Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacking in the archetypal Cambrian Lagerstätten, the Burgess Shale. Here I describe Scathascolex minor gen. et sp. nov, the first unequivocal palaeoscolecid from this site. Scathascolex is armoured with simple Hadimopanella-like plates, but lacks smaller platelets, pointing to a close affinity with the Palaeoscolecida sensu stricto. Neither preservational nor environmental factors account for the scarcity of palaeoscolecids in the Burgess Shale, which presumably represents an ecological phenomenon
Nectocaridids are soft-bodied early to middle Cambrian organisms known from Burgess Shale-type depos...
Cricocosmia jinningensis, one of the most abundant palaeoscolecid worms from the Lower Cambrian Chen...
The 508-million-year-old Burgess Shale (British Columbia) is among the most important fossil localit...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
Three-dimensional fragments of palaeoscolecid cuticle have been recovered from the Furongian (upper ...
The reconstruction of ancestors is a central aim of comparative anatomy and evolutionary development...
The soft-bodied Cambrian organism Wiwaxia poses a taxonomic conundrum. Its imbricated dorsal sclerit...
P>The reconstruction of ancestors is a central aim of comparative anatomy and evolutionary develo...
The fossil record plays a key role in reconstructing deep evolutionary relationships through its doc...
The stem-group priapulid Ottoia Walcott, 1911, is the most abundant worm in the mid-Cambrian Burgess...
SummaryA spectacular Cambrian soft bodied fauna some 40 km from Walcott's original Burgess Shale loc...
Nectocaridids are soft-bodied early to middle Cambrian organisms known from Burgess Shale-type depos...
Cricocosmia jinningensis, one of the most abundant palaeoscolecid worms from the Lower Cambrian Chen...
The 508-million-year-old Burgess Shale (British Columbia) is among the most important fossil localit...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Palaeoscolecid worms are a ubiquitous group of Early Palaeozoic ecdysozoans that are curiously lacki...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with ...
Three-dimensional fragments of palaeoscolecid cuticle have been recovered from the Furongian (upper ...
The reconstruction of ancestors is a central aim of comparative anatomy and evolutionary development...
The soft-bodied Cambrian organism Wiwaxia poses a taxonomic conundrum. Its imbricated dorsal sclerit...
P>The reconstruction of ancestors is a central aim of comparative anatomy and evolutionary develo...
The fossil record plays a key role in reconstructing deep evolutionary relationships through its doc...
The stem-group priapulid Ottoia Walcott, 1911, is the most abundant worm in the mid-Cambrian Burgess...
SummaryA spectacular Cambrian soft bodied fauna some 40 km from Walcott's original Burgess Shale loc...
Nectocaridids are soft-bodied early to middle Cambrian organisms known from Burgess Shale-type depos...
Cricocosmia jinningensis, one of the most abundant palaeoscolecid worms from the Lower Cambrian Chen...
The 508-million-year-old Burgess Shale (British Columbia) is among the most important fossil localit...