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2011 年日本宫城近海地震引发的巨大海啸对浅海软底环境和大型底栖生物组合的干扰。

Disturbance of shallow marine soft-bottom environments and megabenthos assemblages by a huge tsunami induced by the 2011 M9.0 Tohoku-Oki earthquake.

机构信息

Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba, Japan.

出版信息

PLoS One. 2013 Jun 7;8(6):e65417. doi: 10.1371/journal.pone.0065417. Print 2013.

DOI:10.1371/journal.pone.0065417
PMID:23762365
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3676465/
Abstract

Huge tsunami waves associated with megathrust earthquakes have a severe impact on shallow marine ecosystems. We investigated the impact of a tsunami generated by the 2011 M9.0 Tohoku-Oki earthquake on the seafloor and large benthic animals in muddy and sandy ria coasts (Otsuchi and Funakoshi bays) in northeastern Japan. We conducted underwater field surveys using scuba equipment in water depths of <20 m before the tsunami (September 2010) and after the tsunami (September 2011 and September 2012). During the study period, episodic changes in topography and grain-size composition occurred on the seafloor of the study area. Megabenthos sampling revealed a distinct pattern of distribution succession for each benthic species. For example, the protobranch bivalve Yoldia notabilis (Bivalvia: Nuculanidae) and the heterodont bivalve Felaniella usta (Bivalvia: Ungulinidae) disappeared after the tsunami event, whereas the distribution of the venus clam Gomphina melanaegis (Bivalvia: Veneridae) remained unchanged. In addition, the patterns of succession for a single species, such as the giant button top shell Umbonium costatum (Gastropoda: Trochidae) and the heart urchin Echinocardium cordatum (Echinoidea: Loveniidae), varied between the two bays studied. Our data also show that reestablishment of some benthic animal populations began within 18 months of the tsunami disturbance.

摘要

与俯冲带地震相关的巨型海啸波对浅海生态系统有严重影响。我们调查了 2011 年日本东北地区 M9.0 东日本大地震引发的海啸对泥质和沙质河口湾(大船渡湾和船越湾)海底和大型底栖动物的影响。我们使用水肺设备在海啸前(2010 年 9 月)和海啸后(2011 年 9 月和 2012 年 9 月)水深 <20 米的水下进行了实地调查。在研究期间,研究区域的海底地形和粒度组成发生了阶段性变化。大型底栖动物采样揭示了每个底栖物种分布演替的明显模式。例如,原鳃贝类 Yoldia notabilis(双壳纲:Nuculanidae)和异齿贝类 Felaniella usta(双壳纲:Ungulinidae)在海啸事件后消失,而维纳斯蛤 Gomphina melanaegis(双壳纲: Veneridae)的分布则保持不变。此外,单个物种如巨型纽扣贝壳 Umbonium costatum(腹足纲:Trochidae)和心形海胆 Echinocardium cordatum(海星纲:Loveniidae)的演替模式在两个研究湾也有所不同。我们的数据还表明,一些底栖动物种群在海啸干扰后 18 个月内开始重新建立。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/805d3aab4b44/pone.0065417.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/c2af31a131ab/pone.0065417.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/ea06c99be92f/pone.0065417.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/e3fa8c545e91/pone.0065417.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/805d3aab4b44/pone.0065417.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/c2af31a131ab/pone.0065417.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/ea06c99be92f/pone.0065417.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/e3fa8c545e91/pone.0065417.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f2f9/3676465/805d3aab4b44/pone.0065417.g004.jpg

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