Thanahita distos is a new species of lobopodian, an ancient relative of modern-day velvet worms, in 430 million-years-old Silurian rocks in Herefordshire, UK.
Reconstruction
Description[]
Further, morphological analysis places it within a lobopodian group that typifies an earlier period of geological time in the Cambrian – about 520 to 510 million years ago – thus indicating the survival of this group over some 100 million years.[1]
Thanahita was most closely related to Hallucigenia.
Discovery[]
First author Derek Siveter, Professor Emeritus of Earth Sciences at Oxford University and Honorary Research Associate at Oxford University Museum of Natural History, says; the Lobopodians are extremely rare in the fossil record, except in the Cambrian Period. Worm-like creatures with legs, they are an ancestral marine relative of modern-day velvet worms, or onychophorans – predators that live in vegetation, mainly in southern latitudes.
This new lobopodian, was discovered during fieldwork in an area of Silurian rocks in Herefordshire. It is the first lobopodian to be formally described from rocks of Silurian age worldwide; exceptionally, it is fully three-dimensionally preserved, and it represents one of only eight known three-dimensionally preserved lobopodian or onychophoran fossil specimens.
3D reconstruction model
Professor Siveter said: ‘Thanahita distos and the other animals that became fossilised here likely lived 100 to 200 meters down, possibly below the depth to which much light penetrates. It has been deduced because the team found no vestiges of photosynthetic algae, which are common in contemporaneous rocks laid down at shallower points on the seafloor to the east.
Some special circumstances allowed for their remarkable preservation. The first was the immediate precipitation of clay minerals around the dead organisms, which decayed over time, leaving empty spaces behind. The mineral calcite – a form of calcium carbonate – then filled these natural moulds, replicating the shape of the animals. Almost at the same time, hard concretions began to form, being cemented by calcite. Thanks to the early hardening of these Silurian time capsules in this way, the fossils were not squashed as the ash layer slowly compacted. He added: Some lobopodians lie in a position on the tree of life which foreshadows that of the terrestrial velvet worms, while others are precursors of the arthropods: the “king crabs”, spiders, crustaceans and related forms. Since its discovery, the Herefordshire Lagerstätte has yielded a diversity of arthropods that have contributed much to our understanding of the palaeobiology and early history of this very important invertebrate group. The lobopodian Thanahita distos belongs to an extended, panarthropod grouping. [2]