Ocean Deoxygenation: Everyone’S Problem Causes, Impacts, Consequences and Solutions Summary for Policy Makers
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Biogeochemistry of Mediterranean Wetlands: a Review About the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions
water Review Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions Inmaculada de Vicente 1,2 1 Departamento de Ecología, Universidad de Granada, 18071 Granada, Spain; [email protected]; Tel.: +34-95-824-9768 2 Instituto del Agua, Universidad de Granada, 18071 Granada, Spain Abstract: Although Mediterranean wetlands are characterized by extreme natural water level fluctu- ations in response to irregular precipitation patterns, global climate change is expected to amplify this pattern by shortening precipitation seasons and increasing the incidence of summer droughts in this area. As a consequence, a part of the lake sediment will be exposed to air-drying in dry years when the water table becomes low. This periodic sediment exposure to dry/wet cycles will likely affect biogeochemical processes. Unexpectedly, to date, few studies are focused on assessing the effects of water level fluctuations on the biogeochemistry of these ecosystems. In this review, we investigate the potential impacts of water level fluctuations on phosphorus dynamics and on greenhouse gases emissions in Mediterranean wetlands. Major drivers of global change, and specially water level fluctuations, will lead to the degradation of water quality in Mediterranean wetlands by increasing the availability of phosphorus concentration in the water column upon rewetting of dry sediment. CO2 fluxes are likely to be enhanced during desiccation, while inundation is likely to decrease cumulative CO emissions, as well as N O emissions, although increasing CH emissions. Citation: de Vicente, I. 2 2 4 Biogeochemistry of Mediterranean However, there exists a complete gap of knowledge about the net effect of water level fluctuations Wetlands: A Review about the Effects induced by global change on greenhouse gases emission. -
8.4 the Significance of Ocean Deoxygenation for Continental Margin Mesopelagic Communities J
8.4 The significance of ocean deoxygenation for continental margin mesopelagic communities J. Anthony Koslow 8.4 The significance of ocean deoxygenation for continental margin mesopelagic communities J. Anthony Koslow Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia and Scripps Institution of Oceanography, University of California, SD, La Jolla, CA 92093 USA. Email: [email protected] Summary • Global climate models predict global warming will lead to declines in midwater oxygen concentrations, with greatest impact in regions of oxygen minimum zones (OMZ) along continental margins. Time series from these regions indicate that there have been significant changes in oxygen concentration, with evidence of both decadal variability and a secular declining trend in recent decades. The areal extent and volume of hypoxic and suboxic waters have increased substantially in recent decades with significant shoaling of hypoxic boundary layers along continental margins. • The mesopelagic communities in OMZ regions are unique, with the fauna noted for their adaptations to hypoxic and suboxic environments. However, mesopelagic faunas differ considerably, such that deoxygenation and warming could lead to the increased dominance of subtropical and tropical faunas most highly adapted to OMZ conditions. • Denitrifying bacteria within the suboxic zones of the ocean’s OMZs account for about a third of the ocean’s loss of fixed nitrogen. Denitrification in the eastern tropical Pacific has varied by about a factor of 4 over the past 50 years, about half due to variation in the volume of suboxic waters in the Pacific. Continued long- term deoxygenation could lead to decreased nutrient content and hence decreased ocean productivity and decreased ocean uptake of carbon dioxide (CO2). -
The Potential of Mangroves in the Treatment of Shrimp Aquaculture Effluent on the Eastern Coast of Thailand
The Potential of Mangroves in the Treatment of Shrimp Aquaculture Effluent on the Eastern Coast of Thailand 7 Nina Fancy B. Sc.(Horn), Queen's University, 1999 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the Department of Geography O Nina Fancy, 2004 University of Victoria AII rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. Supervisor: Dr. Mark Flaherty ABSTRACT This thesis examines the potential of low-cost, low-maintenance mangroves in the treatment of nutrient-rich effluent originating from a shnmp fmon the coast of Thailand's Chanthaburi province. The objective of this thesis is to identify the environmental impact of shnmp aquaculture effluent and to determine if mangrove wetlands can be used as effective biofiltration areas to remove significant quantities of nitrate, ammonia and nitrite from shrimp wastewater. The study mangrove was found to remove an average of 44.5% of nitrate, 46.6% of ammonia and 59.0% of nitrite from shrimp effluent. The ratio of mangrove treatment area to shrimp fmrequired to adequately treat daily effluxes of wastewater from shrimp fmswas calculated to . be 1: 14. This ratio is significantly less spatially demanding than ratios calculated by .-: P 0 previous researchers and reveals the potential of mangroves to be used as large-scale wastewater treatment areas in shrimp-producing nations. TABLE OF CONTENTS .. ABSTRACT ..............................................................................................................11 -
Issues Brief: Ocean Deoxygenation
DECEMBER 2019 OCEAN DEOXYGENATION • The oxygen content of the ocean has declined by around 2% since the middle of the 20th century overall, while the volume of ocean waters completely depleted of oxygen has quadrupled since the 1960s. • Ocean oxygen levels are expected to fall on average by 3–4% by 2100 overall due to climate change and increased nutrient discharges, though the scale of effect seen will vary regionally. • Consequences of ocean oxygen decline include decreased biodiversity, shifts in species distributions, displacement or reduction in fishery resources and expanding algal blooms. • Ocean deoxygenation threatens to disrupt the ocean’s food provisioning ecosystem services. • To slow and reverse the loss of oxygen, humans must urgently mitigate climate change globally and nutrient pollution locally. What is the issue? conditions. In 2011 there were around 700 reported sites worldwide affected by low oxygen conditions – Globally, oceans have lost around 2% of dissolved up from only 45 before the 1960s. The volume of oxygen since the 1950s and are expected to lose anoxic ocean waters – areas completely depleted of about 3–4% by the year 2100 under a business-as- oxygen – has quadrupled since the 1960s. Evidence usual scenario (Representative Concentration suggests that temperature increases explain about Pathway 8.5), though the scale of effect is predicted 50% of oxygen loss in the upper 1000 m of the to vary regionally. Much of the oxygen loss is ocean. concentrated in the upper 1000m where species richness and abundance is highest. Even slight overall reductions in the levels of oxygen dissolved in the oceans can induce oxygen stress in marine organisms by depriving them of an adequate oxygen supply at the tissue level (termed hypoxia). -
Metaproteomics Reveals Differential Modes of Metabolic Coupling Among Ubiquitous Oxygen Minimum Zone Microbes
Metaproteomics reveals differential modes of metabolic coupling among ubiquitous oxygen minimum zone microbes Alyse K. Hawleya, Heather M. Brewerb, Angela D. Norbeckb, Ljiljana Paša-Tolicb, and Steven J. Hallama,c,d,1 aDepartment of Microbiology and Immunology, cGraduate Program in Bioinformatics, and dGenome Sciences and Technology Training Program, University of British Columbia, Vancouver, BC, Canada V6T 1Z3; and bBiological and Computational Sciences Division, Pacific Northwest National Laboratory, Richland, WA 99352 Edited by Edward F. DeLong, Massachusetts Institute of Technology, Cambridge, MA, and approved June 10, 2014 (received for review November 26, 2013) Marine oxygen minimum zones (OMZs) are intrinsic water column transformations in nonsulfidic OMZs, providing evidence for features arising from respiratory oxygen demand during organic a cryptic sulfur cycle with the potential to drive inorganic carbon matter degradation in stratified waters. Currently OMZs are expand- fixation processes (13). Indeed, many of the key microbial players ing due to global climate change with resulting feedback on marine implicated in nitrogen and sulfur transformations in OMZs, in- ecosystem function. Here we use metaproteomics to chart spatial cluding Thaumarchaeota, Nitrospina, Nitrospira, Planctomycetes, and temporal patterns of gene expression along defined redox and SUP05/ARCTIC96BD-19 Gammaproteobacteria have the gradients in a seasonally stratified fjord to better understand metabolic potential for inorganic carbon fixation (14–19), and -
Linking Biodiversity Above and Below the Marine Sediment–Water Interface
Articles Linking Biodiversity Above and Below the Marine Sediment–Water Interface PAUL V. R. SNELGROVE, MELANIE C. AUSTEN, GUY BOUCHER, CARLO HEIP, PATRICIA A. HUTCHINGS, GARY M. KING, ISAO KOIKE, P. JOHN D. LAMBSHEAD, AND CRAIG R. SMITH hanges in the marine environment are evident on Ca global scale (McGowan et al. 1998), and although bio- THE ORGANISMS LIVING ON THE OCEAN diversity in the oceans is poorly described, abundances and FLOOR ARE LINKED TO THOSE LIVING IN distributions of both commercially exploited (Safina 1998) and nonexploited (Pearson and Rosenberg 1978) species have THE OCEAN ABOVE, BUT WHETHER OR changed. Not only have major changes occurred but the rate of alteration of marine ecosystems appears to be accelerating HOW THE BIODIVERSITY IN THESE TWO (e.g., Cohen and Carlton 1998). Unfortunately, the impact of these changes in biodiversity on the basic functioning of ma- REALMS IS LINKED REMAINS LARGELY rine ecosystems remains uncertain, as does the oceans’ capacity UNKNOWN to withstand multiple human disturbances (Snelgrove et al. 1997). The dynamics of many marine ecosystems, as well as of important fisheries, depend on close coupling between benthic (bottom living) and pelagic (water column) organ- The sediment–water interface (SWI) in marine ecosystems isms (Steele 1974). Our knowledge of the natural history of is one of the most clearly defined ecological boundaries on these systems remains limited, and scientific interest in map- Earth. Many organisms in the water column, such as salps ping the diversity of organisms and how they live has been and jellyfish, have flimsy and attenuated morphologies that marginalized in recent years. -
Mixing Between Oxic and Anoxic Waters of the Black Sea As Traced by Chernobyl Cesium Isotopes
Deep-Sea Research, Vol 38. Suppl 2. pp S72>-S745. 1991. 019~149191 53.00 + 0.00 Pnnted 10 Great Bntam © 1991Pergamon Press pic Mixing between oxic and anoxic waters of the Black Sea as traced by Chernobyl cesium isotopes KEN O. BUESSELER, * HUGH D. LIVINGSTON* and SUSAN A. CASSO* (Received 14 August 1989; in revised form 16 November 1990; accepted 28 November 1990) Abstract-The Chernobyl nuclear power station accident in 1986 released readily measureable quantities of fallout 134CS and 137Cs to Black Sea surface waters. This pulse-like input of tracers can be used to follow the physical mixing of the surface oxic waters, now labeled with the Chemobyl tracers, and the deeper anoxic waters, which were initially Chemobyl free. By 1988, there is clear evidence of Chernobyl Cs penetration below the oxic/anoxic interface at deep water stations in the western and eastern basins of the Black Sea. This rapid penetration of surface waters across the pycnocline cannot be explained by vertical mixing processes alone. Data from profiles at the mouth of the Bosporus suggest that significant ventilation of intermediate depths can occur as the outflowmg Black Sea waters are entrained with the inflowing Mediterranean waters, forming a sub-surface water mass which is recognized by its surface water characteristics, i.e. initially a relatively high oxygen content and Chernobyl Cs signal. The lateral propagation ofthis signal along isopycnals into the basin interior would provide a rapid and effective mechanism for ventilating intermediate depths of the Black Sea. This process could also account for the lateral injection of resuspended margin sediments into the basin interior. -
Climate-Driven Deoxygenation Elevates Fishing Vulnerability for The
RESEARCH ARTICLE Climate-driven deoxygenation elevates fishing vulnerability for the ocean’s widest ranging shark Marisa Vedor1,2, Nuno Queiroz1,3†*, Gonzalo Mucientes1,4, Ana Couto1, Ivo da Costa1, Anto´ nio dos Santos1, Frederic Vandeperre5,6,7, Jorge Fontes5,7, Pedro Afonso5,7, Rui Rosa2, Nicolas E Humphries3, David W Sims3,8,9†* 1CIBIO/InBIO, Universidade do Porto, Campus Agra´rio de Vaira˜ o, Vaira˜ o, Portugal; 2MARE, Laborato´rio Marı´timo da Guia, Faculdade de Cieˆncias da Universidade de Lisboa, Av. Nossa Senhora do Cabo, Cascais, Portugal; 3Marine Biological Association of the United Kingdom, The Laboratory, Citadel Hill, Plymouth, United Kingdom; 4Instituto de Investigaciones Marinas, Consejo Superior de Investigaciones Cientı´ficas (IIM-CSIC), Vigo, Spain; 5IMAR – Institute of Marine Research, Departamento de Oceanografia e Pescas, Universidade dos Ac¸ores, Horta, Portugal; 6MARE – Marine and Environmental Sciences Centre, Faculdade de Cieˆncias da Universidade de Lisboa, Lisbon, Portugal; 7Okeanos - Departamento de Oceanografia e Pescas, Universidade dos Ac¸ores, Horta, Portugal; 8Centre for Biological Sciences, Highfield Campus, University of Southampton, Southampton, United Kingdom; 9Ocean and Earth Science, National Oceanography Centre Southampton, Waterfront Campus, University of Southampton, Southampton, United Kingdom *For correspondence: [email protected] (NQ); Abstract Climate-driven expansions of ocean hypoxic zones are predicted to concentrate [email protected] (DWS) pelagic fish in oxygenated surface layers, but how expanding hypoxia and fisheries will interact to affect threatened pelagic sharks remains unknown. Here, analysis of satellite-tracked blue sharks †These authors contributed equally to this work and environmental modelling in the eastern tropical Atlantic oxygen minimum zone (OMZ) shows shark maximum dive depths decreased due to combined effects of decreasing dissolved oxygen Competing interests: The (DO) at depth, high sea surface temperatures, and increased surface-layer net primary production. -
Ocean Deoxygenation and Copepods: Coping with Oxygen Minimum Zone Variability
Biogeosciences, 17, 2315–2339, 2020 https://doi.org/10.5194/bg-17-2315-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Ocean deoxygenation and copepods: coping with oxygen minimum zone variability Karen F. Wishner1, Brad Seibel2, and Dawn Outram1 1Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA 2College of Marine Science, University of South Florida, St. Petersburg, FL 33701, USA Correspondence: Karen F. Wishner ([email protected]) Received: 27 September 2019 – Discussion started: 28 October 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 24 April 2020 Abstract. Increasing deoxygenation (loss of oxygen) of compression concept). These distribution depths changed by the ocean, including expansion of oxygen minimum zones tens to hundreds of meters depending on the species, oxygen (OMZs), is a potentially important consequence of global profile, and phenomenon. For example, at the lower oxycline, warming. We examined present-day variability of vertical the depth of maximum abundance for Lucicutia hulsemannae distributions of 23 calanoid copepod species in the East- shifted from ∼ 600 to ∼ 800 m, and the depth of diapause for ern Tropical North Pacific (ETNP) living in locations with Eucalanus inermis shifted from ∼ 500 to ∼ 775 m, in an ex- different water column oxygen profiles and OMZ inten- panded OMZ compared to a thinner OMZ, but remained at sity (lowest oxygen concentration and its vertical extent in similar low oxygen levels in -
Ocean Circulation and Climate: an Overview
ocean-climate.org Bertrand Delorme Ocean Circulation and Yassir Eddebbar and Climate: an Overview Ocean circulation plays a central role in regulating climate and supporting marine life by transporting heat, carbon, oxygen, and nutrients throughout the world’s ocean. As human-emitted greenhouse gases continue to accumulate in the atmosphere, the Meridional Overturning Circulation (MOC) plays an increasingly important role in sequestering anthropogenic heat and carbon into the deep ocean, thus modulating the course of climate change. Anthropogenic warming, in turn, can influence global ocean circulation through enhancing ocean stratification by warming and freshening the high latitude upper oceans, rendering it an integral part in understanding and predicting climate over the 21st century. The interactions between the MOC and climate are poorly understood and underscore the need for enhanced observations, improved process understanding, and proper model representation of ocean circulation on several spatial and temporal scales. The ocean is in perpetual motion. Through its DRIVING MECHANISMS transport of heat, carbon, plankton, nutrients, and oxygen around the world, ocean circulation regulates Global ocean circulation can be divided into global climate and maintains primary productivity and two major components: i) the fast, wind-driven, marine ecosystems, with widespread implications upper ocean circulation, and ii) the slow, deep for global fisheries, tourism, and the shipping ocean circulation. These two components act industry. Surface and subsurface currents, upwelling, simultaneously to drive the MOC, the movement of downwelling, surface and internal waves, mixing, seawater across basins and depths. eddies, convection, and several other forms of motion act jointly to shape the observed circulation As the name suggests, the wind-driven circulation is of the world’s ocean. -
Scientific Assessment of Hypoxia in U.S. Coastal Waters
Scientific Assessment of Hypoxia in U.S. Coastal Waters 0 Dissolved oxygen (mg/L) 6 0 Depth (m) 80 32 Salinity 34 Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health September 2010 This document should be cited as follows: Committee on Environment and Natural Resources. 2010. Scientific Assessment of Hypoxia in U.S. Coastal Waters. Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health of the Joint Subcommittee on Ocean Science and Technology. Washington, DC. Acknowledgements: Many scientists and managers from Federal and state agencies, universities, and research institutions contributed to the knowledge base upon which this assessment depends. Many thanks to all who contributed to this report, and special thanks to John Wickham and Lynn Dancy of NOAA National Centers for Coastal Ocean Science for their editing work. Cover and Sidebar Photos: Background Cover and Sidebar: MODIS satellite image courtesy of the Ocean Biology Processing Group, NASA Goddard Space Flight Center. Cover inset photos from top: 1) CTD rosette, EPA Gulf Ecology Division; 2) CTD profile taken off the Washington coast, project funded by Bonneville Power Administration and NOAA Fisheries; Joseph Fisher, OSU, was chief scientist on the FV Frosti; data were processed and provided by Cheryl Morgan, OSU); 3) Dead fish, Christopher Deacutis, Rhode Island Department of Environmental Management; 4) Shrimp boat, EPA. Council on Environmental Quality Office of Science and Technology Policy Executive Office of the President Dear Partners and Friends in our Ocean and Coastal Community, We are pleased to transmit to you this report, Scientific Assessment ofHypoxia in u.s. -
Diversité Phylogénétique Et Fonctionnelle Des Eumycètes Dans Les Écosystèmes Pélagiques Marlène Jobard-Portas
Diversité phylogénétique et fonctionnelle des Eumycètes dans les écosystèmes pélagiques Marlène Jobard-Portas To cite this version: Marlène Jobard-Portas. Diversité phylogénétique et fonctionnelle des Eumycètes dans les écosystèmes pélagiques. Sciences agricoles. Université Blaise Pascal - Clermont-Ferrand II, 2010. Français. NNT : 2010CLF22090. tel-00769938 HAL Id: tel-00769938 https://tel.archives-ouvertes.fr/tel-00769938 Submitted on 4 Jan 2013 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. UNIVERSITE BLAISE PASCAL Année 2010 N°D.U. 2090 ECOLE DOCTORALE DES SCIENCES DE LA VIE, SANTE, AGRONOMIE, ENVIRONNEMENT N° d’ordre 535 Thèse Présentée à l’Université Blaise Pascal pour l’obtention du grade de DOCTEUR D’UNIVERSITE (Spécialité : Ecologie Microbienne) Soutenue le 14 Décembre 2010 Marlène JOBARD Diversité phylogénétique et fonctionnelle des Eumycètes dans les écosystèmes pélagiques Président : Pr Gilles Bourdier, Université Blaise Pascal, Clermont-Fd, France Invité Institutionnel : Dr Henry-Michel Cauchie, CRP, Belvaux, Luxembourg Directeur de