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Fossil Ammonites (Hoploscaphites & Sphenodiscus) - South Dakota
This is a 4.2" wide rock nodule that contains a JHoploscaphites (Jeletzkytes) spedeni ammonite and a small Sphenodiscus lenticularis ammonite, collected from the Fox Hills Formation of South Dakota. The largest ammonite is Jeletzkytes spedeni and it measures 3" wide. A wide variety of complete and fragmented shells can also be found throughout the rock.
There is a repaired crack through the largest ammonite and through what remains of the surrounding rock.
There is a repaired crack through the largest ammonite and through what remains of the surrounding rock.
About These Ammonites
These 70-million-year-old Cretaceous ammonite fossils come from a time when South Dakota was submerged beneath the Western Interior Seaway, a warm, shallow inland ocean that once stretched from the Arctic to the Gulf of Mexico. Ammonites were extinct marine cephalopods related to modern squid, octopus, and cuttlefish, but unlike their soft-bodied relatives, they lived inside coiled, chambered shells. As the animal grew, it added new chambers, using them to regulate buoyancy and move efficiently through the ancient seas. Their abundance and rapid evolution make ammonites some of the most important index fossils for dating marine rocks.
After death, these ammonites settled into seafloor sediments where mineral-rich waters slowly formed concretions around the shells, protecting them from crushing and decay for tens of millions of years. When these stone nodules are split open today, the fossils are revealed locked inside and must be carefully hand-prepared to remove the surrounding rock. This delicate, time-consuming process—often done with air scribes and fine tools—can take many hours per specimen, gradually exposing the shell’s ribs, sutures, and natural curvature. The finished fossils are striking remnants of South Dakota’s ancient ocean, preserving a moment from a world that vanished long before dinosaurs walked on land.
These 70-million-year-old Cretaceous ammonite fossils come from a time when South Dakota was submerged beneath the Western Interior Seaway, a warm, shallow inland ocean that once stretched from the Arctic to the Gulf of Mexico. Ammonites were extinct marine cephalopods related to modern squid, octopus, and cuttlefish, but unlike their soft-bodied relatives, they lived inside coiled, chambered shells. As the animal grew, it added new chambers, using them to regulate buoyancy and move efficiently through the ancient seas. Their abundance and rapid evolution make ammonites some of the most important index fossils for dating marine rocks.
After death, these ammonites settled into seafloor sediments where mineral-rich waters slowly formed concretions around the shells, protecting them from crushing and decay for tens of millions of years. When these stone nodules are split open today, the fossils are revealed locked inside and must be carefully hand-prepared to remove the surrounding rock. This delicate, time-consuming process—often done with air scribes and fine tools—can take many hours per specimen, gradually exposing the shell’s ribs, sutures, and natural curvature. The finished fossils are striking remnants of South Dakota’s ancient ocean, preserving a moment from a world that vanished long before dinosaurs walked on land.
SPECIES
Hoploscaphites (Jeletzkytes) spedeni & Sphenodiscus lenticularis
LOCATION
North Central, South Dakota
FORMATION
Fox Hills Formation
SIZE
Jeletzkytes ammonite 3" wide on 4.2 x 3.4" rock
CATEGORY
SUB CATEGORY
ITEM
#137273
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