Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska
Radiocarbon measurements of ecosystem respiration and soil pore space CO 2 are useful for determining the sources of ecosystem respiration, identifying environmental controls on soil carbon cycling rates, and parameterizing and evaluating models of the carbon cycle. We measured flux rates and radioc...
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ftdoajarticles:oai:doaj.org/article:06ea8d3cd65e476f852921c9c9d230ae 2023-05-15T15:14:15+02:00 Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska L. J. S. Vaughn M. S. Torn 2018-10-01T00:00:00Z https://doi.org/10.5194/essd-10-1943-2018 https://doaj.org/article/06ea8d3cd65e476f852921c9c9d230ae EN eng Copernicus Publications https://www.earth-syst-sci-data.net/10/1943/2018/essd-10-1943-2018.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-10-1943-2018 1866-3508 1866-3516 https://doaj.org/article/06ea8d3cd65e476f852921c9c9d230ae Earth System Science Data, Vol 10, Pp 1943-1957 (2018) Environmental sciences GE1-350 Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.5194/essd-10-1943-2018 2022-12-31T05:14:19Z Radiocarbon measurements of ecosystem respiration and soil pore space CO 2 are useful for determining the sources of ecosystem respiration, identifying environmental controls on soil carbon cycling rates, and parameterizing and evaluating models of the carbon cycle. We measured flux rates and radiocarbon content of ecosystem respiration, as well as radiocarbon in soil profile CO 2 in Utqiaġvik (Barrow), Alaska, during the summers of 2012, 2013, and 2014. We found that radiocarbon in ecosystem respiration (Δ 14 C Reco ) ranged from +60.5 to −160 ‰ with a median value of +23.3 ‰. Ecosystem respiration became more depleted in radiocarbon from summer to autumn, indicating increased decomposition of old soil organic carbon and/or decreased CO 2 production from fast-cycling carbon pools. Across permafrost features, ecosystem respiration from high-centered polygons was depleted in radiocarbon relative to other polygon types. Radiocarbon content in soil pore-space CO 2 varied between −7.1 and −280 ‰, becoming more negative with depth in individual soil profiles. These pore-space radiocarbon values correspond to CO 2 mean ages of 410 to 3350 years, based on a steady-state, one-pool model. Together, these data indicate that deep soil respiration was derived primarily from old, slow-cycling carbon, but that total CO 2 fluxes depended largely on autotrophic respiration and heterotrophic decomposition of fast-cycling carbon within the shallowest soil layers. The relative contributions of these different CO 2 sources were highly variable across microtopographic features and time in the sampling season. The highly negative Δ 14 C values in soil pore-space CO 2 and autumn ecosystem respiration indicate that when it is not frozen, very old soil carbon is vulnerable to decomposition. Radiocarbon data and associated CO 2 flux and temperature data are stored in the data repository of the Next Generation Ecosystem Experiments (NGEE-Arctic) at http://dx.doi.org/10.5440/1364062 and https://doi.org/10.5440/1418853 . Article in Journal/Newspaper Arctic Barrow permafrost Alaska Directory of Open Access Journals: DOAJ Articles Arctic Earth System Science Data 10 4 1943 1957 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 L. J. S. Vaughn M. S. Torn Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
Radiocarbon measurements of ecosystem respiration and soil pore space CO 2 are useful for determining the sources of ecosystem respiration, identifying environmental controls on soil carbon cycling rates, and parameterizing and evaluating models of the carbon cycle. We measured flux rates and radiocarbon content of ecosystem respiration, as well as radiocarbon in soil profile CO 2 in Utqiaġvik (Barrow), Alaska, during the summers of 2012, 2013, and 2014. We found that radiocarbon in ecosystem respiration (Δ 14 C Reco ) ranged from +60.5 to −160 ‰ with a median value of +23.3 ‰. Ecosystem respiration became more depleted in radiocarbon from summer to autumn, indicating increased decomposition of old soil organic carbon and/or decreased CO 2 production from fast-cycling carbon pools. Across permafrost features, ecosystem respiration from high-centered polygons was depleted in radiocarbon relative to other polygon types. Radiocarbon content in soil pore-space CO 2 varied between −7.1 and −280 ‰, becoming more negative with depth in individual soil profiles. These pore-space radiocarbon values correspond to CO 2 mean ages of 410 to 3350 years, based on a steady-state, one-pool model. Together, these data indicate that deep soil respiration was derived primarily from old, slow-cycling carbon, but that total CO 2 fluxes depended largely on autotrophic respiration and heterotrophic decomposition of fast-cycling carbon within the shallowest soil layers. The relative contributions of these different CO 2 sources were highly variable across microtopographic features and time in the sampling season. The highly negative Δ 14 C values in soil pore-space CO 2 and autumn ecosystem respiration indicate that when it is not frozen, very old soil carbon is vulnerable to decomposition. Radiocarbon data and associated CO 2 flux and temperature data are stored in the data repository of the Next Generation Ecosystem Experiments (NGEE-Arctic) at http://dx.doi.org/10.5440/1364062 and https://doi.org/10.5440/1418853 . |
format |
Article in Journal/Newspaper |
author |
L. J. S. Vaughn M. S. Torn |
author_facet |
L. J. S. Vaughn M. S. Torn |
author_sort |
L. J. S. Vaughn |
title |
Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
title_short |
Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
title_full |
Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
title_fullStr |
Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
title_full_unstemmed |
Radiocarbon measurements of ecosystem respiration and soil pore-space CO 2 in Utqiaġvik (Barrow), Alaska |
title_sort |
radiocarbon measurements of ecosystem respiration and soil pore-space co 2 in utqiaġvik (barrow), alaska |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://doi.org/10.5194/essd-10-1943-2018 https://doaj.org/article/06ea8d3cd65e476f852921c9c9d230ae |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Barrow permafrost Alaska |
genre_facet |
Arctic Barrow permafrost Alaska |
op_source |
Earth System Science Data, Vol 10, Pp 1943-1957 (2018) |
op_relation |
https://www.earth-syst-sci-data.net/10/1943/2018/essd-10-1943-2018.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-10-1943-2018 1866-3508 1866-3516 https://doaj.org/article/06ea8d3cd65e476f852921c9c9d230ae |
op_doi |
https://doi.org/10.5194/essd-10-1943-2018 |
container_title |
Earth System Science Data |
container_volume |
10 |
container_issue |
4 |
container_start_page |
1943 |
op_container_end_page |
1957 |
_version_ |
1766344721103323136 |