2020
DOI: 10.1016/j.cosust.2020.09.009
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Rethinking standards of permanence for terrestrial and coastal carbon: implications for governance and sustainability

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Cited by 32 publications
(26 citation statements)
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“…Data-constrained modelling suggests that the zonally-averaged mean time from deep seafloor remineralization to re-exposure to the atmosphere ranges between 700–900 years in the North Atlantic 39 , where GASB biomass is deposited 38 , and increases further along the global conveyor belt to >1400 years in the North Pacific 39 . These timescales are generally longer than those considered for some land-based CDR methods like terrestrial afforestation or soil carbon sequestration, which are on the order of decades to a century 36 , 40 . Nevertheless, the systematic differences reveal that some locations are better suited for seafloor deposition of seaweed biomass than others.…”
Section: Resultsmentioning
confidence: 98%
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“…Data-constrained modelling suggests that the zonally-averaged mean time from deep seafloor remineralization to re-exposure to the atmosphere ranges between 700–900 years in the North Atlantic 39 , where GASB biomass is deposited 38 , and increases further along the global conveyor belt to >1400 years in the North Pacific 39 . These timescales are generally longer than those considered for some land-based CDR methods like terrestrial afforestation or soil carbon sequestration, which are on the order of decades to a century 36 , 40 . Nevertheless, the systematic differences reveal that some locations are better suited for seafloor deposition of seaweed biomass than others.…”
Section: Resultsmentioning
confidence: 98%
“…Seafloor deposition may be associated with less process-related offsets to CDR theoretical , when the deep sea is adjacent to the afforestation site. The value of geological and sea floor deposition depends upon a yet to be established policy framework that needs to clarify how sequestration permanence is factored into a carbon price, and how stringently CO 2 leakage back into the atmosphere must be monitored 36 . Geological sequestration in appropriate formations can be considered long-term with a 66–90% chance of less than 1% CO 2 leakage over 1000 years and possibly beyond 37 .…”
Section: Resultsmentioning
confidence: 99%
“…Emission reductions are innately permanent and do not face a risk of reversal. Policy instruments need to account for such differences in order to be compatible with net-zero ambitions, by differentiating results based on their permanence levels [e.g., recognizing temporary removals without relying on them in the long term; Ruseva et al (2020)] or limiting their role within mitigation targets by further enhancing the pace and scale of emissions reductions accordingly.…”
Section: Differentiation Needed Based On Cdr Characteristicsmentioning
confidence: 99%
“…A land-based system that transitions to a new management regime that is reasonable to continue for even as little as 10-15 years that results in retaining and removing carbon can provide significant value to the atmosphere and to a buyer in a VCM. It should not be required that VCM project developers seek administrative maneuverings or questionable or eccentric science to prove 100 years of permanence (Ruseva et al, 2020).…”
Section: Permanencementioning
confidence: 99%