just some paleo trip pictures ft me being a dweeb

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just some paleo trip pictures ft me being a dweeb

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Zoophycos is a trace fossil - that means it wasn't part of an organism but is a distrubance in the sediments caused by the organism. An example would be burrowing tunnels. In this case it is a grazing trace left as the creature ate away organic-rich sediments. The creature would burrow down to find the choicest beds and then spiral outwards eating all the godies as it went. All that is left is the rasping marks in a radiating or spiral pattern. The bed this one is in must have been particularly rich as teher were 4 or 5 of these in a couple of square metres. You can find these fossils all over Guedalest town in the paving stones, which is surprising since they tend to favour more clay-rich marly sediments which don't normally make good paving stones.
#2783 - Zoophycos sp.
Not a fossil animal. Not a fossil plant, either, although that's what they were originally described as in 1855. They're actually an ichnofossil - a trace fossil preserving the activity of a long-dead animal. What the creature WAS is an open question - it was probably worm-like. Although of course there's no guarantee that it's the same animal that's been making these ichnofossils for 521 million years.
The ichnofossils can be a meter across and deep. In structure they're closely packed J- or U-shaped lobes around a burrow, although as the epochs rolled on Zoophycos traces have been getting more and more elaborate, with branching lobes or layers built up in a corkscrew-fashion. Earlier examples are from shallower depths, but later they're more often found in deepwater turbidite beds, where mud and sand was deposited by huge underwater landslides. However, even in more recent times they're also known from nearshore formations where storms deposit a lot of sediment.
From all the evidence, it would seem the Zoophycos organism (or organisms) lived in places where there aren't many other animals to compete with them, and were methodically searching freshly settled sediment around them for anything to eat.
University of Otago Geology Museum, Dunedin, Aotearoa New Zealand