Carbon Isotope Composition of Nighttime Leaf-Respired CO2 in the Agricultural-Pastoral Zone of the Songnen Plain,Northeast China

Variations in the carbon isotope signature of leaf dark-respired CO₂ (δ¹³C_R) within a single night is a widely observed phenomenon. However, it is unclear whether there are plant functional type differences with regard to the amplitude of the nighttime variation in δ¹³C_R. These differences, if present, would be important for interpreting the short-term variations in the stable carbon signature of ecosystem respiration and the partitioning of carbon fluxes. To assess the plant functional type differences relating to the magnitude of the nighttime variation in δ¹³C_R and the respiratory apparent fractionation, we measured the δ¹³C_R, the leaf gas exchange, and the δ¹³C of the respiratory substrates of 22 species present in the agricultural-pastoral zone of the Songnen Plain, northeast China. The species studied were grouped into C₃ and C₄ plants, trees, grasses, and herbs. A significant nocturnal shift in δ¹³C_R was detected in 20 of the studied species, with the magnitude of the shift ranging from 1‰ to 5.8‰. The magnitude of the nighttime variation in δ¹³C_R was strongly correlated with the daytime cumulative carbon assimilation, which suggests that variation in δ¹³C_R were influenced, to some extent, by changes in the contribution of malate decarboxylation to total respiratory CO₂ flux. There were no differences in the magnitude of the nighttime variation in δ¹³C_R between the C₃ and C₄ plants, as well as among the woody plants, herbs and graminoids. Leaf respired CO₂ was enriched in ¹³C compared to biomass, soluble carbohydrates and lipids; however the magnitude of enrichment differed between 8 pm and 4 am, which were mainly caused by the changes in δ¹³C_R. We also detected the plant functional type differences in respiratory apparent fractionation relative to biomass at 4 am, which suggests that caution should be exercised when using the δ¹³C of bulk leaf material as a proxy for the δ¹³C of leaf-respired CO₂.     

Ratios of Carbon Isotopes in Microbial Lipids as an Indicator of Substrate Usage

The occurrence and abundance of microbial fatty acids have been used for the identification of microorganisms in microbial communities. However, these fatty acids can also be used as indicators of substrate usage. For this, a systematic investigation of the discrimination of the stable carbon isotopes by different microorganisms is necessary. We grew 11 strains representing major bacterial and fungal species with four different isotopically defined carbon sources and determined the isotope ratios of fatty acids of different lipid fractions. A comparison of the differences of δ¹³C values of palmitic acid (C_16:0) with the δ¹³C values of the substrates revealed that the isotope ratio is independent of the growth stage and that most microorganisms showed enrichment of C_16:0 with ¹³C when growing on glycerol. With the exception of Burkholderia gladioli, all microorganism showed depletion of ¹³C in C_16:0 while incorporating the carbons of glucose, and most of them were enriched with ¹³C from mannose, with the exception of Pseudomonas fluorescens and the Zygomycotina. Usually, the glycolipid fractions are depleted in ¹³C compared to the phospholipid fractions. The δ¹³C pattern was not uniform within the different fatty acids of a given microbial species. Generally, tetradecanoic acid (C_14:0) was depleted of ¹³C compared to palmitic acid (C_16:0) while octadecanoic acid (C_18:0) was enriched. These results are important for the calibration of a new method in which δ¹³C values of fatty acids from the environment delineate the use of bacterial substrates in an ecosystem.     

Relationships between C3 Plant Foliar Carbon Isotope Composition and Element Contents of Grassland Species at High Altitudes on the Qinghai-Tibet Plateau,China

Relationships of foliar carbon isotope composition (δ¹³C) with foliar C, N, P, K, Ca, Mg contents and their ratios of 219 C₃ species leaf samples, obtained in August in 2004 to 2007 from 82 high altitude grassland sites on the Qinghai-Tibet Plateau China, were examined. This was done with reference to the proposition that foliar δ¹³C increases with altitude and separately for the life-form groups of graminoids, forbs and shrubs and for the genera Stipa and Kobresia. For all samples, foliar δ¹³C was negatively related to foliar K, P and ∑_{K+ Ca+ Mg}, and positively correlated to foliar C, C/N and C/P. The significance of these correlations differed for the taxonomic and life-form groups. Lack of a relationship of foliar δ¹³C with foliar N was inconsistent with the majority of studies that have shown foliar δ¹³C to be positively related to foliar N due to a decrease of C_i/C_a (the ratio between intercellular and atmospheric concentration of CO₂) and explained as a result of greater photosynthetic capacity at higher foliar N concentration. However this inconsistency relates to other high altitude studies that have found that photosynthetic capacity remains constant as foliar N increases. After accounting for the altitudinal relationship with foliar δ¹³C, of the elements only the K effect was significant and was most strongly expressed for Kobresia. It is concluded that factors critical to plant survival and growth at very high altitudes, such as low atmospheric pressure and low temperatures, may preclude expression of relationships between foliar δ¹³C and foliar elements that have been observed at lower altitudes.     

Photosynthetic carbon metabolism of a marine grass

The δ¹³C value of a tropical marine grass Thalassia testudinum is −9.04‰. This value is similar to the δ¹³C value of terrestrial tropical grasses. The δ¹³C values of the organic acid fraction, the amino acid fraction, the sugar fraction, malic acid, and glucose are: −11.2‰, −13.1‰, −10.1‰, −11.1‰, and −11.5‰, respectively. The δ¹³C values of malic acid and glucose of Thalassia are similar to the δ¹³C values of these intermediates in sorghum leaves and attest to the presence of the photosynthetic C₄-dicarboxylic acid pathway in this marine grass. The inorganic HCO₃⁻ for the growth of the grass fluctuates between −6.7 to −2.7‰ during the day. If CO₂ fixation in Thalassia is catalyzed by phosphoenolpyruvate carboxylase (which would result in a −3‰ fractionation between HCO₃⁻ and malic acid), the predicted δ¹³C value for Thalassia would be −9.7 to −5.7‰. This range is close to the observed range of −12.6 to −7.8‰ for Thalassia and agree with the operation of the C₄-dicarboxylic acid pathway in this plant. The early products of the fixation of HCO₃⁻ in the leaf sections are malic acid and aspartic acid which are similar to the early products of CO₂ fixation in C₄ terrestrial plants.     

Effects of Ontogeny on δ13C of Plant- and Soil-Respired CO2 and on Respiratory Carbon Fractionation in C3 Herbaceous Species

Knowledge gaps regarding potential ontogeny and plant species identity effects on carbon isotope fractionation might lead to misinterpretations of carbon isotope composition (δ¹³C) of respired CO₂, a widely-used integrator of environmental conditions. In monospecific mesocosms grown under controlled conditions, the δ¹³C of C pools and fluxes and leaf ecophysiological parameters of seven herbaceous species belonging to three functional groups (crops, forage grasses and legumes) were investigated at three ontogenetic stages of their vegetative cycle (young foliage, maximum growth rate, early senescence). Ontogeny-related changes in δ¹³C of leaf- and soil-respired CO₂ and ¹³C/¹²C fractionation in respiration (Δ_R) were species-dependent and up to 7‰, a magnitude similar to that commonly measured in response to environmental factors. At plant and soil levels, changes in δ¹³C of respired CO₂ and Δ_R with ontogeny were related to changes in plant physiological status, likely through ontogeny-driven changes in the C sink to source strength ratio in the aboveground plant compartment. Our data further showed that lower Δ_R values (i.e. respired CO₂ relatively less depleted in ¹³C) were observed with decreasing net assimilation. Our findings highlight the importance of accounting for ontogenetic stage and plant community composition in ecological studies using stable carbon isotopes.     

Fractionation of Carbon Isotopes during Biogenesis of Atmospheric Isoprene

The stable carbon isotope composition of isoprene emitted from leaves of red oak (Quercus rubra L.) was measured. Isoprene was depleted in ¹³C relative to carbon recently fixed by photosynthesis. The difference in isotope composition between recently fixed carbon and emitted isoprene was independent of the isotopic composition of the source CO₂. β-Carotene, an isoprenoid plant constituent, was depleted in ¹³C relative to whole leaf carbon to the same degree as isoprene, but fatty acids were more depleted. Isoprene emitted from leaves fed abscisic acid was much less depleted in ¹³C than was isoprene emitted from unstressed leaves. We conclude that isoprene is made from an isoprenoid precursor that is derived from acetyl-CoA made from recent photosynthate. The carbon isotope composition of isoprene in the atmosphere is likely to be slightly more negative (less ¹³C) than C₃ plant material but when plants are stressed the isotopic composition could vary.     

Autotrophy in maize husk leaves : evaluation using natural abundance of stable isotopes

The natural abundance of carbon and hydrogen isotopic composition, expressed as a δ¹³C value of plant dry matter and cellulose in the hypsophylls (husk leaves) of maize (Zea mays L.) was measured and compared with that of leaves and cobs. The δ¹³C values of outer hypsophylls were usually 2 to 3%‰ more negative than leaves or other tissues, and became more negative with increasing chlorophyll content, indicating significant local C₃ pathway fixation of CO₂ in the outer hypsophylls. The δD values indicated a significant part of hypsophyll cellulose was derived from heterotrophic sources (sucrose from C₄ photosynthesis in other tissues). Isotopic mass balance calculations allowed quantitative estimation of these carbon sources and, in the samples examined, about 16% of hypsophyll cellulose was derived from local C₃ photosynthesis, about 62% from local C₄ photosynthesis, and about 22% from sucrose imported from other leaves.     

Experimental Evidence for a Hydride Transfer Mechanism in Plant Glycolate Oxidase Catalysis

In plants, glycolate oxidase is involved in the photorespiratory cycle, one of the major fluxes at the global scale. To clarify both the nature of the mechanism and possible differences in glycolate oxidase enzyme chemistry from C₃ and C₄ plant species, we analyzed kinetic parameters of purified recombinant C₃ (Arabidopsis thaliana) and C₄ (Zea mays) plant enzymes and compared isotope effects using natural and deuterated glycolate in either natural or deuterated solvent. The ¹²C/¹³C isotope effect was also investigated for each plant glycolate oxidase protein by measuring the ¹³C natural abundance in glycolate using natural or deuterated glycolate as a substrate. Our results suggest that several elemental steps were associated with an hydrogen/deuterium isotope effect and that glycolate α-deprotonation itself was only partially rate-limiting. Calculations of commitment factors from observed kinetic isotope effect values support a hydride transfer mechanism. No significant differences were seen between C₃ and C₄ enzymes.     

Fractionation of the stable isotopes of inorganic carbon by seagrasses

The δ¹³C values for seagrasses collected along the Texas Gulf Coast range from −10.9 to −11.4‰. These values are similar to the δ¹³C values of terrestrial C₄ plants, but seagrasses lack bundle sheath cells which are important in determining the δ¹³C values of C₄ plants. This work attempts to explain the reason the δ¹³C values of seagrasses resemble the δ¹³C values of C₄ plants.     

Using the Stable Carbon and Nitrogen Isotope Compositions of Vervet Monkeys (Chlorocebus pygerythrus) to Examine Questions in Ethnoprimatology

This study seeks to understand how humans impact the dietary patterns of eight free-ranging vervet monkey (Chlorocebus pygerythrus) groups in South Africa using stable isotope analysis. Vervets are omnivores that exploit a wide range of habitats including those that have been anthropogenically-disturbed. As humans encroach upon nonhuman primate landscapes, human-nonhuman primate interconnections become increasingly common, which has led to the rise of the field of ethnoprimatology. To date, many ethnoprimatological studies have examined human-nonhuman primate associations largely in qualitative terms. By using stable carbon (δ¹³C) and nitrogen (δ¹⁵N) isotope analysis, we use quantitative data to understand the degree to which humans impact vervet monkey dietary patterns. Based on initial behavioral observations we placed the eight groups into three categories of anthropogenic disturbance (low, mid, and high). Using δ¹³C and δ¹⁵N values we estimated the degree to which each group and each anthropogenically-disturbed category was consuming C₄ plants (primarily sugar cane, corn, or processed foods incorporating these crops). δ¹³C values were significantly different between groups and categories of anthropogenic-disturbance. δ¹⁵N values were significantly different at the group level. The two vervet groups with the highest consumption of C₄ plants inhabited small nature reserves, appeared to interact with humans only sporadically, and were initially placed in the mid level of anthropogenic-disturbance. However, further behavioral observations revealed that the high δ¹³C values exhibited by these groups were linked to previously unseen raiding of C₄ crops. By revealing these cryptic feeding patterns, this study illustrates the utility of stable isotopes analysis for some ethnoprimatological questions.     

In Vitro Study of Lipid Biosynthesis in an Anaerobically Methane-Oxidizing Microbial Mat

The anaerobic oxidation of methane (AOM) is a key process in the global methane cycle, and the majority of methane formed in marine sediments is oxidized in this way. Here we present results of an in vitro ¹³CH₄ labeling study (δ¹³CH₄, ~5,400‰) in which microorganisms that perform AOM in a microbial mat from the Black Sea were used. During 316 days of incubation, the ¹³C uptake into the mat biomass increased steadily, and there were remarkable differences for individual bacterial and archaeal lipid compounds. The greatest shifts were observed for bacterial fatty acids (e.g., hexadec-11-enoic acid [16:1Δ11]; difference between the δ¹³C at the start and the end of the experiment [Δδ¹³C_start-end], ~160‰). In contrast, bacterial glycerol diethers exhibited only slight changes in δ¹³C (Δδ¹³C_start-end, ~10‰). Differences were also found for individual archaeal lipids. Relatively high uptake of methane-derived carbon was observed for archaeol (Δδ¹³C_start-end, ~25‰), a monounsaturated archaeol, and biphytanes, whereas for sn-2-hydroxyarchaeol there was considerably less change in the δ¹³C (Δδ¹³C_start-end, ~2‰). Moreover, an increase in the uptake of ¹³C for compounds with a higher number of double bonds within a suite of polyunsaturated 2,6,10,15,19-pentamethyleicosenes indicated that in methanotrophic archaea there is a biosynthetic pathway similar to that proposed for methanogenic archaea. The presence of group-specific biomarkers (for ANME-1 and ANME-2 associations) and the observation that there were differences in ¹³C uptake into specific lipid compounds confirmed that multiple phylogenetically distinct microorganisms participate to various extents in biomass formation linked to AOM. However, the greater ¹³C uptake into the lipids of the sulfate-reducing bacteria (SRB) than into the lipids of archaea supports the hypothesis that there is autotrophic growth of SRB on small methane-derived carbon compounds supplied by the methane oxidizers.     

Stable Carbon Isotope Ratios of Lipid Biomarkers of Sulfate-Reducing Bacteria

We examined the potential use of natural-abundance stable carbon isotope ratios of lipids for determining substrate usage by sulfate-reducing bacteria (SRB). Four SRB were grown under autotrophic, mixotrophic, or heterotrophic growth conditions, and the δ¹³C values of their individual fatty acids (FA) were determined. The FA were usually ¹³C depleted in relation to biomass, with Δδ¹³C_{(FA − biomass)} of −4 to −17‰; the greatest depletion occurred during heterotrophic growth. The exception was Desulfotomaculum acetoxidans, for which substrate limitation resulted in biomass and FA becoming isotopically heavier than the acetate substrate. The δ¹³C values of FA in Desulfotomaculum acetoxidans varied with the position of the double bond in the monounsaturated C₁₆ and C₁₈ FA, with FA becoming progressively more ¹³C depleted as the double bond approached the methyl end. Mixotrophic growth of Desulfovibrio desulfuricans resulted in little depletion of the i17:1 biomarker relative to biomass or acetate, whereas growth with lactate resulted in a higher proportion of i17:1 with a greater depletion in ¹³C. The relative abundances of 10Me16:0 in Desulfobacter hydrogenophilus and Desulfobacterium autotrophicum were not affected by growth conditions, yet the Δδ¹³C_{(FA − substrate)} values of 10Me16:0 were considerably greater during autotrophic growth. These experiments indicate that FA δ¹³C values can be useful for interpreting carbon utilization by SRB in natural environments.     

Isotope Fractionation in Photosynthetic Bacteria during Carbon Dioxide Assimilation

The δ _PDB¹³C values have been determined for the cellular constituents and metabolic intermediates of autotrophically grown Chromatium vinosum. The isotopic composition of the HCO₃^- in the medium and the carbon isotopic composition of the bacterial cells change with the growth of the culture. The δ _PDB¹³C value of the HCO₃^- in the media changes from an initial value of −6.6‰ to +8.1‰ after 10 days of bacterial growth and the δ _PDB¹³C value of the bacterial cells change from −37.5‰ to −29.2‰ in the same period. The amount of carbon isotope fractionation during the synthesis of hexoses by the photoassimilation of CO₂ has a range of −15.5‰ at time zero to −22.0‰ after 10 days. This range of fractionation compares to the range of carbon isotope fractionation for the synthesis of sugars from CO₂ by ribulose 1,5-diphosphate carboxylase and the Calvin cycle.     

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 Isotope Labeled n-Alkanes to Assess Digesta Passage Kinetics through the Digestive Tract of Ruminants

We describe the use of carbon stable isotope (¹³C) labeled n-alkanes as a potential internal tracer to assess passage kinetics of ingested nutrients in ruminants. Plant cuticular n-alkanes originating from intrinsically ¹³C labeled ryegrass plants were pulse dosed intraruminally in four rumen-cannulated lactating dairy cows receiving four contrasting ryegrass silage treatments that differed in nitrogen fertilization level (45 or 90 kg nitrogen ha⁻¹) and maturity (early or late). Passage kinetics through the gastrointestinal tract were derived from the δ¹³C (i.e. the ratio ¹³C:¹²C) in apparently undigested fecal material. Isotopic enrichment was observed in a wide range of long-chain n-alkanes (C₂₇–C₃₆) and passage kinetics were determined for the most abundant C₂₉, C₃₁ and C₃₃ n-alkanes, for which a sufficiently high response signal was detected by combustion isotope ratio mass spectrometry. Basal diet treatment and carbon chain length of n-alkanes did not affect fractional passage rates from the rumen (K ₁) among individual n-alkanes (3.71–3.95%/h). Peak concentration time and transit time showed a quantitatively small, significant (p≤0.002) increase with carbon chain length. K ₁ estimates were comparable to those of the ¹³C labeled digestible dry matter fraction (3.38%/h; r = 0.61 to 0.71; p≤0.012). A literature review has shown that n-alkanes are not fermented by microorganisms in the rumen and affirms no preferential depletion of ¹³C versus ¹²C. Our results suggest that ¹³C labeled n-alkanes can be used as nutrient passage tracers and support the reliability of the δ¹³C signature of digestible feed nutrients as a tool to measure nutrient-specific passage kinetics.     

Quantifying Inter-Laboratory Variability in Stable Isotope Analysis of Ancient Skeletal Remains

Over the past forty years, stable isotope analysis of bone (and tooth) collagen and hydroxyapatite has become a mainstay of archaeological and paleoanthropological reconstructions of paleodiet and paleoenvironment. Despite this method''s frequent use across anthropological subdisciplines (and beyond), the present work represents the first attempt at gauging the effects of inter-laboratory variability engendered by differences in a) sample preparation, and b) analysis (instrumentation, working standards, and data calibration). Replicate analyses of a ¹⁴C-dated ancient human bone by twenty-one archaeological and paleoecological stable isotope laboratories revealed significant inter-laboratory isotopic variation for both collagen and carbonate. For bone collagen, we found a sizeable range of 1.8‰ for δ¹³C_col and 1.9‰ for δ¹⁵N_col among laboratories, but an interpretatively insignificant average pairwise difference of 0.2‰ and 0.4‰ for δ¹³C_col and δ¹⁵N_col respectively. For bone hydroxyapatite the observed range increased to a troublingly large 3.5‰ for δ¹³C_ap and 6.7‰ for δ¹⁸O_ap, with average pairwise differences of 0.6‰ for δ¹³C_ap and a disquieting 2.0‰ for δ¹⁸O_ap. In order to assess the effects of preparation versus analysis on isotopic variability among laboratories, a subset of the samples prepared by the participating laboratories were analyzed a second time on the same instrument. Based on this duplicate analysis, it was determined that roughly half of the isotopic variability among laboratories could be attributed to differences in sample preparation, with the other half resulting from differences in analysis (instrumentation, working standards, and data calibration). These findings have serious implications for choices made in the preparation and extraction of target biomolecules, the comparison of results obtained from different laboratories, and the interpretation of small differences in bone collagen and hydroxyapatite isotope values. To address the issues arising from inter-laboratory comparisons, we devise a novel measure we term the Minimum Meaningful Difference (MMD), and demonstrate its application.     

Compensation point and isotopic characteristics of c(3)/c(4) intermediates and hybrids in panicum

Leaf CO₂ compensation points and stable hydrogen, oxygen and carbon isotope ratios were determined for Panicum species including C₃/C₄ intermediate photosynthesis plants, hybrids between C₃/C₄ intermediates and C₃ plants, C₃ and C₄ plants in the Panicum genus as well as several other C₃ and C₄ plants. C₃ plants had the highest compensation points, followed by hybrids, C₃/C₄ intermediates, and C₄ plants. δ¹³C values of cellulose nitrate and saponifiable lipids from C₄ plants were about 10‰ higher than those observed for cellulose nitrate and saponifiable lipids of C₃/C₄ intermediates, hybrids, and C₃ plants. Oxygen isotope ratios of cellulose as well as those of leaf water were similar for all plants. There was substantial variability in the δD values of cellulose nitrate among the plants studied. In contrast, such variability was not observed in δD values of water distilled from the leaves, nor in the δD values of the saponifiable lipids. Variability in δD values of cellulose nitrate from C₃/C₄ intermediates, hybrids, C₃, and C₄ plants is due to fractionations occurring during biochemical reactions specific to leaf carbohydrate metabolism.     

Stable isotope canopy effects for sympatric monkeys at Ta? Forest,C?te d'Ivoire

This study tests the hypothesis that vertical habitat preferences of different monkey species inhabiting closed canopy rainforest are reflected in oxygen isotopes. We sampled bone from seven sympatric cercopithecid species in the Taï forest, Côte d''Ivoire, where long-term study has established taxon-specific patterns of habitat use and diet. Modern rib samples (n = 34) were examined for oxygen (δ¹⁸O_ap) and carbon (δ¹³C_ap) from bone apatite (‘bioapatite’), and carbon (δ¹³C_co) and nitrogen (δ¹⁵N_co) from bone collagen. Results are consistent for C₃ feeders in a closed canopy habitat. Low irradiance and evapotranspiration, coupled with high relative humidity and recycled CO₂ in forest understory, contribute to observed isotopic variability. Both δ¹³C_co and δ¹³C_ap results reflect diet; however, δ¹³C values are not correlated with species preference for canopy height. By contrast, δ¹⁸O_ap results are correlated with mean observed height and show significant vertical partitioning between taxa feeding at ground, lower and upper canopy levels. This oxygen isotope canopy effect has important palaeobiological implications for reconstructing vertical partitioning among sympatric primates and other species in tropical forests.     

Fossil Mice and Rats Show Isotopic Evidence of Niche Partitioning and Change in Dental Ecomorphology Related to Dietary Shift in Late Miocene of Pakistan

Stable carbon isotope analysis in tooth enamel is a well-established approach to infer C₃ and C₄ dietary composition in fossil mammals. The bulk of past work has been conducted on large herbivorous mammals. One important finding is that their dietary habits of fossil large mammals track the late Miocene ecological shift from C₃ forest and woodland to C₄ savannah. However, few studies on carbon isotopes of fossil small mammals exist due to limitations imposed by the size of rodent teeth, and the isotopic ecological and dietary behaviors of small mammals to climate change remain unknown. Here we evaluate the impact of ecological change on small mammals by fine-scale comparisons of carbon isotope ratios (δ¹³C) with dental morphology of murine rodents, spanning 13.8 to ∼2.0 Ma, across the C₃ to C₄ vegetation shift in the Miocene Siwalik sequence of Pakistan. We applied in-situ laser ablation GC-IRMS to lower first molars and measured two grazing indices on upper first molars. Murine rodents yield a distinct, but related, record of past ecological conditions from large herbivorous mammals, reflecting available foods in their much smaller home ranges. In general, larger murine species show more positive δ¹³C values and have higher grazing indices than smaller species inhabiting the same area at any given age. Two clades of murine rodents experienced different rates of morphological change. In the faster-evolving clade, the timing and trend of morphological innovations are closely tied to consumption of C₄ diet during the vegetation shift. This study provides quantitative evidence of linkages among diet, niche partitioning, and dental morphology at a more detailed level than previously possible.