One of the identifying characteristics of tetrapods (limbed vertebrates) is the presence of fingers and toes. Whereas the proximal part of the tetrapod limb skeleton can easily be homologized with the paired fin skeletons of sarcopterygian (lobe-finned) fish, there has been much debate about the origin of digits. Early hypotheses 1 interpreted digits as derivatives of fin radials, but during the 1990s the idea gained acceptance that digits are evolutionary novelties without direct equivalents in fish fin skeletons. This was partly based on developmental genetic data 2 , but also substantially on the pectoral fin skeleton of the elpistostegid (transitional fish/ tetrapod) Panderichthys, which appeared to lack distal digit-like radials 3 . Here we present a CT scan study of an undisturbed pectoral fin of Panderichthys demonstrating that the plate-like 'ulnare' of previous reconstructions is an artefact and that distal radials are in fact present. This distal portion is more tetrapod-like than that found in Tiktaalik 4 and, in combination with new data about fin development in basal actinopterygians 5 , sharks 6 and lungfish 7 , makes a strong case for fingers not being a novelty of tetrapods but derived from pre-existing distal radials present in all sarcopterygian fish.A near-complete specimen of Panderichthys from the late Middle Devonian period (385 million years ago; see Supplementary Information) of Lode, Latvia (Institute of Geology at Tallinn University of Technology specimen number GIT434-1) forms the basis of this study. Although the dorsal part of the skull and left side of the body have suffered substantial damage from a mechanical excavator, the specimen was originally well preserved. Notably, its body axis is straight (determined from the alignment of dorsal midline scales and the symmetry plane of the skull) and it appears less dorsoventrally compressed than others from the same locality. This is shown, for example, by the narrow skull outline and near-vertical cheek-plate fragments, distinctly different from the flattened and splayed skulls that have been published 8,9 . The specimen also contains the only known pelvis and pelvic fin skeleton of Panderichthys 10 .The right pectoral fin and most of the shoulder girdle are preserved in articulation, with the fin concealed under the body. This region of the specimen was CT scanned at the East-Tallinn Central Hospital (see Methods Summary and Supplementary Methods). The scanned region comprises the entire fin endoskeleton and an estimated 40% of the lepidotrichial fin web, as well as most of the shoulder girdle. The presence of X-ray-reflective crystal growths in the shoulder region unfortunately prevented complete modelling of the scapulocoracoid. The entire fin is covered by scales and lepidotrichia, which cannot be modelled individually but are easily separated from the darker endoskeleton. The leading or preaxial margin of the fin is dipping ventrolaterally into the substrate (Fig. 1a-c). In contrast to early tetrapods, in which the limb projects at...