Geological Perspectives on the Degradation and Restoration of Coral Reefs

L. Toth
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Abstract

The growth and maintenance of coral-reef structures built over 1000s of years serve as the foundation for the myriad ecosystem services reefs provide to society. Predicting how reef building will change in the future is, therefore, critical to designing effective coral-reef management strategies; however, it is challenging to accurately forecast the long-term process of reef accretion based on short-term ecological studies alone. Geological records, particularly those from sensitive, marginal reef environments such as the subtropical reef system of south Florida, are essential for projecting changes in reef accretion, and for optimizing strategies for coral-reef management. Using a combination of millennial-scale reconstructions of reef accretion and paleoecology from reef cores, and contemporary carbonate budget modeling, I evaluated the past, present, and a possible future of coral-reef development in south Florida. I will show that climate has been the primary control on the rate and extent of regional reef development and, by 3000 years ago, reef accretion was negligible throughout the region. This confined the ecosystem to an unstable equilibrium in which a veneer of living coral was the only barrier to catastrophic reef erosion. In recent decades, climate and other anthropogenic disturbances have pushed many reefs into a novel state characterized by a loss of reef-building corals that is unprecedented in the geological record. These changes have unbalanced Florida’s carbonate budgets, leading to increases in reef-framework erosion. I will show that there is hope for ongoing coral restoration efforts to revive reef growth on a local scale to levels comparable to long-term natural baselines; however, the central role of climate in both the millennial-scale declines in reef building and the modern decline in coral populations suggests that the efficacy of these local efforts will be limited without global-scale action to mitigate anthropogenic climate change.
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珊瑚礁退化与恢复的地质学观点
千百年来建造的珊瑚礁结构的生长和维护是珊瑚礁为社会提供无数生态系统服务的基础。因此,预测未来珊瑚礁建设将如何变化,对于设计有效的珊瑚礁管理策略至关重要;然而,仅凭短期生态学研究,难以准确预测珊瑚礁增生的长期过程。地质记录,特别是那些来自敏感的边缘珊瑚礁环境的记录,如南佛罗里达的亚热带珊瑚礁系统,对于预测珊瑚礁增生的变化和优化珊瑚礁管理策略是必不可少的。通过结合珊瑚礁岩心的千年尺度的珊瑚礁增生和古生态重建,以及当代碳酸盐收支模型,我评估了佛罗里达南部珊瑚礁发展的过去、现在和可能的未来。我将说明,气候一直是区域珊瑚礁发育速度和程度的主要控制因素,到3000年前,整个地区的珊瑚礁增生可以忽略不计。这将生态系统限制在不稳定的平衡状态,在这种平衡状态下,活珊瑚的表面是防止灾难性珊瑚礁侵蚀的唯一屏障。近几十年来,气候和其他人为干扰使许多珊瑚礁进入了一种新的状态,其特征是造礁珊瑚的消失,这在地质记录中是前所未有的。这些变化使佛罗里达的碳酸盐收支不平衡,导致珊瑚礁框架侵蚀增加。我将表明,正在进行的珊瑚恢复工作有希望在局部范围内将珊瑚礁的生长恢复到与长期自然基线相当的水平;然而,气候在千年尺度的珊瑚礁建设减少和现代珊瑚种群减少中所起的核心作用表明,如果没有全球尺度的行动来缓解人为气候变化,这些局部努力的效果将是有限的。
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