Physical,chemical, and regulatory properties of glycolate oxidase in C<Subscript>3</Subscript> and C<Subscript>4</Subscript> plants

Physical, chemical, and regulatory properties of glycolate oxidase (GO) isolated from the leaves of C₄ and C₃ plants (Zea mays L., cv. Voronezhskaya 76 and Glycine max (L.) Merr., cv. Pripyat’, respectively) were studied. The homogenous preparations were obtained by multistage enzyme purification from soybean leaves and maize mesophyll and bundle sheath. The glycolate oxidase (GO) preparations obtained consisted of two types of subunits, 37 and 44 kD. The GO isolated from C₃ plant leaves had many in common with that extracted from C₄ plant bundle sheath as regards physical, chemical, and catalytic properties. The primary function of GO in both plant types is metabolism of glycolate, which is a product of ribulosebisphosphate oxalacetic acid oxidation and is used by plants for biosynthesis of hydrocarbons and amino acids.     

Enhancement of Ethylene Release from Leaf Tissue during Glycolate Decarboxylation : A Possible Role for Photorespiration

When leaf discs of Xanthium strumarium L. and Salvia splendens L. are incubated in sealed flasks in the light, more C₂H₄ gas is released in the presence of added CO₂ (30-200 millimolar NaHCO₃) than without CO₂. In Salvia, the maximum rate of C₂H₄ release occurs when sufficient CO₂ (above 125 millimolar NaHCO₃) is added to saturate photosynthesis confirming previous studies. The maximum rate of C₂H₄ release from illuminated discs is similar to the rate in the dark with or without CO₂ in both species. Glycolate enhances a CO₂-dependent C₂H₄ evolution from illuminated leaf discs. However, the maximum rate of C₂H₄ release with glycolate is the same as that observed with saturating CO₂. When photosynthesis is inhibited by darkness or by 3-(3,4-dichlorophenyl)-1,1-dimethylurea, glycolate has no effect.

Studies with [2,3-¹⁴C]-1-aminocyclopropane-1-carboxylic acid (ACC) show that the pattern of C₂H₄ release and the specific activity of the ¹⁴C₂H₄ in the presence and absence of glycolate is similar to that described above, indicating that glycolate does not alter uptake of the exogenously supplied precursor (ACC) or stimulate C₂H₄ release from an endogenous source at appreciable rates. Glycolate oxidase in vitro generates H₂O₂ which stimulates a slow breakdown of ACC to C₂H₄, but since exogenous glycolate is oxidized to CO₂ in both the light and the dark it is argued that the glycolate-dependent increase in C₂H₄ release from illuminated leaf discs is not mediated directly by the action of enzymes of glycolate catabolism. The effects of glycolate and CO₂ are not easily explained by changes in stomatal resistance. The data support the view that glycolate decarboxylation at subsaturating levels of CO₂ in the light stimulates C₂H₄ release by raising the CO₂ level in the tissue.

     

Kangaroo tooth enamel oxygen and carbon isotope variation on a latitudinal transect in southern Australia: implications for palaeoenvironmental reconstruction

Tooth enamel apatite carbonate carbon and oxygen isotope ratios of modern kangaroos (Macropus spp.) collected on a 900-km latitudinal transect spanning a C₃–C₄ transition zone were analysed to create a reference set for palaeoenvironmental reconstruction in southern Australia. The carbon isotope composition of enamel carbonate reflects the proportional intake of C₃ and C₄ vegetation, and its oxygen isotope composition reflects that of ingested water. Tooth enamel forms incrementally, recording dietary and environmental changes during mineralisation. Analyses show only weak correlations between climate records and latitudinal changes in δ¹³C and δ¹⁸O. No species achieved the δ¹³C values (~?1.0 ‰) expected for 100 % C₄ grazing diets; kangaroos at low latitudes that are classified as feeding primarily on C₄ grasses (grazers) have δ¹³C of up to ?3.5 ‰. In these areas, δ¹³C below ?12 ‰ suggests a 100 % C₃ grass and/or leafy plant (browse) diet while animals from higher latitude have lower δ¹³C. Animals from semi-arid areas have δ¹⁸O of 34–40 ‰, while grazers from temperate areas have lower values (~28–30 ‰). Three patterns with implications for palaeoenvironmental reconstruction emerge: (1) all species in semi-arid areas regularly browse to supplement limited grass resources; (2) all species within an environmental zone have similar carbon and oxygen isotope compositions, meaning data from different kangaroo species can be pooled for palaeoenvironmental investigations; (3) relatively small regional environmental differences can be distinguished when δ¹³C and δ¹⁸O data are used together. These data demonstrate that diet–isotope and climate–isotope relationships should be evaluated in modern ecosystems before application to the regional fossil record.     

Tracing prey origins,proportions and feeding periods for predatory beetles from agricultural systems using carbon and nitrogen stable isotope analyses

Predatory beetles are an important component of the natural enemy complex that preys on insect pests such as aphids within agroecosystems. Tracing diet origins and movement of natural enemies aids understanding their role in the food web and informs strategies for their effective conservation. Field sampling and laboratory experiments were carried out to examine the changes of carbon and nitrogen stable isotope ratios (δ¹³C and δ¹⁵N) among crops (cotton and maize), pests (cotton and maize aphids), and between wing and abdomen of predatory beetles, Propylea japonica, and to test the hypothesis that prey origins, proportions and feeding periods of the predatory beetles can be deduced by this stable isotope analysis. Results showed that the δ¹³C values both in wing and abdomen of adult P. japonica were changing from a C₃- to a C₄-based diet of aphids reared on maize or cotton, respectively; the isotope ratio of their new C₄ substrates were detectable within 7 days and the δ¹⁵N values began to reflect their new C₄ substrates within 3 days. The relationship between δ¹³C and δ¹⁵N values of P. japonica adults in wing or abdomen and diets of aphids from a C₃-based resource transitioning to a C₄-based resource were described best in linear or quadratic equations. Results suggest that integrative analysis of δ¹³C and δ¹⁵N values can be regarded as a useful method for quantifying to trace prey origins, proportions of diets and feeding periods of natural enemies. The results can provide quantifying techniques for habitat management of natural enemies.     

Stable isotope analysis for assessing the intercrop movement of Microplitis mediator,a larval endoparasitoid of Helicoverpa armigera

Methods to trace source habitats and movement of parasitic natural enemies in agroecosystems are limited. This study demonstrates that stable carbon isotope analysis offers a valuable new method for revealing the movement of Microplitis mediator (Haliday) (Hymenoptera: Braconidae), a larval endoparasitoid of Helicoverpa armigera Hübner (Lepidoptera: Noctuidae), between C₃ and C₄ plants. Results indicate that M. mediator with δ¹³C values of lower than −22‰ originate from a C₃ plant, whereas those with δ¹³C values of higher than −19‰ develop on a C₄ plant.     

Desert Tortoise (Gopherus agassizii) Dietary Specialization Decreases across a Precipitation Gradient

We studied the plant resource use between and within populations of desert tortoise (Gopherus agassizii) across a precipitation gradient in the Sonoran Desert of Arizona. The carbon and nitrogen stable isotope values in animal tissues are a reflection of the carbon and nitrogen isotope values in diet, and consequently represent a powerful tool to study animal feeding ecology. We measured the δ¹³C and δ¹⁵N values in the growth rings on the shells of tortoises in different populations to characterize dietary specialization and track tortoise use of isotopically distinct C₄/CAM versus C₃ plant resources. Plants using C₃ photosynthesis are generally more nutritious than C₄ plants and these trait differences can have important growth and fitness consequences for consumers. We found that dietary specialization decreases in successively drier and less vegetated sites, and that broader population niche widths are accompanied by an increase in the dietary variability between individuals. Our results highlight how individual consumer plant resource use is bounded under a varying regime of precipitation and plant productivity, lending insight into how intra-individual dietary specialization varies over a spatial scale of environmental variability.     

Stable isotopes as markers to investigate host use by Rhyzopertha dominica

Rhyzopertha dominica (F.) (Coleoptera: Bostrichidae) is a serious worldwide pest of stored cereal grains that also has the ability to breed in non‐agricultural host plant material. Stable isotope signatures (concentrations of isotopes) were used as internal tissue markers to determine dietary differences among adult R. dominica and to make inferences about source habitats of field‐trapped insects. Adult R. dominica collected near granaries or from non‐agricultural forested sites near Stillwater, OK, USA, and insects reared on selected hosts under laboratory conditions were studied to determine the carbon and nitrogen isotope signatures. Laboratory‐reared R. dominica showed δ¹³C (stable isotope ratio of carbon) values similar to the host on which they developed with an enrichment of about 1 in the insect body. Insects reared on seeds of wheat and oak, which have C₃ photosynthetic pathways, showed much depleted δ¹³C values (–23.7 and –26.2, respectively) in comparison to insects reared on seeds of corn, a C₄ photosynthetic plant (–11.3). A majority of the field‐collected R. dominica showed δ¹³C values similar to expectations for a C₃ host. However, a few field‐collected insects had δ¹³C signatures similar to the C₄ plant‐reared insects in the laboratory experiment. Stored grain of C₄ crops were lacking at many of the sample field sites. These results suggest that R. dominica occurs on either C₃‐ or C₄‐based hosts in the field, and point to utilization of non‐grain C₄ plants as hosts. Our studies indicated that ¹³C isotope is a reliable marker to infer types of hosts used in the feeding history of R. dominica.     

Variation in the carbon isotope composition of a plant with crassulacean Acid metabolism

The content of ¹³C varies in plants with Crassulacean acid metabolism. Differences up to 3.5‰ in the ¹³C/¹²C ratios were observed between leaves of different age in the same plant of Bryophyllum daigremontianum. Soluble and insoluble carbon in the same leaf differed up to 8‰, the largest difference occurring in the leaves with the highest Crassulacean acid metabolism activity. Models to account for the isotope discrimination by C₃, C₄, and Crassulacean acid metabolism plants are proposed.     

Cyclooxygenase reaction mechanism of prostaglandin H synthase from deuterium kinetic isotope effects

Cyclooxygenase catalysis by prostaglandin H synthase (PGHS) is thought to involve a multistep mechanism with several radical intermediates. The proposed mechanism begins with the transfer of the C13 pro-(S) hydrogen atom from the substrate arachidonic acid (AA) to the Tyr385 radical in PGHS, followed by oxygen insertion and several bond rearrangements. The importance of the hydrogen-transfer step to controlling the overall kinetics of cyclooxygenase catalysis has not been directly examined. We quantified the non-competitive primary kinetic isotope effect (KIE) for both PGHS-1 and -2 using several deuterated AAs, including 13-pro-(S) d-AA, 13,13-d₂-AA and 10, 10, 13,13-d₄-AA. The primary KIE for steady-state cyclooxygenase catalysis, ^Dk_cat, ranged between 1.8 and 2.3 in oxygen electrode measurements. The intrinsic KIE of AA radical formation by C13 pro-(S) hydrogen abstraction in PGHS-1 was estimated to be 1.9-2.3 using rapid freeze-quench EPR kinetic analysis of anaerobic reactions and computer modeling to a mechanism that includes a slow formation of a pentadienyl AA radical and a rapid equilibration of the AA radical with a tyrosyl radical, NS1c. The observation of similar values for steady-state and pre-steady state KIEs suggests that hydrogen abstraction is a rate-limiting step in cyclooxygenase catalysis. The large difference of the observed KIE from that of plant lipoxygenases indicates that PGHS and lipoxygenases have very different mechanisms of hydrogen transfer.     

Purification and properties of glycolate oxidase from plants with different photosynthetic pathways: Distinctness of C4 enzyme from that of a C3 species and a C3–C4 intermediate

Glycolate oxidase (GO; EC 1.1.3.1) was purified from the leaves of three plant species:Amaranthus hypochondriacus L.(NAD-ME type C₄ dicot),Pisum sativum L. (C₃ species) andParthenium hysterophorus L. (C₃–C₄. intermediate). A flavin moiety was present in the enzyme from all the three species. The enzyme from the C₄ plant had a low specific activity, exhibited lower K_M for glycolate, and required a lower pH for maximal activity, compared to the C₃ enzyme. The enzyme from the C₄ species oxidized glyoxylate at <10% of the rate with glycolate, while the GO from the C₃ plant oxidized glyoxylate at a rate of about 35 to 40% of that with glycolate. The sensitivity of GO from C₄ plant to -hydroxypyridinemethane sulfonate, 2-hydroxy-3-butynoate and other inhibitors was less than that of the enzyme from C₃ source. The properties of GO fromParthenium hysterophorus, were similar to those of the enzyme fromPisum sativum. The characteristics of glycolate oxidase from leaves of a C₄ plant,Amaranthus hypochondriacus are different from those of the C₃ species or the C₃–C₄ intermediate.     

Variation in bulk tissue, fatty acid and monosaccharide δ13C values between autotrophic and heterotrophic plant organs

The flowers of 23 species of grass and herb plants were collected from a mesotrophic grassland to assess natural variability in bulk, monosaccharide and fatty acid δ¹³C values from one plant community and were compared with previous analyses of leaves from the same species. The total mean bulk δ¹³C value of flower tissues was −28.1‰, and there was no significant difference between the mean δ¹³C_flower values for grass (−27.8‰) and herb (−28.2‰) species. On average bulk δ¹³C_flower values were 1.1‰ higher than bulk δ¹³C_leaf values, however, the δ¹³C_flower and δ¹³C_leaf values of grasses did not differ between organs suggesting that carbon isotope discrimination is different in grass and herb species. The abundance of different monosaccharides abundance varied between plant types, i.e. xylose concentrations in the grass flowers were as high as 40%, compared with up to 15% in the herb species, but the general relationship δ¹³C_arabinose > δ¹³C_xylose > δ¹³C_glucose > δ¹³C_galactose which had been observed in leaves was similar in flowers (total mean δ¹³C values = −25.9‰, −27.2‰, −28.8‰ and −28.1‰, respectively). However, the average 5.4‰ depletion in the δ¹³C values of the C_16:0, C_18:2 and C_18:3 fatty acids in flowers compared to bulk tissue was significantly greater than observed for leaves. The trend C_16:0 < C_18:2 < C_18:3 previously observed in leaves was also observed in grass flowers (δ¹³C_C16:0 = −33.8‰; δ¹³C_C18:2 = −33.1‰; δ¹³C_C18:3 = −34.2‰) but not herb flowers (δ¹³C_C16:0 = −34.1‰; δ¹³C_C18:2 = −32.4‰; δ¹³C_C18:3 = −34.5‰). We conclude: (i) that the biological processes influencing carbon isotope discrimination in grass flowers are different from herbs flowers; and, (ii) that a range of post-photosynthetic fractionation effects caused the observed differences between flower and leaf δ¹³C values, especially the significant ¹³C-depletion in flower fatty acid δ¹³C values.     

Evidence for a nonstatistical carbon isotope distribution in natural glucose

The relative carbon isotope content (δ¹³C value) in each position of glucose from a C₄ plant (maize starch) and a C₃ plant (sugar beet sucrose) has been determined by stepwise chemical and biochemical degradation of the molecule and stable isotope ratio measurement of the fragments. The suitability of the degradation methods has been tested through their chemical yield and isotope balance. The results from both methods agreed perfectly, revealing a defined and reproducible ¹³C distribution in glucose from both origins. Most prominent was a relative ¹³C enrichment by 5 to 6 δ-units in position 4 and a depletion by about 5 δ-units in carbon 6. As possible reasons for these nonstatistical isotope distributions, isotope effects of the aldolase, the triose phosphate isomerase, and the transketolase reactions during carbohydrate biosynthesis are discussed. The practical importance of the results in regard to isotope distributions in secondary plant products as a means for food authenticity control is outlined.     

Photorespiratory rates in wheat and maize as determined by o-labeling

A method was devised to quantify short-term photorespiratory rates in terrestrial plants using ¹⁸O-intermediates of the glycolate pathway, specifically glycolate, glycine, and serine. The pathway intermediates were isolated and analyzed on a GC/MS to determine molecular percent ¹⁸O-enrichment. Rates of glycolate synthesis were determined from ¹⁸O-labeling kinetics of the intermediates, derived rate equations, and nonlinear regression techniques. Glycolate synthesis in wheat (Triticum aestivum L.), a C₃ plant, and maize (Zea mays L.), a C₄ plant, was stimulated by high O₂ concentrations and inhibited by high CO₂ concentrations. The synthesis rates were 7.3, 2.1, and 0.7 micromoles per square decimeter per minute under a 21% O₂ and 0.035% CO₂ atmosphere for leaf tissue of wheat, maize seedlings, and 3-month-old maize, respectively. Photorespiratory CO₂ evolution rates were estimated to be 27, 6, and 2%, respectively, of net photosynthesis for the three groups of plants under the above atmosphere. The results from maize tissue support the hypothesis that C₄ plants photorespire, albeit at a reduced rate in comparison to C₃ plants, and that the CO₂/O₂ ratio in the bundle sheath of maize is higher in mature tissue than in seedling tissue. The pool size of the three photorespiratory intermediates remained constant and were unaffected by changes in either CO₂ or O₂ concentrations throughout the 10-minute labeling period. This suggests that photorespiratory metabolism is regulated by other mechanism besides phosphoglycolate synthesis by ribulose-1,5-bisphosphate carboxylase/oxygenase, at least under short-term conditions. Other mechanisms could be alternate modes of synthesis of the intermediates, regulation of some of the enzymes of the photorespiratory pathway, or regulation of carbon flow between organelles involved in photorespiration. The glycolate pool became nearly 100% ¹⁸O-labeled under an atmosphere of 40% O₂. This pool failed to become 100% ¹⁸O-enriched under lower O₂ concentrations.     

The pathways of oxalate formation from phenylalanine,tyrosine, tryptophan and ascorbic acid in the rat

The metabolic pathway by which L-[¹⁴C₁]phenylalanine, L-[¹⁴C₁]tyrosine, L-[¹⁴C₁]tryptophan, and L-[¹⁴C₁]ascorbic acid are converted to [¹⁴C]oxalate have been investigated in the male rate. Only [¹⁴C]oxalate was detected in the urine of rats injected with L-[¹⁴C₁]ascorbic acid, but [¹⁴C]-labeled oxalate, glycolate, glyoxylate, glycolaldehyde, glycine, and serine were recovered from the [¹⁴C₁]-labeled aromatic amino acids. DL-Phenyllactate, an inhibitor of glycolic acid oxidase and glycolic acid dehydrogenase, reduced the amount of [¹⁴C]oxalate recovered in the urine of rats given the [¹⁴C₁]-labeled aromatic amino acids, but increased the amount of [¹⁴C]glycolate formed from L-[¹⁴C₁]-phenylalanine and L-[¹⁴C₁]tyrosine and the amount of [¹⁴C]glycolate produced from [¹⁴C₁]tryptophan. Based on the [¹⁴C]labeled intermediates identified and the relative distribution of the radioactivity, it is postulated that phenylalanine and tyrosine are converted to oxalate via glycolate which is oxidized directly to oxalate by glycolic acid dehydrogenase. Tryptophan is metabolized via glyxylate which is oxidized directly to oxalate by glycolic acid oxidase. Neither glycolate, glyoxylate, glycolic acid oxidase or glycolic acid dehydrogenase are involved in the formation of oxalate from ascorbic acid.     

A Study of Formate Production and Oxidation in Leaf Peroxisomes during Photorespiration

When glycolate was metabolized in peroxisomes isolated from leaves of spinach beet (Beta vulgaris L., var. vulgaris) formate was produced. Although the reaction mixture contained glutamate to facilitate conversion of glycolate to glycine, the rate at which H₂O₂ became “available” during the oxidation of [1-¹⁴C]glycolate was sufficient to account for the breakdown of the intermediate [1-¹⁴C]glyoxylate to formate (C₁ unit) and ¹⁴CO₂. Under aerobic conditions formate production closely paralleled ¹⁴CO₂ release from [1-¹⁴C]glycolate which was optimal between pH 8.0 and pH 9.0 and was increased 3-fold when the temperature was raised from 25 to 35 C, or when the rate of H₂O₂ production was increased artificially by addition of an active preparation of fungal glucose oxidase.     

Species-specific differences in temporal and spatial variation in δ13C of plant carbon pools and dark-respired CO2 under changing environmental conditions

Stable carbon isotope signatures are often used as tracers for environmentally driven changes in photosynthetic δ¹³C discrimination. However, carbon isotope signatures downstream from carboxylation by Rubisco are altered within metabolic pathways, transport and respiratory processes, leading to differences in δ¹³C between carbon pools along the plant axis and in respired CO₂. Little is known about the within-plant variation in δ¹³C under different environmental conditions or between species. We analyzed spatial, diurnal, and environmental variations in δ¹³C of water soluble organic matter (δ¹³C_WSOM) of leaves, phloem and roots, as well as dark-respired δ¹³CO₂ (δ¹³C_res) in leaves and roots. We selected distinct light environments (forest understory and an open area), seasons (Mediterranean spring and summer drought) and three functionally distinct understory species (two native shrubs—Halimium halimifolium and Rosmarinus officinalis—and a woody invader—Acacia longifolia). Spatial patterns in δ¹³C_WSOM along the plant vertical axis and between respired δ¹³CO₂ and its putative substrate were clearly species specific and the most δ¹³C-enriched and depleted values were found in δ¹³C of leaf dark-respired CO₂ and phloem sugars, ~?15 and ~?33 ‰, respectively. Comparisons between study sites and seasons revealed that spatial and diurnal patterns were influenced by environmental conditions. Within a species, phloem δ¹³C_WSOM and δ¹³C_res varied by up to 4 ‰ between seasons and sites. Thus, careful characterization of the magnitude and environmental dependence of apparent post-carboxylation fractionation is needed when using δ¹³C signatures to trace changes in photosynthetic discrimination.     

pH Dependence and Kinetics of Glycolate Uptake by Intact Pea Chloroplasts

Experiments in which [1-¹⁴C]glycolate uptake is carried out in conjunction with measurements of stromal pH indicate that only glycolic acid and not the glycolate anion is crossing the pea (Pisum sativum var. Progress No. 9, Agway) chloroplast envelope. This mechanism of glycolate transport appears to be too slow to account for observed photorespiratory carbon fluxes in C₃ plants.     

13C isotope fractionation during rhizosphere respiration of C3 and C4 plants

Stable carbon isotopes are used extensively to partition total soil CO₂ efflux into root-derived rhizosphere respiration or autotrophic respiration and soil-derived heterotrophic respiration. However, it remains unclear whether CO₂ from rhizosphere respiration has the same δ¹³C value as root biomass. Here we investigated the magnitude of ¹³C isotope fractionation during rhizosphere respiration relative to root biomass in six plant species. Plants were grown in a carbon-free sand-perlite medium inoculated with microorganisms from a farm soil for 62 days inside a greenhouse. We measured the δ¹³C value of rhizosphere respiration using a closed-circulation 48-hour CO₂ trapping method during 40~42 and 60~62 days after sowing. We found a consistent depletion in ¹³C (0.9~1.7‰) of CO₂ from rhizosphere respiration relative to root biomass in three C₃ species (Glycine max L. Merr., Helianthus annuus L. and Triticum aestivum L.), but a relatively large depletion in ¹³C (3.7~7.0‰) in three C₄ species (Amaranthus tricolor L., Sorghum bicolor (L.) Moench and Zea mays L. ssp. mays). Overall, our results indicate that CO₂ from rhizosphere respiration is more ¹³C-depleted than root biomass. Therefore, accounting for this ¹³C fractionation is required for accurately partitioning total soil CO₂ efflux into root-derived and soil-derived components using natural abundance stable carbon isotope methods.     

Travels in a world of small science*

As a boy, I read Sinclair Lewis's Arrowsmithand dreamed of doing research of potential benefit to society. I describe the paths of my scientific career that followed. Several distinguished scientists served as my mentors and I present their profiles. Much of my career was in a small department at a small institution where independent researchers collaborated informally. I describe the unique method of carrying on research there. My curiosity about glycolate metabolism led to unraveling the enzymatic mechanism of the glycolate oxidase reaction and showing the importance of H₂O₂ as a byproduct. I discovered enzymes catalyzing the reduction of glyoxylate and hydroxypyruvate. I found α-hydroxysulfonates were useful competitive inhibitors of glycolate oxidase. In a moment of revelation, I realized that glycolate metabolism was an essential part of photorespiration, a process that lowers net photosynthesis in C₃ plants. I added inhibitors of glycolate oxidase to leaves and showed: (1) glycolate was synthesized only in light as an early product of photosynthetic CO₂ assimilation, (2) the rate of glycolate oxidation consumed a sizable fraction of net photosynthesis in C₃ but not in C₄ plants, and (3) that glycolate metabolism increased greatly at higher temperatures. For a while I studied the control of stomatal opening in leaves, and this led to the finding that potassium ions are a key solute in guard cells. I describe experiments that show that when photorespiration rates are high, as occurs at higher temperatures, genetically increasing leaf catalase activity reduces photorespiration and increases net photosythetic CO₂ assimilation. This revised version was published online in June 2006 with corrections to the Cover Date.     

Within trophic level shifts in collagen–carbonate stable carbon isotope spacing are propagated by diet and digestive physiology in large mammal herbivores

Stable carbon isotope analyses of vertebrate hard tissues such as bones, teeth, and tusks provide information about animal diets in ecological, archeological, and paleontological contexts. There is debate about how carbon isotope compositions of collagen and apatite carbonate differ in terms of their relationship to diet, and to each other. We evaluated relationships between δ¹³C_collagen and δ¹³C_carbonate among free‐ranging southern African mammals to test predictions about the influences of dietary and physiological differences between species. Whereas the slopes of δ¹³C_collagen–δ¹³C_carbonate relationships among carnivores are ≤1, herbivore δ¹³C_collagen increases with increasing dietary δ¹³C at a slower rate than does δ¹³C_carbonate, resulting in regression slopes >1. This outcome is consistent with predictions that herbivore δ¹³C_collagen is biased against low protein diet components (¹³C‐enriched C₄ grasses in these environments), and δ¹³C_carbonate is ¹³C‐enriched due to release of ¹³C‐depleted methane as a by‐product of microbial fermentation in the digestive tract. As methane emission is constrained by plant secondary metabolites in browse, the latter effect becomes more pronounced with higher levels of C₄ grass in the diet. Increases in δ¹³C_carbonate are also larger in ruminants than nonruminants. Accordingly, we show that Δ¹³C_collagen‐_carbonate spacing is not constant within herbivores, but increases by up to 5 ‰ across species with different diets and physiologies. Such large variation, often assumed to be negligible within trophic levels, clearly cannot be ignored in carbon isotope‐based diet reconstructions.