Atmosphere and Ocean Research Institute, The University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba 277-8564, Japan.
IFREMER, Avenue Jean Monnet, BP171, 34203 Sète Cedex, France.
Biol Rev Camb Philos Soc. 2015 Nov;90(4):1035-64. doi: 10.1111/brv.12144. Epub 2014 Oct 8.
The spawning areas of the Atlantic freshwater eels were discovered about a century ago by the Danish scientist Johannes Schmidt who after years of searching found newly hatched larvae of the European eel, Anguilla anguilla, and the American eel, Anguilla rostrata, in the southern Sargasso Sea. The discovery showed that anguillid eels migrate thousands of kilometers to offshore spawning areas for reproduction, and that their larvae, called leptocephali, are transported equally long distances by ocean currents to their continental recruitment areas. The spawning sites were found to be related to oceanographic conditions several decades later by German and American surveys from 1979 to 1989 and by a Danish survey in 2007 and a German survey in 2011. All these later surveys showed that spawning occurred within a restricted latitudinal range, between temperature fronts within the Subtropical Convergence Zone of the Sargasso Sea. New data and re-examinations of Schmidt's data confirmed his original conclusions about the two species having some overlap in spawning areas. Although there have been additional collections of leptocephali in various parts of the North Atlantic, and both otolith research and transport modelling studies have subsequently been carried out, there is still a range of unresolved questions about the routes of larval transport and durations of migration. This paper reviews the history and basic findings of surveys for anguillid leptocephali in the North Atlantic and analyses a new comprehensive database that includes 22612 A. anguilla and 9634 A. rostrata leptocephali, which provides a detailed view of the spatial and temporal distributions and size of the larvae across the Atlantic basin and in the Mediterranean Sea. The differences in distributions, maximum sizes, and growth rates of the two species of larvae are likely linked to the contrasting migration distances to their recruitment areas on each side of the basin. Anguilla rostrata leptocephali originate from a more western spawning area, grow faster, and metamorphose at smaller sizes of <70 mm than the larvae of A. anguilla, which mostly are spawned further east and can reach sizes of almost 90 mm. The larvae of A. rostrata spread west and northwest from the spawning area as they grow larger, with some being present in the western Caribbean and eastern Gulf of Mexico. Larvae of A. anguilla appear to be able to reach Europe by entering the Gulf Stream system or by being entrained into frontal countercurrents that transport them directly northeastward. The larval duration of A. anguilla is suggested to be quite variable, but gaps in sampling effort prevent firm conclusions. Although knowledge about larval behaviour is lacking, some influences of directional swimming are implicated by the temporal distributions of the largest larvae. Ocean-atmosphere changes have been hypothesized to affect the survival of the larvae and cause reduced recruitment, so even after about a century following the discovery of their spawning areas, mysteries still remain about the marine life histories of the Atlantic eels.
大西洋淡水鳗的产卵场大约在一个世纪前被丹麦科学家约翰内斯·施密特(Johannes Schmidt)发现。经过多年的搜索,他在马尾藻海南部发现了新孵化的欧洲鳗(Anguilla anguilla)和美洲鳗(Anguilla rostrata)幼体。这一发现表明,鳗鲡类鳗鱼会迁徙数千公里到近海产卵场繁殖,而它们的幼体,称为柳叶鳗,会被洋流同样长的距离输送到它们的大陆补充区。几十年后,德国和美国于 1979 年至 1989 年以及丹麦于 2007 年和德国于 2011 年进行的调查发现了这些产卵场与海洋地理条件有关。所有这些后来的调查都表明,产卵发生在一个狭窄的纬度范围内,在马尾藻海亚热带辐合带内的温度锋之间。新的数据和对施密特数据的重新检查证实了他关于这两个物种在产卵区有一些重叠的原始结论。尽管在北大西洋的不同地区已经有了更多的柳叶鳗收集,并且随后进行了耳石研究和运输模型研究,但关于幼虫运输路线和迁徙持续时间仍然存在一系列未解决的问题。本文回顾了北大西洋鳗鲡柳叶鳗调查的历史和基本发现,并分析了一个新的综合数据库,该数据库包括 22612 条欧洲鳗和 9634 条美洲鳗柳叶鳗,该数据库详细显示了大西洋盆地和地中海的幼虫的时空分布和大小。这两个物种的幼虫的分布、最大尺寸和生长率的差异可能与它们在盆地两侧的补充区之间的迁徙距离有关。美洲鳗的柳叶鳗起源于一个更西部的产卵区,生长速度更快,在<70 毫米的体型时就完成变态,而欧洲鳗的幼虫则主要在更东部产卵,体型可达近 90 毫米。随着美洲鳗的柳叶鳗生长变大,它们向西部和西北部扩散,在加勒比海西部和墨西哥湾东部也有一些存在。欧洲鳗的柳叶鳗似乎可以通过进入墨西哥湾流系统或被卷入直接向东北方向输送它们的锋前逆流进入欧洲。欧洲鳗的幼虫持续时间可能变化很大,但由于采样工作的差距,无法得出明确的结论。尽管对幼虫行为的了解还很缺乏,但最大幼虫的时间分布暗示了定向游泳的一些影响。海洋-大气变化被假设会影响幼虫的生存并导致补充减少,因此,即使在发现它们的产卵场大约一个世纪之后,大西洋鳗鱼的海洋生活史仍然存在许多谜团。