Our understanding of when the very first animals started living on land is helped by identifying trace fossils -- the tracks and trails left by ancient animals -- in sedimentary rocks that were deposited on the continents.
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| Trackways [Credit: Anthony Shillito] |
What they discovered is that the trackways occur within volcanic ash that settled under water, and not within freshwater lake and sub-aerial sands (as previously thought). This means that the site is not the oldest evidence for animal communities on land, but instead "is actually a remarkable example of a 'prehistoric Pompeii'," says Shillito -- a suite of rocks that preserve trails made by distressed and dying millipede-like arthropods as they were overcome by ash from volcanic events.
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| Close-up of a looping millipede death-trail [Credit: Anthony Shillito] |
Volcanic ash is known to cause mass death in some modern arthropod communities, particularly in water, because ash is so tiny it can get inside arthropod exoskeletons and stick to their breathing and digestive apparatus. Shilllito and Davies noticed that most of the trails were extremely tightly looping -- a feature which is commonly associated with "death dances" in modern and ancient arthropods.
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| Close-up of one of the millipede trackways [Credit: Anthony Shillito] |
Understanding how life engineered major evolutionary advances within environments, and the rate and impact of these advances on the functioning of the Earth system, provides vital context for understanding global change at the present day, and underlines the inseparable relationship between life and the planet.
Source: Geological Society of America [December 13, 2018]









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