The number of past and future regenerations of iron in the ocean and its intrinsic fertilization efficiency
Iron fertilization is explored by tracking dissolved iron (DFe) through its life cycle from injection by aeolian, sedimentary, and hydrothermal sources (birth) to burial in the sediments (death). We develop new diagnostic equations that count iron and phosphate regenerations with each passage throug...
| Published in: | Biogeosciences |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Copernicus Publications
2018
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| Subjects: | |
| Online Access: | http://hdl.handle.net/1959.4/unsworks_54807 https://unsworks.unsw.edu.au/bitstreams/1fdf3b7f-67fa-4322-960b-2620e53edb0b/download https://doi.org/10.5194/bg-15-7177-2018 |
| Summary: | Iron fertilization is explored by tracking dissolved iron (DFe) through its life cycle from injection by aeolian, sedimentary, and hydrothermal sources (birth) to burial in the sediments (death). We develop new diagnostic equations that count iron and phosphate regenerations with each passage through the biological pump and partition the ocean's DFe concentration according to the number of its past or future regenerations. We apply these diagnostics to a family of data-constrained estimates of the iron cycle with sources σtot in the range 1.9-41 Gmolyr-1. We find that for states with σtot > 7 Gmolyr-1, 50% or more of the DFe inventory has not been regenerated in the past and 85% or more will not be regenerated in the future. The globally averaged mean number of past or future regenerations scales with the bulk iron lifetime τ ∼ σ-1tot and has a range of 0.05-2.2 for past and 0.01-1.4 for future regenerations. Memory of birth location fades rapidly with each regeneration, and DFe regenerated more than approximately five times is found in a pattern shaped by Southern Ocean nutrient trapping. We quantify the intrinsic fertilization efficiency of the unperturbed system at any point r in the ocean as the global export production resulting from the DFe at r per iron molecule. We show that this efficiency is closely related to the mean number of future regenerations that the iron will experience. At the surface, the intrinsic fertilization efficiency has a global mean in the range 0.7-7 molP(mmolFe)-1 across our family of state estimates and is largest in the central tropical Pacific, with the Southern Ocean having comparable importance only for high-iron-source scenarios. |
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