Biomarker analysis revealed tidal organic carbon input enhanced soil respiration and weakened carbon sequestration function of estuarine wetland: Field validation of the Jiuduansha Wetland in the Yangtze River estuary

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE Geoderma Pub Date : 2024-12-05 DOI:10.1016/j.geoderma.2024.117134
Haoyu Dong, Liwei Qian, Jianfang Yan, Lianying Gao, Xiaohua Fu, Lei Wang
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Abstract

In estuarine wetlands, tidal water is an important source of organic carbon input besides plants. However, it remains unclear whether tidal organic carbon input can affect soil organic carbon turnover processes in estuarine wetlands, especially soil respiration (SR) and carbon output. N-alkanes and lignin can be used as biomarker compounds to reflect the input and retention of organic carbon from tidal and plant sources. In the experiment, the contents of n-alkanes and lignin in tidal water, soil and plant samples were measured from upstream to downstream in Jiuduansha Wetland in the Yangtze River Estuary to compare the input intensity and retention capacity of tidal organic carbon with plant organic carbon in soils, and try to verify whether exogenous tidal organic carbon input enhanced SR and weakened carbon sequestration function. N-alkanes analysis revealed tidal organic carbon input gradually reduced from upstream to downstream of Jiuduansha wetland, and its degradability also reduced, which is an important reason for higher SR in upstream wetland. Lignin analysis showed the plant organic carbon input decreased with decreasing elevation, however the retention ratio of plant organic carbon was the highest in low tidal flats which has a high tidal organic carbon input. These results indicated tidal organic carbon was more easily degraded to CO2 than plant organic carbon. N-alkanes analysis also indicated only 11.94%–13.76% of the tidal organic carbon originated from CO2 (phytoplankton organic carbon (OC)), therefore the tidal organic carbon input did not increase the wetland CO2 input significantly, but significantly increase SR and CO2 emission of the wetland, this will weaken carbon sequestration function of estuarine wetland. Therefore, future studies should explore strategies to balance carbon sequestration and tidal organic matter interception and purification functions of estuarine wetlands.
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生物标志物分析显示潮汐有机碳输入增强了河口湿地的土壤呼吸功能,减弱了其固碳功能——以长江口九段沙湿地为例
在河口湿地中,潮汐水是除植物外重要的有机碳输入来源。然而,潮汐有机碳输入是否会影响河口湿地土壤有机碳周转过程,尤其是土壤呼吸(SR)和碳输出,目前尚不清楚。正构烷烃和木质素可以作为生物标志物化合物来反映潮汐和植物来源的有机碳输入和保留。本实验通过对长江口九段沙湿地从上游到下游潮汐水、土壤和植物样品中正构烷烃和木质素含量的测定,比较土壤中潮汐有机碳与植物有机碳的输入强度和滞留能力,试图验证外源潮汐有机碳输入是否增强了SR而减弱了固碳功能。正构烷烃分析显示,九段沙湿地潮汐有机碳输入由上游向下游逐渐减少,其可降解性也随之降低,这是上游湿地SR较高的重要原因。木质素分析表明,植物有机碳输入随海拔的降低而减少,但低潮滩的植物有机碳滞留率最高,潮滩的有机碳输入较高。这些结果表明潮汐有机碳比植物有机碳更容易降解为CO2。正构烷烃分析还表明,潮产有机碳中仅有11.94% ~ 13.76%来源于CO2(浮游植物有机碳(OC)),因此潮产有机碳的输入并未显著增加湿地的CO2输入,反而显著增加了湿地的SR和CO2排放,这将削弱河口湿地的固碳功能。因此,未来的研究应探索河口湿地固碳与潮汐有机质截流净化功能之间的平衡策略。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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