelagic and Turbidite Sedimentation Rates in the Amerasia Basin, Arctic Ocean from Radiocarbon Age-Depth Profiles in Cores</li><li>Late Quaternary Variations in Sediment Accumulation Rates and their Paleoenvironmental Implications: A Case Study from the East Greenland Continental Margin</li></ul>
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