Theropod dinosaurs have captured the imagination of the public and paleontologists alike. Histology of the bones of theropods has revealed much about dinosaur physiology, behavior, and growth. Histology and ultraviolet fluorescence (UVFL) microscopy of one controversial dinosaur, Nanotyrannus lancensis, reveals the presence of blood clots in post-fixed vessel canals of claw, vertebra, and other isolated post-cranial elements collected at Hell Creek, MT. These clots are thicker, more closely adherent to canal walls, and more reactive to 347 nm UVFL incident light than unfixed specimens. Theropod histology images in the literature display similar clots, and those should be subjected to UVFL for confirmation. In addition, nematodes are evidently preserved in vessel canals of dinosaurs.

Dimetrodon sp. femur, jaw, teeth, and rib bones were collected at N.E. Frederick, OK, and sectioned for histological examination. This Oklahoma Museum of Natural History site has yielded well-preserved Paleozoic fossils for decades. All bones were heavily infiltrated with calcite and other minerals, yet a reddish-brown mass obstructed many vascular channels. This reddish-brown mass reacted to 374 nm UV illumination by emitting bright blue autofluorescence. This was true for every specimen and indicates a heavy presence of iron. We conclude that the iron in the canals is the crystallized remains of blood that clotted during an asphyxiation event that killed the animal. Remarkably similar reddish-brown obstructive material has also been observed in other histological studies performed on Dimetrodon bones. We conclude that these are also the remains of blood clots and simply await examination under UV fluorescence.

Remarkable discoveries such as condensed chromatin in duckbill dinosaur cartilage and newly presented discoveries of dinosaur vascular veins, venule valves, and nerve fibers (this report) warrant study of global dinosaur remains for preserved soft tissue (dST). Dinosaur osteocytes feature dendritic projections (filipodia) of lengths up to 18 µm, while osteocytes collected from a Triceratops horn have lengths of 25 µm or longer. While preservation methods for dST involve the degradation of sugars into glycation end products and the employment of highly oxidative hydroxyl radicals to “fix” tissues, we note that lengthy and narrow osteocyte filipodia show no signs of hydroxyl radical infiltration into the lacuna-canalicular network. Moreover, our ultraviolet fluorescence (UVFL) study of Triceratops horn, rib, vertebra, and frill thin sections shows extensive clotting in most vessel canals, probably as a result of asphyxia while drowning. Further UVFL autofluorescence study of dinosaur bone sections is vital for characterization of dinosaur blood clots.