Utahcaris orion Conway Morris & Robison, 1988, from the lower middle Cambrian (Series 3, Stage 5) Spence Shale Member situated in Utah, USA, is redescribed based on a restudy of the original material. Newly recognized features, including ventral lateral eyes, trunk appendages, and a bulbous cephalic shield with subtriangular extension, reinforce similarities with Sanctacaris uncata from the middle Cambrian Burgess Shale. Both are assigned to the new family, Sanctacarididae. Sanctacaridids represent the oldest chelicerates. Their ecology and that of their nearest non-chelicerate relatives indicate that Chelicerata were plesiomorphically predatory
Bulk sampling of middle Cambrian carbonate units in the lower Burgess Shale Formation (Wuliuan) and ...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The Guzhangian Weeks Formation (house Range, Utah, USA) contains a virtually unstudied but diverse a...
The Emu Bay Shale Lagerstätte (Cambrian Series 2, Stage 4) occurs on the north coast of Kangaroo Isl...
Abstract Background Chelicerata represents a vast cla...
The Emu Bay Shale Lagerstätte (Cambrian Series 2, Stage 4) occurs on the north coast of Kangaroo Isl...
The morphology of two new bivalved arthropods, Loricicaris spinocaudatus gen. et sp. nov. and Nereoc...
The Leanchoiliidae is well−known from abundant material of Leanchoilia, from the Burgess Shale and C...
The Spence Shale of northern Utah is the oldest North American middle Cambrian (~506–505 Ma) Burgess...
Traditionally, the origin and evolution of modern arthropod body plans has been revealed through inc...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
SummaryThe Cambrian fossil record of euarthropods (extant arachnids, myriapods, crustaceans, hexapod...
Characterized by atypical frontalmost appendages, leanchoiliids are early arthropods whose phylogene...
A new arthropod, Kootenichela deppi n. gen. n. sp., is described from the Stanley Glacier exposure o...
The Middle Ordovician (Darriwilian) Winneshiek Shale from Winneshiek County, Iowa, USA, hosts a Kons...
Bulk sampling of middle Cambrian carbonate units in the lower Burgess Shale Formation (Wuliuan) and ...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The Guzhangian Weeks Formation (house Range, Utah, USA) contains a virtually unstudied but diverse a...
The Emu Bay Shale Lagerstätte (Cambrian Series 2, Stage 4) occurs on the north coast of Kangaroo Isl...
Abstract Background Chelicerata represents a vast cla...
The Emu Bay Shale Lagerstätte (Cambrian Series 2, Stage 4) occurs on the north coast of Kangaroo Isl...
The morphology of two new bivalved arthropods, Loricicaris spinocaudatus gen. et sp. nov. and Nereoc...
The Leanchoiliidae is well−known from abundant material of Leanchoilia, from the Burgess Shale and C...
The Spence Shale of northern Utah is the oldest North American middle Cambrian (~506–505 Ma) Burgess...
Traditionally, the origin and evolution of modern arthropod body plans has been revealed through inc...
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It ...
SummaryThe Cambrian fossil record of euarthropods (extant arachnids, myriapods, crustaceans, hexapod...
Characterized by atypical frontalmost appendages, leanchoiliids are early arthropods whose phylogene...
A new arthropod, Kootenichela deppi n. gen. n. sp., is described from the Stanley Glacier exposure o...
The Middle Ordovician (Darriwilian) Winneshiek Shale from Winneshiek County, Iowa, USA, hosts a Kons...
Bulk sampling of middle Cambrian carbonate units in the lower Burgess Shale Formation (Wuliuan) and ...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The Guzhangian Weeks Formation (house Range, Utah, USA) contains a virtually unstudied but diverse a...