Pronunciation: veh-NEN-o-SOR-us
Meaning: Poison Lizard
Author/s: Tidwell et al. (2001)
Synonyms: None known
First Discovery: Utah, USA
Discovery Chart Position: #490
Venenosaurus dicrocei
Being that venomous critters generally use their poison as a means to incapacitate something that they wish to eat, the "veneno" of Venenosaurus—from the Latin venenum meaning poison—may seem like a strange word to be attaching to a strict vegetarian, even one that's 12 meters long. And it would be. But it all makes sense when you look at its place of discovery: the Poison Strip Member of Utah's Cedar Mountain Formation, where Anthony DiCroce discovered its fossils in 1998. So the search for a toxin-crippling dinosaur continues. Humphh.
Venenosaurus, formally described in 2001, represents a gracile titanosauriform—a lightly built member of a group of long-necked plant-eating sauropods—from the Early Cretaceous, roughly 112 million years ago. Its partial skeleton—comprising vertebrae, limb bones, and pelvic elements—reveals a creature more lightly built than the barrel-bodied Camarasaurus, yet not as slender as Cedarosaurus, with which it shared its stratigraphic neighborhood. Its hand bones are long and slim, the forearms proportionally delicate, and the tail vertebrae display unusual side fossae (depressions or cavities). But unlike the fossae on most sauropods, which led to chambers for air-sacs to lighten their skeletons and enhance respiratory efficiency, these were merely deep depressions divided by internal ridges, hinting at a less specialized breathing system. The vertebrae also boast articulations not reported in any other sauropod.
In short, Venenosaurus is the kind of awkwardly gorgeous fossil that keeps paleontologists honest: fragmentary enough to provoke questions, rich enough to suggest answers. It borrows the long-armed look of brachiosaurids and flashes pelvic and vertebral traits that nod toward titanosaurs, yet refuses to commit to either identity. That half-and-half quality provides a valuable glimpse at titanosauriform experimentation—a snapshot of evolution in the act—and a reminder that Early Cretaceous localities like the Poison strip still have stories left to tell.
Venenosaurus, formally described in 2001, represents a gracile titanosauriform—a lightly built member of a group of long-necked plant-eating sauropods—from the Early Cretaceous, roughly 112 million years ago. Its partial skeleton—comprising vertebrae, limb bones, and pelvic elements—reveals a creature more lightly built than the barrel-bodied Camarasaurus, yet not as slender as Cedarosaurus, with which it shared its stratigraphic neighborhood. Its hand bones are long and slim, the forearms proportionally delicate, and the tail vertebrae display unusual side fossae (depressions or cavities). But unlike the fossae on most sauropods, which led to chambers for air-sacs to lighten their skeletons and enhance respiratory efficiency, these were merely deep depressions divided by internal ridges, hinting at a less specialized breathing system. The vertebrae also boast articulations not reported in any other sauropod.
In short, Venenosaurus is the kind of awkwardly gorgeous fossil that keeps paleontologists honest: fragmentary enough to provoke questions, rich enough to suggest answers. It borrows the long-armed look of brachiosaurids and flashes pelvic and vertebral traits that nod toward titanosaurs, yet refuses to commit to either identity. That half-and-half quality provides a valuable glimpse at titanosauriform experimentation—a snapshot of evolution in the act—and a reminder that Early Cretaceous localities like the Poison strip still have stories left to tell.
(Di Croce's Poison Strip Lizard)Etymology
Venenosaurus is derived from the Latin "venenum" (poison, for the Poison Strip Member of the Cedar Mountain Formation in Utah) and the Greek "sauros" (lizard).The species epithet, dicrocei (dee-KROH-chee-eye), honours Tony DiCroce.
Discovery
The remains of Venenosaurus were discovered at "Tony's Bone Bed" in the Poison Strip Sandstone Member of the Cedar Mountain Formation, Grand County, Utah, by Denver Museum of Natural History volunteer Tony DiCroce in 1998.
The holotype (DMNH 40932, housed at the Denver Museum of Natural History) includes nine tail (caudal) vertebrae, the left shoulder blade (scapula), right lower arm bone (radius), left lower arm bone (ulna), five hand bones (metacarpals), four finger bones (phalanges), a partial hip (right pubis, left and right ischia), some foot bones (metatarsals), plus chevrons and ribs. A partial juvenile specimen was found at the same site.
















