Cited by 445Marine and coastal ecosystemsPeatlands and Wetlands EcologySoil Carbon and Nitrogen Dynamics

Dissolved humic substances of the Amazon River system1

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Ertel, John R., Hedges, John I., Devol, Allan H., Richey, Jeffrey E., Ribeiro, Maria de Nazaré Góes·1986·Limnology and Oceanography

Abstract

Aquatic humic and fulvic acids from nine mainstem and seven major tributary sites in the Amazon River Basin are characterized by their elemental and lignin phenol compositions. Combined humic substances represent 60% of the riverine dissolved organic carbon (DOC), with fulvic to humic acid (FA : HA) ratios in the mainstem averaging 4.7±1.0. All dissolved humic and fulvic acids have clearly recognizable lignin components at levels (8 and 3% of the carbon) suggesting a predominantly allochthonous source. Lignin compositional characteristics are dominated by diagenetic transformations, which include preferential loss of methoxylated structural units and oxidative degradation of lignin side chains. Fulvic acids have consistently lower lignin levels, lower lignin phenol methoxylation, higher acid : aldehyde ratios, and higher C: N ratios than coexisting humic acids, all indicative of greater aerobic degradation of the fulvic acid fraction. An extreme example of lignin degradation is seen in the Rio Negro humic and fulvic acids, which differ significantly in lignin and elemental compositions from other blackwater tributary and mainstem samples. Over most of the mainstem humic and fulvic acids behave conservatively. However, downstream of the Rio Negro confluence, humic acids appear to be selectively adsorbed onto fine suspended particles. Approximately 25 and 40% of the total fluxes of lignin and of carbon are represented in the dissolved humic substances. The annual flux of dissolved, chemically recognizable lignin in the Amazon River at Obidos is calculated to be 1.2 × 10 11 g yr−1.

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Crossref · 10.4319/lo.1986.31.4.0739

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  • In forested Amazonian floodplain lakes, local allochthonous inputs are high, comprising most of the suspended organic matter and nutrient inputs.

    “In forested Amazonian floodplain lakes, local allochthonous inputs are high, comprising most of the suspended organic matter and nutrient inputs (Ertel et al., 1986; Hedges et al., 1986; Sobrinho et al., 2016).”

    From Threshold responses of floating meadow fish communities to floodplain forest cover in the lower Amazon River (2025) · cites this paper as Ertel et al., 1986

    The Discussion (page not provided) says suspended particulate organic matter in the Amazon system is essentially all derived from soil or vascular plants, supporting its allochthonous origin. The paper does not establish that local inputs supply most suspended organic matter or nutrients to forested floodplain lakes; its measurements concern riverine dissolved humic substances. (LLM, conf=0.84)

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Research works printed but not linked: 9

  1. Zn K. V. Sarkanen and C. H. Ludwig [eds.], Lignins. Wiley-Interscience.
  2. CRAWFORD, R. L. 198 1. Lignin biodegradation and transformation. Wiley-Interscience.
  3. ERTEL, J. R. 1985. Lignin geochemistry of sedimen- tary and aquatic humic substances. Ph.D. thesis, Univ. Washington, Seattle. 139 p.
  4. LIKENS, G. E., F. T. MACKENZIE, J. E. RICHEY, J. R. SEDELL, AND K. K. TUREKIAN [EDS.]. 198 1. Flux of organic carbon by rivers to the ocean. Conf. 8009140. DOE, Office Energy Res., Washington, D.C. LYTLE, C. R., AND E. M. PERDUE. 198 1. Free, pro- teinaceous, and humic-bound amino acids in river water containing high concentrations of aquatic humus. Environ. Sci. Technol. 15: 224-228.
  5. MEYBECK, M. 198 1. River transport of organic car- bon to the ocean, p. 219-269. Zn Flux of organic carbon by rivers to the ocean. Conf. 8009140.
  6. SARKANEN, K. V., AND C. H. LUDWIG. 197 1. Lignins. Wiley-Interscience.
  7. Zn A. D. Hasler [ed.], Coupling of land and water systems. Springer.
  8. STALLARD, R. F. 1980. Major element geochemistry of the Amazon River system. Ph.D. thesis, Mass. Inst. Technol.
  9. WANGERSKY, P, J. 1981. The fate of sedimented or- ganic carbon in estuaries, p. 294-3 13. Zn Flux of organic carbon by rivers to the ocean. Conf. 8009 140. DOE, Office Energy Res., Washington, D.C. WILSON, M. A., R. P. PHILP, A. H. GILLAM, AND K. R. TATE. 1983. Comparison of the structures of hu- mic substances from aquatic and terrestrial sources by pyrolysis gas chromatography-mass spectrom- etry. Geochim. Cosmochim. Acta 47: 497-502.

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Authors
Ertel, J. R., Hedges, J. I., Devol, A. H., Richey, J. E., & Ribeiro, M. D. N. G.
Affiliations
  • University of Washington (US)
  • Instituto Nacional de Pesquisas da Amazônia (BR)
Corresponding author
Ertel, John R.
Venue
Limnology and Oceanography
Publisher
Wiley
Published
1986-07
Volume
31
Issue
4
Pages
739-754
ISSN
  • 0024-3590 (ISSN-L)
  • 1939-5590
OpenAlex
W2120891916
Cited by
445
References
1
Citations by year
2026: 3 · 2025: 6 · 2024: 7 · 2023: 4 · 2022: 5 · 2021: 11 · 2020: 6 · 2019: 15 · 2018: 57 · 2017: 13 · 2016: 18 · 2015: 10 · 2014: 18 · 2013: 13 · 2012: 10
FWCI
11.71
Type
journal article
Language
en
Open access
Locations
Limnology and Oceanography (publishedVersion)
Funders
  • National Science Foundation
  • University of Washington
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
  • Physical Sciences › Environmental Science › Ecology › Peatlands and Wetlands Ecology
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
Keywords
dissolved humic substances, fulvic acid, humic acid, Amazon River, dissolved organic carbon, lignin phenols, lignin degradation, allochthonous organic matter, Rio Negro, organic carbon flux, diagenesis

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