Equipe Ecosystèmes Littoraux, FRES 3041/UMR CNRS SPE 6134, Université de Corse, Faculté des Sciences et Techniques, Campus Grimaldi BP 52, 20250 Corte, France; GIS Posidonie, Université de Corse, Faculté des Sciences et Techniques, Campus Grimaldi BP 52, 20250 Corte, France; Centro de Estudios Avanzados de Blanes, Consejo Superior de Investigaciones Científicas, 17300 Blanes, Girona, Spain.
Equipe Ecosystèmes Littoraux, FRES 3041/UMR CNRS SPE 6134, Université de Corse, Faculté des Sciences et Techniques, Campus Grimaldi BP 52, 20250 Corte, France; GIS Posidonie, Université de Corse, Faculté des Sciences et Techniques, Campus Grimaldi BP 52, 20250 Corte, France.
Sci Total Environ. 2022 Sep 10;838(Pt 1):155864. doi: 10.1016/j.scitotenv.2022.155864. Epub 2022 May 13.
In the last decades, the increasing necessity to reduce atmospheric carbon dioxide (CO) concentrations has intensified interest in quantifying the capacity of coastal ecosystems to sequester carbon, referred to commonly as 'Blue Carbon' (BC). Among coastal habitats, seagrass meadows are considered as natural carbon sinks due to their capacity to store large amounts of carbon in their sediments over long periods of time. However, the spatial heterogeneity of carbon stocks in seagrass sediments needs to be better understood to improve the accuracy of BC assessments, particularly where there is high environmental variability. In the Mediterranean, Posidonia oceanica (L.) Delile constitutes extensive meadows considered as long-term carbon sinks due to the development of an exceptional structure known as 'matte', reaching several meters in height, which can be preserved over millennia. In order to specify the role of P. oceanica meadows in climate change mitigation, an estimate of carbon stocks has been conducted along the eastern coast of Corsica (NW Mediterranean). The approach is mainly based on the biogeochemical analysis of 39 sediment cores. Organic carbon (C; 327 ± 150 t ha, mean ± SE) and inorganic carbon stocks (C; 245 ± 45 t ha) show a high variability related to water depth, matrix (sandy vs rocky substrate) or the depositional environment (coastal vs estuary). The isotopic signature (δC) revealed a substantial contribution of allochthonous inputs of organic matter (macroalgae and sestonic sources) mainly in estuarine environment and shallow areas. The carbon stocks in the first 250 cm of matte (average thickness) were estimated at 5.6-14.0 million t C (study site) and 14.6-36.9 million t C (Corsica), corresponding to 11.6-29.2 and 30.4-76.8 years of CO emissions from the population of Corsica.
在过去的几十年里,减少大气二氧化碳(CO)浓度的需求不断增加,这使得人们对量化沿海生态系统固碳能力(通常称为“蓝碳”(BC))产生了浓厚的兴趣。在沿海生境中,由于其在长时间内将大量碳储存在沉积物中的能力,海草草甸被认为是天然碳汇。然而,需要更好地了解海草草甸沉积物中碳储量的空间异质性,以提高 BC 评估的准确性,特别是在环境变化较大的情况下。在地中海,波西多尼亚海草(L.)Delile 构成了广泛的海草床,由于其发育了一种被称为“草皮”的特殊结构,被认为是长期碳汇,这种结构可达数米高,可以保存数千年。为了明确波西多尼亚海草草甸在减缓气候变化中的作用,对科西嘉岛(西北地中海)东海岸的碳储量进行了估算。该方法主要基于对 39 个沉积物岩芯的生物地球化学分析。有机碳(C;327±150 t ha,平均值±SE)和无机碳储量(C;245±45 t ha)与水深、基质(沙质与基岩)或沉积环境(沿海与河口)高度相关,表现出很大的变异性。稳定同位素(δC)表明,有机物质(大型藻类和悬浮物质)的异源输入有很大贡献,主要存在于河口环境和浅水区。草皮(平均厚度)前 250 厘米的碳储量估计为 560-1400 万 t C(研究地点)和 1460-3690 万 t C(科西嘉岛),相当于科西嘉岛人口每年排放的 CO 56-292 年和 304-768 年。