Suppr超能文献

特大城市发展与沿海珊瑚群落消亡:珠江口珊瑚骨骼 δ N 记录的证据。

Megacity development and the demise of coastal coral communities: Evidence from coral skeleton δ N records in the Pearl River estuary.

机构信息

Max Planck Institute for Chemistry, Otto Hahn Institute, Mainz, Germany.

The Swire Institute of Marine Science, The University of Hong Kong, Shek O, HKSAR.

出版信息

Glob Chang Biol. 2020 Mar;26(3):1338-1353. doi: 10.1111/gcb.14923. Epub 2020 Jan 16.

Abstract

Historical coral skeleton (CS) δ O and δ N records were produced from samples recovered from sedimentary deposits, held in natural history museum collections, and cored into modern coral heads. These records were used to assess the influence of global warming and regional eutrophication, respectively, on the decline of coastal coral communities following the development of the Pearl River Delta (PRD) megacity, China. We find that, until 2007, ocean warming was not a major threat to coral communities in the Pearl River estuary; instead, nitrogen (N) inputs dominated impacts. The high but stable CS-δ N values (9‰-12‰ vs. air) observed from the mid-Holocene until 1980 indicate that soil and stream denitrification reduced and modulated the hydrologic inputs of N, blunting the rise in coastal N sources during the early phase of the Pearl River estuary urbanization. However, an unprecedented CS-δ N peak was observed from 1987 to 1993 (>13‰ vs. air), concomitant to an increase of NH concentration, consistent with the rapid Pearl River estuary urbanization as the main cause for this eutrophication event. We suggest that widespread discharge of domestic sewage entered directly into the estuary, preventing removal by natural denitrification hotspots. We argue that this event caused the dramatic decline of the Pearl River estuary coral communities reported from 1980 to 2000. Subsequently, the coral record shows that the implementation of improved wastewater management policies succeeded in bringing down both CS-δ N and NH concentrations in the early 2000s. This study points to the potential importance of eutrophication over ocean warming in coral decline along urbanized coastlines and in particular in the vicinity of megacities.

摘要

历史珊瑚骨骼(CS)的δ O 和 δ N 记录是从沉积沉积物中回收的样本中产生的,这些样本保存在自然历史博物馆的收藏品中,并被钻成现代珊瑚头。这些记录被用来评估全球变暖与区域富营养化对中国珠江三角洲(PRD)特大城市发展后沿海珊瑚群落衰退的影响。我们发现,直到 2007 年,海洋变暖并不是珠江河口珊瑚群落的主要威胁;相反,氮(N)输入是主要的影响因素。从中全新世到 1980 年,CS-δ N 值(9‰-12‰与大气相比)一直很高且稳定,这表明土壤和溪流的反硝化作用减少并调节了 N 的水文输入,从而削弱了珠江河口城市化早期沿海 N 源的增加。然而,从 1987 年到 1993 年,CS-δ N 观测值出现了前所未有的峰值(高于大气的 13‰),同时 NH4+浓度增加,与珠江河口城市化的快速发展相一致,这是富营养化事件的主要原因。我们认为,大量的生活污水直接排入河口,阻止了自然反硝化热点对其的去除。我们认为,这一事件导致了从 1980 年到 2000 年珠江河口珊瑚群落的急剧减少。随后,珊瑚记录显示,21 世纪初,实施了改善的废水管理政策,成功地降低了 CS-δ N 和 NH4+浓度。本研究表明,在城市化沿海地区,特别是在特大城市附近,富营养化对珊瑚减少的潜在重要性超过海洋变暖。

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验