EcoPast (GI-1553), Facultade de Bioloxía, Universidade de Santiago de Compostela, Campus Sur s/n, Santiago de Compostela 15782, Spain; Group of Aquatic Macrophytes Ecology, Centre d'Estudis Avançats de Blanes (CEAB-CSIC), 17300 Blanes, Girona, Spain.
Group of Aquatic Macrophytes Ecology, Centre d'Estudis Avançats de Blanes (CEAB-CSIC), 17300 Blanes, Girona, Spain.
Sci Total Environ. 2021 May 10;768:144352. doi: 10.1016/j.scitotenv.2020.144352. Epub 2020 Dec 29.
Seagrasses are distributed all along the coast of the Mediterranean Sea being Posidonia oceanica and Cymodocea nodosa the most common species. They promote sedimentation, leading to the formation of well-structured soils. Over the last decade, a growing attention has been paid to their role as CO sinks in the form of organic carbon (C) and to their use as environmental archives. However, most of the knowledge about pedogenetic processes in these soils refer to the rhizosphere. This study aims to understand seagrass soils biogeochemistry in the rhizosphere and below, which in turn can help to understand their long term formation processes. Fifteen cores were strategically sampled along a 350 km stretch of the Southeast Iberian coast, and analyzed for elemental composition (XRF core-scanning), magnetic susceptibility, C content and gran size distribution. The cores were dated by Pb and C-AMS techniques to estimate soil accretion. Principal component analysis was used to explore the main geochemical processes linked to soil formation. The results showed that terrestrial runoff plays a key role in meadow soil composition. Furthermore, C accumulation did not follow any general depth trend in our soil records, suggesting that temporal variation in C inputs is an important factor in determining carbon depth distribution within the soil. We obtained evidence that the establishment of well-developed, stable C. nodosa meadows in the Mediterranean Sea may be promoted by adverse environmental conditions to P. oceanica settlement. Metal's behavior within the meadow deposit and their interaction with organic matter and carbonates is unclear. The results presented in this paper highlight the importance of the influence of land-based inputs in the characteristics of seagrass meadow deposits, highly determining their C content, as well as the need for further studies on metal behavior, to understand their full potential as environmental records.
沿地中海海岸分布着各种海草,最常见的物种是海洋波喜荡草和地中海真海枣。它们促进了沉积物的沉淀,形成了结构良好的土壤。在过去的十年中,人们越来越关注它们作为 CO 汇的作用,以有机碳 (C) 的形式存在,并将其用作环境档案。然而,关于这些土壤中成土过程的大部分知识都涉及根际。本研究旨在了解根际和根际以下海草土壤的生物地球化学,这反过来又有助于了解它们的长期形成过程。在伊比利亚东南海岸的 350 公里长的海岸线上,战略性地采集了 15 个岩芯进行元素组成(XRF 岩芯扫描)、磁化率、C 含量和粒度分布分析。通过 Pb 和 C-AMS 技术对岩芯进行定年来估计土壤堆积。主成分分析用于探索与土壤形成相关的主要地球化学过程。结果表明,陆地径流在草甸土壤组成中起着关键作用。此外,C 积累在我们的土壤记录中没有遵循任何一般的深度趋势,这表明 C 输入的时间变化是决定土壤中碳深度分布的一个重要因素。我们有证据表明,在地中海中建立发达、稳定的地中海真海枣草地可能是由不利的环境条件促进了海洋波喜荡草的定居。金属在草甸沉积物中的行为及其与有机物和碳酸盐的相互作用尚不清楚。本文的研究结果强调了陆地输入对海草草甸沉积物特征的影响的重要性,这极大地决定了它们的 C 含量,同时需要进一步研究金属的行为,以了解它们作为环境记录的全部潜力。