Palaeoscolecidan worms are rare, Early Palaeozoic fossils with uncertain affinities within the Ecdysozoa. They are locally abundant in the Cambrian and scattered in the Early Ordovician, but very sparse thereafter. Forty-four specimens have been collected from the Middle Ordovician of the Builth-Llandrindod Inlier of Mid Wales and include well-preserved material assigned to seven new genera, with four additional species in open nomenclature. An additional specimen from the Arenig Pontyfenni Formation of South Wales is also described in open nomenclature. The total demonstrates much greater palaeoscolecid diversity than hitherto suspected for this time. The specimens are preserved as cuticle fragments in shales and siltstones, often of submi...
Konservat-Lagerstätten are a source of insurmountable information on the diversity of fossil assembl...
The attribute traditionally used to recognise the occurrence of ostracods in the Palaeozoic stratigr...
The renowned soft-bodied faunas of the Cambrian period, which include the Burgess Shale, disappear f...
Palaeoscolecidan worms are rare, Early Palaeozoic fossils with uncertain affinities within the Ecdys...
The Lower Ordovician Fezouata Lagerstatte from Morocco (central Anti-Atlas, Zagora area) has yielded...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
The Late Ordovician Tafilalt Biota of the Moroccan Anti-Atlas includes a diverse range of soft-bodie...
Exceptional preservation of non-biomineralized arthropods, sponges and vermiform taxa occurs in the ...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
A diverse fauna of three-dimensionally preserved sponges is described from nearshore volcanogenic sa...
Three-dimensional fragments of palaeoscolecid cuticle have been recovered from the Furongian (upper ...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Here we report a locality containing exceptionally preserved (soft-bodied) fossils of mid-Late Ordov...
Scolecodonts are common microfossils in Palaeozoic rocks, bearing witness to the extensive radiation...
Majority of the palaeontological data are collectedfrom skeletonized specimens. As a result, our per...
Konservat-Lagerstätten are a source of insurmountable information on the diversity of fossil assembl...
The attribute traditionally used to recognise the occurrence of ostracods in the Palaeozoic stratigr...
The renowned soft-bodied faunas of the Cambrian period, which include the Burgess Shale, disappear f...
Palaeoscolecidan worms are rare, Early Palaeozoic fossils with uncertain affinities within the Ecdys...
The Lower Ordovician Fezouata Lagerstatte from Morocco (central Anti-Atlas, Zagora area) has yielded...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
The Late Ordovician Tafilalt Biota of the Moroccan Anti-Atlas includes a diverse range of soft-bodie...
Exceptional preservation of non-biomineralized arthropods, sponges and vermiform taxa occurs in the ...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
A diverse fauna of three-dimensionally preserved sponges is described from nearshore volcanogenic sa...
Three-dimensional fragments of palaeoscolecid cuticle have been recovered from the Furongian (upper ...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Here we report a locality containing exceptionally preserved (soft-bodied) fossils of mid-Late Ordov...
Scolecodonts are common microfossils in Palaeozoic rocks, bearing witness to the extensive radiation...
Majority of the palaeontological data are collectedfrom skeletonized specimens. As a result, our per...
Konservat-Lagerstätten are a source of insurmountable information on the diversity of fossil assembl...
The attribute traditionally used to recognise the occurrence of ostracods in the Palaeozoic stratigr...
The renowned soft-bodied faunas of the Cambrian period, which include the Burgess Shale, disappear f...