Water table is one of the key factors that controlling the peatland initiation and development,
and therefore has attracted a lot of attentions in the field of peatland paleoenvironment …

Testate amoebae are a group of single-celled protists found in abundance on the surface of
peatlands and form a well-preserved shell (test) in Holocene peats. They have been …

In this study, three typical peat cores were collected from Tuqiang (TQ) of Great Hinggan
Mountain, Youhao (YH) of Small Hinggan Mountain and Honghe (HH) of Sanjiang Plain …

Testate amoebae are sensitive indicators of substrate moisture in peatlands. Over the last
decades, they have been studied to reconstruct hydrological changes since the Holocene …

Reconstructing historical hydrologic and vegetation conditions can provide useful insights
into the mechanisms underlying peatland development and can be used to construct …

Diatom-inferred changes in past water levels and the evolution of peatlands during the
Holocene period are investigated in the Honghe National Natural Reserve (HNNR), which is …

Natural radionuclide 210 Pb, soil water content, and dry bulk density data were used to
calculate the geochronology and characterize the recent peat sedimentation rate of a soil …

Testate amoebae are a diverse and abundant group of protozoa that constitute a large
proportion of biomass in many ecosystems and probably fill important roles in ecosystem …

Testate amoebae (TA) community composition records from peat cores are often used to
infer past water-table conditions on peatland sites. However, one of the problems is that …

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 …