The Epigenetic Bridge: Genetic Assimilation and the Record of Transitional Fossils
The traditional view of evolution, often called the Modern Synthesis, suggests that transitions between species occur primarily through the slow accumulation of random genetic mutations. However, the fossil record occasionally reveals bursts of morphological change that seem to happen more rapidly than simple point mutations might allow. This is where genetic assimilation, a process fueled by epigenetics, provides a revolutionary explanation for the "transitional" forms we see in the Earth’s strata. From Plasticity to Permanence At its core, genetic assimilation is the process by which a physical trait that was originally triggered by the environment becomes "hard-wired" into the genome. This concept was pioneered by biologist C.H. Waddington in the 1940s and 1950s. He proposed that organisms possess a high degree of phenotypic plasticity the ability to change their physical form in response to environmental stress without changing their underlying DNA s...