ArticleScientific reports2017
Nitrogen recycling at the Costa Rican subduction zone: The role of incoming plate structure.
Article in Scientific reports, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed.
- Impacts of Groundwater Pumping on Subterranean Microbial Communities in a Deep Aquifer Associated with an Accretionary Prism.Microorganisms · 2024Article
- High nitrogen solubility in stishovite (SiOScientific reports · 2020Article
- The Potential for CHMicrobes and environments · 2020Article
- Mantle degassing along strike-slip faults in the Southeastern Korean Peninsula.Scientific reports · 2019Article
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6 authors.
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Abstract
Efficient recycling of subducted sedimentary nitrogen (N) back to the atmosphere through arc volcanism has been advocated for the Central America margin while at other locations mass balance considerations and N contents of high pressure metamorphic rocks imply massive addition of subducted N to the mantle and past the zones of arc magma generation. Here, we report new results of N isotope compositions with gas chemistry and noble gas compositions of forearc and arc front springs in Costa Rica to show that the structure of the incoming plate has a profound effect on the extent of N subduction into the mantle. N isotope compositions of emitted arc gases (9-11 N°) imply less subducted pelagic sediment contribution compared to farther north. The N isotope compositions (δ
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