Tracking the history of Baltic Sea hypoxia with bivalve shells

用双壳贝壳追踪波罗的海缺氧的历史

• 批准号: 406557478
• 负责人: Professor Dr. Bernd R. Schöne
• 金额: --
• 依托单位: Institut für Geowissenschaften
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2018
• 资助国家: 德国
• 起止时间: 2017-12-31 至 2022-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/406557478?language=en
• 关键词: Tracking; history; Baltic; Sea; hypoxia

Bottom hypoxia (less than 2 mg/L dissolved oxygen, DO) is a growing environmental problem in coastal and offshore waters. Severe and prolonged low-oxygen conditions can be lethal for bottom dwellers, destroy benthic communities, cause ecosystem disturbances and eventually form dead zones. The spatial distribution, intensity and duration of hypoxia in the Baltic Sea, home of the largest oxygen-deficient zone, has increased strikingly during the last century, both in shallow nearshore and deeper offshore settings. Due to lacking data, the occurrence of coastal hypoxia in time and space is much less well characterized than in deeper waters. Yet, the main unresolved question concerns the causes for the drastic expansion of hypoxia in the Baltic Sea: How important are physical forcings (stratification) and nutrient-driven eutrophication? A strong halocline preventing downward-mixing of oxygenated surface waters is controlled by climate and maintained by riverine freshwater influx and precipitation as well as saline inflows from the North Sea. Conversely, anthropogenic nutrient input has greatly stimulated primary production and oxygen consumption by decomposing organic matter. To obtain a mechanistic understanding of these complex processes requires long, high-resolution records. Such data are currently not available. In fact, long-term monitoring data sets of DO levels are lacking, and knowledge of the history of Baltic Sea hypoxia (prior to the instrumental era) relies almost exclusively on proxies archived in laminated sediments. While the latter can provide unique insights into long-term DO trends of, they come with poor temporal resolution, are not available from shallow settings and do not permit to quantify DO levels.The main objective of the planned project is to establish a virtually untapped archive for hypoxia and eutrophic state, namely shells of long-lived bivalves. We will develop a multiproxy approach for the reconstruction of DO (Mn/Ca, Fe/Ca, I/Ca, delta34S) and apply this technique to infer the Late Holocene history of hypoxia in selected regions of the Baltic Sea with unprecedented temporal resolution. For this purpose, shells of live-collected and subfossil specimens of two long-lived bivalve species will be used, namely Arctica islandica and Astarte borealis. Master chronologies will be constructed that provide uninterrupted seasonally to inter-annually resolved information on DO levels during the last 200 years or so. In addition, radiocarbon (AMS) dated subfossil shells will be used to open windows into environmental/climate baseline conditions. In order to disentangle the relative importance of physical forcings and anthropogenic eutrophication on the drastic expansion of the hypoxic zone in recent decades, we will also develop and apply proxies for the eutrophic state (delta15N, P/Ca). Results of the planned study can be transferred to other oceanic settings and will thus significantly advance marine ecology research.

海底缺氧(DO<2 mg/L)是近海和近海日益严重的环境问题。严重和长期的低氧条件可能会对海底生物造成致命影响，破坏海底群落，造成生态系统紊乱，并最终形成死区。波罗的海是最大的缺氧区，波罗的海的缺氧空间分布、强度和持续时间在上个世纪显著增加，无论是在浅海近岸还是更深的近海环境中都是如此。由于缺乏数据，沿海缺氧的发生在时间和空间上的特征远远比不上更深的水域。然而，主要悬而未决的问题涉及波罗的海缺氧急剧扩大的原因：物理强迫(分层)和营养驱动的富营养化有多重要？防止含氧地表水向下混合的强烈盐跃层受气候控制，并由河流淡水流入和降水以及来自北海的盐水流入维持。相反，人为的养分输入通过分解有机物，极大地刺激了初级生产力和氧气消耗。要从机制上理解这些复杂的过程，需要长时间、高分辨率的记录。目前还没有这样的数据。事实上，缺乏溶解氧水平的长期监测数据集，对波罗的海缺氧历史(在仪器时代之前)的了解几乎完全依赖于层状沉积物中存档的替代物。虽然后者可以提供对DO的长期趋势的独特见解，但它们具有较低的时间分辨率，无法从浅层环境中获得，也不允许量化DO水平。计划项目的主要目标是建立一个几乎未开发的缺氧和富营养状态档案，即长期生存的双壳类贝壳。我们将开发一种重建DO(Mn/Ca，Fe/Ca，I/Ca，delta34S)的多代理方法，并应用该技术以前所未有的时间分辨率推断波罗的海部分地区晚全新世的缺氧史。为此，将使用两个长寿双壳类物种的活体采集和亚化石标本的贝壳，即Arctica Island andica和Astarte borealis。将构建主年表，不间断地提供过去200年左右DO水平的季节性到年际解析信息。此外，放射性碳(AMS)亚化石贝壳将被用来打开了解环境/气候基线条件的窗户。为了弄清物理作用力和人为富营养化在近几十年来缺氧带急剧扩张中的相对重要性，我们还将开发和应用富营养化状态的替代指标(Delta15N，P/Ca)。计划中的研究成果可以转移到其他海洋环境中，从而大大促进海洋生态研究。