Causes and Effects of Eutrophication in the Black Sea
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Probing the Changing Redfield Ratio of Phytoplankton
Probing the Changing Redfield Ratio of phytoplankton Supervisory Team Rosalind Rickaby www.earth.ox.ac.uk/people/rosalind-rickaby Katsumi Matsumoto www.esci.umn.edu/people/katsumi-matsumoto Key Research Question What controls the Redfield Ratio amongst algae? Overview under different conditions of Fe and C availability In 1934, Alfred Redfield made the notable to test the hypothesis that it is the nutrient observation that the relative ratios of C:N:P of efficiency of photosynthesis that dictates the C:N organic matter appeared to be constant throughout ratio of organic matter. the surface oceans, and also matched the Applicants would ideally have a background in dissolved ratios of those nutrients (C106N16P1). Biology/Chemistry/Earth Sciences or The Redfield ratio is fundamental in dictating the Environmental Sciences. strength of the biological sequestration of carbon, and the amount of oxygen that is used for respiration hence is an intimate control on the biotic feedback of phytoplankton on future climate. Despite efforts to understand the co-evolution of Methodology these ratios between the phytoplankton and the Methods to be used will include: Phytoplankton seawater from experimental, field observations Culture and sterile techniques, EA IRMS, and modelling efforts, there is still no mechanistic Spectrophotometry, and Microscopy. understanding of what drives the enormous variability seen across different phytoplankton lineages with various environmental conditions (Garcia et al., 2018). References & Further Reading Nature Geoscience -
Early Anthropogenic Transformation of the Danube-Black Sea System SUBJECT AREAS: Liviu Giosan1, Marco J
Early Anthropogenic Transformation of the Danube-Black Sea System SUBJECT AREAS: Liviu Giosan1, Marco J. L. Coolen2, Jed O. Kaplan3, Stefan Constantinescu4, Florin Filip4, EARTH SCIENCES Mariana Filipova-Marinova5, Albert J. Kettner6 & Nick Thom7 CLIMATE CHANGE OCEANOGRAPHY 1Geology & Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA, 2Marine Chemistry & BIODIVERSITY Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA, 3ARVE Group, Ecole Polytechnique Fe´de´rale de Lausanne, 1015 Lausanne, Switzerland, 4Department of Geography, University of Bucharest, Bucharest, 70709, Romania, 5Museum of Natural History, 9000 Varna, Bulgaria, 6Institute of Arctic and Alpine Research, University of Colorado, Received Boulder, CO 80309-0450, USA, 7Faculty of Engineering, University of Nottingham, Nottingham, NG7 2RD, UK. 22 March 2012 Accepted Over the last century humans have altered the export of fluvial materials leading to significant changes in 1 August 2012 morphology, chemistry, and biology of the coastal ocean. Here we present sedimentary, paleoenvironmental Published and paleogenetic evidence to show that the Black Sea, a nearly enclosed marine basin, was affected by land use long before the changes of the Industrial Era. Although watershed hydroclimate was spatially and 30 August 2012 temporally variable over the last ,3000 years, surface salinity dropped systematically in the Black Sea. Sediment loads delivered by Danube River, the main tributary of the Black Sea, significantly increased as land use intensified in the last two millennia, which led to a rapid expansion of its delta. Lastly, proliferation Correspondence and of diatoms and dinoflagellates over the last five to six centuries, when intensive deforestation occurred in requests for materials Eastern Europe, points to an anthropogenic pulse of river-borne nutrients that radically transformed the should be addressed to food web structure in the Black Sea. -
Nitrogen and Phosphorus Inputs to the Black Sea in 1970–2050
Reg Environ Change (2013) 13:179–192 DOI 10.1007/s10113-012-0328-z ORIGINAL ARTICLE Nitrogen and phosphorus inputs to the Black Sea in 1970–2050 Maryna Strokal • Carolien Kroeze Received: 18 June 2011 / Accepted: 13 June 2012 / Published online: 29 June 2012 Ó The Author(s) 2012. This article is published with open access at Springerlink.com Abstract Increased nitrogen (N) and phosphorus Introduction (P) inputs are major causes of eutrophication in the coastal waters of the Black Sea. The objective of this study is to Eutrophication has been a serious problem in the Black Sea analyze the past and future trends in river export of nitrogen since the 1970s (Borysova et al. 2005; Tokarev and Shul- and phosphorus to the coastal waters of the Black Sea and to man 2007; McGinley 2008; Zaitsev and Mamaev 1997; assess the associated potential for coastal eutrophication. Yunev et al. 2007; BSC 2008, 2009). This eutrophication is The Global NEWS-2 (Nutrient Export from WaterSheds) caused by increased nitrogen (N) and phosphorus (P) inputs model was used for this purpose. Currently, most eutro- to the sea, as a result of human activities on the land. In phication occurs in the North Black Sea and the Azov Sea. particular, the rapid growth of fertilizer and manure In the future, however, this may change. We analyzed applications in agriculture contributed to this, as well as trends up to 2050 on the basis of the Millennium Ecosystem changes in land use and poor wastewater treatment (Bo- Assessment (MEA) scenarios. The results indicate that rysova et al. -
Surface Runoff to the Black Sea from the East European Plain During Last Glacial Maximum–Late Glacial Time
Downloaded from specialpapers.gsapubs.org on September 18, 2012 The Geological Society of America Special Paper 473 2011 Surface runoff to the Black Sea from the East European Plain during Last Glacial Maximum–Late Glacial time Aleksey Yu. Sidorchuk Andrey V. Panin Geographical Faculty, Moscow State University, Vorob’evy Gory, Moscow 119991, Russia Olga K. Borisova Institute of Geography, Russian Academy of Sciences, Staromonetny per., Moscow 119017, Russia ABSTRACT Hydromorphological and hydroclimatic methods were used to reconstruct the former surface runoff from the East European part of the Black Sea drainage basin. Data on the shape and dynamics of the last Fennoscandian ice sheet were used to cal- culate meltwater supply to the headwaters of the Dnieper River. The channel width and meander wavelength of well-preserved fragments of large paleochannels were measured at 51 locations in the Dnieper and Don River basins (East European Plain), which allowed reconstruction of the former surface runoff of the ancient rivers, as well as the total volume of fl ow into the Black Sea, using transform functions. Studies of the composition of fossil fl oras derived from radiocarbon-dated sediments of vari- ous origins and ages make it possible to locate their modern region analogues. These analogues provide climatic and hydrological indexes for the Late Pleniglacial and Late Glacial landscapes. Morphological, geological, geochronological, and palyno- logical studies show that the landscape, climatic, and hydrologic history of the region included: -
Ch. 9: Ocean Biogeochemistry
6/3/13 Ch. 9: Ocean Biogeochemistry NOAA photo gallery Overview • The Big Picture • Ocean Circulation • Seawater Composition • Marine NPP • Particle Flux: The Biological Pump • Carbon Cycling • Nutrient Cycling • Time Pemitting: Hydrothermal venting, Sulfur cycling, Sedimentary record, El Niño • Putting It All Together Slides borrowed from Aradhna Tripati 1 6/3/13 Ocean Circulation • Upper Ocean is wind-driven and well mixed • Surface Currents deflected towards the poles by land. • Coriolis force deflects currents away from the wind, forming mid-ocean gyres • Circulation moves heat poleward • River influx is to surface ocean • Atmospheric equilibrium is with surface ocean • Primary productivity is in the surface ocean Surface Currents 2 6/3/13 Deep Ocean Circulation • Deep and Surface Oceans separated by density gradient caused by differences in Temperature and Salinity • This drives thermohaline deep circulation: * Ice forms in the N. Atlantic and Southern Ocean, leaving behind cold, saline water which sinks * Oldest water is in N. Pacific * Distribution of dissolved gases and nutrients: N, P, CO2 Seawater Composition • Salinity is defined as grams of salt/kg seawater, or parts per thousand: %o • Major ions are in approximately constant concentrations everywhere in the oceans • Salts enter in river water, and are removed by porewater burial, sea spray and evaporites (Na, Cl). • Calcium and Sulfate are removed in biogenic sediments • Magnesium is consumed in hydrothermal vents, in ionic exchange for Ca in rock. • Potassium adsorbs in clays. 3 6/3/13 Major Ions in Seawater The Two-Box Model of the Ocean Precipitation Evaporation River Flow Upwelling Downwelling Particle Flux Sedimentation 4 6/3/13 Residence time vs. -
Black Sea Environment Programme
Annex 1 PROJECT BRIEF 1. IDENTIFIERS PROJECT NUMBER : PROJECT NAME: GEF Strategic Partnership on the Danube/Black Sea Basin, Element 1 - Regional (Bulgaria, Romania, Georgia, Russian Federation, Turkey, Ukraine): Control Of Eutrophication, Hazardous Substances And Related Measures For Rehabilitating The Black Sea Ecosystem: Phase 1 PROJECT DURATION: 2 Years (followed by 3 year Phase 2) IMPLEMENTING AGENCY: UNDP, in association with UNEP and the World Bank EXECUTING AGENCY: UNOPS REQUESTING COUNTRIES : Bulgaria, Romania, Georgia, Russian Federation, Turkey and Ukraine ELIGIBILITY: Eligible under para. 9(b) of GEF Instrument GEF FOCAL AREA: International Waters GEF PROGRAMMING OP#8: Waterbody-Based Operational Program FRAMEWORK SUMMARY The long-term objective of the project is to assist the beneficiary countries to take measures to reduce nutrient levels and other hazardous substances to such levels necessary to permit Black Sea ecosystems to recover to similar conditions as those observed in the 1960s. This will be achieved through a process of adaptive management in which agreed common targets are pursued throughout the 17 country Black Sea Basin. The present project will assist the coastal countries to meet the agreed first target (maintenance of nutrient loads at their 1997 levels) and to set the subsequent target using the best available scientific information coupled with benefit/cost studies and political pragmatism. The current project will also help to reduce fisheries pressure on sensitive habitats and contribute towards rational -
Marine Microorganisms and Global Nutrient Cycles Kevin R
03 Arrigo 15-21 6/9/05 11:17 AM Page 15 NATURE|Vol 437|15 September 2005|doi:10.1038/nature04158 INSIGHT REVIEW Marine microorganisms and global nutrient cycles Kevin R. Arrigo1 The way that nutrients cycle through atmospheric, terrestrial, oceanic and associated biotic reservoirs can constrain rates of biological production and help structure ecosystems on land and in the sea. On a global scale, cycling of nutrients also affects the concentration of atmospheric carbon dioxide. Because of their capacity for rapid growth, marine microorganisms are a major component of global nutrient cycles. Understanding what controls their distributions and their diverse suite of nutrient transformations is a major challenge facing contemporary biological oceanographers. What is emerging is an appreciation of the previously unknown degree of complexity within the marine microbial community. To understand how carbon and nutrients, such as nitrogen and phos- through the activities of marine phytoplankton. phorus, cycle through the atmosphere, land and oceans, we need a Unfortunately, a clear mechanism explaining the observed magni- clearer picture of the underlying processes. This is particularly impor- tude of the Redfield C:N:P ratio of 106:16:1 for either phytoplankton tant in the face of increasing anthropogenic nutrient release and or the deep ocean has been elusive. It has long been recognized that climate change. Marine microbes, which are responsible for approxi- conditions exist under which phytoplankton stoichiometry diverges mately half of the -
Chapter 13 Lecture
ChapterChapter 1 13 Clickers Lecture Essentials of Oceanography Eleventh Edition Biological Productivity and Energy Transfer Alan P. Trujillo Harold V. Thurman © 2014 Pearson Education, Inc. Chapter Overview • Primary productivity is photosynthesis. • Productivity is globally and seasonally variable. • Feeding relationships are represented by food chains and food webs. • Oceans are being overfished. © 2014 Pearson Education, Inc. Primary Productivity • Rate at which energy is stored in organic matter – Photosynthesis uses solar radiation. – Chemosynthesis uses chemical reactions. • 99.9% of the ocean’s biomass relies directly or indirectly on photosynthesis for food. © 2014 Pearson Education, Inc. Photosynthesis © 2014 Pearson Education, Inc. Measurement of Primary Productivity • Directly – capture plankton in plankton nets • Measure radioactive carbon in seawater © 2014 Pearson Education, Inc. Measurement of Primary Productivity • Monitor ocean color with satellites – Photosynthetic phytoplankton use green pigment chlorophyll • SeaWiFS (Sea-viewing Wide Field of View Sensor) satellite sensor collected ocean color data 1997–2010 • MODIS (Moderate Resolution Imaging Spectroradiometer) – current – Measures 36 spectral frequencies © 2014 Pearson Education, Inc. Factors Affecting Primary Productivity • Nutrient availability – Nitrate, phosphorous, iron, silica – Most from river runoff – Productivity high along continental margins – Redfield ratio – C:N:P © 2014 Pearson Education, Inc. Factors Affecting Primary Productivity • Solar radiation – Uppermost surface seawater and shallow seafloor – Compensation depth – net photosynthesis becomes zero – Euphotic zone —from surface to about 100 meters (330 feet) • Enough light for photosynthesis © 2014 Pearson Education, Inc. Light Transmission in Ocean Water • Visible light portion of the electromagnetic spectrum • Blue wavelengths penetrate deepest • Longer wavelengths (red, orange) absorbed first © 2014 Pearson Education, Inc. Transmission of Light in Seawater © 2014 Pearson Education, Inc. -
Introduction to Marine Primary Productivity and Carbon Cycle
Introduction to marine primary productivity and carbon cycle Satya Prakash [email protected] 400 Law Dome Ice Core, Antarctica 380 Mauna Loa, Hawaii Slope: 360 1970 - 1979: 1.3 ppm y-1 -1 340 2000 - 2006: 1.9 ppm y 320 Concentration (ppm) 2 CO 300 280 1820 1840 1860 1880 1900 1920 1940 1960 1980 2000 2020 Year CO2 – Temperature Relationship CO2 Concentration Temperature 380 4 2 340 0 300 -2 (ppmv) 2 260 -4 Degree C Degree CO -6 220 -8 180 -10 0 50 100 150 200 250 300 350 400 450 Age (Kyr) VOSTOK Ice Core data How much is 100 ppm?? 1 ppm = 2.12 * 1015 gm = 2.12*109 tonnes 100 ppm = 2.12 thousand crore tonnes 1m. 1m. = 1000 kg = 2.44 टन 1m. CO2 1m. Water or one tonne 1m. 1m. Partition of Anthropogenic Carbon Emissions into Sinks [2000-2006] 45% of all CO2 emissions accumulated in the atmosphere 55% were removed by natural sinks Ocean removes ~ 24% Land removes ~ 30% Upper Photic Layer Photosynthesis O2 O2 CO2 CO2 Respiration Deeper Aphotic Layer The Ocean Euphotic zone light - ~little N Aphotic zone no light - lots N Photosynthesis is a process that generates the organic matter in phytoplankton cells. The process of photosynthesis can be represented as: hv 106CO2 + 122H2O + 16HNO3 + H3PO4 (CH2O)106(NH3)16H3PO4 + 138O2 Available solar energy in the waveband 400-700 nm. This reaction illustrates the need for the nutrients: nitrate and phosphate. It also shows that for every 106 CO2 molecules taken up, approximately 138 O2 molecules are produced. -
A Review of the Methods and Metrics in Research, Implementation, and Management of Integrated Multi-Trophic Aquaculture
The University of San Francisco USF Scholarship: a digital repository @ Gleeson Library | Geschke Center Master's Projects and Capstones Theses, Dissertations, Capstones and Projects Spring 5-14-2020 A Review of the Methods and Metrics in Research, Implementation, and Management of Integrated Multi-Trophic Aquaculture Cassandra Erickson [email protected] Follow this and additional works at: https://repository.usfca.edu/capstone Part of the Sustainability Commons, and the Water Resource Management Commons Recommended Citation Erickson, Cassandra, "A Review of the Methods and Metrics in Research, Implementation, and Management of Integrated Multi-Trophic Aquaculture" (2020). Master's Projects and Capstones. 1028. https://repository.usfca.edu/capstone/1028 This Project/Capstone is brought to you for free and open access by the Theses, Dissertations, Capstones and Projects at USF Scholarship: a digital repository @ Gleeson Library | Geschke Center. It has been accepted for inclusion in Master's Projects and Capstones by an authorized administrator of USF Scholarship: a digital repository @ Gleeson Library | Geschke Center. For more information, please contact [email protected]. This Master’s Project A Review of Methods and Metrics in Research, Implementation, and Management of Integrated Multi-Trophic Aquaculture By: Cassandra Erickson is submitted in partial fulfillment of the requirements for the degree of Master of Science in Environmental Management at the University of San Francisco Submitted: Received: .................................................. -
EBRD 9571 Project Document
DOCUMENT OF THE EUROPEAN BANK FOR RECONSTRUCTION AND DEVELOPMENT REGIONAL EBRD and Global Environment Facility Promoting accelerated uptake of environmental technologies and promotion of best practices for improved water, chemicals and waste management in the Black Sea Basin Project Document 30 May 2019 This document has a restricted distribution and may be used by the recipients only in the performance of their official duties. Its contents may not otherwise be disclosed without the Bank's authorisation. Black Sea Basin: Project Document Table of Contents List of figures ......................................................................................................................................... ii List of tables........................................................................................................................................... ii Abbreviations and acronyms .............................................................................................................. iii Executive summary ............................................................................................................................... v 1 Context ........................................................................................................................................... 1 1.1 Overview of the EBRD region ............................................................................................................ 1 1.2 Overview of the Black Sea Basin ...................................................................................................... -
The Elements of Marine Life Noah J
commentary most direct effect of human activity on the whether they do so through phenotypic Nicolas Gruber is in the Environmental oceanic N cycle is the massive application or genotypic changes. Clear latitudinal Physics group, Institute of Biogeochemistry and of fertilizers full of bioavailable N, much trends in the N:P ratio of phytoplankton Pollutant Dynamics, ETH Zürich, 8092 Zürich, of which makes its way to the ocean communities have been found14,15. It Switzerland. Curtis A. Deutsch is at the School of either via rivers or through long-range remains to be seen whether the shifting Oceanography, University of Washington, Seattle, atmospheric transport13. boundaries of major ocean biomes can Washington 98195, USA. Currently, we can only speculate alter the large-scale patterns of plankton e-mail: [email protected] about how these perturbations, and their N:P ratios, and how that would modify the interactions, will alter the marine nitrogen stabilizing feedbacks. References cycle and affect its homeostasis. Given Redfield’s pioneering view of the 1. Redfield, A. C. in James Johnston Memorial Volume that most stabilizing feedbacks operate ocean as a system capable of homeostatic (ed. Daniel, R. J.) 176–192 (Univ. Press of Liverpool, 1934). 2. Redfield, A. C. Am. Sci. 46, 205–221 (1958). on timescales of decades and longer, it is regulation helped pave the way for the 3. Deutsch, C., Sigman, D. M., Thunell, R. C., Meckler, A. N. & likely that we will see widespread temporal broader and now commonplace recognition Haug, G. H. Glob. Biogeochem. Cycles 18, GB4012 (2004). imbalances in the marine nitrogen cycle.