Path of the Kuroshio Current affects the presence of several goby species in the brackish water area in northeastern Kyushu Island, Japan : results of a decade long survey in the Kita River
Path of the Kuroshio Current affects the presence of several goby species in the brackish water area in northeastern Kyushu Island, Japan : results of a decade long survey in the Kita River
复制标题
黑潮的路径影响了日本九州岛东北部咸水水域中几种虾虎鱼的存在：北河长达十年的调查结果
DOI：
10.1007/s10228-012-0305-z
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发表时间：
2013
影响因子：
1.2
通讯作者：
S Oikawa
中科院分区：
文献类型：
--
作者：
N. Onikura;R. Inui;S Oikawa
黑潮将包括热带和亚热带鱼类在内的各种海洋生物从日本南部地区运送到北太平洋沿岸（Senou et al. 2006; Matsuura 2012）。包括半咸水虾虎鱼在内的底栖鱼类在远洋幼虫期被运输（Senou et al. 2006; Maeda et al. 2007; Matsuura 2012）。然而，水流的路径显示了日本列岛在不同时期的各种变化，从几天到几十年（Kawabe 1995； Yamashiro和Kawabe 1996； Nagano和Kawabe 2004）。因此，黑潮的路径变化有可能影响群岛沿海地区鱼类的存在/缺失。在这项研究中，我们通过对九州岛东北部地区进行长达十年的监测，研究了黑潮的路径与几种虾虎鱼的存在之间的关系（图1a）。1999年至2011年，在九州岛东北部流入Nobeoka湾的北河，Gokase河系统的半咸淡水区域收集了鱼类存在/缺失的数据（图1b）。监测在人工环境中进行
The Kuroshio Current transports various marine organisms, including tropical and subtropical fishes, from the southern regions to the northern Pacific coast of Japan (Senou et al. 2006; Matsuura 2012). The demersal fishes, including brackish water gobies, are transported during the pelagic larval phase (Senou et al. 2006; Maeda et al. 2007; Matsuura 2012). However, the path of the current shows various changes along the Japanese archipelago at various time periods, from days to decades (Kawabe 1995; Yamashiro and Kawabe 1996; Nagano and Kawabe 2004). Thus, it is possible that the path changes of the Kuroshio Current influence the presence/absence of fishes along the coastal areas of the archipelago. In this study, we examined the relationships between the path of the Kuroshio Current and the presence of several gobies by conducting a decadelong monitoring of the northeastern region of the Kyushu Island (Fig. 1 a).Data on the presence/absence of fishes were collected from 1999 to 2011 in the brackish water area of the Kita River, Gokase River system, located at the northeastern region of the Kyushu Island and flowing into the Nobeoka Bay (Fig. 1 b). Monitoring was conducted in an artificial