Contribution of the C-terminal region to the thermostability of the archaeal group II chaperonin from Thermococcus sp. strain KS-1
Contribution of the C-terminal region to the thermostability of the archaeal group II chaperonin from Thermococcus sp. strain KS-1
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DOI:
10.1007/s00792-006-0519-y
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发表时间:
2006-05
期刊:
影响因子:
2.9
通讯作者:
Takao Yoshida;Taro Kanzaki;R. Iizuka;Toshihiro Komada;T. Zako;R. Suzuki;T. Maruyama;M. Yohda
中科院分区:
文献类型:
--
作者:
Takao Yoshida;Taro Kanzaki;R. Iizuka;Toshihiro Komada;T. Zako;R. Suzuki;T. Maruyama;M. Yohda
Chaperonin is a double ring-shaped oligomeric protein complex, which captures a protein in the folding intermediate state and assists its folding in an ATP-dependent manner. The chaperonin from a hyperthermophilic archaeum,Thermococcussp. strain KS-1, is a group II chaperonin and is composed of two distinct subunits, α and β. Although these subunits are highly homologous in sequence, the homo-oligomer of the β-subunit is more thermostable than that of the α-subunit. To identify the region responsible for this difference in thermostability, we constructed domain-exchange mutants. The mutants containing the equatorial domain of the β-subunit were more resistant to thermal dissociation than the mutants with that of the α-subunit. Thermostability of a β-subunit mutant whoseC-terminal 22 residues were replaced with those of the α-subunit decreased to the comparable level of that of the α-subunit homo-oligomer. These results indicate that the difference in thermostability between α- and β-subunits mainly originates in theC-terminal residues in the equatorial domain, only where they exhibit substantial sequence difference.