Evolutionary stasis of sporopollenin biochemistry revealed by unaltered Pennsylvanian spores

The biopolymer sporopollenin present in the spore/pollen walls of all land plants is regarded as one of the most recalcitrant biomacromolecules (biopolymers), providing protection against a range of abiotic stresses. This long-term stability is demonstrated by the near-ubiquitous presence of pollen and spores in the fossil record with spores providing the first evidence for the colonization of the land. Here, we report for the first time chemical analyses of geologically unaltered sporopollenin from Pennsylvanian (c. 310?million yr before present (MyBP)) cave deposits. Our data show that Pennsylvanian Lycophyta megaspore sporopollenin has a strong chemical resemblance to extant relatives and indicates that a co-polymer model of sporopollenin formation is the most likely configuration. Broader comparison indicates that extant sporopollenin structure is similar across widely spaced phylogenetic groups and suggests land plant sporopollenin structure has remained stable since embryophytes invaded land.     

Sporopollenin monomer biosynthesis in arabidopsis

Land plants have evolved aliphatic biopolymers that protect their cell surfaces against dehydration, pathogens, and chemical and physical damage. In flowering plants, a critical event during pollen maturation is the formation of the pollen surface structure. The pollen wall consists essentially of the microspore-derived intine and the sporophyte-derived exine. The major component of the exine is termed sporopollenin, a complex biopolymer. The chemical composition of sporopollenin remains poorlycharacterized because it is extremely resistant to chemical and biological degradation procedures. Recent characterization of Arabidopsis thaliana genes and corresponding enzymes involved in exine formation has demonstrated that the sporopollenin polymer consists of phenolic and fatty acid-derived constituents that are covalently coupled by ether and ester linkages. This review illuminates the outlines of a biosynthetic pathway involved in generating monomer constituents of the sporopollenin biopolymer component of the pollen wall.     

Studies on sporopollenin biosynthesis in Tulipa anthers

Summary Extensive tracer experiments were carried out on Tulipa with the aim of determining the structure and biosynthesis of sporopollenin. The radiolabeled precursors were applied using an improved technique previously selected. The sporopollenin fraction was purified using either a gentle method — hydrolyzing enzymes (pronase, amylase, amyloglucosidase, cellulase, pectinase and lipase) and alkaline hydrolysis (method A) — or by a conventional aggressive procedure, where the material was enriched by alkaline hydrolysis and treated several days with 80% phosphoric acid (method B). The ¹⁴C-labeled precursors applied were mevalonate, glucose, acetate, malonic acid, phenylalanine, tyrosine, p-coumaric acid. Regardless of the method of enrichment, a higher level of incorporation into the sporopollenin fraction was always seen with [U-¹⁴C]-phenylalanine. The level of radioactivity found in sporopollenin labeled by phenylalanine or malonate was sufficiently high for the labeled polymer to be degraded and the products released analyzed for the first time. In the case of phenylalanine-labeled sporopollenin, the main degradation component, p-hydroxybenzoic acid, was also the most heavily labeled substance. This result was not dependent on the procedure used for sporopollenin enrichment. These findings are interpreted as meaning that phenylpropane metabolism via phenylalanine-ammonia lyase is involved in sporopollenin biosynthesis.     

Studies on Sporopollenin Biosynthesis in Tulipa Anthers

Investigations were carried out to clarify sporopollenin biosynthesis. Tracer experiments were focussed on the incorporation of specifically labeled ¹⁴C-phenylalanine into sporopollenin. In addition, the incorporation of further ¹⁴C-labeled substances, such as glucose, acetate, malonic acid, mevalonate and tyrosine, was investigated. The sporopollenin fraction was isolated and purified by a gentle method including extractions by different solvents, incubations with hydrolyzing enzymes and fractionated saponifications. During the purification procedure the whereabouts of the initially applied radioactivity was followed. After each step the remaining as well as the released radioactivity was determined. Saponification of samples labeled after application of phenylalanine yielded p-coumaric acid and p-coumaric acid methyl ester as labeled products. In comparison with the other substances applied, the highest incorporation rates were obtained with phenylalanine, regardless of the position of labeling. After degradation of the sporopollenin sample labeled with ring-¹⁴C-phenylalanine, p-hydroxybenzoic acid was detected as the main labeled product. These results unequivocally show that an integral incorporation of the aromatic ring system occurred. Tracer experiments were carried out at different stages of development. Their results show that, although the incorporation rates of ¹⁴C-phenylalanine into sporopollenin differ, the substantial incorporation of this substance is not bound to defined stages of development.     

New insights from MALDI-ToF MS, NMR, and GC-MS: mass spectrometry techniques applied to palynology

Summary. The present study for the first time describes the application of matrix-assisted laser desorption ionisation time-of-flight mass spectrometry (MALDI-ToF MS) to palynology. With an accessible mass range of up to about 350,000 Da at subpicomolar range, this technique is ideal for the characterisation of bio-macromolecules, such as sporopollenin, found in fossil and extant pollen and spore walls, which often can only be isolated in very small quantities. At this stage, the limited solubility of sporopollenin allows for the identification of sections of this biopolymer, but with the optimisation of MALDI-ToF matrices, further structure elucidation will become possible. Furthermore, gas chromatography–mass spectrometry (GC-MS) and ¹H nuclear magnetic resonance (¹H NMR) spectroscopy data obtained from a number of experiments revealed that some previously reported data were misinterpreted. These results add support to the hypothesis that common plasticizers were wrongly described as sporopollenin compounds. Correspondence and reprints: School of Earth, Ocean and Planetary Sciences, Cardiff University, Park Place, Cardiff CF10 3YE, United Kingdom. Permanent address: Albion College, Albion, Michigan, U.S.A.     

Receptor-Independent Sporopollenin

Pollen of some species of the genus Quercus shows rod-shaped substructures in fresh or acetolysed exines, while in other species rod substructure is mostly masked by sporopollenin. Oxidation with potassium permanganate removes exine substance (sporopollenin) from between the rod substructures. We propose that the rods include receptors for sporopollenin. The sporopollenin between rods we refer to as ‘receptor-independent sporopollenin’. Pollen of Typha, when mature, has tectal surfaces with concave tops and sides, whereas during development the tectal surfaces are smoothly rounded. After acetolysis treatment followed by potassium permanganate the tectum surfaces again appear rounded. When these exines are subsequently eroded by a fast atom source, rod-shaped substructures are seen to protrude from the tectum. These structures are equivalent in size and shape to the rods of the exine of Quercus. Sporopollenin that accumulates over and masks rod substrucutre is less resistant to our degradative methods than the sporopollenin in rod structures of exines. We suggest that the exine material we call “receptor-independent sporopollenin” be given a simple positive name, such as masking-sporopollenin or abbreviated to masking-spn.     

ULTRASTRUCTURAL STUDY ON MICROSPORE WALL MORPHOGENESIS IN ISOETES JAPONICA (ISOETACEAE)

Spore wall morphogenesis of the microspore of Isoetes japonica was studied by transmission electron microscopy. The microspore wall consists of four layers: the perispore, outer exospore, inner exospore, and endospore. The perispore consists of electron-dense materials. The exospore is divided into outer and inner sections, with a large gap between the two. The outer exospore appears as an undulating plate consisting of tripartite lamellae with homogeneous sporopollenin. The inner exospore consists of an accumulation of tripartite lamellae on the microspore cell membrane. Immediately after meiosis, the tripartite lamellae of the outer exospore forms around the microspore. The lamellated inner exospore forms next, which adheres to the cell membrane of the microspore. The deposition of homogeneous sporopollenin material on the tripartite lamellae causes the plates of the outer exospore to thicken. Some homogeneous material may also be deposited on the inner exospore. Lastly, the electron-dense perispore is deposited on the outer exospore, and the electron-lucent endospore forms beneath the inner exospore. We conclude that the lamellae of the outer exospore, inner exospore, and endospore are formed and derived, in that order, from the gametophytic microspore cytoplasm. The homogeneous sporopollenin material of the outer exospore and perispore may be derived from the sporophytic tapetal cytoplasm.     

CYP704B1 Is a Long-Chain Fatty Acid ω-Hydroxylase Essential for Sporopollenin Synthesis in Pollen of Arabidopsis

Sporopollenin is the major component of the outer pollen wall (exine). Fatty acid derivatives and phenolics are thought to be its monomeric building blocks, but the precise structure, biosynthetic route, and genetics of sporopollenin are poorly understood. Based on a phenotypic mutant screen in Arabidopsis (Arabidopsis thaliana), we identified a cytochrome P450, designated CYP704B1, as being essential for exine development. CYP704B1 is expressed in the developing anthers. Mutations in CYP704B1 result in impaired pollen walls that lack a normal exine layer and exhibit a characteristic striped surface, termed zebra phenotype. Heterologous expression of CYP704B1 in yeast cells demonstrated that it catalyzes ω-hydroxylation of long-chain fatty acids, implicating these molecules in sporopollenin synthesis. Recently, an anther-specific cytochrome P450, denoted CYP703A2, that catalyzes in-chain hydroxylation of lauric acid was also shown to be involved in sporopollenin synthesis. This shows that different classes of hydroxylated fatty acids serve as essential compounds for sporopollenin formation. The genetic relationships between CYP704B1, CYP703A2, and another exine gene, MALE STERILITY2, which encodes a fatty acyl reductase, were explored. Mutations in all three genes resulted in pollen with remarkably similar zebra phenotypes, distinct from those of other known exine mutants. The double and triple mutant combinations did not result in the appearance of novel phenotypes or enhancement of single mutant phenotypes. This implies that each of the three genes is required to provide an indispensable subset of fatty acid-derived components within the sporopollenin biosynthesis framework.The biopolymer sporopollenin is the major component of the outer walls in pollen and spores (exines). It is highly resistant to nonoxidative physical, chemical, and biological treatments and is insoluble in both aqueous and organic solvents. While the stability and resistance of sporopollenin account for the preservation of ancient pollen grains for millions of years with nearly full retention of morphology (Doyle and Hickey, 1976; Friis et al., 2001), these same qualities make it extremely difficult to study the chemical structure of sporopollenin. Thus, although the first studies on the composition of sporopollenin were reported in 1928 (Zetzsche and Huggler, 1928), the exact structure of sporopollenin remains unresolved. At present, it is thought that sporopollenin is a complex polymer primarily made of a mixture of fatty acids and phenolic compounds (Guilford et al., 1988; Wiermann et al., 2001).Fatty acids were first implicated as sporopollenin components when ozonolysis of Lycopodium clavatum and Pinus sylvestris exine yielded significant amounts of straight- and branched-chain monocarboxylic acids, characteristic fatty acid breakdown products (Shaw and Yeadon, 1966). More recently, improved purification and degradation techniques coupled with analytical methods, such as solid-state ¹³C-NMR spectroscopy, Fourier transform infrared spectroscopy, and ¹H-NMR, have shown that sporopollenin is made up of polyhydroxylated unbranched aliphatic units and also contains small amounts of oxygenated aromatic rings and phenylpropanoids (Guilford et al., 1988; Ahlers et al., 1999; Domínguez et al., 1999; Bubert et al., 2002). Biochemical studies using thiocarbamate herbicide inhibition of the chain-elongating steps in the synthesis of long-chain fatty acids and radioactive tracer experiments provided further evidence that lipid metabolism is involved in the biosynthesis of sporopollenin (Wilwesmeier and Wiermann, 1995; Meuter-Gerhards et al., 1999).Relatively little is known about the genetic network that determines sporopollenin synthesis. However, several Arabidopsis (Arabidopsis thaliana) genes implicated in exine biosynthesis encode proteins with sequence homology to enzymes that are involved in fatty acid metabolism. Mutations in MALE STERILITY2 (MS2) eliminate exine and affect a protein with sequence similarity to fatty acyl reductases; the predicted inability of ms2 plants to reduce pollen wall fatty acids to the corresponding alcohols suggests that this reaction is a key step in sporopollenin synthesis (Aarts et al., 1997). The FACELESS POLLEN1 (FLP1) gene, whose loss causes the flp1 exine defect, encodes a protein similar to those involved in wax synthesis (Ariizumi et al., 2003). The no exine formation1 (nef1) mutant accumulates reduced levels of lipids, and the NEF1 protein was suggested to be involved in either lipid transport or the maintenance of plastid membrane integrity, including those plastids in the secretory tapetum of anthers, where many of the sporopollenin components are synthesized (Ariizumi et al., 2004). The dex2 mutant has mutations in the evolutionarily conserved anther-specific cytochrome P450, CYP703A2 (Morant et al., 2007), which catalyzes in-chain hydroxylation of saturated medium-chain fatty acids, with lauric acid (C12:0) as a preferred substrate (Morant et al., 2007). A recently described gene, ACOS5, encodes a fatty acyl-CoA synthetase that has in vitro preference for medium-chain fatty acids (de Azevedo Souza et al., 2009). Mutations in all of these genes compromise exine formation.Here, we describe an evolutionarily conserved cytochrome P450, CYP704B1, and demonstrate that this gene is essential for exine biosynthesis and plays a role different from that of CYP703A2. Heterologously expressed CYP704B1 catalyzed ω-hydroxylation of several saturated and unsaturated C14-C18 fatty acids. These results suggest the possibility that ω-hydroxylated fatty acids produced by CYP704B1, together with in-chain hydroxylated lauric acids provided by the action of CYP703A2, may serve as key monomeric aliphatic building blocks in sporopollenin formation. Analyses of the genetic relationships between CYP704B1, MS2, and CYP703A2 suggest that all three genes are involved in the same pathway within the sporopollenin biosynthesis framework.     

The nature of oxygen in sporopollenin from the pollen of Typha angustifolia L

Native and peracetylated sporopollenin from the pollen of Typha angustifolia L. was investigated using several spectroscopic methods, inducing Fourier transform infrared spectroscopy (FTIR), solid-state 13C-nuclear magnetic resonance spectroscopy (13C-NMR) and X-ray photoelectron spectrometry (XPS). Interpretation of the experimental data shows that the greater part of oxygen found in sporopollenin originates from hydroxyl groups and must be derived from aliphatics and not from aromatics. This result indicates that not only aromatics and long unbranched aliphatics but also poly-hydroxyl aliphatic components are involved in the complex structure of the polymer. Furthermore, it is most probable that the monomers of the sporopollenin skeleton are linked by ether- and not by ester-linkage. Two possible approaches are suggested for the characterisation of sporopollenin structure.     

THE ULTRASTRUCTURE OF PHYCOPELTIS (CHROOLEPIDACEAE: CHLOROPHYTA). I. SPOROPOLLENIN IN THE CELL WALLS

Electron microscope observations on Phycopeltis epiphyton, a subaerial green alga found growing on the leaves of vascular plants and bryophytes, revealed the presence of a densely staining material within the inner and outer zones of the cell walls. This material resists acetolysis, is degraded by chromic acid, is unaffected by ethanolamine and exhibits secondary fluorescence when stained with the fluorochrome Primuline. These characteristics, together with infrared absorption spectra indicate that, on the basis of currently accepted criteria, the densely staining material is a sporopollenin and that it is a major component of the cell wall. Tests for cellulose, chitin, and lignin were negative, and little if any silica is present. It is suggested that negative results in tests for cellulose may be due to a masking effect by the sporopollenin. Comparison of the fine structure of the cell walls of P. epiphyton, pollen grains, and algal cells (known to contain sporopollenin) supports the suggestion that sporopollenin deposition on “unit membranes” is universal. Morphological similarity among sporopollenin lamellae in P. epiphyton, pollen grains, spores of land plants, and the trilaminar sporopollenin sheath in Chlorella, Scenedesmus, and Pediastrum indicates that the structures may be analogous. As in pollen grains, sporopollenin may provide protection against desiccation and parasitism. It may also be involved in the adhesion of Phycopeltis to host plants and in the adhesion between adjacent filaments of the thallus.     

Sporopollenin formation in the ascospore wall of Neurospora crassa

Chemical extraction procedures have shown that sporopollenin is a major component of the ascospore wall of Neurospora crassa and Neurospora tetrasperma. The sporopollenin is about 12% total dryweight of ascospores, and is localised in the ribbed perispore layer. Radioactive β-carotene is efficiently incorporated into the sporopollenin, and it is suggested that carotenoids are the natural precursors that are polymerised in the perispore. However, three carotenoid-deficient mutants of N. crassa produced perispores of normal appearance and properties.     

THE POLLEN WALL OF CANNA AND ITS SIMILARITY TO THE GERMINAL APERTURES OF OTHER POLLEN

The pollen wall of Canna generalis Bailey is exceptionally thick, but only a minor part of it contains detectable amounts of sporopollenin. The sporopollenin is in isolated spinules at the exine surface and in the intine near the plasma membrane. There is no sporopollenin in the > 10 μ thick channeled region between spinules and intine. We suggest that the entire pollen wall of C. generalis is similar to the thick intine and thin exine typical for germinal apertures in many pollen grain types. Considered functionally, the Canna pollen wall may offer an infinite number of sites for pollen tube initiation and would differ significantly from grains that are inaperturate in the sense of an exine lacking definite germinal apertures.     

(Poly)phenolic compounds in pollen and spores of Antarctic plants as indicators of solar UV-B – A new proxy for the reconstruction of past solar UV-B?

The morphology, size and characteristics of the pollen of the plant species Antarctic hairgrass (Deschampsia antarctica, Poaceae) and Antarctic pearlwort (Colobanthus quitensis, Caryophyllaceae) are described by scanning electron microscopy and light microscopy. Based on the number of pores the pollen of Colobanthus quitensis is classified as periporate or polypantorate, while that of Deschampsia antarctica is monoporate.

Pollen of Vicia faba plants, exposed to enhanced UV-B (10.6 kJ m^?2 day^?1 UV-B_BE) in a greenhouse, showed an increased content of UV-B absorbing compounds. There was also an increase of UV-B absorbing compounds in response to exposure to UV-A. By sequential chemical extraction three `compartments' of UV-B absorbance of pollen can be distinguished: a cytoplasmic fraction consisting of, e.g., flavonoids (acid-methanol extractable), a wall-bound fraction, consisting of, e.g., ferulic acid (NaOH extractable) and aromatic groups in the bioresistant polymer sporopollenin possibly consisting of, e.g., para-coumaric acid monomers (fraction remaining after acetolysis). The sporopollenin fraction in the pollen of Helleborus foetidus showed considerable UV-B absorbance (280–320 nm). There is evidence that enhanced solar UV-B induces increased UV-B absorbance (of sporopollenin) in pollen and spores of mosses, which may be preserved in the fossil record. As there are no instrumental records of solar UV-B in the Antarctic before 1970 and no instrumental records of stratospheric ozone over the Antarctic before 1957, the use of UV-B absorbing polyphenolics in pollen (and spores) as bio-indicator, or proxy of solar UV-B, may allow reconstruction of pre-ozone hole and subrecent UV-B and stratospheric ozone levels. Pollen and spores from herbarium specimens and from frozen moss banks (about 5000–10?000 years old) in the Antarctic may, therefore, represent a valuable archive of historical UV-B levels.

     

Extracellular Black Yeast Polysaccharide composed of N-Acetyl Glucosamine and N-Acetyl Glucosaminuronic Acid

POLYSACCHARIDES containing N-acylated hexosaminuronic acids as major components have been isolated from bacterial cells^1–4,7 and capsules^5,6. Most of these polysaccharides are antigens from pathogens^1,2,4,5,7. Polysaccharides from cells or pathogens, however, are unsuitable for investigations of the basic properties and possible practical value of biopolymers, because they are recovered with difficulty and in low yields. It is significant, therefore, that we have isolated in good yield from cultures of an unidentified black yeast (apparently a non-pathogen) an extracellular polysaccharide composed of residues of N-acetyl glucosamine (GlcNAc) and N-acetyl glucosaminuronic acid (GlcNAcUA) in a molar ratio of approximately 2:1. The composition and extracellular occurrence of this polysaccharide make it unique among those from microorganisms. It is the first practicably obtainable member of a new class of biopolymers to be characterized^1–7. Additional members of this class are foreseen from our exploratory research.     

Molecular preservation.

The differing patterns of molecular abundances in organisms are fundamental to the understanding of the biomolecular palaeontological record. All organisms contain DNA, RNA, protein, polysaccharides and lipid components, together with glycolipids, lipopolysaccharides and other complex molecules. Certain biopolymers, however, are restricted in their distributions; for example, lignin, cutin and sporopollenin are found only in terrestrial plants. The detailed chemical structures, namely the bond types present and their precise intramolecular environments, determine resistance to degradation. Observations of biomolecular preservation are compared with predictions based on chemical structure and on conditions encountered during decay.     

The Ediacaran Aspidella‐type impressions in the Jinxian successions of Liaoning Province,northeastern China

Macroscopic impression fossils from the Xingmincun Formation of the Jinxian Group, Liaoning Province of northeastern China, are identified as members of the Aspidella plexus of Ediacaran age. This is the first recognition of the taxon in the Liaoning Province, although such fossils have been previously recorded in the succession, but were referred to as new species and relegated to an earlier Neoproterozoic age. A revision of the taxonomic interpretation and relative age estimation of the previous record is provided, as well as an evaluation of abiotic vs. biotic processes that could produce similar structures to studied impressions. The mode of preservation of the fossils is considered from a biochemical point of view and along with the properties of organic matter in the integument of soft‐bodied metazoans. The selective preservation of the Ediacaran organisms, including metazoans, as impressions (moulds and casts) against the organically preserved contemporaneous cyanobacterial and algal microfossils, and an exceptionally small number of terminal Ediacaran metazoan fossils (Sabellidites, Conotubus and Shaanxilithes), demonstrates the non‐resistant characteristics and the very different biochemical constitution of the Ediacaran metazoans compared with those that evolved in the Cambrian and after. The refractory biomacromolecules in cell walls of photosynthesizing microbiota (bacterans, cutans, algaenan and sporopollenin groups) and in the chitinous body walls of Sabellidites contrast sharply with the labile biopolymers in Ediacaran metazoans known only from impressions. The newly emerging biosynthesis of resistant biopolymers in metazoans (chitin and collagen groups) initiated by the annelids at the end of Ediacaran and fully evolved in Cambrian metazoans, considered with the ability to biomineralize, made their body preservation possible. The Chengjiang and Burgess Shale metazoans show evidence of this new biochemistry in body walls and cuticles, and not only because of the specific taphonomic window that enhanced their preservation.     

Pollen sporopollenin: degradation and structural elucidation

We report the isolation of purified sporopollenin from pollen grains of different species and its complete solubilization. Exine from Pinus pinaster, Betula alba, Ambrosia elatior and Capsicum annuum was extracted by treatment with hydrogen fluoride in pyridine. These exines were purified from their aromatic moieties and from fatty acids linked by ester bonds using acidolysis and saponification treatments. The biopolymer obtained retains almost completely the shape of the original pollen grain. Fourier-transform infrared spectroscopy analysis of the isolated sporopollenin showed the absence of polysaccharide and phenolic material and the presence of carboxylic acid groups joined to unsaturations and ether linkages. Sporopollenin samples were successfully degraded by exhaustive 24-h ozonolysis at room temperature. Gentle ozonolysis (3 h at 0°C) did not completely degrade the biopolymer. The compounds obtained after exhaustive ozonolysis were analysed by gas chromatography-mass spectrometry. Dicarboxylic acids with a low number of carbon atoms were identified as major components of sporopollenin from P. pinaster, A. elatior and C. annuum, representing 28.8%, 63.2% and 88.5%, respectively, of the total compounds obtained. Fatty acids and n-alkanes also were identified in P. pinaster, A. elatior and B. alba sporopollenin. From the data obtained, an hypothesis about the chemical nature and structural arrangement of the sporopollenin is proposed. Received: 8 November 1998 / Revision accepted: 14 April 1999     

Antibodies to pollen exines

A polyclonal antiserum and monoclonal antibodies have been prepared to purified pollen exines of Calocedrus decurrens Florin. The location of the antigen is in the exine, as shown by light-and electron-microscopic immunocytochemistry. The greatest reduction in antibody binding follows treatment of the exine with chemicals known to alter sporopollenin. These results provide evidence that sporopollenin is antigenic. Exines of ten species of gymnosperms and angiosperms also bound the polyclonal antiserum, indicating similarity of sporopollenin structure.     

Anaerobic Biodegradation of the Lignin and Polysaccharide Components of Lignocellulose and Synthetic Lignin by Sediment Microflora

Specifically radiolabeled [¹⁴C-lignin]lignocelluloses and [¹⁴C-polysaccharide]lignocelluloses were prepared from a variety of marine and freshwater wetland plants including a grass, a sedge, a rush, and a hardwood. These [¹⁴C]lignocellulose preparations and synthetic [¹⁴C]lignin were incubated anaerobically with anoxic sediments collected from a salt marsh, a freshwater marsh, and a mangrove swamp. During long-term incubations lasting up to 300 days, the lignin and polysaccharide components of the lignocelluloses were slowly degraded anaerobically to ¹⁴CO₂ and ¹⁴CH₄. Lignocelluloses derived from herbaceous plants were degraded more rapidly than lignocellulose derived from the hardwood. After 294 days, 16.9% of the lignin component and 30.0% of the polysaccharide component of lignocellulose derived from the grass used (Spartina alterniflora) were degraded to gaseous end products. In contrast, after 246 days, only 1.5% of the lignin component and 4.1% of the polysaccharide component of lignocellulose derived from the hardwood used (Rhizophora mangle) were degraded to gaseous end products. Synthetic [¹⁴C]lignin was degraded anaerobically faster than the lignin component of the hardwood lignocellulose; after 276 days, 3.7% of the synthetic lignin was degraded to gaseous end products. Contrary to previous reports, these results demonstrate that lignin and lignified plant tissues are biodegradable in the absence of oxygen. Although lignocelluloses are recalcitrant to anaerobic biodegradation, rates of degradation measured in aquatic sediments are significant and have important implications for the biospheric cycling of carbon from these abundant biopolymers.