© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 8 (2018): 17437, doi:10.1038/s41598-018-35309-3.During recent years, rapid seasonal growth of macroalgae covered extensive areas within the Yellow Sea, developing the world’s most spatially extensive “green tide”. The remarkably fast accumulation of macroalgal biomass is the joint result of high nitrogen supplies in Yellow Sea waters, plus ability of the macroalgae to optionally use C4 photosynthetic pathways that facilitate rapid growth. Stable isotopic evidence shows that the high nitrogen supply is derived from anthropogenic sources, conveyed from watersheds via river d...
International audienceAlthough nitrogen stable isotope ratio (d15N) in macroalgae is widely used as ...
To discover the original source and clarify development of the world's largest transregional green t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
The world's largest trans-regional macroalgal blooms during 2008-2012 occurred in the Yellow Sea, Ch...
Large macroalgal blooms (i.e. green tides of Ulva prolifera) occurred in the southern Yellow Sea, Ch...
1. Macroalgal blooms (green tides) are occurring more frequently in many regions of the world, leadi...
International audienceThe marine macrophyte Ulva prolifera is the dominant green-tide-forming seawee...
World's largest macroalgal blooms (MAB) caused by Ulva prolifera outbreak every summer in the Yellow...
RATIONALE: Stable nitrogen isotope ratios (d15N values) can be used to discern sources of excess ni...
Nitrogen stable isotope ratios (δ15N) in macroalgae are often used to identify sources of nitrogenou...
Annually recurrent green-tides in the Yellow Sea have been shown to result from direct disposal into...
International audienceWorld-largest super floating macroalgal blooms of Ulva prolifera have lasted 7...
The three large marine ecosystems (LMEs) bordering China (Yellow Sea/Bohai Sea, East China Sea, and ...
The three large marine ecosystems (LMEs) bordering China (Yellow Sea/Bohai Sea, East China Sea, and ...
293-297Green tide caused by macroalgae is one of the global ocean ecological disasters and nutrients...
International audienceAlthough nitrogen stable isotope ratio (d15N) in macroalgae is widely used as ...
To discover the original source and clarify development of the world's largest transregional green t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
The world's largest trans-regional macroalgal blooms during 2008-2012 occurred in the Yellow Sea, Ch...
Large macroalgal blooms (i.e. green tides of Ulva prolifera) occurred in the southern Yellow Sea, Ch...
1. Macroalgal blooms (green tides) are occurring more frequently in many regions of the world, leadi...
International audienceThe marine macrophyte Ulva prolifera is the dominant green-tide-forming seawee...
World's largest macroalgal blooms (MAB) caused by Ulva prolifera outbreak every summer in the Yellow...
RATIONALE: Stable nitrogen isotope ratios (d15N values) can be used to discern sources of excess ni...
Nitrogen stable isotope ratios (δ15N) in macroalgae are often used to identify sources of nitrogenou...
Annually recurrent green-tides in the Yellow Sea have been shown to result from direct disposal into...
International audienceWorld-largest super floating macroalgal blooms of Ulva prolifera have lasted 7...
The three large marine ecosystems (LMEs) bordering China (Yellow Sea/Bohai Sea, East China Sea, and ...
The three large marine ecosystems (LMEs) bordering China (Yellow Sea/Bohai Sea, East China Sea, and ...
293-297Green tide caused by macroalgae is one of the global ocean ecological disasters and nutrients...
International audienceAlthough nitrogen stable isotope ratio (d15N) in macroalgae is widely used as ...
To discover the original source and clarify development of the world's largest transregional green t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...