2006
DOI: 10.1007/s11157-006-0002-3
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Ultraviolet radiation shapes seaweed communities

Abstract: Stratospheric ozone depletion and the concomitant increase in irradiance of ultraviolet-B radiation (UVB) at the earth's surface represent major threats to terrestrial and aquatic ecosystems. In costal rocky shore environments, seaweeds constitute a group of organisms of particular significance to ecosystem function. Thus, impairment of seaweed performance by UVB-exposure may result in severe changes in the functioning of coastal ecosystems. Here we present our view on how UVB radiation affects seaweed physiol… Show more

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Cited by 202 publications
(131 citation statements)
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“…Macroalgae regulate their biochemical composition to changes in solar radiation (Bischof et al, 2006;Figueroa et al, 2014a,b). Whilst light obviously affects photosynthesis, other variables such pH, nutrients and the availability of different DIC species all have the potential to affect photosynthetic rates .…”
Section: Discussionmentioning
confidence: 99%
“…Macroalgae regulate their biochemical composition to changes in solar radiation (Bischof et al, 2006;Figueroa et al, 2014a,b). Whilst light obviously affects photosynthesis, other variables such pH, nutrients and the availability of different DIC species all have the potential to affect photosynthetic rates .…”
Section: Discussionmentioning
confidence: 99%
“…The high irradiance and transparency of shallow water in this region suggest that macroalgae have de-veloped efficient photoprotection mechanisms to tolerate light stress (Figueroa and Gómez 2001). In fact, intertidal macroalgae subject to high solar irradiance and desiccation can survive and grow under the stressful conditions of the intertidal system due to active photoprotection mechanisms such as dynamic photoinhibition, accumulation of UV screen substances and increase in antioxidant capacity (Häder and Figueroa 1997, Korbee et al 2006, Bischof et al 2006, Hanelt and Figueroa 2012.…”
Section: Introductionmentioning
confidence: 99%
“…As more CO 2 dissolves in seawater, changes in the speciation of inorganic carbon occur, resulting in more bicarbonate ions (HCO 3 − ), more protons (H + ) and fewer carbonate ions (CO 3 drop by 0.3 to 0.5 units (Caldeira & Wickett 2003, Feely et al 2004, Orr et al 2005 due to increasing concentrations of atmospheric CO 2 that could reach up to 970 ppm CO 2 (Houghton et al 2001). In addition, both ocean temperature increases due to global warming and increased UVR due to the development of ozone holes may represent a real threat for all sessile marine organisms (Bischof et al 2006).…”
Section: Introductionmentioning
confidence: 99%