Diatom evidence for late Holocene environmental change in a permafrost peatland in the northern Greater Khingan Mountains, Northeast China
High-latitude permafrost peatlands are sensitive to global warming, and understanding their
paleohydrological evolution is critical for assessing future hydrological and environmental …
paleohydrological evolution is critical for assessing future hydrological and environmental …
Effects of climate change on a subtropical montane peatland over the last two centuries: Evidence from diatom records
Climate variability can induce rapid changes in peatland ecosystems, affecting both carbon
cycling and vegetation succession. Diatoms are an important group of ubiquitous and …
cycling and vegetation succession. Diatoms are an important group of ubiquitous and …
Late-Holocene ecosystem dynamics and climate sensitivity of a permafrost peatland in Northeast China
Northern peatlands play an important role in the global carbon cycle. Here we use multi-core
and multi-proxy records from a peatland near Darbin Lake in the Arxan region of Northeast …
and multi-proxy records from a peatland near Darbin Lake in the Arxan region of Northeast …
Evidence of Holocene water level changes inferred from diatoms and the evolution of the Honghe Peatland on the Sanjiang Plain of Northeast China
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 …
Holocene period are investigated in the Honghe National Natural Reserve (HNNR), which is …
Diatom evidence for mid-Holocene peatland water-table variations and their possible link to solar forcing
Peatlands located at the northern edge of the East Asian monsoon (EAM) are well placed to
provide a terrestrial record of past climate and hydrological changes for this globally …
provide a terrestrial record of past climate and hydrological changes for this globally …
Peat development in the Napahai wetland and its response to variations in the intensity of the Indian summer monsoon, southwestern China, since the last …
B Liu, E Sheng, J Lan, K Yu - Palaeogeography, Palaeoclimatology …, 2022 - Elsevier
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 …
summer monsoon (ISM) is crucial to predict the future fate of the peatlands in the …
The persistent lake level decreasing induced Phragmites peatland development in the Bosten Lake (Northwest China) during the Medieval Warm Period
Y Dong, H Li, H He, S Wang - Quaternary International, 2022 - Elsevier
Abstract Northwest China (NW China) falls within Arid Central Asia (ACA) and has a climate
dominated by westerly winds, a fragile ecosystem, and a high sensitivity to climate change …
dominated by westerly winds, a fragile ecosystem, and a high sensitivity to climate change …
Holocene paleohydrological reconstruction and carbon accumulation of a permafrost peatland using testate amoeba and macrofossil analyses, Kuujjuarapik …
A Lamarre, M Garneau, H Asnong - Review of Palaeobotany and …, 2012 - Elsevier
Testate amoeba analyses were realized to reconstruct Holocene hydroclimatic variations
and carbon accumulation from two peat cores collected in a permafrost peatland located at …
and carbon accumulation from two peat cores collected in a permafrost peatland located at …
A 4000-yr multi-proxy record of Holocene hydrology and vegetation from a peatland in the Sanjiang Plain, Northeast China
Reconstructing historical hydrologic and vegetation conditions can provide useful insights
into the mechanisms underlying peatland development and can be used to construct …
into the mechanisms underlying peatland development and can be used to construct …
[HTML][HTML] Recent climate change has driven divergent hydrological shifts in high-latitude peatlands
High-latitude peatlands are changing rapidly in response to climate change, including
permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century …
permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century …
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