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东南太平洋大陆和岛屿海岸的漂浮碎片和附着生物的日积累率:对基于全球模型的预测的检验。

Daily accumulation rates of floating debris and attached biota on continental and oceanic island shores in the SE Pacific: testing predictions based on global models.

机构信息

Departamento de Biologia Marina, Facultad de Ciencias del Mar, Universidad Catolica del Norte, Coquimbo, Chile.

Center for Ecology and Sustainable Management of Oceanic Islands ESMOI, Universidad Catolica del Norte, Coquimbo, Chile.

出版信息

PeerJ. 2023 Jul 27;11:e15550. doi: 10.7717/peerj.15550. eCollection 2023.

DOI:10.7717/peerj.15550
PMID:37525658
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10387232/
Abstract

BACKGROUND

Long-distance rafting on anthropogenic marine debris (AMD) is thought to have a significant impact on global marine biogeography and the dispersal of non-indigenous species. Therefore, early identification of arrival sites of AMD and its epibionts is crucial for the prioritization of preventive measures. As accumulation patterns along global coastlines are largely unstudied, we tested if existing oceanographic models and knowledge about upstream sources of litter and epibionts can be used as a simple and cost-efficient approach for predicting probable arrival sites of AMD-rafting biota in coastal zones.

METHODS

Using the Southeast Pacific as a model system, we studied daily accumulation rates, composition, and minimum floating times of AMD with and without epibionts on seven sandy beaches, covering the oceanic environment (Rapa Nui/Easter Island) and three regions (south, centre, north) along the Chilean continental coast, over a minimum of 10 consecutive days, and we contrast our results with predictions from published models.

RESULTS

Total AMD accumulation rates varied from 56 ± 36 (mean ± standard deviation) to 388 ± 433 items km d and differed strongly between regions, in accordance with local geomorphology and socioeconomic conditions (presence of larger cities and rivers upstream, main economic activities, .). Daily accumulation of items with pelagic epibionts (indicators of a pelagic trajectory) ranged from 46 ± 29 (Rapa Nui) to 0.0 items km d (northern continental region). Minimum floating times of rafts, as estimated from the size of pelagic epibionts, were longest in the South Pacific Subtropical Gyre's (SPSG) centre region, followed by the high-latitude continental region under the influence of the onshore West Wind Drift, and decreased along the continental alongshore upwelling current, towards lower latitudes. Apart from pelagic rafters, a wide range of benthic epibionts, including invasive and cryptogenic species, was found on rafts at the continental beaches. Similarly, we present another record of local benthic corals sp., on Rapa Nui rafts.

DISCUSSION

Our results agree with the predictions made by recent models based on the prevailing wind and surface current regimes, with high frequencies of long-distance rafting in the oceanic SPSG centre and very low frequencies along the continental coast. These findings confirm the suitability of such models in predicting arrival hotspots of AMD and rafting species. Moreover, storm surges as well as site-related factors seem to influence AMD arrival patterns along the Chilean continental coast and might cause the observed high variability between sampling sites and days. Our results highlight the possible importance of rafting as a vector of along-shore dispersal and range expansions along the SE Pacific continental coast and add to the discussion about its role in benthic species dispersal between South Pacific oceanic islands.

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/e2cd5ba46c8d/peerj-11-15550-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/dc4fb380231d/peerj-11-15550-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/fdd823f548f9/peerj-11-15550-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/b18e1e2ccd83/peerj-11-15550-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/4b102a25d378/peerj-11-15550-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/e2cd5ba46c8d/peerj-11-15550-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/dc4fb380231d/peerj-11-15550-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/fdd823f548f9/peerj-11-15550-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/b18e1e2ccd83/peerj-11-15550-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/4b102a25d378/peerj-11-15550-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0078/10387232/e2cd5ba46c8d/peerj-11-15550-g005.jpg
摘要

背景

人们认为,在人为海洋碎片(AMD)上进行长途漂流对 全球海洋生物地理学和外来物种的扩散有重大影响。因此,尽早确定 AMD 及其附生物到达的地点对于优先采取预防措施至关重要。由于全球海岸线的积累模式在很大程度上尚未得到研究,我们测试了现有的海洋学模型和关于垃圾和附生物上游来源的知识是否可用于作为一种简单且经济高效的方法来预测 AMD 漂流生物在沿海地区可能到达的地点。

方法

我们以南太平洋为模型系统,在七个沙滩上研究了 AMD 及其附生物的日积累率、组成和最小漂浮时间,这些沙滩覆盖了海洋环境(复活节岛)和智利大陆海岸的三个区域(南部、中部和北部),至少连续 10 天,我们将结果与已发表模型的预测进行了对比。

结果

AMD 的总积累率从 56±36(平均值±标准差)到 388±433 项 km d 不等,且在区域之间差异很大,这与当地地貌和社会经济条件(存在较大的城市和上游河流、主要经济活动等)相符。具有远洋附生物(远洋轨迹的指示物)的物品的日积累量从 46±29(复活节岛)到 0.0 项 km d(北部大陆区域)不等。根据远洋附生物的大小估算出的 AMD 筏子的最小漂浮时间,在南太平洋亚热带回旋区(SPSG)中心区域最长,其次是受近岸西向漂流影响的高纬度大陆区域,然后沿着大陆沿岸上升流逐渐减少,向较低纬度地区减少。除了远洋筏子外,在大陆海滩的 AMD 筏子上还发现了包括入侵种和隐生种在内的广泛的底栖附生物。同样,我们还记录了另一种在复活节岛 AMD 筏子上的当地底栖珊瑚。

讨论

我们的结果与最近基于盛行风和表面流模式的模型的预测一致,即在海洋 SPSG 中心区域,长距离漂流的频率很高,而在大陆海岸的频率非常低。这些发现证实了这些模型在预测 AMD 和漂流物种到达热点方面的适用性。此外,风暴潮以及与地点相关的因素似乎会影响智利大陆海岸的 AMD 到达模式,并导致采样点和日期之间的高变异性。我们的结果突出了漂流作为沿东南太平洋大陆海岸进行的扩散和范围扩大的重要性,并增加了关于其在南太平洋海洋岛屿之间的底栖物种扩散中的作用的讨论。

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