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Disturbance legacies increase and synchronize nutrient concentrations and bacterial productivity in coastal ecosystems

机译:干扰遗产增加并同步了沿海生态系统中的养分浓度和细菌生产力

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摘要

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 (  > 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.
机译:长期的生态研究可以通过捕获扰动的规模以及与环境变化的相互作用来解决扰动对生态系统动力学的影响。为了量化扰动如何与长期方向变化(海平面上升,淡水恢复)相互作用,我们研究了17年的月溶解有机碳(DOC),总氮(TN)和磷(TP)浓度以及整个浮游细菌的生产力暴露于多种干扰事件(例如干旱,火灾,飓风和低温异常)和长期水位上升的淡水到海洋河口梯度。通过研究水文连通性不同的两个相邻排水,我们还测试了水文连通性如何影响遗留遗产。我们预测干扰事件将与淡水和海洋生态系统中水位的长期增加发生相互作用,从而增加有机物,养分和微生物活动的时空相似性(即同步性)。沿较大,较深和受潮汐影响的鲨鱼河泥沼(SRS)排水带的湿地比沿较小,较浅,受潮汐约束的泰勒河泥沼/潘汉德尔(TS / Ph)排水带的湿地具有更高,更多的DOC,TN和TP浓度变化。沿着SRS,DOC浓度随着靠近海岸而下降,并且在2015年干旱和洪灾以及2017年飓风之后,其强度和变异性有所增加。沿着TS / Ph,DOC浓度随地点而变化(海洋比淡水湿地高),但没有年份。在这两个排水系统中,上游淡水沼泽的总氮含量在2008年大火以及2010年和2015年的干旱之后出现,而下游总磷的增加是由于2005年和2017年飓风带来的沿海风暴激增。DOC:TN和DOC:TP的下降是TN和TP升高解释了这一点。在低温事件(2010年和2011年)和飓风(2017年)之后的两个排水系统中,浮游细菌的生产力均得到提高。在一系列采样距离(1-50 km)内,长期TN和TP浓度与浮游细菌的生产力相关(> 0.5),表明时空同步。 DOC浓度在空间或时间上不同步。我们的研究通过说明扰动事件如何与长期环境变化和水文连通性相互作用来确定扰动遗留的程度和程度,从而改进了扰动生态学理论。了解扰动的遗留因素将增强预测,并能更有效地管理迅速变化的生态系统。

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