2014
DOI: 10.1007/s13157-014-0544-z
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Understanding the Long Term Ecosystem Stability of a Fen Mire by Analyzing Subsurface Geology, Eco-Hydrology and Nutrient Stoichiometry – Case Study of the Rospuda Valley (NE Poland)

Abstract: We explored the background of differences in long-term stability between two parts in an undisturbed mire system (Rospuda fen, NE Poland). We re-constructed the Holocene history of the mire and compared it with current vegetation, water level dynamics, water chemistry and nutrient availability in two basins: A, where the mire terrestrialised a deep gyttja-filled lake, and B, where peatland developed directly on fluvial sands. The current vegetation of sedgemoss fens was described in 10 relevés from each basin,… Show more

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Cited by 19 publications
(16 citation statements)
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References 34 publications
(36 reference statements)
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“…PO 4 -P concentrations in terrace groundwater or in fen surface water did not vary appreciably ranging from approximately 0.04 to 0.1 mg/l, but concentrations in fen groundwater were significantly higher (1.2 mg/l; Table I). P release from fens has been linked to redox-status and P availability (Bailey Boomer and Bedford, 2008;Jablonska et al, 2014). Phosphorus will be released under hypoxic or anoxic conditions in the fen as a result of microbial Fe reduction process, which are known to have a dominant influence on P-dynamics (Sharpley, 1995).…”
Section: Nutrient Enrichment Riskmentioning
confidence: 99%
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“…PO 4 -P concentrations in terrace groundwater or in fen surface water did not vary appreciably ranging from approximately 0.04 to 0.1 mg/l, but concentrations in fen groundwater were significantly higher (1.2 mg/l; Table I). P release from fens has been linked to redox-status and P availability (Bailey Boomer and Bedford, 2008;Jablonska et al, 2014). Phosphorus will be released under hypoxic or anoxic conditions in the fen as a result of microbial Fe reduction process, which are known to have a dominant influence on P-dynamics (Sharpley, 1995).…”
Section: Nutrient Enrichment Riskmentioning
confidence: 99%
“…These threats affect the long-term stability of fen ecosystems, changing a system that once was resilient over long periods of time to one that may be rapidly degraded and altered (Dise, 2009;Jablonska et al, 2014). Existing fens are often fragmented and degraded, and many have been lost all together (Bedford and Godwin, 2003).…”
Section: Introductionmentioning
confidence: 99%
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“…At present, the largest preserved mire fragments occur in Poland in the Biebrza River valley (Herbichowa and Wołejko, 2004) and in the Rospuda River valley (Jabłońska et al, 2014). The Biebrza valley is an excellent area to study alkaline fens preserved over a large area with a varied conservation status (Jarzombkowski, 2010;Koczur, 2010;Kotowski et al, 2013).…”
Section: Why Alkaline Fens?mentioning
confidence: 99%
“…The shift of peatland vegetation towards treedominated ecosystems may likely be accelerated by anthropogenic disturbances (i.e., drainage; Tousignant et al 2010), climate change (i.e., future warming; Heijmans et al 2013), external eutrophication (i.e., atmospheric deposition; Riemersma et al 2006;Jickells 2005;Smith et al 1999), and abiotic variables (i.e., water fluctuations, N:P ratio; Økland et al 2001;Jabłońska et al 2014). Thus, protecting open wetland ecosystems is a priority of nature conservation policy.…”
Section: Introductionmentioning
confidence: 99%