thin filaments. Plumaceous, down-like feathering typically has an opposite appearance, with a short central quill and long tufts. In addition, the thick filaments preserve no evidence of Calcium phosphate, the mineral which modern feather quills are made of. The large amount of curvature present in the filaments also makes a strong central quill unlikely. Thus, the idea that thick filaments are simply bundles of thin filaments is less unusual than the idea that they were a variant of quilled plumaceous feathers which developed a morphology opposite that of birds and other feathered theropods. As a whole, the study preferred the hypothesis that Sinosauropteryx feathers were simple single-branch filaments, although it is conceivable that they were occasionally joined at the base into tufts as predecessors to down-like plumaceous feathers. While Sinosauropteryx had feather-like structures, it was not very closely related to the previous "first bird" Archaeopteryx. There are many dinosaur clades that were more closely related to Archaeopteryx than Sinosauropteryx was, including the deinonychosaurians, the oviraptorosaurians, and the therizinosauroids. This indicates that feathers may have been a characteristic of many theropod dinosaurs, not just the obviously bird-like ones, making it quite likely that equally distant animals such as Compsognathus had feathers as well. Colouration Sinosauropteryx was the first dinosaur to have its life colouration described by scientists based on physical evidence. Some fossils of Sinosauropteryx show an alternation of lighter and darker bands preserved on the tail. Chen and colleagues initially interpreted this banding pattern as an artifact of the splitting between the main slab and counter-slab in which the original specimen was preserved. However, Longrich suggested in his 2002 presentation for the Society of Vertebrate Paleontology that these specimens actually preserve remnants of the colouration pattern the animal would have exhibited in life. He argued that the dark, banded areas on the tail were too evenly spaced to have been caused by random separation of the fossil slabs, and that they represent fossilized pigments present in the feathers. Additionally, rather than an artifact of preservation or decomposition, the presence of dark feathers along only the top of the body may also reflect the colour pattern in life, indicating that Sinosauropteryx prima was countershaded with dark colouration on its back and lighter colouration on its underside, with bands or stripes on the tail for camouflage. Longrich's conclusions were supported in a paper first published online in the journal Nature in January