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A 95-cm subalpine peat core from the Daping Swamp, located in the transition zone between the middle and southern subtropical regions of China, provides an environmental mineral magnetism record over the past ~ 3000 years. Magnetic concentration-dependent parameters [i.e. magnetic susceptibility (χlf), anhysteretic susceptibility (χARM), and saturation isothermal remanent magnetization (SIRM)] and...
A 95-cm-thick peat sequence obtained from Daping Swamp in the western Nanling Mountains provides evidence for climate variability in the past ~3,000 year. Multi-proxy records (including organic carbon isotopes, humification degree, organic matter content, and dry bulk density) revealed three intensified Asian summer monsoon (ASM) intervals (i.e.~2900–2700, 2500–1700 and 1000–600 cal. yr BP) and three...
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