For long stretches of the Paleozoic Era, roughly 340 to 270 million years ago, the Tucson area sat near the equator under shallow seas. Layer after layer of lime mud and shell debris piled up on those sea floors and hardened into the thick gray limestones you can now trace along the flanks of the Catalinas, Rincons, and the ranges just outside Tucson.
The cast of characters preserved in those Tucson-area limestones is consistent and, once you learn it, easy to spot:
- Crinoids — "sea lilies," animals on stalks built from stacked disc segments. Weathered-out stem pieces look exactly like stone Cheerios, and they are far and away the most common fossil around Tucson.
- Brachiopods — ribbed, clam-like shells, often preserved whole in the rock face.
- Horn corals — solitary corals shaped like curved ice cream cones, showing internal ribbing in cross-section.
- Bryozoans — colonial animals leaving delicate fan and mesh patterns in the stone.
Much later, in the Cretaceous, rivers and floodplains crossed southern Arizona, and a few formations from that world have produced rare dinosaur material. Rare is the operative word — the everyday fossils around Tucson are marine, and they're wonderful.