Department of Biological Sciences & Institute of Environment/Southeast Environmental Research Center, Florida International University, Miami, Florida, 33199, USA.
Everglades Foundation, Palmetto Bay, Florida, 33157, USA.
Ecology. 2020 May;101(5):e02988. doi: 10.1002/ecy.2988. Epub 2020 Mar 27.
Long-term ecological research can resolve effects of disturbance on ecosystem dynamics by capturing the scale of disturbance and interactions with environmental changes. To quantify how disturbances interact with long-term directional changes (sea-level rise, freshwater restoration), we studied 17 yr of monthly dissolved organic carbon (DOC), total nitrogen (TN), and phosphorus (TP) concentrations and bacterioplankton productivity across freshwater-to-marine estuary gradients exposed to multiple disturbance events (e.g., droughts, fire, hurricanes, and low-temperature anomalies) and long-term increases in water levels. By studying two neighboring drainages that differ in hydrologic connectivity, we additionally tested how disturbance legacies are shaped by hydrologic connectivity. We predicted that disturbance events would interact with long-term increases in water levels in freshwater and marine ecosystems to increase spatiotemporal similarity (i.e., synchrony) of organic matter, nutrients, and microbial activities. Wetlands along the larger, deeper, and tidally influenced Shark River Slough (SRS) drainage had higher and more variable DOC, TN, and TP concentrations than wetlands along the smaller, shallower, tidally restricted Taylor River Slough/Panhandle (TS/Ph) drainage. Along SRS, DOC concentrations declined with proximity to coast, and increased in magnitude and variability following drought and flooding in 2015 and a hurricane in 2017. Along TS/Ph, DOC concentrations varied by site (higher in marine than freshwater wetlands) but not year. In both drainages, increases in TN from upstream freshwater marshes occurred following fire in 2008 and droughts in 2010 and 2015, whereas downstream increases in TP occurred with coastal storm surge from hurricanes in 2005 and 2017. Decreases in DOC:TN and DOC:TP were explained by increased TN and TP. Increases in bacterioplankton productivity occurred throughout both drainages following low-temperature events (2010 and 2011) and a hurricane (2017). Long-term TN and TP concentrations and bacterioplankton productivity were correlated (r > 0.5) across a range of sampling distances (1-50 km), indicating spatiotemporal synchrony. DOC concentrations were not synchronized across space or time. Our study advances disturbance ecology theory by illustrating how disturbance events interact with long-term environmental changes and hydrologic connectivity to determine the magnitude and extent of disturbance legacies. Understanding disturbance legacies will enhance prediction and enable more effective management of rapidly changing ecosystems.
长期生态研究可以通过捕捉干扰的规模以及与环境变化的相互作用,来解决干扰对生态系统动态的影响。为了量化干扰如何与长期的定向变化(海平面上升、淡水恢复)相互作用,我们研究了横跨淡水到海洋河口梯度的 17 年的每月溶解有机碳(DOC)、总氮(TN)和磷(TP)浓度以及细菌浮游生物生产力,这些区域暴露在多种干扰事件(例如干旱、火灾、飓风和低温异常)和长期水位上升中。通过研究两个在水文连通性方面存在差异的相邻流域,我们还测试了干扰遗留物如何受到水文连通性的影响。我们预测,干扰事件将与淡水和海洋生态系统的长期水位上升相互作用,以增加有机物质、养分和微生物活动的时空相似性(即同步性)。较大、较深且受潮汐影响的 Shark River Slough(SRS)流域的湿地的 DOC、TN 和 TP 浓度高于较小、较浅且受潮汐限制的 Taylor River Slough/Panhandle(TS/Ph)流域的湿地。在 SRS 流域,DOC 浓度随距海岸的距离而降低,并且在 2015 年干旱和洪水以及 2017 年飓风之后,其幅度和变异性增加。在 TS/Ph 流域,DOC 浓度因地点而异(海洋湿地高于淡水湿地),但与年份无关。在两个流域中,上游淡水沼泽的 TN 增加发生在 2008 年火灾和 2010 年和 2015 年干旱之后,而下游 TP 增加发生在 2005 年和 2017 年飓风的沿海风暴潮之后。DOC:TN 和 DOC:TP 的减少是由 TN 和 TP 的增加解释的。在 2010 年和 2011 年低温事件以及 2017 年飓风之后,整个流域的细菌浮游生物生产力都有所增加。长期的 TN 和 TP 浓度和细菌浮游生物生产力在一定范围内的采样距离(1-50 公里)呈正相关(r>0.5),表明时空同步性。DOC 浓度在空间和时间上都没有同步。我们的研究通过说明干扰事件如何与长期环境变化和水文连通性相互作用来确定干扰遗留物的大小和范围,从而推进了干扰生态学理论。了解干扰遗留物将增强预测能力,并使我们能够更有效地管理快速变化的生态系统。