Abstract Knowledge of peatland dynamics and its response to the intensity of the Indian
summer monsoon (ISM) is crucial to predict the future fate of the peatlands in the …

Central China has experienced stronger summer monsoon during warm periods such as
Marine Isotope Stages (MIS) 1 and 3, and weaker summer monsoon during cool periods …

Knowledge of the hydroclimatic changes in Southwest China since the Last Glacial
Maximum (LGM) is crucial for disentangling the long-term evolution of the Asia Monsoon …

Climate change in the Holocene is closely related to the development of mash peat. Study
the initiation of peatland and its relative climatic controls will provide a better understanding …

Peatlands are one of the optimal archives for paleoclimate research and their records
contain a detailed history of climatic and environmental variations during their formation …

The Dajiuhu mire deposit is a sensitive archive of palaeoenvironmental evolution in the East
Asian monsoon region. The aim of this study of the elemental geochemistry of a sediment …

Peatland development is closely correlated with regional environment and climate changes.
In this study, two sediment cores covering the past 13.8 cal kyr BP were collected from Hani …

Peatland of the eastern Qinghai–Tibetan Plateau lies at the convergence of the East Asian
and Indian monsoon systems in eastern Asia. To understand the evolution of this peatland …

The Sanjiang Plain (SJP) wetland is the largest freshwater marshland in China. Peatlands
were initiated early and are widely distributed across the SJP and form a large carbon (C) …

Throughout northeast China, the widely distributed peatlands have formed a large carbon
(C) pool. However, the relationship between peatland initiation and climate controls is still …