Elsevier

Organic Geochemistry

Volume 141, March 2020, 103963
Organic Geochemistry

Improving the extraction efficiency of sedimentary carbohydrates by sequential hydrolysis

https://doi.org/10.1016/j.orggeochem.2019.103963Get rights and content

Highlights

  • A sequential hydrolysis protocol is developed to extract sedimentary carbohydrates.

  • The protocol greatly reduces lose of labile carbohydrates by strong acid treatment.

  • Carbohydrate recoveries are increased by on average ~60% by this protocol.

  • This protocol is appropriate for different sediment types.

  • It provides more accurate information on carbohydrate inventories and compositions.

Abstract

Carbohydrates serve as structural materials, energy storage compounds, and energy carriers in organisms and provide insights into the dominant sources and the degradation state of organic matter (OM). Several studies have analyzed dissolved and/or particulate carbohydrates in the environment, often with the aim of studying particular carbohydrate groups of interest. These studies have often employed different acids and hydrolytic conditions, making comparisons across studies a challenge. Here, we introduce a sequential acid hydrolysis protocol for the comprehensive extraction, quantification and compositional investigation of carbohydrates in sediment samples. This protocol has four acid hydrolysis steps that sequentially increase in extraction strength, where each subsequent hydrolysis step is performed on the unextracted remains previously hydrolyzed. The four hydrolysis steps consist of 1 M HCl for 2 h at (1) room temperature, (2) 50 °C, and (3) 105 °C, followed by incubation for 8 h using (4) 6 M HCl and 105 °C. Based on tests using diverse carbohydrate standard compounds, the protocol recovers most di- and oligosaccharides and soluble polysaccharides during the initial hydrolysis steps, whereas the recovery of most insoluble polysaccharides is highest during the final extraction step. Applying this protocol to different sediment types shows that recoveries of neutral sugars, amino sugars and sugar alcohols are on average ~60% higher than with a reference one-step extraction method using only hydrolysis with hot 6 M HCl. This sequential extraction protocol thus provides an important new tool for the quantitative and compositional analysis of carbohydrates in aquatic sediments.

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)

  • D. Fabbri et al.

    Characterization of the tetramethylammonium hydroxide thermochemolysis products of carbohydrates

    Journal of Analytical and Applied Pyrolysis

    (1999)
  • D. Fabbri et al.

    Pyrolysis–GC–MS to trace terrigenous organic matter in marine sediments: a comparison between pyrolytic and lipid markers in the Adriatic Sea

    Analytica Chimica Acta

    (2005)
  • D. Fabbri et al.

    Analytical pyrolysis of dipeptides containing proline and amino acids with polar side chains. Novel 2,5-diketopiperazine markers in the pyrolysates of proteins

    Journal of Analytical and Applied Pyrolysis

    (2012)
  • M.B. Flannery et al.

    Chitin in the fossil record: identification and quantification of D-glucosamine

    Organic Geochemistry

    (2001)
  • L. Gerber et al.

    Multivariate curve resolution provides a high-throughput data processing pipeline for pyrolysis-gas chromatography/mass spectrometry

    Journal of Analytical and Applied Pyrolysis

    (2012)
  • P. Kerhervé et al.

    Neutral monosaccharides in surface sediments of the northwestern Mediterranean Sea

    Organic Geochemistry

    (2002)
  • H. Knicker et al.

    Identification of protein remnants in insoluble geopolymers using TMAH thermochemolysis/GC–MS

    Organic Geochemistry

    (2001)
  • K. Knudsen

    Carbohydrate and lignin contents of plant materials used in animal feeding

    Animal feed science and technology

    (1997)
  • G. Liebezeit et al.

    Water-extractable carbohydrates in particulate matter of the Bransfield Strait

    Marine Chemistry

    (1991)
  • V. Micić et al.

    Organic geochemistry of Danube River sediments from Pančevo (Serbia) to the Iron Gate dam (Serbia-Romania)

    Organic Geochemistry

    (2010)
  • K. Mopper et al.

    A new noncorrosive dye reagent for automatic sugar chromatography

    Analytical Biochemistry

    (1973)
  • K. Mopper

    Sugars and uronic-acids in sediment and water from Black Sea and North Sea with emphasis on analytical techniques

    Marine Chemistry

    (1977)
  • S.M. Myklestad et al.

    A sensitive and rapid method for analysis of dissolved mono-and polysaccharides in seawater

    Marine Chemistry

    (1997)
  • R.T. Nguyen et al.

    Preservation of algaenan and proteinaceous material during the oxic decay of Botryococcus braunii as revealed by pyrolysis-gas chromatography/mass spectrometry and 13C NMR spectroscopy

    Organic Geochemistry

    (2003)
  • J. Niggemann et al.

    Sources and fate of amino sugars in coastal Peruvian sediments

    Geochimica et Cosmochimica Acta

    (2006)
  • A. Nouara et al.

    Simultaneous determination of neutral sugars, alditols and anhydrosugars using anion-exchange chromatography with pulsed amperometric detection: application for marine and atmospheric samples

    Marine Chemistry

    (2019)
  • D.W. Page

    Characterisation of organic matter in sediment from Corin Reservoir, Australia

    Journal of Analytical and Applied Pyrolysis

    (2003)
  • R. Pel et al.

    Mesophilic chitin-degrading anaerobes isolated from an estuarine environment

    FEMS Microbiology Ecology

    (1986)
  • A. Pielesz et al.

    Mild acid hydrolysis of fucoidan: characterization by electrophoresis and FT-Raman spectroscopy

    Carbohydrate Research

    (2011)
  • M. Quijada et al.

    Neutral aldoses derived from sequential acid hydrolysis of sediments as indicators of diagenesis over 120,000 years

    Organic Geochemistry

    (2015)
  • J. Schellekens et al.

    Selecting parameters for the environmental interpretation of peat molecular chemistry – a pyrolysis-GC/MS study

    Organic Geochemistry

    (2009)
  • J. Tolu et al.

    High-throughput characterization of sediment organic matter by pyrolysis–gas chromatography/mass spectrometry and multivariate curve resolution: A promising analytical tool in (paleo)limnology

    Analytica Chimica Acta

    (2015)
  • M. Uzaki et al.

    Determination of cellulose and non-cellulose carbohydrates in recent sediments by gas chromatography

    Journal of Chromatography A

    (1983)
  • K. Vancampenhout et al.

    Differences in chemical composition of soil organic matter in natural ecosystems from different climatic regions - A pyrolysis-GC/MS study

    Soil Biology and Biochemistry

    (2009)
  • Cited by (0)

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