School of Biological & Chemical Sciences, Queen Mary University of London, London E1 4NS, UK; Freshwater Biological Association, The Ferry Landing, Far Sawrey, Ambleside, Cumbria LA22 OLP, UK.
Cardiff University Water Research Institute and School of Biosciences, Cardiff CF10 3TL, UK.
Sci Total Environ. 2017 Jan 1;574:1294-1304. doi: 10.1016/j.scitotenv.2016.07.212. Epub 2016 Oct 7.
The longitudinal distribution of many taxa in rivers is influenced by temperature. Here we took advantage of two older datasets on net-spinning caddisflies (Hydropsychidae) from contrasting European rivers to assess changes in species occurrence and relative abundance along the river by resampling the same sites, postulating that an increase in river temperature over the intervening period should have resulted in cool-adapted species retreating into the headwaters and warm adapted species expanding upstream. Distributional changes in the Welsh Usk were slight between 1968/69 and 2010, one rare species appearing at a single headwater site and one warm-adapted species disappearing from the main river. Distributional changes in the French Loire, between 1989-93 and 2005, were similarly modest, with no consistent movement of species up- or downstream. We estimate that the decadal rate of increase in the mean summer daily maximum in the Usk was only 0.1°C at one 'summer cool' headwater site, while a neighbouring 'summer warm' tributary increased by 0.16°C per decade, and the main river by 0.22°C. The Loire is warmer than the Usk and the mean decadal rates of increase, over the period 1989-2005, at three sites along the lower reaches were 0.39, 0.48 and 0.77°C. Increases in stream and river temperature, therefore, were spatially variable and were not associated with consistent upstream movement of species in either of these (very different) rivers. We conclude that either the temperature increases have hitherto been insufficient to affect species distribution or, more speculatively, that it may not be possible for river organisms (that do not respond only to temperature) to move upstream because of a developing spatial mismatch between key habitat characteristics, some of them changing with the climate but others not.
许多河流中的生物分类群的纵向分布受到温度的影响。在这里,我们利用来自对比鲜明的欧洲河流的两个较旧的网纺石蛾(Hydropsychidae)数据集,通过重新采样相同的地点来评估物种出现和相对丰度沿河流的变化,推测在这段时间内河流温度的升高应该导致适应寒冷的物种退缩到源头,而适应温暖的物种则向上游扩张。1968/69 年至 2010 年间,威尔士乌斯克河的分布变化很小,一种稀有物种出现在一个源头地点,一种适应温暖的物种从主河道消失。1989-93 年至 2005 年间,法国卢瓦尔河的分布变化也同样不大,没有物种持续向上游或下游移动。我们估计,乌斯克河一个“夏季凉爽”源头地点的夏季日最高平均温度的十年增长率仅为 0.1°C,而一个相邻的“夏季温暖”支流每十年增加 0.16°C,主河增加 0.22°C。卢瓦尔河比乌斯克河温暖,在 1989-2005 年期间,下游三个地点的平均十年增长率分别为 0.39°C、0.48°C 和 0.77°C。因此,溪流和河流温度的增加在空间上是可变的,并且与这两条(非常不同)河流中物种的一致向上移动无关。我们得出结论,要么温度升高迄今还不足以影响物种分布,要么更推测性地说,由于关键栖息地特征之间出现空间不匹配,河流生物(不仅仅对温度做出反应)可能无法向上游移动,其中一些特征随气候而变化,但其他特征则没有。