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Proc Natl Acad Sci U S A. 2005 January 11; 102(2): 285–290.
Published online 2004 December 30. doi: 10.1073/pnas.0405779102.
PMCID: PMC544287
Biochemistry
The effects of upstream DNA on open complex formation by Escherichia coli RNA polymerase
Caroline A. Davis,* Michael W. Capp, M. Thomas Record, Jr,* and Ruth M. Saecker
Departments of *Biochemistry and Chemistry, University of Wisconsin, Madison, WI 53706
To whom correspondence should be addressed. E-mail: rmsaecker/at/wisc.edu.
Edited by E. Peter Geiduschek, University of California at San Diego, La Jolla, CA
Received August 6, 2004; Accepted November 16, 2004.
Binding of activators to upstream DNA sequences regulates transcription initiation by affecting the stability of the initial RNA polymerase (RNAP)–promoter complex and/or the rate of subsequent conformational changes required to form the open complex (RPO). Here we observe that the presence of nonspecific upstream DNA profoundly affects an early step in formation of the transcription bubble. Kinetic studies with the λPR promoter and Escherichia coli RNAP reveal that the presence of DNA upstream of base pair -47 greatly increases the rate of forming RPO, without significantly affecting its rate of dissociation. We find that this increase is largely due to an acceleration of the rate-limiting step (isomerization) in RPO formation, a step that occurs after polymerase binds. Footprinting experiments reveal striking structural differences downstream of the transcription start site (+1) in the first kinetically significant intermediate when upstream DNA is present. On the template strand, the DNase I downstream boundary of this early intermediate is +20 when upstream DNA is present but is shortened by approximately two helical turns when upstream DNA beyond -47 is removed. KMnO4 footprinting reveals an identical initiation bubble (-11 to +2), but unusual reactivity of template strand upstream cytosines (-12, -14, and -15) on the truncated promoter. Based on this work, we propose that early wrapping interactions between upstream DNA and the polymerase exterior strongly affect the events that control entry and subsequent unwinding of the DNA start site in the jaws of polymerase.
Early steps in transcription initiation require interactions with DNA sequences located upstream from the start site (+1). In eukaryotes, assembly of the RNA polymerase (RNAP) II preinitiation complex hinges on the recruitment of the TATA-binding protein to sequences typically located ≈25 bp upstream from +1 (see, for example, ref. 1). In Escherichia coli, the specificity factor σ70 brings the polymerase machinery to a promoter via interactions with the so-called -35/-10 elements (2, 3). The rates and equilibria of steps involved in binding and opening the DNA are further modulated by proteins (activators, enhancers, and repressors) that bind to sites located even further upstream (1, 4). Strikingly, high-resolution structures of bacterial RNAP and yeast RNAP II reveal a conserved architecture that dictates that upstream interactions cannot place downstream DNA directly in the cleft containing the active site (57). Instead, significant DNA deformations must occur to access the cleft. Additionally, the width of the cleft fundamentally determines whether single- or double-stranded DNA can enter. How do interactions with upstream DNA sequences influence these critical steps or other conformational changes that occur in forming the open complex?
A paradigmatic example of the role of upstream DNA sequences in regulating transcription is found in the lysis/lysogeny decision of λ phage after infection of E. coli (8). DNA sequences separating two divergent phage promoters (λPR and λPRM) contain three sites for the phage protein λcI. In a precise balance between λcI concentration, site affinity, and position, transcription is repressed from λPR and activated at λPRM (911). λcI activates λPRM by facilitating the rate-limiting conformational change (isomerization) in open complex formation, a step that occurs after polymerase binds (1214). λcI activation of λPRM has been hypothesized to depend critically on the formation of a correctly aligned λcI-σ interface (15, 16), recently defined by x-ray crystallography (16). How does formation of such an interface increase the rate-limiting isomerization rate constant (k2)by ≈10-fold at 37°C, with no net effect on the stability of the preceding intermediate (12, 14)? Additional puzzles are presented by activation of a polymerase containing a mutant σ70 by WT λcI, which increases the stability of the first intermediate by ≈10-fold, with only a 2-fold increase in k2 (13). Intriguingly, modeling indicates that the transition from a nonproductive to a productive interface may alter the path of the DNA upstream of λcI (approximately -50) (16).
These data, along with other studies, suggest to us that the trajectory of upstream DNA is defined in the earliest steps of open complex formation, and that this trajectory and the resulting interactions between upstream DNA and polymerase dictate subsequent downstream events. For E. coli RNAP, interactions between σ70 and the -35 element likely set the initial trajectory; binding to the -35 consensus sequence by the homologous σ from Thermus aquaticus changes the DNA helical axis by 36 degrees (17). Changes to or reinforcements of this initial trajectory presumably occur when the C-terminal domains (CTD) of the α subunits (18) and/or proteins such as catabolite activator protein (CAP), λcI, IHF, or FIS bind upstream, bend their DNA sites (16, 1921), and as a consequence activate transcription initiation. Possibly more significantly, the phasing of these activator sites with respect to the promoter critically affects their function (2224). For example, repositioning of CAP at the gal P1 promoter by 1 bp, from a site centered at -41.5 to -40.5, converts CAP from an activator to a repressor (23). Do these experiments indicate that upstream DNA plays a direct role in activation, possibly by contacting core RNAP, or does it serve primarily as an assembly platform that mediates protein–protein interactions?
Several lines of evidence suggest that upstream DNA wraps around E. coli RNAP during initiation, even in the absence of transcription factors. In particular, hydroxyl radical footprinting studies of the open complex (RPO) formed at several promoters (λPR, lacUV5, and T7 A1) reveal a pattern of periodic protection of upstream DNA extending to approximately -70 (2527). To reconcile the length and periodicity of the RPO footprint with the dimensions of E. coli RNAP determined by electron microscopy (28), upstream DNA was proposed to wrap in a surface groove of RNAP (25, 28). A similar model of RPO at λPR was deduced from atomic force microscopy data (29). However, for RPO formed at lacUV5, only the flexibly tethered αCTDs were found to crosslink to DNA positions -43 to -93 (30). If this crosslinking pattern is general, and αCTD binding explains upstream protection in RPO (18, 2527, 3134), then it is necessary to propose rapidly reequilibrating nonspecific binding of the αCTDs to the minor groove of DNA throughout this region (30). Consistent with, but by no means a proof of, this hypothesis, deletion or mutation of the αCTDs eliminates protection from -40 to -70 in RPO (18, 27, 35, 36).
Although it is evident that interactions with upstream DNA influence formation of RPO, little quantitative data exist regarding upstream contacts in the intermediates that precede it. How do these interactions influence the individual steps that form and then convert the initial polymerase–DNA complexes into RPO? To elucidate the role of upstream DNA in open complex formation, we compared a λPR promoter truncated at position -47 [upstream truncated (UT)] with full-length (FL) λPR using kinetic and footprinting experiments.
The kinetics of formation and dissociation of RPO complexes at the λPR promoter require a minimal three-step mechanism:
Figure 1 where R is free polymerase; P is promoter DNA; I1 and I2 are the first and second kinetically significant intermediates, respectively; and RPO is the final open complex (3741). (K1 and K3 are equilibrium constants for the first and third steps, and k2 and k-2 are the forward and reverse rate constants for the rate-determining interconversions of I1 and I2). Our studies demonstrate that DNA sequences upstream of -47 do not greatly affect the stability of the first intermediate or the kinetics of dissociation of RPO at λPR. Instead, we find that they greatly accelerate the conversion of the first to the second intermediate by a factor of 35- to 60-fold. DNase I footprints reveal that the presence of upstream DNA permits downstream DNA to fully enter the active-site cleft of polymerase early in the process. These results motivate our proposal that contacts to upstream DNA sequences directly influence movements in the transcriptional machinery that place the start site in the jaws of polymerase.
Buffers. RNAP storage buffer (25), binding buffer (Table 1) (41), wash buffer (41), 90 mM Tris/64.6 mM boric acid/2.5 mM EDTA, pH 8.3 (TBE buffer) (25), urea loading buffer (25), and KMnO4 stop buffer (40) have been described. DNase I stop buffer is 200 mM EDTA and 2 M NaCl.
Table 1.
Table 1.
Kinetic quantities for RNA polymerase interactions with FL and UT λPR
RNAP. E. coli K12 RNAP holoenzyme (Eσ70) was purified by modification of the Burgess and Jendrisak procedure (42, 43) and stored at -70°C in storage buffer; working stocks were stored at -20°C. Promoter-binding activities of the RNAP preparations were determined as described (41) and ranged from 36% to 77%. Binding activities were determined in parallel with the experiments described here and did not change significantly over the course of 1 month. All RNAP concentrations reported refer to the active RNAP.
λPR Promoter DNA. The WT λPR promoter sequence from -60 to +20, centered in a FL 190-bp fragment (-110 to +80), was isolated from plasmid pBR81 and labeled on the nontemplate (nt) strand as described (25). A 191-bp FL λPR fragment (-102 to +89) was isolated from a pBR80 derivative by using XbaI and SmaI, and the upstream end of the template (t) strand was labeled with 32P-dCTP by using Sequenase DNA polymerase. The 5′ overhang was filled in with dNTPs. FL λPR used in association assays performed at 37°C was an 898-bp fragment, as described (41). We observed no difference in the kinetics of association with the 898- and 187-bp fragments (data not shown).
A UT promoter, consisting of the WT λPR sequence from -42 to +20, centered in a 136-bp fragment (-47 to +89), was isolated from plasmid pRLG936 (31) by cleavage with EcoRI and SmaI. The upstream end of the t strand was labeled with 32P-dATP. To label the downstream end of the nt strand, an UT λPR promoter fragment (-47 to +64) was generated by cutting pRLG936 with EcoRI and filling in the 5′ overhang with dNTPs. The fragment was then cut with XhoI, and the 3′ end of the nt strand was labeled with 32P-dTTP. All λPR fragments were isolated and purified as described (25).
To label the nt strand of UT λPR for KMnO4 probing, pRLG936 was cut with EcoRI. The resulting 5′ γ phosphate was removed and replaced with γ32 phosphate as described (25). Proteins were phenol-extracted, and pRLG936 was cut with SmaI. The λPR fragment was precipitated, and the upstream overhang was filled in with dNTPs. UT λPR was isolated and purified as described in ref. 25.
Association Kinetics. Nitrocellulose filter-binding assays were performed in binding buffer by manual mixing (41). RNAP concentrations ranged from 2 to 112 nM; DNA concentrations ranged from 0.2 to 0.5 nM. To test that heparin (50 μg/ml final) was a nonperturbing competitor for free RNAP, representative experiments were repeated by using 100 and 250 μg/ml heparin. Equilibrium occupancy of competitor-resistant (CR) complexes and values of kobs exhibited no dependence on heparin concentration, indicating that it is an inert competitor (data not shown).
Dissociation Kinetics. RNAP and DNA were mixed in binding buffer and incubated at 17 or 37°C until binding equilibrium was reached. At 37°C, 12 nM RNAP was used for FL and UT λPR; at 17°C, 70 nM RNAP was used with UT λPR and 12 nM RNAP with FL λPR. Irreversible dissociation was initiated by the addition of heparin (50 μg/ml final), and 100 μl of the reaction was removed and filtered at recorded time intervals (41). Heparin is not a perturbing competitor for the dissociation of CR complexes at FL (44) and UT λPR (data not shown).
Data Analysis. Observed first-order rate constants (βCR) for reversible and irreversible association to form CR complexes (RPO, I2) were determined as described (41). The irreversible association rate constant (αCR) was obtained from βCR and the equilibrium fraction of promoter DNA in the form of CR complexes (equation M1): equation M2, where equation M3 was calculated as described (41). The dependence of αCR on RNAP concentration ([R]T) is hyperbolic and αCR = k2K1[R]T/(1+K1[R]T) [(41); see Mechanism 1Figure 1]. The product k2K1 is the composite second-order association rate constant (ka). All fits were weighted by 1/σ2, where σ2 is the variance of αCR. t1/2 for isomerization is given by t1/2 = 0.693/k2. First-order dissociation rate constants (kd), where kd = k-2/(1 + K3) (41), were determined by plotting cpmcorr [counts per minute at a given time (t) corrected for background retention] as a function of time. Dissociation reactions were fit to a first-order decay equation: cpmcorr= (cpm0)e-kdt, where cpm0 is the initial (t = 0) counts per minute. All kinetic data were analyzed by using sigmaplot 2000 (Systast, Point Richmond, CA).
DNase I Footprinting. RNAP (70 nM) and promoter DNA (0.4–1 nM) were mixed and incubated at 17°C. To characterize I1, samples were incubated for 15 (FL) or 350 s (UT); RPO was characterized at 2,500 (FL) or 10,000 s (UT). At the appropriate time, heparin (50 μg/ml final) or H2O was added, and DNase I (0.3 μg/ml final) was added 10 s later; DNase I cleavage was stopped after 10 s. Samples were prepared and loaded on sequencing gels as described in ref. 25. All DNase I footprints were reproduced in three to seven independent experiments.
Fractions of DNA in CR and I1 Complexes. The fraction of promoter DNA in CR complexes (equation M4) at any given time in an association experiment at 17°C and 70 nM RNAP was determined from the integrated relaxation rate equation equation M5. At 350 s after mixing, for UT λPR, equation M6; at 15 s after mixing, for FL λPR, equation M7. The fraction of promoter DNA present as I1 complexes (θI1) was calculated from θI1 = (1 - equation M8) [K1[R]T/(1 + K1[R]T)]. At 17°C and 70 nM RNAP, θI1 = 0.68 at 350 s for UT λPR and θI1 = 0.55 at 15 s for FL λPR. Approximately 24% of total UT λPR was uncomplexed at 350 s, and 33% of total FL λPR was uncomplexed at 15 s.
KMnO4 Footprinting. RNAP (20 nM) and promoter DNA (≈8 nM) were incubated at 37°C for 30 min and at 17°C for 2,500 s (FL) or 10,000 s (UT), then challenged for 10 s with heparin (50 μg/ml) or H2O. KMnO4 (0.5–3.5 mM) was added and stopped after 10 s. KMnO4 modification reactions were followed by piperidine cleavage (40). Piperidine was removed from the samples as described (40); final samples were resuspended in 3 μl of 1 × 10 mM Tris/1 mM EDTA, pH 8.0 (TE buffer) and 4 μl of urea loading buffer and loaded onto an 8% acrylamide gel. KMnO4 footprints were reproduced in 10 independent experiments run on seven gels.
PhosphorImager Analysis. Gel images were obtained by using a Molecular Dynamics PhosphorImager and analyzed as described (25) by using imagequant Ver. 4.2 (Molecular Dynamics).
Transcription Assays. Single round transcription assays were performed by using unlabeled FL and UT λPR. RNAP (20 nM) and promoter DNA (10 nM) were mixed and, after a 30-min incubation at 37°C, 32P-UTP (50 μM), NTPs (500 μM ATP, 10 μM UTP, 100 μM GTP, and CTP) and heparin (50 μg/ml) were added simultaneously to the reaction. Reactions were stopped after 30 s with urea loading buffer and run on a 15% polyacrylamide gel.
Presence of Upstream DNA Results in Faster Kinetics of Association of RNAP at the λPR Promoter. To examine the role of upstream DNA in association at λPR, rates of forming CR complexes, assumed to be primarily RPO, at the UT and FL λPR promoters were measured at 17 and 37°C in excess polymerase ([RNAP] >> [promoter]). At both temperatures and at all RNAP concentrations, CR complexes form much more quickly at FL λPR than at UT λPR (Fig. 1Fig. 1.; Fig. 4, which is published as supporting information on the PNAS web site). In contrast to FL λPR, not all UT promoter DNA is converted to CR complexes at 17°C, even though RNAP is in vast excess over promoter DNA. Instead, the equilibrium fraction of promoters in CR complexes (equation M9) increases with increasing RNAP concentration (reversible association), such that equation M10 at the highest RNAP concentration investigated (112 nM). However, at 37°C, formation of CR complexes at UT λPR goes to completion (equation M11; irreversible association) at all RNAP concentrations investigated.
Fig. 1.
Fig. 1.
Fig. 1.
Rate of formation of RPO is increased by the presence of DNA upstream of -47. Values of the irreversible association rate constant (αCR) for the formation of CR complexes are plotted as a function of total RNAP concentration ([RNAP]T) at 17°C (more ...)
Observation of single exponential kinetics indicates that free RNAP and DNA rapidly equilibrate with a first kinetically significant intermediate (generically abbreviated I1) on the time scale of its conversion to a CR complex (45). [Because formation of I1 from reactants is a rapidly established equilibrium, the kinetics of forming I1 are not relevant for the total observed kinetics (αCR). Hence, facilitated diffusion makes no contribution to αCR.] Analysis of the irreversible rate constant αCR as a function of RNAP concentration (Fig. 1Fig. 1.) allows one to determine the overall composite association rate constant ka and to dissect it into its contributions from the binding (K1) and isomerization (k2) steps. The presence of DNA upstream of -47 increases ka significantly (≈36-fold increase at 17°C and ≈7-fold increase at 37°C; Table 1). Unexpectedly, we find that this large effect on ka results primarily from the isomerization step (Table 1). At 17°C, the presence of upstream DNA greatly reduces the time required for the isomerization of I1, from a half time of 3,000 s (UT) to 50 s (FL)! At 37°C, the half time for isomerization is reduced from 35 s for UT λPR to 1 s on FL. Equally surprising is the fact that the equilibrium constant for forming I1 (K1) increases ≈2-fold upon deletion of upstream DNA (Table 1). Similar results have been observed for a series of upstream deletions of the lacUV5 promoter (46).
Similar Kinetics of Dissociation of RNAP from UT and FL λPR. Given the large effects on the kinetics of association, we next examined whether the dissociation of CR complexes was similarly affected. Irreversible dissociation of CR complexes at UT and FL λPR was induced by the addition of heparin (50 μg/ml final), which prevents free RNAP from rebinding to the promoter. The decay kinetics of both UT and FL λPR complexes are single exponential and are significantly slower at 37°C than at 17°C (Fig. 5, which is published as supporting information on the PNAS web site). This behavior demonstrates the existence of a second kinetically significant intermediate (I2) in rapid equilibrium with RPO on the time scale of the slow step in dissociation (38, 47). Fits of these data reveal only minor differences in kd for FL and UT λPR. At 17°C, kd is slightly (1.2-fold) greater for FL than for UT λPR; at 37°C, kd is ≈2-fold greater for UT than for FL λPR (Table 1).
DNase I Footprinting of I1 at UT and FL λPR and Comparisons with RPO. Because the presence of upstream DNA dramatically affects the isomerization of I1 to I2, we asked whether the structure of I1 at FL λPR (equation M12) differs from that at UT λPR (equation M13). To address this question, DNase I footprinting was performed at 17°C at times in the association process when the principal polymerase–promoter complex is predicted to be I1. DNase I footprints of CR complexes (primarily RPO) formed at binding equilibrium were also obtained. Analyses of these footprints reveal that equation M14 is competitor-sensitive and has a continuous footprint with downstream boundaries of +20 on the t strand (Fig. 2 AFig. 2.; Fig. 6, which is published as supporting information on the PNAS web site) and ≈+25 on the nt strand (Fig. 2BFig. 2.; Fig. 7, which is published as supporting information on the PNAS web site). Both the sensitivity to heparin and the downstream boundaries of the footprint agree with previous characterizations of a equation M15 at equilibrium at 0°C (40). In sharp contrast, the downstream DNase I boundary of equation M16 extends only to +2 (t) and +7 (nt), with an isolated site of protection at +27 (nt) (Fig. 2 C and DFig. 2., respectively; Figs. 8 and 9, which are published as supporting information on the PNAS web site). In the footprints of equation M17 and equation M18, any protection observed after the 10 s heparin challenge is attributed to the small fraction of CR complexes (see Experimental Procedures) present in these experiments. No end-bound complexes were detected in these footprints. Because the structures of the first kinetic intermediates differ, we continue to designate them equation M19 and equation M20.
Fig. 2.
Fig. 2.
Fig. 2.
Differences in the downstream boundary of equation M43 versus equation M44. Representative scans of DNase I cleavage of free DNA and of equation M45 and equation M46 complexes (±heparin challenge) formed at 17°C on FL [t strand (A); nt strand (B)] or UT λPR [t strand (C); nt (more ...)
On the t strand, protection of DNA in equation M21 is continuous to position -8; partial protection is observed from positions -1 to +2. Despite the lack of strong DNase I cleavage sites between positions -7 and -2 on the free DNA, comparison of weak signals with and without RNAP from at least three independent experiments suggests that this region is not protected by RNAP. Enhancements at positions -15 (t) and -16 (t) of the UT promoter are reproducibly observed; these positions are protected in the footprint of equation M22. On the nt strand, protection of equation M23 is continuous to -4, with partial protection from +1 to +7, followed by cleavage of the backbone from +8 to +26. The DNA backbone at +27 is reproducibly protected in all footprints of equation M24. Gels run for short times to resolve bands downstream from +27 demonstrate that this isolated site of protection is not the result of an end-bound RNAP (data not shown).
In the upstream direction, DNase I protection of equation M25 extends at least to -45 (nt), essentially the end of the fragment. The protection of equation M26 extends to at least -52 (t) and -45 (nt). In equation M27, DNase I enhancements are located at positions -23 (nt) and -34 (nt); in equation M28, enhancements occur at -22 and -45 (nt). Fractional protection of the upstream (-35 to -3) and downstream (+2 to +27) regions of the equation M29 footprint is the same within error (see Figs. 6 and 7). Thus under these conditions, as well as at equilibrium at 0°C (40), DNase I footprinting detects a homogeneous population of competitor-sensitive complexes with extended downstream footprints on FL λPR.
At binding equilibrium, RPO formed on FL and UT λPR (Figs. 6–9 and Fig. 10, which is published as supporting information on the PNAS web site) have the same downstream boundaries: +20 (t) and ~+25 (nt). As reported (25), DNase I enhancements occur at -38 (t), -48 (t), and -45 (nt) in RPO formed on the FL promoter, indicative of DNA deformations (e.g., bending); no enhancements are observed at any position in RPO formed on the UT promoter. No end-bound complexes were detected on UT or FL λPR.
Differences in UT and FL RPO as Detected by KMnO4. Equilibrium complexes formed at 37°C and 17°C were next probed with KMnO4 to estimate the span of the initiation bubble and the pyrimidines (T >> C) that are solvent-accessible in RPO. For both FL and UT promoters, thymines at +1, -8, -9, and -11 (t) and at -10, -4, -3 and +2 (nt) [Fig. 3Fig. 3.; (40)] are oxidized by KMnO4 and are therefore solvent-accessible. Reactivity of the thymine at -13 (nt) is not detected at either UT or FL λPR. Surprisingly, cytosines at -12, -14, and -15 (t) in RPO on the UT λPR promoter are KMnO4 reactive at both 37°C (Fig. 3Fig. 3.) and 17°C (data not shown), whereas these positions are completely unreactive for FL λPR (Fig. 3Fig. 3.). Does this result indicate additional opening of the transcription bubble at the UT promoter? To address this, we probed the t strand of the UT promoter with DMS, which methylates single-stranded cytosines (48). In both FL and UT promoters, only cytosines at -2, -5, and -6 are reactive; positions -12, -14, and -15 (t) are not reactive (Fig. 11 and Supporting Text, which are published as supporting information on the PNAS web site) (49). The lack of dimethyl sulfate reactivity suggests that these cytosines are distorted but remain base paired or are unpaired but interact with RNAP in such a way that the N3 is protected. Although the structural details of RPO formed at FL and UT λPR appear to differ, both are competent to transcribe DNA upon addition of nucleotides (data not shown).
Fig. 3.
Fig. 3.
Fig. 3.
KMnO4 (3.5 mM) probing of solvent-accessible pyrimidines in RPO formed on UT and FL λPR promoter at 37°C. On the t strand, the KMnO4 reactivity extends to -11 at FL λPR and to -15 at UT λPR; thymines at -10, -4, -3, and (more ...)
Creation of a transcriptionally competent open complex occurs through a series of steps, whose rates and equilibria can be tuned by regulatory factors. In both prokaryotes and eukaryotes, activators often stabilize an early intermediate (e.g., I1 or its precursors) at least in part by favorable protein–protein interactions. For promoters where the rate-limiting step occurs after binding, activation by driving subsequent conformational changes provides the most direct method of accelerating open complex formation. Upstream binding of the bacterial protein CAP and the phage protein λcI alters the rate of the isomerization step in open complex formation; at 37°C, CAP binding at -41.5 increases k2 by ≈7-fold at gal P1 (23), whereas the activating effect of λcI on k2, when bound immediately upstream of the -35 hexamer, is ≈10-fold at λPRM (12, 14). Changing the αCTD-binding sites upstream of -40 from nonspecific DNA sequences to AT-rich “UP” sequences (50) also accelerates this “bottleneck” step, with effects on k2 ranging from 2- to 10-fold, depending on the temperature and promoter studied (5153). Although these effects have been quantified, the precise nature of the critical isomerization step remains unknown.
Because DNase I protection of sequences upstream of -38 suggests that both αCTDs are nonspecifically bound to regions centered at -43 (t) and -54 (t) in equation M30, we expected that deletion of DNA upstream of -47 would reduce the stability of I1. Instead, we find that deletion of this upstream DNA from FL λPR has little effect on the stability of this first kinetically significant intermediate but instead profoundly reduces the rate constant k2 for the subsequent rate-determining conformational change in open complex formation. Under the conditions studied, these effects (Table 1) are significantly larger than those reported previously for CAP or λcI (12, 14, 23) or alterations in the DNA sequence of the αCTD-binding site (5153). For the lengths studied here, the presence of upstream DNA increases the rate constant k2 for formation of CR complexes (I2 and RPO) from I1 by 60-fold at 17°C and 33-fold at 37°C.
Analogous effects are reported for kinetics of association between WT RNAP and a series of upstream DNA deletions at the lacUV5 promoter in the accompanying paper (46): upstream truncation of DNA at -63 and -42 increases K1 by 20- and 10-fold, respectively, but decreases k2 by ≈30- and 50-fold, respectively, relative to lacUV5 promoters extending to -100 and -130. However, when the αCTDs are absent, the presence of upstream DNA increases k2 by only 2.5-fold (46). These results clearly indicate that the αCTDs are necessary to observe the effect of upstream DNA. Discerning whether upstream DNA merely provides additional nonspecific αCTD-binding sites or whether the αCTDs set a trajectory required for wrapping interactions between upstream DNA and other elements of RNAPinI1 or other early complexes awaits further experiments.
When upstream DNA is present, downstream DNA is continuously protected from DNase I to +20 (t) and ≈+25 (nt) in equation M31, presumably due to a cascade of events accompanying upstream wrapping and/or αCTD–DNA interactions. When upstream DNA is removed, promoter DNA is protected only to +2 (t) and +7 (nt) in equation M32 with an isolated site of protection at +27 (nt). Therefore, downstream contacts that extend this initial protection to continuous protection to +20 (t) and +27 (nt) in RPO on UT λPR must form during or subsequent to the conversion of I1 to the (I1–I2) transition state. If such contacts are established in forming (I1–I2), we speculate that these additional events are responsible for dramatically reducing k2 on UT λPR relative to FL λPR and for concomitantly increasing the activation enthalpy [-Rdlnk2/d(1/T)] required to drive I1 to (I1–I2) from ≈34 to ≈40 kcal.
Surprisingly, even though a much smaller polymerase–promoter DNA interface is formed in equation M33, its stability (-RTlnK1) is comparable to that of the larger one formed at the FL promoter. We suggest that under these conditions, the loss of upstream and downstream contacts in equation M34 is nearly compensated for by a reduction in the energetic costs required to make these contacts (e.g., DNA distortions). One implication of this proposal is that the absence of large effects of activators on K1 should not be interpreted to mean that the activator has no effect on the structure of I1. That is, activators observed to affect only k2 may do so by altering the interface in I1, even if not detected in K1.
Similarly, differences in the structure of RPO observed by KMnO4 reactivity may offset differences in upstream interactions and cause kd to remain the same even when upstream DNA is removed. Comparison of KMnO4 and dimethyl sulfate footprints indicates the presence of DNA distortions at the upstream end of the initiation bubble [-12 to -15 (t)] on UT but not FL λPR. The DNA backbone in this region is also distorted in equation M35. Although the KMnO4 reactivity detected at these positions could result from a small population of off-pathway complexes formed on UT λPR, the lack of a similar shift in KMnO4 reactivity of the nt strand suggests that this is unlikely.
A model of equation M36 proposes that formation of a sharp kink at -11/-12 directs downstream DNA into the jaws created by the β and β′ subunits of RNAP (41), thus protecting it from DNase I cleavage to ≈+25 (40). The observation that the DNase I footprint of I1 on the UT promoter is shorter by two helical turns indicates that either the DNA is not properly placed in the jaws and/or the jaws are not in the appropriate conformation to make extensive downstream contacts. Complexes formed at low temperature at other promoters, thought to correspond to early competitor-sensitive intermediates (referred to as RPC), exhibit even shorter downstream DNase I footprints (to ≈-5) (7, 23, 26, 54). Darst and coworkers (7) inferred from these data and their structure of the bacterial RNAP bound to a 33-bp forked-junction promoter fragment (from -40 to -7) that DNA downstream of the -10 region in RPC is not yet bent into the jaws but instead passes above them. A superposition of the DNA backbone bound in the active site of DNase I [Protein Data Bank ID code file 1DNK (55)] onto the DNA bound in RPC (7) demonstrates that any position downstream of -5 can be cleaved. To explain protection extending to +2(t)/+7 (nt) in equation M37, we hypothesize that downstream DNA must be bent into the jaws, but that its disposition fundamentally differs from that in equation M38. The isolated site of protection at +27 (nt) in equation M39 may also be consistent with an altered downstream DNA trajectory or change in the position of the downstream jaw (see below).
Interestingly, the downstream DNase I boundary of equation M40 is very similar to that of the unusual open complex formed at the T7 A2 promoter DNA by a variant E. coli RNAP [+1 (t) and +8 (nt); (56)]. This variant contains a large deletion in β (Δ186–433) that essentially removes the downstream lobe of the jaw. The downstream footprint of equation M41 may also reflect an altered conformation of the downstream jaw resulting from the loss of upstream contacts. In free holoenzyme, the negatively charged N-terminal domain of σ70 (region 1.1) has been proposed to bind in this region of the jaws (57) and thereby prop them open (58, 59). Possibly the absence of upstream contacts somehow impedes the expulsion of region 1.1 from the active site cleft, a transition required to form RPO. In this scenario, which is currently being investigated, downstream DNA would be bent into the jaws in equation M42, but prevented from descending into them by σ70.
Supplementary Material
Supporting Information
Acknowledgments
We thank W. Ross and R. Gourse (University of Wisconsin, Madison) for providing pRLG936, for helpful discussions, and for sharing unpublished data. We are grateful to W. Kontur for labeling some λPR used in this study, S. Darst (The Rockefeller University, New York) for providing coordinates for the model of RPC, C. Bingman (University of Wisconsin, Madison) for valuable discussion, and the reviewers for their comments. This work was supported by National Institutes of Health Grant GM23467.
Notes
Author contributions: C.A.D., M.T.R., and R.M.S. designed research; C.A.D., M.W.C., and R.M.S. performed research; M.W.C. contributed new reagents/analytic tools; C.A.D., M.T.R., and R.M.S. analyzed data; and C.A.D., M.T.R., and R.M.S. wrote the paper
This paper was submitted directly (Track II) to the PNAS office.
Abbreviations: RNAP, RNA polymerase; RPO, open complex; UT, upstream truncated; FL, full length; CR, competitor resistant; t, template; nt, nontemplate; CTD, C-terminal domain; I, kinetically significant intermediate.
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