Wetlands rich in carbon are important ecosystems for storing organic carbon, with their
carbon storage capacity closely linked to water levels. Therefore, it is valuable to explore the …

The history and drivers of hydroclimate changes during the last deglaciation in Northeast
China remain contentious. We present a high-resolution record of vegetation and climate …

Understanding the factors behind past vegetation changes is instructive to anticipate how
vegetation will react to future climate change and human activities. The factors that …

Reconstructing the Holocene megaflood history is a key component of understanding the
mechanism of past climate change and assessing the potential impact of future catastrophic …

In the subtropical monsoon region of China, the climate differs from that of most northern
peatlands, where many peatlands have developed in mountainous areas. However, it …

The C 3 plant leaf wax δ 13 C (δ 13 C alk) is commonly used to reconstruct past climates.
However, our understanding of how precipitation and temperature influence terrestrial C 3 δ …

Peatlands are one of the largest natural terrestrial carbon store, which evolve closely with
the hydrological functioning. Evapotranspiration serves as a nexus of the carbon and water …

Sphagnum, a crucial peat-forming plant, is essential for sustaining the ecosystem and
counteracting climate change. In recent years, attempts have been made to cultivate …

Abstracts Sediments deposited on the continental shelf are indicative of paleo sea-level and
terrestrial-marine interaction. A reliable chronology of the continental shelf sediments is …

Paleoclimate records in central China reveal asynchronous hydroclimate changes to those
from both northern and southern China during the Holocene. Whether such a spatial mode …