Salt marshes along the coast of The Netherlands

The area of salt marshes does no longer increase. The recent erosion coincides with a rise on MHT-level in the last 25 years. Despite the decrease in area, sedimentation continues, especially in the lower salt marsh, which acts as a sink of nitrogen. Assimilation and mineralization of nitrogen are i...

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Published in:Hydrobiologia
Main Authors: Bakker, J.P., de Leeuw, J., Dijkema, K.S., Leendertse, P.C., Prins, H.H.T., Rozema, J.
Format: Article in Journal/Newspaper
Language:English
Published: 1993
Subjects:
Online Access:https://hdl.handle.net/11370/f59bda9c-27da-46a8-8bac-669bc863034d
https://research.rug.nl/en/publications/f59bda9c-27da-46a8-8bac-669bc863034d
https://doi.org/10.1007/BF00007263
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spelling ftunigroningenpu:oai:pure.rug.nl:publications/f59bda9c-27da-46a8-8bac-669bc863034d 2024-06-23T07:50:53+00:00 Salt marshes along the coast of The Netherlands Bakker, J.P. de Leeuw, J. Dijkema, K.S. Leendertse, P.C. Prins, H.H.T. Rozema, J. 1993-08-13 https://hdl.handle.net/11370/f59bda9c-27da-46a8-8bac-669bc863034d https://research.rug.nl/en/publications/f59bda9c-27da-46a8-8bac-669bc863034d https://doi.org/10.1007/BF00007263 eng eng https://research.rug.nl/en/publications/f59bda9c-27da-46a8-8bac-669bc863034d info:eu-repo/semantics/closedAccess Bakker , J P , de Leeuw , J , Dijkema , K S , Leendertse , P C , Prins , H H T & Rozema , J 1993 , ' Salt marshes along the coast of The Netherlands ' , Hydrobiologia , vol. 265 , no. 1-3 , pp. 73-95 . https://doi.org/10.1007/BF00007263 EXPLOITATION FAUNA MANAGEMENT NITROGEN CYCLE VEGETATION SALT MARSH SEA LEVEL RISE TIDAL EXCHANGE PLANT ZONATION SW NETHERLANDS NITROGEN COMMUNITIES ECOSYSTEMS NUTRIENTS ESTUARY BIOMASS article 1993 ftunigroningenpu https://doi.org/10.1007/BF00007263 2024-05-27T16:09:30Z The area of salt marshes does no longer increase. The recent erosion coincides with a rise on MHT-level in the last 25 years. Despite the decrease in area, sedimentation continues, especially in the lower salt marsh, which acts as a sink of nitrogen. Assimilation and mineralization of nitrogen are in balance in most plant communities along the gradient from lower to higher salt marshes. Mineralization of nitrogen increases towards the higher salt marsh, whereas the above-ground production and the mean nitrogen content of plants decrease. There is a positive correlation between quality of food plants in salt marshes and breeding success of Brent geese in the arctic tundra.Sedimentation on mainland salt marshes can compensate for the expected sea level rise. This is not the case for island salt marshes, if the relative sea level rise is more than 0.5-1.0 cm yr-1. The natural succession on salt marshes results in an accumulation of organic material, which is related to the dominance of single plant species. It is not clear to which extent this process is enhanced by eutrophication from acid deposition and seawater. Human exploitation of unprotected salt marshes is old and heavy in the system of mound settlements. Reclamation rates by dikes in the last centuries were higher than the rate of area increase.Grazing by cattle as a management practice results in both a higher plant species-richness and community diversity than abandoning; hay-making is intermediate, but shows less structural diversity than grazing with low stocking density. The invertebrate fauna is favoured by a short period of abandoning, but eventually characteristic salt marsh invertebrates are replaced by inland species. Many bird species prefer grazed salt marshes.The final section gives some perspectives. Provided that no further embankments take place the optimal nature management option for plants and animals is a vegetation pattern, which includes areas with a low canopy (grazed) and areas with a tall canopy. Article in Journal/Newspaper Arctic brent geese University of Groningen research database Arctic Hydrobiologia 265 1-3 73 95
institution Open Polar
collection University of Groningen research database
op_collection_id ftunigroningenpu
language English
topic EXPLOITATION
FAUNA
MANAGEMENT
NITROGEN CYCLE
VEGETATION
SALT MARSH
SEA LEVEL RISE
TIDAL EXCHANGE
PLANT ZONATION
SW NETHERLANDS
NITROGEN
COMMUNITIES
ECOSYSTEMS
NUTRIENTS
ESTUARY
BIOMASS
spellingShingle EXPLOITATION
FAUNA
MANAGEMENT
NITROGEN CYCLE
VEGETATION
SALT MARSH
SEA LEVEL RISE
TIDAL EXCHANGE
PLANT ZONATION
SW NETHERLANDS
NITROGEN
COMMUNITIES
ECOSYSTEMS
NUTRIENTS
ESTUARY
BIOMASS
Bakker, J.P.
de Leeuw, J.
Dijkema, K.S.
Leendertse, P.C.
Prins, H.H.T.
Rozema, J.
Salt marshes along the coast of The Netherlands
topic_facet EXPLOITATION
FAUNA
MANAGEMENT
NITROGEN CYCLE
VEGETATION
SALT MARSH
SEA LEVEL RISE
TIDAL EXCHANGE
PLANT ZONATION
SW NETHERLANDS
NITROGEN
COMMUNITIES
ECOSYSTEMS
NUTRIENTS
ESTUARY
BIOMASS
description The area of salt marshes does no longer increase. The recent erosion coincides with a rise on MHT-level in the last 25 years. Despite the decrease in area, sedimentation continues, especially in the lower salt marsh, which acts as a sink of nitrogen. Assimilation and mineralization of nitrogen are in balance in most plant communities along the gradient from lower to higher salt marshes. Mineralization of nitrogen increases towards the higher salt marsh, whereas the above-ground production and the mean nitrogen content of plants decrease. There is a positive correlation between quality of food plants in salt marshes and breeding success of Brent geese in the arctic tundra.Sedimentation on mainland salt marshes can compensate for the expected sea level rise. This is not the case for island salt marshes, if the relative sea level rise is more than 0.5-1.0 cm yr-1. The natural succession on salt marshes results in an accumulation of organic material, which is related to the dominance of single plant species. It is not clear to which extent this process is enhanced by eutrophication from acid deposition and seawater. Human exploitation of unprotected salt marshes is old and heavy in the system of mound settlements. Reclamation rates by dikes in the last centuries were higher than the rate of area increase.Grazing by cattle as a management practice results in both a higher plant species-richness and community diversity than abandoning; hay-making is intermediate, but shows less structural diversity than grazing with low stocking density. The invertebrate fauna is favoured by a short period of abandoning, but eventually characteristic salt marsh invertebrates are replaced by inland species. Many bird species prefer grazed salt marshes.The final section gives some perspectives. Provided that no further embankments take place the optimal nature management option for plants and animals is a vegetation pattern, which includes areas with a low canopy (grazed) and areas with a tall canopy.
format Article in Journal/Newspaper
author Bakker, J.P.
de Leeuw, J.
Dijkema, K.S.
Leendertse, P.C.
Prins, H.H.T.
Rozema, J.
author_facet Bakker, J.P.
de Leeuw, J.
Dijkema, K.S.
Leendertse, P.C.
Prins, H.H.T.
Rozema, J.
author_sort Bakker, J.P.
title Salt marshes along the coast of The Netherlands
title_short Salt marshes along the coast of The Netherlands
title_full Salt marshes along the coast of The Netherlands
title_fullStr Salt marshes along the coast of The Netherlands
title_full_unstemmed Salt marshes along the coast of The Netherlands
title_sort salt marshes along the coast of the netherlands
publishDate 1993
url https://hdl.handle.net/11370/f59bda9c-27da-46a8-8bac-669bc863034d
https://research.rug.nl/en/publications/f59bda9c-27da-46a8-8bac-669bc863034d
https://doi.org/10.1007/BF00007263
geographic Arctic
geographic_facet Arctic
genre Arctic
brent geese
genre_facet Arctic
brent geese
op_source Bakker , J P , de Leeuw , J , Dijkema , K S , Leendertse , P C , Prins , H H T & Rozema , J 1993 , ' Salt marshes along the coast of The Netherlands ' , Hydrobiologia , vol. 265 , no. 1-3 , pp. 73-95 . https://doi.org/10.1007/BF00007263
op_relation https://research.rug.nl/en/publications/f59bda9c-27da-46a8-8bac-669bc863034d
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1007/BF00007263
container_title Hydrobiologia
container_volume 265
container_issue 1-3
container_start_page 73
op_container_end_page 95
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