Mangrove forests have survived a number of catastrophic climate events since first
appearing along the shores of the Tethys Sea during the late Cretaceous-Early Tertiary. The …

Mangroves occur on upper intertidal shorelines in the tropics and subtropics. Complex
hydrodynamic and salinity conditions, related primarily to elevation and hydroperiod …

The response of mangroves to high rates of relative sea level rise (RSLR) is poorly
understood. We explore the limits of mangrove vertical accretion to sustained periods of …

A detailed spatial inventory of the extent and depth distribution for tropical peatlands is not
currently available; however, there is a critical need for new detailed peatland information at …

Abstract Tropical Southeast (SE) Asia harbors extraordinary species richness and in its
entirety comprises four of the Earth's 34 biodiversity hotspots. Here, we examine the …

The intertropical convergence zone (ITCZ) plays a key role in regulating tropical
hydroclimate and global water cycle through changes in its convection strength, latitudinal …

Abstract Reconstructing the Plio-Pleistocene sedimentary history of the Yellow Sea, is
important for understanding the long-term influence of the Yellow River (Huanghe) and/or …

Abstract The Vietnamese Mekong Delta was formed by rapid transgression during the
second half of the Holocene by deposition of mainly unconsolidated, fine-grained (clayey) …

Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …

Peatlands have been recognised as globally important carbon sinks over long timescales
that produced a global, net-climatic cooling effect over the Holocene. However, little is …