Articles | Volume 14, issue 9
Biogeosciences, 14, 2495–2512, 2017
Biogeosciences, 14, 2495–2512, 2017

Research article 17 May 2017

Research article | 17 May 2017

Origin and processing of terrestrial organic carbon in the Amazon system: lignin phenols in river, shelf, and fan sediments

Shuwen Sun1,2,7, Enno Schefuß2, Stefan Mulitza2, Cristiano M. Chiessi3, André O. Sawakuchi4, Matthias Zabel2, Paul A. Baker5,6, Jens Hefter7, and Gesine Mollenhauer1,2,7 Shuwen Sun et al.
  • 1Department of Geosciences, University of Bremen, 28359 Bremen, Germany
  • 2MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany
  • 3School of Arts, Sciences and Humanities, University of São Paulo, 03828-000 São Paulo, Brazil
  • 4Institute of Geosciences, Department of Sedimentary and Environmental Geology, University of São Paulo, 05508-080 São Paulo, Brazil
  • 5Nicolas School of the Environment, Duke University, 301 Old Chemistry, Box 90227, Durham, NC 27708, USA
  • 6School of Geological Sciences and Engineering, Yachay Tech, Yachay City of Knowledge, 100650 Urcuqui, Ecuador
  • 7Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, 25570 Bremerhaven, Germany

Abstract. The Amazon River transports large amounts of terrestrial organic carbon (OCterr) from the Andean and Amazon neotropical forests to the Atlantic Ocean. In order to compare the biogeochemical characteristics of OCterr in the fluvial sediments from the Amazon drainage basin and in the adjacent marine sediments, we analysed riverbed sediments from the Amazon mainstream and its main tributaries as well as marine surface sediments from the Amazon shelf and fan for total organic carbon (TOC) content, organic carbon isotopic composition (δ13CTOC), and lignin phenol compositions. TOC and lignin content exhibit positive correlations with Al ∕ Si ratios (indicative of the sediment grain size) implying that the grain size of sediment discharged by the Amazon River plays an important role in the preservation of TOC and leads to preferential preservation of lignin phenols in fine particles. Depleted δ13CTOC values (−26.1 to −29.9 ‰) in the main tributaries consistently correspond with the dominance of C3 vegetation. Ratios of syringyl to vanillyl (S ∕ V) and cinnamyl to vanillyl (C ∕ V) lignin phenols suggest that non-woody angiosperm tissues are the dominant source of lignin in the Amazon basin. Although the Amazon basin hosts a rich diversity of vascular plant types, distinct regional lignin compositions are not observed. In the marine sediments, the distribution of δ13CTOC and Λ8 (sum of eight lignin phenols in organic carbon (OC), expressed as mg/100 mg OC) values implies that OCterr discharged by the Amazon River is transported north-westward by the North Brazil Current and mostly deposited on the inner shelf. The lignin compositions in offshore sediments under the influence of the Amazon plume are consistent with the riverbed samples suggesting that processing of OCterr during offshore transport does not change the encoded source information. Therefore, the lignin compositions preserved in these offshore sediments can reliably reflect the vegetation in the Amazon River catchment. In sediments from the Amazon fan, low lignin content, relatively depleted δ13CTOC values and high (Ad ∕ Al)V ratios indicating highly degraded lignin imply that a significant fraction of the deposited OCterr is derived from petrogenic (sourced from ancient rocks) sources.

Final-revised paper