Pikaia gracilens is an extinct animal known from the Middle Cambrian Burgess Shale of British Columbia. Sixteen specimens of Pikaia are known from the Greater Phyllopod bed, where they comprised 0.03% of the community. P. gracilens was discovered by Charles Walcott and first described by him in 1911. It was named after Pika Peak, a mountain in Alberta, Canada. Based on the obvious and regular segmentation of the body, Walcott classified it as a polychaete worm. It resembles a living chordate commonly known as the lancelet and perhaps swam much like an eel. Scale diagram of various Burgess Shale invertebrates, P. gracilens in yellow During his re-examination of the Burgess Shale fauna in 1979, paleontologist Simon Conway Morris placed P. gracilens among the chordates, making it perhaps the oldest known ancestor of modern vertebrates. He did this because it seemed to have a very primitive, proto-notochord, however, the status of Pikaia as a chordate is not universally accepted; its preservational mode suggests that it had cuticle, which is uncharacteristic of the vertebrates [2] (although characteristic of other cephalochordates); further, its tentacles are unknown from other vertebrate lineages.[2] The presence of earlier chordates among the Chengjiang, including Haikouichthys and Myllokunmingia, appears to show that cuticle is not necessary for preservation, overruling the taphonomic argument,[3] but the presence of tentacles remains intriguing, and the organism cannot be assigned conclusively, even to the vertebrate stem group. Its anatomy closely resembles the modern creature Branchiostoma.[4] Fossil specimen on display at the Smithsonian in Washington, D.C. Averaging about 11?2 inches (3.8 cm) in length, Pikaia swam above the sea floor using its body and an expanded tail fin. Pikaia may have filtered particles from the water as it swam along.[citation needed] Its "tentacles" may be comparable to those in the present-day hagfish, a jawless chordate.[citation needed] Only 60 specimens have been found to date. [edit]Description Pikaia was a primitive creature without a well defined head, being less than 2 inches (5 centimetres) long. It swam in the mid-Cambrian seas, and is closely related to the ancestor of all animals with backbones (vertebrates), from fish to amphibians, reptiles, birds, and mammals. Pikaia is one of the most interesting of the multitude of animal fossils found in the famous Burgess Shale in the mountains of British Columbia, Canada. When alive, Pikaia was a sideways-flattened, a leaf-shaped animal. It swam by throwing its body into a series of S-shaped,

zig-zag curves, similar to movement of snakes. Fish inherited the same swimming movement, but they generally have stiffer backbones. Pikaia had a pair of large head tentacles and a series of short appendages, which may be linked to gill slits, on either side of its head. In these ways, it differs from the living lancelet. Pikaia's anatomy is still not fully known and palaeontologists are still researching its details. This primitive marine creature shows the essential prerequisites for vertebrates. The flattened body is divided into pairs of segmented muscle blocks, seen as faint vertical lines. The muscles lie on either side of a flexible structure resembling a rod that runs from the tip of the head to the tip of the tail.[5] [edit]Unlikely ancestor At first glance, Pikaia does not seem like a vertebrate ancestor, and, in fact there is a lot of debate regarding the topic in scientific circles. It looks like a worm that has been flattened sideways. But in detail, the fossils compressed within the Burgess Shale clearly show chordate features such as traces of an elongate notochord, dorsal nerve cord, and blocks of muscles (myotomes) down either side of the body all critical features for the evolution of the vertebrates. The notochord is a flexible rod-like structure that runs along the back of the animal, lengthening and stiffening the body so that it can be flexed from side to side by the muscle blocks for swimming. In the fish and all subsequent vertebrates, the notochord forms the backbone (or vertebral column). The backbone strengthens the body, supports strut-like limbs, and protects the vital dorsal nerve cord, while at the same time allowing the body to bend. Surprisingly, a Pikaia lookalike still exists today, the lancelet Branchiostoma. This little animal was familiar to biologists long before the Pikaia fossil was discovered. With notochord and paired muscle blocks, the lancelet and Pikaia belong to the chordate group of animals from which the vertebrates have descended. Molecular studies have refuted earlier beliefs that lancelets might be the closest living relative to the vertebrates, and instead favor tunicates in this position.[6] While the lancelet is a chordate, other living and fossil groups, such as acorn worms and graptolite, are more primitive. Called the hemichordates, they have only a notochord-like structure at an early stage of their lives. The presence of a creature as complex as Pikaia some 530 million years ago reinforces the controversial view that the diversification of life must have extended back well before Cambrian times, deep into the Precambrian.