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The impact of conifer plantation forestry on the Chydoridae communities of blanket bog lakes. Tom J. Drinan , Conor T. Graham, John O’Halloran and Simon S.C. Harrison HYDROFOR Project . Background.
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The impact of conifer plantation forestry on the Chydoridaecommunities of blanket bog lakes Tom J. Drinan, Conor T. Graham, John O’Halloran and Simon S.C. Harrison HYDROFOR Project
Background • Plantation forests cover an estimated 10% of the Irish land surface area. Many of these plantations are on peat soils • Extensive afforestation of peat soils has taken place since the 1950’s – this crop is now reaching harvestable age • Previous studies have demonstrated a high risk of plant nutrient and sediment run-off to receiving waters from afforested catchments, particularly on peat soils • There is a clear risk to the ecological status of high conservation value peatland water bodies from catchment forestry operations
Aims • To investigate how conifer plantation forestry operations affect blanket bog lakes in terms of: • Their hydrochemical status • 2) Their Chydoridae(Cladocera) communities
Study design Sedimentary (Sandstone) Geology Igneous (Granite) Geology • 6 lakes non-forested (‘blanket bog’) • 6 lakes afforested: • 3 lakes surrounded by mature conifer forests (‘mature plantation’) • 3 lakes surrounded by clearfelling (‘clearfell’) • 7 lakes non-forested (‘blanket bog’) • 7 lakes afforested: • 4 lakes surrounded by mature conifer forests (‘mature plantation’) • 3 lakes surrounded by clearfelling (‘clearfell’)
Study lakes • The lakes underlain by granite are located at lower altitude and in closer proximity to the coast than the lakes underlain by sandstone • S = Sandstone • G= Granite • B= Blanket bog • M= Mature plantation • C= Clearfell GB1 GM1 SB1 SB3 GM2 GB2 SB2 SB4 SM1 GM3 GB3 SB5 GB4 GM4 SM2 SB6 SM3 GC1 GB5 SC1 GC2 GB6 SC2 GB7 GC3 SC3
Blanket bog lake: catchment containing only undisturbed blanket bog
Mature plantation lake: catchment dominated by closed-canopy conifer plantation
Clearfell lake: catchment containing mature conifer plantation with recently (within 2 – 5 years) clearfelled areas
Methodology Water Chemistry • Dip samples (a single sample from the water column) were taken every two months from each lake, beginning March 2009 • We measured pH, conductivity, temperature, dissolved oxygen, colour, alkalinity, TDOC, TP, SRP, TN, TON, ammonia, SO4, Ca, Na, Cl, Mg, Al, Mn and Fe Chydoridae • Semi-quantitative method: slowly sweeping a hand-held sweep net (100 μm mesh, 0.15 m diameter frame) horizontally both inside and outside a stand of vegetation for 30 seconds in the littoral zone of each lake
a) Results – water chemistry Water Chemistry PCA • Higher plant nutrients, TDOC, major ions, heavy metals, and reduced dissolved oxygen concentrations in lakes with forestry b) • Sandstone blanket bog • Granite blanket bog • lSandstone mature plantation • pGranite mature plantation lSandstone clearfell pGraniteclearfell
Results – water chemistry Total Nitrogen Ammonia Soluble Reactive Phosphorus Granite Sandstone Chlorophyll a
Results – water chemistry Total monomeric aluminium pH Dissolved oxygen Dissolved organic carbon Granite Sandstone
Discussion of water chemistry Likely sources of forestry inputs include: • Decomposition of the clearfell residue (brash, foliage etc.) • Decomposition of peat soil • Artificial fertilisers applied during the forest crop cycle Potential impacts of forestry-mediated hydrochemical change: • Enhanced autotrophicand heterotrophic production • Reduced dissolved oxygen concentrations • Elevated heavy metal concentrations.
Results – chydorids Chydorid community nMDS • Sandstone blanket bog • Granite blanket bog • lSandstone mature plantation • pGranite mature plantation lSandstone clearfell pGraniteclearfell
Results – chydorids Chydorussphaericus Alonopsis elongata Alonellaexcisa Alonella nana Granite Sandstone
Results – chydorids • Alonopsiselongatadominant in blanket bog lakes and Chydorussphaericus, Alonellanana and Alonellaexcisadominant in clearfelland mature plantation lakes • Only two individuals of a single species (Alonaguttata) were recorded from a recently clearfelled lake underlain by granite. This lake also contained the highest concentrations of Al & Fe • Alonellaexcisawas more abundant in sandsone lakes
Discussion of chydorids • Increased autotrophy and heterotrophy leads to a reductionin size of the dominant food particles available A. elongata feeds on larger food particles, C.sphaericus, A. nana and A. excisafeed on smaller food particles • C. sphaericus is more tolerant to the general decline in lake water quality • Toxicity from heavy metals only important following recent extensive catchment clearfelling • The higher pH and base cation concentration, driven primarily by marine sea-spray deposition, may account for geological effects on chydorids
Conclusions • Chydorid community change is consistent with conifer plantation forestry exerting a trophic, rather than an acidic or toxic effect on lake ecosystems • Plantation forestry effect was consistent across geologies and regions, indicating that the anthropogenic effect overrides any effect of catchment geology, altitude and proximity to sea
Acknowledgements • This study was funded by the HYDROFOR project which is co-funded by the Department of Agriculture, Fisheries and Food, and Environmental Protection Agency (EPA) under the STRIVE Programme 2007–2013 • We thank Dr. Elvira de Eyto for her help with zooplankton identification and various aspects of the research