Dating errors in high-resolution stratig
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Ludvig Löwemark; Friedrich Werner
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Article
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2001
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Elsevier Science
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English
⚖ 385 KB
Bioturbation in oxic deep-sea settings is often considered (if considered at all) to consist of a 2±10 cm thick homogenized layer and some easily recognizable distinct burrows which could be avoided when sub-sampling the sediment cores. However, there is one trace that is often dif®cult to discern i