Different populations have different allele frequencies of these genes, and it is the combination of these allele variations that bring about the complex, continuous variation in skin coloration we can observe today in modern humans. Population and admixture studies suggest a 3-way model for the evolution of human skin color, with dark skin evolving in early hominids in sub-Saharan Africa and light skin evolving independently in Europe and East Asia after modern humans had expanded out of Africa.For skin color, the broad sense heritability (defined as the overall effect of genetic vs. nongenetic factors) is very high, provided one is able to control for the most important nongenetic factor, exposure to sunlight. Many aspects of the evolution of human skin and skin color can be reconstructed using comparative anatomy, physiology, and genomics. Enhancement of thermal sweating was a key innovation in human evolution that allowed maintenance of homeostasis (including constant brain temperature) during sustained physical activity in hot environments. Dark skin evolved pari passu with the loss of body hair and was the original state for the genus Homo. Melanin pigmentation is adaptive and has been maintained by natural selection. In recent prehistory, humans became adept at protecting themselves from the environment through clothing and shelter, thus reducing the scope for the action of natural selection on human skin. Credit for describing the relationship between latitude and skin color in modern humans is usually ascribed to an Italian geographer, Renato Basutti, whose widely reproduced "skin color maps" illustrate the correlation of darker skin with equatorial proximity.
In the fourth stage taking place 12 to 96 hours after ingestion, liver toxicity and failure occurs as the cells begin to die. In the last stage of iron poisoning following 2 to 8 weeks after ingestion, scarring of the gastrointestinal mucosal lining resulting in bowel obstruction. Cause
Pathophysiology
Iron is essential for the production of hemoglobin in red blood cells which is responsible for transporting oxygen throughout the body. In normal physiologic conditions, nonionic forms of iron (Fe°) are converted into ferrous iron (Fe2+) by gastric acid in the stomach. Ferrous iron is then absorbed in the small intestine where it is oxidized into its ferric iron (Fe3+) form before being released into the bloodstream. Free iron in the blood is toxic to the body as it disrupts normal cell function, damaging organs such as the liver, stomach, and cardiovascular system. The human body has protective mechanisms in place to prevent excess free ferric iron from circulating the body. When being transported throughout the body, iron is bound to an iron transporting protein called transferrin to prevent iron from being absorbed into different cells. Any excess iron is stored as ferritin in the liver. In the event of iron overdose, iron stores become oversaturated and the bodys protective mechanisms fail resulting in excess free circulating iron. Toxic Dose
Iron poisoning can occur when doses of 20 to 60 mg/kg or more of elemental iron is ingested with most cases reporting primarily gastrointestinal symptoms. Systemic signs and symptoms shown in serious toxicity occur at higher doses exceeding 60 mg/kg.