Modelling Aquatic Ecosystems
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Supporting Information
1 Supporting Information 2 Contents: 3 Table S1 : TOC-MAR and OC gross sedimentation data from four lakes page S-1 4 Table S2 : Fred and TOC MAR values of six selected lakes page S-1 5 Figure S1 : Porewater profiles from Lake Zug page S-2 6 Figure S2 : Seasonal development of O2 concentration page S-3 7 8 9 Table S1: Average fluxes of TOC MAR, TOC gross sedimentation and the corresponding OC burial efficiency based on sediment trap data. TOC MAR at deepest benthic gross OC Burial Monitoring duration, Sampling Lake point sedimentation ref effiency % month-year interval gC m-2 yr-1 gC m-2 yr-1 Lake 43.79 45.62 104.19 4-2013 to 11-2014 2 weeks Baldegg Lake Aegeri 77.45 22.77 29.40 3-2014 to 12-2014 2 weeks Lake Hallwil 41.59 22.51 54.12 1-2014 to 12-2014 monthly Lake Rene Gächter 45.96 28.00 60.92 1-1984 to 12-1992 varying Sempach unpublished 10 11 12 Table S2: Characteristics of three eutrophic, one mesotrophic, and two oligotrophic lakes. Fred data for Rotsee, Türlersee, Lake Sempach, Lake 13 Murten and Pfäffikersee are from Müller et al. (2012) and Fred was calculated for Lake Erie (Adams et al., 1982), Lake Superior (Richardson 14 and Nealson, 1989; Remsen et al., 1989; Klump et al., 1989; Heinen and McManus, 2004; Li et al., 2012), and Lake Baikal (Och et al., 2012). 15 TOC MAR was calculated for all lakes based on literature data: Lake Murten (Müller and Schmid, 2009), Lake Baikal (Och et al., 2012), Lake 16 Sempach (Müller et al., 2012), Rotsee (RO) (Naeher et al., 2012), Pfäffikersee (unpublished data), Türlersee (Matzinger et al., 2008), Lake Erie 17 (Smith and Matisoff, 2008; Matisoff et al., 1977) and Lake Superior (Klump et al., 1989; Li et al., 2012). -
Change of Phytoplankton Composition and Biodiversity in Lake Sempach Before and During Restoration
Hydrobiologia 469: 33–48, 2002. S.A. Ostroumov, S.C. McCutcheon & C.E.W. Steinberg (eds), Ecological Processes and Ecosystems. 33 © 2002 Kluwer Academic Publishers. Printed in the Netherlands. Change of phytoplankton composition and biodiversity in Lake Sempach before and during restoration Hansrudolf Bürgi1 & Pius Stadelmann2 1Department of Limnology, ETH/EAWAG, CH-8600 Dübendorf, Switzerland E-mail: [email protected] 2Agency of Environment Protection of Canton Lucerne, CH-6002 Lucerne, Switzerland E-mail: [email protected] Key words: lake restoration, biodiversity, evenness, phytoplankton, long-term development Abstract Lake Sempach, located in the central part of Switzerland, has a surface area of 14 km2, a maximum depth of 87 m and a water residence time of 15 years. Restoration measures to correct historic eutrophication, including artificial mixing and oxygenation of the hypolimnion, were implemented in 1984. By means of the combination of external and internal load reductions, total phosphorus concentrations decreased in the period 1984–2000 from 160 to 42 mg P m−3. Starting from 1997, hypolimnion oxygenation with pure oxygen was replaced by aeration with fine air bubbles. The reaction of the plankton has been investigated as part of a long-term monitoring program. Taxa numbers, evenness and biodiversity of phytoplankton increased significantly during the last 15 years, concomitant with a marked decline of phosphorus concentration in the lake. Seasonal development of phytoplankton seems to be strongly influenced by the artificial mixing during winter and spring and by changes of the trophic state. Dominance of nitrogen fixing cyanobacteria (Aphanizomenon sp.), causing a severe fish kill in 1984, has been correlated with lower N/P-ratio in the epilimnion. -
Population Dynamics of Whitefish ( Coregonus Suidteri Fatio) in Artificially Oxygenated Lake Hallwil, with Special Emphasis on L
Diss. ETH No. 13706 Population dynamics of whitefish ( Coregonus suidteri Fatio) in artificially oxygenated Lake Hallwil, with special emphasis on larval mortality and sustainable management Dissertation submitted to the SWISS FEDERAL INSTITUTE OF TECHNOLOGY, ZURICH for the degree of Doctor of Natural Sciences presented by Carole Andrea Enz Dipl. Natw. ETH Zurich bon1 August 3, 1972 Citizen of Sch(1nholzerswilen (TG), Switzerland accepted on the recommendation of Prof. Dr. J. V. Ward, examiner Prof. Dr. H. Lehtonen, co-examiner Dr. R. Muller, co-examiner Kastanienbaum, 2000 Meinen Eltern und Max Copyright ~;i 2000 by Carole A. Enz, EA WAG Kastanienbaurn All rights reserved. No part of this book rnay be reproduced, stored in a retrieval systen1 or transmitted, in any fonn or by any ineans, electronic, rnechanical, pho- tocopying, recording or otherwise, without the prior written permission of the copyright holder. First Edition 2000 PUBLICATIONS CHAPTER 3 OF THE THESIS HAS BEEN ACCEPTED FOR PUBLICATION: ENZ, C. A., SCHAFFER E. & MOLLER R. Growth and survival of Lake Hallwil whitefish (Co reg onus suidteri) larvae reared on dry and live food. - Archiv fUr Hyclrobiologie. CHAPTERS 4, 5, 6 Ai~D 7 OF THESIS HA VE BEEN SUBMITTED FOR PUBLICATION: ENZ, C. A., MBWENEMO BIA, M. & MULLER. R. Fish species diversity of Lake Hallwil (Switzerland) in the course of eutrophication, with special reference to whitefish ( Coregonus suidteri). Submitted to Conservation Biology. ENZ, C. A .. SCHAFFER, E. & MULLER, R. Importance of prey movement, food particle and tank circulation for rearing Lake Ha11wil whitefish (Coregonus suidteri) larvae. Submitted to North Alnerican Journal of Aquaculture. -
Swiss Express Index Part 3 V3 : Editions 125 to 140 (March 2016-December 2019)
Swiss Express Index Part 3 v3 : Editions 125 to 140 (March 2016-December 2019) Part 1 covered issues 1 to 60 (January 1985 to December 1999) while Part 2 dealt with issues 61 to 124 (January 2000 to December 2015). This new Part follows the principles set out in Part 2 and runs from Issue 125 (March 2016) to 140 (December 2019). Issue Diagram(s) - General If Major (M) or Photo(s) Subject track, stock etc category Brief (B) only Edition Edition as appropriate Number date Boats Commuting by paddle steamer. 133 Mar-18 Boats DS St Urs on River Aare 125 Mar-16 Lakes Brienz/Thun - rise in passenger numbers Boats B 137 Mar-19 in 2018 compared to 2017. Boats Bodensee Train Ferries 139 Sep-19 Lake Geneva - parade of (mostly) paddle Boats 127 Sep-16 steamers, May 2016. Boats Lake Geneva - return of PS Italie to traffic. B 129 Mar-17 Lake Hallwil - new MV Delphin (dolphin) entered Boats B 135 Sep-18 service June 2018. Lake Luzern - MV Bürgenstock - new ship now Boats 135 Sep-18 in service. Lake Luzern - MV Diamant in service May 17 Boats 131 Sep-17 (replacing the "Rigi"). Lake Luzern - MV Diamant holed in an Boats B 133 Mar-18 accident, Dec.18. Update in Issue 134. Boats Lake Luzern - scrapping of freighter MV Luzern 137 Mar-19 Boats Lake Luzern - MV Mythen damaged at Gersau. B 135 Sep-18 Boats Lake Luzern - MV Rigi to be withdrawn in 2017. 127 Sep-16 Boats Lake Luzern - A quick trip on MV Rütli. -
Organic Carbon Mass Accumulation Rate Regulates the Flux of Reduced Substances from the Sediments of Deep Lakes
Research Collection Journal Article Organic carbon mass accumulation rate regulates the flux of reduced substances from the sediments of deep lakes Author(s): Steinsberger, Thomas; Schmid, Martin; Wüest, Alfred; Schwefel, Robert; Wehrli, Bernhard; Müller, Beat Publication Date: 2017-07-10 Permanent Link: https://doi.org/10.3929/ethz-b-000191117 Originally published in: Biogeosciences 14(13), http://doi.org/10.5194/bg-14-3275-2017 Rights / License: Creative Commons Attribution 3.0 Unported This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Biogeosciences, 14, 3275–3285, 2017 https://doi.org/10.5194/bg-14-3275-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Organic carbon mass accumulation rate regulates the flux of reduced substances from the sediments of deep lakes Thomas Steinsberger1,2, Martin Schmid1, Alfred Wüest1,3, Robert Schwefel3, Bernhard Wehrli1,2, and Beat Müller1 1Eawag, Swiss Federal Institute of Aquatic Science and Technology, 6047 Kastanienbaum, Switzerland 2Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, 8092 Zurich, Switzerland 3Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, École Polytechnique Fédérale de Lausanne, Institute of Environmental Engineering, 1015 Lausanne, Switzerland Correspondence to: Beat Müller ([email protected]) Received: 31 January 2017 – Discussion started: 17 February 2017 Revised: 23 May 2017 – Accepted: 2 June 2017 – Published: 10 July 2017 Abstract. The flux of reduced substances, such as methane hypolimnetic O2 consumption (Livingstone and Imboden, and ammonium, from the sediment to the bottom water (Fred/ 1996; Hutchinson, 1938; Cornett and Rigler, 1980), yet the is one of the major factors contributing to the consumption key processes are still debated. -
Sales Manual. Swiss Travel System
Sales Manual. Swiss Travel System. Version 1, 2020 Swiss Travel Guide Button-PRINT.pdf 1 20.08.19 14:27 Go digital – get the app! English Bernina at Lago Bianco Express STS-GB-L-20-en.pdfSTS-GB-L-20-en.pdfSTS-GB-L-20-en.pdf 1 1 18.09.19 18.09.19 11:301 11:30 18.09.19 11:30 StrasbourgStrasbourg | Paris | StrasbourgParis | Paris KarlsruheKarlsruhe | Frankfurt |Karlsruhe Frankfurt | Dortmund | | FrankfurtDortmund | Hamburg | Dortmund | Hamburg | Berlin | Hamburg| Berlin | Berlin Stuttgart StuttgartStuttgart Ulm | MünchenUlmUlm | München | München München MünchenMünchen Stockach StockachStockach Engen Engen Engen Blumberg-ZollhausBlumberg-ZollhausBlumberg-Zollhaus DEUTSCHLANDDEUTSCHLANDDEUTSCHLAND SeebruggSeebruggSeebrugg Bargen BargenOpfertshofenBargen Opfertshofen Ravensburg RavensburgRavensburg Train,Train,Train, busbus and andbus boat boatand boat Opfertshofen Überlingen ÜberlingenÜberlingen BeggingenBeggingenBeggingen Singen SingenSingen Thayngen ThayngenThayngen HemmentalHemmentalHemmental atat aa glanceglanceat a glance Rhein/Rhein/ Rhein/ SchleitheimSchleitheimSchleitheim MulhouseMulhouse Mulhouse Radolfzell RadolfzellRadolfzell Le RhinLe Rhin Le Rhin Mainau MainauMainau Version:Version: 12.20 12.201919 Version: 12.2019 Meersburg MeersburgMeersburg DueDue to to lack lack of of space spaceDue not not toall alllack lines lines of are spaceare indicated. indicated. not all Subjectlines Subject are to indicated. tochange. change. Subject to change. SchaffhausenSchaffhausenSchaffhausenRamsen RamsenRamsen Wangen (Allgäu)WangenWangen (Allgäu) -
HOTELS 2018 Luzern Weggis Vitznau Rigi Greppen Entlebuch Sempachersee Seetal Willisau
HOTELS 2018 Luzern Weggis Vitznau Rigi Greppen Entlebuch Sempachersee Seetal Willisau Deutsch | English Region Sempachersee Region Seetal eell 25 km 20 km P. Lucendro Region Willisau 2963 Gemsstock Gotthardpass 30 km Region 2961 2109 Luzern Weggis Vitznau Rigi 20 km Furkapass DisentisDisentis Hospental SedruSedrunn OOberalppassberalppass Realp 2431 Andermatt ObOberalpstockeralpstock 20204444 3328 UNESCO 50 km Biosphäre r Göschenen Göscheneralp Dammastock sche eglet Entlebuch BristenBristen 3630 Rhon 30733073 Sustenhorn MaderanertalMaderanert WWassen al 3503 Gr.Gr. WindgällenWindgällen BristenBristen GuGurtnellenrtnellen r e h 31883188 Amstegg Meiental c s t e l g Gutta t f ri T Gr. Spannort Sustenpass 3198 2224 Titlis Erstfeld 3238 S c h ä Gadmen c h e n Innertki t a l Surenenpass Schattdorf 2291 Jochpass Bürglen Urirotstock Hasliberg Kaiserstock Attinghausen 2928 2515 Melchsee-Frutt Altdorf Seedorf Engelberg Klingenstock Flüelen Bannalp 1935 Isenthal Brisen Fronalpstock Isleten 2404 Lungern 1922 o tatal Melchtal Stoos Sisikon Lungernsee Bauen Niederbauen Klewenalp Morschach 1593 Niederrickenbach Urnersee Giswil Seelisberg Wolfenschiessen Wirzweli G Schlattli Sachseln Emmetten Stanserhorn Flüeli- Ibach 1898 Ranft Brunnen Dallenwil Sarnersee V i e Beckenried Kerns Schwyz r w Gersau a Sarnen l d Buochs - Lauerz Stans ers Glaubenbergpass ee Ennetbürgen Alpnach- 1543 erg Vitznau Dorf Steinen Bürgenstock s Alpnachersee Pilatus Rigi Kulm t 2120 1798 ä Stansstad Rossberg Goldau t t Kehrsiten-Dorf Weggis e Hergiswil r s e e Kastanienbaum Arth -
How Aquatic Ecosystems Are Altered by Nutrients
Focus Focus How aquatic ecosystems Piet Spaak, biologist, is head of the Aquatic Ecology department. are altered by nutrients Co-author: Pascal Vonlanthen The reduction of phosphorus loads in Swiss lakes is a positive outcome of water pollution control efforts. But now, in order to increase fish yields on Lake Brienz and other waterbodies, members of the fishing community have called for phosphorus elimination to be reduced at local wastewater treatment plants. However, increases in phosphorus inputs to nutrient-poor lakes can lead to the extinction or merging of species, producing irreversible changes in aquatic ecosystems. The past few decades have seen a marked decrease in eutrophi- be increased as part of a pilot project. The supporters of this plan cation of Swiss lakes, thanks to the construction of wastewater argue that fish yields would then rise as a result of higher primary treatment plants (WWTPs), a ban on phosphates in detergents production (algal growth) [1]. Similar ideas are under consideration (enacted in 1985) and additional phosphorus precipitation at for Lake Lucerne and other waterbodies. WWTPs. As a result, water quality has improved substantially and habitats and species compositions have returned to a more nat- Displacement and merging of species. In the absence of nu- ural state. But the subject of phosphorus inputs has recently been trients, surface waters would be inhospitable to any form of life. raised once again, in particular because some people believe To be able to exist in a lake, organisms require a certain minimum that a lack of this nutrient is partly to blame for declining yields level of nutrients, which enter waters via natural processes of ero- of fish from certain lakes. -
Settling Waterscapes in Europe. the Archaeology of Neolithic and Bronze Age Pile-Dwellings
et al. (eds.) et Hafner Albert Hafner, Ekaterina Dolbunova, Andrey Mazurkevich, Elena Pranckenaite, Martin Hinz (eds.) Settling Waterscapes in Europe in Waterscapes Settling Settling Waterscapes in Europe in Europe Waterscapes Settling Pile dwellings have been explored over a vast The volume thus provides a current insight region for a number of decades now. This has into international research into life in and ar- led to the development of different ways, me- ound a vast array of prehistoric waterscapes. thods, and even schools of underwater and Extensive multidisciplinary research carried peat-bog excavation practices and data ana- out in recent years has provided new data with lysis techniques under the influence of differ- regard to the anthropogenic influence on the ent research traditions in individual countries. landscapes around Neolithic and Bronze Age These and other factors can limit our under- pile dwellings, which allows us to characterise standing of the past, whilst on the other hand in more detail the lifestyles of the settlements’ they can also open up further avenues of inter- inhabitants, the peculiarities of the ecological pretation. niche and the interaction between humans and their environment. The volume also contains By collecting the papers presented at the 2016 various case studies that demonstrate the im- session of the EAA in Vilnius, this book aims to portance of scientific analysis for the study of take this diversity as an opportunity. The geo- settlement between land and water. graphical scope extends from the Baltic to Russia, Belarus, Albania, North Macedonia, Bul- Overall, the volume presents an important new garia, Bosnia, Coratia, Greece, Germany, Austria body of data and international perspectives on and Switzerland to France. -
Oxygen Consumption in Seasonally Stratified Lakes Decreases Only
www.nature.com/scientificreports OPEN Oxygen consumption in seasonally stratifed lakes decreases only below a marginal phosphorus threshold Beat Müller 1*, Thomas Steinsberger 1, Robert Schwefel 2,3, René Gächter 1, Michael Sturm 1 & Alfred Wüest 1,2 Areal oxygen (O2) consumption in deeper layers of stratifed lakes and reservoirs depends on the amount of settling organic matter. As phosphorus (P) limits primary production in most lakes, protective and remediation eforts often seek to reduce P input. However, lower P concentrations do not always lead to lower O2 consumption rates. This study used a large hydrochemical dataset to show that hypolimnetic O2 consumption rates in seasonally stratifed European lakes remain consistently −2 −1 elevated within a narrow range (1.06 ± 0.08 g O2 m d ) as long as areal P supply (APS) exceeded 0.54 ± 0.06 g P m−2 during the productive season. APS consists of the sum of total P present in the productive top 15 m of the water column after winter mixing plus the load of total dissolved P imported during the stratifed season, normalized to the lake area. Only when APS sank below this threshold, the areal hypolimnetic mineralization rate (AHM) decreased in proportion to APS. Sediment trap material showed increasing carbon:phosphorus (C:P) ratios in settling particulate matter when APS declined. This suggests that a decreasing P load results in lower P concentration but not necessarily in lower AHM rates because the phytoplankton community is able to maintain maximum biomass production by counteracting the decreasing P supply by a more efcient P utilization. -
Supplement of Organic Carbon Mass Accumulation Rate Regulates the flux of Reduced Substances from the Sediments of Deep Lakes
Supplement of Biogeosciences, 14, 3275–3285, 2017 https://doi.org/10.5194/bg-14-3275-2017-supplement © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement of Organic carbon mass accumulation rate regulates the flux of reduced substances from the sediments of deep lakes Thomas Steinsberger et al. Correspondence to: Beat Müller ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 3.0 License. 1 2 Contents: 3 Table S1 : TOC-MAR and OC gross sedimentation data from four lakes page S-1 4 Table S2 : Fred and TOC MAR values of six selected lakes page S-1 5 Figure S1 : Porewater profiles from Lake Zug page S-2 6 Figure S2 : Seasonal development of O2 concentration page S-3 7 8 9 Table S1: Average fluxes of TOC MAR, TOC gross sedimentation and the corresponding OC burial efficiency based on sediment trap data. TOC MAR at deepest Benthic gross OC burial Monitoring duration, Sampling Lake point sedimentation ref effiency % month-year interval gC m-2 yr-1 gC m-2 yr-1 Lake 49.83 45.62 91.56 4-2013 to 11-2014 2 weeks Baldegg Lake Aegeri 77.45 22.77 29.40 3-2014 to 12-2014 2 weeks Lake Hallwil 41.59 22.51 54.12 1-2014 to 12-2014 monthly Lake Rene Gächter 45.96 28.00 60.92 1-1984 to 12-1992 varying Sempach unpublished 10 11 12 Table S2: Characteristics of three eutrophic, one mesotrophic, and two oligotrophic lakes. -
Hypolimnetic Oxygen Depletion Rates in Deep Lakes: Effects of Trophic State and Organic Matter Accumulation
Limnol. Oceanogr. 65, 2020, 3128–3138 © 2020 The Authors. Limnology and Oceanography published by Wiley Periodicals LLC on behalf of Association for the Sciences of Limnology and Oceanography. doi: 10.1002/lno.11578 Hypolimnetic oxygen depletion rates in deep lakes: Effects of trophic state and organic matter accumulation Thomas Steinsberger ,1 Robert Schwefel ,2,3 Alfred Wüest ,1,3 Beat Müller 1* 1Eawag, Swiss Federal Institute of Aquatic Science and Technology, Kastanienbaum, Switzerland 2UC Santa Barbara, Santa Barbara, California 3Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, École Polytechnique Fédérale de Lausanne, Institute of Environmental Engineering, Lausanne, Switzerland Abstract This study investigated the consumption of oxygen (O2) in 11 European lakes ranging from 48 m to 372 m deep. In lakes less than ~ 100 m deep, the main pathways for O2 consumption were organic matter (OM) mineralization at the sediment surface and oxidation of reduced compounds diffusing up from the sedi- ment. In deeper lakes, mineralization of OM transported through the water column to the sediment represented a greater proportion of O2 consumption. This process predominated in the most productive lakes but declined with decreasing total phosphorous (TP) concentrations and hence primary production, when TP concentrations − fell below a threshold value of ~ 10 mg P m 3. Oxygen uptake by the sediment and the flux of reduced com- − − pounds from the sediment in these deep lakes were 7.9–10.6 and 0.6–3.6 mmol m 2 d 1, respectively. These parameters did not depend on the lake’s trophic state but did depend on sedimentation rates for the primarily allochthonous or already degraded OM.