A new type of shell damage on Late Jurassic ammonite Kachpurites fulgens is described. The new type of shell malformation consists of small elongated pits, arranged in groups on the surface of ammonite shell and concentrated near the terminal aperture. The examination of the pits demonstrated no signs of drilling, biting, or healing of punctures. The shell layers in the pits are bent downward without changing in thickness. At the same time the pits, in some cases, significantly distort the shape of the shell walls. Deformed growth lines are associated with some of the pits. All of this supports the hypothesis that the pits had been formed by epifauna located at a flexible uncalcified part of the periostracum in the apertural region of the growing ammonite shell. It is likely that epizoan attachment led to the deformation of the thin periostracum film and to the distortion of the growing shell wall. The nature of epizoans is discussed, but remains unclear due to their rather poor preservation. The relationship between epizoans and ammonites is also an open question: they could have been parasites, but other types of biotic relationships cannot be entirely ruled out.
The article is devoted to the description of a new type of shell malformation which is found in the Upper Jurassic (Upper Volgian) ammonites Kachpurites fulgens. These are shallow elongated pits on the shells, in which all the aragonitic layers of the shell bend downward. These pits are often accompanied by curved growth lines. Most likely, these pits were caused by epizoans or parasites which lived in the apertural part of the ammonite shell and curved the newly formed periostracum.
Ammonoidea, Craspeditidae, Kachpurites, parasites, epifauna, Jurassic, Russia.