Climate-driven long-term development of North Atlantic cold-water coral ecosystems - growth and migration patterns on a trans-Atlantic perspective

气候驱动的北大西洋冷水珊瑚生态系统的长期发展——跨大西洋视角的生长和迁徙模式

• 批准号: 211131939
• 负责人: Professor Dr. Dierk Hebbeln
• 金额: --
• 依托单位: Zentrum für Marine Umweltwissenschaften (MARUM)
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2012
• 资助国家: 德国
• 起止时间: 2011-12-31 至 2015-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/211131939?language=en
• 关键词: Climate; driven; long; term; development

Cold‐water corals (CWCs) along the NE Atlantic margin show a temporally and spatially structured occurrence over the last glacial‐interglacial cycle that indicates a close coupling between these ecosystems and climate (i.e. environmental) change. Off NW Africa corals have been widespread during the last glacial and largely demised at the end of this cold period. In contrast, corals off northern Europe started to develop to the most vivid CWC sites worldwide during the recent interglacial. This pattern points to a climate induced northward shift of areas with optimum coral growth conditions with the onset of the Holocene likely caused by dramatic environmental changes that occurred during this time in the North Atlantic realm. However, the main factors controlling the prosperity and demise of CWCs are only partly understood. Moreover, a potential connectivity between the NE and NW Atlantic coral occurrences has not been considered so far, which is mainly attributed to a lack of appropriate data from NW Atlantic coral sites. Therefore, the proposed project will be based on sample material to be collected from CWC sites along the NW Atlantic margin during a cruise with RV MARIA S. MERIAN in spring 2012 and will be correlated with existing data already obtained for the NE Atlantic. The overall aim is to study the development of CWC ecosystems under changing environmental conditions during the last glacial‐interglacial cycle on a trans‐Atlantic perspective and to identify the underlying controlling factors.

大西洋东北部边缘的冷水珊瑚（CWC）在最后一个冰期-间冰期循环中表现出时间和空间结构，表明这些生态系统与气候（即环境）变化之间存在密切联系。非洲西北部附近的珊瑚在末次冰期期间广泛分布，并在寒冷时期结束时大部分死亡。相比之下，北欧附近的珊瑚在最近的间冰期开始发展成为世界上最生动的 CWC 地点。这种模式表明，随着全新世的开始，气候导致具有最佳珊瑚生长条件的地区向北移动，这可能是由于北大西洋地区在此期间发生的巨大环境变化造成的。然而，人们对控制化学武器的繁荣和消亡的主要因素知之甚少。此外，到目前为止，尚未考虑东北大西洋珊瑚礁和西北大西洋珊瑚礁之间的潜在连通性，这主要是由于缺乏来自西北大西洋珊瑚地点的适当数据。因此，拟议项目将基于 2012 年春季 RV MARIA S. MERIAN 巡航期间从西北大西洋边缘 CWC 站点收集的样本材料，并将与已获得的东北大西洋现有数据相关联。总体目标是从跨大西洋的角度研究末次冰期-间冰期循环期间不断变化的环境条件下 CWC 生态系统的发展，并确定潜在的控制因素。

项目成果

Scale worms (Polychaeta: Aphroditiformia) associated with cold-water corals in the eastern Gulf of Mexico

• DOI: 10.1017/s002531541300088x
• 发表时间: 2013-12-01
• 期刊: JOURNAL OF THE MARINE BIOLOGICAL ASSOCIATION OF THE UNITED KINGDOM
• 影响因子: 1.2
• 作者: Barnich, Ruth;Beuck, Lydia;Freiwald, Andre
• 通讯作者: Freiwald, Andre

Global ocean conveyor lowers extinction risk in the deep sea

全球海洋输送机降低深海灭绝风险

• DOI: 10.1016/j.dsr.2014.03.004
• 发表时间: 2014
• 作者: Henry LA;Frank N;Hebbeln D;Wienberg C;Robinson L;van de Flierdt T;Dahl M;Douarin M;Morrison CL;Correa ML;Rogers AD;Ruckelshausen M;Roberts JM
• 通讯作者: Roberts JM

Interglacial occurrence of cold-water corals off Cape Lookout (NW Atlantic): First evidence of the Gulf Stream influence

卢考特角（大西洋西北部）冷水珊瑚的间冰期现象：墨西哥湾流影响的第一个证据

• DOI: 10.1016/j.dsr.2015.09.003
• 发表时间: 2015
• 作者: Matos L;Mienis F;Wienberg C;Frank N;Kwiatkowski C;Groeneveld J;Thil F;Abrantes F;Cunha M;Hebbeln D
• 通讯作者: Hebbeln D

Framework-Forming Scleractinian Cold-Water Corals Through Space and Time: A Late Quaternary North Atlantic Perspective

穿越时空形成框架的石珊瑚冷水珊瑚：晚第四纪北大西洋视角

• DOI: 10.1007/978-3-319-17001-5_16-1
• 发表时间: 2016
• 作者: Wienberg C;Titschack J
• 通讯作者: Titschack J