Abstract

Dissolved organic matter (DOM) is recognized for its importance in freshwater ecosystems, but historical reliance on DOM quantity rather than indicators of DOM composition has led to an incomplete understanding of DOM and an underestimation of its role and importance in biogeochemical processes. A single sample of DOM can be composed of tens of thousands of distinct molecules. Each of these unique DOM molecules has their own chemical properties and reactivity or role in the environment. Human activities can modify DOM composition and recent research has uncovered distinct DOM pools laced with human markers and footprints. Here we review how land use change, climate change, nutrient pollution, browning, wildfires, and dams can change DOM composition which in turn will affect internal processing of freshwater DOM. We then describe how human-modified DOM can affect biogeochemical processes. Drought, wildfires, cultivated land use, eutrophication, climate change driven permafrost thaw, and other human stressors can shift the composition of DOM in freshwater ecosystems increasing the relative contribution of microbial-like and aliphatic components. In contrast, increases in precipitation may shift DOM towards more relatively humic-rich, allochthonous forms of DOM. These shifts in DOM pools will likely have highly contrasting effects on carbon outgassing and burial, nutrient cycles, ecosystem metabolism, metal toxicity, and the treatments needed to produce clean drinking water. A deeper understanding of the links between the chemical properties of DOM and biogeochemical dynamics can help to address important future environmental issues, such as the transfer of organic contaminants through food webs, alterations to nitrogen cycling, impacts on drinking water quality, and biogeochemical effects of global climate change.

Highlights

  • The movement and processing of organic matter within and among terrestrial, freshwater, and oceanic environments has extensive implications for global climate and carbon (C) cycles (Battin et al 2009; Tranvik et al 2009)

  • We describe how human-modified dissolved organic matter (DOM) can affect biogeochemical processes

  • While organic matter pools in freshwater ecosystems are relatively small compared to the marine pool, omission of freshwater organic matter pools leads to [ 25% overestimation in terrestrial net ecosystem production (Aufdenkampe et al 2011; Butman et al 2016; Cole et al 2007)

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Summary

Introduction

The movement and processing of organic matter within and among terrestrial, freshwater, and oceanic environments has extensive implications for global climate and carbon (C) cycles (Battin et al 2009; Tranvik et al 2009). It is expected that increases in terrestrial DOC loads should shift the DOM pools in inland waters towards a more ‘‘terrestrial’’ composition, including large, humic-like molecules with high molecular weight and aromatic structures (Creed et al 2018) This shift should be most pronounced where residence time is short and soil organic matter is well connected to hydrologic flow paths. The amount of DOC exported (1.04 Tg C year-1; Hood et al 2015) is small compared to nonglaciated catchments (Bhatia et al 2010) but the relatively higher bioavailability of glacier-derived DOM compared to forested, agricultural and wetland dominated catchments (Fasching et al 2016; RisseBuhl et al 2013) supports heterotrophic metabolism in proglacial streams (Hood et al 2009; Singer et al 2012; Spencer et al 2014) It follows that one consequence of an increase in microbial-like, N-rich, aliphatic DOM from human activities is an increase in microbial metabolism in downstream ecosystems (see below). A more thorough examination of DOM characteristics may be useful for the development of early warning indicators able to detect the contamination of drinking water with wastewater (Stedmon et al 2011)

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