4.7 Article

The oxidized phospholipids linked to human apolipoprotein(a) do not derive from circulating low-density lipoproteins and are probably of cellular origin

Journal

FASEB JOURNAL
Volume 23, Issue 3, Pages 950-956

Publisher

WILEY
DOI: 10.1096/fj.08-122002

Keywords

human embryonic kidney cells; HEK 293; kringle V; monoclonal antibody T15

Funding

  1. U. S. National Institutes of Health, National Heart, Lung and Blood Institute (NIH-NLBI) [HL63200]
  2. NIH-NHLBI Cardiovascular Pathophysiology and Biochemistry [T31 HL07237]

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Lipoprotein (a) [Lp(a)], a cardiovascular risk factor, is a low-density lipoprotein (LDL) variant shown to bind to oxidized phospholipids (oxPLs); however, its binding mode and origin have not been clearly established. We isolated both LDL and Lp(a) from the plasma of a population of high-Lp(a) subjects and in each Lp(a) particle separated apolipoprotein(a) [apo(a)], from the LDL component, Lp(a(-)). These products were assayed by an ELISA using monoclonal antibody T15 with a known specificity for oxPLs. In each subject, the T15 reactivity was confined to apo(a). Moreover, the amount of oxPL bound to apo(a) was unaffected by plasma Lp(a) levels and apo(a) size polymorphism. We have previously shown that kringle V (KV) is the site of oxPL linkage in human apo(a). In this work, we expressed in human embryonic kidney cells a KV-containing recombinant that, when purified from the medium, contained oxPLs. In summary, in human plasma Lp(a), the oxPLs are located in apo(a) and not in the circulating LDLs, suggesting a cellular origin. This latter concept is supported by the studies in which an expressed KV-containing apo(a) microdomain exhibited oxPL reactivity. Thus, apo(a) can undergo potentially pathogenic posttranslational modifications in a cellular environment able to generate oxPL.-Edelstein, C., Philips, B., Pfaffinger, D., Scanu, A. M. The oxidized phospholipids linked to human apolipoprotein(a) do not derive from circulating low-density lipoproteins and are probably of cellular origin. FASEB J. 23, 950-956 (2009)

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