Reisdorf and Wuttke, in 2012, provided an extensive discussion on the
taphonomy of the
Juravenator specimen, i.e. the events that lead to its death, transportation, and fossilization. The specimen was deposited within a lagoon, to where it must been transported, possibly from the nearby islands. It is possible that a flash flood swept the animal into the sea, in which case it likely died by drowning. It is also possible that the animal swam or drifted onto the sea, or that it rafted on plants, and was then transported by surface currents to its place of burial. The rafting hypothesis is supported by tree trunks found at the Schamhaupten locality. The specimen would have arrived on the sea floor within a few hours after its death, as otherwise gases forming in its body cavity would have prevented it from sinking in one piece. Water depth at the burial site would have been large enough to prevent refloating of the carcass after such gases were produced. The specimen was found in almost in full (bones still connected together), only the skull, pelvic girdle, and front section of the tail were disarticulated to some degree. The skeleton is nearly complete, and missing parts in the tail were likely lost during excavation. Some discussion have revolved around the original orientation of the fossil within the rock, that is if the slab was prepared from its top or bottom site, or whether the individual lay on its back or its belly. Chiappe and Göhlich, in their 2010 description, assumed that it lay on its belly, an interpretation that is further supported by an
aptychus (body part of an
ammonite) found within the slab; aptychi are almost always embedded with their concave sides pointing upwards. However, the original excavator later confirmed that the specimen is on the bottom site of the slab, and that it therefore lay on its back. Reisdorf and Wuttke, in 2012, discovered small, rounded stones within the belly area that they interpreted as
ooids. These ooids formed in shallow water and were likely transported with the individual to the place of burial. The authors speculate that
Juravenator might have lived on the shores, where the ooids might have been swallowed. It is also possible that the individual drowned in shallow water, inhaling ooids suspended in the water. Chiappe and Göhlich identified fossils of
isopods found with the specimen, and concluded that these animals likely have scavenged the carcass while it was still floating. Reisdorf and Wuttke, in 2012, stated that the isopods could alternatively have parasitising the living animal. When the cadaver arrived at the seafloor, its head came to rest on its right side and the tail bent to the left. The seafloor was devoid of life except for a covering of microbial mats, preventing disruption by scavengers. In contrast to many other specimens from the Solnhofen archipelago, including
Compsognathus, the
Juravenator specimen was not found in a typical
death pose with the neck and tail curved over the torso. Reisdorf and Wuttke concluded that death poses resulted from the release of elastic ligaments during decay that spanned the vertebral column. The
Juravenator specimen does not show such a pose because it was lying on its back, preventing the spine from bending. ==References==