Effects of Ocean Acidification on Marine Biodiversity and Ecosystem Function

Total Page:16

File Type:pdf, Size:1020Kb

Effects of Ocean Acidification on Marine Biodiversity and Ecosystem Function University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Biological and Marine Sciences 2011-09-15 Effects of ocean acidification on marine biodiversity and ecosystem function Barry, JP http://hdl.handle.net/10026.1/1314 Oxford University Press All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. OUP CORRECTED PROOF – FINAL, 08/11/2011, SPi CHAPTER 10 Effects of ocean acidifi cation on marine biodiversity and ecosystem function J ames P . B arry, S tephen W iddicombe, and J ason M . H all- S pencer be diffi cult to detect amidst the variability associ- 10.1 Introduction ated with other human and non-human factors, and The biodiversity of the oceans, including the strik- the greatest impacts are expected to occur as acidifi - ing variation in life forms from microbes to whales cation intensifi es through this century. and ranging from surface waters to hadal trenches, In theory, large and rapid environmental changes forms a dynamic biological framework enabling the are expected to decrease the stability and produc- fl ow of energy that shapes and sustains marine eco- tivity of ecosystems due to a reduction in biodiver- systems. Society relies upon the biodiversity and sity caused by the loss of sensitive species that play function of marine systems for a wide range of serv- important roles in energy fl ow (i.e. food web func- ices as basic as producing the seafood we consume tion) or other processes (e.g. ecosystem engineers; or as essential as generating much of the oxygen we Cardinale et al. 2006 ). In practice, however, most breathe. Perhaps most obvious is the global seafood research concerning the biological effects of ocean harvest totalling over 100 Mt yr –1 (82 and 20 Mt in acidifi cation has focused on aspects of the perform- 2008 for capture and aquaculture, respectively; FAO ance and survival of individual species during 2009 ) from fi shing effort that expands more broadly short-term studies, assuming that a change in indi- and deeper each year as fi shery stocks are depleted vidual performance will infl uence ecosystem func- ( Pauly et al. 2003 ). Less apparent ecosystem services tion. By their nature, controlled experimental linked closely to biodiversity and ecosystem func- studies are limited in both space and time, and thus tion are waste processing and improved water may not capture important processes (e.g. acclima- quality, elemental cycling, shoreline protection, rec- tization and adaptation, multispecies biological reational opportunities, and aesthetic or educational interactions, chronic low-level impacts) that can experiences ( Cooley et al. 2009 ). ultimately play large roles in the response of marine There is growing concern that ocean acidifi cation systems to ocean acidifi cation. This ‘scaling up’ caused by fossil fuel emissions, in concert with the from individual- to ecosystem-level effects is the effects of other human activities, will cause signifi - most challenging goal for research on the potential cant changes in the biodiversity and function of effects of ocean acidifi cation. marine ecosystems, with important consequences To plan for the future, society needs information to for resources and services that are important to understand how ocean acidifi cation and other envi- society. Will the effects of ocean acidifi cation on eco- ronmental changes will affect fi sheries, aqua culture, systems be similar to those arising from other envi- and other services deriving from the effi cient func- ronmental perturbations observed during human tion of marine ecosystems. The infl ux of fossil fuel or earth history? Although changes in biodiversity CO2 into the upper ocean from the atmosphere is and ecosystem function due to ocean acidifi cation altering the chemistry of ocean waters at a faster have not yet been widely observed, their onset may rate and greater magnitude than is thought to have 192 OUP CORRECTED PROOF – FINAL, 08/11/2011, SPi EFFECTS OF ACIDIFICATION ON MARINE BIODIVERSITY AND ECOSYSTEMS 193 occurred on earth for at least a million years and per- tems in a region), or functional diversity (the number haps as much as 40 Myr ( Pelejero et al. 2010 ; see of functional roles performed by the species present) Chapter 2 ). In this chapter, the infl uence of this (see Fig. 10.1 ; Petchey and Gaston 2006 ). Biodiversity important change in ocean chemistry on the biodi- is a dynamic feature of natural systems, refl ecting versity and function of marine ecosystems is consid- the continual evolutionary response of species in a ered, from basic physiological responses of individual region to selection across a broad range of environ- organisms and species, to the potential changes in mental and ecological pressures. Biodiversity can various ocean environments. expand and contract as species diversity or other elements of biological diversity are created, main- 10.2 Biodiversity and ecosystem tained, or lost to extinction. function The function of ecosystems is wholly dependent on biodiversity that allows energy to fl ow through The term biodiversity is broadly defi ned, and used trophic webs and biological networks. Moreover, to characterize aspects of the biological complexity the stability and resilience of ecosystem functions, of natural systems. Often cast simply as the number from nutrient cycling and energy fl ow, to the of species in a region (i.e. species richness ), biodiver- population dynamics of species, are thought to be sity has a far larger scope that spans the variation sensitive to the loss of biodiversity caused by per- within and among systems and organisms over turbations of both human and non-human origin. multiple scales and levels of genetic, organismal, This concept has long been considered theoreti- ecological, or ecosystem diversity. Measures of bio- cally, with more diverse and trophically complex diversity attempt to estimate the richness and even- systems expected to be more stable and resistant ness of biological characteristics at different levels, to perturbations. Species complementarity (different such as species richness and species diversity (the species have similar ecological roles) and species number and evenness of species in a region), taxo- redundancy (different species perform the same nomic diversity (not just species richness, but diver- function) are thought to provide ‘insurance’ for sity at higher taxonomic levels), genetic diversity ecosystem function in diverse systems by promot- (genetic variation in a population or species), habitat ing functional diversity and maintaining energy or ecosystem diversity (range of habitats or ecosys- fl ow among trophic levels (i.e. ecosystem function) Figure 10.1 Species diversity does not necessarily represent functional diversity. Note that both groups have equal species richness and diversity (a single individual from each of eight molluscan species), but the group on the right has greater taxonomic distinctness and functional diversity. Photo R. M. Warwick. OUP CORRECTED PROOF – FINAL, 08/11/2011, SPi 194 OCEAN ACIDIFICATION upon a reduction or loss of species in response to ture) are intolerable. Range shifts along other environmental variation or other factors ( Loreau gradients in pH or carbonate saturation (e.g. depth- et al. 2001 ). related or horizontally in coastal regions) may also Field studies in terrestrial and marine ecosystems be possible. over the past two decades have provided both sup- Whether marine organisms, from microbes to port (e.g. Steneck et al. 2002 ) and moderate contro- long-lived megafauna, will be able to acclimatize or versy concerning the diversity–stability concept adapt to future ocean acidifi cation is an important, ( Loreau et al. 2001 ; Cardinale et al. 2006 ). The contro- but unresolved, question. Acclimatization is the versy relates, in part, to the disproportionate role of process by which individuals adjust to environmen- key species in many systems studied, without which tal changes (i.e. physiological adjustment). This stability is reduced. This issue may be important in may result in a change in energy costs (positive or several marine ecosystems where key prey species negative) associated with living. Adaptation is the (e.g. pteropods, krill, anchovies, and squid in coastal adjustment of species to environmental change systems) or taxa that play an important structural between generations, through natural selection of role (e.g. habitat-forming corals) can be critical individuals tolerant of new conditions. Tolerance or resources for other taxa. Thus, reduced biodiversity acclimatization by at least some individuals in the due to the loss of prey taxa or habitat-forming spe- population allows for adaptation, assuming that the cies may not have large effects on energy fl ow or tolerant traits are heritable and suffi cient time is ecosystem function and stability, so long as key spe- available for selection to increase the frequency of cies that maintain the functional diversity of the tolerant genotypes through multiple generations. If system are relatively unaffected ( Tilman et al. 1997 ). individuals in most populations are able to acclima- Although this debate continues, a recent examina- tize
Recommended publications
  • Slow-Onset Processes and Resulting Loss and Damage
    Publication Series ADDRESSING LOSS AND DAMAGE FROM SLOW-ONSET PROCESSES Slow-onset Processes and Resulting Loss and Damage – An introduction Table of contents L 4 22 ist of a bbre Summary of Loss and damage via tio key facts and due to slow-onset ns definitions processes AR4 IPCC Fourth Assessment Report 6 22 What is loss and damage? Introduction AR5 IPCC Fifth Assessment Report COP Conference of the Parties to the 23 United Nations Framework Convention on 9 What losses and damages IMPRINT Climate Change can result from slow-onset Slow-onset ENDA Environment Development Action Energy, processes? Authors Environment and Development Programme processes and their Laura Schäfer, Pia Jorks, Emmanuel Seck, Energy key characteristics 26 Oumou Koulibaly, Aliou Diouf ESL Extreme Sea Level What losses and damages Contributors GDP Gross Domestic Product 9 can result from sea level rise? Idy Niang, Bounama Dieye, Omar Sow, Vera GMSL Global mean sea level What is a slow-onset process? Künzel, Rixa Schwarz, Erin Roberts, Roxana 31 Baldrich, Nathalie Koffi Nguessan GMSLR Global mean sea level rise 10 IOM International Organization on Migration What are key characteristics Loss and damage Editing Adam Goulston – Scize Group LLC of slow-onset processes? in Senegal due to IPCC Intergovernmental Panel on Climate Change sea level rise Layout and graphics LECZ Low-elevation coastal zone 14 Karin Roth – Wissen in Worten OCHA Office for the Coordination of Humanitarian Affairs What are other relevant January 2021 terms for the terminology on 35 RCP Representative
    [Show full text]
  • Ocean Acidification in Washington State
    University of Washington • Washington Sea Grant Ocean Acidification in Washington State What is Ocean Acidification? OA in Washington State cean Acidification (or ‘OA’) is a long-term decrease ur region is experiencing ocean acidification sooner Oin seawater pH that is primarily caused by the Oand more severely than expected, due to a combina- ocean’s uptake of carbon dioxide (CO2 ) from the atmo- tion of human and natural causes. In the spring and sum- sphere. CO2 generated by humans’ use of fossil fuels and mer, acidification along our coast is compounded by up- deforestation has been accumulating in the atmosphere welling, which mixes deep, naturally low-pH seawater into since the industrial revolution. About one quarter of this the already acidified surface layer. In Puget Sound, nutri- CO2 is absorbed by the oceans, pH describes the acidity of a liquid ents generated by human activities (mostly where it reacts with water to form nitrogen and phosphorus from sewage, carbonic acid. As a result, the aver- fertilizers and manure) fuel processes that age pH of seawater at the ocean add even more CO2 to this ‘doubly-acidified’ surface has already dropped by ~0.1 seawater. The combination can be deadly units, a 30% increase in acidity. If to vulnerable organisms. pH levels as low atmospheric CO2 levels continue as 7.4 have been recorded in Hood Canal, to climb at the present rate, ocean an important shellfish-growing region. acidity will double by the end of this State and federal agencies, scientists, tribes, century. shellfish growers and NGOs are working together to address OA in our region.
    [Show full text]
  • Ocean Acidification Due to Increasing Atmospheric Carbon Dioxide
    Ocean acidification due to increasing atmospheric carbon dioxide Policy document 12/05 June 2005 ISBN 0 85403 617 2 This report can be found at www.royalsoc.ac.uk ISBN 0 85403 617 2 © The Royal Society 2005 Requests to reproduce all or part of this document should be submitted to: Science Policy Section The Royal Society 6-9 Carlton House Terrace London SW1Y 5AG email [email protected] Copy edited and typeset by The Clyvedon Press Ltd, Cardiff, UK ii | June 2005 | The Royal Society Ocean acidification due to increasing atmospheric carbon dioxide Ocean acidification due to increasing atmospheric carbon dioxide Contents Page Summary vi 1 Introduction 1 1.1 Background to the report 1 1.2 The oceans and carbon dioxide: acidification 1 1.3 Acidification and the surface oceans 2 1.4 Ocean life and acidification 2 1.5 Interaction with the Earth systems 2 1.6 Adaptation to and mitigation of ocean acidification 2 1.7 Artificial deep ocean storage of carbon dioxide 3 1.8 Conduct of the study 3 2 Effects of atmospheric CO2 enhancement on ocean chemistry 5 2.1 Introduction 5 2.2 The impact of increasing CO2 on the chemistry of ocean waters 5 2.2.1 The oceans and the carbon cycle 5 2.2.2 The oceans and carbon dioxide 6 2.2.3 The oceans as a carbonate buffer 6 2.3 Natural variation in pH of the oceans 6 2.4 Factors affecting CO2 uptake by the oceans 7 2.5 How oceans have responded to changes in atmospheric CO2 in the past 7 2.6 Change in ocean chemistry due to increases in atmospheric CO2 from human activities 9 2.6.1 Change to the oceans
    [Show full text]
  • 9. AM Ecocide
    Amendments to draft resolution On the crime of Ecocide № Party Line Action Current Text Proposed Amendment Explanation 1 Bündnis 90/ 1 replace On an international recognition of the Tackle environmental destruction: Die Grünen crime of ecocide: 2 Bündnis 90/ 25 replace that global warming must be limited to agreed to holding the increase in the global Die Grünen 1,5°C. average temperature to well below 2°C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5°C above pre-industrial levels, recognising that this would significantly reduce the risks and impacts of climate change. Amendments on Draft Resolution on an international recognition of the crime of ecocide European Green Party - 5th Congress, Liverpool, UK, 30 March-2 April 2017 1 № Party Line Action Current Text Proposed Amendment Explanation 3 Vihreät - De 30-36 delete According to environmental scientists Not necessary for making the point, Gröna Johan Rockström (Stockholm Resilience the chapter draws the attention Centre) and Will Steffen (Australian away from the point of the National University), these are two among resolution making it unnecessarily four “planetary boundaries” that have long. 4 Strana 30-36 replace already been exceeded. These “planetary These present two out of nine “planetary The original text presents the zelenych boundaries” involve nine thresholds on boundaries”, or nine thresholds on core concept of "planetary boundaries" (Czech core environmental issues (greenhouse gas environmental issues, beyond which human only as an opinion of Rockstrom Greens) amount in atmosphere, biodiversity, but existence would be threatened. The concept and Steffen and, moreover, it does also ocean acidification, land use for crop, has been introduced by a group of not state any source, that this consumption of freshwater...) beyond international scientists, led by Johan opinion is based on.
    [Show full text]
  • Ocean Acidification and the Permo- Triassic Mass Extinction: Process and Manifestation
    Goldschmidt2015 Abstracts Ocean acidification and the permo- Triassic mass extinction: Process and manifestation S. A. KASEMANN1, R. WOOD2*, M. O. CLARKSON3, T. M. LENTON4, S. J. DAINES4, S. RICHOZ5, F. OHNEMUELLER1, A. MEIXNER1, S. W. POULTON6 AND E. T. TIPPER7 1Department of Geosciences & MARUM-Center for Marine Environmental Sciences, Univ. of Bremen, Germany 2School of GeoSciences, University of Edinburgh, UK (*[email protected]) 3Department of Chemistry, Univ. of Otago, New Zealand 4College of Life and Environmental Sciences, Univ. of Exeter 5Institute of Earth Sciences, University of Graz, Austria 6School of Earth and Environment, University of Leeds, UK 7Dept. of Earth Sciences, University of Cambridge, UK Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for the Permian-Triassic Boundary (PTB) mass extinction, but direct evidence for an acidification event is lacking. We present a high resolution seawater pH record across this interval, utilizing boron isotope data (δ11B) combined with petrographic analysis and a quantitative modeling approach. Through this integration we are able to produce an envelope that encompasses the most realistic range in pH, which then allows us to resolve three distinct chronological phases of carbon cycle perturbation, each with very different environmental consequences for the Late Permian-Early Triassic Earth system. In the latest Permian, increased ocean alkalinity, primed the Earth system with a low level of atmospheric CO2 and a high ocean buffering capacity. The first phase of extinction was coincident with a slow injection of carbon into the atmosphere and ocean pH remained stable. During the second extinction pulse, however, a rapid and large injection of carbon caused an abrupt acidification event that drove the preferential loss of heavily calcified marine biota.
    [Show full text]
  • Ocean Acidification During the Early Toarcian
    https://doi.org/10.1130/G47781.1 Manuscript received 20 April 2020 Revised manuscript received 29 June 2020 Manuscript accepted 6 July 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 13 August 2020 Ocean acidification during the early Toarcian extinction event: Evidence from boron isotopes in brachiopods Tamás Müller1*, Hana Jurikova2,3, Marcus Gutjahr2, Adam Tomašových1, Jan Schlögl4, Volker Liebetrau2, Luís v. Duarte5, Rastislav Milovský1, Guillaume Suan6, Emanuela Mattioli6,7, Bernard Pittet6 and Anton Eisenhauer2 1 Earth Science Institute, Slovak Academy of Sciences, Dˇ umbierska 1, 974 01 Banská Bystrica, Slovakia 2 GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Wischhofstr. 1-3, 24148 Kiel, Germany 3 GFZ Deutsches GeoForschungsZentrum–Helmholtz-Zentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany 4 Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovicˇova 6, SK-842 15 Bratislava, Slovakia 5 University of Coimbra, MARE–Marine and Environmental Sciences Centre–Department of Earth Sciences, Polo II, Rua Sílvio Lima, 3030-790 Coimbra, Portugal 6 Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, F-69622, Villeurbanne, France 7 Institut Universitaire de France (IUF), 75231 Paris Cedex 05, France ABSTRACT methane, have also been postulated (Hesselbo The loss of carbonate production during the Toarcian Oceanic Anoxic Event (T-OAE, ca. et al., 2000; Them et al., 2017). 183 Ma) is hypothesized to have been at least partly triggered by ocean acidification linked The changes in the carbon cycle are globally to magmatism from the Karoo-Ferrar large igneous province (southern Africa and Antarc- expressed as a short negative shift in the car- tica).
    [Show full text]
  • Ocean Acidification and Climate Change: Synergies and Challenges
    n synthesis 5 Ocean acidification and climate change: synergies and challenges of addressing both under the UNFCCC ELLYCIA R. HARROULD-KOLIEB1, DOROTHE´E HERR2* 1 10 School of Land and Environment, University of Melbourne, Melbourne, VIC 3010, Australia 2 Global Marine and Polar Programme, International Union for Conservation of Nature (IUCN), Suite 300, 1630 Connecticut Avenue NW, Washington, DC 20001, USA 15 Ocean acidification and climate change are linked by their common driver: CO2. Climate change is the consequence of a range of GHG emissions, but ocean acidification on a global scale is caused solely by increased concentrations of atmospheric CO2. Reducing CO2 emissions is therefore the most effective way to mitigate ocean acidification. Acting to prevent further ocean acidification by reducing CO2 emissions will also provide simultaneous benefits by alleviating future climate change. Although it is possible that reducing CO2 emissions to a level low enough to address ocean acidification will simultaneously address climate change, the reverse is unfortunately not necessarily true. Despite the ocean’s integral role in the climate system and the 20 potentially wide-ranging impacts on marine life and humans, the problem of ocean acidification is largely absent from most policy discussions pertaining to CO2 emissions. The linkages between ocean acidification, climate change and the United Nations Framework Convention on Climate Change (UNFCCC) are identified and possible scenarios for developing common solutions to reduce and adapt to ocean acidification and climate change are offered. Areas where the UNFCCC is currently lacking capacity to effectively tackle rising ocean acidity are also highlighted. 25 Keywords: climate change; climate policy; ocean acidification; oceans; UNFCCC L’acidification des oce´ans et le changement climatique sont lie´s par leur cause commune : le CO2.
    [Show full text]
  • Ocean Acidification Summary for Policymakers – Third
    O A Summary for Policymakers Third Symposium on the Ocean in a High-CO2 World Scientific sponsors: The International Geosphere-Biosphere Programme (IGBP) was launched in 1987 to coordinate international research on global-scale and regional-scale interactions between Earth’s biological, chemical and physical processes and their interactions with human systems. IGBP’s international core projects Integrated Marine Biogeochemistry and Ecosystem Research (IMBER), Surface Ocean–Lower Atmosphere Study (SOLAS), Past Global Changes (PAGES) and Land–Ocean Interactions in the Coastal Zone (LOICZ) study ocean acidification. The Intergovernmental Oceanographic Commission (IOC-UNESCO) was established by the United Nations Educational, Scientific and Cultural Organization (UNESCO) in 1960 to provide Member States of the United Nations with an essential mechanism for global cooperation in the study of the ocean. The Scientific Committee on Oceanic Research (SCOR) was established by the International Council for Science (ICSU) in 1957 and is a co-sponsor of the international projects IMBER and SOLAS. Citation: IGBP, IOC, SCOR (2013). Ocean Acidification Summary for Policymakers – Third Symposium on the Ocean in a High-CO2 World. International Geosphere-Biosphere Programme, Stockholm, Sweden. Editors: Wendy Broadgate (IGBP), Owen Gaffney (IGBP), Kirsten Isensee (IOC-UNESCO), Ulf Riebesell (GEOMAR), Ed Urban (SCOR) and Luis Valdés (IOC-UNESCO). Authors: Wendy Broadgate, IGBP; Ulf Riebesell, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany; Claire
    [Show full text]
  • Climate Torts and Ecocide in the Context of Proposals for an International Environmental Court
    City University of New York (CUNY) CUNY Academic Works Dissertations and Theses City College of New York 2011 Climate Torts and Ecocide in the Context of Proposals for an International Environmental Court Patrick Foster CUNY City College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/cc_etds_theses/40 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Climate Torts and Ecocide in the Context of Proposals for an International Environmental Court Patrick Foster Graduating June, 2011 Advisor: Professor Jürgen Dedring Submitted in Partial Fulfillment of the Requirements for the Degree of Master of International Affairs at the City College of New York TABLE OF CONTENTS ABSTRACT ..........................................................................................................................................................3 CHAPTER ONE: NECESSITY AND FEASIBILITY...................................................................................4 CAUSES OF ACTION AND THEORIES OF JUSTICE...............................................................................................5 DIPLOMATIC THEORY IN THE CONTEXT OF ENVIRONMENTAL TREATY MAKING ...........................................7 CHAPTER TWO: INTERNATIONAL ENVIRONMENTAL TORTS: CLIMATE CHANGE LITIGATION .......................................................................................................................................................9
    [Show full text]
  • Effects of Climate Change on Ocean Acidification Relevant to the Pacific Islands
    PACIFIC MARINE CLIMATE CHANGE REPORT CARD Science Review 2018: pp 31-42 Effects of Climate Change on Ocean Acidification Relevant to the Pacific Islands Andrew Lenton, Richard J. Matear, and Mathieu Mongin, CSIRO Oceans and Atmosphere, Australia. EXECUTIVE SUMMARY Ocean acidification has the potential to significantly impact Pacific Island ecosystems and the ecosystem services they provide. There is compelling evidence that the ocean has become more acidic in response to rising atmospheric CO2 levels. As atmospheric CO2 levels continue to rise the ocean will increasingly become more acidic, and these changes are likely to persist for hundreds to thousands of years. The rate and magnitude of these changes will be directly proportional to the future carbon emission pathway followed. While a low carbon emissions pathway will clearly limit the impacts of ocean acidification, a high carbon emission pathway will lead to conditions that will threaten the long-term viability of important marine ecosystems, such as coral reefs. In the future, increased confidence in projected changes will come through a better understanding of how the large-scale changes are modulated by processes at the island scale. This will be achieved through a combination of sustained long-term measurements and higher-resolution modelling. There is also critical need to understand the impact of multiple environmental stressors, as future ocean acidification will be accompanied by ocean warming and other environmental consequences (e.g. invasive species). Finally, implementation of a viable emission pathway is urgently needed to underpin the development of sustainable adaption and resilience options, and to explore potential engineering and adaptation solutions that may be required to offset long-term ocean acidification changes.
    [Show full text]
  • Ocean Acidification and the UNFCCC
    Climate Change and Ocean Acidification Synergies and Opportunities within the UNFCCC Discussion Paper Ellycia Harrould-Kolieba and Dorothée Herrb Executive Summary Ocean acidification is arguably one of the most serious threats facing the oceans and humans this century. Ocean acidification is not a symptom of climate change; rather, it is a threat concurrent with climate change and caused by a common root problem: ongoing anthropogenic CO2 emissions. It is a serious global challenge of unprecedented scale and importance that requires immediate action. Preventing further acidification of the oceans will require stabilizing and reducing the level of CO2 in the atmosphere, which is most effectively done through reducing CO2 emissions. The United Nations Framework Convention on Climate Change (UNFCCC) is clearly an appropriate environmental policy regime to deal with the mitigation of ocean acidification, through CO2 reductions. It is also a suitable forum for devising and providing funding for responses to ocean acidification that can be incorporated into national adaptation plans. Many efforts are underway to raise awareness and inform policy and decision makers about ocean acidification and its potential impacts. So far, however, no concrete recommendations have been made on how ocean acidification could be integrated within the UNFCCC. This paper attempts to address this gap by offering an initial suite of possible ways to address ocean acidification alongside climate change mitigation and adaptation strategies. Recommendations: - Recognize
    [Show full text]
  • An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity CBD Technical Series No
    Secretariat of the CBD Technical Series Convention on No. 75 Biological Diversity 75 An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity CBD Technical Series No. 75 AN UPDATED SYNTHESIS OF THE IMPACTS OF OCEAN ACIDIFICATION ON MARINE BIODIVERSITY The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the copyright holders concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. This publication may be reproduced for educational or non-profit purposes without special permission, provided acknowledgement of the source is made. The Secretariat of the Convention would appreciate receiving a copy of any publications that use this document as a source. Reuse of the figures is subject to permission from the original rights holders. Published by the Secretariat of the Convention on Biological Diversity. ISBN 92-9225-527-4 (print version); ISBN 92-9225-528-2 (web version) Copyright © 2014, Secretariat of the Convention on Biological Diversity Citation: Secretariat of the Convention on Biological Diversity (2014). An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity (Eds: S. Hennige, J.M. Roberts & P. Williamson). Montreal, Technical Series No. 75, 99 pages For further information, contact: Secretariat of the Convention on Biological Diversity World Trade Centre, 413 Rue St. Jacques, Suite 800, Montréal, Quebec,Canada H2Y 1N9 Tel: +1 (514) 288 2220 Fax: +1 (514) 288 6588 E-mail: [email protected] Website: www.cbd.int Cover images, top to bottom: Katharina Fabricius; N.
    [Show full text]