Improving the extraction efficiency of sedimentary carbohydrates by sequential hydrolysis
Introduction
Carbohydrates are present in Bacteria, Archaea, and Eukarya and are the most abundant group of biomolecules on Earth, accounting for up to ~90% of land plant, 20–40% of phytoplankton, and ~ 20% of total microbial biomass (Knudsen, 1997, Panagiotopoulos and Sempéré, 2005, Lever et al., 2015). Carbohydrates can be grouped into four major size classes, namely monosaccharides (monomers), disaccharides (dimers), oligosaccharides (typically 3–10 units), and polysaccharides (>10 units). They can serve as metabolic intermediates, as energy storage compounds, or as essential structural components in organisms. Mono- and disaccharides are generally considered to be highly biologically labile and are respired or fermented by many organisms to obtain energy for growth and maintenance (Handa and Mizuno, 1973, Pel and Gottschal, 1986, Killops and Killops, 2005). Depending on the chemical configuration, oligo- and polysaccharides are used to store energy within cells (e.g., raffinose, starch and glycogen) or to form essential structural components. The latter include cell walls of phytoplankton and vascular plants (e.g., cellulose and hemicellulose), exoskeletons of arthropods and cell walls of fungi (e.g., chitin and chitosan), cell walls of many Bacteria and Archaea (e.g., peptidoglycan and pseudomurein), and side chains that link and stabilize other biomolecules, such as proteins and lipids (e.g., glycoproteins, glycolipids) (Hecky et al., 1973, Benner and Kaiser, 2003, Barton, 2005; Madigan and Martinko, 2005; Souza et al., 2011, Meyer and Albers, 2014, Gangl and Tenhaken, 2016). Structural carbohydrates account for the largest pools of carbohydrates, with cellulose and chitin representing the two most abundant biopolymers on Earth (Souza et al., 2011).
In addition to being important components of living organisms, carbohydrates are present in vast quantities as detritus within aquatic sediments. Accordingly, it has been estimated that 1–40% of total organic carbon (TOC) (for review see Burdige, 2007), and 5–85% of dissolved organic carbon (DOC) in recent aquatic sediments is made of carbohydrates (Arnosti and Holmer, 1999, Burdige et al., 2000). A large fraction of these carbohydrates is made up of neutral sugars, including arabinose, fucose, galactose, glucose, mannose, rhamnose, and xylose (Handa and Mizuno, 1973, Burdige et al., 2000, da Cunha et al., 2002, Duan et al., 2017), and amino sugars, including glucosamine, galactosamine, and muramic acid (Niggemann and Schubert, 2006, Carstens et al., 2012).
In recognition of the importance of carbohydrates as building blocks and energy sources to many organisms and as major components of organic carbon pools in sediments, a substantial effort has been made over the last decades to improve the identification and quantification of carbohydrates in the environment (e.g., Cowie and Hedges, 1984a, Pakulski and Benner, 1992, Amelung et al., 1996, Myklestad et al., 1997, Kerhervé et al., 2002, Zhu et al., 2014, Quijada et al., 2015, Nouara et al., 2019). A typical carbohydrate extraction protocol begins with an acid hydrolysis that is followed by neutralization, purification, and final determination of carbohydrate monomers by colorimetric or chromatographic detection (see review by Panagiotopoulos and Sempéré, 2005). The hydrolysis step is crucial to release carbohydrate monomers from biopolymers and/or sample matrices into the extraction solution. Monosaccharide yields after hydrolysis depend on many factors, including type of acid, acid strength, hydrolysis duration, hydrolysis temperature, and types of glycosidic bonds (e.g., α or β anomer) within the carbohydrates present (Panagiotopoulos and Sempéré, 2005). Both mild and strong hydrolysis protocols have been applied to environmental samples. Mild hydrolysis is usually performed using trifluoroacetic acid (TFA), hydrochloric acid (HCl), or sulfuric acid (H2SO4) at concentrations of 0.09–2 M (e.g., Mopper, 1977, Uzaki and Ishiwatari, 1983, Walters and Hedges, 1988, Borch and Kirchman, 1997) and is suitable for the release of carbohydrates from biologically labile biopolymers (e.g., fucoidan, laminarin, mannan; Borch and Kirchman, 1997, Pielesz and Paluch, 2011). By contrast, strong acid hydrolysis is often employed for structural polysaccharides, such as alginic acid, chitin, and cellulose, and typically involves hot HCl (e.g., 6 M HCl heated at 105 °C for 8 h; Zhang and Amelung, 1996, Zhu et al., 2014), or concentrated H2SO4 (e.g., 12 M H2SO4 at ambient for 2 h, followed by diluting to 1.2 M H2SO4 and heated at 100 °C for 3 h; Mopper, 1977, Cowie and Hedges, 1984a).
Previous evaluations of hydrolysis methods suggest that hydrolysis efficiencies vary with sample types (seawater or sediment) and depend on carbohydrate source compounds and sugar losses during recovery with each method (Cowie and Hedges, 1984a, Borch and Kirchman, 1997). These sample- and method-inherent biases make it difficult to directly compare environmental carbohydrate data produced by different protocols, or to estimate the contribution of carbohydrates to global organic carbon pools.
The goal of this study is to establish a universal extraction protocol that maximizes the recovery of carbohydrates from a wide range of aquatic sediments. We first compare the monomer recoveries from chemically diverse soluble di-, oligo- and polysaccharides and insoluble polysaccharides based on hydrolysis protocols that involve different acid types (TFA, HCl, H2SO4), acid strengths (0.5–12 M), durations (0.5–8 h), and temperatures (room temperature to 105 °C). Based on these tests, we identify four hydrolysis steps that, when applied sequentially, maximize monomer recoveries across the entire suite of compounds tested. We then apply this sequential protocol to diverse marine and lacustrine sediment types, and compare the hydrolysis yields and extraction efficiency to those obtained with a previously published one-step hydrolysis method based on gas chromatography with flame-ionization detection (GC-FID). Finally, we use pyrolysis-gas chromatography/mass spectrometry (Py-GC/MS) to estimate the amount of remaining, non-extracted carbohydrates after our sequential extraction protocol.
Section snippets
Standard compounds and sediment samples
Standards of mono-, di-, tri-, and polysaccharides (Table 1) were purchased from Sigma-Aldrich Chemie GmbH (Buchs, Switzerland), or Carbosynth Limited (Berkshire, United Kingdom). These carbohydrates are widespread in nature and span a broad range of sources and functions (Table 1). Acids (HCl, TFA and H2SO4), derivatization reagents (hydroxylamine hydrochloride, 4-(dimethylamino)pyridine, methanol, pyridine and acetic anhydride), and all other chemicals (barium hydroxide (Ba(OH)2), sodium
Effect of acid type and strength on soluble carbohydrate yields under mild hydrolytic conditions
Effects of acid types and acid concentrations on a range of 12 soluble di-, tri-, and polysaccharides initially were tested at room temperature for 2 h (Fig. 1). Hydrolysis with HCl generally yielded significantly higher recoveries of the soluble di-, tri-, and polysaccharides (p < 0.05, n = 12, multivariate analysis of variance; IBM SPSS statistics software, version 19) than hydrolysis with TFA or H2SO4 at all concentration levels, whereas acid concentrations showed only minor effects on
Conclusions
We established a sequential extraction protocol for the analysis of carbohydrates in aquatic sediments. Investigations on different sediment sample types from multiple locations show that this protocol increases total carbohydrate recoveries by ~60% compared to a previously published one-step extraction method. The higher yields are due to enhanced recoveries of neutral sugars (+69%), sugar alcohols (+84%), and amino sugars (+36%), large fractions of which are destroyed by direct strong acid
Acknowledgements
Samples were retrieved from field trips to Aarhus Bay (Denmark), Lake Lucerne (Switzerland), Lake Greifen (Switzerland), and during RV Meteor cruise SO241 to Guaymas Basin (Gulf of California). All Py-GC/MS measurements were performed at the Department of Ecology and Environmental Science, Umeå University, Sweden. We thank all participating scientists and ship crews for sample recovery, Kristopher McNeill and Sam Zeeman for instrument support, Junko Takahashi-Schmidt for the Py-GC/MS analysis,
References (69)
- et al.
Determination of neutral and acidic sugars in soil by capillary gas-liquid chromatography after trifluoroacetic acid hydrolysis
Soil Biology and Biochemistry
(1996) - et al.
Carbohydrate dynamics and contributions to the carbon budget of an organic-rich coastal sediment
Geochimica et Cosmochimica Acta
(1999) Hydrolysis and other cleavages of glycosidic linkages in polysaccharides
Advances in Carbohydrate Chemistry and Biochemistry
(1988)- et al.
Concentration and composition of dissolved combined neutral sugars (polysaccharides) in seawater determined by HPLC-PAD
Marine Chemistry
(1997) - et al.
Dissolved and particulate carbohydrates in contrasting marine sediments
Geochimica et Cosmochimica Acta
(2000) - et al.
Analytical pyrolysis and thermally assisted hydrolysis and methylation of EUROSOIL humic acid samples — A key to their source
Geoderma
(2009) - et al.
Contribution of bacterial cells to lacustrine organic matter based on amino sugars and d-amino acids
Geochimica et Cosmochimica Acta
(2012) - et al.
Carbohydrate sources in a coastal marine environment
Geochimica et Cosmochimica Acta
(1984) - et al.
Neutral sugars as biomarkers in the particulate organic matter of a French Mediterranean river
Organic Geochemistry
(2002) - et al.
Factors controlling the distribution and early diagenesis of organic material in marine sediments