@phdthesis{Kowalski2011,
  author    = {Nicole Kowalski},
  title     = {Transformation processes of redox-sensitive trace metals in the water column and sediments of temperate tidal systems},
  journal    = {Transformationsprozesse redox-sensitiver Spurenmetalle in Wassers{\"a}ule und Sediment gem{\"a}{\"s}igter tidaler Systeme},
  url       = {https://nbn-resolving.org/urn:nbn:de:gbv:9-001037-3},
  year      = {2011},
  abstract  = {Tidal flats represent the transition zone between the terrestrial and marine realm. They are subject to pronounced dynamics due to distinct tidal and seasonal variations of physical, chemical, and biological parameters significantly influencing redox-sensitive element cycles. Thus, redox-sensitive trace metals may be suitable indicators for variations in bioproductivity and microbial activity. Therefore, seasonal and tidal dynamics of manganese, iron, molybdenum, uranium, and vanadium were studied in the water column and sediments of tidal systems of the German Wadden Sea (southern North Sea) in the years 2007 to 2009 involving also previously analysed data from year 2002. To demonstrate the response of the trace metal cycles on phytoplankton blooms and enhanced biological activity time series data of nutrients and phytoplankton dynamics were also involved in this study. Pronounced cycling is seen for pelagic manganese revealing distinctly higher values during low tide. Complex seasonal cycling showing maxima of dissolved manganese in spring and late summer and a depletion period in early summer is caused by benthic-pelagic coupling and reflection of exhaustion and replenishing periods in the surface sediments. Vanadium dynamics are coupled to the manganese cycling due to vanadium scavenging and release during manganese oxide formation and reduction, respectively. Molybdenum and uranium behave almost conservatively following changes in salinity and thus, being slightly enhanced during high tide. Deviations from conservative behaviour are found to occur during breakdowns of summer phytoplankton blooms. In the following, significant enrichments of manganese, molybdenum, iron, and uranium are observed in the shallow pore waters. These coherences are assumed to be caused by a tight coupling of geochemical, biological, and sedimentological processes. Intense release of organic matter during the breakdowns of algae blooms leads together with enhanced bacterial activity in summer to the formation of organic- and trace metal-rich aggregates which are deposited and incorporated into the tidal surface sediments. Microbial decomposition of the aggregates and corresponding shifts in redox-conditions effect a release of dissolved trace metals into the pore water. Subsequently, the trace metals are fixed in the sediment as sulphides, adsorbed to organic compounds or released to the overlying bottom water. Furthermore, two tidal systems, one from the East Frisian and one from the North Frisian Wadden Sea are compared. Although, both areas show different hydrodynamical, sedimentological, and ecological conditions similar manganese dynamics are observed implying that this is a common behaviour in the entire Wadden Sea. However, distinct quantitative differences appear showing a 6-fold higher level of dissolved manganese in the water column of the East Frisian area. This is explained by a higher manganese release from tidal flat sediments and a larger sediment area/water volume ratio compared to the North Frisian area. Detailed time-series data of the nutrients phosphate, silica, and nitrite+nitrate are used to verify model simulations and to calculate nutrient export budgets considering tidal and seasonal variations. The model results imply an export of nutrients from the tidal flats into the open waters of the German Bight which is in the same order of magnitude as the combined discharge of the rivers Elbe, Weser, and Ems. To investigate the importance of the Wadden Sea as a potential manganese source for the North Sea, transects were carried out into several tidal flat areas of the North Frisian Wadden Sea. The results suggest that the North Frisian Wadden Sea is a less important source for dissolved manganese compared to the East Frisian area. In contrary, the export of particulate manganese seems to be more important showing distinctly higher concentrations in the North Frisian study areas in summer. The influence of sediment permeability and bioturbation on trace metal budgets of the pore waters are investigated in natural and experimentally manipulated tidal flat sediments. Advective pore water transport in highly permeable sandy sediments and bioturbation promote exchange processes at the sediment/water interface probably leading to reduced nutrient and trace metal enrichments in the shallow pore waters. Furthermore, the penetration of oxygen into deeper sediment layers induces a release of sulphidic bound molybdenum to the pore water. During laboratory experiments with natural anoxic sediments an effective oxidative molybdenum release is determined during resuspension of the sediments in oxic seawater. Thus, pronounced sediment resuspension during storm events is suggested to cause significant release of molybdate from displaced anoxic sediment components thereby enhancing the molybdate level of the open water column. In addition to the examination of recent biogeochemical processes, the paleo-environmental influence on geochemical and microbiological processes in Holocene and Pleistocene sediments of the East Frisian study area were analysed in an interdisciplinary study. It is found that the microbial abundance and activity are higher in the Holocene than in the Pleistocene sediments. However, this is mainly caused by present environmental conditions. The impact of the paleo-environment on the microbiology is less pronounced. The lithological succession affects hydrological processes which enable the transfer of electron donors and acceptors for present early diagenetic processes into deep sediment layers. The paleo-environmental imprint is still detectable but the modern biogeochemical processes dominate in the sediment-pore water system.},
  language  = {en}
}