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预测玻璃海绵 Vazella pourtalesi 在斯科舍浅滩的分布及其在气候变化面前的持续存在。

Predicted distribution of the glass sponge Vazella pourtalesi on the Scotian Shelf and its persistence in the face of climatic variability.

机构信息

Department of Fisheries and Oceans, Bedford Institute of Oceanography, Dartmouth, Nova Scotia, Canada.

Department of Biological Sciences and K.G. Jebsen Centre for Deep-Sea Research, University of Bergen, Bergen, Norway.

出版信息

PLoS One. 2018 Oct 24;13(10):e0205505. doi: 10.1371/journal.pone.0205505. eCollection 2018.

DOI:10.1371/journal.pone.0205505
PMID:30356324
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6200246/
Abstract

Emerald Basin on the Scotian Shelf off Nova Scotia, Canada, is home to a globally unique aggregation of the glass sponge Vazella pourtalesi, first documented in the region in 1889. In 2009, Fisheries and Oceans Canada (DFO) implemented two Sponge Conservation Areas to protect these sponge grounds from bottom fishing activities. Together, the two conservation areas encompass 259 km2. In order to ascertain the degree to which the sponge grounds remain unprotected, we modelled the presence probability and predicted range distribution of V. pourtalesi on the Scotian Shelf using random forest modelling on presence-absence records. With a high degree of accuracy the random forest model predicted the highest probability of occurrence of V. pourtalesi in the inner basins on the central Scotian Shelf, with lower probabilities at the shelf break and in the Fundian and Northeast Channels. Bottom temperature was the most important determinant of its distribution in the model. Although the two DFO Sponge Conservation Areas protect some of the more significant concentrations of V. pourtalesi, much of its predicted distribution remains unprotected (over 99%). Examination of the hydrographic conditions in Emerald Basin revealed that the V. pourtalesi sponge grounds are associated with a warmer and more saline water mass compared to the surrounding shelf. Reconstruction of historical bottom temperature and salinity in Emerald Basin revealed strong multi-decadal variability, with average bottom temperatures varying by 8°C. We show that this species has persisted in the face of this climatic variability, possibly indicating how it will respond to future climate change.

摘要

加拿大新斯科舍省斯科蒂亚架上的翡翠盆地,是玻璃海绵瓦泽拉·波塔莱西全球唯一的聚集区,该海绵于 1889 年首次在该地区被记录。2009 年,加拿大渔业和海洋部(DFO)设立了两个海绵保护区,以保护这些海绵免受底鱼捕捞活动的影响。这两个保护区总面积为 259 平方公里。为了确定海绵场仍然不受保护的程度,我们使用基于存在-缺失记录的随机森林模型,对翡翠盆地斯科蒂亚架上的 V. pourtalesi 的存在概率和预测分布进行建模。随机森林模型以很高的准确性预测了 V. pourtalesi 在中央斯科蒂亚架内盆地中出现的最高概率,在架边缘和 Fundian 和 Northeast 海峡中的概率较低。底部温度是模型中其分布的最重要决定因素。尽管 DFO 的两个海绵保护区保护了一些更重要的 V. pourtalesi 集中地,但仍有超过 99%的预测分布未受保护。对翡翠盆地水文学条件的研究表明,与周围大陆架相比,V. pourtalesi 海绵场与更温暖、更咸的水团有关。对翡翠盆地历史底部温度和盐度的重建显示出强烈的数十年变化,平均底部温度变化了 8°C。我们表明,该物种在面对这种气候变异性时得以幸存,这可能表明它将如何应对未来的气候变化。

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