Fossils show that during the Earth's Late Carboniferous period (around 300 million years ago) there were several species of insects - e.g. Meganeura (giant dragonflies) and Arthropleura (giant millipedes) - which reached sizes far larger than known today.
There are currently (at least) three theories regarding the phenomenon. See : Wikipedia
The upper limit on insect size is generally assumed to be associated with the way in which insects 'breathe' through absorption. After a certain size limit, they would not be able to absorb enough oxygen to operate.
As early as 1911, theories were proposed that there must have been more oxygen in the Earth's atmosphere - roughly 10-15% higher than today, which would have allowed them to grow much larger than is currently viable.
Another theory suggests that they may not have had many (or any) predators, and this allowed them to grow. Many of today's largest animals have very few, if any predators.
The third explanation is that water-dwelling larvae had to grow bigger in order to protect themselves from toxic levels of dissolved oxygen in the water. See : PLOS ONE, 2011
Ideas for new topics, and suggested additions / corrections for old ones, are always welcome.
If you have skills or interests in a particular field, and have suggestions for Wikenigma, get in touch !
Or, if you'd like to become a regular contributor . . . request a login password. Registered users can edit the entire content of the site, and also create new pages.
( The 'Notes for contributors' section in the main menu has further information and guidelines etc.)
You are currently viewing an auto-translated version of Wikenigma
Please be aware that no automatic translation engines are 100% accurate, and so the auto-translated content will very probably feature errors and omissions.
Nevertheless, Wikenigma hopes that the translated content will help to attract a wider global audience.