Greenhorn Limestone

were cut from a layer in the Greenhorn. The formation was named for the Greenhorn Station on Greenhorn Creek in Colorado in 1896 by Grove Karl Gilbert; In Kansas, the Greenhorn Formation is divided into the (lowest) Lincoln Limestone, Hartland Shale, Jetmore Chalk, and (highest) Pfeifer shale members, each noted by changes in chalkiness and limestone rhythmite patterns. In eastern Colorado and western Kansas Hydrocarbon exploration, the divisions are Lincoln Limestone, Hartford Shale, and Bridge Creek Limestone. In other states, where the formation is less developed, the unit is not subdivided and is named the Greenhorn Limestone, as a formation or as a member of another formation, e.g., Cody Shale, Colorado Shale, and Mancos Shale. Within Kansas and a small neighboring portion of Nebraska, the Greenhorn Formation is particularly noted for its uppermost bed, the Fencepost limestone, from which the Kansas stone posts were quarried. The combination of the toughness of the Fencepost limestone with the softness of the chalk and shale above and below as resulted in the formation of the main range of the Smoky Hills north and west of Salina. In 2018, Kansas Legislation HB 2650 designated the Greenhorn Limestone formation, specifically "the famous "post rock" limestone" bed of that unit, to be the state rock of Kansas. == Lithologic character ==

road cut shows the chalky rhythmites of the formation. The Greenhorn Formation is characterized as shale to chalky shale, light bluish-gray in color, with rhythmically repeating beds of chalk or limestone that become marly closer to the Rocky Mountains. The shale can weather to buff color under hilltops. Exposures show many thin, rust-colored bentonite beds (named for the Old Benton Limestone classification that the Greenhorn and other names replaced), several of which are consistent and widespread marker beds. These orange seams in the weathered shale and the yellow/orange stainings of some of the weathered limestones in the Greenhorn are associated with volcanic events in the Sevier orogeny. The oceanic iron (Fe) and volcanic sulfur (S) that precipitated with the volcanic ash into the calcareous mud (CaCO3) formed pyrite (FeS2), which later altered to selenite (CaSO4·2H2O), siderite (FeCO3), and limonite (FeO(OH)·nH2O), leading to the yellow to orange staining. == Paleofauna ==

The formation is recognized for its sequence of index fossils, including oysters, Ammonoidea, Belemnitida, and Inoceramidae. • Ammonoidea and Belemnitida were common, free-swimming pelagic predators, reflecting abundant fish populations in a broad sea. • The occasionally low oxygen bottom was soft mud to which the broad, flat Inoceramidae were particularly adapted. These stationary filter feeders are evidence of currents sufficient to carry enough food to support such very large invertebrates, but not so strong as to suffocated them with drifting mud. • Oysters are smaller filter feeders. Several species were common. Larval oysters require clear, mud-free hard surfaces to attach and develop into mature oysters. Ostrea congesta was particular for colonizing the top valve of large Inoceramidae and oyster-encrusted shell fragments litter slopes of eroded Greenhorn. • In 2022, Schumacher & Everhart described Plesioelasmosaurus based on a partial skeleton previously known as the "Holyrood elasmosaur" from the Greenhorn Limestone (Lincoln Limestone Member, Calcarenite beds). The Greenhorn marine cycle was the deepest and broadest stage of the Western Interior Seaway, and supported large sharks and the largest of marine reptiles, including Mosasauridae and Pliosauroidea. Fossilized driftwood and dinosaur remains have been recovered from the formation; such remains are presumed washed into the sea by rivers swollen by the heavy rainfalls of the hothouse Cretaceous. File:Styxosaurus and Xiphactinus.jpg| Paleoart depicting two large marine predators of the late Cretaceous; Elasmosauridae and Xiphactinus. == See also ==