Determination of 13Cα relaxation times in uniformly 13C/15N-enriched proteins

Summary Relaxation times of ¹³C carbons of uniformly ¹³C/¹⁵N-enriched probes have been investigated. The relaxation behaviour was analyzed in terms of a multispin system. Pulse sequences for the determination of T₁, T₂ and the heteronuclear NOE of ¹³C in uniformly ¹³C/¹⁵N-enriched ribonuclease T1 are presented. The experiments performed in order to obtain T₁ and the heteronuclear NOE were similar to those of the corresponding ¹⁵N experiments published previously. The determination of T₂ for the C-carbon in a completely labeled protein is more complicated, since the magnetization transfer during the T₂ evolution period owing to the scalar coupling of C–C must be suppressed. Various different pulse sequences for the T₂ evolution period were simulated in order to optimize the bandwidth for which reliable T₂ relaxation times can be obtained. A proof for the quality of these pulse sequences is given by fitting the intensity decay of individual ¹H–¹³C cross peaks, in a series of (¹H, ¹³C)-ct-HSQC spectra with a modified CPMG sequence as well as a T_1p sequence for the transverse relaxation time, to a single exponential using a simplex algorithm.     

Synthesis and SAR of C12–C13-oxazoline derivatives of epothilone A

The SAR of a series of new epothilone A derivatives with a 2-substituted-1,3-oxazoline moiety trans-fused to the C12–C13 bond of the deoxy macrocycle have been investigated with regard to tubulin polymerization induction and cancer cell growth inhibition. Significant differences in antiproliferative activity were observed between different analogs, depending on the nature of the substituent at the 2-position of the oxazoline ring. The most potent compounds showed comparable activity with the natural product epothilone A. Modeling studies provide a preliminary rationale for the observed SAR.     

Identification of Zinc-ligated Cysteine Residues Based on 13Cα and 13Cβ Chemical Shift Data

Although a significant number of proteins include bound metals as part of their structure, the identification of amino acid residues coordinated to non-paramagnetic metals by NMR remains a challenge. Metal ligands can stabilize the native structure and/or play critical catalytic roles in the underlying biochemistry. An atom’s chemical shift is exquisitely sensitive to its electronic environment. Chemical shift data can provide valuable insights into structural features, including metal ligation. In this study, we demonstrate that overlapped ¹³Cβ chemical shift distributions of Zn-ligated and non-metal-ligated cysteine residues are largely resolved by the inclusion of the corresponding ¹³Cα chemical shift information, together with secondary structural information. We demonstrate this with a bivariate distribution plot, and statistically with a multivariate analysis of variance (MANOVA) and hierarchical logistic regression analysis. Using 287 ¹³Cα/¹³Cβ shift pairs from 79 proteins with known three-dimensional structures, including 86 ¹³Cα and¹³Cβ shifts for 43 Zn-ligated cysteine residues, along with corresponding oxidation state and secondary structure information, we have built a logistic regression model that distinguishes between oxidized cystines, reduced (non-metal ligated) cysteines, and Zn-ligated cysteines. Classifying cysteines/cystines with a statisical model incorporating all three phenomena resulted in a predictor of Zn ligation with a recall, precision and F-measure of 83.7%, and an accuracy of 95.1%. This model was applied in the analysis of Bacillus subtilis IscU, a protein involved in iron–sulfur cluster assembly. The model predicts that all three cysteines of IscU are metal ligands. We confirmed these results by (i) examining the effect of metal chelation on the NMR spectrum of IscU, and (ii) inductively coupled plasma mass spectrometry analysis. To gain further insight into the frequency of occurrence of non-cysteine Zn ligands, we analyzed the Protein Data Bank and found that 78% of the Zn ligands are histidine and cysteine (with nearly identical frequencies), and 18% are acidic residues aspartate and glutamate. Electronic Supplementary Material Supplementary material is available for this article at and is accessible for authorized users.     

Stratification of δ13C values of leaves in Amazonian rain forests

Summary The contribution of soil respiration to the photosynthesis of the shade flora in the Amazon forest was evaluated by measuring the ¹³C values of leaves collected at different levels in two forest communities. Canopy leaves have an average ¹³C of-30.5 in the podsol forest and-28.7 in the laterite forest. Leaves from plants in the lower forest strata have a significantly lower value of-35.2 in the podsol forest and-34.3 in the laterite forest.Mailing address of the first author: Before May 31, 1980: Department of Biological Sciences, Stanford University, Stanford, California 94305 USA. After May 31: Centro de Ecologia, IVIC Aptdo. 1827. Caracas, Venezuela     

Study of protein dynamics in solution by measurement of 13Cα-13CO NOE and 13CO longitudinal relaxation

Summary ¹³C-¹³CO homonuclear NOE and ¹³CO T₁ relaxation were measured for a 20 kDa protein using tripleresonance pulse sequences. The experiments were sufficiently sensitive to obtain statistically significant differences in relaxation parameters over the molecule. The ¹³C-¹³CO cross-relaxation rate, obtained from these data, is directly proportional to an order parameter describing local motion and it is largely independent of the local correlation time. It is therefore a relatively straightforward observable for the identification of local dynamics.     

Automated prediction of 15N, 13Cα, 13Cβ and 13C′ chemical shifts in proteins using a density functional database

A database of peptide chemical shifts, computed at the density functional level, has been used to develop an algorithm for prediction of ¹⁵N and ¹³C shifts in proteins from their structure; the method is incorporated into a program called SHIFTS (version 4.0). The database was built from the calculated chemical shift patterns of 1335 peptides whose backbone torsion angles are limited to areas of the Ramachandran map around helical and sheet configurations. For each tripeptide in these regions of regular secondary structure (which constitute about 40% of residues in globular proteins) SHIFTS also consults the database for information about sidechain torsion angle effects for the residue of interest and for the preceding residue, and estimates hydrogen bonding effects through an empirical formula that is also based on density functional calculations on peptides. The program optionally searches for alternate side-chain torsion angles that could significantly improve agreement between calculated and observed shifts. The application of the program on 20 proteins shows good consistency with experimental data, with correlation coefficients of 0.92, 0.98, 0.99 and 0.90 and r.m.s. deviations of 1.94, 0.97, 1.05, and 1.08 ppm for ¹⁵N, ¹³C, ¹³C and ¹³C, respectively. Reference shifts fit to protein data are in good agreement with `random-coil' values derived from experimental measurements on peptides. This prediction algorithm should be helpful in NMR assignment, crystal and solution structure comparison, and structure refinement.     

Measurement of 13Cα-13CO cross-relaxation rates in 15N-/13C-labelled proteins

Summary Internal motions play an important role in the biological function of proteins and NMR relaxation studies may characterize them over a wide range of frequencies. An experimental pulse scheme is proposed for the measurement of the ¹³CO-¹³C cross-relaxation rate. For sensitivity reasons, this measurement is performed in an indirect manner through several coherence transfer steps, which should thus be calibrated independently. Contributions of other relaxation pathways can be eliminated by the determination of the initial slope of the buildup curve. The cross-relaxation rates have been determined on a ¹⁵N-/¹³C-labelled 116-residue protein and the significant variations along the sequence have been interpreted as evidence of an increased amount of fast local motion.     

δ13C values of some succulent plants from Madagascar

Summary ¹³C values were determined in 20 succulents from Madagascar. The values were indicative of Crassulacean Acid Metabolism in 10 species of the Didiereaceae, 4 species of the Euphorbiaceae, 2 species of the Crassulaceae and 1 species of the Cucurbitaceae. The Didiereaceae and Euphorbiaceae studied are major components of a high biomass xerophytic flora in the semi-arid southwest and south of Madagascar. Three species of the Euphorbiaceae with succulent stems and non-succulent leaves, which were cultivated outdoors in the Tananarive Botanic Garden, showed C₃ like ¹³C values for both leaves and stems. ¹³C values of leaf and stem material from a similar species, collected in the south of Madagascar, indicated Crassulacean Acid Metabolism.Abbreviations CAM Crassulacean Acid Metabolism     

Does the 13C of foliage‐respired CO2 and biochemical pools reflect the 13C of recently assimilated carbon?

Isotopic labelling experiments were conducted to assess relationships among ¹³C of recently assimilated carbon ( δC _A), foliage respiration ( δC _F), soluble carbohydrate ( δC _SC), leaf waxes ( δC _LW) and bulk organic matter ( δC _OM). Slash pine, sweetgum and maize were grown under ¹³C depleted CO₂ to label biomass and then placed under ambient conditions to monitor the loss of label. In pine and sweetgum, δC _F of labelled plants (∼−44 and −35‰, respectively) rapidly approached control values but remained depleted by ∼4–6‰ after 3–4 months. For these tree species, no or minimal label was lost from δC _SC, δC _LW and δC _OM during the observation periods. δC _F and δC _SC of labelled maize plants rapidly changed and were indistinguishable from controls after 1 month, while δC _LW and δC _OM more slowly approached control values and remained depleted by 2–6‰. Changes in δC _F in slash pine and sweetgum fit a two-pool exponential model, with the fast turnover metabolic pool (∼3–4 d half-life) constituting only 1–2% of the total. In maize, change in δC _F fits a single pool model with a half-life of 6.4 d. The ¹³C of foliage respiration and biochemical pools reflect temporally integrated values of δC _A, with change in isotopic composition dampened by the size of metabolic carbon reserves and turnover rates.     

Biosynthesis of trehalose byBrevibacterium flavum: Use of long range13C−13C coupling data to characterize triose phosphate isomerase activity

The¹³C isotopic labeling pattern in the disaccharide trehalose (l,1---D-glucose) produced by the micro-organismBrevibacterium flavum when grown on a medium containing [1-{au13}C]glucose has been determined. Long range coupling between C-1 and C-6 carbons of the glucose units can be observed in the excreted material . It is proposed that some of the¹³C isotopomers in the excreted trehalose reflect the labeling pattern in (unobserved) fructose 1,6-diphosphate. Analysis of the label distribution within the framework of a steady state kinetic model allows an analysis of the contributions of the hexose monophosphate shunt and the degree of equilibration of triose phosphate isomerase. Analogous measurements on excreted glucose could be carried out in other organisms.     

δ13C values of an herbivore and the ratio of C3 to C4 plant carbon in its diet

Summary The ¹³C values of whole body samples of the beetle Tribolium castaneum are closely correlated with the ¹³C values of the plant carbon in its diet. The correlation is always high for diets ranging from 100% C₄ to 100% C₃ plant material. The degree of correlation is independent of the growth rate of the animals.     

Quantitative J correlation methods for the accurate measurement of 13C′-13Cαdipolar couplings in proteins

Methods are described for the precise and accurate measurement of one-bond dipolar (13)C'-(13)C(alpha) couplings in weakly aligned proteins. The experiments are based on the principle of quantitative J correlation, where (1)J(C'C(alpha)) (or (1)J(C'C(alpha)) + 1D(C'C(alpha)) is measured from the relative intensity of two interleaved 3D TROSY-HN(CO)CA or 3DTROSY-HNCO spectra recorded with dephasing intervals of zero (reference spectrum) and approximately 3/(2(1)J(C'C(alpha)) (attenuated spectrum). In analogy to other quantitative J correlation techniques, the random error in the measured (1)J(C'C(alpha)) value is inversely proportional to the signal-to-noise ratio in the reference spectrum. It is shown that for weakly aligned proteins, with the magnitude of the alignment tensor of D(a)(NH) < or = 10-15 Hz, the systematic errors are typically negligible. The methods are demonstrated for the third IgG-binding domain of protein G (GB3) and a-synuclein in complex with a detergent micelle, where errors in (1)D(C'C(alpha)) of less than 0.1 Hz and ca. 0.2 Hz,respectively, are estimated. Remarkably, the dipolar couplings determined for GB3 are in even better agreement with the recently refined 1.1-angstroms X-ray structure than the input (13)C'-(13)C(alpha) couplings used for the refinement.     

A 13C NMR spectrometric method for the determination of intramolecular δ13C values in fructose from plant sucrose samples

Recent developments in (13) C NMR spectrometry have allowed the determination of intramolecular (13) C/(12) C ratios with high precision. However, the analysis of carbohydrates requires their derivatization to constrain the anomeric carbon. Fructose has proved to be particularly problematic because of a byproduct occurring during derivatization and the complexity of the NMR spectrum of the derivative. Here, we describe a method to determine the intramolecular (13) C/(12) C ratios in fructose by (13) C NMR analysis of the acetyl-isopropylidene derivative. We have applied this method to measure the intramolecular (13) C/(12) C distribution in the fructosyl moiety of sucrose and have compared this with that in the glucosyl moiety. Three prominent features stand out. First, in sucrose from both C(3) and C(4) plants, the C-1 and C-2 positions of the glucosyl and fructosyl moieties are markedly different. Second, these positions in C(3) and C(4) plants show a similar profile. Third, the glucosyl and fructosyl moieties of sucrose from Crassulacean acid metabolism (CAM) metabolism have a different profile. These contrasting values can be interpreted as a result of the isotopic selectivity of enzymes that break or make covalent bonds in glucose metabolism, whereas the distinctive (13) C pattern in CAM sucrose probably indicates a substantial contribution of gluconeogenesis to glucose synthesis.     

The 13C/12C isotopic signal of day-respired CO2 in variegated leaves of Pelargonium × hortorum

In leaves, although it is accepted that CO(2) evolved by dark respiration after illumination is naturally (13) C-enriched compared to organic matter or substrate sucrose, much uncertainty remains on whether day respiration produces (13) C-depleted or (13) C-enriched CO(2). Here, we applied equations described previously for mesocosm CO(2) exchange to investigate the carbon isotope composition of CO(2) respired by autotrophic and heterotrophic tissues of Pelargonium × hortorum leaves, taking advantage of leaf variegation. Day-respired CO(2) was slightly (13) C-depleted compared to organic matter both under 21% O(2) and 2% O(2). Furthermore, most, if not all CO(2) molecules evolved in the light came from carbon atoms that had been fixed previously before the experiments, in both variegated and green leaves. We conclude that the usual definition of day respiratory fractionation, that assumes carbon fixed by current net photosynthesis is the respiratory substrate, is not valid in Pelargonium leaves under our conditions. In variegated leaves, total organic matter was slightly (13) C-depleted in white areas and so were most primary metabolites. This small isotopic difference between white and green areas probably came from the small contribution of photosynthetic CO(2) refixation and the specific nitrogen metabolism in white leaf areas.     

Analysis of δ13C of CO2 distinguishes between microbial respiration of added C4-sucrose and other soil respiration in a C3-ecosystem

The main aim of this study was to test various hypotheses regarding the changes in ¹³C of emitted CO₂ that follow the addition of C₄-sucrose to the soil of a C₃-ecosystem. It forms part of an experimental series designed to assess whether or not the contributions from C₃-respiration (root and microbial) and C₄-respiration (microbial) to total soil respiration can be calculated from such changes. A series of five experiments, three on sieved (root-free) mor-layer material, and two in the field with intact mor-layer (and consequently with active roots), were performed. Both in the experiments on sieved mor-layer and the field experiments, we found a C₄-sucrose-induced increase in C₃-respiration that accounted for between 30% and 40% of the respiration increase 1 h after sucrose addition. When the course of C₃-, C₄- and total respiration was followed in sieved material over four days following addition of C₄-sucrose, the initially increased respiration of C₃-C was transient, passing within less than 24 h. In a separate pot experiment, neither ectomycorrhizal Pinus sylvestrisL. roots nor non-mycorrhizal roots of this species showed respiratory changes in response to exogenous sucrose. No shift in the ¹³C of the evolved CO₂ after adding C₃-sucrose to sieved mor-layer material was found, confirming that the sucrose-induced increase in respiration of endogenous C was not an artefact of discrimination against ¹³C during respiration. Furthermore, we conclude that the C₄-sucrose induced transient increase in C₃-respiration is most likely the result of accelerated turnover of C in the microbial biomass. Thus, neither respiration of mycorrhizal roots, nor processes discriminating against ¹³C were likely sources of error in the field. The estimated ¹³C of evolved soil CO₂ in three field experiments lay between –25.2 and –23.6. The study shows that we can distinguish between CO₂ evolved from microbial mineralisation of added C₄-sucrose, and CO₂ evolved from endogenous carbon sources (roots and microbial respiration).     

Seasonal Variation of δ13C of Four Tree Species: A Biological Integrator of Environmental Variables

Foliar δ13C values, an indicator of long-term intercellular carbon dioxide concentration and, thus,of long-term water use efficiency (WUE) in plants, were measured for Pinus massoniana Lamb., P. elliottii Engelm., Cunninghamia laceolata (Lamb.) Hook., and Schima superba Gardn. et Champ. in a restored forest ecosystem in the Jiazhu River Basin. Seasonal variation and the relationship between the foliar δ13Cvalues of the four species and environmental factors (monthly total precipitation, monthly average air temperature, relative humidity, atmospheric pressure, and monthly total solar radiation and evaporation)were investigated. The monthly δ13C values and WUE of the four species increased with increasing precipitation, air temperature, solar radiation, and evaporation, whereas δ13C values of the four species decreased with increasing relative humidity and atmospheric pressure. Despite significant differences in δ13C seasonal means for the four species, our results demonstrate a significant convergence in the responses of δ13C values and WUE to seasonal variations in environmental factors among the species investigated and that the δ13C signature for each species gives a strong indication of environmental variables.     

Intraresidue 1H-15N-13C′ and 1Hα-13Cα-13C′ dipole-CSA relaxation interference as a source of constraints for structural refinement of metal-binding sites in zinc-finger proteins

¹H(i)-¹⁵N(i)-¹³C(i) dipole-chemical shift anisotropy (CSA) relaxation interference was quantified for the ¹³C,¹⁵N labeled zinc-finger protein qCRP2(LIM2). The cross-correlation rates obtained for residues located in the metal coordination sites of qCRP2(LIM2) show a high degree of correlation with the peptide plane torsion angles and taken from the solution structure. ¹H(i)-¹⁵N(i)-¹³C(i) as well as ¹³C(i)-¹H(i)-¹³C(i) dipole-CSA cross-correlation rates were subsequently used to improve the geometry of the metal binding site. The optimized dihedral angles of the two zinc-binding sites in qCRP2(LIM2) are in better agreement with values obtained from crystal structures of other zinc-finger proteins and thus establish the utility of this approach to improve the metal-binding site geometry of zinc-finger proteins studied by NMR spectroscopy in solution.     

Accurate measurements of the effects of deuteration at backbone amide positions on the chemical shifts of 15N, 13Cα, 13Cβ, 13CO and 1Hα nuclei in proteins

An approach towards accurate NMR measurements of deuterium isotope effects on the chemical shifts of all backbone nuclei in proteins (¹⁵N, ¹³C_α, ¹³CO, ¹H_α) and ¹³C_β nuclei arising from ¹H-to-D substitutions at amide nitrogen positions is described. Isolation of molecular species with a defined protonation/deuteration pattern at successive backbone nitrogen positions in the polypeptide chain allows quantifying all deuterium isotope shifts of these nuclei from the first to the fourth order. Some of the deuterium isotope shifts measured in the proteins ubiquitin and GB1 can be interpreted in terms of backbone geometry via empirical relationships describing their dependence on (φ; ψ) backbone dihedral angles. Because of their relatively large variability and notable dependence on the protein secondary structure, the two- and three-bond ¹³C_α isotope shifts, ²ΔC_α(N_iD) and ³ΔC_α(N_i+1D), and three-bond ¹³C_β isotope shifts, ³ΔC_β(N_iD), are useful reporters of the local geometry of the protein backbone.     

Estimation of canopy average mesophyll conductance using δ(13) C of phloem contents

Conductance to CO(2) inside leaves, known as mesophyll conductance (g(m)), imposes large limitations on photosynthesis. Because g(m) is difficult to quantify, it is often neglected in calculations of (13)C photosynthetic discrimination. The 'soluble sugar method' estimates g(m) via differences between observed photosynthetic discrimination, calculated from the δ(13)C of soluble sugars, and discrimination when g(m) is infinite. We expand upon this approach and calculate a photosynthesis-weighted average for canopy mesophyll conductance ((c) g(m)) using δ(13)C of stem phloem contents. We measured gas exchange at three canopy positions and collected stem phloem contents in mature trees of three conifer species (Pseudotsuga menziesii, Thuja plicata and Larix occidentalis). We generated species-specific and seasonally variable estimates of (c)g(m) . We found that (c)g(m) was significantly different among species (0.41, 0.22 and 0.09 mol m(-2) s(-1) for Larix, Pseudotsuga and Thuja, respectively), but was similar throughout the season. Ignoring respiratory and photorespiratory fractionations ((c)Δ(ef)) resulted in ≈30% underestimation of (c)g(m) in Larix and Pseudotsuga, but was innocuous in Thuja. Substantial errors (~1-4‰) in photosynthetic discrimination calculations were introduced by neglecting (c)g(m) and (c)Δ(ef) . Our method is easy to apply and cost-effective, captures species variation and would have captured seasonal variation had it existed. The method provides an average canopy value, which makes it suitable for parameterization of canopy-scale models of photosynthesis, even in tall trees.