Illinois State Geological Survey, Prairie Research Institute, University of Illinois at Urbana-Champaign, 615 E Peabody Drive, Champaign, IL, 61820, USA.
Program in Environmental Sciences, Northwestern University, 2145 Sheridan Road, Evanston, IL, 60208, USA.
Sci Rep. 2019 Mar 12;9(1):4204. doi: 10.1038/s41598-019-40855-5.
Shoreline erosion can transition freshwater coastal wetlands from carbon sinks to carbon sources. No studies have explored the impacts of coastal geomorphic processes on freshwater wetland carbon budgets. To do so, we modified a saltmarsh carbon budget model for application in freshwater coastal wetlands. We validated the model with data from a shoreline wetland in the Laurentian Great Lakes. The model generates the carbon budget by differencing carbon export and carbon storage. The inputs for carbon storage are the carbon inventory and maximum wetland age. Inputs for carbon export include erosion rates and overwash extent. The model demonstrates that the wetland examined in this study transitioned to a source of carbon during periods of erosion. In fact, the net carbon export between 2015 and 2018 was 10% of the wetland's original carbon stock. This study indicates that geomorphic change can dictate whether and how freshwater coastal wetlands serve as sources or sinks for terrestrial carbon, and that carbon stocks can fluctuate on a geologically rapid timescale. We recommend that such geomorphic processes be considered when developing carbon budgets for these marginal environments. Furthermore, the carbon budget model refined in this study can be used to prioritize wetlands in land management and conservation efforts.
海岸侵蚀可使淡水滨海湿地由碳汇转变为碳源。目前尚无研究探讨海岸地貌过程对淡水湿地碳收支的影响。为此,我们对盐沼碳预算模型进行了修正,以应用于淡水滨海湿地。我们使用大湖地区的一个滨海湿地的数据对模型进行了验证。该模型通过碳输出与碳储存的差值来生成碳预算。碳储存的输入是碳清单和最大湿地年龄。碳输出的输入包括侵蚀率和漫滩范围。该模型表明,在本研究中,所研究的湿地在侵蚀期间转变为碳源。实际上,2015 年至 2018 年间,净碳输出量为湿地原始碳储量的 10%。本研究表明,地貌变化可以决定淡水滨海湿地是否以及如何成为陆地碳的源或汇,并且碳储量可以在地质上快速波动。我们建议在为这些边缘环境制定碳预算时考虑这些地貌过程。此外,本研究中改进的碳预算模型可用于在土地管理和保护工作中优先考虑湿地。