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当下是过去的关键:将海带床中的生态系统剧变与深海海胆的分布联系起来。

The present is the key to the past: linking regime shifts in kelp beds to the distribution of deep-living sea urchins.

机构信息

Department of Biology, Dalhousie University, Halifax, Nova Scotia, B3H 4R2, Canada.

出版信息

Ecology. 2017 Jan;98(1):253-264. doi: 10.1002/ecy.1638.

DOI:10.1002/ecy.1638
PMID:28052391
Abstract

Understanding processes that drive sudden shifts in ecosystem structure and function has become an important research focus for coastal management. In kelp bed ecosystems, regime shifts occur when high densities of sea urchins destructively graze kelp and create coralline algal barrens. While the importance of predation and disease in mediating shifts between kelp beds and barrens on shallow rocky reefs has been well documented, little is known about the role of deep-living urchins in these alternative stable-state dynamics. In this study, we test the hypothesis that deep-living urchins along the central Atlantic coast of Nova Scotia move onshore and trigger shifts from kelp beds to barrens on shallow rocky reefs. We documented urchin distribution and abundance using tow-camera surveys down to 140 m depth and spanning 140 km of coast and created a predictive species-distribution model using these observations and spatial data on environmental factors that likely delineate suitable habitat for urchins. We used a random forest model to generate our predictions, which correctly classified 91% of observations into a positive or negative occurrence of urchins. Sea urchins predominantly occurred within 1.5 km of shore, in depressions and flat habitats between 40 and 85 m depth. We found that shallow regions where destructive grazing fronts have been documented over the past four decades were closer to deep-living sea urchin habitats compared to regions that remained in a kelp bed state during the same period. This supports our prediction that deep-living urchins play an important role in driving shallow regime shift dynamics, and indicates that their distribution can help identify areas of coast that are most vulnerable to a collapse to barrens.

摘要

了解驱动生态系统结构和功能突然变化的过程已成为沿海管理的一个重要研究重点。在海带床生态系统中,当高密度的海胆破坏性地啃食海带并形成珊瑚藻荒地时,就会发生状态转变。虽然捕食和疾病在介导浅岩礁上的海带床和荒地之间的转变方面的重要性已得到充分证明,但对于深居的海胆在这些替代稳定状态动态中的作用知之甚少。在这项研究中,我们检验了这样一个假设,即新斯科舍省中部大西洋沿岸的深居海胆会向岸移动,并在浅岩礁上引发从海带床到荒地的转变。我们使用拖曳式摄像机调查记录了海胆的分布和丰度,调查范围可达 140 米深,覆盖了 140 公里的海岸线,并使用这些观察结果和有关环境因素的空间数据创建了一个预测物种分布模型,这些因素可能划定了海胆适宜的栖息地。我们使用随机森林模型生成预测结果,该模型正确地将 91%的观察结果分为海胆存在或不存在的情况。海胆主要出现在离海岸 1.5 公里以内的地方,在 40 到 85 米深的凹陷和平坦栖息地中。我们发现,在过去四十年中记录到破坏性放牧前沿的浅水区比在同一时期仍处于海带床状态的区域更接近深居海胆的栖息地。这支持了我们的预测,即深居海胆在驱动浅海状态转变动态方面发挥着重要作用,并表明它们的分布可以帮助确定最容易崩溃为荒地的沿海地区。

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