Crotty Sinead M, Angelini Christine, Bertness Mark D
Department of Environmental Engineering Sciences, Engineering School of Sustainable Infrastructure and Environment, University of Florida, Gainesville, FL, United States of America.
Department of Ecology and Evolutionary Biology, Brown University, Providence, RI, United States of America.
PLoS One. 2017 Aug 31;12(8):e0183058. doi: 10.1371/journal.pone.0183058. eCollection 2017.
Climate change and other anthropogenic stressors are converging on coastal ecosystems worldwide. Understanding how these stressors interact to affect ecosystem structure and function has immediate implications for coastal planning, however few studies quantify stressor interactions. We examined past and potential future interactions between two leading stressors on New England salt marshes: sea-level rise and marsh crab (Sesarma reticulatum) grazing driven low marsh die-off. Geospatial analyses reveal that crab-driven die-off has led to an order of magnitude more marsh loss than sea-level rise between 2005 and 2013. However, field transplant experimental results suggest that sea-level rise will facilitate crab expansion into higher elevation marsh platforms by inundating and gradually softening now-tough high marsh peat, exposing large areas to crab-driven die-off. Taking interactive effects of marsh softening and concomitant overgrazing into account, we estimate that even modest levels of sea-level rise will lead to levels of salt marsh habitat loss that are 3x greater than the additive effects of sea-level rise and crab-driven die-off would predict. These findings highlight the importance of multiple stressor studies in enhancing mechanistic understanding of ecosystem vulnerabilities to future stress scenarios and encourage managers to focus on ameliorating local stressors to break detrimental synergisms, reduce future ecosystem loss, and enhance ecosystem resilience to global change.
气候变化和其他人为压力源正在影响全球范围内的沿海生态系统。了解这些压力源如何相互作用以影响生态系统的结构和功能对沿海规划具有直接意义,然而很少有研究对压力源之间的相互作用进行量化。我们研究了新英格兰盐沼两个主要压力源之间过去和未来可能的相互作用:海平面上升和食草沼泽蟹(网纹泽蟹)啃食导致的低海拔沼泽死亡。地理空间分析表明,在2005年至2013年期间,蟹类导致的沼泽损失比海平面上升导致的沼泽损失高出一个数量级。然而,野外移植实验结果表明,海平面上升将通过淹没并逐渐软化目前坚硬的高海拔沼泽泥炭,促使蟹类向更高海拔的沼泽平台扩张,使大片区域遭受蟹类导致的死亡。考虑到沼泽软化和随之而来的过度啃食的交互作用,我们估计,即使是适度的海平面上升也将导致盐沼栖息地丧失的程度比海平面上升和蟹类导致的死亡的累加效应所预测的高出3倍。这些发现凸显了多压力源研究对于增强对生态系统应对未来压力情景脆弱性的机制理解的重要性,并鼓励管理者专注于缓解局部压力源,以打破有害的协同作用,减少未来的生态系统损失,并增强生态系统对全球变化的恢复力。