2013
DOI: 10.1038/nature12860
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Green and golden seaweed tides on the rise

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Cited by 730 publications
(450 citation statements)
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References 35 publications
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“…Although in general macroalgae blooms worldwide have increased due to coastal eutrophication (Smetacek and Zingone, 2013), for a particular region many factors can play a role. Among all environmental factors that could possibly influence Ulva amount, the following have been well documented by a number of studies: seaweed aquaculture size and production (which may determine the amount of Ulva initially released to the ocean), temperature, light, wind, and nutrient availability (Liu et al, 2009Hu et al, 2010;Keesing et al, 2011;Xing et al, 2015b).…”
Section: Factors Leading To Annual Changesmentioning
confidence: 99%
“…Although in general macroalgae blooms worldwide have increased due to coastal eutrophication (Smetacek and Zingone, 2013), for a particular region many factors can play a role. Among all environmental factors that could possibly influence Ulva amount, the following have been well documented by a number of studies: seaweed aquaculture size and production (which may determine the amount of Ulva initially released to the ocean), temperature, light, wind, and nutrient availability (Liu et al, 2009Hu et al, 2010;Keesing et al, 2011;Xing et al, 2015b).…”
Section: Factors Leading To Annual Changesmentioning
confidence: 99%
“…It was suggested that one of the main processes of carbon sequestration by seaweed beds is transfer of the drifting seaweeds (i.e., Macrocystis, Durvillaea, Eisenia, Ecklonia, and Sargassum) before sinking to benthic habitats and the offshore mesopelagic zone (Harrold et al 1998;Ito et al 2009;Fraser et al 2011). Some species of seaweeds can be transported to new areas far from their origin (e.g., Sargassum in the Sargasso Sea) and can substantially increase their biomass in a free-floating stage, with a tendency to rapidly sink to the deep sea floor, which makes it much more efficient vehicle to carbon sequestration (Johnson and Richardson 1977;Smetacek and Zingone 2013). Thalli are eroded and dislodged whole kelp thalli form rafts on the ocean surface (Hobday 2000;Xu et al 2016) and these are deposited as wrack along shorelines, inshore subtidal habitats, and canyons (Vetter and Dayton 1998;Orr et al 2005;Wernberg et al 2006;Crawley et al 2009).…”
Section: Seaweeds and Sabs Capabilities In Co 2 Sequestrationmentioning
confidence: 99%
“…Satellite imagery analysis shows that there were negligible floating macroalgae between 2000 and 2007 (Hu et al 2010). Massive algal blooms occurred in 2008 (3489 km 2 ) in the open waters of Yellow Sea, and since then the macroalgal blooms have become an annual summer event with increasing spatial and temporal scale, with the 2013 event reportedly reaching a record level (Smetacek and Zingone 2013). In 2008, the world's largest green tide caused aquaculture losses of about 130 million USD, and costs for the emergency response to the green tide, before the 2008 Beijing Olympic games in Qingdao, were estimated to be 320 million USD (Ye et al 2011).…”
Section: Shift To Macroalgae-dominant Statesmentioning
confidence: 99%
“…Nutrient deposited in sediment following degradation of dead seaweeds can be returned to the surface by vertical mixing, which forms the sediment nutrient pool available for algal growth. As a result, seaweed can continue to proliferate and maintain a eutrophic state, even if nutrient input level is reduced substantially (Yabe et al 2009;Smetacek and Zingone 2013).…”
Section: Shift To Macroalgae-dominant Statesmentioning
confidence: 99%
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