TY - JOUR A1 - Reverey, Florian A1 - Grossart, Hans-Peter A1 - Premke, Katrin A1 - Lischeid, Gunnar T1 - Carbon and nutrient cycling in kettle hole sediments depending on hydrological dynamics: a review JF - Hydrobiologia : acta hydrobiologica, hydrographica, limnologica et protistologica N2 - Kettle holes as a specific group of isolated, small lentic freshwater systems (LFS) often are (i) hot spots of biogeochemical cycling and (ii) exposed to frequent sediment desiccation and rewetting. Their ecological functioning is greatly determined by immanent carbon and nutrient transformations. The objective of this review is to elucidate effects of a changing hydrological regime (i.e., dry-wet cycles) on carbon and nutrient cycling in kettle hole sediments. Generally, dry-wet cycles have the potential to increase C and N losses as well as P availability. However, their duration and frequency are important controlling factors regarding direction and intensity of biogeochemical and microbiological responses. To evaluate drought impacts on sediment carbon and nutrient cycling in detail requires the context of the LFS hydrological history. For example, frequent drought events induce physiological adaptation of exposed microbial communities and thus flatten metabolic responses, whereas rare events provoke unbalanced, strong microbial responses. Different potential of microbial resilience to drought stress can irretrievably change microbial communities and functional guilds, gearing cascades of functional responses. Hence, dry-wet events can shift the biogeochemical cycling of organic matter and nutrients to a new equilibrium, thus affecting the dynamic balance between carbon burial and mineralization in kettle holes. KW - Drought KW - Rewetting KW - Temporary pond KW - Kettle hole KW - Organic matter KW - Nitrogen KW - Phosphorus Y1 - 2016 U6 - https://doi.org/10.1007/s10750-016-2715-9 SN - 0018-8158 SN - 1573-5117 VL - 775 SP - 1 EP - 20 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Nitzsche, Kai Nils A1 - Kleeberg, Andreas A1 - Hoffmann, Carsten A1 - Merz, Christoph A1 - Premke, Katrin A1 - Gessler, Arthur A1 - Sommer, Michael A1 - Kayler, Zachary E. T1 - Kettle holes reflect the biogeochemical characteristics of their catchment area and the intensity of the element-specific input JF - Journal of soils and sediments : protection, risk assessment and remediation N2 - Purpose Kettle holes are small inland water bodies known to be dominated by terrigenous material; however, the processes and structures that drive the enrichment and depletion of specific geochemical elements in the water column and kettle hole sediment remain unclear. We hypothesized that the mobile elements (Ca, Fe, K, P) behave different from each other in their transport, intermediate soil retention, and final accumulation in the kettle hole sediment. Methods Topsoils from transects spanning topographic positions from erosional to depositional areas, sediment cores, shallow groundwater, and kettle hole water of two glacial kettle holes in NE Germany (Rittgarten (RG) and Kraatz (KR)) were collected. The Fe, Ca, K, and total P (TP) concentrations were quantified and additionally the major anions in shallow groundwater and kettle hole water. The element-specific mobilization, relocation, and, finally, accumulation in the sediment were investigated by enrichment factors. Furthermore, a piper diagram was used to estimate groundwater flow directions and pond-internal processes. Results At KR only, the upper 10 cm of the kettle hole sediment reflected the relative element composition of the eroded terrestrial soils. The sediment from both kettle holes was enriched in Ca, Fe, K, and P compared to topsoils, indicating several possible processes including the input of clay and silt sized particles enriched in these elements, fertilizer input, and pond-internal processes including biogenic calcite and hydroxyapatite precipitation, Fe-P binding (KR), FeSx formation (RG), and elemental fixation and deposition via floating macrophytes (RG). High Ca concentrations in the kettle hole water indicated a high input of Ca from shallow groundwater inflow, while Ca precipitation in the kettle hole water led to lower Ca concentration in groundwater outflow. Conclusions The considerable element losses in the surrounding soils and the inputs into the kettle holes should be addressed by comprehensive soil and water protection measures, i.e., avoiding tillage, fertilizing conservatively, and creating buffer zones. KW - Agricultural soils KW - Soil erosion KW - Element mobility KW - Phosphorus KW - Kettle hole KW - Sediment Y1 - 2022 U6 - https://doi.org/10.1007/s11368-022-03145-8 SN - 1439-0108 SN - 1614-7480 VL - 22 IS - 3 SP - 994 EP - 1009 PB - Springer CY - Heidelberg ER -