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一种用于推导沿海盐沼沉积速率的生态参数方法。

An eco-parametric method to derive sedimentation rates for coastal saltmarshes.

机构信息

Ministry of Education Key Laboratory of Coast and Island Development, Nanjing University, Nanjing 210023, China.

Ministry of Education Key Laboratory of Coast and Island Development, Nanjing University, Nanjing 210023, China; State Key laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China.

出版信息

Sci Total Environ. 2021 May 20;770:144756. doi: 10.1016/j.scitotenv.2020.144756. Epub 2021 Jan 4.

Abstract

The saltmarsh plant Spartina alterniflora was introduced to the Jiangsu coasts, China and serves as an ecological engineer to reduce near-bed shear stress, trap fine-grained sediments and protect the coast from wave-induced erosion. The saltmarshes thus could record the Spartina colonization-driven changes within the sedimentary layers. Based on these ecological and sedimentological changes in sediments, we present a new eco-parametric method to estimate the sedimentation rate for the newly-formed wetlands in the Yancheng Wetland Nature Reserve for Rare Birds, Jiangsu. Sediment cores and satellite imagery were used to identify the thickness of accumulated sediment layers and the time since the Spartina colonization. We defined the original ground on which Spartina alterniflora initially colonized using pigment concentrations, grain size and stable carbon isotopic compositions of organic matter (δC) in sediments. We also determined the time mark of the Spartina colonization by examining the Landsat images over 1982-2018 to discriminate the Spartina alterniflora from other native plants and geomorphological features. These two datasets yielded a sedimentation rate of 3.3 cm/yr for Core A and of 9.6 cm/yr for Core B, the latter evidenced by an increase of ~ 0.51 m in the bed level from 2008 to 2014. Combining the Pb dating method, we further estimated the sedimentation rate for the layers beneath the original ground, which was comparable to that of the bare flats in the Jiangsu coast. Even though this new method is only applicable to newly-formed saltmarshes, it helps identify the recent sedimentation events as well as reveal the environmental changes and the evolution of saltmarsh-bare flat systems due to the interplay between vegetation, hydrodynamics and sediment dynamics. It thus could be an efficient and cost-effective tool for an improved understanding of the response of coastal wetlands to a changing climate/environment.

摘要

互花米草是一种引入中国江苏海岸的盐沼植物,它作为一种生态工程师,可以降低近底剪切应力、捕获细颗粒沉积物并保护海岸免受波浪引起的侵蚀。因此,盐沼可以记录沉积物中互花米草殖民化驱动的变化。基于这些沉积物中的生态和沉积变化,我们提出了一种新的生态参数方法来估计江苏盐城珍禽自然保护区新形成湿地的沉积速率。利用沉积岩心和卫星图像来识别积累的沉积层的厚度以及互花米草殖民化的时间。我们使用沉积物中色素浓度、粒径和有机物质稳定碳同位素组成(δC)来定义互花米草最初殖民的原始地面。我们还通过检查 1982-2018 年的 Landsat 图像来确定互花米草殖民化的时间标记,以区分互花米草与其他本地植物和地貌特征。这两个数据集得出了 A 岩心的沉积速率为 3.3 cm/yr,B 岩心的沉积速率为 9.6 cm/yr,后者的证据是 2008 年至 2014 年床面高程增加了约 0.51 m。结合 Pb 测年法,我们进一步估算了原始地面以下层的沉积速率,与江苏海岸的裸地相当。尽管这种新方法仅适用于新形成的盐沼,但它有助于识别最近的沉积事件,并揭示由于植被、水动力和沉积动力之间的相互作用,盐沼-裸地系统的环境变化和演化。因此,它可以成为一种有效且具有成本效益的工具,用于更好地了解沿海湿地对气候变化/环境变化的响应。

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