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Thermal denaturation of nucleosomal core particles
Nucleic Acids Research
|January 1, 1978
Summary
Chicken erythrocyte chromatin core particles exhibit biphasic thermal denaturation, indicating distinct DNA and histone structural changes. Increased ionic strength simplifies melting curves, suggesting stabilization of the histone-DNA complex.
Area of Science:
- Biochemistry
- Molecular Biology
- Structural Biology
Background:
- Core particles are fundamental units of chromatin, composed of DNA and histone proteins.
- Understanding their thermal stability is crucial for elucidating DNA packaging and accessibility within the nucleus.
Purpose of the Study:
- To investigate the thermal denaturation process of chicken erythrocyte chromatin core particles.
- To characterize the distinct contributions of DNA and histone structures to thermal stability.
Main Methods:
- Differential scanning calorimetry (DSC) to measure heat capacity changes.
- UV-Vis spectroscopy to monitor base unstacking via absorbance changes.
- Circular dichroism (CD) spectroscopy to assess DNA and histone secondary structure alterations.
Main Results:
- Thermal denaturation of core particles occurred in two phases, with inflexions at 60°C and 74°C, distinct from isolated DNA denaturation at 44°C.
- CD spectroscopy revealed biphasic changes in DNA secondary structure preceding base unstacking.
- Histone secondary structure alterations were observed only in the second denaturation phase (melting at 71°C).
- Increasing ionic strength from 1 mM to 10 mM resulted in nearly monophasic melting curves without inducing conformational changes at room temperature.
Conclusions:
- The biphasic melting of core particles suggests sequential denaturation events: initial DNA denaturation followed by histone-DNA complex breakdown.
- The findings highlight the cooperative nature of histone-DNA interactions in maintaining chromatin structure.
- Ionic strength plays a significant role in stabilizing the core particle structure.