Backbone dynamics of bacteriorhodopsin as studied by <Superscript>13</Superscript>C solid-state NMR spectroscopy

The surface dynamics of bacteriorhodopsin was examined by measurements of site-specific ¹³C–¹H dipolar couplings in [3-¹³C]Ala-labeled bacteriorhodopsin. Motions of slow or intermediate frequency (correlation time <50 µs) scale down ¹³C–¹H dipolar couplings according to the motional amplitude. The two-dimensional dipolar and chemical shift (DIPSHIFT) correlation technique was utilized to obtain the dipolar coupling strength for each resolved peak in the ¹³C MAS solid-state NMR spectrum, providing the molecular order parameter of the respective site. In addition to the rotation of the Ala methyl group, which scales the dipolar coupling to 1/3 of the rigid limit value, fluctuations of the C–C vector result in additional motional averaging. Typical order parameters measured for mobile sites in bacteriorhodopsin are between 0.25 and 0.29. These can be assigned to Ala103 of the C–D loop and Ala235 at the C-terminal -helix protruded from the membrane surface, and Ala196 of the F–G loop, as well as to Ala228 and Ala233 of the C-terminal -helix and Ala51 from the transmembrane -helix. Such order parameters departing significantly from the value of 0.33 for rotating methyl groups are obviously direct evidence for the presence of fluctuation motions of the Ala C–C vectors of intact preparations of fully hydrated, wild-type bacteriorhodopsin at ambient temperature. The order parameter for Ala160 from the expectantly more flexible E–F loop, however, is unavailable under highest-field NMR conditions, probably because increased chemical shift anisotropy together with intrinsic fluctuation motions result in an unresolved ¹³C NMR signal.     

Temporal variability in <Superscript>13</Superscript>C of respired CO<Subscript>2</Subscript> in a pine and a hardwood forest subject to similar climatic conditions

Temporal variability in the ¹³C of foliage (¹³C_F), soil (¹³C_S) and ecosystem (¹³C_R) respired CO₂ was contrasted between a 17.2-m tall evenly aged loblolly pine forest and a 35-m tall unevenly aged mature second growth mixed broadleaf deciduous forest in North Carolina, USA, over a 2-year period. The two forests are located at the Duke Forest within a kilometer of each other and are subject to identical climate and have similar soil types. The ¹³C_F, collected just prior to dawn, was primarily controlled by the time-lagged vapor pressure deficit (VPD) in both stands; it was used for calculating the ratio of intercellular to ambient CO₂ (Ci/Ca). A remarkable similarity was observed in the relationship between Ci/Ca and time-lagged VPD in these two forests despite large differences in hydraulic characteristics. This similarity emerged as a result of physiological adjustments that compensated for differences in plant hydraulic characteristics, as predicted by a recently proposed equilibrium hypothesis, and has implications to ecophysiological models. We found that in the broadleaf forest, the ¹³C of forest floor CO₂ efflux dominated the ¹³C_R, while in the younger pine forest, the ¹³C of foliage respired CO₂ dominated ¹³C_R. This dependence resulted in a more variable ¹³C_R in the pine forest when compared to the broadleaf forest due to the larger photosynthetic contribution. Given the sensitivity of the atmospheric inversion models to ¹³C_R, the results demonstrate that these models could be improved by accounting for stand characteristics, in addition to previously recognized effects of moisture availability, when estimating ¹³C_R.     

The Use of the [13C]/[12C] Ratio for the Assay of the Microbial Oxidation of Hydrocarbons

The study deals with a comparative analysis of the relative abundances of the carbon isotopes ¹²C and ¹³C in the metabolites and biomass of the Burkholderia sp. BS3702 and Pseudomonas putida BS202-p strains capable of utilizing aliphatic (n-hexadecane) and aromatic (naphthalene) hydrocarbons as sources of carbon and energy. The isotope compositions of the carbon dioxide, biomass, and exometabolites produced during the growth of Burkholderia sp. BS3702 on n-hexadecane (¹³C = –44.6 ± 0.2) were characterized by the values of ¹³C_{CO 2} = –50.2 ± 0.4, ¹³C_biom = –46.6 ± 0.4, and ¹³C_exo = –41.5 ± 0.4, respectively. The isotope compositions of the carbon dioxide, biomass, and exometabolites produced during the growth of the same bacterial strain on naphthalene (¹³C = –21 ± 0.4) were characterized by the isotope effects ¹³C_{CO 2} = –24.1 ± 0.4, ¹³C_biom = –19.2 ± 0.4, and ¹³C_exo = –19.1 ± 0.4, respectively. The possibility of using the isotope composition of metabolic carbon dioxide for the rapid monitoring of the microbial degradation of petroleum hydrocarbons in the environment is discussed.     

Identification of N-terminal helix capping boxes by means of 13C chemical shifts

Summary We have examined the ¹³C and ¹³C chemical shifts of a number of proteins and found that their values at the N-terminal end of a helix provide a good predictor for the presence of a capping box. A capping box consists of a hydrogen-bonded cycle of four amino acids in which the side chain of the N-cap residue forms a hydrogen bond with the backbone amide of the N3 residue, whose side chain in turn may accept a hydrogen bond from the amide of the N-cap residue. The N-cap residue exhibits characteristic values for its backbone torsion angles, with and clustering around 94±15° and 167±5°, respectively. This is manifested by a 1–2 ppm upfield shift of the ¹³C resonance and a 1–4 ppm downfield shift of the ¹³C resonance, relative to their random coil values, and is mainly associated with the unusually large value of . The residues following the N-cap residue exhibit downfield shifts of 1–3 ppm for the ¹³C resonances and small upfield shifts for the ¹³C ones, typical of an -helix.     

Natural<Superscript>15</Superscript> N Abundance of Plants and Soil N in a Temperate Coniferous Forest

Measurement of nitrogen isotopic composition (¹⁵N) of plants and soil nitrogen might allow the characteristics of N transformation in an ecosystem to be detected. We tested the measurement of ¹⁵N for its ability to provide a picture of N dynamics at the ecosystem level by doing a simple comparison of ¹⁵N between soil N pools and plants, and by using an existing model. ¹⁵N of plants and soil N was measured together with foliar nitrate reductase activity (NRA) and the foliar NO₃^– pool at two sites with different nitrification rates in a temperature forest in Japan. ¹⁵N of plants was similar to that of soil NO₃^– in the high-nitrification site. Because of high foliar NRA and the large foliar NO₃^– pool at this site, we concluded that plant ¹⁵N indicated a great reliance of plants on soil NO₃^– there. However, many ¹⁵N of soil N overlapped each other at the other site, and ¹⁵N could not provide definitive evidence of the N source. The existing model was verified by measured ¹⁵N of soil inorganic N and it explained the variations of plant ¹⁵N between the two sites in the context of relative importance of nitrification, but more information about isotopic fractionations during plant N uptake is required for quantitative discussions about the plant N source. The model applied here can provide a basis to compare ¹⁵N signatures from different ecosystems and to understand N dynamics.     

Measurement of inter-glycosidic 13C-1H coupling constants in a cyclic β(1→2)-glucan by 13C-filtered 2D {1H,1H}ROESY

Summary A method for measuring three-bond ¹³C-¹H scalar coupling constants across glycosidic bonds in a cyclic (12)-glucan icosamer is presented. This oligosaccharide molecule, with its high degree of symmetry, represents a particular challenge for NMR spectroscopy to distinguish inter-residue from intra-residue heteronuclear coupling effects. Chemically equivalent H2 protons in adjacent glucosyl residues are distinguished on the basis of their different through-space, dipolar interactions with the anomeric protons (H1). The strong NOE contact between anomeric (H1) and aglyconic (H2) protons permits the selective observation of the inter-residue heteronuclear couplings ³J_C1H2 and ³J_C2H1 in a natural-abundance ¹³C-₁-half-filtered {¹H,¹H} ROESY experiment.Abbreviations COSY scalar correlated spectroscopy - NOE nuclear Overhauser effect - NOESY NOE spectroscopy - ROESY rotating-frame NOE spectroscopy     

Contribution of methanol to the production of methane and its <Superscript>13</Superscript>C-isotopic signature in anoxic rice field soil

Conversion of methanol to CH₄ has a large isotope effect so that a small contribution of methanol-dependent CH₄ production may decrease the ¹³CH₄ of total CH₄ production. Therefore, we investigated the role of methanol for CH₄ production. Methanol was not detectable above 10 M in anoxic methanogenic rice field soil. Nevertheless, addition of ¹³C-labeled methanol (99% enriched) resulted in immediate accumulation of ¹³CH₄. Addition of 0.1 M ¹³C-methanol resulted in increase of the ¹³CH₄ from –47 to –6 within 2 h, followed by a slow decrease. Addition of 1 M ¹³C-methanol increased ¹³CH₄ to +500 within 4 h, whereas 10 M increased ¹³CH₄ to +2500 and continued to increase. These results indicate that the methanol concentrations in situ, which diluted the ¹³C-methanol added, were 0.1 M and that the turnover of methanol contributed only about 2% to total CH₄ production at 0.1 M. However, contribution increased up to 5 and 17% when 1 and 10 M methanol were added, respectively. Anoxic rice soil that was incubated at different temperatures between 10 and 37 °C exhibited maximally 2–6% methanol-dependent methanogenesis about 1–2 h after addition of 1 M ¹³C-methanol. Only at 50 °C, contribution of methanol to CH₄ production reached a maximum of 10%. After longer (7–10 h) incubation, however, contribution generally was only 2–4%. Methanol accumulated in the soil when CH₄ production was inhibited by chloroform. However, the accumulated methanol accounted for only up to 0.7 and 1.2% of total CH₄ production at 37 and 50 °C, respectively. Collectively, our results show that methanol-dependent methanogenesis was operating in anoxic rice field soil but contributed only marginally to total CH₄ production and the isotope effect observed at both low and high temperature.     

Significance of rooting depth in mire plants: Evidence from natural <Superscript>15</Superscript>N abundance

Variation in stable nitrogen isotope ratios (¹⁵N) was assessed for plants comprising two wetland communities, a bog-fen system and a flood plain, in central Japan. ¹⁵N of 12 species from the bog-fen system and six species from the flood plain were remarkably variable, ranging from –5.9 to +1.1 and from +3.1 to +8.7, respectively. Phragmites australis exhibited the highest ¹⁵N value at both sites. Rooting depth also differed greatly with plant species, ranging from 5cm to over 200cm in the bog-fen system. There was a tendency for plants having deeper root systems to exhibit higher ¹⁵N values; plant ¹⁵N was positively associated with rooting depth. Moreover, an increasing gradient of peat ¹⁵N was found along with depth. This evidence, together with the fact that inorganic nitrogen was depleted under a deep-rooted Phragmites australis stand, strongly suggests that deep-rooted plants actually absorb nitrogen from the deep peat layer. Thus, we successfully demonstrated the diverse traits of nitrogen nutrition among mire plants using stable isotope analysis. The ecological significance of deep rooting in mire plants is that it enables those plants to monopolize nutrients in deep substratum layers. This advantage should compensate for any consequential structural and/or physiological costs. Good evidence of the benefits of deep rooting is provided by the fact that Phragmites australis dominates as a tall mire grass.     

Preparation and heteronuclear 2D NMR spectroscopy of a DNA dodecamer containing a thymidine residue with a uniformly 13C-labeled deoxyribose ring

Summary [¹³C₅]-2-Deoxy-d-ribose, synthesized from [¹³C₆]-d-glucose (98% ¹³C), was coupled with thymine to give [1,2,3,4,5-¹³C₅]-thymidine (T) in an 18% overall yield. The thymidine was converted to the 3-phosphoramidite derivative and was then incorporated into a dodecamer 5-d(CGCGAATTCGCG)-3 by solid-phase DNA synthesis. Preparation of 0.24 mole of the labeled dodecamer, which is sufficient for a single NMR sample, consumed only 25 mg of glucose. By virtue of the ¹³C labels, all of the ¹H-¹H vicinal coupling constants in the sugar moieties were accurately determined by HCCH-E.COSY.     

Keeling plots for hummingbirds: a method to estimate carbon isotope ratios of respired CO<Subscript>2</Subscript> in small vertebrates

The carbon isotope composition of an animals breath reveals the composition of the nutrients that it catabolizes for energy. Here we describe the use of Keeling plots, a method widely applied in ecosystem ecology, to measure the ¹³C of respired CO₂ of small vertebrates. We measured the ¹³C of Rufous Hummingbirds (Selasphorus rufus) in the laboratory and of Mourning (Zenaida macroura) and White-winged (Z. asiatica) Doves in the field. In the laboratory, when hummingbirds were fed a sucrose based C3 diet, the ¹³C of respired CO₂ was not significantly different from that of their diet (¹³C_{C3 diet}). The ¹³C of respired CO₂ for C3 fasted birds was slightly, albeit significantly, depleted in ¹³C relative to ¹³C_{C3 diet}. Six hours after birds were shifted to a sucrose based C4 diet, the isotopic composition of their breath revealed that birds were catabolizing a mixture of nutrients derived from both the C3 and the C4 diet. In the field, the ¹³C of respired CO₂ from Mourning and White-winged Doves reflected that of their diets: the CAM saguaro cactus (Carnegeia gigantea) and C3 seeds, respectively. Keeling plots are an easy, effective and inexpensive method to measure ¹³C of respired CO₂ in the lab and the field.     

Rotational diffusion tensor of nucleic acids from 13C NMR relaxation

Rotational diffusion properties have been derived for the DNA dodecamer d(CGCGAATTCGCG)₂ from ¹³C R₁ and R₁ measurements on the C₁, C₃, and C₄ carbons in samples uniformly enriched in ¹³C. The narrow range of C-H bond vector orientations relative to the DNA axis make the analysis particularly sensitive to small structural deviations. As a result, the R₁/R₁ ratios are found to fit poorly to the crystal structures of this dodecamer, but well to a recent solution NMR structure, determined in liquid crystalline media, even though globally the structures are quite similar. A fit of the R₁/R₁ ratios to the solution structure is optimal for an axially symmetric rotational diffusion model, with a diffusion anisotropy, D_||/D, of 2.1±0.4, and an overall rotational correlation time, (2D_||+4D)^–1, of 3.35 ns at 35 °C in D₂O, in excellent agreement with values obtained from hydrodynamic modeling.     

1H, 15N, 13C and 13CO assignments and secondary structure determination of basic fibroblast growth factor using 3D heteronuclear NMR spectroscopy

Summary The assignments of the ¹H, ¹⁵N, ¹³CO and ¹³C resonances of recombinant human basic fibroblast growth factor (FGF-2), a protein comprising 154 residues and with a molecular mass of 17.2 kDa, is presented based on a series of three-dimensional triple-resonance heteronuclear NMR experiments. These studies employ uniformly labeled ¹⁵N- and ¹⁵N-/¹³C-labeled FGF-2 with an isotope incorporation >95% for the protein expressed in E. coli. The sequence-specific backbone assignments were based primarily on the interresidue correlation of C, C and H to the backbone amide ¹H and ¹⁵N of the next residue in the CBCA(CO)NH and HBHA(CO)NH experiments and the intraresidue correlation of C, C and H to the backbone amide ¹H and ¹⁵N in the CBCANH and HNHA experiments. In addition, C and C chemical shift assignments were used to determine amino acid types. Sequential assignments were verified from carbonyl correlations observed in the HNCO and HCACO experiments and C correlations from the carbonyl correlations observed in the HNCO and HCACO experiments and C correlations from the HNCA experiment. Aliphatic side-chain spin systems were assigned primarily from H(CCO)NH and C(CO)NH experiments that correlate all the aliphatic ¹H and ¹³C resonances of a given residue with the amide resonance of the next residue. Additional side-chain assignments were made from HCCH-COSY and HCCH-TOCSY experiments. The secondary structure of FGF-2 is based on NOE data involving the NH, H and H protons as well as ³J_H n _H coupling constants, amide exchange and ¹³C and ¹³C secondary chemical shifts. It is shown that FGF-2 consists of 11 well-defined antiparallel -sheets (residues 30–34, 39–44, 48–53, 62–67, 71–76, 81–85, 91–94, 103–108, 113–118, 123–125 and 148–152) and a helix-like structure (residues 131–136), which are connected primarily by tight turns. This structure differs from the refined X-ray crystal structures of FGF-2, where residues 131–136 were defined as -strand XI. The discovery of the helix-like region in the primary heparin-binding site (residues 128–138) instead of the -strand conformation described in the X-ray structures may have important implications in understanding the nature of heparin-FGF-2 interactions. In addition, two distinct conformations exist in solution for the N-terminal residues 9–28. This is consistent with the X-ray structures of FGF-2, where the first 17–19 residues were ill defined.     

The 13C Chemical-Shift Index: A simple method for the identification of protein secondary structure using 13C chemical-shift data

Summary A simple technique for identifying protein secondary structures through the analysis of backbone ¹³C chemical shifts is described. It is based on the Chemical-Shift Index [Wishart et al. (1992) Biochemistry, 31, 1647–1651] which was originally developed for the analysis of ¹H chemical shifts. By extending the Chemical-Shift Index to include ¹³C, ¹³C and carbonyl ¹³C chemical shifts, it is now possible to use four independent chemical-shift measurements to identify and locate protein secondary structures. It is shown that by combining both ¹H and ¹³C chemical-shift indices to produce a consensus estimate of secondary structure, it is possible to achieve a predictive accuracy in excess of 92%. This suggests that the secondary structure of peptides and proteins can be accurately obtained from ¹H and ¹³C chemical shifts, without recourse to NOE measurements.Supplementary material is available in the form of a 10-page table (Table S1) describing the exact location of secondary structures in all 20 proteins as determined using the methods described in this paper. Requests for Table S1 should be directed to the authors.     

Insect food preferences analysed using 13C/12C ratios

Summary Stable carbon isotope ratio analysis is a powerful technique in tracing ecosystem carbon flows, especially those between primary and secondary producers. The distinctive ¹³C/¹²C ratios of plant species tend to pass along the food chain with little further fractionation, hence the stable carbon isotope composition of an animal is an important clue to what it has eaten. We compared the stable carbon isotope composition of plants and insects in an old field in Georgia. Of the dominant plants in the old field, 6 were C₄ species and had ¹³C¹ values of-10.9 to 12.9, and 7 were C₃ species with values of-27.3 to-29.1. Insects known to be feeding on only one plant species had ¹³C values within 1 of the isotopic composition of the plant. Wasp larvae parasitizing two insect species had ¹³C values 1.3 and 1.7 higher than that of the food plant. A variety of insects of unknown food habits collected on monospecific and mixed species plant stands in the old field had ¹³C values ranging from-10.1 to-30.0. Two species of leafhopper and a grasshopper had isotopic compositions within the range of C₄ plant values; a tortoise beetle and a lace bug had isotopic compositions within C₃ plant values. Other insects had intermediate ¹³C values, suggesting a mixed diet composed of both C₃ and C₄ plants. The carbon isotopic ratios of field collected insects appears to be a useful qualitative indicator of their feeding preference.     

CO_H(N)CACB experiments for assigningbackbone resonances in 13C/15N-labeledproteins

A triple resonance NMR experiment, denoted CO_H(N)CACB, correlates¹H^N and ¹³CO spins with the¹³C and¹³C spins of adjacent amino acids. Thepulse sequence is an out-and-back design that starts with¹H^N magnetization and transfers coherence viathe ¹⁵N spin simultaneously to the ¹³CO and¹³C spins, followed by transfer to the¹³C spin. Two versions of the sequence arepresented: one in which the ¹³CO spins are frequency labeledduring an incremented t₁ evolution period prior to transfer ofmagnetization from the ¹³C to the¹³C resonances, and one in which the¹³CO spins are frequency labeled in a constant-time mannerduring the coherence transfer to and from the¹³C resonances. Because ¹³COand ¹⁵N chemical shifts are largely uncorrelated, thetechnique will be especially useful when degeneracy in the¹H^N-¹⁵N chemical shifts hindersresonance assignment. The CO_H(N)CACB experiment is demonstrated usinguniformly ¹³C/¹⁵N-labeled ubiquitin.     

Cross-correlated spin relaxation effects in methyl <Superscript>1</Superscript>H CPMG-based relaxation dispersion experiments: Complications and a simple solution

Artifacts associated with the measurement of methyl ¹H single quantum CPMG-based relaxation dispersion profiles are described. These artifacts arise due to the combination of cross-correlated spin relaxation effects involving intra-methyl ¹H–¹H dipolar interactions and imperfections in ¹H refocusing pulses that are applied during CPMG intervals that quantify the effects of chemical exchange on measured transverse relaxation rates. As a result substantial errors in extracted exchange parameters can be obtained. A simple work-around is presented where the ¹H chemical shift difference between the exchanging states is extracted from a combination of ¹³C single quantum and ¹³C–¹H multiple quantum dispersion profiles. The approach is demonstrated with an application to a folding/unfolding reaction involving a G48M mutant Fyn SH3 domain.     

Selectively 13C-enriched DNA: 13C and 1H assignments of a triple helix by two-dimensional relayed HMQC experiments

Summary We present NMR studies of an intramolecular triple helix, the three strands of which have been linked by a hexaethylene glycol chain. To overcome the generally encountered difficulties of assignment in the homopyrimidine strands, the carbon C1 of the pyrimidines were selectively ¹³C-enriched. Assignments of the aromatic and sugar protons were obtained from NOESY-HMQC and TOCSY-HMQC spectra. We show that the recognition of a DNA duplex by a third strand via triplex formation is easily carried out in solution by observing the changes of the ¹H1–¹³C1 connectivities as a function of pH. Furthermore, the conformation of the sugars has been found to be C2-endo, on the basis of the coupling constant values directly measured in an HSQC spectrum.     

13C shieldings, 18O isotope effects on 13C shieldings, and 57Fe-13C spin couplings of the Fe-C-O unit in superstructured hemoprotein models: Comparison with hemoproteins, C-O vibrational frequencies, and X-ray structural data

¹³C NMR spectra of several carbon monoxide (99.7% ¹³C and 11.8% ¹⁸O enriched) hemoprotein models with varying polar and steric effects of the distal organic superstructure and constraints of the proximal side are reported. This enables the ⁵⁷Fe-¹³C(O) coupling constants ( ), ¹³C shieldings ((¹³C)), and ¹⁸O isotope effects on¹³ C shieldings (¹¹³C(¹⁸O/¹⁶O)) to be measured and hence comparisons with hemoproteins, C-O vibrational frequencies and X-ray structural data to be made. Negative polar interactions in the binding pocket and inhibition of Fe//CO back-donation or positive distal polar interactions with amide NH groups appear to have little direct effect on couplings. Similarly, the axial hindered base 1,2-dimethylimidazole has a minor effect on the values despite higher rates of CO desorption being observed for such complexes. On the contrary,¹³ C shieldings vary widely and an excellent correlation was found between the infrared C-O vibrational frequencies ((C-O)) and¹³ C shieldings and a reasonable correlation with¹⁸ O isotope effects on ¹³C shieldings. This suggests that (¹³C), (C-O) and^{1 13} C(¹⁸O/¹⁶O) are accurate monitors of the multiple mechanisms by which steric and electronic interactions are released in superstructured heme model compounds. The ¹³C shieldings of heme models cover a 4.0 ppm range which is extended to 7.0 ppm when several HbCO and MbCO species at different pH values are included. The latter were found to obey a similar linear (¹³ (¹³C) versus (C-O) relationship, which proves that both heme models and heme proteins are homogeneous from the structural and electronic viewpoint. Our results suggest that (C-O), (¹³C) and ¹¹³C(¹⁸O/¹⁶O) measurements reflect similar interaction which is primarily the modulation of back-bonding from the Fe d to the CO * orbital by the distal pocket polar interactions. The lack of correlation between^{1 13} C(¹⁸O/¹⁶O) and crystallographic CO bond lengths (r(C-O)) reflects significant uncertainties in the X-ray determination of the carbon and oxygen positions.     

HNCCH-TOCSY,a triple resonance experiment for the correlation of backbone 13Cα and 15N resonances with aliphatic side-chain proton resonances and for measuring vicinal 13CO, 1Hβ coupling constants in proteins

Summary A 3D triple resonance experiment has been designed to provide intraresidual and sequential correlations between amide nitrogens and -carbons in uniformly ¹³C¹⁵N-labeled proteins. In-phase ¹³C magnetization is transferred to the aliphatic side-chain protons via the side-chain carbons using a CC-TOCSY mixing sequence. Thus, the experiment alleviates the resonance assignment process by providing information about the amino acid type as well as establishing sequential connectivities. Leaving the carbonyl spins untouched throughout the transfer from ¹³C to ¹H leads to E.COSY-type cross peaks, from which the ³J_{H co} coupling constants can be evaluated. The pulse sequence is applied to oxidized Desulfovibrio vulgaris flavodoxin.     

Internal motions of apo-neocarzinostatin as studied by 13C NMR methine relaxation at natural abundance

Summary Dynamics of the backbone and some side chains of apo-neocarzinostatin, a 10.7 kDa carrier protein, have been studied from ¹³C relaxation rates R1, R2 and steady-state ¹³C-{¹H} NOEs, measured at natural abundance. Relaxation data were obtained for 79 nonoverlapping C resonances and for 11 threonine C single resonances. Except for three C relaxation rates, all data were analysed from a simple two-parameter spectral density function using the model-free approach of Lipari and Szabo. The corresponding C–H fragments exhibit fast (_e < 40 ps) restricted libration motions (S²=0.73 to 0.95). Global examination of the microdynamical parameters S² and _e along the amino acid sequence gives no immediate correlation with structural elements. However, different trends for the three loops involved in the binding site are revealed. The -ribbon comprising residues 37 to 47 is spatially restricted, with relatively large _e values in its hairpin region. The other -ribbon (residues 72 to 87) and the large disordered loop ranging between residues 97–107 experience small-amplitude motions on a much faster (picosecond) time scale. The two N-terminal residues, Ala¹ and Ala², and the C-terminal residue Asn¹¹³, exhibit an additional slow motion on a subnanosecond time scale (400–500 ps). Similarly, the relaxation data for eight threonine side-chain C must be interpreted in terms of a three-parameter spectral density function. They exhibit slower motions, on the nanosecond time scale (500–3000 ps). Three threonine (Thr⁶⁵, Thr⁶⁸, Thr⁸¹) side chains do not display a slow component, but an exchange contribution to the observed transverse relaxation rate R2 could not be excluded at these sites. The microdynamical parameters (S², _e and R2_ex) or (S _infslow ^sup2 , S _inffast ^sup2 and _slow) were obtained from a straightforward solution of the equations describing the relaxation data. They were calculated assuming an overall isotropic rotational correlation time _e for the protein of 5.7 ns, determined using standard procedures from R2/R1 ratios. However, it is shown that the product (1–S²)× _e is nearly independent of _e for residues not exhibiting slow motions on the nanosecond time scale. In addition, this parameter very closely follows the heteronuclear NOEs, which therefore could be good indices for local fast motions on the picosecond time scale.