2017
DOI: 10.3389/fmars.2017.00038
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Flux of Dissolved and Particulate Low-Temperature Pyrogenic Carbon from Two High-Latitude Rivers across the Spring Freshet Hydrograph

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Cited by 18 publications
(46 citation statements)
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References 76 publications
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“…As expected, significant export of both PBC and POC were observed during the wet season (PBC: 1.3 Gg/year; POC: 9.2 Gg/year) and were significantly higher compared to the dry season (PBC: 0.3 Gg/year; POC: 2.2 Gg/year). This observation agrees with the suggested enhanced mobilization and export of particulate material under high flow conditions (Myers‐Pigg et al, ; Wagner et al, ). However, there was no significant difference in the seasonal contributions of PBC to the bulk POC pool (Student's t test, p = 0.05; dry: 15.3 ± 9.2%; wet: 14.8 ± 9.8%).…”
Section: Discussionsupporting
confidence: 92%
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“…As expected, significant export of both PBC and POC were observed during the wet season (PBC: 1.3 Gg/year; POC: 9.2 Gg/year) and were significantly higher compared to the dry season (PBC: 0.3 Gg/year; POC: 2.2 Gg/year). This observation agrees with the suggested enhanced mobilization and export of particulate material under high flow conditions (Myers‐Pigg et al, ; Wagner et al, ). However, there was no significant difference in the seasonal contributions of PBC to the bulk POC pool (Student's t test, p = 0.05; dry: 15.3 ± 9.2%; wet: 14.8 ± 9.8%).…”
Section: Discussionsupporting
confidence: 92%
“…However, we note that this relationship between DBC and PBC in the Altamaha River appears to be driven in response to an initial pulsing from storm events at the onset of the wet season, as a strong significant correlation between DBC and PBC fluxes ( r = 0.96, p < 0.01) is observed when not considering the data corresponding to January 2016. In a similar manner to our study, Myers‐Pigg et al () reported that the coupling of low‐temperature‐derived PyC in Arctic systems is disrupted at high flow, stimulated by an early release of dissolved‐PyC along the rising limb of the major discharge peak compared to particulate‐PyC peaking during the falling limb of the major discharge peak. Wagner et al () also reported an early release of DBC during rising discharge in a recently burned watershed in Colorado.…”
Section: Discussionsupporting
confidence: 89%
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“…Levoglucosan can be transported to marine sediments through the atmosphere and by rivers (Hunsinger et al, 2008). Furthermore, recent work confirms that levoglucosan is exported by particulate matter, although varying spatially and temporally, in rivers at a high enough level to potentially enter sedimentary deposits and record historical wildfire signatures (Myers-Pigg et al, 2017). However, before we can confidently apply levoglucosan as a biomass burning proxy in marine sediments, there is a need for studies on how levoglucosan is transported to the marine environment, how it is reflecting biomass burning on continents, as well as the fate of levoglucosan and its isomers while settling through the marine water column and during deposition in marine sediments.…”
Section: Introductionmentioning
confidence: 85%