Holocene shelf sedimentation patterns off equatorial East Africa constrained by climatic and sea-level changes
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文摘

The first high resolution Holocene sediment record off Tanzania, Indian Ocean

Climate and sea level control the sedimentation patterns of the Tanzanian shelf.

Lower sea level and humid climate result in river mouth bypassing during 10–8 ka.

High sea level during the mid- and late Holocene leads to shoreface bypassing.

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