Remmert Hermann
II. Zoologisches Institut Erlangen, Erlangen, Deutschland.
Oecologia. 1968 Nov;1(4):296-303. doi: 10.1007/BF00386686.
Since animals of the marine littoral and supralitoral zones tolerate greater salinity-fluctuations than those of deep water layers they are far better adapted to colonize estuaries and brackish waters.This is why there live only few animals from the seabottom in brackish water even if it is very deep. Only animals from the littoral invade water with low or fluctuationg salinities.Those which are not restricted to surface regions (by their food - many depend on green plants) extend their range in brackish waters into deep layers since there is almost no competition.Therefore the bottom communities of the sea differ very much from the bottom communities of deep brackish waters.The extension of the range of marine littoral animals in deep brackish basins ("Brackwassersubmergenz") therefore is characteristic for deep brackish-water-zones and no special case of the Baltic Sea.
由于海洋潮间带和潮上带的动物比深水层的动物能耐受更大的盐度波动,所以它们更能适应在河口和咸淡水中栖息。这就是为什么即使咸淡水很深,海底也只有很少的海洋动物生存。只有来自潮间带的动物会侵入盐度低或波动的水域。那些不受限于表层区域(因其食物——许多依赖绿色植物)的动物,由于几乎没有竞争,所以它们在咸淡水中的分布范围会延伸到深层。因此,海洋底部群落与深咸淡水底部群落有很大差异。海洋潮间带动物在深咸淡水盆地中的分布范围扩展(“咸淡水下沉”)因此是深咸淡水区域的特征,并非波罗的海的特殊情况。