In the past decade, the 800 km elongated mud belt off Zhejiang-Fujian coast, East China
Sea (ECS), has been extensively studied for understanding the source to sink processes on …

While mean grain size of sensitive component in muddy sediments from Chinese coastal
seas was widely used as a proxy for reconstruction of the East Asian winter monsoon …

The source to sink process of terrigenous sediment from East Asia continent to the marginal
seas is crucial for the understanding of land–ocean interaction and marine sedimentary …

Sedimentary pyrite and the ratio between organic carbon and pyrite sulfur (C/S ratio) have
been widely used as paleosalinity indicators to distinguish between marine and freshwater …

Globally mud areas on continental shelves are conduits for the dispersal of fluvial-sourced
sediment. We address fundamental issues in sediment dynamics focusing on how mud is …

Abstract The Mid-Miocene Climatic Optimum (MMCO) is one of Earth's most recent
prolonged warming events, recorded in both the deep ocean and mid-to high-latitude …

Sedimentary responses to the cross-shelf transport on the East China Sea continental shelf
are ascertained based on analyses of the sediment grain size and detrital mineral …

The uplift of the Tibetan Plateau (TP) during the late Cenozoic is thought to be one of crucial
factors controlling Asian climate. However, the complex interaction between tectonics and …

Previous studies have considered that the wedge-shaped muddy body on the inner shelf of
the East China Sea was formed by the deposition of resuspended fine-grained sediments …

As major sites of carbon burial and remineralization, continental margins are key
components of the global carbon cycle. However, heterogeneous sources of organic matter …