Tarbeker Moor

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FFH area Tarbeker Moor
Bodies of water and peat banks

Bodies of water and peat banks

location Approx. 10 km north of Bad Segeberg
surface 131 ha
Identifier FFH area no .: 1927-352
WDPA ID 555517969
Natura 2000 ID DE1927352
Geographical location 54 ° 2 ′  N , 10 ° 18 ′  E Coordinates: 54 ° 1 ′ 31 ″  N , 10 ° 18 ′ 18 ″  E
Tarbeker Moor (Schleswig-Holstein)
Tarbeker Moor
Setup date 2004
administration LLUR
f6
Degenerate moor

The Tarbeker Moor is the remainder of a larger moor complex that formed within a meltwater channel after the last Ice Age . In the 19th and 20th centuries, the surrounding moors were peeled off and almost all of them turned into grassland . Between 1951 and 1990, the Tarbeker Moor was partly pelted down to the mineral subsoil. The peat removal led to the complete destruction of the raised bog vegetation.

In 1991, the renaturation of the Tarbeker Moor (still profitable high moor ) began. Due to the damming up of the water from the Tensfelder Au and the influx of spring water from the subsoil and from the slopes, a large area of ​​vegetation of the transitional and vibrating turf bogs has developed on the former mining areas . In the western shallow lakes, peat moss-rich suspended blankets of swamp calla ( Calla palustris ) and open water areas with the common water hose ( Utricularia vulgaris ) dominate. Have in the Eastern Abgrabungsflächen from gray willow interspersed extensive holdings of Carex paniculata ( Carex paniculata ), the Scheinzyper sedge ( Carex pseudocyperus ) and the Tonquil ( Juncus effusus ) formed. Rare peat mosses ( Sphagnum subnitens , S. riparium ), reeds ( Phragmites australis ), cattails ( Typha spec.) And crab claws ( Stratiotes alioides ) occur in places . In the hollows, which are moistened by rainwater, stocks of the White Schnabelriedes ( Rhynchospora alba ) and the Scheidigen Cottongrass ( Eriophorum vaginatum ) are formed (peat bog ditches).

Overall, a small-scale mosaic of typical bog vegetation, bodies of water and dry peat dams was created. The area is home to numerous amphibian species such as the common spadefoot and the moor frog. The otter occurs in the Tensfelder Au area . The successfully initiated renaturation of the Tarbeker Moor has developed into a diverse, species-rich moor complex and is particularly worthy of protection as a remnant of an originally large moor landscape. It is of national importance in terms of its species and habitat diversity, its regeneration approaches and its large area. The overarching protection goal is the promotion of regenerating transitional moor vegetation and further development into raised moor . To this end, it is particularly important to optimize the wetness state in the moor and its surroundings. Furthermore, the suitability of the area as a walking corridor for the otter should be preserved.

Habitat types

  • Renatured degraded raised bogs
  • Transitional and swinging lawn bogs
  • Peat swamps with rush communities

Individual evidence

  1. ↑ Leaflet on the FFH area Tarberker Moor of the visitor information system (BIS) of the LLUR (PDF). Retrieved May 1, 2017 .
  2. ↑ a b c Regional Checklist of the State of Schleswig-Holstein (PDF). Retrieved May 1, 2017 .
  3. ↑ 1927-352 Tarbeker Moor (FFH area). Published by the Federal Agency for Nature Conservation . Retrieved February 7, 2019.

Web links

Commons : Tarbeker Moor  - Collection of images, videos and audio files