2014
DOI: 10.1016/j.earscirev.2013.11.003
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Peatland initiation and carbon accumulation in China over the last 50,000years

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Cited by 77 publications
(55 citation statements)
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“…Similarly, the peak peatland initiation and peat C sequestration occurred at the Holocene Thermal Maximum (HTM) period in Zoige (Fig. 6), in line with the previous study (Sun et al, 1998;Wang et al, 2014;Zhao et al, 2014). Also, a study indicated that warming in recent decades increased the height, coverage and corresponding aboveground biomass of vegetation on the QTP (Zhou et al, 2000).…”
supporting
confidence: 75%
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“…Similarly, the peak peatland initiation and peat C sequestration occurred at the Holocene Thermal Maximum (HTM) period in Zoige (Fig. 6), in line with the previous study (Sun et al, 1998;Wang et al, 2014;Zhao et al, 2014). Also, a study indicated that warming in recent decades increased the height, coverage and corresponding aboveground biomass of vegetation on the QTP (Zhou et al, 2000).…”
supporting
confidence: 75%
“…Hitherto, many studies have focused on the long-term C sequestration of peatlands on the Zoige Plateau, the Northeast part of QTP (Sun et al, 2001;Zhao et al, 2011;Zhou et al, 2011). Very recently, some authors even have tried to identify the controlling factors for C accumulation dynamics during the Holocene Zhao et al, 2014). However, limited attention has been paid to the carbon fate of modern peats.…”
Section: Introductionmentioning
confidence: 99%
“…They also tried to identify the influencing factors for peat accumulation (Large et al, 2009;Gao et al, 2010;Zhou et al, 2010). Very recently, a synthesis effort by Zhao et al (2014) did well in providing a systematic knowledge of climate controls of peat expansion in the last 50 ka, the peat C accumulation rates based on only six peat cores, however, could not represent the C accumulation dynamic patterns on either regional or national scale. Therefore, we still lack a fundamental and comprehensive understanding of peat C accumulation and its climate controls in different regions of China.…”
Section: Introductionmentioning
confidence: 99%
“…According to lake sediment records and peat-based records, wetlands in the QTP started to form in the last deglaciation and the early Holocene, and expand quickly in the early and middle Holocene which corresponds to the higher and increasing insolation and stronger Asian summer monsoon (Zhao et al, 2011(Zhao et al, , 2014Xu et al, 2013). In the QTP, suitable combination of climate (temperature and precipitation) and local topography is critical for the distribution of wetlands.…”
Section: Factors Affecting Alpine Wetlands Distribution and Shiftmentioning
confidence: 99%