Department of Earth and Environmental Sciences, Macquarie University, Macquarie Park, NSW, Australia.
Department of Earth Sciences, University of Hong Kong, Hong Kong, China.
Science. 2020 Jun 5;368(6495):1118-1121. doi: 10.1126/science.aba2656.
The response of mangroves to high rates of relative sea level rise (RSLR) is poorly understood. We explore the limits of mangrove vertical accretion to sustained periods of RSLR in the final stages of deglaciation. The timing of initiation and rate of mangrove vertical accretion were compared with independently modeled rates of RSLR for 78 locations. Mangrove forests expanded between 9800 and 7500 years ago, vertically accreting thick sequences of organic sediments at a rate principally driven by the rate of RSLR, representing an important carbon sink. We found it very likely (>90% probability) that mangroves were unable to initiate sustained accretion when RSLR rates exceeded 6.1 millimeters per year. This threshold is likely to be surpassed on tropical coastlines within 30 years under high-emissions scenarios.
红树林对相对海平面上升(RSLR)的响应机制还不太清楚。我们研究了在末次冰消期的最后阶段,红树林垂直堆积对持续的 RSLR 的极限。红树林垂直堆积的开始时间和速度与 78 个地点的独立建模 RSLR 速度进行了比较。红树林森林在 9800 到 7500 年前扩张,以 RSLR 速度为主导的速率,堆积了厚厚的有机沉积物序列,这代表了一个重要的碳汇。我们发现红树林在 RSLR 速度超过 6.1 毫米/年时,极有可能(>90%的概率)无法启动持续的堆积。在高排放情景下,这个阈值可能在 30 年内被热带海岸线超越。