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Pericardial-fluid complement: normal values

Insights

Normal pericardial fluid complement levels are established for accurate diagnosis. Storing samples at -70°C is crucial, as lower temperatures significantly reduce complement levels, impacting interpretation of immunologic diseases.

Area of Science:

  • Immunology
  • Rheumatology
  • Clinical Chemistry

Background:

  • Pericardial fluid complement levels in systemic lupus erythematosus and rheumatoid arthritis are difficult to interpret due to limited data in healthy individuals.
  • Establishing normal complement concentrations is essential for accurate diagnosis and understanding of pericardial diseases.

Purpose of the Study:

  • To determine normal ranges for pericardial fluid complement components (C3, C4, and total hemolytic complement) under standardized conditions.
  • To assess the impact of sample storage temperature on complement levels.

Main Methods:

  • Standardized collection, storage, and assay methods were employed.
  • Pericardial fluid samples were analyzed for C3, C4, and total hemolytic complement (CH50).
  • The effect of storage at -20°C versus -70°C on complement levels was evaluated.

Main Results:

  • Normal ranges were established: C3 (35-127 mg/dl), C4 (6.3-23 mg/dl), and total hemolytic complement (1.9-9.1 CH50 units).
  • Storage at -20°C caused a 50% reduction in complement values compared to optimal storage.
  • Optimal storage at -70°C is recommended to preserve complement integrity.

Conclusions:

  • Normal pericardial fluid complement levels are relatively low.
  • Caution is advised when interpreting reduced complement levels in pericardial fluid, especially if storage conditions are suboptimal.
  • Accurate reference ranges and proper sample handling are critical for diagnosing immunologic conditions affecting the pericardium.

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