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Evolution of spiders

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Spiders are highly successful predators that have inhabited Earth for at least 380 million years.

Spider in amber
Spider in amber

They belong to a group of animals called chelicerates, which evolved from aquatic ancestors. Today, scientists have described more than 45,000 different species of spiders. These are organized into 114 families and 3,958 genera. Researchers believe there may actually be more than 120,000 species in total. Every year, new species are identified and described by researchers in the field.

A major part of spider evolution involves the development of silk and spinnerets. Spinnerets are specialized organs used to produce and direct silk. Early spider-like creatures, known as trigonotarbids, lived on land and had eight legs. They used book lungs to breathe, which are internal organs for respiration. However, trigonotarbids were not true spiders because they lacked spinnerets and could not spin silk. They are now extinct and have no living descendants.

Scientists use a method called a molecular clock to trace spider history. This tool uses genetic data to estimate when different groups diverged from one another. By using a molecular clock calibrated with 27 chelicerate fossils, researchers found that spiders likely diverged from other chelicerates between 375 and 328 million years ago. In the past, a fossil named Attercopus was thought to be the oldest spider. Now, experts believe it belonged to an extinct order called Uraraneida. This group could produce silk but lacked true spinnerets.

The oldest reported true spiders date back to the Carboniferous Period. Most of these early fossil spiders likely belonged to a group called Mesothelae. These spiders were different from modern spiders because their spinnerets were located underneath the middle of the abdomen. They lived in giant clubmoss and fern forests as ground-dwelling predators. They probably used silk for simple tasks, such as lining retreat holes or covering eggs. They may have also built basic ground sheet webs or trapdoor constructions.

As plant and insect life diversified, spiders developed more complex ways to use silk. Spiders with spinnerets located at the end of the abdomen appeared more than 200 million years ago. This group includes the Mygalomorphae and Araneomorphae. This anatomical change likely helped them create elaborate sheet and maze webs. It also allowed for the development of the safety dragline. The oldest known mygalomorph is a fossil called Rosamygale from the Triassic of France.

By the Jurassic period, many spiders had developed sophisticated aerial webs. The famous circular orb web was already in use by orb-weaver spiders.

Nephila burmanica attacking Cascoscelio incassa in Burmese amber
Nephila burmanica attacking Cascoscelio incassa in Burmese amber

A 110 million-year-old web preserved in amber shows a perfect orb structure. This ancient web even contains trapped prey, including a beetle, a mite, a fly, and a wasp's leg. One of the largest known fossil spiders, Mongolarachne jurassica, lived about 95 million years ago in China.

Modern spider diversity is quite different from the species that lived during the Mesozoic era. During the Cretaceous-Cenozoic interval, there was a major turnover in spider populations. The Cretaceous was dominated by groups like Synspermiata and Palpimanoidea. The Cenozoic era is now dominated by the RTA clade and araneoid spiders. The RTA clade is a large group of modern spiders linked by a specific trait on the male pedipalp called the retrolateral tibial apophysis.

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File:Spider in amber.jpg
Spider in amber.jpg
File:Nephila burmanica attacking Cascoscelio incassa in Burmese amber.jpg
Nephila burmanica attacking Cascoscelio...
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