Abstract
The formation of the transcriptionally-competent open complex (RPo) by E. coli RNA polymerase at the λPR promoter involves at least three steps and two kinetically-significant intermediates (I1 and I2). Understanding the sequence of conformational changes (rearrangements in the jaws of RNAP, DNA opening) that occur in the conversion of I1 to RPo requires: 1) dissecting the rate constant kd for the dissociation of RPo into contributions from individual steps and 2) isolating and characterizing I2. To deconvolute kd, we develop experiments involving rapid upshifts to elevated concentrations of RPo-destabilizing solutes (“perturbants”: urea and KCl) to create a burst in the population of I2. At high concentrations of either perturbant, kd approaches the same [perturbant]-independent value at both 10 °C and 37 °C, interpreted as the rate constant k−2 for I2 → I1. The large effects of [urea] and [salt] on K3 (the equilibrium constant for I2 ⇄ RPo) indicate that a large-scale folding transition in polymerase forms a new interface with the DNA late in the mechanism. We deduce that I2 at the λPR promoter is always unstable relative to RPo, even at 0 °C, explaining previous difficulties in detecting it by using temperature downshifts. Evidence for an additional unstable intermediate (I3) in the mechanism between I2 and RPo is presented. The large positive enthalpy change associated with open complex formation is divided between the steps converting I1 to RPo, consistent with a mechanism in which DNA opening occurs in several stages.
Keywords: Bacterial RNA polymerase, open complex formation, kinetics, solute effects, conformational changes
INTRODUCTION
To initiate RNA synthesis, RNA polymerase (RNAP) locally separates the complementary strands of promoter DNA around the transcription start site and places the start site base on the template strand into its active site. Defining the cascade of conformational changes that occur during initiation and how they are regulated by promoter sequence and transcription factors is essential for understanding genetic expression, for defining the input into transcriptional networks, and for designing inhibitors of this essential process in disease-causing organisms. For the bacterial RNAP, open complex formation occurs in the absence of NTP hydrolysis or a helicase cofactor. For eukaryotic RNAP, additional protein cofactors are required to open the start site, although their roles in opening the DNA remain unclear 1. Despite evolutionary differences in complexity, the extensive structural and functional homology between multi-subunit RNAPs from all kingdoms 2 renders the relatively simple E. coli enzyme a relevant model for the key steps in initiation, as well as providing a reference point for comparison with transcription by eukaryotic RNAP.
For E. coli RNAP holoenzyme (core enzyme (α2, β, β’, and ω subunits) and σ70 specificity subunit), formation of the transcriptionally-competent open complex (RPo) proceeds through a series of steps following the recognition of a specific promoter DNA sequence. In RPo, the DNA is unpaired and unstacked from the AT-rich −10 hexamer to just downstream of the transcription start site, a span of ~14 base pairs. At the λPR promoter, this open region extends from position −11 to +3 3; 4; 5, with numbering relative to the start site, +1. Despite decades of study of open complex formation, fundamental questions remain regarding this essential cellular process. For example, it is still unclear what conformational changes in RNAP are required for DNA opening and whether opening occurs in a single step or in several.
Addressing these mechanistic questions requires kinetic studies to provide essential information regarding the numbers of steps and intermediates involved in the overall process of forming RPo and the characteristic rate and/or equilibrium constants of these steps. Kinetic data for formation and dissociation of RPo involving E. coli RNAP (R) and the λPR promoter (P) is described by a mechanism consisting of a minimum of three steps with two kinetically significant intermediates 6; 7; 8:
| (Mechanism I) |
In Mechanism I, under conditions typically used in studies of open complex formation (4 – 42 °C, moderate salt concentration), I1 rapidly equilibrates with free RNAP and promoter DNA on the time scale required for I1 to convert to I2, and I2 rapidly equilibrates with RPo on the time scale required for I2 to convert to I1. Notably, the interconversion I1 ⇄ I2 is the rate-limiting step in both the forward and reverse directions 6; 9; 10. Additional intermediates between the free species and I1 and between I2 and RPo may exist. However, they are not included in Mechanism I because evidence for them has not been obtained from previous kinetic studies. (Other intermediate complexes must be included in nested sets of rapid equilibria that determine K1 and K3.)
In excess RNAP, the kinetics of formation of open complexes between free RNAP and λPR promoter DNA are single exponential. In this case, measurements of the [RNAP]-dependence of the observed association rate constant are unambiguously interpreted in terms of K1 (K1 = k1/k−1; the equilibrium constant for R + P ⇄ I1) and k2 (the rate constant for I1 → I2) 9; 10. The behaviors of K1 and k2 as functions of reaction conditions (such as temperature 9 and solute concentrations 11) provide insight into the driving forces and molecular processes involved in the formation of I1 from free RNAP and DNA and its conversion to the subsequent transition state, (I1-I2)‡. For example, the small dependence of K1 on urea concentration 11 implies that no large-scale folding transitions in RNAP occur concurrently with binding in R + P ⇄ I1 (see Background Section).
Analogous information regarding the molecular processes that occur in the steps of the latter half of Mechanism I (the conversion of (I1-I2‡) into RPo via I2) is contained in the kinetics of conversion of RPo back into free reactants (dissociation). At a minimum, the kinetically-significant steps of irreversible dissociation (initiated by addition of an excess of the polyanionic competitor heparin, which acts as a DNA mimic to sequester free RNAP) are 10:
| (Mechanism II) |
Previous studies of the kinetics of dissociation indicate that large-scale conformational changes occur in the latter half of Mechanism I. The large increases in the rate of dissociation with increasing concentrations of univalent salt 7; 12; 13 and urea 11 indicate that a new RNAP-DNA interface forms and that ~120 amino acid residues fold in (I1-I2)‡⇄I2 ⇄ RPo (see Background Section). The large positive activation heat capacity change 8; 13 associated with the rate constant for dissociation (kd; see Background Section) is also consistent with the hypothesis that a large-scale folding transition in RNAP occurs in (I1-I2)‡ ⇄ I2 ⇄ RPo (as a heat capacity change in a biopolymer process often signals a protein folding event 14). The strong acceleration of RPo dissociation by the in vivo regulatory factors ppGpp and DksA at all promoters studied to date15; 16 indicates that they bind to (I1-I2)‡ and/or I2 more strongly than to RPo. These large effects are consistent with the existence of large-scale conformational changes occurring in the conversions between these species. For example, we have proposed that ppGpp and DksA accelerate dissociation by disfavoring the folding transition involved in converting I2 to RPo 11.
Evidence also shows that DNA opening at the λPR promoter may occur, at least in part, during the latter half of Mechanism I. In I1, promoter DNA around the transcription start site is unreactive to KMnO4 and therefore presumably still double helical 3; 17, while fourteen base pairs (−11 to +3) are deduced to be open in RPo 3; 4; 5. Thus, DNA opening must occur in I1 → I2 and/or I2 → RPo. Large positive enthalpy changes are also associated with these steps, consistent with the large enthalpic cost associated with melting DNA. A large positive activation energy (activation enthalpy) is observed for the conversion of I1 to (I1-I2)‡ (Ea (2) = 34 kcal/mol 9), and the negative activation energy of dissociation indicates that the van’t Hoff enthalpy change ΔHo(3) for I2 ⇄ RPo must be large and positive at low temperature 8; 13.
Because RPo and I2 equilibrate rapidly on the time scale of converting I2 to I1, it has proven difficult to separate the steps that determine the dissociation kinetics (Mechanism II) and to isolate and characterize I2. The goal of the present study is to unambiguously dissect, for the first time, the contributions of RPo ⇄ I2 and I2 → I1 to the rate of open complex dissociation. This information can, in turn, be used to characterize the molecular processes occurring in the steps and to design experiments to trap and characterize the elusive I2.
One method of deconvoluting the kinetics of dissociation is a so-called “burst” experiment, in which a reaction variable is rapidly shifted in an attempt to destabilize RPo and increase the population of I2. Use of temperature downshift bursts after initially forming RPo at high temperatures were attempted based on the conclusion that ΔHo(3) for I2 ⇄ RPo is large and positive and the inference that a downshift in temperature will therefore rapidly depopulate RPo 3; 18; 19; 20. However, the difficulty of performing a temperature downshift rapidly, the temperature dependence of the rate of KMnO4 reactivity (activation energy ~ 8 kcal/mol; M. Capp, unpublished data), and the possibility of artifacts (such as off-pathway complexes formed in the downshifts 21; 22) may have complicated the interpretations of these experiments.
In this study, we have designed isothermal burst (upshift) experiments, in which preformed open complexes are rapidly shifted to elevated concentrations of either urea or KCl and the dissociation kinetics are followed. We find that the rate constant for dissociation of open complexes (kd) reaches or approaches a [urea]- and [KCl]-independent value at both 10 and 37 °C, signifying that either k−3 (RPo → I2) or k−2 (I2 → I1) is independent of [perturbant]. Based on an analogy between our data and the effect of [urea] on the kinetics and equilibria of protein folding, we propose that the plateau value of kd represents the rate constant k−2, and that the entire effects of [urea] and [salt] on kd are contained in RPo ⇄ I2 (i.e. k−3 and k3). Implications of these results for the nature of I2 and of the steps converting I1 to RPo are discussed.
BACKGROUND
Formulation of the dissociation rate constant kd
For systems where the kinetics of dissociation of open complexes are single exponential (as observed for the λPR promoter under almost all conditions studied 6; 7; 11), the dissociation rate constant kd is interpreted without approximation as 10:
| (1) |
where K3 = k3/k−3.
Under conditions where the interconversion of RPo and I2 in Mechanism II rapidly equilibrates on the time scale required for I2 to convert to I1 (k3 ≫ k−2), deduced experimentally from the negative activation energy of kd 6; 8; 13, eq 1 can be simplified, depending on the relative magnitude of K3 10:
| (2a) |
or
| (2b) |
Interpretation of the effect of nondenaturing concentrations of urea on a biopolymer process and application to the study of the kinetics of open complex formation
Urea has been shown to interact preferentially (i.e. relative to interactions with water) primarily with amide groups (specifically with the polar N and O atoms) of proteins and model compounds 23; 24; 25; 26; 27; 28; 29; 30. Preferential interactions of urea with other groups on proteins and nucleic acids (such as predominantly nonpolar or charged groups) have not been detected in studies with biopolymers 24; 25. We have quantified this interaction per unit of polar amide surface area (ASApolar amide) 24; 28; 30, thus making [urea] an effective quantitative probe of changes in the solvent exposure of amide surface area associated with biopolymer processes:
| (3) |
where Kobs is the observed equilibrium quotient for a biopolymer process and ΔASApolar amide is the change in the amount of water-accessible polar amide surface area in converting the reactant state to the product state. A test of the usefulness of [urea] as a probe of ΔASApolar amide was provided by a study of lac repressor binding to operator DNA; the observed effect of [urea] on the binding constant Kobs agrees with that predicted from structural information on the amount of polar amide surface buried in complex formation 30.
This method of analysis has been used to interpret the [urea]-dependences of K1, k2, and kd in Mechanism I and Mechanism II 11. The moderate initial dependence of K1 on [urea] is consistent with the polar amide surface area known or predicted to be buried in the large RNAP-DNA interface formed in R + P ⇄ I1, without having to invoke additional large-scale folding transitions. The lack of a dependence of k2 on [urea] implies that there is no net exposure of polar amide surface in the conversion of I1 to the subsequent transition state (I1-I2)‡. The large dependence of kd on [urea] was interpreted as a large-scale folding transition in a region of RNAP in (I1-I2)‡ ⇄ RPo. Specifically, we proposed that disordered regions in the C-terminus of the β’ subunit, including the downstream jaw, fold in I2 ⇄ RPo.
Experiments performed at moderate urea concentrations under reversible conditions, where the kinetics of the association and dissociation reactions can be measured simultaneously (Supporting Information of 11 and unpublished data), result in values for kd that are the same within error as those obtained from irreversible dissociation experiments at the same urea concentrations. This result provides evidence that the intermediates involved in the forward and reverse processes in the presence of perturbant are the same.
RESULTS
The dissociation of RNAP-promoter open complexes following upshifts in perturbant (urea or KCl) concentration shows single exponential kinetics
The rate of dissociation of open complexes (RPo) formed between E. coli RNAP and λPR promoter DNA is greatly accelerated by increasing concentrations of urea 11 and salt 6; 7; 12. We monitored the dissociation of pre-formed open complexes following a rapid upshift in either [urea] (up to 5.0 M) or [KCl] (up to 1.10 M) in order to dissect the contributions of RPo ⇄ I2 and I2 → I1 (Mechanism II) to the overall [perturbant] dependences of kd. [Evidence that these experiments monitor the dissociation kinetics of RPo by Mechanism II and not by an alternative mechanism induced by high [salt] or [urea] (such as holoenzyme or DNA denaturation) is presented in the Analysis Section.] Representative data for these dissociation experiments are shown in Figure 1([urea] upshifts) and Figure 2 ([KCl] upshifts). These data are well fit by single-exponential decays (eq 4, Methods) under every set of reaction conditions studied; fits are represented by solid lines for the 10 °C data and dashed lines for the 37 °C data. Values of the dissociation rate constant kd from fits to eq 4 are given in Table 1 (for the [urea] upshifts) and Table 2 (for the [KCl] upshifts). The single exponential character of the data validates the use of eq 1 (Background Section) in the analysis of all values of kd 10.
Figure 1.

Dissociation of RNA polymerase (RNAP)-λPR promoter open complexes after upshifts in urea concentration. Preformed open complexes in Dissociation Buffer (DB) were mixed with a solution of DB containing urea and heparin to obtain the urea concentrations listed. Data are plotted as the fraction of DNA originally bound in open complexes remaining bound after upshift (θt/θ0). Black symbols represent data taken at 37 °C. White symbols represent data taken at 10 °C. Lines are fits of the data to a single exponential decay (eq 4 in the text). Dashed lines are fits to the 37 °C data, and solid lines are fits to the 10 °C data. Rate constants (kd) from the fits are contained in Table 1. (a) Upshifts to 0 (circles), 0.5 (triangles), and 1.0 (squares) M urea. (b) Upshifts to 1.5 (circles), 2.0 (triangles), and 3.0 (squares) M urea. (c) Upshifts to 3.5 (circles), 4.0 (triangles), and 4.5 (squares) M urea.
Figure 2.

Dissociation of RNAP-λPR promoter open complexes after upshifts in KCl concentration. Preformed open complexes in Dissociation Buffer (DB) were mixed with a solution of DB containing additional KCl and heparin to obtain the KCl concentrations listed. Data are plotted as the fraction of DNA originally bound in open complexes remaining bound after upshift (θt/θ0). Black symbols represent data taken at 37 °C. White symbols represent data taken at 10 °C. Lines are fits of the data to a single exponential decay (eq 4 in the text). Dashed lines are fits to the 37 °C data, and solid lines are fits to the 10 °C data. Rate constants (kd) from the fits are contained in Table 2. (a) Upshifts to 0.12 (circles), 0.15 (triangles), and 0.18 (squares) M KCl. (b) Upshifts to 0.24 (circles), 0.30 (triangles), and 0.38 (squares) M KCl. (c) Upshifts to 0.60 (circles), 0.80 (triangles), and 1.10 (squares) M KCl. Note: The data at 0 M urea in Figure 1 is the same as the data at 0.12 M KCl in Figure 2 (replotted for comparison).
Table 1.
Values of the rate constant for the dissociation of open complexes (kd) following upshift in urea concentration.
| kd (s−1)a |
||
|---|---|---|
| [urea] (M) | 37 °C | 10 °C |
| 0 | 1.9 (±0.6) × 10−5 | 2.1 (±0.2) × 10−4 |
| 0.5 | 6.0 (±1.2) × 10−5 | 1.35 (±0.06) × 10−3 |
| 1.0 | 3.2 (±0.6) × 10−4 | 7.1 (±0.5) × 10−3 |
| 1.5 | 1.4 (±0.3) × 10−3 | 4.1 (±0.7) × 10−2 |
| 2.0 | 8.9 (±2.2) × 10−3 | 1.2 (±0.2) × 10−1 |
| 2.5 | 3.8 (±1.5) × 10−2 | 2.0 (±0.2) × 10−1 |
| 3.0 | 9.4 (±1.4) × 10−2 | 3.1 (±0.2) × 10−1 |
| 3.5 | 2.5 (±0.7) × 10−1 | 4.7 (±0.2) × 10−1 |
| 4.0 | 5.5 (±2.2) × 10−1 | 7.0 (±1.2) × 10−1 |
| 4.5 | 6.9 (±0.4) × 10−1 | 7.0 (±0.6) × 10−1 |
| 5.0 | 1.4 ±0.2 | - |
Table 2.
Values of the rate constant for the dissociation of open complexes (kd) following upshift in KCl concentration.
| kd (s−1)a |
||
|---|---|---|
| [KCl] (M) | 37 °C | 10 °C |
| 0.12 | 1.9 (±0.6) × 10−5 | 2.1 (±0.2) × 10−4 |
| 0.15 | 7.3 (±0.7) × 10−5 | 6.9 (±0.4) × 10−4 |
| 0.18 | 1.9 (±0.4) × 10−4 | 1.6 (±0.2) × 10−3 |
| 0.24 | 1.3 (±0.1) × 10−3 | 1.15 (±0.07) × 10−2 |
| 0.30 | 1.0 (±0.3) × 10−2 | 5.3 (±0.9) × 10−2 |
| 0.38 | 9.1 (±5.2) × 10−2 | 1.1 (±0.1) × 10−1 |
| 0.48 | 4.8 (±0.6) × 10−1 | - |
| 0.60 | 1.6 ±0.7 | 4.2 (±0.7) × 10−1 |
| 0.80 | 2.3 ±0.8 | 5.5 (±1.4) × 10−1 |
| 1.10 | 3.3 ±0.2 | 7.3 (±0.6) × 10−1 |
The rate of open complex dissociation is strongly driven by [perturbant] at low perturbant concentrations but independent of [perturbant] at high perturbant concentrations
In Figure 3, the natural logarithm of kd (ln kd) is plotted versus [urea] (panel a), and against ln [KCl] (panel b). At the lowest concentrations of both urea (up to ~1.5 M at 10 °C and ~2.5 M at 37 °C) and KCl (up to ~0.30 M at 10 °C and ~0.48 M at 37 °C), ln kd increases dramatically with increasing [perturbant] (linearly versus [urea] and with a slight positive (upward) curvature versus ln [KCl]). At higher concentrations of both perturbants, the rate of open complex dissociation becomes less dependent on [perturbant], resulting in negative (downward) curvature in the data in Figure 3. For example, while dlnkd/d[urea] at 10 °C between 0 M urea and 0.5 M urea is ~3.5 M−1, dlnkd/d[urea] is only ~1 M−1 between 2.0 M urea and 3.0 M urea (Fig 3a). Likewise, at 37 °C, between 0.30 M KCl and 0.38 M KCl, dlnkd/dln[KCl] = ~9.3, while between 0.48 M KCl and 0.60 M KCl, dlnkd/dln[KCl] = ~5.4 (Fig 3b).
Figure 3.

The natural logarithm (ln) of the dissociation rate constant kd (from fits of the kinetic data represented in Fig 1 and Fig 2 to eq 4) plotted versus [urea] (a) and ln [KCl] (b). Black points are for data taken at 37 °C; white points are for data taken at 10 °C. In (a), solid lines are fits of the data to an expression (utilizing eq 5, eq 7, and eq 8 in the text) in which dependences of the equilibrium constant K3 (I2 ⇄ RPo) and the rate constant k−3 (RPo → I2) on [urea] are incorporated into the general expression for kd (eq 1). Dashed lines are fits of the data to an expression (utilizing eq 6 and eq 7) in which only the dependence of K3 on [urea] is incorporated into a simplified expression for kd (eq 2a). In (b), solid lines are fits of the data to an expression (utilizing eq 6, eq 9–eq 11) in which a dependence of K3 on [KCl] was incorporated into the simplified expression for kd (eq 2a). Horizontal dotted lines represent values of ln k−2 determined from the fits.
At the highest concentrations of either perturbant, the rate of open complex dissociation becomes essentially independent of [perturbant]. This is particularly evident in Figure 3b, where kd appears to have reached a [KCl]-independent plateau at both 10 and 37 °C (for example, at 37 °C, kd = 2.3 ± 0.8 s−1 at 0.80 M KCl and 3.3 ± 0.2 s−1 at 1.10 M KCl (Fig. 2c, Table 2)). Similarly, in Fig 3a, kd at 10 °C appears to have reached a [urea]-independent plateau (kd =7.0 (± 1.2) × 10−1 s−1 at 4.0 M urea and 7.0 (± 0.6) × 10−1 s−1 at 4.5 M urea (Fig. 1c, Table 1)). While kd at 37 °C is still increasing with [urea] at the highest urea concentration studied (kd = 6.9 (± 0.4) × 10−1 s−1 at 4.5 M urea and 1.4 ± 0.2 s−1 at 5.0 M urea (Fig. 1c, Table 1)), it also appears to be gradually approaching a plateau at even higher [urea] (Fig 3a).
The dissociation of open complexes is characterized by a negative activation energy at low perturbant concentrations and a positive activation energy at high perturbant concentrations
At the lowest urea and KCl concentrations studied, kd is much larger at 10 °C than at 37 °C (Fig 3 and Table 1 and Table 2). This difference is vividly demonstrated in Fig 1a and Fig 2a: dissociation of open complexes is much faster at 10 °C than at 37 °C in 0, 0.5, and 1.0 M urea (Fig 1a) and in 0.12, 0.15, and 0.18 M KCl (Fig 2a). The negative activation energy for kd implies that a rapidly equilibrating initial step (or steps) precedes the rate-determining step in dissociation (because an elementary rate constant cannot have a negative activation energy). The earlier observation of this negative activation energy originally motivated the inclusion of a second kinetically-significant intermediate (I2) into Mechanism I 6; 8; 19.
As the perturbant concentrations are increased, the differences between kd at 10 and 37 °C decrease (i.e. the negative activation energy in each perturbant decreases in magnitude) until, after upshift to some [urea] and [KCl], the values of kd at 10 and 37 °C converge (where the activation energy is zero) (Fig 3 and Table 1 and Table 2). As seen in Fig 1c, this occurs at ~4.5 M urea, where open complexes dissociate at roughly the same rate at 10 and 37 °C (kd is 6.9 (± 0.4) × 10−1 s−1 at 37 °C and 7.0 (± 0.6) × 10−1 s−1 at 10 °C). In Fig 2b, the rate of dissociation is essentially independent of temperature at 0.38 M KCl (kd = 9.1 (± 5.2) × 10−2 s−1 at 37 °C and 1.1 (± 0.1) × 10−1 s−1 at 10 °C).
At concentrations of KCl higher than 0.38 M, kd is significantly larger at 37 °C than at 10 °C (Fig 3b and Table 2); this is dramatically apparent in Fig 2c, where dissociation of open complexes is clearly faster at 37 °C than at 10 °C in 0.60, 0.80, and 1.10 M KCl. This temperature dependence of dissociation at high [KCl] results in a positive activation energy for the process. The data indicate that a positive activation energy is likely at high concentrations of urea as well. While kd is the same at 10 and 37 °C at 4.5 M urea (the highest concentration for which there is data at both temperatures), kd has reached its [urea]-independent value already by 4.5 M urea at 10 °C (Fig. 3a, Table 1), and so would be expected to have that same value at all higher concentrations of urea. However, at 37 °C, kd is still increasing: at 5.0 M urea, kd = 1.4 ± 0.2 s−1. Thus, at urea concentrations greater than 4.5 M, kd is likely larger at 37 °C than at 10 °C. Because values of kd at high [KCl] and [urea] at both 10 and 37 °C are independent of perturbant concentration, the positive activation energy of kd in this regime is also independent of perturbant concentration.
ANALYSIS
Interpretation of kd at high perturbant concentrations: The rate of dissociation is determined by the rate of I2 → I1
The simplest interpretation of the [perturbant]-independent positive activation energy for open complex dissociation at high perturbant concentrations (represented by the higher plateau value of kd at 37 °C than at 10 °C in Fig 3) is that I2 no longer rapidly converts back to the higher enthalpy state RPo on the time scale over which I2 converts to I1. In order for the rapid equilibrium in I2 ⇄ RPo to break down, I2 → I1 must become faster than I2 → RPo, resulting in a mechanism of dissociation consisting of two sequential uni-directional steps at high [perturbant]:
| (Mechanism III) |
In general, analysis of Mechanism III for the situation where both RPo and I2 are detectable and where k−3 and k−2 are of comparable magnitude yields a lag phase in the dissociation of detectable complexes. Since the data in Fig 1c and Fig 2c (for dissociation of detectable complexes at high perturbant concentrations) are well fit by a single exponential decay (without an apparent lag phase), one of the rate constants in the back direction, either k−2 or k−3, must be large enough that it does not contribute to the overall observable kinetics of dissociation. In this high [perturbant] regime, dissociation of detectable complexes must therefore be represented by one or the other of the following mechanisms:
| (Mechanism IVa) |
or
| (Mechanism IVb) |
For Mechanism IVa to be applicable, k−2 would have to exceed k−3 by enough so that no I2 accumulates on the time scale of the conversion of RPo to I2. For Mechanism IVb to be applicable, k−3 would have to exceed k−2 by enough so that all RPo converts to I2 before significant dissociation of I2 commences (and within the time resolution of the experiment). Because the plateaus at high perturbant concentrations are independent of [perturbant], whichever rate constant determines kd in this regime (either k−3 or k−2) is independent of [perturbant].
Although the data alone do not allow us to distinguish between Mechanism IVa and Mechanism IVb because of the symmetry between k−2 and k−3 in the general expression for kd (eq 1), we propose that Mechanism IVb describes the dissociation of detectable complexes at high [perturbant]. Our reasoning is based on an analogy between the [urea]-dependent step in open complex formation and the two-state process of folding a single-domain globular protein. In general, for proteins for which the rates of folding (kfold) and unfolding (kunfold) have been determined as functions of urea concentration, the overall [urea]-dependence of the equilibrium constant (Kobs = kfold/kunfold) is distributed to some extent (between 30 and 70% of the overall effect on each) between kfold and kunfold (see 31). The rate constants k2 (I1 → I2) and k−2 (I2 → I1) are the forward and reverse elementary rate constants that make up the equilibrium K2 (I1 ⇄ I2); because we previously found that k2 is independent of [urea] 11, it is unlikely that k−2 would contain a significant [urea]-dependence. Thus, it is most likely that the [urea]-dependence is contained within k3 and k−3. (While a situation in which the [urea]-dependence of a biopolymer process is fully contained within only one of the rate constants that make up the equilibrium constant for the process may not be physically impossible, to our knowledge no examples of it exist.)
The behavior of kd at high concentrations of urea and KCl strongly supports our conclusion that Mechanism II (at low [perturbant]) and Mechanism IVb (at high [perturbant]) characterize the dissociation of RNAP-promoter complexes, and that other mechanisms (such as RNAP or DNA denaturation) are not significant. In particular, if perturbant-induced denaturation were occurring, we would expect the rate of dissociation to continue increasing with perturbant concentration, rather than reaching [perturbant]-independent plateaus, as are seen in the data. Moreover, the native forms of RNAP holoenzyme 32 and DNA 33 are stable at high salt concentrations, so upshifts in KCl concentration cannot be inducing denaturation. The observation that the rate of dissociation at high [perturbant] is independent of the identity of perturbant (most explicitly evident at 10 °C; Fig 3) implies that the same dissociation process is occurring at both high [urea] and high [KCl]. Thus, we conclude that if other salt- or urea-induced processes do occur, they do so only after the transition state (I1-I2)‡ has been formed in the dissociation direction, and therefore do not influence the observed kinetics of dissociation.
The step I1 ⇄ I2 is highly endothermic
From the values of k−2 at 10 and 37 °C (Table 3), we estimate the activation energy for k−2 (Ea(−2) = −RΔlnk−2/Δ (1/T)) to be 9.9 kcal/mol. This activation energy is smaller than that of k2 (Ea(2) = 34 kcal/mol)9, resulting in an estimated enthalpy change for the overall step (I1 ⇄ I2) that is large and positive (ΔH2o = 24 kcal/mol). Our calculation assumes that there is no activation heat capacity change for k−2(ΔCp‡(−2) = ΔEa(−2)/ΔT ~0), and thus that Ea(−2) is constant between 10 and 37 °C. This assumption is consistent with the observed lack of an activation heat capacity change for the forward rate constant k2 9, and is analogous to the argument (above) that the lack of a [urea]-dependence of k2 implies that k−2 is independent of [urea] as well. A heat capacity change in a biopolymer process, like a [urea]-dependence, is often a sign of a conformational change in which biopolymer surface is either buried from or exposed to the solvent 14. We propose that the [urea]-dependence and the heat capacity change in kd both result from the same folding transition in RNAP; the extension of this proposal is that both are contained in the same step (I2 ⇄ RPo).
Table 3.
Parameters from the analysis of the [urea] and [KCl] upshifts at 37 and 10 °C
| 37 °C | 10 °C | |
|---|---|---|
| k−2 (s−1) | 3.3 ± 0.7 | 7.2 (±0.7) × 10−1 |
| K3o a | 2.7 (±0.9) × 105 | 3.2 (±0.6) × 103 |
| dlnK3/d[urea] b | −3.3 ± 0.1 M−1 | −3.5 ± 0.1 M−1 |
| k−3o (s−1) a c | 1.1 (±0.7) × 10−2 | 3.3 (±1.0) × 10−2 |
| k3o (s−1) a d | 3.0 (±2.2) × 103 | 1.0 (±0.4) × 102 |
| dlnk−3/d[urea] c | 1.1 ± 0.2 M−1 | |
| dlnk3/d[urea] e | −2.2 ± 0.2 M−1 | −2.5 ± 0.2 M−1 |
Xo is the value of X in DB (containing 0.12 M KCl and no urea)
Determined from a fit of the linear regions of the data in Fig 3a (0–1.5 M urea at 10 °C and 0–2.5 M urea at 37 °C)
Calculated from values of K3 (= k3/k−3) and k−3 in this table
Calculated from: dlnk3/d[urea] = dlnK3/d[urea] + dlnk−3/d[urea]
Interpretation of kd at low perturbant concentrations: The [perturbant]-dependence of the rate of dissociation is determined by the [perturbant]-dependence of RPo ⇄ I2
As seen in Fig 3, kd increases dramatically with increasing [perturbant] at low perturbant concentrations. The logarithm of kd increases linearly with increasing [urea] (up to ~1.5 M urea at 10 °C and ~2.5 M urea at 37 °C; Figure 3a) and nonlinearly (with slight upward curvature) with ln [KCl] (up to ~0.30 M KCl at 10 °C and to ~0.48 M KCl at 37 °C; Figure 3b). These trends in kd correspond closely to the behaviors expected for the equilibrium constants for protein unfolding and for disruption of a protein-DNA interface, respectively. In studies of protein unfolding, ln Kobs is almost invariably a linear function of [urea] (giving rise to the so-called ‘m-value’), even to zero urea 29. For studies of the dissociation of positively charged ligands from DNA in the presence of both univalent salt and Mg2+, ln Kobs shows a nonlinear dependence on ln [univalent salt], with curvature resulting from the [univalent salt]-dependent association of Mg2+ with the DNA phosphate backbone 34. The trends in the data at low [perturbant] in Fig 3, coupled with the assumption that k−2 is independent of [perturbant], imply that the denominator of the expression for kd (eq 1) is completely dominated by K3 (K3 ≫ 1 + k−2/k−3). The expression for kd at low [perturbant] can therefore be simplified to eq 2b: kd = k−2/K3. Thus, the initial dependences of kd on [urea] and [KCl] are equal in magnitude to the dependences of K3 on those perturbants: dlnkd/d[urea] = −dlnK3/d[urea] and Skd (=dlnkd/dln[KCl]) = −SK3.
Fits of the linear regions of the [urea] upshift data in Fig 3a give the following values of dlnK3/d[urea]: −3.3 ± 0.2 M−1 at 37 °C and −3.5 ± 0.1 M−1 at 10 °C. These dependences agree well with that determined previously at 17 °C over a smaller range of urea concentrations (dlnkd/d[urea] (= −dlnK3/d[urea]) = 3.1 ± 0.1 M−1 from 0 to 0.6 M urea 11). Using eq 3 (Background Section), these values of dlnK3/d[urea] reveal that ~2.4 × 103 Å2 of polar amide biopolymer surface (corresponding to ~120 amino acid residues) is buried in the conversion of I2 to RPo.
I2 is unstable under typical transcription assay conditions
One implication of the values of k−2 and K3 obtained from the fits of the upshift data (Table 3) is that I2 is unstable relative to both I1 and RPo at the λPR promoter under typical assay conditions. In Dissociation Buffer, the equilibrium constant K2 for I1 ⇄ I2 is ~3 × 10−3 at 10 °C and ~0.2 at 37 °C (with K2 = k2/k−2 calculated using the values of k−2 from Table 3 and values of k2 determined previously 9). The equilibrium constant K3 for I2 ⇄ RPo is 3.2 (± 0.6) × 103 at 10 °C and 2.7 (± 0.9) × 105 at 37 °C (Table 3). Calculation of K2 and K3 between 0 and 42 °C (data not shown) shows that essentially none of the promoter DNA exists as I2 at equilibrium at any temperature, explaining previous difficulties in isolating and characterizing I2. [Notably, at 0 °C, K3 is calculated to be ~120, indicating that our previous attempt to rapidly populate I2 through means of a temperature downshift to 0 °C 35 was unsuccessful and therefore incorrectly interpreted.]
Interpretation of kd at intermediate perturbant concentrations
At moderate perturbant concentrations, K3 has decreased by enough such that it contributes less to the denominator of kd than it did at low concentrations (where it so completely dominated the denominator that dlnkd/d(ln)[perturbant] = −dlnK3/d(ln)[perturbant]), but not by so much that it is negligible compared to unity (as is the case at high [perturbant], where kd = k−2). Thus, the dependences of K3 on [perturbant] contribute progressively less to the overall dependences of kd, and these overall dependences begin to decrease in magnitude. These transition regions between the low (kd = k−2/K3) and high (kd = k−2) [perturbant] regimes are characterized by downward (negative) curvature in the trends in ln kd with [urea] (~1.5–3.5 M at 10 °C and >2.5 M at 37 °C) and with ln [KCl] (~0.30–0.80 M at 10 °C and ~0.48–0.80 M at 37 °C) (Fig 3).
The exact dependences of kd on [perturbant] in the transition regions depend on the relationship between the individual rate constants that comprise kd: k−2, k3, and k−3. There are two possible scenarios: either all three terms (1 + K3 + k−2/k−3) contribute to the denominator of kd (eq 1), or only two terms (1 + K3) contribute to the denominator of kd (eq 2a). These scenarios are considered below for the [urea] and [KCl] upshifts.
i) Intermediate urea concentrations: Evidence that an additional kinetically significant intermediate (I3) may exist between I2 and RPo
We initially attempted fits of ln kd versus [urea] (Fig 3a) to eq 6 (Methods), in which we assume that only the expression 1+ K3 (and not k−2/k−3) contributes to the denominator of kd throughout the entire range of urea concentrations studied (using values of k−2, K3, and dlnK3/d[urea] in Table 3 for the fits). It is visually apparent that these fits, shown as dashed lines in Fig 3a, are not optimal. While the fits are good at low and high [urea], the fitted curves lie systematically and significantly above the data points at intermediate [urea] (i.e. kd approaches the plateau values of k−2 at high [urea] more slowly than predicted by the fits). While this discrepancy exists for both the 10 and 37 °C data sets, it is much more pronounced at 37 °C.
One possible reason for this discrepancy is that the k−2/k−3 term contributes significantly to kd in this range of urea concentrations. To test this possibility, the data in Figure 3a were refit to eq 5 (Methods), in which the k−2/k−3 term is included. The fits to eq 5, shown as solid lines, clearly agree with the experimental data at intermediate urea concentrations better than the fits to eq 6. Values of k−3o (the value in Dissociation Buffer in the absence of urea) and dlnk−3/d[urea] for 10 and 37 °C determined from these fits are given in Table 3.
One interesting feature of these fits is that the resultant value of k−3o at 10 °C (3.3 (± 1.0) × 10−2 s−1) is larger than the value at 37 °C (1.1 (± 0.7) × 10−2 s−1). This difference results from the fact that the discrepancy between the data and the fit to eq 6 for the 37 °C data set is larger than that for the 10 °C data set; thus, the 37 °C data set requires a larger value of k−2/k−3 in the denominator of the expression for kd to correct for the discrepancy. The resulting negative activation energy for k−3 (Ea (−3) ~ −7 kcal/mol, based on a two-point fit) implies that, in the context of this analysis, k−3 is not an elementary rate constant. If k−3 were in fact non-elementary, it would contain one or more additional equilibrium steps, resulting in the following minimal mechanism:
| (Mechanism V) |
where k3 ≫ k−2 (rapid equilibrium in I2 ⇄ I3) and (rapid equilibrium in I3 ⇄ RPo). The quantity k−3 from Mechanism I (RPo → I2) would be a composite rate constant containing , k4, and k−4.
From the fits of the data to eq 5, the [urea]-dependence of I2 → RPo (dlnk3/d[urea] = −2.2 ± 0.2 M−1 at 37 °C) is larger in magnitude than that of the reverse process RPo → I2 (dlnk−3/d[urea] = 1.1 ± 0.2 M−1). While the [urea]-dependence of RPo → I2 (k−3) could conceivably be distributed between I3 → I2 (k−3*) and I3 ⇄ RPo (K4 = k4/k−4) in the context of Mechanism V, we assume that the [urea]-dependence of k−3 is wholly contained in k−3* for the following reason. The ratio of the calculated values of dlnk3/d[urea] and dlnk−3/d[urea] places roughly 70% of the overall [urea]-dependence of I2⇄ RPo in k3; this ratio is typical of the two-state folding of a globular protein, for which the forward rate constant (kfold) generally contains ~70% of the overall [urea] dependence, with the back rate constant (kunfold) providing the remaining ~30% 31. Since the forward elementary rate constant k3 contains 70% of the overall [urea]-dependence, we surmise that the corresponding back direction elementary rate constant k−3* contains the remainder of the [urea]-dependence. The extension of this assumption is that the folding transition in RNAP implied by the [urea]-dependence is wholly contained within .
ii) Intermediate KCl concentrations
For the [KCl] upshift experiments, we find that eq 6 adequately models the dependence of ln kd on ln [KCl] throughout the range of KCl concentrations studied. For the fits of the data to eq 6, shown as solid lines in Fig 3b, we used the values of k−2 and K3o in Dissociation Buffer at 37 and 10 °C determined from the fits of the [urea] upshift data (Table 3). As detailed in the Methods Section, the best fits to the data necessitated the inclusion of a small temperature dependence of the equilibrium constant for the interaction of Mg2+ with the DNA phosphate backbone.
Fits of the [KCl] upshift data (Fig 3b) to eq 5 (which includes the k−2/k−3 term in the expression for kd; eq 1) did not improve the quality of the fit (not shown), suggesting that the quantity k−2/k−3 does not significantly contribute to kd at any KCl concentration. Use of eq 6 is consistent with the fact that the large [salt]-dependence of I2 ⇄ RPo (K3 = k3/k−3) likely stems from the formation of a new interface between RNAP and DNA. In general, for the formation of a protein-DNA interface, the dissociation-direction rate constant (the breaking of the interface, concurrent with the re-association of salt cations with the DNA phosphate backbone) is expected to be much more salt dependent (by roughly 6-fold 36) than the forward-direction rate constant (in our case making Sk−3 ≈ 6Sk3). Thus, k−2/k−3 never becomes significant compared to K3 while K3 still measurably contributes to kd because K3 (= k3/k−3) is much greater than k−2/k−3 at low [KCl] and both terms decrease with similar [KCl]-dependences (Skd ≈ Sk−3). This is demonstrated in Figure 4, which shows the values of K3 and k−2/k−3 predicted by the parameters determined from our fits throughout the range of salt concentrations studied. In contrast to the [KCl] upshifts, the k−2/k−3 term does become significant in our analysis of the [urea] upshifts because most of the [urea]-dependence of K3 is contained in k3 (~70%). Thus, while K3 is much larger than k−2/k−3 at low [urea], and though both quantities decrease with increasing [urea], the [urea]-dependence of K3 is much larger than that of k−2/k−3, and the two terms become comparable at an intermediate urea concentration (Figure 5).
Figure 4.

Predicted values of the terms in the denominator of the general expression for kd (= k−2/(1 + K3 + k−2/k−3); eq 1) as functions of ln [KCl] at 37 °C (a) and 10 °C (b). k−2/k−3 is shown as a dashed line, K3 (= k3/k−3) is shown as a solid line, and unity is shown as a horizontal dotted line. Values of K3 were calculated throughout the range of [KCl] shown from the values of K3o in DB (Table 3) and eq 9–eq 11 in the text. Values of k−3 used to calculate k−2/k−3 were calculated from values of k−3o (Table 3) and eq 9–eq 11 in the text (with K3 in the equations replaced by k−3). The value of Sk−3 −Mg used in eq 9 for calculating k−3 was 7.9 (assuming that Sk−3 is ~(6/7)SK3; see Analysis Section). Values of k−2 used to calculate k−2/k−3 were calculated from the plateau values of kd in Figure 3b (Table 3).
Figure 5.

Values of the terms in the denominator of the general expression for kd (= k−2/(1 + K3 + k−2/k−3); eq 1) as functions of [urea] at 37 °C (a) and 10 °C (b). k−2/k−3 is shown as a dashed line, K3 (= k3/k−3) is shown as a solid line, and unity is shown as a horizontal dotted line. Values of K3 were calculated throughout the range of [urea] shown from the values of K3o and dlnK3/d[urea] (Table 3) and eq 7 in the text. Values of k−3 used to calculate k−2/k−3 were calculated from values of k−3o and dlnk−3/d[urea] (Table 3) and eq 8 in the text. Values of k−2 used to calculate k−2/k−3 were calculated from the plateau values of kd in Figure 3a (Table 3).
Although it is likely that the [salt]-dependence of the composite rate constant for RPo → I2 is much larger than that for I2 → RPo, the individual contributions of I2 ⇄ I3 and I3 ⇄ RPo in Mechanism V to the overall [salt]-dependence of I2 ⇄ RPo cannot be determined from our data. Since the [salt]-dependence of kd is assumed to result from the formation of a new RNAP-DNA interface, which is, in turn, likely coupled to the folding of a region of RNAP implied by the [urea]-dependence, we would expect most, if not all, of the [salt]-dependence of kd to reside in the conversion of I3 to I2.
DISCUSSION
The large [urea]- and [salt]-dependences of are consistent with the proposed large-scale folding transition late in open complex formation to form a new RNAP-DNA interface
We previously interpreted the large increase in the rate of dissociation of RNAP-λPR open complexes with increasing [urea] as reflecting the large-scale burial of polar amide surface (corresponding to the folding of ~120 amino acid residues) in the conversion of the transition state (I1-I2)‡ into RPo 11. We proposed that the major folding process in which this surface is buried is the transition of disordered regions in the C-terminus of the β’ subunit, including parts of the downstream jaw of RNAP, to an ordered state, and that this transition occurs in I2 ⇄ RPo (K3 in Mechanism I) 11. (Over 100 conserved residues in this region of the C-terminus of β’ are predicted to be intrinsically disordered in free RNAP by the computer algorithm PONDR (Predictor of Naturally Disordered Regions 37; 38).) The present study corroborates this large [urea] effect and provides strong evidence (see Analysis Section) that the folding transition does in fact occur in the conversion of I2 to RPo. Our deduction that the equilibrium constant K3 for I2 ⇄ RPo is also strongly [salt]-dependent implies that a new RNAP-DNA interface is formed in the step. Located at the downstream end of the active site channel, the downstream jaw appears ideally positioned to fold onto the downstream DNA in RPo formation, an interaction that could be the origin of the large [salt]-dependence of K3.
The lack of significant [urea] and [salt] effects on indicate no change in the exposure of polar amide surface to the solvent and no net release/uptake of salt ions in this bottleneck step
We previously reported that the rate constant k2 for I1 → I2 is independent of urea concentration 11. Based on the analysis of our current results described above, we deduce that the rate constant k−2 for I2 → I1 and thus the equilibrium constant K2 (= k2/k−2) for I1 ⇄ I2 are also independent of urea concentration. The lack of a measurable effect of [urea] on K2 suggests that there is no significant net change in the amount of polar amide biopolymer surface exposed to the solvent, such as would result from a folding/unfolding transition in a region of RNAP, in I1 ⇄ I2. We also deduce that k−2 is independent of salt concentration. In a separate study, we find that k2 is only slightly affected by salt concentration (dlnk2/dln[KCl] = Sk2 ~ −1 in the absence of Mg2+) (Kontur et al. in prep). Thus, K2 has only a slight dependence on salt concentration (SK2 ~−1), revealing that no significant net uptake or release of ions occurs in I1 ⇄ I2, such as would result from the burial/exposure of DNA phosphates and cationic groups on RNAP in the formation/disruption of an RNAP-DNA interface. The lack of significant [urea] or [salt] effects on K2 is surprising, as the interconversion of I1 and I2 is the rate-limiting bottleneck step in both the formation and dissociation of open complexes and would therefore be expected to involve large-scale conformational changes in RNAP and/or DNA. These findings lead us to propose that the major conformational change in I1 ⇄ I2 may occur within the active site channel of RNAP, largely shielded from the solution (and thus solute-inaccessible). This proposal is consistent with DNA backbone footprinting experiments 3; 17, which reveal that both strands of the DNA are protected from cleavage from the −10 hexamer to ~+15 in both I1 and RPo.
The strongly endothermic steps in the conversion of I1 to RPo may signify DNA opening
At λPR, DNA opening occurs at some point or points in the steps I1 ⇄ I2 ⇄ RPo 3; 17. DNA melting is a highly endothermic process (ΔHoobs = ~5 kcal/(mol base pair) for converting a duplex to partially stacked single strands at 20 °C 39). Thus, the step(s) in Mechanism I in which melting occurs is (are) expected to be characterized by a large positive enthalpy change. Our previous and current results suggest that the latter two steps of Mechanism I, I1 ⇄ I2 and I2 ⇄ RPo, are both accompanied by large positive enthalpy changes. [ΔHo(2) = 24 kcal/mol, based on the activation energy of k2 9 and a two-point estimate of the activation energy of k−2; see Analysis Section. ΔH3o for I2 ⇄ RPo may exceed ~45 kcal/mol at low temperatures; see below.] Is DNA opening distributed to some extent between I1 ⇄ I2 and I2 ⇄ RPo?
Indirect experimental evidence suggests that local DNA melting occurs in discrete steps for the Bacillus subtilis RNAP 40; 41, as well as for mutant 42; 43 and wild type 21; 44; 45 E. coli RNAP. However, the mechanism of DNA opening and the precise temporal sequence of opening events have not been established for any multi-subunit RNAP at any promoter. We propose that DNA opening by E. coli RNAP at the λPR promoter may be distributed between I1 ⇄ I2 and I2 ⇄ RPo. The large activation energy and slow kinetics of I1 → I2 are consistent with the initiation of DNA opening in the −10 region, and the large positive enthalpy change of I2 ⇄ RPo may reflect further opening downstream to +3. We are currently developing [KCl] upshift experiments in conjunction with MnO4− footprinting reactions to test this prediction.
Evidence for an additional step in the mechanism of open complex formation
As detailed in the Analysis Section (and demonstrated in Fig 3a), the dependence of kd on [urea] between ~1.5 and 3.5 M urea at 10 °C and above ~2.5 M urea at 37 °C provides evidence for the possible existence of an additional kinetically significant intermediate (I3) late in the mechanism of open complex formation:
| (Mechanism V) |
In the context of this mechanism, the folding transition in RNAP and the formation of a new RNAP-DNA interface in I2 ⇄ RPo likely occurs in I2 ⇄ I3 and not in I3 ⇄ RPo (see Analysis Section).
The conversion of I2 into RPo is characterized by a large positive enthalpy change, but we cannot conclusively divide the thermodynamics of this step between the formation of I3 and its conversion to RPo. The activation energy of the composite rate constant k−3 for RPo → I2 (Eact (−3)) is ~−7 kcal/mol (based on a two-point determination using the values of k−3 at 10 and 37 °C from Table 3). Because of this negative activation energy, the conversion of I3 into RPo (K4 = k4/k−4) must be highly endothermic, although we lack sufficient information (such as the activation energy for the elementary rate constant k−3* (I3 → I2)) to conclusively determine the thermodynamics of K3* (= k3/k−3* for I2 ⇄ I3).
An analysis of the thermodynamics of folding for various proteins indicates that the value of TH (the temperature at which ΔHo = 0) is typically low (0–10 °C) (R. Saecker, unpublished data). We previously found that kd is characterized by a large negative activation energy at low temperatures (Ea(d) = ~−35 kcal/mol at 7 °C 13 and ~−30 kcal/mol between 10 and 15 °C 8), which implies a large positive enthalpy change for the conversion of I2 to RPo at low temperatures (ΔHo(3) = ~45 kcal/mol at 7 °C, calculated from Ea (d) and Ea (−2) (Analysis Section)). If the TH of the folding step in open complex formation is near 7 °C (by analogy to the TH values for protein folding), then this folding step (predicted to be part of I2 ⇄ I3) would not contribute significantly to this large enthalpy change. Thus, the majority of the large enthalpy change in I2 ⇄ RPo is likely in I3 ⇄ RPo and not in I2 ⇄ I3. In this scenario, if the enthalpy changes do reflect DNA opening, the two steps in which opening occurs are I1 ⇄ I2 and I3 ⇄ RPo, separated by the folding of a region of RNAP to form a new interface with the promoter DNA in I2 ⇄ I3:
| (Mechanism VI) |
We are currently testing this proposed mechanism with RNAP and DNA variants and with MnO4− footprinting experiments following upshift to high concentrations of KCl.
MATERIALS AND METHODS
Buffers
Storage Buffer for RNAP holoenzyme contained 50% glycerol (v/v), 10 mM Tris-HCl (pH 7.5 at 4 °C), 100 mM NaCl, 0.1 mM DTT, and 0.1 mM Na2EDTA. Dissociation Buffer (DB) contained 10 mM (10.7 mm (millimolal)) MgCl2, 41 mM (44 mm) Tris-HCl buffer (pH 8.0 at temperature of experiment), 884 mM (948 mm) glycerol, 1 mM (1mm) DTT, 100 µg/mL BSA, 13 mM (13.9 mm) NaCl, at least 120 mM (129 mm) KCl, and the final desired dissociation concentration of urea or additional KCl. In [urea] upshift experiments, concentrations of all species were held constant on the molal scale. In [KCl] upshift experiments, concentrations of all species were held constant on the molar scale. Wash Buffer contained 0.1 M NaCl, 10 mM Tris-HCl (pH 8.0 at room temperature), and 0.1 mM Na2EDTA.
Wild-type Eσ70 RNA polymerase holoenzyme
E. coli K12 wild type RNA polymerase holoenzyme was purified as described 46 and stored in storage buffer in 500 µL samples at −70 °C. All RNAP concentrations reported here refer to active concentrations, determined as described 6. Individual samples of RNAP used were 45–60% active.
λPR promoter DNA
A DNA fragment containing the λPR promoter was obtained from the plasmid pBR81 and labeled at the 3’ end with 32P as described 47. The resulting blunt-ended fragment contains the λPR wild type sequence (from positions −60 to +20, relative to the transcription start site) centrally located in a DNA fragment extending from position −115 to +76. The specific activity of the fragment was generally ~1017 cpm/mole.
[Solute] upshift-induced dissociation kinetics
The irreversible kinetics of dissociation of RNAP-promoter DNA open complexes were measured at 10 and 37 °C using either manual mixing or rapid mixing, and nitrocellulose filter binding. Dissociation was initiated by addition of either urea or additional KCl, and the polyanionic competitor heparin.
i) Manual mixing experiments
RNAP (final concentration 6–15 nM) and DNA (final concentration 0.05–0.5 nM) were combined in DB and allowed to associate to equilibrium or completion either at the temperature at which dissociation was to occur or at room temperature. The preformed open complexes were incubated at the temperature of dissociation for at least 20 minutes before dissociation was initiated. (Longer times of incubation had no effect on the kinetics of the process.) At time t = 0, the reaction was combined (in ≤ 10 s) with an equal volume of DB containing heparin and sufficient urea or additional KCl to obtain the final concentration of perturbant for the dissociation reaction (and 100 µg/mL heparin) for a final volume of 1–1.2 mL. At given time points, 100 µL of the reaction was filtered through nitrocellulose.
ii) Rapid quench mixing experiments
RNAP (final concentration 5–30 nM) and DNA (final concentration 0.05–0.5 nM) were combined in DB and allowed to associate to completion at room temperature (30–60 min). Samples of these pre-formed open complexes in DB and of DB containing heparin (final concentration 100 µg/mL) and either urea or additional KCl were loaded into sample ports of a rapid mixer (Chemical-Quench-Flow Model RQF-3; KinTek Co., Austin, TX) where they were incubated at the final temperature of dissociation for at least five minutes. A water bath was used to regulate the temperature of the reaction loops in the apparatus (monitored by a Fluke 51K/J temperature probe). At time zero, known (approximately equal) volumes of the two samples were rapidly mixed (in less than 20 ms) in the reaction loop, resulting in final concentrations of 100 µg/mL heparin and the reported dissociation concentrations of urea or KCl. The solutions used to push the two reactant solutions together matched the reactant solutions in composition. At time t, the reaction was rapidly combined with ‘quench solution’ (a buffered low [KCl] solution), effectively stopping the dissociation reaction by diluting perturbant concentrations to 0.08–0.12 M KCl and <1.5 M urea at room temperature. The quenched sample was collected and filtered through nitrocellulose at room temperature.
Nitrocellulose filter binding assays
Nitrocellulose filter binding assays were performed as described 11. As nitrocellulose retains RNAP but not dsDNA, the only radioactive DNA remaining on the nitrocellulose after filtering and rinsing with Wash Buffer is that still complexed with RNAP. For manual mixing reactions, the total counts per minute filtered (cpmTOT, generally ~1000–3500 cpm) was determined by spotting 20 µl from the reaction mixture onto a dried nitrocellulose filter. For rapid mixing reactions, cpmTOT was determined by performing a reaction and applying the entire expelled sample to three dried nitrocellulose filters. Background retention of radiolabeled DNA on filters (cpmbkgd) was determined by filtering an aliquot of the reaction mixture lacking RNAP. Filter efficiency (FE; the fraction of label retained on a filter under conditions where all promoter DNA in solution is complexed as open complexes) for a given perturbant concentration was determined by dividing the extrapolated intercept from a reaction performed at 37 °C by cpmTOT from the reaction. Filter efficiencies were generally ~0.70–0.95, and were not found to be significantly affected by perturbant up to 0.24 M KCl and 1.5 M urea. (All higher concentrations of perturbant were diluted to lower perturbant concentrations before filtering). The observed fraction of promoter DNA in the form of open complexes at a given time point (θobs) was determined by dividing the counts per minute (cpmt = cpmobs − cpmbkgd) by the total counts per minute, cpmTOT. θobs was corrected for filter efficiency to determine the fraction of promoter DNA capable of binding to RNAP in the form of open complexes, .
DATA ANALYSIS
Fitting of dissociation data to single-exponential decay
The observed rate constant (kd) for the irreversible dissociation of open complexes was determined by fitting θt versus time for a given perturbant concentration to a single-exponential decay equation:
| (4) |
where is the value of θt at time t = 0
Dependences of ln kd on [urea] and on ln [KCl]
Expressions for the dependence of ln kd on [perturbant] are as follow (depending on whether k−2/k−3 is significant compared to K3; see eq 1 and eq 2):
| (5) |
| (6) |
where both K3 and k−3 are functions of KCl and urea concentration.
The expressions for K3 and k−3 as functions of [urea] in eq 5 and eq 6 are (assuming that ln K3 and ln k−3 are both linearly dependent on [urea]):
| (7) |
| (8) |
where K3o and k−3o are the values of K3 and k−3 in DB in the absence of urea.
K3 was determined as a function of [KCl] according to:
| (9) |
where:
| (10) |
is the equilibrium constant for the association of Mg2+ with the DNA phosphate backbone. The best fits of the data at 10 and 37 °C necessitated using different expressions for as a function of [KCl], implying a temperature dependence of at a given KCl concentration:
| (11a) |
| (11b) |
Acknowledgments
This research was supported by NIH GM23467. WSK acknowledges support from NIH 5 T32 GM08349. The authors would like to thank Oleg Tsodikov for helpful early discussions regarding analysis of the data. We thank the reviewer and editor for their careful reading of the manuscript and helpful suggestions.
Abbreviations used
- RNAP
RNA polymerase
- SKobs = dlnκobs/dln[monovalent salt]
where κobs is a rate or equilibrium constant
Footnotes
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