2018
DOI: 10.1016/j.chemgeo.2018.08.012
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The remineralization of sedimentary organic carbon in different sedimentary regimes of the Yellow and East China Seas

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Cited by 68 publications
(61 citation statements)
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“…Statistical analyses show that the annual average DO concentration decreased as the nitrate concentration increased, whereas the AOU increased as the nitrate concentration increased (Figure 8), further reflecting the role of enhanced nutrient availability in the decreases in bottom DO concentration in the NYS. Furthermore, as reported by previous studies (Hu, 1984;Zhao, 1996), the NYSCWM is characterized by a cyclonic eddy in summer. Due to the convergence of the cold cyclonic eddy, the terrigenous and marinederived particulate organic matter can gradually aggregate and settle down, forming the central mud deposits (Figure 1b) within the NYSCWM (Cheng et al, 2004;Hu, 1984;Hu et al, 2011Hu et al, , 2013.…”
Section: Journal Of Geophysical Research: Oceanssupporting
confidence: 78%
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“…Statistical analyses show that the annual average DO concentration decreased as the nitrate concentration increased, whereas the AOU increased as the nitrate concentration increased (Figure 8), further reflecting the role of enhanced nutrient availability in the decreases in bottom DO concentration in the NYS. Furthermore, as reported by previous studies (Hu, 1984;Zhao, 1996), the NYSCWM is characterized by a cyclonic eddy in summer. Due to the convergence of the cold cyclonic eddy, the terrigenous and marinederived particulate organic matter can gradually aggregate and settle down, forming the central mud deposits (Figure 1b) within the NYSCWM (Cheng et al, 2004;Hu, 1984;Hu et al, 2011Hu et al, , 2013.…”
Section: Journal Of Geophysical Research: Oceanssupporting
confidence: 78%
“…This mud area also corresponds to the bottom high‐AOU and low‐DO saturation zone in the NYSCWM, suggesting that the accumulation of organic matter and remineralization in this region can be conducive to the drawdown of DO concentration in summer. Actually, the terrestrially derived particulate organic carbon (POC) accounts for a small fraction (~3%) of the sedimentary organic carbon in the YS muddy areas (Tao et al, ; Zhao et al, ). Moreover, these inputs of POC, mainly from the Yellow River, were pre‐aged and thus contributed a more decay‐resistant component to the POC in the YS (Bao et al, ; Tao et al, , ; Wang et al, ; Xue et al, ; Zhao et al, ); over the past decades, due to the decrease in the total suspended solids load, POC flux form of the Yellow River has also decreased by 90% (Ran et al, ).…”
Section: Discussionmentioning
confidence: 99%
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