The Barnbruch is a wetland of international importance in the old glacial valley of the river Aller that provides a habitat for endangered species of birds , amphibians and insects . It lies between the city of Wolfsburg and town of Gifhorn and consists of an enclosed woodland area of around 1,500 hectares (3,700 acres) with surrounding meadows and pastures. This low-lying depression lies partly within the territory of the city of Wolfsburg and partly within Gifhorn district . Together with the Drömling around 15 km to the east, the Barnbruch is the most valuable ecological lowland region along the upper course of the Aller .
6-456: The Barnbruch is about 4 x 7 kilometres across and is bordered: Originally the Barnbruch was a carr ( Bruchwald ) or fen woodland. In 1830 it was the cause of complaint by the inhabitants of the neighbouring villages to their king. They said that, for years, they had not been able to harvest any hay and that their farms had been ruined by floods. Following a state treaty in 1860 between Prussia ,
12-415: A succession stage between the original reedy marsh and the likely eventual formation of forest in a sub - maritime climate . Carrs are wetlands that are dominated by shrubs rather than trees . The carr is one stage in a hydrosere : the progression of vegetation beginning from a terrain submerged by fresh water along a river or lake margin. In sub-maritime regions, it begins with reed -marsh. As
18-642: The Kingdom of Hanover and Duchy of Brunswick over the regulation of the Aller and the Ohre , work began on draining the area. The main contribution to this effort was the Aller Canal , built 1860-63, between Wolfsburg and Gifhorn . Draining the land of water turned the swamps into a wetland with a rich variety of trees, in which both fen and riverside woods with birch, oak, ash and alder trees could flourish. Today large parts of
24-448: The alder accounted for 82% of the total area, whilst pines covered only 1%. In 1875, as a result of the drainage, this had fundamentally changed. Now alders on covered 42% of the land, whilst pine and birch now made up 51%. 52°27′23″N 10°39′09″E / 52.45643°N 10.65262°E / 52.45643; 10.65262 Carr (landform) A carr is a type of waterlogged wooded terrain that, typically, represents
30-404: The Barnbruch are nature reserves , in which several areas have been left to evolve without any human intervention. Up to 1770 the swampy Bruchwald was not forested and pine trees only grew on a few higher points (sand dunes of ice age origin). The high levels of ground water and periodic flooding created alder groves which were largely inaccessible to people. In 1833 softwood trees, especially
36-437: The reeds decay, the soil surface eventually rises above the water, creating fens that allow vegetation such as sedge to grow. As this progression continues, riparian trees and bushes appear and a carr landscape is created – in effect a wooded fen in a waterlogged terrain. At this stage, overall, unlike the overwhelming acidity of decaying reeds, the pH is not too acidic and the soil is not too deficient in minerals, making
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