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Tertiary structure of apolipoprotein A-I in nascent high-density lipoproteins.


ABSTRACT: Understanding the function of high-density lipoprotein (HDL) requires detailed knowledge of the structure of its primary protein, apolipoprotein A-I (APOA1). However, APOA1 flexibility and HDL heterogeneity have confounded decades of efforts to determine high-resolution structures and consistent models. Here, molecular dynamics simulations totaling 30 ?s on two nascent HDLs, each with 2 APOA1 and either 160 phospholipids and 24 cholesterols or 200 phospholipids and 20 cholesterols, show that residues 1-21 of the N-terminal domains of APOA1 interact via strong salt bridges. Residues 26-43 of one APOA1 in the smaller particle form a hinge on the disc edge, which displaces the C-terminal domain of the other APOA1 to the phospholipid surface. The proposed structures are supported by chemical cross-linking, Rosetta modeling of the N-terminal domain, and analysis of the lipid-free ?185APOA1 crystal structure. These structures provide a framework for understanding HDL maturation and revise all previous models of nascent HDL.

SUBMITTER: Pourmousa M 

PROVIDER: S-EPMC5960303 | biostudies-literature | 2018 May

REPOSITORIES: biostudies-literature

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Tertiary structure of apolipoprotein A-I in nascent high-density lipoproteins.

Pourmousa Mohsen M   Song Hyun D HD   He Yi Y   Heinecke Jay W JW   Segrest Jere P JP   Pastor Richard W RW  

Proceedings of the National Academy of Sciences of the United States of America 20180430 20


Understanding the function of high-density lipoprotein (HDL) requires detailed knowledge of the structure of its primary protein, apolipoprotein A-I (APOA1). However, APOA1 flexibility and HDL heterogeneity have confounded decades of efforts to determine high-resolution structures and consistent models. Here, molecular dynamics simulations totaling 30 μs on two nascent HDLs, each with 2 APOA1 and either 160 phospholipids and 24 cholesterols or 200 phospholipids and 20 cholesterols, show that res  ...[more]

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2014-02-27 | GSE53314 | GEO