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Cited by 248

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CO2 efflux from Amazonian headwater streams represents a significant fate for deep soil respiration

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Johnson, Mark S., Lehmann, Johannes, Riha, Susan J., Krusche, Alex V., Richey, Jeffrey E., Ometto, Jean Pierre H. B., Couto, Eduardo Guimarães·2008·Geophysical Research Letters

Abstract

Large Amazonian rivers are known to emit substantial amounts of CO 2 to the atmosphere, while the magnitude of CO 2 degassing from small streams remains a major unknown in regional carbon budgets. We found that 77% of carbon transported by water from the landscape was as terrestrially‐respired CO 2 dissolved within soils, over 90% of which evaded to the atmosphere within headwater reaches of streams. Hydrologic transport of dissolved CO 2 was equivalent to nearly half the gaseous CO 2 contributions from deep soil (>2 m) to respiration at the soil surface. Dissolved CO 2 in emergent groundwater was isotopically consistent with soil respiration, and demonstrated strong agreement with deep soil CO 2 concentrations and seasonal dynamics. During wet seasons, deep soil (2–8 m) CO 2 concentration profiles indicated gaseous diffusion to deeper layers, thereby enhancing CO 2 drainage to streams. Groundwater discharge of CO 2 and its subsequent evasion is a significant conduit for terrestrially‐respired carbon in tropical headwater catchments.

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Metadata

Authors
Johnson, M. S., Lehmann, J., Riha, S. J., Krusche, A. V., Richey, J. E., Ometto, J. P. H. B., & Couto, E. G.
Venue
Geophysical Research Letters
Published
2008-09
Volume
35
Issue
17
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2016102970
Cited by
248
References
0
FWCI
6.46
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: CO2 efflux from Amazonian headwater streams represents a significant fate for deep soil respiration. https://app.cochat.ai/papers/10.1029/2008gl034619
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Johnson, M. S., Lehmann, J., Riha, S. J., Krusche, A. V., Richey, J. E., Ometto, J. P. H. B., & Couto, E. G. (2008). CO2 efflux from Amazonian headwater streams represents a significant fate for deep soil respiration. Geophysical Research Letters. https://doi.org/10.1029/2008gl034619

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