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岩石潮间生物的垂直分布随着东北太平洋海岸的海平面变化而变化

Nikolas J Kaplanis¹, Mark W Denny², Peter T Raimondi¹

¹Department of Ecology and Evolutionary Biology, University of California, Santa Cruz, Santa Cruz, California, USA.

Global change biology

|October 23, 2024

概括

岩石的潮间区域的生态变化受到长期海平面上升 (SLR) 和周期性的天体力学的影响. 这些自然循环可以放大或减弱SLR影响,使潮间社区的预测变得复杂.

科学领域:

海洋生态海洋生态学
气候变化科学气候变化科学
海洋学海洋学海洋学

背景情况:

从长期气候变化中解脱环境强迫变化,对于生态系统管理至关重要.
潮间群落对海平面变化很敏感,这是由于不同的垂直区域划分.
了解这些动态对于预测全球变化下的社区结构和功能至关重要.

研究的目的:

为了研究岩石潮间物种的垂直分布的变化,以应对海平面变化和长期海平面上升 (SLR).
区分短期海平面波动,周期性天体力学和人类SLR对潮间生物的影响.
评估种群特异性反应如何影响社区结构和功能.

主要方法:

在东北太平洋海岸 (NPC) 跨多个时间尺度的海平面数据分析.
检查潮幅度的变化,包括18.6年的月球衰减周期.
潮间种群的垂直分布转移与短期变化,月球周期和十年SLR的相关性.

主要成果:

潮间种群对短期 (每月/每年) 的海平面变化表现出有限的反应.
观察到显著的,特定于种群的垂直分布变化与18.6年的月球周期和长期SLR相关.
各种类型的反应不同,主要是基于它们的垂直分布,周期动态调节SLR影响.

结论:

长期的SLR正在对潮间生态系统产生可衡量的影响.
循环的天体力学混了SLR效应的解释,创造了复杂的压力模式.
潮间社区因持续的气候变化而面临周期性的压力和非线性转变,需要持续的大规模监测.

关键词:

东北太平洋海岸的太平洋海岸.分布转移转移分配转移的时间.环境变化的变化.长期监测长期监测长期监测月亮的月球衰减.岩石的潮间区域岩石的潮间区域海平面上升的海平面上升区域划分区分区分区分区分区分区分区分区分区分区分区分

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