Fossil Burrows Issue to Historical Seafloor Colonization by Big Maritime Worms
Large ambush-predator worms, doable ancestors of the ‘bobbit worm’, may possibly have colonized the seafloor of the Eurasian continent all over 20 million a long time back. The findings, based on the reconstruction of substantial, L-shaped burrows from layers of seafloor courting back to the Miocene (23 million to 5.3 million decades back) of northeast Taiwan, are noted in Scientific Stories this 7 days.
Ludvig Löwemark and colleagues reconstructed a new trace fossil, which they name Pennichnus formosae, utilizing 319 specimens preserved in layers of seafloor shaped in the course of the Miocene period throughout northeast Taiwan. Trace fossils are geological functions such as burrows, track marks and plant root cavities preserved in rocks, which let for conclusions to be drawn about the conduct of ancient organisms. The trace fossil is made up of an L-shaped burrow, approximately 2 meters in length and 2-3 centimeters in diameter.
The morphology of Pennichnus indicates the burrows had been probable inhabited by big maritime worms, these as the bobbit worm (Eunice aphroditois), which are continue to found now. Bobbit worms disguise in long, slim burrows within the seafloor and propel upwards to seize prey. The authors recommend that the retreat of an historic worm and its prey into the sediment prompted distinct feather-like collapse buildings preserved in Pennichnus formosae, which are indicative of disturbance of the sediment bordering the burrow. Additional examination disclosed a significant focus of iron to the top rated section of the burrow. The authors propose this might reveal that the worm re-constructed its burrow by secreting mucus to reinforce the burrow wall, as microorganisms that feed on mucus made by maritime invertebrates are recognised to produce iron-wealthy environments.
Although marine worms have existed considering that the early Palaeozoic, their bodies comprise largely of smooth tissue and are therefore not often preserved. The trace fossil offered in the review is considered to be the initially recognized fossil of this type made by a sub-area ambush predator. It gives a rare glimpse into these creatures’ behaviour beneath the seafloor.
Reference: “The 20-million-yr aged lair of an ambush-predatory worm preserved in northeast Taiwan” 21 January 2021, Scientific Reports.