Waptia is an extinct genus of marine arthropod from the Middle Cambrian of North America. It grew to a length of 6.65 cm (3 in), and had a large bivalved carapace and a segmented body terminating into a pair of tail flaps. It was an active swimmer and likely a predator of soft-bodied prey. It is also one of the oldest animals with direct evidence of brood care. Waptia fieldensis is the only species classified under the genus Waptia, and is known from the Burgess Shale Lagerstätte of British Columbia, Canada. Specimens of Waptia are also known from the Spence Shale of Utah, United States. Based on the number of individuals, Waptia fieldensis is the third most abundant arthropod from the Burgess Shale Formation, with thousands of specimens collected. It was among the first fossils found by the American paleontologist Charles D. Walcott in 1909. He described it in 1912 and named it after two mountains near the discovery site – Wapta Mountain and Mount Field. Although it bears a remarkable resemblance to modern crustaceans, its taxonomic affinities were long unclear. A comprehensive redescription published in 2018 classified it a member of Hymenocarina (which contains numerous other bivalved arthropods) within Mandibulata.
Description
Known specimens of Waptia range in length from 13.5 to 66.5 millimetres (0.53 to 2.62 in) with the vast majority (~85%) being 40 to 60 millimetres (1.6 to 2.4 in) long. The bivalved carapace was saddle shaped, and was thin and non mineralised, and was likely flexible in life. The carapace was laterally compressed (narrow along the sideways axis), and had no distinct boundary between the two halves. The carapace was only attached to the body in a small section near the front of the head. The body was divided into three main segments, the cephalothorax (head), the post-cephalothorax, and the abdomen. The front of the head bore a pair of reniform (kidney shaped) compound eyes, about 1 millimetre (0.039 in) across, which were born on short stalks. One specimen with preserved ommatidia shows that density of ommatidia in the eye was about 600 per square millimetre. It is suggested that this allowed good forward and peripheral vision. A pair of small lobes, about 1 millimetre (0.039 in) long, protrude near the eyes. Similar structures are known from the related Canadaspis as well as other mandibulates, and are thought to correspond to the hemi-ellipsoid bodies of crustaceans, and thus likely have an olfactory function. Between the eyes is a triangular structure, dubbed the "median triangular projection", which is probably homologous to the 'anterior sclerite' of other Cambrian arthropods. The head bears a pair of antennae, which are composed of 10 elongate cylindrical segments/podomeres, which sequentially reduce in width towards the tip of the antenna. The front ends of each podomere bear setae (hair-like structures), which are orientated at an angle of 75° to 95° relative to the antennae axis. The mandibles have a three-segmented projection, which are covered with setae. The mandibles shows evidence of sclerotisation toward the edge where the two mandibles contacted, which have a toothed margin. The mandibles likely had a biting and grinding function. The maxillae are composed of at least six, probably nine podomeres, the end podomere bears a pair of claws, along with numerous setae. These likely assisted food manipulation alongside the mandibles. The cephalothorax has four additional pairs of uniramous (single branched) leg-like appendages (endopods), the first three of which are well segmented, with 5 segments, which are tipped with claws, with a 4 or 5 segmented basipod with well developed endites (structures present on the underside of the limb), particularly on the first pair, which project inward from the legs. The fourth leg differs in the fact that only the very end of the leg is segmented, with the rest being annulated, with the annulated regions being fringed by lamellae.
The "post-cephalothorax" has 5 segments, associated with 6 somites with corresponding pairs of uniramous annulated appendages, which are fringed with lamellae. The following abdomen is approximately 60% of the total length, with 6 segments and no corresponding legs, which terminates in a forked tail fluke, in which each fluke is composed of three segments.
Discovery
Waptia fieldensis was one of the first fossils discovered by Charles D. Walcott from the Burgess Shale in August 1909. A rough sketch of Waptia is present in his diary for August 31, 1909, alongside sketches of Marrella and Naraoia. A formal description for the species was published by Walcott in 1912. The species was named after the two mountains connected by the Fossil Ridge containing the Burgess Shale locality, Wapta Mountain and Mount Field of Yoho National Park, British Columbia, Canada. The name of Wapta Mountain itself comes from the First Nation Nakoda word wapta, meaning "running water"; while Mount Field was named after the American telecommunications pioneer Cyrus West Field.
Taphonomy Specimens of Waptia fieldensis were recovered from the Burgess Shale Lagerstätte of Canada, which dates from the Middle Cambrian period (510 to 505 million years ago). The locality was once about 200 m (660 ft) underwater; it was located at the bottom of a warm and shallow tropical sea adjacent to a submarine limestone cliff (now the Cathedral Limestone Formation). Undersea landslides caused by the collapse of parts of the limestone cliff would periodically bury the organisms in the area (as well as organisms carried by the landslides) in fine-grained mud that later became shale. Based on the number of individuals, Waptia fieldensis constitutes about 2.55% of the total number of organisms recovered from the Burgess Shale, and 0.86% of the Greater Phyllopod bed. This makes them the third most abundant arthropods of the Burgess Shale (after Marrella and Canadaspis). The National Museum of Natural History alone houses more than a thousand specimens of the species from the Burgess Shale. Waptia fieldensis are often found disarticulated, with parts remaining in close proximity to each other. Specimens of Waptia, referred to as Waptia cf. fieldensis have also found recovered from the Middle Cambrian Spence Shale in Utah, USA. Some of these specimens are associated with three dimensionally preserved eggs.
… excerpt ends here. Continue reading the full article.
