The DynaDeep observatory – a unique approach to study high-energy subterranean estuaries

Subterranean estuaries are connective zones between inland aquifers and the open sea where terrestrial freshwater and circulating seawater mix and undergo major biogeochemical changes. They are biogeochemical reactors that modify groundwater chemistry prior to discharge into the sea. We propose that subterranean estuaries of high-energy beaches are particularly dynamic environments, where the effect of the dynamic boundary conditions propagates tens of meters into the subsurface, leading to strong spatio-temporal variability of geochemical conditions. We hypothesize that they form a unique habitat with an adapted microbial community unlike other typically more stable subsurface environments. So far, however, studies concerning subterranean estuaries of high-energy beaches have been rare and therefore their functioning, and their importance for coastal ecosystems, as well as for carbon, nutrient and trace element cycling, is little understood. We are addressing this knowledge gap within the interdisciplinary research project DynaDeep by studying the combined effect of surface (hydro- and morphodynamics) on subsurface processes (groundwater flow and transport, biogeochemical reactions, microbiology). A unique subterranean estuary observatory was established on the northern beach of the island of Spiekeroog facing the North Sea, serving as an exemplary high-energy research site and model system. It consists of fixed and permanent infrastructure such as a pole with measuring devices, multi-level groundwater wells and an electrode chain. This forms the base for autonomous measurements, regular repeated sampling, interdisciplinary field campaigns and experimental work, all of which are integrated via mathematical modelling to understand and quantify the functioning of the biogeochemical reactor. First results show that the DynaDeep observatory is collecting the intended spatially and temporally resolved morphological, sedimentological and biogeochemical data. Samples and data are further processed ex-situ and combined with experiments and modelling. Ultimately, DynaDeep aims at elucidating the global relevance of these common but overlooked environments.

[1]  G. Massmann,et al.  Redox-zoning in high-energy subterranean estuaries as a function of storm floods, temperatures, seasonal groundwater recharge and morphodynamics , 2023, Estuarine, Coastal and Shelf Science.

[2]  T. Günther,et al.  Salinity distribution in the subterranean estuary of a meso-tidal high-energy beach characterized by Electrical Resistivity Tomography and Direct Push technology , 2023, Journal of Hydrology.

[3]  S. Kasten,et al.  The iron "redox battery" in sandy sediments: Its impact on organic matter remineralization and phosphorus cycling. , 2022, The Science of the total environment.

[4]  B. Engelen,et al.  The Spiekeroog Coastal Observatory: A Scientific Infrastructure at the Land-Sea Transition Zone (Southern North Sea) , 2022, Frontiers in Marine Science.

[5]  B. Engelen,et al.  Cross-Shore and Depth Zonations in Bacterial Diversity Are Linked to Age and Source of Dissolved Organic Matter across the Intertidal Area of a Sandy Beach , 2021, Microorganisms.

[6]  J. Scholten,et al.  A State-Of-The-Art Perspective on the Characterization of Subterranean Estuaries at the Regional Scale , 2021, Frontiers in Earth Science.

[7]  M. Beck,et al.  Cycling of redox-sensitive trace metals in barrier island freshwater lenses. , 2021, The Science of the total environment.

[8]  A. Boehm,et al.  The Beach Aquifer Microbiome: Research Gaps and Data Needs , 2021, Frontiers in Environmental Science.

[9]  B. Engelen,et al.  The Three Domains of Life Within the Discharge Area of a Shallow Subterranean Estuary at a High Energy Beach , 2021, Frontiers in Environmental Science.

[10]  M. Beck,et al.  Thallium cycling in pore waters of intertidal beach sediments , 2021 .

[11]  G. Massmann,et al.  The impact of morphodynamics and storm floods on pore water flow and transport in the subterranean estuary , 2021, Hydrological Processes.

[12]  M. Böttcher,et al.  Hydrogeochemistry of near-surface groundwater on a developing barrier island (Spiekeroog, Germany): The role of inundation, season and vegetation , 2021 .

[13]  T. Dittmar,et al.  Molecular Traits of Dissolved Organic Matter in the Subterranean Estuary of a High-Energy Beach: Indications of Sources and Sinks , 2021, Frontiers in Marine Science.

[14]  C. Ruiz‐González,et al.  The microbial dimension of submarine groundwater discharge: current challenges and future directions , 2021, FEMS microbiology reviews.

[15]  M. Beck,et al.  A Multi-Method Approach for Quantification of In- and Exfiltration Rates from the Subterranean Estuary of a High Energy Beach , 2020, Frontiers in Earth Science.

[16]  M. Böttcher,et al.  The impact of temperature on the water isotope (2H/1H, 17O/16O, 18O/16O) fractionation upon transport through a low-density polyethylene membrane , 2020, Isotopes in environmental and health studies.

[17]  B. Engelen,et al.  Seasonal Dynamics of Microbial Diversity at a Sandy High Energy Beach Reveal a Resilient Core Community , 2020, Frontiers in Marine Science.

[18]  G. Massmann,et al.  Groundwater flow and residence times below a meso-tidal high-energy beach: A model-based analyses of salinity patterns and 3H-3He groundwater ages , 2020 .

[19]  T. Günther,et al.  Monitoring freshwater–saltwater interfaces with SAMOS – installation effects on data and inversion , 2020 .

[20]  S. Littmann,et al.  The effect of sediment grain properties and porewater flow on microbial abundance and respiration in permeable sediments , 2020, Scientific Reports.

[21]  H. Marchant,et al.  Seasonality of Organic Matter Degradation Regulates Nutrient and Metal Net Fluxes in a High Energy Sandy Beach , 2020, Journal of Geophysical Research: Biogeosciences.

[22]  B. Blossier,et al.  The role of frequency spread on swash dynamics , 2019, Geo-Marine Letters.

[23]  H. Michael,et al.  Hydrologic Shifts Create Complex Transient Distributions of Particulate Organic Carbon and Biogeochemical Responses in Beach Aquifers , 2019, Journal of Geophysical Research: Biogeosciences.

[24]  H. Prommer,et al.  Modeling of biogeochemical processes in a barrier island freshwater lens (Spiekeroog, Germany) , 2019, Journal of Hydrology.

[25]  W. Arnold,et al.  Quantitative Dissolution of Environmentally Accessible Iron Residing in Iron-Rich Minerals: A Review , 2019, ACS Earth and Space Chemistry.

[26]  J. Jiao,et al.  Tidal induced dynamics and geochemical reactions of trace metals (Fe, Mn, and Sr) in the salinity transition zone of an intertidal aquifer. , 2019, The Science of the total environment.

[27]  T. Dittmar,et al.  Spatial and Temporal Patterns of Pore Water Chemistry in the Inter-Tidal Zone of a High Energy Beach , 2019, Frontiers in Marine Science.

[28]  L. Giani,et al.  Iron sulfide formation in young and rapidly-deposited permeable sands at the land-sea transition zone. , 2019, The Science of the total environment.

[29]  L. Giani,et al.  Landscapes and soils of North Sea barrier islands: a comparative analysis of the old West and young East of Spiekeroog Island (Germany) , 2018, Erdkunde.

[30]  T. Sachs,et al.  Sulfate deprivation triggers high methane production in a disturbed and rewetted coastal peatland , 2018, Biogeosciences.

[31]  S. Higgins,et al.  The dimensionality of niche space allows bounded and unbounded processes to jointly influence diversification , 2018, Nature Communications.

[32]  J. Jiao,et al.  Seasonality of Nutrient Flux and Biogeochemistry in an Intertidal Aquifer , 2018, Journal of Geophysical Research: Oceans.

[33]  J. Jiao,et al.  Tidal Fluctuation Influenced Physicochemical Parameter Dynamics in Coastal Groundwater Mixing Zone , 2018, Estuaries and Coasts.

[34]  L. Giani,et al.  Hydrochemical evolution of a freshwater lens below a barrier island (Spiekeroog, Germany): The role of carbonate mineral reactions, cation exchange and redox processes , 2018 .

[35]  M. Larocque,et al.  Flow and discharge of groundwater from a snowmelt-affected sandy beach , 2018 .

[36]  T. Günther,et al.  CONSTRAINING ELECTRIC RESISTIVITY TOMOGRAPHY BY DIRECT PUSH ELECTRIC CONDUCTIVITY LOGS AND VIBRACORES: AN EXEMPLARY STUDY OF THE FIUME MORTO SILTED RIVERBED (OSTIA ANTICA, WESTERN ITALY) , 2018 .

[37]  D. A. Barry,et al.  Groundwater dynamics in subterranean estuaries of coastal unconfined aquifers: Controls on submarine groundwater discharge and chemical inputs to the ocean , 2017 .

[38]  H. Freund,et al.  Impact of storm tides and inundation frequency on water table salinity and vegetation on a juvenile barrier island , 2017 .

[39]  M. Kuypers,et al.  Denitrifying community in coastal sediments performs aerobic and anaerobic respiration simultaneously , 2017, The ISME Journal.

[40]  Christian Winter,et al.  Spatial and temporal scales of shoreline morphodynamics derived from video camera observations for the island of Sylt, German Wadden Sea , 2017, Geo-Marine Letters.

[41]  Oliver Zielinski,et al.  The drivers of biogeochemistry in beach ecosystems: A cross-shore transect from the dunes to the low-water line , 2017 .

[42]  T. Dittmar,et al.  Molecular Fractionation of Dissolved Organic Matter in a Shallow Subterranean Estuary: The Role of the Iron Curtain , 2016, Environmental science & technology.

[43]  A. Paytan,et al.  Submarine Groundwater Discharge as a Source of Nutrients to the North Pacific and Arctic Coastal Ocean , 2016 .

[44]  H. Brumsack,et al.  Transformation of silicon in a sandy beach ecosystem: Insights from stable silicon isotopes from fresh and saline groundwaters , 2016 .

[45]  S. Bujan,et al.  Measuring pore water oxygen of a high-energy beach using buried probes , 2016 .

[46]  J. Famiglietti,et al.  Continental patterns of submarine groundwater discharge reveal coastal vulnerabilities , 2016, Science.

[47]  Bernd Brügge,et al.  The Coastal Observing System for Northern and Arctic Seas (COSYNA) , 2016 .

[48]  C. Rocha,et al.  Oxygen transport and reactivity within a sandy seepage face in a mesotidal lagoon (Ria Formosa, Southwestern Iberia) , 2016 .

[49]  T. Riedel,et al.  Benthic-pelagic coupling of nutrients and dissolved organic matter composition in an intertidal sandy beach , 2015 .

[50]  C. Winter,et al.  The impact of bedform migration on benthic oxygen fluxes , 2015 .

[51]  C. Winter,et al.  Tidally- and wind-driven residual circulation at the multiple-inlet system East Frisian Wadden Sea , 2015 .

[52]  A. Wehrmann,et al.  Carbon, nutrient and trace metal cycling in sandy sediments: A comparison of high-energy beaches and backbarrier tidal flats , 2015 .

[53]  P. Masqué,et al.  Submarine groundwater discharge as a major source of nutrients to the Mediterranean Sea , 2015, Proceedings of the National Academy of Sciences.

[54]  M. Böttcher,et al.  Tidal and spatial variations of DI13C and aquatic chemistry in a temperate tidal basin during winter time , 2015 .

[55]  A. Findlay,et al.  Dynamic hydrologic and biogeochemical processes drive microbially enhanced iron and sulfur cycling within the intertidal mixing zone of a beach aquifer , 2015 .

[56]  J. Melack,et al.  Temporal evolution and variability of dissolved inorganic nitrogen in beach pore water revealed using radon residence times. , 2014, Environmental science & technology.

[57]  M. Kuypers,et al.  The Fate of Nitrate in Intertidal Permeable Sediments , 2014, PloS one.

[58]  H. Michael,et al.  Saltwater‐freshwater mixing dynamics in a sandy beach aquifer over tidal, spring‐neap, and seasonal cycles , 2014 .

[59]  B. Jørgensen,et al.  Determination of dissimilatory sulfate reduction rates in marine sediment via radioactive 35S tracer , 2014 .

[60]  B. Schnetger,et al.  Determination of nitrate plus nitrite in small volume marine water samples using vanadium(III)chloride as a reduction agent , 2014 .

[61]  D. A. Barry,et al.  Groundwater flow and salt transport in a subterranean estuary driven by intensified wave conditions , 2014 .

[62]  H. Hemond,et al.  Transient groundwater dynamics in a coastal aquifer: The effects of tides, the lunar cycle, and the beach profile , 2013 .

[63]  H. Freund,et al.  Freshwater lens formation below juvenile dunes on a barrier island (Spiekeroog, Northwest Germany) , 2013 .

[64]  Roland Martin,et al.  Imaging artificial salt water infiltration using electrical resistivity tomography constrained by geostatistical data , 2012 .

[65]  K. Kröger,et al.  Groundwater ages, recharge conditions and hydrochemical evolution of a barrier island freshwater lens (Spiekeroog, Northern Germany) , 2012 .

[66]  W. Moore,et al.  Radium-based pore water fluxes of silica, alkalinity, manganese, DOC, and uranium: A decade of studies in the German Wadden Sea , 2011 .

[67]  M. Grinat,et al.  An Automated Electrical Resistivity Tomography System to Monitor the Freshwater/saltwater Zone on a North Sea Island , 2010 .

[68]  A. Loveless,et al.  Natural attenuation of nitrogen in groundwater discharging through a sandy beach , 2010 .

[69]  J. Deborde,et al.  Tidal sands as biogeochemical reactors , 2009 .

[70]  B. Engelen,et al.  The subsurface of tidal-flat sediments as a model for the deep biosphere , 2009 .

[71]  W. Burnett,et al.  Nutrient biogeochemistry in a Gulf of Mexico subterranean estuary and groundwater-derived fluxes to the coastal ocean , 2008 .

[72]  H. Prommer,et al.  Multicomponent reactive transport simulation of the Elder problem: Effects of chemical reactions on salt plume development , 2007 .

[73]  Ling Li,et al.  Salt-freshwater dynamics in a subterranean estuary over a spring-neap tidal cycle , 2007 .

[74]  Wayne S Gardner,et al.  Respiration and denitrification in permeable continental shelf deposits on the South Atlantic Bight: Rates of carbon and nitrogen cycling from sediment column experiments , 2007 .

[75]  D. A. Barry,et al.  Effect of tidal forcing on a subterranean estuary , 2007 .

[76]  Martin S. Andersen,et al.  Discharge of nitrate-containing groundwater into a coastal marine environment , 2007 .

[77]  M. Charette,et al.  Trace element cycling in a subterranean estuary: Part 2. Geochemistry of the pore water , 2006 .

[78]  Badin Gibbes,et al.  Driving mechanisms for groundwater flow and salt transport in a subterranean estuary , 2006 .

[79]  P. Groffman,et al.  Denitrification capacity in a subterranean estuary below a Rhode Island fringing salt marsh , 2005 .

[80]  A. Mulligan,et al.  Seasonal oscillations in water exchange between aquifers and the coastal ocean , 2005, Nature.

[81]  Gerald R. Dickens,et al.  Distributions of Microbial Activities in Deep Subseafloor Sediments , 2004, Science.

[82]  T. Dahlin,et al.  A numerical comparison of 2D resistivity imaging with 10 electrode arrays , 2004 .

[83]  M. Charette,et al.  Oxidative precipitation of groundwater‐derived ferrous iron in the subterranean estuary of a coastal bay , 2002 .

[84]  A. Roychoudhury,et al.  The ferrozine method revisited: Fe(II)/Fe(III) determination in natural waters , 2000 .

[85]  Jens Tronicke,et al.  Joint application of surface electrical resistivity- and GPR-measurements for groundwater exploration on the island of Spiekeroog—northern Germany , 1999 .

[86]  W. Moore The subterranean estuary: a reaction zone of ground water and sea water , 1999 .

[87]  G. Luther,et al.  PARTITIONING AND SPECIATION OF SOLID PHASE IRON IN SALTMARSH SEDIMENTS , 1994 .

[88]  P. Nielsen Tidal dynamics of the water table in beaches , 1990 .

[89]  B. Jørgensen,et al.  Measurement of bacterial sulfate reduction in sediments: Evaluation of a single-step chromium reduction method , 1989 .

[90]  D. Hammond,et al.  Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis , 1979 .

[91]  R. Benesch,et al.  Eine Methode zur colorimetrischen Bestimmung von Ammoniak in Meerwasser , 1972, Helgoländer wissenschaftliche Meeresuntersuchungen.

[92]  Joel D. Cline,et al.  SPECTROPHOTOMETRIC DETERMINATION OF HYDROGEN SULFIDE IN NATURAL WATERS1 , 1969 .

[93]  Jenna L. Luek,et al.  Chemical Flux Associated with Spatially and Temporally Variable Submarine Groundwater Discharge, and Chemical Modification in the Subterranean Estuary at Gloucester Point, VA (USA) , 2015, Estuaries and Coasts.

[94]  A. Stark,et al.  BaMn[CO3]2 – a previously unrecognized double carbonate in low-temperature environments: Structural, spectroscopic, and textural tools for future identification , 2012 .

[95]  W. Moore The effect of submarine groundwater discharge on the ocean. , 2010, Annual review of marine science.

[96]  Alyssa M. Dausman,et al.  SEAWAT Version 4: A Computer Program for Simulation of Multi-Species Solute and Heat Transport , 2008 .

[97]  J. R. Scotti,et al.  Available From , 1973 .

[98]  G. F. Humphrey,et al.  New spectrophotometric equations for determining chlorophylls a, b, c1 and c2 in higher plants, algae and natural phytoplankton , 1975 .