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首页> 外文期刊>Marine ecology progress series >Spatial dynamics, ecological thresholds and phase shifts: modelling grazer aggregation and gap formation in kelp beds
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Spatial dynamics, ecological thresholds and phase shifts: modelling grazer aggregation and gap formation in kelp beds

机译:空间动力学,生态阈值和相移:模拟海藻床上的放牧者聚集和缺口形成

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On the Atlantic coast of Nova Scotia, transitions between alternative states of the subti-dal ecosystem, kelp beds and sea urchin barrens, occur on a decadal scale. To explore the process of urchin aggregation within kelp beds that leads to the shift to barrens, we developed a coupled map lattice model to simulate the spatial dynamics of kelp and green sea urchin Strongylocentrotus droe-bachiensis abundance over time. Our simulations show that the following factors can cause sea urchins to form grazing aggregations that create gaps in a kelp bed: (1) random movement by >60% of sea urchins residing in the bed, (2) moderate to high levels of spatial variability in sea urchin recruitment (30 to 90 [urchins m~(-2)]~2), (3) localized aggregation of sea urchins (150 urchins m~(-2)) amid a moderate to high background density of sea urchins within the kelp bed (>10 urchins m~(-2)), with or without a chemotactic response of sea urchins to kelp, and (4) removal of kelp from areas >20 m~2 (to simulate physical or biological disturbance, or harvesting). Gaps formed at random locations within the spatial domain and expanded and coalesced to form barrens in which sea urchins were randomly distributed. Sea urchins formed circular fronts around gaps in the kelp bed. The rate of advance of fronts (and increase in gap size) was linearly related to the density of sea urchins at the front. The duration of the transition to the barrens state decreased with increases in (1) the proportion (P_m) of sea urchins moving (from >6 yr for P_m = 0.8 to <2 yr for P_m = 1) and (2) the variance of sea urchin recruitment (from >5 yr for 30 (urchins m~(-2)]~2 to <3 yr for 90 (urchins M~(-2)]~2). Our findings support observations of gap formation within kelp beds that resulted in widespread destructive grazing on this coast in the late 1960s. Our model provides a predictive tool for the design of monitoring programs and field experiments to explore the underlying mechanisms of an ecosystem phase shift that has major ecological conseguences.
机译:在新斯科舍省的大西洋沿岸,潮下带生态系统的替代状态,海带床和海胆贫瘠之间的过渡发生在年代际尺度上。为了探索海带床中海胆聚集的过程,从而导致其向贫瘠状态转移,我们开发了一种耦合的地图格模型,以模拟海带和绿海顽童Strongylocentrotus droe-bachiensis随时间推移的空间动态。我们的模拟结果表明,以下因素可能导致海胆形成放牧聚集体,从而在海带床上形成缝隙:(1)居住在该海床中的海胆中有60%以上的海胆随机运动;(2)中度到高水平的空间变异性在海胆募集中(30至90 [海胆m〜(-2)]〜2),(3)在中等至高背景密度的海胆中局部聚集海胆(150海胆m〜(-2))海藻床(> 10 urchins m〜(-2)),有或没有海胆对海带的趋化反应,以及(4)从> 20 m〜2的区域去除海带(以模拟物理或生物干扰,或收获)。间隙在空间域内的任意位置形成,并扩展并聚结在一起,形成海胆随机分布的贫瘠之地。海胆在海带床上的缝隙周围形成了圆形的锋面。锋面的前进速度(以及缝隙大小的增加)与锋面海胆的密度线性相关。过渡到贫瘠状态的持续时间随着(1)海胆移动比例(P_m = 0.8从> 6 yr到P_m = 1从<2 yr)和(2)海胆募集(从> 5年(30个海胆m〜(-2)]〜2到<3年,90个海胆M〜(-2)]〜2)我们的发现支持观察海藻床中间隙的形成该模型在1960年代后期对该海岸造成了广泛的破坏性放牧,为设计监测程序和野外实验提供了预测工具,以探索具有重大生态影响的生态系统相移的潜在机制。

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