Abstract

Dissolved lignin is a well-established biomarker of terrigenous dissolved organic matter (DOM) in the ocean, and a chromophoric component of DOM. Although evidence suggests there is a strong linkage between lignin concentrations and chromophoric DOM (CDOM) absorption coefficients in coastal waters, the characteristics of this linkage and the existence of a relationship that is applicable across coastal oceans remain unclear. Here, 421 paired measurements of dissolved lignin concentrations (sum of 9 lignin phenols) and CDOM absorption coefficients (ag(λ)) were used to examine their relationship along the river-ocean continuum (0-37 salinity) and across contrasting coastal oceans (sub-tropical, temperate, high-latitude). Overall, lignin concentrations spanned four orders of magnitude and revealed a strong, non-linear relationship with ag(λ). The characteristics of the relationship (shape, wavelength dependency, lignin-composition dependency) and evidence from degradation indicators were all consistent with lignin being an important driver of CDOM variability in coastal oceans, and suggested physical mixing and long-term photodegradation were important in shaping the relationship. These observations were used to develop two simple empirical models for estimating lignin concentrations from ag(λ) with a +/- 20% error relative to measured values. The models are expected to be applicable in most coastal oceans influenced by terrigenous inputs.

Highlights

  • Lignin is a major biochemical component of vascular plant tissues, and a well-established biomarker of terrigenous organic matter in the ocean

  • The objectives of this study were to reveal the characteristics of the relationship between chromophoric dissolved organic matter (CDOM) absorption and dissolved lignin concentration in the ocean, provide insights about the factors driving and affecting the relationship, and provide simple models for predicting dissolved lignin concentration from CDOM absorption coefficients that are widely applicable in terrestrially-influenced coastal systems

  • A total of 421 paired water samples for CDOM and dissolved lignin analyses were collected as part of different research projects between September 2005 and October 2013

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Summary

Introduction

Lignin is a major biochemical component of vascular plant tissues, and a well-established biomarker of terrigenous organic matter in the ocean. During decomposition of plant matter by microorganisms in litter and soils, some lignin is mobilized in particulate or dissolved form to nearby streams and rivers (Aiken et al, 1985; Aiken and Cotsaris, 1995; Eriksson, 2010). Lignin eventually reaches the ocean, where its vascular-plant origin makes it an unambiguous biomarker of terrigenous organic matter (Hedges et al, 1997). Lignin extracted from seawater and marine sediments has long been used to derive qualitative and quantitative information about the origins, transformations, and fates of terrigenous organic matter in the ocean (Opsahl and Benner, 1997; Hernes and Benner, 2006; Goni et al, 2008; Amon et al, 2012; Fichot and Benner, 2014; Tesi et al, 2014; Medeiros et al, 2015)

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