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DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska
Understanding the entirety of basin-scale C cycling (DOC fluxes and CO(2) exchanges) are central to a holistic perspective of boreal forest biogeochemistry today. Shifts in the timing and magnitude of dissolved organic carbon (DOC) delivery in streams and eventually into oceans can be expected, whil...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6867643/ https://www.ncbi.nlm.nih.gov/pubmed/31747438 http://dx.doi.org/10.1371/journal.pone.0225271 |
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author | Tomco, Patrick L. Zulueta, Rommel C. Miller, Leland C. Zito, Phoebe A. Campbell, Robert W. Welker, Jeffrey M. |
author_facet | Tomco, Patrick L. Zulueta, Rommel C. Miller, Leland C. Zito, Phoebe A. Campbell, Robert W. Welker, Jeffrey M. |
author_sort | Tomco, Patrick L. |
collection | PubMed |
description | Understanding the entirety of basin-scale C cycling (DOC fluxes and CO(2) exchanges) are central to a holistic perspective of boreal forest biogeochemistry today. Shifts in the timing and magnitude of dissolved organic carbon (DOC) delivery in streams and eventually into oceans can be expected, while simultaneously CO(2) emission may exceed CO(2) fixation, leading to forests becoming stronger CO(2) sources than sinks amplifying rising trace gases in the atmosphere. At May Creek, a representative late-successional boreal forest watershed at the headwaters of the Copper River Basin, Alaska, we quantified the seasonality of DOC flux and landscape-scale CO(2) exchange (eddy covariance) over two seasonal cycles. We deployed in situ fDOM and conductivity sensors, performed campaign sampling for water quality (DOC and water isotopes), and used fluorescence spectroscopy to ascertain DOC character. Simultaneously, we quantified net CO(2) exchange using a 100 ft eddy covariance tower. Results indicate DOC exports were pulse-driven and mediated by precipitation events. Both frequency and magnitude of pulse-driven DOC events diminished as the seasonal thaw depth deepened, with inputs from terrestrial sources becoming major contributors to the DOC pool with decreasing snowmelt contribution to the hydrograph. A three-component parallel factorial analysis (PARAFAC) model indicated DOC liberated in late-season may be bioavailable (tyrosine-like). Combining Net Ecosystem Exchange (NEE) measurements indicate that the May Creek watershed fixes 142–220 g C m(-2) yr(-1) and only 0.40–0.57 g C m(-2) yr(-1) is leached out as DOC. Thus, the May Creek watershed and similar mature spruce forest dominated watersheds in the Copper River Basin are currently large ecosystem C sinks and exceeding C conservative. An understanding of DOC fluxes from Gulf of Alaska watersheds is important for characterizing future climate change-induced seasonal shifts. |
format | Online Article Text |
id | pubmed-6867643 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-68676432019-12-07 DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska Tomco, Patrick L. Zulueta, Rommel C. Miller, Leland C. Zito, Phoebe A. Campbell, Robert W. Welker, Jeffrey M. PLoS One Research Article Understanding the entirety of basin-scale C cycling (DOC fluxes and CO(2) exchanges) are central to a holistic perspective of boreal forest biogeochemistry today. Shifts in the timing and magnitude of dissolved organic carbon (DOC) delivery in streams and eventually into oceans can be expected, while simultaneously CO(2) emission may exceed CO(2) fixation, leading to forests becoming stronger CO(2) sources than sinks amplifying rising trace gases in the atmosphere. At May Creek, a representative late-successional boreal forest watershed at the headwaters of the Copper River Basin, Alaska, we quantified the seasonality of DOC flux and landscape-scale CO(2) exchange (eddy covariance) over two seasonal cycles. We deployed in situ fDOM and conductivity sensors, performed campaign sampling for water quality (DOC and water isotopes), and used fluorescence spectroscopy to ascertain DOC character. Simultaneously, we quantified net CO(2) exchange using a 100 ft eddy covariance tower. Results indicate DOC exports were pulse-driven and mediated by precipitation events. Both frequency and magnitude of pulse-driven DOC events diminished as the seasonal thaw depth deepened, with inputs from terrestrial sources becoming major contributors to the DOC pool with decreasing snowmelt contribution to the hydrograph. A three-component parallel factorial analysis (PARAFAC) model indicated DOC liberated in late-season may be bioavailable (tyrosine-like). Combining Net Ecosystem Exchange (NEE) measurements indicate that the May Creek watershed fixes 142–220 g C m(-2) yr(-1) and only 0.40–0.57 g C m(-2) yr(-1) is leached out as DOC. Thus, the May Creek watershed and similar mature spruce forest dominated watersheds in the Copper River Basin are currently large ecosystem C sinks and exceeding C conservative. An understanding of DOC fluxes from Gulf of Alaska watersheds is important for characterizing future climate change-induced seasonal shifts. Public Library of Science 2019-11-20 /pmc/articles/PMC6867643/ /pubmed/31747438 http://dx.doi.org/10.1371/journal.pone.0225271 Text en © 2019 Tomco et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. |
spellingShingle | Research Article Tomco, Patrick L. Zulueta, Rommel C. Miller, Leland C. Zito, Phoebe A. Campbell, Robert W. Welker, Jeffrey M. DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title | DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title_full | DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title_fullStr | DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title_full_unstemmed | DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title_short | DOC export is exceeded by C fixation in May Creek: A late-successional watershed of the Copper River Basin, Alaska |
title_sort | doc export is exceeded by c fixation in may creek: a late-successional watershed of the copper river basin, alaska |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6867643/ https://www.ncbi.nlm.nih.gov/pubmed/31747438 http://dx.doi.org/10.1371/journal.pone.0225271 |
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