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Robinson SA, Revell LE, Mackenzie R, Ossola R. Extended ozone depletion and reduced snow and ice cover-Consequences for Antarctic biota. GLOBAL CHANGE BIOLOGY 2024; 30:e17283. [PMID: 38663017 DOI: 10.1111/gcb.17283] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/02/2024] [Revised: 04/01/2024] [Accepted: 04/02/2024] [Indexed: 05/25/2024]
Abstract
Stratospheric ozone, which has been depleted in recent decades by the release of anthropogenic gases, is critical for shielding the biosphere against ultraviolet-B (UV-B) radiation. Although the ozone layer is expected to recover before the end of the 21st century, a hole over Antarctica continues to appear each year. Ozone depletion usually peaks between September and October, when fortunately, most Antarctic terrestrial vegetation and soil biota is frozen, dormant and protected under snow cover. Similarly, much marine life is protected by sea ice cover. The ozone hole used to close before the onset of Antarctic summer, meaning that most biota were not exposed to severe springtime UV-B fluxes. However, in recent years, ozone depletion has persisted into December, which marks the beginning of austral summer. Early summertime ozone depletion is concerning: high incident UV-B radiation coincident with snowmelt and emergence of vegetation will mean biota is more exposed. The start of summer is also peak breeding season for many animals, thus extreme UV-B exposure (UV index up to 14) may come at a vulnerable time in their life cycle. Climate change, including changing wind patterns and strength, and particularly declining sea ice, are likely to compound UV-B exposure of Antarctic organisms, through earlier ice and snowmelt, heatwaves and droughts. Antarctic field research conducted decades ago tended to study UV impacts in isolation and more research that considers multiple climate impacts, and the true magnitude and timing of current UV increases is needed.
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Affiliation(s)
- Sharon A Robinson
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, New South Wales, Australia
- Environmental Futures, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, New South Wales, Australia
| | - Laura E Revell
- School of Physical and Chemical Sciences, University of Canterbury, Christchurch, New Zealand
| | - Roy Mackenzie
- Cape Horn International Center CHIC, Universidad de Magallanes, Puerto Williams, Chile
- Millenium Institut Biodiversity of Antarctic and Subantarctic Ecosystems BASE, Santiago, Chile
| | - Rachele Ossola
- Department of Chemistry, Colorado State University, Fort Collins, Colorado, USA
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2
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Yin H, Perera-Castro AV, Randall KL, Turnbull JD, Waterman MJ, Dunn J, Robinson SA. Basking in the sun: how mosses photosynthesise and survive in Antarctica. PHOTOSYNTHESIS RESEARCH 2023; 158:151-169. [PMID: 37515652 PMCID: PMC10684656 DOI: 10.1007/s11120-023-01040-y] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/15/2023] [Accepted: 07/10/2023] [Indexed: 07/31/2023]
Abstract
The Antarctic environment is extremely cold, windy and dry. Ozone depletion has resulted in increasing ultraviolet-B radiation, and increasing greenhouse gases and decreasing stratospheric ozone have altered Antarctica's climate. How do mosses thrive photosynthetically in this harsh environment? Antarctic mosses take advantage of microclimates where the combination of protection from wind, sufficient melt water, nutrients from seabirds and optimal sunlight provides both photosynthetic energy and sufficient warmth for efficient metabolism. The amount of sunlight presents a challenge: more light creates warmer canopies which are optimal for photosynthetic enzymes but can contain excess light energy that could damage the photochemical apparatus. Antarctic mosses thus exhibit strong photoprotective potential in the form of xanthophyll cycle pigments. Conversion to zeaxanthin is high when conditions are most extreme, especially when water content is low. Antarctic mosses also produce UV screening compounds which are maintained in cell walls in some species and appear to protect from DNA damage under elevated UV-B radiation. These plants thus survive in one of the harshest places on Earth by taking advantage of the best real estate to optimise their metabolism. But survival is precarious and it remains to be seen if these strategies will still work as the Antarctic climate changes.
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Affiliation(s)
- Hao Yin
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
| | | | - Krystal L Randall
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
| | - Johanna D Turnbull
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
| | - Melinda J Waterman
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
| | - Jodie Dunn
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
| | - Sharon A Robinson
- Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, NSW, 2522, Australia.
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia.
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Madronich S, Sulzberger B, Longstreth JD, Schikowski T, Andersen MPS, Solomon KR, Wilson SR. Changes in tropospheric air quality related to the protection of stratospheric ozone in a changing climate. Photochem Photobiol Sci 2023; 22:1129-1176. [PMID: 37310641 PMCID: PMC10262938 DOI: 10.1007/s43630-023-00369-6] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/19/2022] [Accepted: 01/13/2023] [Indexed: 06/14/2023]
Abstract
Ultraviolet (UV) radiation drives the net production of tropospheric ozone (O3) and a large fraction of particulate matter (PM) including sulfate, nitrate, and secondary organic aerosols. Ground-level O3 and PM are detrimental to human health, leading to several million premature deaths per year globally, and have adverse effects on plants and the yields of crops. The Montreal Protocol has prevented large increases in UV radiation that would have had major impacts on air quality. Future scenarios in which stratospheric O3 returns to 1980 values or even exceeds them (the so-called super-recovery) will tend to ameliorate urban ground-level O3 slightly but worsen it in rural areas. Furthermore, recovery of stratospheric O3 is expected to increase the amount of O3 transported into the troposphere by meteorological processes that are sensitive to climate change. UV radiation also generates hydroxyl radicals (OH) that control the amounts of many environmentally important chemicals in the atmosphere including some greenhouse gases, e.g., methane (CH4), and some short-lived ozone-depleting substances (ODSs). Recent modeling studies have shown that the increases in UV radiation associated with the depletion of stratospheric ozone over 1980-2020 have contributed a small increase (~ 3%) to the globally averaged concentrations of OH. Replacements for ODSs include chemicals that react with OH radicals, hence preventing the transport of these chemicals to the stratosphere. Some of these chemicals, e.g., hydrofluorocarbons that are currently being phased out, and hydrofluoroolefins now used increasingly, decompose into products whose fate in the environment warrants further investigation. One such product, trifluoroacetic acid (TFA), has no obvious pathway of degradation and might accumulate in some water bodies, but is unlikely to cause adverse effects out to 2100.
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Affiliation(s)
- S Madronich
- National Center for Atmospheric Research, Boulder, USA.
- USDA UV-B Monitoring and Research Program, Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, USA.
| | - B Sulzberger
- Academic Guest after retirement from Eawag: Swiss Federal Institute of Aquatic Science and Technology, CH-8600, Duebendorf, Switzerland
| | - J D Longstreth
- The Institute for Global Risk Research, LLC, Bethesda, USA
| | - T Schikowski
- IUF-Leibniz Research Institute for Environmental Medicine, Dusseldorf, Germany
| | - M P Sulbæk Andersen
- Department of Chemistry and Biochemistry, California State University, Northridge, USA
| | - K R Solomon
- School of Environmental Sciences, University of Guelph, Guelph, Canada
| | - S R Wilson
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia.
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4
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Barnes PW, Robson TM, Zepp RG, Bornman JF, Jansen MAK, Ossola R, Wang QW, Robinson SA, Foereid B, Klekociuk AR, Martinez-Abaigar J, Hou WC, Mackenzie R, Paul ND. Interactive effects of changes in UV radiation and climate on terrestrial ecosystems, biogeochemical cycles, and feedbacks to the climate system. Photochem Photobiol Sci 2023; 22:1049-1091. [PMID: 36723799 PMCID: PMC9889965 DOI: 10.1007/s43630-023-00376-7] [Citation(s) in RCA: 13] [Impact Index Per Article: 13.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/22/2022] [Accepted: 01/13/2023] [Indexed: 02/02/2023]
Abstract
Terrestrial organisms and ecosystems are being exposed to new and rapidly changing combinations of solar UV radiation and other environmental factors because of ongoing changes in stratospheric ozone and climate. In this Quadrennial Assessment, we examine the interactive effects of changes in stratospheric ozone, UV radiation and climate on terrestrial ecosystems and biogeochemical cycles in the context of the Montreal Protocol. We specifically assess effects on terrestrial organisms, agriculture and food supply, biodiversity, ecosystem services and feedbacks to the climate system. Emphasis is placed on the role of extreme climate events in altering the exposure to UV radiation of organisms and ecosystems and the potential effects on biodiversity. We also address the responses of plants to increased temporal variability in solar UV radiation, the interactive effects of UV radiation and other climate change factors (e.g. drought, temperature) on crops, and the role of UV radiation in driving the breakdown of organic matter from dead plant material (i.e. litter) and biocides (pesticides and herbicides). Our assessment indicates that UV radiation and climate interact in various ways to affect the structure and function of terrestrial ecosystems, and that by protecting the ozone layer, the Montreal Protocol continues to play a vital role in maintaining healthy, diverse ecosystems on land that sustain life on Earth. Furthermore, the Montreal Protocol and its Kigali Amendment are mitigating some of the negative environmental consequences of climate change by limiting the emissions of greenhouse gases and protecting the carbon sequestration potential of vegetation and the terrestrial carbon pool.
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Affiliation(s)
- P W Barnes
- Biological Sciences and Environment Program, Loyola University New Orleans, New Orleans, USA.
| | - T M Robson
- Organismal & Evolutionary Biology (OEB), Faculty of Biological and Environmental Sciences, Viikki Plant Sciences Centre (ViPS), University of Helsinki, Helsinki, Finland.
- National School of Forestry, University of Cumbria, Ambleside, UK.
| | - R G Zepp
- ORD/CEMM, US Environmental Protection Agency, Athens, GA, USA
| | - J F Bornman
- Food Futures Institute, Murdoch University, Perth, Australia
| | | | - R Ossola
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, USA
| | - Q-W Wang
- Institute of Applied Ecology, Chinese Academy of Sciences (CAS), Shenyang, China
| | - S A Robinson
- Global Challenges Program & School of Earth, Atmospheric and Life Sciences, Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, Australia
| | - B Foereid
- Environment and Natural Resources, Norwegian Institute of Bioeconomy Research, Ås, Norway
| | - A R Klekociuk
- Antarctic Climate Program, Australian Antarctic Division, Kingston, Australia
| | - J Martinez-Abaigar
- Faculty of Science and Technology, University of La Rioja, Logroño (La Rioja), Spain
| | - W-C Hou
- Department of Environmental Engineering, National Cheng Kung University, Tainan City, Taiwan
| | - R Mackenzie
- Cape Horn International Center (CHIC), Puerto Williams, Chile
- Millennium Institute Biodiversity of Antarctic and Subantarctic Ecosystems (BASE), Santiago, Chile
| | - N D Paul
- Lancaster Environment Centre, Lancaster University, Lancaster, UK
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Lee JR, Waterman MJ, Shaw JD, Bergstrom DM, Lynch HJ, Wall DH, Robinson SA. Islands in the ice: Potential impacts of habitat transformation on Antarctic biodiversity. GLOBAL CHANGE BIOLOGY 2022; 28:5865-5880. [PMID: 35795907 PMCID: PMC9542894 DOI: 10.1111/gcb.16331] [Citation(s) in RCA: 16] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/19/2022] [Accepted: 06/15/2022] [Indexed: 05/04/2023]
Abstract
Antarctic biodiversity faces an unknown future with a changing climate. Most terrestrial biota is restricted to limited patches of ice-free land in a sea of ice, where they are adapted to the continent's extreme cold and wind and exploit microhabitats of suitable conditions. As temperatures rise, ice-free areas are predicted to expand, more rapidly in some areas than others. There is high uncertainty as to how species' distributions, physiology, abundance, and survivorship will be affected as their habitats transform. Here we use current knowledge to propose hypotheses that ice-free area expansion (i) will increase habitat availability, though the quality of habitat will vary; (ii) will increase structural connectivity, although not necessarily increase opportunities for species establishment; (iii) combined with milder climates will increase likelihood of non-native species establishment, but may also lengthen activity windows for all species; and (iv) will benefit some species and not others, possibly resulting in increased homogeneity of biodiversity. We anticipate considerable spatial, temporal, and taxonomic variation in species responses, and a heightened need for interdisciplinary research to understand the factors associated with ecosystem resilience under future scenarios. Such research will help identify at-risk species or vulnerable localities and is crucial for informing environmental management and policymaking into the future.
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Affiliation(s)
- Jasmine R. Lee
- British Antarctic SurveyNERCCambridgeUK
- Securing Antarctica's Environmental Future, School of Biology and Environmental ScienceQueensland University of TechnologyBrisbaneQLDAustralia
| | - Melinda J. Waterman
- Securing Antarctica's Environmental Future, School of Earth, Atmospheric and Life SciencesUniversity of WollongongWollongongNew South WalesAustralia
| | - Justine D. Shaw
- Securing Antarctica's Environmental Future, School of Biology and Environmental ScienceQueensland University of TechnologyBrisbaneQLDAustralia
| | - Dana M. Bergstrom
- Australian Antarctic Division, Department of AgricultureWater and the EnvironmentKingstonTASAustralia
- Global Challenges ProgramUniversity of WollongongWollongongNew South WalesAustralia
| | - Heather J. Lynch
- Department of Ecology and EvolutionStony Brook UniversityStony BrookNew YorkUSA
| | - Diana H. Wall
- Department of Biology and School of Global Environmental SustainabilityColorado State UniversityFort CollinsColoradoUSA
| | - Sharon A. Robinson
- Securing Antarctica's Environmental Future, School of Earth, Atmospheric and Life SciencesUniversity of WollongongWollongongNew South WalesAustralia
- Global Challenges ProgramUniversity of WollongongWollongongNew South WalesAustralia
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6
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Robinson SA. Climate change and extreme events are changing the biology of Polar Regions. GLOBAL CHANGE BIOLOGY 2022; 28:5861-5864. [PMID: 35821589 DOI: 10.1111/gcb.16309] [Citation(s) in RCA: 8] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/20/2022] [Accepted: 06/20/2022] [Indexed: 06/15/2023]
Abstract
Polar landscapes and their unique biodiversity are threatened by climate change. Wild reindeer are cultural and ecological keystone species, traversing across the northern Eurasian Arctic throughout the year (Wild reindeer in the sub-Arctic in Kuhmo, Finland. Photo: Antti Leinonen, Snowchange Cooperative. Used with permission). In contrast, Antarctic terrestrial biodiversity is found on islands in the ice (or ocean) which support unique assemblages of plants and animals (King George Island, South Shetlands; photo Andrew Netherwood. Used with permission). This VSI examines how the changing climate threatens these diverse marine and terrestrial habitats and the biodiversity that they support.
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Affiliation(s)
- Sharon A Robinson
- Securing Antarctica's Environmental Future, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, New South Wales, Australia
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7
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Snyder KA, Robinson SA, Schmidt S, Hultine KR. Stable isotope approaches and opportunities for improving plant conservation. CONSERVATION PHYSIOLOGY 2022; 10:coac056. [PMID: 35966756 PMCID: PMC9367551 DOI: 10.1093/conphys/coac056] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Subscribe] [Scholar Register] [Received: 08/05/2020] [Revised: 04/15/2021] [Accepted: 08/01/2022] [Indexed: 06/01/2023]
Abstract
Successful conservation of threatened species and ecosystems in a rapidly changing world requires scientifically sound decision-making tools that are readily accessible to conservation practitioners. Physiological applications that examine how plants and animals interact with their environment are now widely used when planning, implementing and monitoring conservation. Among these tools, stable-isotope physiology is a potentially powerful, yet under-utilized cornerstone of current and future conservation efforts of threatened and endangered plants. We review the underlying concepts and theory of stable-isotope physiology and describe how stable-isotope applications can support plant conservation. We focus on stable isotopes of carbon, hydrogen, oxygen and nitrogen to address plant ecophysiological responses to changing environmental conditions across temporal scales from hours to centuries. We review examples from a broad range of plant taxa, life forms and habitats and provide specific examples where stable-isotope analysis can directly improve conservation, in part by helping identify resilient, locally adapted genotypes or populations. Our review aims to provide a guide for practitioners to easily access and evaluate the information that can be derived from stable-isotope signatures, their limitations and how stable isotopes can improve conservation efforts.
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Affiliation(s)
- Keirith A Snyder
- Corresponding author: USDA Agricultural Research Service, Great Basin Rangelands Research Unit, Reno,
920 Valley Road, NV 89512, USA.
| | - Sharon A Robinson
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, New South Wales 2522, Australia
- Securing Antarctica’s Environmental Future, University of Wollongong, Wollongong, New South Wales 2522, Australia
| | - Susanne Schmidt
- School of Agriculture and Food Sciences, The University of Queensland, Building 62, Brisbane Queensland 4075, Australia
| | - Kevin R Hultine
- Department of Research, Conservation and Collections, Desert Botanical Garden, 1201 Galvin Parkway, Phoenix, AZ 85008, USA
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8
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Barnes PW, Bornman JF, Pandey KK, Bernhard GH, Bais AF, Neale RE, Robson TM, Neale PJ, Williamson CE, Zepp RG, Madronich S, Wilson SR, Andrady AL, Heikkilä AM, Robinson SA. The success of the Montreal Protocol in mitigating interactive effects of stratospheric ozone depletion and climate change on the environment. GLOBAL CHANGE BIOLOGY 2021; 27:5681-5683. [PMID: 34392574 DOI: 10.1111/gcb.15841] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/29/2021] [Revised: 08/18/2021] [Accepted: 08/09/2021] [Indexed: 06/13/2023]
Abstract
The Montreal Protocol and its Amendments have been highly effective in protecting the stratospheric ozone layer, preventing global increases in solar ultraviolet-B radiation (UV-B; 280-315 nm) at Earth's surface, and reducing global warming. While ongoing and projected changes in UV-B radiation and climate still pose a threat to human health, food security, air and water quality, terrestrial and aquatic ecosystems, and construction materials and fabrics, the Montreal Protocol continues to play a critical role in protecting Earth's inhabitants and ecosystems by addressing many of the United Nations Sustainable Development Goals.
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Affiliation(s)
- Paul W Barnes
- Department of Biological Sciences and Environment Program, Loyola University New Orleans, New Orleans, Louisiana, USA
| | - Janet F Bornman
- Food Futures Institute, Murdoch University, Perth, Western Australia, Australia
| | - Krishna K Pandey
- Department of Wood Properties and Uses, Institute of Wood Science and Technology, Bangalore, India
| | | | - Alkiviadis F Bais
- Department of Physics, Laboratory of Atmospheric Physics, Aristotle University, Thessaloniki, Greece
| | - Rachel E Neale
- Population Health Department, QIMR Berghofer Medical Research Institute, Brisbane, Queensland, Australia
| | - Thomas Matthew Robson
- Organismal & Evolutionary Biology (OEB), Viikki Plant Sciences Centre (ViPS), University of Helsinki, Helsinki, Finland
| | - Patrick J Neale
- Smithsonian Environmental Research Center, Edgewater, Maryland, USA
| | | | - Richard G Zepp
- ORD/CEMM, US Environmental Protection Agency, Athens, Georgia, USA
| | - Sasha Madronich
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, Colorado, USA
| | - Stephen R Wilson
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, New South Wales, Australia
| | - Anthony L Andrady
- Department of Chemical and Biomolecular Engineering, North Carolina State University, Raleigh, North Carolina, USA
| | | | - Sharon A Robinson
- Securing Antarctica's Environmental Future, Global Challenges Program & School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, New South Wales, Australia
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Neale RE, Barnes PW, Robson TM, Neale PJ, Williamson CE, Zepp RG, Wilson SR, Madronich S, Andrady AL, Heikkilä AM, Bernhard GH, Bais AF, Aucamp PJ, Banaszak AT, Bornman JF, Bruckman LS, Byrne SN, Foereid B, Häder DP, Hollestein LM, Hou WC, Hylander S, Jansen MAK, Klekociuk AR, Liley JB, Longstreth J, Lucas RM, Martinez-Abaigar J, McNeill K, Olsen CM, Pandey KK, Rhodes LE, Robinson SA, Rose KC, Schikowski T, Solomon KR, Sulzberger B, Ukpebor JE, Wang QW, Wängberg SÅ, White CC, Yazar S, Young AR, Young PJ, Zhu L, Zhu M. Environmental effects of stratospheric ozone depletion, UV radiation, and interactions with climate change: UNEP Environmental Effects Assessment Panel, Update 2020. Photochem Photobiol Sci 2021; 20:1-67. [PMID: 33721243 PMCID: PMC7816068 DOI: 10.1007/s43630-020-00001-x] [Citation(s) in RCA: 47] [Impact Index Per Article: 15.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/05/2020] [Accepted: 11/10/2020] [Indexed: 01/31/2023]
Abstract
This assessment by the Environmental Effects Assessment Panel (EEAP) of the United Nations Environment Programme (UNEP) provides the latest scientific update since our most recent comprehensive assessment (Photochemical and Photobiological Sciences, 2019, 18, 595-828). The interactive effects between the stratospheric ozone layer, solar ultraviolet (UV) radiation, and climate change are presented within the framework of the Montreal Protocol and the United Nations Sustainable Development Goals. We address how these global environmental changes affect the atmosphere and air quality; human health; terrestrial and aquatic ecosystems; biogeochemical cycles; and materials used in outdoor construction, solar energy technologies, and fabrics. In many cases, there is a growing influence from changes in seasonality and extreme events due to climate change. Additionally, we assess the transmission and environmental effects of the severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2), which is responsible for the COVID-19 pandemic, in the context of linkages with solar UV radiation and the Montreal Protocol.
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Affiliation(s)
- R E Neale
- Population Health Department, QIMR Berghofer Medical Research Institute, Brisbane, Australia
| | - P W Barnes
- Biological Sciences and Environmental Program, Loyola University New Orleans, New Orleans, LA, USA
| | - T M Robson
- Organismal and Evolutionary Biology (OEB), Viikki Plant Sciences Centre (ViPS), University of Helsinki, Helsinki, Finland
| | - P J Neale
- Smithsonian Environmental Research Center, Maryland, USA
| | - C E Williamson
- Department of Biology, Miami University, Oxford, OH, USA
| | - R G Zepp
- ORD/CEMM, US Environmental Protection Agency, Athens, GA, USA
| | - S R Wilson
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia
| | - S Madronich
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - A L Andrady
- Chemical and Biomolecular Engineering, North Carolina State University, Raleigh, NC, USA
| | - A M Heikkilä
- Finnish Meteorological Institute, Helsinki, Finland
| | - G H Bernhard
- Biospherical Instruments Inc, San Diego, CA, USA
| | - A F Bais
- Department of Physics, Laboratory of Atmospheric Physics, Aristotle University, Thessaloniki, Greece
| | - P J Aucamp
- Ptersa Environmental Consultants, Pretoria, South Africa
| | - A T Banaszak
- Unidad Académica de Sistemas Arrecifales, Universidad Nacional Autónoma de México, Puerto Morelos, México
| | - J F Bornman
- Food Futures Institute, Murdoch University, Perth, Australia.
| | - L S Bruckman
- Department of Materials Science and Engineering, Case Western Reserve University, Cleveland, OH, USA
| | - S N Byrne
- The University of Sydney, School of Medical Sciences, Discipline of Applied Medical Science, Sydney, Australia
| | - B Foereid
- Environment and Natural Resources, Norwegian Institute of Bioeconomy Research, Ås, Norway
| | - D-P Häder
- Department of Biology, Friedrich-Alexander University, Möhrendorf, Germany
| | - L M Hollestein
- Department of Dermatology, Erasmus MC Cancer Institute, Rotterdam, The Netherlands
| | - W-C Hou
- Department of Environmental Engineering, National Cheng Kung University, Tainan, Taiwan, Republic of China
| | - S Hylander
- Centre for Ecology and Evolution in Microbial model Systems-EEMiS, Linnaeus University, Kalmar, Sweden.
| | - M A K Jansen
- School of BEES, Environmental Research Institute, University College Cork, Cork, Ireland
| | - A R Klekociuk
- Antarctic Climate Program, Australian Antarctic Division, Kingston, Australia
| | - J B Liley
- National Institute of Water and Atmospheric Research, Lauder, New Zealand
| | - J Longstreth
- The Institute for Global Risk Research, LLC, Bethesda, MD, USA
| | - R M Lucas
- National Centre of Epidemiology and Population Health, Australian National University, Canberra, Australia
| | - J Martinez-Abaigar
- Faculty of Science and Technology, University of La Rioja, Logroño, Spain
| | | | - C M Olsen
- Cancer Control Group, QIMR Berghofer Medical Research Institute, Brisbane, Australia
| | - K K Pandey
- Department of Wood Properties and Uses, Institute of Wood Science and Technology, Bangalore, India
| | - L E Rhodes
- Photobiology Unit, Dermatology Research Centre, School of Biological Sciences, Faculty of Biology Medicine and Health, University of Manchester, Manchester, UK
| | - S A Robinson
- Securing Antarctica's Environmental Future, Global Challenges Program and School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia
| | - K C Rose
- Department of Biological Sciences, Rensselaer Polytechnic Institute, Troy, NY, USA
| | - T Schikowski
- IUF-Leibniz Institute of Environmental Medicine, Dusseldorf, Germany
| | - K R Solomon
- Centre for Toxicology, School of Environmental Sciences, University of Guelph, Guelph, Canada
| | - B Sulzberger
- Academic Guest Eawag: Swiss Federal Institute of Aquatic Science and Technology, Duebendorf, Switzerland
| | - J E Ukpebor
- Chemistry Department, Faculty of Physical Sciences, University of Benin, Benin City, Nigeria
| | - Q-W Wang
- Institute of Applied Ecology, Chinese Academy of Sciences (CAS), Shenyang, China
| | - S-Å Wängberg
- Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden
| | - C C White
- Bee America, 5409 Mohican Rd, Bethesda, MD, USA
| | - S Yazar
- Garvan Institute of Medical Research, Sydney, Australia
| | - A R Young
- St John's Institute of Dermatology, King's College London, London, UK
| | - P J Young
- Lancaster Environment Centre, Lancaster University, Lancaster, UK
| | - L Zhu
- Center for Advanced Low-Dimension Materials, Donghua University, Shanghai, China
| | - M Zhu
- State Key Laboratory for Modification of Chemical Fibers and Polymer Materials, Donghua University, Shanghai, China
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10
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Wang H, Liu S, Wang T, Liu H, Xu X, Chen K, Zhang P. The moss flavone synthase I positively regulates the tolerance of plants to drought stress and UV-B radiation. PLANT SCIENCE : AN INTERNATIONAL JOURNAL OF EXPERIMENTAL PLANT BIOLOGY 2020; 298:110591. [PMID: 32771149 DOI: 10.1016/j.plantsci.2020.110591] [Citation(s) in RCA: 30] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/11/2020] [Revised: 06/30/2020] [Accepted: 07/01/2020] [Indexed: 05/24/2023]
Abstract
Flavonoids are extensively distributed secondary metabolites in land plants. They play a critical role in plant evolution from aquatic to terrestrial and plant adaption to ultraviolet radiation. However, the downstream branching pathway of flavonoids and its regulatory mechanism in bryophytes, which are the most ancient of terrestrial plants, remain unclear. Here, a type I flavone synthase (PnFNSI) was characterized from the Antarctic moss Pohlia nutans. PnFNSI was primarily distributed in the cytoplasm, as detected by subcellular localization. PnFNSI could catalyze the conversion of naringenin to apigenin with an optimal temperature between 15 and 20 °C in vitro. Overexpression of PnFNSI in Arabidopsis alleviated the growth restriction caused by naringenin and accumulated apigenin product. PnFNSI-overexpressing plants showed enhanced plant tolerance to drought stress and UV-B radiation. PnFNSI also increased the enzyme activities and gene transcription levels of reactive oxygen species (ROS) scavengers, protecting plants against oxidative stress. Moreover, overexpression of PnFNSI enhanced the flavone biosynthesis pathway in Arabidopsis. Therefore, this moss FNSI-type enzyme participates in flavone metabolism, conferring protection against drought stress and UV-B radiation.
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Affiliation(s)
- Huijuan Wang
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China
| | - Shenghao Liu
- Marine Ecology Research Center, First Institute of Oceanography, Natural Resources Ministry, Qingdao, 266061, China
| | - Tailin Wang
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China
| | - Hongwei Liu
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China
| | - Xinhui Xu
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China
| | - Kaoshan Chen
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China
| | - Pengying Zhang
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Qingdao, 266237, China.
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11
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Biersma EM, Convey P, Wyber R, Robinson SA, Dowton M, van de Vijver B, Linse K, Griffiths H, Jackson JA. Latitudinal Biogeographic Structuring in the Globally Distributed Moss Ceratodon purpureus. FRONTIERS IN PLANT SCIENCE 2020; 11:502359. [PMID: 32983208 PMCID: PMC7484499 DOI: 10.3389/fpls.2020.502359] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 10/02/2019] [Accepted: 08/13/2020] [Indexed: 06/11/2023]
Abstract
Biogeographic patterns of globally widespread species are expected to reflect regional structure, as well as connectivity caused by occasional long-distance dispersal. We assessed the level and drivers of population structure, connectivity, and timescales of population isolation in one of the most widespread and ruderal plants in the world - the common moss Ceratodon purpureus. We applied phylogenetic, population genetic, and molecular dating analyses to a global (n = 147) sampling data set, using three chloroplast loci and one nuclear locus. The plastid data revealed several distinct and geographically structured lineages, with connectivity patterns associated with worldwide, latitudinal "bands." These imply that connectivity is strongly influenced by global atmospheric circulation patterns, with dispersal and establishment beyond these latitudinal bands less common. Biogeographic patterns were less clear within the nuclear marker, with gene duplication likely hindering the detection of these. Divergence time analyses indicated that the current matrilineal population structure in C. purpureus has developed over the past six million years, with lineages diverging during the late Miocene, Pliocene, and Quaternary. Several colonization events in the Antarctic were apparent, as well as one old and distinct Antarctic clade, possibly isolated on the continent since the Pliocene. As C. purpureus is considered a model organism, the matrilineal biogeographic structure identified here provides a useful framework for future genetic and developmental studies on bryophytes. Our general findings may also be relevant to understanding global environmental influences on the biogeography of other organisms with microscopic propagules (e.g., spores) dispersed by wind.
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Affiliation(s)
- Elisabeth M. Biersma
- Biodiversity, Evolution and Adaptation Team, British Antarctic Survey, Cambridge, United Kingdom
- Department of Plant Sciences, University of Cambridge, Cambridge, United Kingdom
- Natural History Museum of Denmark, University of Copenhagen, Copenhagen, Denmark
| | - Peter Convey
- Biodiversity, Evolution and Adaptation Team, British Antarctic Survey, Cambridge, United Kingdom
| | - Rhys Wyber
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, NSW, Australia
| | - Sharon A. Robinson
- School of Earth, Atmospheric and Life Sciences, University of Wollongong, NSW, Australia
| | - Mark Dowton
- School of Chemistry and Molecular Bioscience, University of Wollongong, Wollongong, NSW, Australia
| | - Bart van de Vijver
- Research Department, Botanic Garden Meise, Meise, Belgium
- Ecosystem Management (ECOBE), Department of Biology, University of Antwerp, Antwerp, Belgium
| | - Katrin Linse
- Biodiversity, Evolution and Adaptation Team, British Antarctic Survey, Cambridge, United Kingdom
| | - Howard Griffiths
- Department of Plant Sciences, University of Cambridge, Cambridge, United Kingdom
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12
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Robinson SA, Klekociuk AR, King DH, Pizarro Rojas M, Zúñiga GE, Bergstrom DM. The 2019/2020 summer of Antarctic heatwaves. GLOBAL CHANGE BIOLOGY 2020; 26:3178-3180. [PMID: 32227664 DOI: 10.1111/gcb.15083] [Citation(s) in RCA: 31] [Impact Index Per Article: 7.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/10/2020] [Accepted: 03/10/2020] [Indexed: 05/08/2023]
Abstract
This summer, a heatwave across Antarctica saw temperatures soar above average. Temperatures above zero are especially significant because they accelerate ice melt. Casey Station had its highest temperature ever, reaching a maximum of 9.2°C and minimum of 2.5°C. The highest temperature in Antarctica was 20.75°C on 9 February. Here we discuss the biological implications of such extreme events.
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Affiliation(s)
- Sharon A Robinson
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmosphere and Life Sciences & Global Challenges Program, University of Wollongong, Wollongong, NSW, Australia
| | - Andrew R Klekociuk
- Australian Antarctic Division, Department of Agriculture, Water and the Environment, Kingston, Tas., Australia
- Australian Antarctic Program Partnership, University of Tasmania, Hobart, Tas., Australia
| | - Diana H King
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmosphere and Life Sciences & Global Challenges Program, University of Wollongong, Wollongong, NSW, Australia
| | - Marisol Pizarro Rojas
- Facultad de Química y Biología and CEDENNA, Universidad de Santiago de Chile, Santiago, Chile
| | - Gustavo E Zúñiga
- Facultad de Química y Biología and CEDENNA, Universidad de Santiago de Chile, Santiago, Chile
| | - Dana M Bergstrom
- Centre for Sustainable Ecosystem Solutions, School of Earth, Atmosphere and Life Sciences & Global Challenges Program, University of Wollongong, Wollongong, NSW, Australia
- Australian Antarctic Division, Department of Agriculture, Water and the Environment, Kingston, Tas., Australia
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13
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Häder DP, Barnes PW. Comparing the impacts of climate change on the responses and linkages between terrestrial and aquatic ecosystems. THE SCIENCE OF THE TOTAL ENVIRONMENT 2019; 682:239-246. [PMID: 31121350 DOI: 10.1016/j.scitotenv.2019.05.024] [Citation(s) in RCA: 28] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/05/2019] [Revised: 04/23/2019] [Accepted: 05/03/2019] [Indexed: 05/20/2023]
Abstract
Aquatic and terrestrial organisms are being exposed to a number of anthropogenically-induced environmental stresses as a consequence of climate change. In addition, climate change is altering various linkages that exist between ecosystems on land and in water. Here we compare and contrast how climate change is altering aquatic and terrestrial environments and address some of the ways that the organisms in these ecosystems, especially the primary producers, are being affected by climate change factors, including changes in temperature, moisture, atmospheric carbon dioxide and solar UV radiation. Whereas there are some responses to climate change in common between terrestrial and aquatic ecosystems (e.g., changes in species composition and shifting geographic ranges and distributions), there are also responses that fundamentally differ between these two (e.g., responses to UV radiation). Climate change is also disrupting land-water connections in ways that influence biogeochemical and hydrologic cycles, and biosphere-atmosphere interactions in ways that can modify how aquatic and terrestrial ecosystems are affected by climate change and can influence climate change. The effects of climate change on these ecosystems are having wide-ranging effects on ecosystem biodiversity, structure and function and the abilities of these systems to provide essential services.
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Affiliation(s)
- Donat-P Häder
- Friedrich-Alexander University Erlangen-Nürnberg, Dept. Biology, 91096 Möhrendorf, Neue Str. 9, Germany.
| | - Paul W Barnes
- Loyola University New Orleans, Dept. Biological Sciences and Environment Program, 6363 St. Charles Ave., New Orleans, LA 70118, USA
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14
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Sulzberger B, Austin AT, Cory RM, Zepp RG, Paul ND. Solar UV radiation in a changing world: roles of cryosphere-land-water-atmosphere interfaces in global biogeochemical cycles. Photochem Photobiol Sci 2019; 18:747-774. [PMID: 30810562 PMCID: PMC7418111 DOI: 10.1039/c8pp90063a] [Citation(s) in RCA: 36] [Impact Index Per Article: 7.2] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/19/2018] [Accepted: 12/19/2018] [Indexed: 12/29/2022]
Abstract
Global change influences biogeochemical cycles within and between environmental compartments (i.e., the cryosphere, terrestrial and aquatic ecosystems, and the atmosphere). A major effect of global change on carbon cycling is altered exposure of natural organic matter (NOM) to solar radiation, particularly solar UV radiation. In terrestrial and aquatic ecosystems, NOM is degraded by UV and visible radiation, resulting in the emission of carbon dioxide (CO2) and carbon monoxide, as well as a range of products that can be more easily degraded by microbes (photofacilitation). On land, droughts and land-use change can reduce plant cover causing an increase in exposure of plant litter to solar radiation. The altered transport of soil organic matter from terrestrial to aquatic ecosystems also can enhance exposure of NOM to solar radiation. An increase in emission of CO2 from terrestrial and aquatic ecosystems due to the effects of global warming, such as droughts and thawing of permafrost soils, fuels a positive feedback on global warming. This is also the case for greenhouse gases other than CO2, including methane and nitrous oxide, that are emitted from terrestrial and aquatic ecosystems. These trace gases also have indirect or direct impacts on stratospheric ozone concentrations. The interactive effects of UV radiation and climate change greatly alter the fate of synthetic and biological contaminants. Contaminants are degraded or inactivated by direct and indirect photochemical reactions. The balance between direct and indirect photodegradation or photoinactivation of contaminants is likely to change with future changes in stratospheric ozone, and with changes in runoff of coloured dissolved organic matter due to climate and land-use changes.
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Affiliation(s)
- B Sulzberger
- Eawag: Swiss Federal Institute of Aquatic Science and Technology, Duebendorf, Switzerland.
| | - A T Austin
- Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA) and Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Facultad de Agronomía, Universidad de Buenos Aires en las afiliations, Buenos Aires, Argentina
| | - R M Cory
- University of Michigan, Earth & Environmental Science, Ann Arbor, Michigan, USA
| | - R G Zepp
- United States Environmental Protection Agency, Athens, Georgia, USA
| | - N D Paul
- Lancaster Environment Centre, Lancaster University, LA1 4YQ, UK
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15
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Wilson SR, Madronich S, Longstreth JD, Solomon KR. Interactive effects of changing stratospheric ozone and climate on tropospheric composition and air quality, and the consequences for human and ecosystem health. Photochem Photobiol Sci 2019; 18:775-803. [PMID: 30810564 DOI: 10.1039/c8pp90064g] [Citation(s) in RCA: 35] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/15/2022]
Abstract
The composition of the air we breathe is determined by emissions, weather, and photochemical transformations induced by solar UV radiation. Photochemical reactions of many emitted chemical compounds can generate important (secondary) pollutants including ground-level ozone (O3) and some particulate matter, known to be detrimental to human health and ecosystems. Poor air quality is the major environmental cause of premature deaths globally, and even a small decrease in air quality can translate into a large increase in the number of deaths. In many regions of the globe, changes in emissions of pollutants have caused significant changes in air quality. Short-term variability in the weather as well as long-term climatic trends can affect ground-level pollution through several mechanisms. These include large-scale changes in the transport of O3 from the stratosphere to the troposphere, winds, clouds, and patterns of precipitation. Long-term trends in UV radiation, particularly related to the depletion and recovery of stratospheric ozone, are also expected to result in changes in air quality as well as the self-cleaning capacity of the global atmosphere. The increased use of substitutes for ozone-depleting substances, in response to the Montreal Protocol, does not currently pose a significant risk to the environment. This includes both the direct emissions of substitutes during use and their atmospheric degradation products (e.g. trifluoroacetic acid, TFA).
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Affiliation(s)
- S R Wilson
- Centre for Atmospheric Chemistry, School of Earth, Atmosphere and Life Sciences, University of Wollongong, NSW, Australia.
| | - S Madronich
- National Center for Atmospheric Research, Boulder, CO, USA
| | - J D Longstreth
- The Institute for Global Risk Research, LLC, Bethesda, MD, USA and Emergent BioSolutions, Gaithersburg, MD, USA
| | - K R Solomon
- Centre for Toxicology and School of Environmental Sciences, University of Guelph, ON, Canada
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16
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Williamson CE, Neale PJ, Hylander S, Rose KC, Figueroa FL, Robinson SA, Häder DP, Wängberg SÅ, Worrest RC. The interactive effects of stratospheric ozone depletion, UV radiation, and climate change on aquatic ecosystems. Photochem Photobiol Sci 2019; 18:717-746. [DOI: 10.1039/c8pp90062k] [Citation(s) in RCA: 78] [Impact Index Per Article: 15.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/28/2022]
Abstract
Summary of current knowledge about effects of UV radiation in inland and oceanic waters related to stratospheric ozone depletion and climate change.
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Affiliation(s)
| | | | - Samuel Hylander
- Centre for Ecology and Evolution in Microbial model Systems
- Linnaeus Univ
- Kalmar
- Sweden
| | - Kevin C. Rose
- Department of Biological Sciences
- Rensselaer Polytechnic Institute
- Troy
- USA
| | | | - Sharon A. Robinson
- Centre for Sustainable Ecosystem Solutions
- School of Earth
- Atmosphere and Life Sciences and Global Challenges Program
- University of Wollongong
- Australia
| | - Donat-P. Häder
- Department of Biology
- Friedrich-Alexander Universität
- Möhrendorf
- Germany
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17
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Li C, Liu S, Zhang W, Chen K, Zhang P. Transcriptional profiling and physiological analysis reveal the critical roles of ROS-scavenging system in the Antarctic moss Pohlia nutans under Ultraviolet-B radiation. PLANT PHYSIOLOGY AND BIOCHEMISTRY : PPB 2019; 134:113-122. [PMID: 30448024 DOI: 10.1016/j.plaphy.2018.10.034] [Citation(s) in RCA: 13] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/31/2018] [Revised: 09/23/2018] [Accepted: 10/30/2018] [Indexed: 05/21/2023]
Abstract
Organisms suffer more harmful ultraviolet radiation in the Antarctica due to the ozone layer destruction. Bryophytes are the dominant flora in the Antarctic continent. However, the molecular mechanism of Antarctic moss adaptation to UV-B radiation remains unclear. In the research, the transcriptional profiling of the Antarctic moss Pohlia nutans under UV-B radiation was conducted by Illumina HiSeq2500 platform. Totally, 72,922 unigenes with N50 length of 1434 bp were generated. Differential expression analysis demonstrated that 581 unigenes were markedly up-regulated and 249 unigenes were significantly down-regulated. The gene clustering analysis showed that these differentially expressed genes (DEGs) includes several transcription factors, photolyases, antioxidant enzymes, and flavonoid biosynthesis-related genes. Further analyses suggested that the content of malondialdehyde (MDA), the activities of several antioxidant enzymes (i.e., catalase, peroxidase, and glutathione reductase) were significantly enhanced upon UV-B treatment. Furthermore, the content of flavonoids and the gene expression levels of their synthesis-related enzymes were also markedly increased when plants were exposed to UV-B light. Therefore, these results suggested that the pathways of antioxidant enzymes, flavonoid synthesis and photolyases were the main defense systems that contributed to the adaption of Pohlia nutans to the enhanced UV-B radiation in Antarctica.
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Affiliation(s)
- Chengcheng Li
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Jinan, 250100, China
| | - Shenghao Liu
- Key Laboratory of Marine Bioactive Substance, The First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
| | - Wei Zhang
- School of Environment, Qingdao University, Qingdao, 266061, China
| | - Kaoshan Chen
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Jinan, 250100, China
| | - Pengying Zhang
- National Glycoengineering Research Center, School of Life Sciences, Shandong University, Jinan, 250100, China.
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18
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Bornman JF, Barnes PW, Robson TM, Robinson SA, Jansen MAK, Ballaré CL, Flint SD. Linkages between stratospheric ozone, UV radiation and climate change and their implications for terrestrial ecosystems. Photochem Photobiol Sci 2019; 18:681-716. [DOI: 10.1039/c8pp90061b] [Citation(s) in RCA: 90] [Impact Index Per Article: 18.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
Linkages between stratospheric ozone, UV radiation and climate change: terrestrial ecosystems.
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Affiliation(s)
- Janet F. Bornman
- College of Science
- Health
- Engineering and Education
- Murdoch University
- Perth
| | - Paul W. Barnes
- Department of Biological Sciences and Environment Program
- Loyola University
- USA
| | - T. Matthew Robson
- Research Programme in Organismal and Evolutionary Biology
- Viikki Plant Science Centre
- University of Helsinki
- Finland
| | - Sharon A. Robinson
- Centre for Sustainable Ecosystem Solutions
- School of Earth
- Atmosphere and Life Sciences and Global Challenges Program
- University of Wollongong
- Wollongong
| | - Marcel A. K. Jansen
- Plant Ecophysiology Group
- School of Biological
- Earth and Environmental Sciences
- UCC
- Cork
| | - Carlos L. Ballaré
- University of Buenos Aires
- Faculty of Agronomy and IFEVA-CONICET, and IIB
- National University of San Martin
- Buenos Aires
- Argentina
| | - Stephan D. Flint
- Department of Forest
- Rangeland and Fire Sciences
- University of Idaho
- Moscow
- USA
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19
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Waterman MJ, Bramley-Alves J, Miller RE, Keller PA, Robinson SA. Photoprotection enhanced by red cell wall pigments in three East Antarctic mosses. Biol Res 2018; 51:49. [PMID: 30463628 PMCID: PMC6247747 DOI: 10.1186/s40659-018-0196-1] [Citation(s) in RCA: 20] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/06/2017] [Accepted: 11/03/2018] [Indexed: 11/21/2022] Open
Abstract
BACKGROUND Antarctic bryophytes (mosses and liverworts) are resilient to physiologically extreme environmental conditions including elevated levels of ultraviolet (UV) radiation due to depletion of stratospheric ozone. Many Antarctic bryophytes synthesise UV-B-absorbing compounds (UVAC) that are localised in their cells and cell walls, a location that is rarely investigated for UVAC in plants. This study compares the concentrations and localisation of intracellular and cell wall UVAC in Antarctic Ceratodon purpureus, Bryum pseudotriquetrum and Schistidium antarctici from the Windmill Islands, East Antarctica. RESULTS Multiple stresses, including desiccation and naturally high UV and visible light, seemed to enhance the incorporation of total UVAC including red pigments in the cell walls of all three Antarctic species analysed. The red growth form of C. purpureus had significantly higher levels of cell wall bound and lower intracellular UVAC concentrations than its nearby green form. Microscopic and spectroscopic analyses showed that the red colouration in this species was associated with the cell wall and that these red cell walls contained less pectin and phenolic esters than the green form. All three moss species showed a natural increase in cell wall UVAC content during the growing season and a decline in these compounds in new tissue grown under less stressful conditions in the laboratory. CONCLUSIONS UVAC and red pigments are tightly bound to the cell wall and likely have a long-term protective role in Antarctic bryophytes. Although the identity of these red pigments remains unknown, our study demonstrates the importance of investigating cell wall UVAC in plants and contributes to our current understanding of UV-protective strategies employed by particular Antarctic bryophytes. Studies such as these provide clues to how these plants survive in such extreme habitats and are helpful in predicting future survival of the species studied.
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Affiliation(s)
- Melinda J. Waterman
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW 2522 Australia
- Department of Chemistry and Biology, University of Santiago, Alameda, 3363 Santiago, Chile
| | - Jessica Bramley-Alves
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW 2522 Australia
| | - Rebecca E. Miller
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW 2522 Australia
- School of Ecosystem and Forest Sciences, University of Melbourne, Richmond, VIC 3121 Australia
| | - Paul A. Keller
- School of Chemistry, University of Wollongong, Wollongong, NSW 2522 Australia
| | - Sharon A. Robinson
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW 2522 Australia
- Department of Chemistry and Biology, University of Santiago, Alameda, 3363 Santiago, Chile
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20
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Núñez-Pons L, Avila C, Romano G, Verde C, Giordano D. UV-Protective Compounds in Marine Organisms from the Southern Ocean. Mar Drugs 2018; 16:E336. [PMID: 30223486 PMCID: PMC6165330 DOI: 10.3390/md16090336] [Citation(s) in RCA: 26] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/12/2018] [Revised: 09/03/2018] [Accepted: 09/12/2018] [Indexed: 12/20/2022] Open
Abstract
Solar radiation represents a key abiotic factor in the evolution of life in the oceans. In general, marine, biota-particularly in euphotic and dysphotic zones-depends directly or indirectly on light, but ultraviolet radiation (UV-R) can damage vital molecular machineries. UV-R induces the formation of reactive oxygen species (ROS) and impairs intracellular structures and enzymatic reactions. It can also affect organismal physiologies and eventually alter trophic chains at the ecosystem level. In Antarctica, physical drivers, such as sunlight, sea-ice, seasonality and low temperature are particularly influencing as compared to other regions. The springtime ozone depletion over the Southern Ocean makes organisms be more vulnerable to UV-R. Nonetheless, Antarctic species seem to possess analogous UV photoprotection and repair mechanisms as those found in organisms from other latitudes. The lack of data on species-specific responses towards increased UV-B still limits the understanding about the ecological impact and the tolerance levels related to ozone depletion in this region. The photobiology of Antarctic biota is largely unknown, in spite of representing a highly promising reservoir in the discovery of novel cosmeceutical products. This review compiles the most relevant information on photoprotection and UV-repair processes described in organisms from the Southern Ocean, in the context of this unique marine polar environment.
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Affiliation(s)
- Laura Núñez-Pons
- Department of Biology and Evolution of Marine Organisms (BEOM), Stazione Zoologica Anton Dohrn (SZN), 80121 Villa Comunale, Napoli, Italy.
| | - Conxita Avila
- Department of Evolutionary Biology, Ecology, and Environmental Sciences, and Biodiversity Research Institute (IrBIO), Faculty of Biology, University of Barcelona, Av. Diagonal 643, 08028 Barcelona, Catalonia, Spain.
| | - Giovanna Romano
- Department of Marine Biotechnology (Biotech), Stazione Zoologica Anton Dohrn (SZN), 80121 Villa Comunale, Napoli, Italia.
| | - Cinzia Verde
- Department of Biology and Evolution of Marine Organisms (BEOM), Stazione Zoologica Anton Dohrn (SZN), 80121 Villa Comunale, Napoli, Italy.
- Institute of Biosciences and BioResources (IBBR), CNR, Via Pietro Castellino 111, 80131 Napoli, Italy.
| | - Daniela Giordano
- Department of Biology and Evolution of Marine Organisms (BEOM), Stazione Zoologica Anton Dohrn (SZN), 80121 Villa Comunale, Napoli, Italy.
- Institute of Biosciences and BioResources (IBBR), CNR, Via Pietro Castellino 111, 80131 Napoli, Italy.
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21
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Bais F, Luca RM, Bornman JF, Williamson CE, Sulzberger B, Austin AT, Wilson SR, Andrady AL, Bernhard G, McKenzie RL, Aucamp PJ, Madronich S, Neale RE, Yazar S, Young AR, de Gruijl FR, Norval M, Takizawa Y, Barnes PW, Robson TM, Robinson SA, Ballaré CL, Flint SD, Neale PJ, Hylander S, Rose KC, Wängberg SÅ, Häder DP, Worrest RC, Zepp RG, Paul ND, Cory RM, Solomon KR, Longstreth J, Pandey KK, Redhwi HH, Torikai A, Heikkilä AM. Environmental effects of ozone depletion, UV radiation and interactions with climate change: UNEP Environmental Effects Assessment Panel, update 2017. Photochem Photobiol Sci 2018; 17:127-179. [PMID: 29404558 PMCID: PMC6155474 DOI: 10.1039/c7pp90043k] [Citation(s) in RCA: 88] [Impact Index Per Article: 14.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/21/2017] [Accepted: 12/21/2017] [Indexed: 12/11/2022]
Abstract
The Environmental Effects Assessment Panel (EEAP) is one of three Panels of experts that inform the Parties to the Montreal Protocol. The EEAP focuses on the effects of UV radiation on human health, terrestrial and aquatic ecosystems, air quality, and materials, as well as on the interactive effects of UV radiation and global climate change. When considering the effects of climate change, it has become clear that processes resulting in changes in stratospheric ozone are more complex than previously held. Because of the Montreal Protocol, there are now indications of the beginnings of a recovery of stratospheric ozone, although the time required to reach levels like those before the 1960s is still uncertain, particularly as the effects of stratospheric ozone on climate change and vice versa, are not yet fully understood. Some regions will likely receive enhanced levels of UV radiation, while other areas will likely experience a reduction in UV radiation as ozone- and climate-driven changes affect the amounts of UV radiation reaching the Earth's surface. Like the other Panels, the EEAP produces detailed Quadrennial Reports every four years; the most recent was published as a series of seven papers in 2015 (Photochem. Photobiol. Sci., 2015, 14, 1-184). In the years in between, the EEAP produces less detailed and shorter Update Reports of recent and relevant scientific findings. The most recent of these was for 2016 (Photochem. Photobiol. Sci., 2017, 16, 107-145). The present 2017 Update Report assesses some of the highlights and new insights about the interactive nature of the direct and indirect effects of UV radiation, atmospheric processes, and climate change. A full 2018 Quadrennial Assessment, will be made available in 2018/2019.
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Affiliation(s)
- F. Bais
- Aristotle Univ. of Thessaloniki, Laboratory of Atmospheric Physics, Thessaloniki, Greece
| | - R. M. Luca
- National Centre for Epidemiology and Population Health, Australian National Univ., Canberra, Australia
| | - J. F. Bornman
- Curtin Univ., Curtin Business School, Perth, Australia
| | | | - B. Sulzberger
- Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland
| | - A. T. Austin
- Univ. of Buenos Aires, Faculty of Agronomy and IFEVA-CONICET, Buenos Aires, Argentina
| | - S. R. Wilson
- School of Chemistry, Centre for Atmospheric Chemistry, Univ. of Wollongong, Wollongong, Australia
| | - A. L. Andrady
- Department of Chemical and Biomolecular Engineering, North Carolina State Univ., Raleigh, NC, USA
| | - G. Bernhard
- Biospherical Instruments Inc., San Diego, CA, USA
| | | | - P. J. Aucamp
- Ptersa Environmental Consultants, Faerie Glen, South Africa
| | - S. Madronich
- National Center for Atmospheric Research, Boulder, Colorado, USA
| | - R. E. Neale
- Queensland Institute of Medical Research, Royal Brisbane Hospital, Brisbane, Australia
| | - S. Yazar
- Univ. of Western Australia, Centre for Ophthalmology and Visual Science, Lions Eye Institute, Perth, Australia
| | | | - F. R. de Gruijl
- Department of Dermatology, Leiden Univ. Medical Centre, Leiden, The Netherlands
| | - M. Norval
- Univ. of Edinburgh Medical School, UK
| | - Y. Takizawa
- Akita Univ. School of Medicine, National Institute for Minamata Disease, Nakadai, Itabashiku, Tokyo, Japan
| | - P. W. Barnes
- Department of Biological Sciences and Environment Program, Loyola Univ., New Orleans, USA
| | - T. M. Robson
- Research Programme in Organismal and Evolutionary Biology, Viikki Plant Science Centre, Univ. of Helsinki, Finland
| | - S. A. Robinson
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, Univ. of Wollongong, Wollongong, NSW 2522, Australia
| | - C. L. Ballaré
- Univ. of Buenos Aires, Faculty of Agronomy and IFEVA-CONICET, Buenos Aires, Argentina
| | - S. D. Flint
- Dept of Forest, Rangeland and Fire Sciences, Univ. of Idaho, Moscow, ID, USA
| | - P. J. Neale
- Smithsonian Environmental Research Center, Edgewater, Maryland, USA
| | - S. Hylander
- Centre for Ecology and Evolution in Microbial model Systems, Linnaeus Univ., Kalmar, Sweden
| | - K. C. Rose
- Dept of Biological Sciences, Rensselaer Polytechnic Institute, Troy, NY, USA
| | - S.-Å. Wängberg
- Dept Marine Sciences, Univ. of Gothenburg, Göteborg, Sweden
| | - D.-P. Häder
- Friedrich-Alexander Univ. Erlangen-Nürnberg, Dept of Biology, Möhrendorf, Germany
| | - R. C. Worrest
- CIESIN, Columbia Univ., New Hartford, Connecticut, USA
| | - R. G. Zepp
- United States Environmental Protection Agency, Athens, Georgia, USA
| | - N. D. Paul
- Lanter Environment Centre, Lanter Univ., LA1 4YQ, UK
| | - R. M. Cory
- Earth and Environmental Sciences, Univ. of Michigan, Ann Arbor, MI, USA
| | - K. R. Solomon
- Centre for Toxicology, School of Environmental Sciences, Univ. of Guelph, Guelph, ON, Canada
| | - J. Longstreth
- The Institute for Global Risk Research, Bethesda, MD, USA
| | - K. K. Pandey
- Institute of Wood Science and Technology, Bengaluru, India
| | - H. H. Redhwi
- Chemical Engineering Dept, King Fahd Univ. of Petroleum and Minerals, Dhahran, Saudi Arabia
| | - A. Torikai
- Materials Life Society of Japan, Kayabacho Chuo-ku, Tokyo, Japan
| | - A. M. Heikkilä
- Finnish Meteorological Institute R&D/Climate Research, Helsinki, Finland
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22
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Pecl GT, Araújo MB, Bell JD, Blanchard J, Bonebrake TC, Chen IC, Clark TD, Colwell RK, Danielsen F, Evengård B, Falconi L, Ferrier S, Frusher S, Garcia RA, Griffis RB, Hobday AJ, Janion-Scheepers C, Jarzyna MA, Jennings S, Lenoir J, Linnetved HI, Martin VY, McCormack PC, McDonald J, Mitchell NJ, Mustonen T, Pandolfi JM, Pettorelli N, Popova E, Robinson SA, Scheffers BR, Shaw JD, Sorte CJB, Strugnell JM, Sunday JM, Tuanmu MN, Vergés A, Villanueva C, Wernberg T, Wapstra E, Williams SE. Biodiversity redistribution under climate change: Impacts on ecosystems and human well-being. Science 2017; 355:355/6332/eaai9214. [PMID: 28360268 DOI: 10.1126/science.aai9214] [Citation(s) in RCA: 968] [Impact Index Per Article: 138.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/24/2023]
Abstract
Distributions of Earth's species are changing at accelerating rates, increasingly driven by human-mediated climate change. Such changes are already altering the composition of ecological communities, but beyond conservation of natural systems, how and why does this matter? We review evidence that climate-driven species redistribution at regional to global scales affects ecosystem functioning, human well-being, and the dynamics of climate change itself. Production of natural resources required for food security, patterns of disease transmission, and processes of carbon sequestration are all altered by changes in species distribution. Consideration of these effects of biodiversity redistribution is critical yet lacking in most mitigation and adaptation strategies, including the United Nation's Sustainable Development Goals.
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Affiliation(s)
- Gretta T Pecl
- Institute for Marine and Antarctic Studies, Hobart, Tasmania 7001, Australia. .,Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia
| | - Miguel B Araújo
- Department of Biogeography and Global Change, Museo Nacional de Ciencias Naturales, Consejo Superior de Investigaciones Científicas, 28006 Madrid, Spain.,Centro de Investigação em Biodiversidade e Recursos Geneticos, Universidade de Évora, 7000-890 Évora, Portugal.,Department of Biology, Center for Macroecology, Evolution and Climate, University of Copenhagen, Universitetsparken 15, 2100 Copenhagen O, Denmark
| | - Johann D Bell
- Australian National Centre for Ocean Resources and Security, University of Wollongong, New South Wales 2522, Australia.,Betty and Gordon Moore Center for Science and Oceans, Conservation International, Arlington, VA 22202, USA
| | - Julia Blanchard
- Institute for Marine and Antarctic Studies, Hobart, Tasmania 7001, Australia.,Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia
| | - Timothy C Bonebrake
- School of Biological Sciences, The University of Hong Kong, Hong Kong SAR, China
| | - I-Ching Chen
- Department of Life Sciences, National Cheng Kung University, Tainan 701, Taiwan, Republic of China
| | - Timothy D Clark
- Institute for Marine and Antarctic Studies, Hobart, Tasmania 7001, Australia.,Commonwealth Scientific and Industrial Research Organization (CSIRO) Agriculture and Food, Hobart, Tasmania 7000, Australia
| | - Robert K Colwell
- Department of Biology, Center for Macroecology, Evolution and Climate, University of Copenhagen, Universitetsparken 15, 2100 Copenhagen O, Denmark.,Department of Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269, USA.,University of Colorado Museum of Natural History, Boulder, CO 80309, USA.,Departmento de Ecologia, Universidade Federal de Goiás, CP 131, 74.001-970 Goiânia, Goiás, Brazil
| | | | - Birgitta Evengård
- Division of Infectious Diseases, Department of Clinical Microbiology, Umea University, 90187 Umea, Sweden
| | - Lorena Falconi
- College of Marine and Environmental Science, James Cook University, Townsville, Queensland 4811, Australia
| | - Simon Ferrier
- CSIRO Land and Water, Canberra, Australian Capital Territory 2601, Australia
| | - Stewart Frusher
- Institute for Marine and Antarctic Studies, Hobart, Tasmania 7001, Australia.,Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia
| | - Raquel A Garcia
- Centre for Statistics in Ecology, the Environment and Conservation, Department of Statistical Sciences, University of Cape Town, Rondebosch 7701, Cape Town, South Africa.,Centre for Invasion Biology, Department of Botany and Zoology, Faculty of Science, Stellenbosch University, Matieland 7602, South Africa
| | - Roger B Griffis
- National Oceanic and Atmospheric Administration (NOAA) Fisheries Service, Silver Spring, MD 20912, USA
| | - Alistair J Hobday
- Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia.,CSIRO Oceans and Atmosphere, Hobart, Tasmania 7000, Australia
| | | | - Marta A Jarzyna
- Department of Ecology and Evolutionary Biology, Yale University, New Haven, CT 06520, USA
| | - Sarah Jennings
- Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia.,Tasmanian School of Business and Economics, University of Tasmania, Hobart, Tasmania 7001, Australia
| | - Jonathan Lenoir
- EDYSAN (FRE 3498 CNRS-UPJV), Université de Picardie Jules Verne, 80037 Amiens Cedex 1, France
| | - Hlif I Linnetved
- Institute of Food and Resource Economics, Faculty of Science, University of Copenhagen, Rolighedsvej 25, DK-1958 Frederiksberg C, Denmark
| | - Victoria Y Martin
- School of Environment, Science and Engineering, Southern Cross University, Lismore, New South Wales 2480, Australia
| | | | - Jan McDonald
- Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia.,Faculty of Law, University of Tasmania, Hobart, Tasmania 7001, Australia
| | - Nicola J Mitchell
- School of Biological Sciences, The University of Western Australia, Crawley, Western Australia 6009, Australia
| | - Tero Mustonen
- Snowchange Cooperative, University of Eastern Finland, Joensuu, FIN 80100 Finland
| | - John M Pandolfi
- School of Biological Sciences, Autralian Research Council (ARC) Centre of Excellence for Coral Reef Studies, The University of Queensland, Brisbane, Queensland 4072, Australia
| | - Nathalie Pettorelli
- Institute of Zoology, Zoological Society of London, Regent's Park, NW1 4RY London, UK
| | - Ekaterina Popova
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
| | - Sharon A Robinson
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Wollongong, New South Wales 2522, Australia
| | - Brett R Scheffers
- Department of Wildlife Ecology and Conservation, Institute of Food and Agricultural Sciences, University of Florida, Gainesville, FL 32611, USA
| | - Justine D Shaw
- Centre for Biodiversity and Conservation Science, School of Biological Sciences, The University of Queensland, St Lucia, Queensland 4072, Australia
| | - Cascade J B Sorte
- Department of Ecology and Evolutionary Biology, University of California, Irvine, CA 92697, USA
| | - Jan M Strugnell
- Centre for Sustainable Tropical Fisheries and Aquaculture, College of Science and Engineering, James Cook University, Townsville, 4811 Queensland, Australia.,Department of Ecology, Environment and Evolution, School of Life Sciences, La Trobe University, Melbourne, Victoria 3086, Australia
| | - Jennifer M Sunday
- Biodiversity Research Centre, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada
| | - Mao-Ning Tuanmu
- Biodiversity Research Center, Academia Sinica, Taipei 115, Taiwan, Republic of China
| | - Adriana Vergés
- Centre for Marine Bio-Innovation and Evolution and Ecology Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales 2052, Australia
| | - Cecilia Villanueva
- Institute for Marine and Antarctic Studies, Hobart, Tasmania 7001, Australia.,Centre for Marine Socioecology, Hobart, Tasmania 7001, Australia
| | - Thomas Wernberg
- School of Biological Sciences, The University of Western Australia, Crawley, Western Australia 6009, Australia.,Oceans Institute, The University of Western Australia, Perth, Western Australia 6009, Australia
| | - Erik Wapstra
- School of Biological Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia
| | - Stephen E Williams
- College of Marine and Environmental Science, James Cook University, Townsville, Queensland 4811, Australia
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23
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Waterman MJ, Nugraha AS, Hendra R, Ball GE, Robinson SA, Keller PA. Antarctic Moss Biflavonoids Show High Antioxidant and Ultraviolet-Screening Activity. JOURNAL OF NATURAL PRODUCTS 2017; 80:2224-2231. [PMID: 28783339 DOI: 10.1021/acs.jnatprod.7b00085] [Citation(s) in RCA: 27] [Impact Index Per Article: 3.9] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/08/2023]
Abstract
Ceratodon purpureus is a cosmopolitan moss that survives some of the harshest places on Earth: from frozen Antarctica to hot South Australian deserts. In a study on the survival mechanisms of the species, nine compounds were isolated from Australian and Antarctic C. purpureus. This included five biflavonoids, with complete structural elucidation of 1 and 2 reported here for the first time, as well as an additional four known phenolic compounds. Dispersion-corrected DFT calculations suggested a rotational barrier, leading to atropisomerism, resulting in the presence of diastereomers for compound 2. All isolates absorbed strongly in the ultraviolet (UV) spectrum, e.g., biflavone 1 (UV-A, 315-400 nm), which displayed the strongest radical-scavenging activity, 13% more efficient than the standard rutin; p-coumaric acid and trans-ferulic acid showed the highest UV-B (280-315 nm) absorption. The more complex and abundant 1 and 2 presumably have dual roles as both UV-screening and antioxidant compounds. They are strongly bound to Antarctic moss cell walls as well as located inside the cells of moss from both locations. The combined high stability and photoprotective abilities of these isolates may account for the known resilience of this species to UV-B radiation and its survival in some of the toughest locations in the world.
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Affiliation(s)
| | | | | | - Graham E Ball
- School of Chemistry, UNSW , Sydney, NSW 2052, Australia
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24
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Malenovský Z, Lucieer A, King DH, Turnbull JD, Robinson SA. Unmanned aircraft system advances health mapping of fragile polar vegetation. Methods Ecol Evol 2017. [DOI: 10.1111/2041-210x.12833] [Citation(s) in RCA: 54] [Impact Index Per Article: 7.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- Zbyněk Malenovský
- Surveying and Spatial Sciences Group School of Land and Food University of Tasmania Hobart Tas. Australia
- Centre for Sustainable Ecosystem Solutions School of Biological Sciences University of Wollongong Wollongong NSW Australia
- Biospheric Sciences Laboratory USRA/GESTAR NASA Goddard Space Flight Center Greenbelt MD USA
| | - Arko Lucieer
- Surveying and Spatial Sciences Group School of Land and Food University of Tasmania Hobart Tas. Australia
| | - Diana H. King
- Centre for Sustainable Ecosystem Solutions School of Biological Sciences University of Wollongong Wollongong NSW Australia
| | - Johanna D. Turnbull
- Centre for Sustainable Ecosystem Solutions School of Biological Sciences University of Wollongong Wollongong NSW Australia
| | - Sharon A. Robinson
- Centre for Sustainable Ecosystem Solutions School of Biological Sciences University of Wollongong Wollongong NSW Australia
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25
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Lee JR, Raymond B, Bracegirdle TJ, Chadès I, Fuller RA, Shaw JD, Terauds A. Climate change drives expansion of Antarctic ice-free habitat. Nature 2017; 547:49-54. [DOI: 10.1038/nature22996] [Citation(s) in RCA: 193] [Impact Index Per Article: 27.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/05/2016] [Accepted: 05/18/2017] [Indexed: 02/06/2023]
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26
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Václavík T, Beckmann M, Cord AF, Bindewald AM. Effects of UV-B radiation on leaf hair traits of invasive plants-Combining historical herbarium records with novel remote sensing data. PLoS One 2017; 12:e0175671. [PMID: 28414764 PMCID: PMC5393584 DOI: 10.1371/journal.pone.0175671] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/12/2017] [Accepted: 03/29/2017] [Indexed: 11/19/2022] Open
Abstract
Ultraviolet-B (UV-B) radiation is a key but under-researched environmental factor that initiates diverse responses in plants, potentially affecting their distribution. To date, only a few macroecological studies have examined adaptations of plant species to different levels of UV-B. Here, we combined herbarium specimens of Hieracium pilosella L. and Echium vulgare L. with a novel UV-B dataset to examine differences in leaf hair traits between the plants' native and alien ranges. We analysed scans of 336 herbarium specimens using standardized measurements of leaf area, hair density (both species) and hair length (H. pilosella only). While accounting for other bioclimatic variables (i.e. temperature, precipitation) and effects of herbivory, we examined whether UV-B exposure explains the variability and geographical distribution of these traits in the native (Northern Hemisphere) vs. the alien (Southern Hemisphere) range. UV-B explained the largest proportion of the variability and geographical distribution of hair length in H. pilosella (relative influence 67.1%), and hair density in E. vulgare (66.2%). Corresponding with higher UV-B, foliar hairs were 25% longer for H. pilosella and 25% denser for E. vulgare in records from the Southern as compared to those from the Northern Hemisphere. However, focusing on each hemisphere separately or controlling for its effect in a regression analysis, we found no apparent influence of UV-B radiation on hair traits. Thus, our findings did not confirm previous experimental studies which suggested that foliar hairs may respond to higher UV-B intensities, presumably offering protection against detrimental levels of radiation. We cannot rule out UV-B radiation as a possible driver because UV-B radiation was the only considered variable that differed substantially between the hemispheres, while bioclimatic conditions (e.g. temperature, precipitation) and other considered variables (herbivory damage, collection date) were at similar levels. However, given that either non-significant or inconclusive relationships were detected within hemispheres, alternative explanations of the differences in foliar hairs are more likely, including the effects of environment, genotypes or herbivory.
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Affiliation(s)
- Tomáš Václavík
- UFZ-Helmholtz Centre for Environmental Research, Department of Computational Landscape Ecology, Leipzig, Germany
- Palacký University Olomouc, Department of Ecology and Environmental Sciences, Faculty of Science, Olomouc, Czech Republic
| | - Michael Beckmann
- UFZ-Helmholtz Centre for Environmental Research, Department of Computational Landscape Ecology, Leipzig, Germany
| | - Anna F Cord
- UFZ-Helmholtz Centre for Environmental Research, Department of Computational Landscape Ecology, Leipzig, Germany
| | - Anja M Bindewald
- UFZ-Helmholtz Centre for Environmental Research, Department of Computational Landscape Ecology, Leipzig, Germany
- University of Applied Sciences Bremen, Bremen, Germany
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27
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Kuttippurath J, Nair PJ. The signs of Antarctic ozone hole recovery. Sci Rep 2017; 7:585. [PMID: 28373709 PMCID: PMC5429648 DOI: 10.1038/s41598-017-00722-7] [Citation(s) in RCA: 55] [Impact Index Per Article: 7.9] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/13/2016] [Accepted: 03/09/2017] [Indexed: 11/09/2022] Open
Abstract
Absorption of solar radiation by stratospheric ozone affects atmospheric dynamics and chemistry, and sustains life on Earth by preventing harmful radiation from reaching the surface. Significant ozone losses due to increases in the abundances of ozone depleting substances (ODSs) were first observed in Antarctica in the 1980s. Losses deepened in following years but became nearly flat by around 2000, reflecting changes in global ODS emissions. Here we show robust evidence that Antarctic ozone has started to recover in both spring and summer, with a recovery signal identified in springtime ozone profile and total column measurements at 99% confidence for the first time. Continuing recovery is expected to impact the future climate of that region. Our results demonstrate that the Montreal Protocol has indeed begun to save the Antarctic ozone layer.
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Affiliation(s)
- Jayanarayanan Kuttippurath
- CORAL, Indian Institute of Technology Kharagpur, Kharagpur, 721302, India. .,LATMOS/CNRS, UPMC University of Paris 06, Paris, France.
| | - Prijitha J Nair
- CORAL, Indian Institute of Technology Kharagpur, Kharagpur, 721302, India.,Centre for Earth Science Studies, Thiruvananthapuram, India
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28
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Environmental effects of ozone depletion and its interactions with climate change: Progress report, 2016. Photochem Photobiol Sci 2017; 16:107-145. [PMID: 28124708 PMCID: PMC6400464 DOI: 10.1039/c7pp90001e] [Citation(s) in RCA: 33] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/05/2017] [Accepted: 01/05/2017] [Indexed: 12/12/2022]
Abstract
The Parties to the Montreal Protocol are informed by three Panels of experts. One of these is the Environmental Effects Assessment Panel (EEAP), which deals with two focal issues. The first focus is the effects of UV radiation on human health, animals, plants, biogeochemistry, air quality, and materials. The second focus is on interactions between UV radiation and global climate change and how these may affect humans and the environment. When considering the effects of climate change, it has become clear that processes resulting in changes in stratospheric ozone are more complex than previously believed. As a result of this, human health and environmental issues will be longer-lasting and more regionally variable. Like the other Panels, the EEAP produces a detailed report every four years; the most recent was published as a series of seven papers in 2015 (Photochem. Photobiol. Sci., 2015, 14, 1-184). In the years in between, the EEAP produces less detailed and shorter Progress Reports of the relevant scientific findings. The most recent of these was for 2015 (Photochem. Photobiol. Sci., 2016, 15, 141-147). The present Progress Report for 2016 assesses some of the highlights and new insights with regard to the interactive nature of the direct and indirect effects of UV radiation, atmospheric processes, and climate change. The more detailed Quadrennial Assessment will be made available in 2018.
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29
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Environmental effects of ozone depletion and its interactions with climate change: progress report, 2015. Photochem Photobiol Sci 2016; 15:141-74. [PMID: 26822392 DOI: 10.1039/c6pp90004f] [Citation(s) in RCA: 45] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/27/2022]
Abstract
The Environmental Effects Assessment Panel (EEAP) is one of three Panels that regularly informs the Parties (countries) to the Montreal Protocol on the effects of ozone depletion and the consequences of climate change interactions with respect to human health, animals, plants, biogeochemistry, air quality, and materials. The Panels provide a detailed assessment report every four years. The most recent 2014 Quadrennial Assessment by the EEAP was published as a special issue of seven papers in 2015 (Photochem. Photobiol. Sci., 2015, 14, 1-184). The next Quadrennial Assessment will be published in 2018/2019. In the interim, the EEAP generally produces an annual update or progress report of the relevant scientific findings. The present progress report for 2015 assesses some of the highlights and new insights with regard to the interactive nature of the effects of UV radiation, atmospheric processes, and climate change.
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30
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Wolf R, Andersen T, Hessen DO, Hylland K. The influence of dissolved organic carbon and ultraviolet radiation on the genomic integrity of
Daphnia magna. Funct Ecol 2016. [DOI: 10.1111/1365-2435.12730] [Citation(s) in RCA: 17] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/30/2022]
Affiliation(s)
- Raoul Wolf
- Department of Biosciences University of Oslo 0316 Oslo Norway
| | - Tom Andersen
- Department of Biosciences University of Oslo 0316 Oslo Norway
| | - Dag O. Hessen
- Department of Biosciences University of Oslo 0316 Oslo Norway
| | - Ketil Hylland
- Department of Biosciences University of Oslo 0316 Oslo Norway
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31
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Sulzberger B, Arey JS. Impacts of Polar Changes on the UV-induced Mineralization of Terrigenous Dissolved Organic Matter. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2016; 50:6621-6631. [PMID: 27110903 DOI: 10.1021/acs.est.5b05994] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/05/2023]
Abstract
Local climates in the Northern and Southern Hemisphere are influenced by Arctic Amplification and by interactions of the Antarctic ozone hole with climate change, respectively. Polar changes may affect hydroclimatic conditions in temperate regions, for example, by increasing the length and intensity of precipitation events at Northern Hemisphere midlatitudes. Additionally, global warming has led to the thawing of ancient permafrost soils, particularly in Arctic regions, due to Arctic Amplification. Both heavy precipitation events and thawing of permafrost are increasing the net transfer of terrestrially derived dissolved organic matter (DOM) from land to surface waters. In aquatic ecosystems, UV-induced oxidation of terrigenous DOM (tDOM) produces atmospheric CO2 and this process is one of several mechanisms by which natural organic matter in aquatic and soil environments may play an important role in climate feedbacks. The Arctic is particularly affected by these processes: for example, melting of Arctic sea ice allows solar UV radiation to penetrate into the ice-free Arctic Ocean and to cause photochemical reactions that result in bleaching and mineralization of tDOM. Open questions, in addition to those shown in the Graphical Abstract, remain regarding the resulting contributions of tDOM photomineralization to CO2 production and global warming.
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Affiliation(s)
- Barbara Sulzberger
- Academic Guest, Eawag: Swiss Federal Institute of Aquatic Science and Technology , P.O. Box 611, CH-8600 Duebendorf, Switzerland
| | - J Samuel Arey
- Environmental Chemistry Modeling Laboratory, Department of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne (EPFL), Ecole Polytechnique Fédérale de Lausanne (EPFL) , CH-1015 Lausanne, Switzerland
- Department of Environmental Chemistry, Eawag: Swiss Federal Institute of Aquatic Science and Technology , P.O. Box 611, CH-8600 Duebendorf, Switzerland
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32
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Raven JA, Colmer TD. Life at the boundary: photosynthesis at the soil-fluid interface. A synthesis focusing on mosses. JOURNAL OF EXPERIMENTAL BOTANY 2016; 67:1613-23. [PMID: 26842980 DOI: 10.1093/jxb/erw012] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/24/2023]
Abstract
Mosses are among the earliest branching embryophytes and probably originated not later than the early Ordovician when atmospheric CO2 was higher and O2 was lower than today. The C3 biochemistry and physiology of their photosynthesis suggests, by analogy with tracheophytes, that growth of extant bryophytes in high CO2 approximating Ordovician values would increase the growth rate. This occurs for many mosses, including Physcomitrella patens in suspension culture, although recently published transcriptomic data on this species at high CO2 and present-day CO2 show down-regulation of the transcription of several genes related to photosynthesis. It would be useful if transcriptomic (and proteomic) data comparing growth conditions are linked to measurements of growth and physiology on the same, or parallel, cultures. Mosses (like later-originating embryophytes) have been subject to changes in bulk atmospheric CO2 and O2 throughout their existence, with evidence, albeit limited, for positive selection of moss Rubisco. Extant mosses are subject to a large range of CO2 and O2 concentrations in their immediate environments, especially aquatic mosses, and mosses are particularly influenced by CO2 generated by, and O2 consumed by, soil chemoorganotrophy from organic C produced by tracheophytes (if present) and bryophytes.
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Affiliation(s)
- John A Raven
- Permanent address: Division of Plant Sciences, University of Dundee at the James Hutton Institute, Invergowrie, Dundee DD2 5DA, UK School of Plant Biology, The University of Western Australia, M084, 35 Stirling Highway, Crawley, WA 6009, Australia
| | - Timothy D Colmer
- School of Plant Biology, The University of Western Australia, M084, 35 Stirling Highway, Crawley, WA 6009, Australia
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33
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Jing L, Dombinov V, Shen S, Wu Y, Yang L, Wang Y, Frei M. Physiological and genotype-specific factors associated with grain quality changes in rice exposed to high ozone. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2016; 210:397-408. [PMID: 26807986 DOI: 10.1016/j.envpol.2016.01.023] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/10/2015] [Revised: 01/08/2016] [Accepted: 01/08/2016] [Indexed: 05/22/2023]
Abstract
Rising tropospheric ozone concentrations in Asia affect the yield and quality of rice. This study investigated ozone-induced changes in rice grain quality in contrasting rice genotypes, and explored the associated physiological processes during the reproductive growth phase. The ozone sensitive variety Nipponbare and a breeding line (L81) containing two tolerance QTLs in Nipponbare background were exposed to 100 ppb ozone (8 h per day) or control conditions throughout their growth. Ozone affected grain chalkiness and protein concentration and composition. The percentage of chalky grains was significantly increased in Nipponbare but not in L81. Physiological measurements suggested that grain chalkiness was associated with a drop in foliar carbohydrate and nitrogen levels during grain filling, which was less pronounced in the tolerant L81. Grain total protein concentration was significantly increased in the ozone treatment, although the albumin fraction (water soluble protein) decreased. The increase in protein was more pronounced in L81, due to increases in the glutelin fraction in this genotype. Amino acids responded differently to the ozone treatment. Three essential amino acids (leucine, methionine and threonine) showed significant increases, while seven showed significant treatment by genotype interactions, mostly due to more positive responses in L81. The trend of increased grain protein was in contrast to foliar nitrogen levels, which were negatively affected by ozone. A negative correlation between grain protein and foliar nitrogen in ozone stress indicated that higher grain protein cannot be explained by a concentration effect in all tissues due to lower biomass production. Rather, ozone exposure affected the nitrogen distribution, as indicated by altered foliar activity of the enzymes involved in nitrogen metabolism, such as glutamine synthetase and glutamine-2-oxoglutarate aminotransferase. Our results demonstrate differential responses of grain quality to ozone due to the presence of tolerance QTL, and partly explain the underlying physiological processes.
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Affiliation(s)
- Liquan Jing
- Key Lab of Crop Genetics & Physiology of Jiangsu Province, Yangzhou University, PR China
| | - Vitalij Dombinov
- Institute of Crop Science and Resource Conservation (INRES), University of Bonn, Germany
| | - Shibo Shen
- Key Lab of Crop Genetics & Physiology of Jiangsu Province, Yangzhou University, PR China
| | - Yanzhen Wu
- Key Lab of Crop Genetics & Physiology of Jiangsu Province, Yangzhou University, PR China
| | - Lianxin Yang
- Key Lab of Crop Genetics & Physiology of Jiangsu Province, Yangzhou University, PR China
| | - Yunxia Wang
- College of Environmental Science and Engineering, Yangzhou University, PR China
| | - Michael Frei
- Institute of Crop Science and Resource Conservation (INRES), University of Bonn, Germany.
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Malenovský Z, Turnbull JD, Lucieer A, Robinson SA. Antarctic moss stress assessment based on chlorophyll content and leaf density retrieved from imaging spectroscopy data. THE NEW PHYTOLOGIST 2015; 208:608-24. [PMID: 26083501 DOI: 10.1111/nph.13524] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/23/2015] [Accepted: 05/17/2015] [Indexed: 05/04/2023]
Abstract
The health of several East Antarctic moss-beds is declining as liquid water availability is reduced due to recent environmental changes. Consequently, a noninvasive and spatially explicit method is needed to assess the vigour of mosses spread throughout rocky Antarctic landscapes. Here, we explore the possibility of using near-distance imaging spectroscopy for spatial assessment of moss-bed health. Turf chlorophyll a and b, water content and leaf density were selected as quantitative stress indicators. Reflectance of three dominant Antarctic mosses Bryum pseudotriquetrum, Ceratodon purpureus and Schistidium antarctici was measured during a drought-stress and recovery laboratory experiment and also with an imaging spectrometer outdoors on water-deficient (stressed) and well-watered (unstressed) moss test sites. The stress-indicating moss traits were derived from visible and near infrared turf reflectance using a nonlinear support vector regression. Laboratory estimates of chlorophyll content and leaf density were achieved with the lowest systematic/unsystematic root mean square errors of 38.0/235.2 nmol g(-1) DW and 0.8/1.6 leaves mm(-1) , respectively. Subsequent combination of these indicators retrieved from field hyperspectral images produced small-scale maps indicating relative moss vigour. Once applied and validated on remotely sensed airborne spectral images, this methodology could provide quantitative maps suitable for long-term monitoring of Antarctic moss-bed health.
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Affiliation(s)
- Zbyněk Malenovský
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW, 2522, Australia
- Surveying and Spatial Sciences Group, School of Land and Food, University of Tasmania, Private Bag 76, Hobart, TAS, 7001, Australia
| | - Johanna D Turnbull
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW, 2522, Australia
| | - Arko Lucieer
- Surveying and Spatial Sciences Group, School of Land and Food, University of Tasmania, Private Bag 76, Hobart, TAS, 7001, Australia
| | - Sharon A Robinson
- Centre for Sustainable Ecosystem Solutions, School of Biological Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW, 2522, Australia
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Bramley-Alves J, Wanek W, French K, Robinson SA. Moss δ(13) C: an accurate proxy for past water environments in polar regions. GLOBAL CHANGE BIOLOGY 2015; 21:2454-64. [PMID: 25545349 DOI: 10.1111/gcb.12848] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/22/2014] [Accepted: 12/01/2014] [Indexed: 05/08/2023]
Abstract
Increased aridity is of global concern. Polar regions provide an opportunity to monitor changes in bioavailable water free of local anthropogenic influences. However, sophisticated proxy measures are needed. We explored the possibility of using stable carbon isotopes in segments of moss as a fine-scale proxy for past bioavailable water. Variation in δ(13) C with water availability was measured in three species across three peninsulas in the Windmill Islands, East Antarctica and verified using controlled chamber experiments. The δ(13) C from Antarctic mosses accurately recorded long-term variations in water availability in the field, regardless of location, but significant disparities in δ(13) C between species indicated some make more sensitive proxies. δ(13) CSUGAR derived from living tissues can change significantly within the span of an Antarctic season (5 weeks) in chambers, but under field conditions, slow growth means that this technique likely represents multiple seasons. δ(13) CCELLULOSE provides a precise and direct proxy for bioavailable water, allowing reconstructions for coastal Antarctica and potentially other cold regions over past centuries.
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Affiliation(s)
- Jessica Bramley-Alves
- Institute for Conservation Biology, School of Biological Sciences, University of Wollongong, Wollongong, NSW, 2522, Australia
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Abundance and diversity of soil invertebrates in the Windmill Islands region, East Antarctica. Polar Biol 2015. [DOI: 10.1007/s00300-015-1703-2] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/02/2023]
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Royles J, Griffiths H. Invited review: climate change impacts in polar regions: lessons from Antarctic moss bank archives. GLOBAL CHANGE BIOLOGY 2015; 21:1041-57. [PMID: 25336089 DOI: 10.1111/gcb.12774] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/22/2014] [Revised: 09/24/2014] [Accepted: 10/08/2014] [Indexed: 05/13/2023]
Abstract
Mosses are the dominant plants in polar and boreal regions, areas which are experiencing rapid impacts of regional warming. Long-term monitoring programmes provide some records of the rate of recent climate change, but moss peat banks contain an unrivalled temporal record of past climate change on terrestrial plant Antarctic systems. We summarise the current understanding of climatic proxies and determinants of moss growth for contrasting continental and maritime Antarctic regions, as informed by 13C and 18O signals in organic material. Rates of moss accumulation are more than three times higher in the maritime Antarctic than continental Antarctica with growing season length being a critical determinant of growth rate, and high carbon isotope discrimination values reflecting optimal hydration conditions. Correlation plots of 13C and 18O values show that species (Chorisodontium aciphyllum / Polytrichum strictum) and growth form (hummock / bank) are the major determinants of measured isotope ratios. The interplay between moss growth form, photosynthetic physiology, water status and isotope composition are compared with developments of secondary proxies, such as chlorophyll fluorescence. These approaches provide a framework to consider the potential impact of climate change on terrestrial Antarctic habitats as well as having implications for future studies of temperate, boreal and Arctic peatlands. There are many urgent ecological and environmental problems in the Arctic related to mosses in a changing climate, but the geographical ranges of species and life-forms are difficult to track individually. Our goal was to translate what we have learned from the more simple systems in Antarctica, for application to Arctic habitats.
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Affiliation(s)
- Jessica Royles
- British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK; Department of Plant Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EA, UK
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Erickson III DJ, Sulzberger B, Zepp RG, Austin AT. Effects of stratospheric ozone depletion, solar UV radiation, and climate change on biogeochemical cycling: interactions and feedbacks. Photochem Photobiol Sci 2015; 14:127-48. [DOI: 10.1039/c4pp90036g] [Citation(s) in RCA: 45] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/21/2022]
Abstract
Solar UV radiation and climate change interact to influence and determine the environmental conditions for humans on planet Earth.
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Affiliation(s)
- David J. Erickson III
- Computational Earth Sciences Group Computer Science and Mathematics Division
- Oak Ridge National Laboratory
- MS 6016 Oak Ridge TN 37831-6016
- USA
| | - Barbara Sulzberger
- Eawag: Swiss Federal Institute of Aquatic Science and Technology
- CH-8600 Duebendorf
- Switzerland
| | - Richard G. Zepp
- United States Environmental Protection Agency
- Georgia 30605-2700
- USA
| | - Amy T. Austin
- Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA) and Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET)
- Universidad de Buenos Aires
- Buenos Aires
- Argentina
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Bornman JF, Barnes PW, Robinson SA, Ballaré CL, Flint SD, Caldwell MM. Solar ultraviolet radiation and ozone depletion-driven climate change: effects on terrestrial ecosystems. Photochem Photobiol Sci 2015; 14:88-107. [DOI: 10.1039/c4pp90034k] [Citation(s) in RCA: 132] [Impact Index Per Article: 14.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/14/2022]
Abstract
We summarise advances in our knowledge of how UV-B radiation (280–315 nm) together with other climate change factors interact in their influence on terrestrial organisms and ecosystems.
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Affiliation(s)
- J. F. Bornman
- International Institute of Agri-Food Security (IIAFS)
- Curtin University
- Perth
- Australia
| | - P. W. Barnes
- Department of Biological Sciences and Environment Program
- Loyola University New Orleans
- New Orleans
- USA
| | - S. A. Robinson
- Institute for Conservation Biology
- School of Biological Sciences
- The University of Wollongong
- New South Wales 2522
- Australia
| | - C. L. Ballaré
- IFEVA Universidad de Buenos Aires and IIB Universidad Nacional de San Martín
- Consejo Nacional de Investigaciones Científicas y Técnicas
- C1417DSE Buenos Aires
- Argentina
| | - S. D. Flint
- Department of Forest
- Rangeland
- and Fire Sciences
- University of Idaho
- Moscow
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Bais AF, McKenzie RL, Bernhard G, Aucamp PJ, Ilyas M, Madronich S, Tourpali K. Ozone depletion and climate change: impacts on UV radiation. Photochem Photobiol Sci 2015; 14:19-52. [DOI: 10.1039/c4pp90032d] [Citation(s) in RCA: 180] [Impact Index Per Article: 20.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/12/2023]
Abstract
Percentage changes in the UV Index (UVI) for 2090 relative to 2015 due to changes in ozone (left) and aerosols (right) only. Large decreases are projected over Antarctica due to stratospheric ozone recovery. Increases are projected for parts of Asia due to decreases in aerosols, partly reversing the possible large reductions in UVI after the 1950s.
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Affiliation(s)
- A. F. Bais
- Laboratory of Atmospheric Physics
- Aristotle University of Thessaloniki
- 54124 Thessaloniki
- Greece
| | - R. L. McKenzie
- National Institute of Water and Atmospheric Research
- PB 50061 Omakau, Central Otago
- New Zealand
| | | | - P. J. Aucamp
- Ptersa Environmental Management Consultants
- Faerie Glen
- South Africa
| | - M. Ilyas
- School of Environmental Engineering
- University Malaysia Perlis
- Kangar
- Malaysia
| | - S. Madronich
- National Center for Atmospheric Research
- Boulder
- USA
| | - K. Tourpali
- Laboratory of Atmospheric Physics
- Aristotle University of Thessaloniki
- 54124 Thessaloniki
- Greece
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