The marine redox change and nitrogen cycle in the Early Cryogenian interglacial time: Evidence from nitrogen isotopes and Mo contents of the basal Datangpo Formation, northeastern Guizhou, South China

2016 ◽  
Vol 27 (2) ◽  
pp. 233-241 ◽  
Author(s):  
Wei Wei ◽  
Dan Wang ◽  
Da Li ◽  
Hongfei Ling ◽  
Xi Chen ◽  
...  
2022 ◽  
Vol 369 ◽  
pp. 106501
Author(s):  
Hongzuo Wang ◽  
Dan Wang ◽  
Guang-Yi Wei ◽  
Hong-Fei Ling ◽  
Ulrich Struck ◽  
...  

2017 ◽  
Vol 74 (1) ◽  
pp. 101-113 ◽  
Author(s):  
Zhi Yang ◽  
Jianfang Chen ◽  
Min Chen ◽  
Lihua Ran ◽  
Hongliang Li ◽  
...  

2019 ◽  
Vol 322 ◽  
pp. 160-169 ◽  
Author(s):  
Haoming Wei ◽  
Xinqiang Wang ◽  
Xiaoying Shi ◽  
Ganqing Jiang ◽  
Dongjie Tang ◽  
...  

2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Pearse J. Buchanan ◽  
Olivier Aumont ◽  
Laurent Bopp ◽  
Claire Mahaffey ◽  
Alessandro Tagliabue

AbstractThe open ocean nitrogen cycle is being altered by increases in anthropogenic atmospheric nitrogen deposition and climate change. How the nitrogen cycle responds will determine long-term trends in net primary production (NPP) in the nitrogen-limited low latitude ocean, but is poorly constrained by uncertainty in how the source-sink balance will evolve. Here we show that intensifying nitrogen limitation of phytoplankton, associated with near-term reductions in NPP, causes detectable declines in nitrogen isotopes (δ15N) and constitutes the primary perturbation of the 21st century nitrogen cycle. Model experiments show that ~75% of the low latitude twilight zone develops anomalously low δ15N by 2060, predominantly due to the effects of climate change that alter ocean circulation, with implications for the nitrogen source-sink balance. Our results highlight that δ15N changes in the low latitude twilight zone may provide a useful constraint on emerging changes to nitrogen limitation and NPP over the 21st century.


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