Iron occupies an unusual position in longevity nutrition: both deficiency and excess are detrimental, and the optimal range is narrower than most people realize. Iron deficiency anemia is the most common nutritional deficiency worldwide. But iron accumulation with aging — driven by dietary iron absorption continuing while iron losses decline — contributes to oxidative stress, cardiovascular disease, and neurodegeneration through mechanisms that are increasingly well-understood.
Iron's central role in oxygen transport (hemoglobin), energy production (cytochromes in the electron transport chain), and enzymatic catalysis (iron-sulfur cluster proteins, ribonucleotide reductase) makes it absolutely essential for life. Its redox chemistry — the ease with which it cycles between Fe2+ and Fe3+ states via the Fenton reaction — makes it uniquely capable of generating hydroxyl radicals from hydrogen peroxide. This double-edged biochemistry means that iron homeostasis is tightly regulated in healthy physiology — and that disruption of this regulation in either direction produces significant biological consequences.1
Iron homeostasis in humans is regulated primarily by hepcidin — a peptide hormone produced by the liver that regulates intestinal iron absorption and macrophage iron recycling. When iron stores are adequate, hepcidin expression is high, suppressing the ferroportin transporter that exports iron from intestinal enterocytes and macrophages into circulation. When iron stores are low (or when erythropoiesis is upregulated), hepcidin falls, increasing iron absorption and recycling. This elegant feedback system maintains iron homeostasis across a wide range of dietary iron exposure — but it is imperfect, particularly under conditions of chronic inflammation (which elevates hepcidin and causes anemia of chronic disease) or in genetic disorders affecting hepcidin or ferroportin regulation.2
A critical feature of human iron biology: there is no regulated iron excretion pathway. Iron leaves the body only through blood loss (menstruation, donation, bleeding), skin cell shedding, and very small amounts in bile and urine. This means that dietary iron absorption must be precisely matched to losses — and that any imbalance that persists for years to decades produces progressive iron accumulation or iron depletion.
Serum ferritin — the primary indicator of body iron stores — rises progressively with age in both men and women in population surveys. In men, ferritin rises continuously from young adulthood onward. In women, ferritin rises sharply after menopause when menstrual iron losses cease. By age 70 to 80, many adults have ferritin levels substantially above the young adult range. This age-related iron accumulation, driven by continued dietary iron absorption against declining iron losses, may contribute to the oxidative stress and mitochondrial dysfunction of aging via excess Fenton chemistry in tissues.3
The epidemiological evidence linking higher ferritin (within the normal range) to adverse outcomes is growing: elevated ferritin is associated with higher rates of type 2 diabetes, metabolic syndrome, cardiovascular disease, and all-cause mortality in large cohort studies, particularly in men. The relationship is dose-dependent and appears to extend below the standard "high" ferritin threshold.
Hereditary hemochromatosis (HH) — caused primarily by the HFE C282Y mutation that reduces hepcidin production and leads to progressive iron overload — affects approximately 1 in 250 people of Northern European ancestry as C282Y homozygotes and approximately 1 in 10 as heterozygous carriers. C282Y homozygosity produces clinically significant iron overload in approximately 40 percent of affected men and 10 percent of women (menstruation providing protective blood loss in premenopausal women). Complications include cirrhosis, hepatocellular carcinoma, cardiomyopathy, diabetes, arthritis, and skin hyperpigmentation. Treatment with therapeutic phlebotomy (bloodletting) to reduce iron stores is straightforward and effective when initiated before organ damage occurs.4
Regular blood donation reduces body iron stores by approximately 200-250 mg per donation (each donation removes approximately 450-500 mL of blood containing approximately 200-250 mg of iron). This produces measurable reductions in serum ferritin (by 30-50 ng/mL per donation) and reduces markers of oxidative stress. Observational studies of regular blood donors versus non-donors find lower rates of cardiovascular events in the donor population — though residual healthy donor effect confounding is difficult to eliminate. The mechanistic rationale (iron reduction reduces oxidative stress) and the safety record (blood donation is the most carefully monitored elective procedure in medicine) make regular donation a reasonable iron management strategy for adults with ferritin in the upper normal range, particularly post-menopausal women and men who no longer have significant blood loss.5
