Water Bodies and Fish Communities
Berlin’s waterscape was shaped during the second stage of the Weichselian Glaciation, known as the Brandenburg Stage, which ended about 10,300 years ago. The Berlin Glacial Spillway is part of the Glogau-Baruth Glacial Spillway, which extends along the Weichselian end moraines of the Brandenburg Stage. Nestled within the North German Plain, Berlin’s waterscape is characterised by its prominent rivers, the Spree and the Havel. Together with their lake-like expansions, these rivers account for nearly two-thirds of Berlin’s water surface, totalling 5,952 hectares, or about 6.67 % of the city’s area. The Dahme and Spree rivers flow from the southeast into the Berlin Glacial Spillway, weaving through the city from east to west over 16.4 kilometres and 45.1 kilometres, respectively. Meanwhile, the Havel river enters from the north and meanders southward for 27.1 kilometres. The city’s largest water body is the lake-like expansion of the Unterhavel, spanning 1,175 hectares.
In addition to the rivers and canals that shape Berlin’s unique cityscape, there are 58 lakes larger than one hectare that lie at least partially within the city limits. Among these, the most remarkable are the fluvial lakes, featuring both river inflows and outflows. The Großer Müggelsee reigns as the largest lake, stretching across 766 hectares. In contrast, the Groß-Glienicker See stands as the sole substantial groundwater-fed lake. It is situated along Berlin’s southwestern border with Brandenburg, covering 667 hectares.
Small and very small water bodies dominate in terms of numbers. Berlin is home to a multitude of ponds, both artificial and natural, perennial and seasonal. It also features a number of quarry lakes and artificial rainwater retention basins. In total, 388 such water bodies are registered. They are joined by 316 drainage channels and ditches, some of which are piped, extending over a total length of more than 390 kilometres. These standing and flowing water bodies, small and very small in size, are predominantly managed and maintained by the city boroughs.
In Berlin, larger water bodies, such as rivers with catchment areas of more than 10 square kilometres and lakes exceeding 50 hectares, are subject to reporting under the European Water Framework Directive (WFD). Every six years, the European Commission requires updates on their ecological status and ecological potential, along with measures aimed at achieving a ‘good ecological status’. Therefore, current efforts and studies are primarily focused on this reduced network of lakes and rivers in Berlin that fall under this Directive.
Approximately 200 kilometres of Berlin’s flowing waters and ten lakes are monitored under the Water Framework Directive (WFD). Many of these flowing waters are manmade, such as canals and ditches. Type 21 ‘Flowing water discharging into a lake’ is the most common type of flowing water also among natural water bodies, due to the prevalence of fluvial lakes. Additionally, substantial portions fall into Type 15 ‘Sandy lowland river’, Type 14 ‘Sandy lowland stream’, and Type 11 ‘Humic stream’. Smaller areas at the mouths of tributaries are classified as Type 19 ‘Lowland water body’, while the Panke river, stretching from the Verteilerbauwerk, (tributary of the Nordgraben canal) to around Pankstraße, is classified as Type 12 ‘Gravelly lowland stream’. Some of these flowing waters transition between types, reflecting the natural longitudinal zonation of the rivers. For instance, the Spree changes type around the Elsenbrücke (at river km 22.05), shifting from a lowland river discharging into a lake to a sandy lowland river (SenUMVK 2021).
The lakes subject to reporting are mostly fluvial lakes with large catchment areas. They are classified as follows: the Großer Wannsee and Tegeler See are categorised as Type 10 ‘Stratified with a water residence time of more than 30 days’. Three other lakes fall into Type 11 ‘Unstratified with a water residence time of more than 30 days’, and a further four lakes are classified as Type 12 ‘Unstratified with a water residence time of 3 to 30 days’. The Groß-Glienicke See, a non-fluvial lake, also remains stratified during the summer, meaning its warm surface layer stays separate from the colder deep water below. It is therefore classified as a Type 10 lake. Unlike lakes with inflows and outflows, the water in the Groß-Glienicke See has a theoretical residence time of seven years (SenUMVK 2021).
The various types of flowing water are a lot more alike in their current morphological state, than the classification might suggest. Additionally, the reduced network of water bodies under the WFD overlooks the smaller water bodies. Similar to previous overviews of Berlin’s fish fauna, the present update is therefore based on a slightly different classification, which is, however, rather relevant when it comes to fish fauna. Flowing waters, canals, ditches, fluvial lakes, groundwater-fed lakes, and small standing water bodies of less than one hectare were classified based on their size, shape, connections, water sources, and potential as fish habitats.
The following section provides a brief overview of the main types of water bodies.