Nepedia
Back to Discover
Advanced Reader
🧬

Evolution of insects

life science Maturity 9-11 evolution Next article →

This article covers sensitive topics: evolution. Parents can manage visibility in Parental Controls.

Insects are among the most diverse and successful groups of animals on Earth. Their long history is a story of constant adaptation to a changing planet. Scientists study this history through many different scientific lenses. They use molecular biology to look at DNA and morphology to study body shapes. They also use paleoentomology, which is the study of insect fossils, to piece together the past. By combining these fields with bioinformatics and embryology, researchers can reconstruct how insects became the creatures we see today.

Insect antennae
Insect antennae

The evolutionary journey of insects likely began hundreds of millions of years ago. Many scientists believe insects evolved from a group of crustaceans. Molecular analysis suggests that hexapods, or six-legged animals, diverged from their relatives around the start of the Silurian period. This timing coincides with the appearance of vascular plants on land. While some researchers argue insects appeared even earlier during the Ordovician period, this remains a controversial idea. This is because there is a lack of insect fossils from the Cambrian or Silurian periods to prove it.

Rhyniognatha specimen
Rhyniognatha specimen
Strudiella interpretation
Strudiella interpretation

As insects moved onto land, they underwent several major evolutionary stages. The first insects were landbound, but the Devonian period brought a massive change. About 400 million years ago, one lineage of insects evolved flight. These were the very first animals to ever fly. Later, during the Carboniferous period, which lasted from 358 to 299 million years ago, the Pterygotes, or winged insects, underwent a major radiation. This means they rapidly diversified into many new forms. Following this, the Endopterygota, which are insects that go through distinct life stages via metamorphosis, radiated during the Permian period.

Mazothairos1
Mazothairos1

Earth's history has been marked by dramatic shifts in climate and life. About 252 million years ago, the Permo-Triassic boundary saw the largest mass extinction in Earth's history. Many early insect groups were lost during this event. However, the survivors evolved during the Triassic period into the modern insect orders we recognize today. Most modern insect families appeared during the Jurassic period, between 201 and 145 million years ago. By the Cretaceous period, many insect groups began to evolve alongside flowering plants. This process is known as co-evolution, where two different groups change together in a way that affects both. Today, about 20% of extant insects depend on flowers, nectar, or pollen for food. In return, more than two-thirds of flowering plants rely on insect pollination to reproduce.

Fossil insect (Diptera, Nematocera in Baltic amber. Age 50 Mill. years (the Lower Eocene)
Fossil insect (Diptera, Nematocera in Baltic amber. Age 50 Mill. years (the Lower Eocene)

Understanding this history requires a deep look at how insects become fossils. Because insects are small and light, they do not always leave a strong fossil record. Only about 1/100 of known insect species are represented in the fossil record. Most insect fossils are found in lake environments, known as lacustrine settings. Insects might live in the lake or be carried into it by wind or water. If they die and settle into anoxic, or oxygen-poor, sediments, they may be preserved. Some insects are preserved as compressions or impressions in rocks. These show the shape of the insect, sometimes even the texture of the wing membranes.

Other fossils are much more detailed. Some insects are preserved in amber, which is fossilized tree resin. This type of preservation became abundant during the Mesozoic era. Amber can capture insects in perfect condition, sometimes even preserving their original color and patterns. Another method is mineral replication, or petrifaction. This happens when minerals replace the insect's body, often creating a three-dimensional replica. Some fossils are also found as concretions, which are stones with a fossil at the core. These form when minerals precipitate around a decaying organism. These diverse preservation methods allow scientists to study everything from ancient feeding damage to fossilized nests and fecal pellets.

Rhyniognatha specimen
Rhyniognatha specimen

Insects continue to play a vital role in global ecosystems. Their ability to fill available environmental niches is driven by rapid adaptation and high fecundity, which is the ability to produce many offspring. While many insects are helpful pollinators, others act as vectors for pathogens. Some insects, like flies and mosquitoes, can spread diseases that have impacted other species. Despite these complexities, the evolutionary success of insects is undeniable. They have survived massive extinctions and shaped the very plants they live upon, creating a complex web of life that continues to evolve every day.

713 words

Where will your curiosity go next?

Keep exploring at your chosen reading level.

🖼️ Images & Media (5)
File:Insect antennae.jpg
Insect antennae.jpg
File:Fossil insect (Diptera, Nematocera in Baltic amber. Age 50 Mill. years (the Lower Eocene).jpg
Fossil insect (Diptera, Nematocera in...
File:Strudiella_interpretation.png
Strudiella_interpretation.png
File:Mazothairos1.jpg
Mazothairos1.jpg
File:Rhyniognatha specimen.png
Rhyniognatha specimen.png
More to explore

🔬 Go deeper

More advanced topics to explore

🪜 Step back

Simpler topics to build understanding

What is Nepedia?

A free, ad-free encyclopedia for children. Every article is written at five reading levels, so the same page works for a five-year-old and a fifteen-year-old — use the level switcher above to see this one change. No account needed to read.