The very smol-est orthocone cephalopod from the Ordovician Juab Formation of western Utah. If you look close you can see the chambers are variably filled with calcite cement and carbonate mud. You can also see the siphuncle toward the narrow end. ⚒️
The very smol-est orthocone cephalopod from the Ordovician Juab Formation of western Utah. If you look close you can see the chambers are variably filled with calcite cement and carbonate mud. You can also see the siphuncle toward the narrow end. ⚒️
This a block of limestone from the lower Fillmore Formation in western Utah filled with tons of Ordovician fossil goodness: trilobites, broyzoans, and criniods. ⚒️
This a block of limestone from the lower Fillmore Formation in western Utah filled with tons of Ordovician fossil goodness: trilobites, broyzoans, and criniods. ⚒️