Brenner Moor

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"Brenner Moor" nature reserve
Trave on the northern border of the Brenner Moor

Trave on the northern border of the Brenner Moor

location City of Bad Oldesloe
surface 24 ha
Identifier NSG No. 92
WDPA ID 81458
Natura 2000 ID 2127-391
Geographical location 53 ° 49 '  N , 10 ° 21'  E Coordinates: 53 ° 49 '5 "  N , 10 ° 21' 10"  E
Brenner Moor (Schleswig-Holstein)
Brenner Moor
Setup date 1978
administration LLUR
particularities Inland salt moor
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The Brenner Moor is the largest inland salt moor in Schleswig-Holstein . In the Traven lowlands, it is almost entirely within the urban area of ​​Bad Oldesloe. It is limited to the north and east by the Trave. In the south it cuts through a small wooded area. A drainage ditch that flows into the Trave forms the border in the west, see maps.

Nature reserve

The area was declared a nature reserve on October 20, 1978 . Responsible is the lower landscape maintenance authority, Stormarn district . The state office for agriculture, the environment and rural areas (LLUR) of the state of Schleswig-Holstein transferred the care of the area to the geobotany working group in Schleswig-Holstein and Hamburg.

The nature reserve is part of the connected NATURA 2000 network of protected areas within the European Union . It is listed there under the profile number "2127-391 Travetal ( FFH area )".

In § 2 of the state ordinance on the nature reserve "Brenner Moor" (Nature Conservation Ordinance) it says: "The nature reserve serves to protect a flat salt moor in the Traven lowlands that has largely been preserved in its natural state. The plant communities occurring here are in some areas particularly characterized by the unique occurrence of salt springs in the interior. The soil and hydrological peculiarities that differ from the other Schleswig-Holstein moors are also responsible for a specific animal world. "

The nature reserve is easily accessible by paths. There are 10 observation stations on different topics on a circular route. Using the QR code on the number posts placed there, you can view more information on your smartphone .

Hydrology and botany

The saline springs are the specialty of this moor. The brine, which also comes to the surface in other places in Bad Oldesloe, has a salt concentration of 15 g / l and comes from a depth of around 500 meters. The salty environment attracts plants that are otherwise only found near the coast, e.g. B. Bottenbinse ( Juncus gerardii ), beach-trident ( Triglochin maritima ), samphire , salt aster , Salt Schuppenmiere , milkweed , the Prominent swaths and the beach cornices represented. Vaucheria algae feel particularly comfortable in carpets around the brine outlet. In some places the water has a salt content that corresponds to that of the North Sea . In the less salty parts of the nature reserve, reeds grow among other things .

Fauna in the lowlands and in the moor

Bird species

The reeds birds like come reed warbler , sedge warbler , marsh warbler , grasshopper warbler and reed bunting before.

Kingfisher , little grebe , marsh harrier and gray heron mainly come to forage in the moor and on the water , while bluethroat and nightingale also breed in the area.

The meadows are visited by meadow wilts , mountain pipits , starlings , swallows and finch birds as a resting place. The goldeneye use next tree cavities and nest boxes erected for rearing their chicks.

Snails

The salty springs are the ideal habitat for special mollusks . Therefore, the species common amber snail ( Succinea putris ), common smooth snail ( Cochlicopa lubrica ), smooth grass snail ( Vallonia pulchella ), water snail ( Deroceras laeve ), gray field snail ( Deroceras agreste ) and shiny dagger snail ( Zonitoides nitidus ) come before.

Early history

Since the beginning of the 1950s, the Brenner Moor and its immediate surroundings have repeatedly been the subject of archaeological investigations, especially by the Institute for Prehistory and Early History at Kiel University. In 2009 and 2010 geophysical and archaeological prospections were carried out using new methods in order to identify suitable excavation sites. During the excavations, stone-age settlement remains were found on the Trave and in the moor, as well as megalithic graves on the surrounding hills. The age of the pile remains with the 14 C method showed a settlement in the period 2700–2800 BC. Over 10,000 finds were recovered. Some of the finds are shown in the Bad Oldesloe local history museum.

Panorama Brenner Moor in December 2009

Web links

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

Individual evidence

  1. ↑ a b c d e f Dr. Ulrike Graeber, Holger Mordhorst-Bretschneider: Nature reserve "Brenner Moor" and Wolkenweher Niederung (2015). In: Leaflet 6292 of the BIS. State Office for Agriculture, Environment and Rural Areas of the State of Schleswig-Holstein (LLUR), November 2016, p. 1 , accessed on March 15, 2020 : "The Brenner Moor nature reserve includes the largest inland salt station in Schleswig-Holstein"
  2. ↑ Brenner Moor in Germany. In: protected planet. United Nations, accessed March 18, 2020 .
  3. ^ State ordinance on the nature reserve "Brenner Moor". GVOBl. 1978 324. In: Landesportal Schleswig-Holstein. State government of Schleswig-Holstein, October 20, 1978, accessed on March 15, 2020 .
  4. ^ State ordinance on the nature reserve "Brenner Moor" of October 20, 1978 § 2. Article (2). In: State portal: State regulations and state case law. State government of Schleswig-Holstein, January 16, 2019, accessed on March 16, 2020 : "District Administrator of the Stormarn District as a lower landscape maintenance authority"
  5. ^ Andrea Kühl: Care of protected areas in Schleswig-Holstein according to § 20 LNatSchG. In: Schleswig-Holstein state portal. State Office for Agriculture, Environment and Rural Areas of the State of Schleswig-Holstein (LLUR), April 2017, p. 3 , accessed on March 15, 2020 (see table serial no. 1.6.5).
  6. ↑ Profiles of the Natura 2000 areas. 2127-391 Travetal (FFH area). In: BfN website. Federal Agency for Nature Conservation, accessed on March 17, 2020 (mentioned salt springs and moors).
  7. ↑ § 2 of the "State Ordinance on the Nature Reserve" Brenner Moor "of October 20, 1978". sh.juris.de, accessed on October 22, 2013 .
  8. ↑ a b Dr. Ulrike Graeber: Nature reserve "Brenner Moor" and Wolkenweher Niederung. 10 stations to do your own research. In: Leaflet 6292 Special of the BIS. State Office for Agriculture, Environment and Rural Areas of the State of Schleswig-Holstein (LLUR), November 2016, p. 1 , accessed on March 16, 2020 : "The golden-bellied duck breeds in tree hollows near the Trave"
  9. ↑ T. Krause, S. Studenroth, M. Furchner, A. Hoffman, S. Lippe, K. Kotte and HF Schöler: The Brenner Moor - A saline bog as a source for halogenated and non-halogenated volatile compounds. (pdf 484 kB) 2012, accessed on August 28, 2017 .
  10. ↑ Susanne Rohde (2007), The Salt of Life - in the Brenner Moor, supplement to the Stormarner Tageblatt
  11. ↑ Dr. Ulrike Graeber, Holger Mordhorst-Bretschneider: Nature reserve "Brenner Moor" and Wolkenweher Niederung. Planting the salt springs. In: Leaflet 6292 of the BIS. State Office for Agriculture, Environment and Rural Areas of the State of Schleswig-Holstein (LLUR), November 2016, p. 1 , accessed on March 16, 2020 : "In addition to the samphire, the salt aster, the botany, the beach trident ... are represented"
  12. ^ Siegfried Jaeckel junior: The land snails Schleswig-Holstein and their distribution . In: Natural Science Association for Schleswig-Holstein (Hrsg.): Writings of the Natural Science Association Schleswig-Holstein . tape 24 , no. 1 . Kiel, Edaphic Factors, page 84, paragraph 3 ( uni-kiel.de [PDF]): “At the salt areas of the inland near Oldesloe, namely on the richest one, the Brenner Moor near Wolkenwehe, z. B. Succinea putris, Cochlicopa lubrica, Vallonia pulchella, Hydrolimax laevis, Deroceras agreste, Zonitoides nitidus encountered "
  13. ↑ Jan Piet Brozio: Megalithic systems and settlement patterns in the funnel-beaker-age Ostholstein . In: Johannes Müller (Ed.): Early monumentality and social differentiation . Institute for Prehistory and Protohistory at Kiel University. tape 9 . Publishing house Dr Rudolf Habelt GmbH, Bonn 2016, p. 528 ( uni-kiel.de [PDF; 85.0 MB ] E-Book): “Wood findings from the period 2800–2700 BC. Chr. "
  14. ↑ Article Kieler Nachrichten December 11, 2008 ( Memento from December 6, 2010 in the Internet Archive ) (PDF approx. 4MB)