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Linkages between stratospheric ozone, UV radiation and climate change and their implications for terrestrial ecosystems.
Bornman, Janet F; Barnes, Paul W; Robson, T Matthew; Robinson, Sharon A; Jansen, Marcel A K; Ballaré, Carlos L; Flint, Stephan D.
  • Bornman JF; College of Science, Health, Engineering and Education, Murdoch University, Perth, W. Australia. Janet.Bornman@Murdoch.edu.au.
  • Barnes PW; Department of Biological Sciences and Environment Program, Loyola University, New Orleans, USA. pwbarnes@loyno.edu.
  • Robson TM; Research Programme in Organismal and Evolutionary Biology, Viikki Plant Science Centre, University of Helsinki, Finland.
  • Robinson SA; Centre for Sustainable Ecosystem Solutions, School of Earth, Atmosphere and Life Sciences and Global Challenges Program, University of Wollongong, Wollongong, NSW 2522, Australia.
  • Jansen MAK; Plant Ecophysiology Group, School of Biological, Earth and Environmental Sciences, UCC, Cork, Ireland.
  • Ballaré CL; University of Buenos Aires, Faculty of Agronomy and IFEVA-CONICET, and IIB, National University of San Martin, Buenos Aires, Argentina.
  • Flint SD; Department of Forest, Rangeland and Fire Sciences, University of Idaho, Moscow, ID, USA.
Photochem Photobiol Sci ; 18(3): 681-716, 2019 Mar 01.
Article en En | MEDLINE | ID: mdl-30810560
ABSTRACT
Exposure of plants and animals to ultraviolet-B radiation (UV-B; 280-315 nm) is modified by stratospheric ozone dynamics and climate change. Even though stabilisation and projected recovery of stratospheric ozone is expected to curtail future increases in UV-B radiation at the Earth's surface, on-going changes in climate are increasingly exposing plants and animals to novel combinations of UV-B radiation and other climate change factors (e.g., ultraviolet-A and visible radiation, water availability, temperature and elevated carbon dioxide). Climate change is also shifting vegetation cover, geographic ranges of species, and seasonal timing of development, which further modifies exposure to UV-B radiation. Since our last assessment, there has been increased understanding of the underlying mechanisms by which plants perceive UV-B radiation, eliciting changes in growth, development and tolerances of abiotic and biotic factors. However, major questions remain on how UV-B radiation is interacting with other climate change factors to modify the production and quality of crops, as well as important ecosystem processes such as plant and animal competition, pest-pathogen interactions, and the decomposition of dead plant matter (litter). In addition, stratospheric ozone depletion is directly contributing to climate change in the southern hemisphere, such that terrestrial ecosystems in this region are being exposed to altered patterns of precipitation, temperature and fire regimes as well as UV-B radiation. These ozone-driven changes in climate have been implicated in both increases and reductions in the growth, survival and reproduction of plants and animals in Antarctica, South America and New Zealand. In this assessment, we summarise advances in our knowledge of these and other linkages and effects, and identify uncertainties and knowledge gaps that limit our ability to fully evaluate the ecological consequences of these environmental changes on terrestrial ecosystems.
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Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Rayos Ultravioleta / Cambio Climático / Ozono Estratosférico Tipo de estudio: Prognostic_studies Límite: Animals Idioma: En Año: 2019 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Rayos Ultravioleta / Cambio Climático / Ozono Estratosférico Tipo de estudio: Prognostic_studies Límite: Animals Idioma: En Año: 2019 Tipo del documento: Article