Drivers and Patterns of Sediment Organic Carbon in European Regional Seas

IF 6.9 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Christian Lønborg, Anna Elizabeth Løvgren Graversen, Anna Maria Addamo, Jorge Assis, Michael Timothy Burrows, Eleanor Stewart, Helen Lillis, Mark John Costello, Dorte Krause-Jensen
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Abstract

Mapping organic carbon (OC) stores in marine sediments is a management priority to potentially minimize the anthropogenic release of organic carbon from the seabed. Sediment OC content shows high regional variability, shaped by a complex interplay of physical, chemical, biological and anthropogenic factors. In this study, we present an assessment of the drivers and patterns of sediment OC across European regional seas, with a particular focus on the role of large-scale habitats, substratum characteristics, and environmental conditions. To investigate these relationships, we integrated data sets encompassing sediment OC, benthic habitats, sediment substrata and 11 environmental variables. Applying machine learning techniques, we identified wave exposure (estimated from wave fetch), light availability, seafloor geomorphic features, and maximum bottom water temperature as the most important environmental predictors of sediment OC content across European regional seas. While the model captured broad spatial patterns in sediment OC, it did not resolve local scale variability, making it better suited for regional assessments than for site-specific predictions. Overall, the highest OC contents were found in sediments underlying vegetated habitats such as Posidonia oceanica and other seagrass meadows as well as in mud, and mixed sediment substrata. OC hotspots were generally located in inshore areas with low wave fetch and temperature; these include areas of the Baltic Sea, North Sea, Adriatic Sea, Barents Sea, and the Black Sea. Our data-driven approach provides a robust foundation for identifying OC-rich sediments, which are critical for conservation planning and assessing anthropogenic impacts on marine OC.

欧洲区域海洋沉积物有机碳驱动因素与模式
绘制海洋沉积物中有机碳(OC)储量是一项管理重点,可以最大限度地减少海底人为释放的有机碳。沉积物OC含量表现出高度的区域变异性,受物理、化学、生物和人为因素的复杂相互作用影响。在这项研究中,我们对欧洲区域海洋沉积物OC的驱动因素和模式进行了评估,特别关注了大尺度栖息地、基质特征和环境条件的作用。为了研究这些关系,我们整合了包含沉积物OC、底栖生物栖息地、沉积物基质和11个环境变量的数据集。应用机器学习技术,我们确定了波浪暴露(从波浪获取估计),光可用性,海底地貌特征和最高底水温作为欧洲区域海洋沉积物OC含量最重要的环境预测因子。虽然该模型捕获了沉积物OC的广泛空间格局,但它并没有解决局部尺度的变化,这使得它更适合于区域评估,而不是特定地点的预测。总体而言,有机碳含量最高的是植被生境下的沉积物,如Posidonia oceanica和其他海草草甸,以及泥浆和混合沉积物基质。高温热点一般位于低浪高和低温度的近岸地区;这些地区包括波罗的海、北海、亚得里亚海、巴伦支海和黑海。我们的数据驱动方法为识别富含OC的沉积物提供了坚实的基础,这对保护规划和评估海洋OC的人为影响至关重要。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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