Coralline algae as recorders of environmental change

珊瑚藻作为环境变化的记录者

• 批准号: 341876-2012
• 负责人: Halfar, Jochen
• 金额: $ 3.35万
• 依托单位: University of Toronto
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2015
• 资助国家: 加拿大
• 起止时间: 2015-01-01 至 2016-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=572395
• 关键词: Coralline; algae; recorders; environmental; change

Quantifying the role and contribution of the world's oceans in past, present, and future global change is an essential goal in climate and paleoenvironmental studies. Although the global oceans influence climate greatly, the marine environment is substantially underrepresented in key climate assessment reports, especially during the last millennium. Over the past decades multicentury climate time series have emerged from tropical corals, and more recently from mid-latitude long-lived bivalves. However, subarctic and arctic proxy archival records are sparse. In order to fill this gap, a number of studies have demonstrated that mid- and high-latitude crustose coralline algae are an emerging extratropical marine environmental archive as they are amongst the longest lived shallow marine calcified organisms with life spans of several hundred years. More importantly, coralline algae occur in subarctic and arctic latitudes, both in the Pacific and Atlantic, where other high-resolution century-scale marine environmental proxies are non-existent. Hence, coralline algae have recently started to fill an important niche in marine paleoenvironmental proxy research, with several decadally to seasonally-resolved multicentury climate reconstructions published to date. This proposal will address two key themes to be answered using coralline proxy archives: A) Recently collected coralline algae from central and northern Labrador will be used to provide the first >500 year record of Labrador Current temperature and salinity variability and related climate oscillations in the northwestern Atlantic - a region where poorly understood climate and oceanographic changes have had a dramatic impact on ecosystems and fishery yields. B) Ongoing ocean acidification has been shown to potentially have a detrimental impact on the skeletons of calcareous plants and animals such as shellfish and corals. This is especially true in cold-water regions such as the subarctic North Pacific and northwest Atlantic, which are predicted to be amongst the first negatively affected by a decreasing ocean pH. Coralline algae from both oceans will be analyzed for temporal changes in skeletal structure and elemental composition, and as a proxy for reconstructing ocean pH over several centuries.

量化世界海洋在过去、现在和未来全球变化中的作用和贡献是气候和古环境研究的一个重要目标。虽然全球海洋对气候影响很大，但海洋环境在主要气候评估报告中的代表性严重不足，特别是在上一个千年期间。在过去的几十年里，多世纪的气候时间序列已经出现了热带珊瑚，最近从中纬度长寿的双壳类。然而，亚北极和北极代理档案记录稀少。为了填补这一空白，一些研究表明，中纬度和高纬度甲壳珊瑚藻是一种新兴的热带外海洋环境档案，因为它们是寿命最长的浅海钙化生物之一，寿命长达数百年。更重要的是，珊瑚藻出现在太平洋和大西洋的亚北极和北极纬度，在那里不存在其他高分辨率的世纪尺度海洋环境代用指标。因此，珊瑚藻最近开始填补海洋古环境代理研究的一个重要的利基，与几个十年到季节性解决的多世纪气候重建出版。这项建议将解决两个关键主题，以回答使用珊瑚代理档案：A）最近从拉布拉多中部和北方收集的珊瑚藻将用于提供拉布拉多海流温度和盐度变化以及西北大西洋相关气候振荡的第一个>500年记录-该区域对气候和海洋变化知之甚少，对生态系统和渔业产量产生了巨大影响。B）持续的海洋酸化已被证明可能对贝类和珊瑚等钙质植物和动物的骨骼产生有害影响。 这是尤其如此，在冷水区，如亚北极的北太平洋和西北大西洋，这是预计将首先受到海洋pH值下降的负面影响。珊瑚藻从两个海洋将分析骨骼结构和元素组成的时间变化，并作为代理重建海洋pH值超过几个世纪。