Biogeochemical processes at the sediment- water interface of intertidal sediments sub-project 7 MPI-Bremen DAPI stain of microbes on sand grains Method Parameter Biogeochemistry Michael Böttcher photopaper monitoring metals Bo Barker Jörgensen gelsampler sulfur species Katja Bosselman isotope spectrometry stable isotope ratios Alexandra Theune sulfate reduction with 35S 2D sulfide imaging Tim Ferdelman Experimental incubations sulfate reduction metal reduction rates Microsensor group Dirk de Beer microsensors pH, O 2 , Ca 2+ , H 2 S Paul Bird autonomous landers aerobic and anaerobic Eva Walpersdorf laboratory incubations mineralization Uschi Werner sulfate reduction with 35S DOC, POC Flux group Markus Hüttel benthic chambers respiration, nutrients, DIC Markus Billerbeck pore water analysis metal fluxes flow measurements pore water flow column experiments hydrodynamics Molecular ecology Rudolf Amann FISH SRB Quique Llobet-Brossa DGGE SOB Marc Mußmann CSLM 3-D imaging of distributions Lateral sediment transport Resuspension Advective transport Percolation and filtration Low tide level variable pore water flow and cotransport of solutes and particulates during ebb tide during flood tide currents and wave action In this project, the cycles of manganese, iron, and sulfur in the different sediment types will be investigated in a quantitative manner in order to understand the fluxes of matter and the biogeochemistry of the intertidal sediments. Through the interaction of geochemical and microbial processes, the decomposition of organic matter is tightly linked to the cycles of O, N, S, Mn, Fe and other elements. Manganese and iron are important for the electron transfer and are recirculated through various redox processes. However, our understanding of the role of these elements in the decomposition pathways is still poor. This project will address: (1) the biogeochemical processes that are important at the sediment-water interface and in the uppermost sediment layer (2) the mineralization rates of organic matter (3) the influence of environmental factors on the mineralization and biogeochemical zonation, (4) the relationship between the distribution of microorganisms and the biogeochemical processes and (5) the role of the hydrodynamic processes. All processes will be investigated with respect to their variability on tidal, day-night and seasonal scales in situ as well as in laboratory experiments. Transport processes in intertidal sand flats Setting up a lander equipped with microsensors Lander arrangement to measure flow above the sediment with ADV and equipment after accident with vessel Sulfide leaks out at low tide and is oxidized to sulfur

Biogeochemical processes at the sediment- water …Biogeochemical processes at the sediment-water interface of intertidal sediments sub-project 7 MPI-Bremen DAPI stain of microbes

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Biogeochemical processes at the sediment-water interface of intertidal sediments

sub-project 7MPI-Bremen

DAPI stain of microbeson sand grains

Method Parameter

BiogeochemistryMichael Böttcher photopaper monitoring metalsBo Barker Jörgensen gelsampler sulfur speciesKatja Bosselman isotope spectrometry stable isotope ratiosAlexandra Theune sulfate reduction with 35S 2D sulfide imagingTim Ferdelman Experimental incubations sulfate reduction

metal reduction ratesMicrosensor groupDirk de Beer microsensors pH, O2 , Ca2+ , H2SPaul Bird autonomous landers aerobic and anaerobicEva Walpersdorf laboratory incubations mineralizationUschi Werner sulfate reduction with 35S DOC, POC

Flux groupMarkus Hüttel benthic chambers respiration, nutrients, DICMarkus Billerbeck pore water analysis metal fluxes

flow measurements pore water flowcolumn experiments hydrodynamics

Molecular ecologyRudolf Amann FISH SRBQuique Llobet-Brossa DGGE SOBMarc Mußmann CSLM 3-D imaging of distributions

Lateral sediment transport

ResuspensionAdvective transport

Percolation and filtration

Low tidelevel

variable pore water flow andcotransport of solutesand particulates

during ebb tideduring flood tide

currents and wave action

In this project, the cycles of manganese, iron, and sulfur in the different sediment types will be investigated in a quantitative manner in order tounderstand the fluxes of matter and the biogeochemistry of the intertidal sediments. Through the interaction of geochemical and microbial processes, thedecomposition of organic matter is tightly linked to the cycles of O, N, S, Mn, Fe and other elements. Manganese and iron are important for the electron transferand are recirculated through various redox processes. However, our understanding of the role of these elements in the decomposition pathways is still poor.This project will address: (1) the biogeochemical processes that are important at the sediment-water interface and in the uppermost sediment layer (2) the mineralization rates of organic matter (3) the influence of environmental factors on the mineralization and biogeochemical zonation, (4) the relationship between the distribution of microorganisms and the biogeochemical processes and (5) the role of the hydrodynamic processes.All processes will be investigated with respect to their variability on tidal, day-night and seasonal scales in situ as well as in laboratory experiments.

Transport processes in intertidal sand flats

Setting up a lander equipped with microsensors

Lander arrangement to measure flow above the sediment withADV and equipment after accident with vesselSulfide leaks out at low tide and is oxidized to sulfur