Calcium is abundant, which means that people in the past figured out some great ways to use it as tools, decoration, and, of course, pottery. In nature, we typically find calcium bound in carbonate minerals, which also contain carbon and oxygen. The limestone bedrock of Florida and the Bahamas is carbonate, and so are coral, the shells of oysters, conch, and other shellfish.

Crushed shell (Pensacola series pottery)
Crushed shell (Pensacola series pottery)
Cross section of sherd showing shell temper
Cross section of sherd showing shell temper

In the past, crushed shells, limestone, and bone have been used as tempering materials for pottery, especially in places where there isn’t much other “hard stuff” around. In the Southeastern US, they were used specifically to make cooking pots, because the clay and the calcium minerals expand the same amount when heated. This is important to avoid cracks in your cookware.

Crushed limestone (Pasco and Perico series pottery)
Crushed limestone (Pasco and Perico series pottery)
Perico Incised (Perico series)
Perico Incised (Perico series)

But, and it’s a big but, calcium minerals are tricky to work with. This is because above around 700°C, the calcium carbonate (CaCO3) converts into quicklime (CaO) and carbon dioxide (CO2). Quicklime is softer than calcium carbonate, so an overfired pot will feel light and fragile. Here’s an example showing how shell temper inclusions change with increasing temperature, with a major difference between 600°C and 700°C. Notice how the shell particles are more visible in the top two briquettes, both whiter and larger. Aside from temperature, the briquettes are identical. We usually think that hotter is better to make a stronger pot, but in this case it’s the opposite.

stack of briquettes ranging from unfired clay to 800 degrees celsius. The inclusions 600 and below are brownish/gray, and above 700 are white and larger
Stack of red clay briquettes with shell temper, replicating Bahamian Palmetto Ware

Most devastating, quicklime readily combines with water, including the water suspended in our humid Florida air. Over time, that means that the quicklime particles begin to expand, taking on water. As they grow, they become more fragile and cracks begin to form. In the most severe cases, you’re left with a pile of dust. Here’s a clay that naturally contained a lot of calcium carbonate, but didn’t have tempering added:

showing disintegration calcium-rich pottery over time
Calcium-rich pottery fired hot enough to convert CaCO3 particles to quicklime (CaO) will disintegrate quickly

In bad news for archaeologists, even low-fired carbonate tempered pottery doesn’t always preserve well. This is because the calcium (which is basic), gets eroded over time from acidic conditions in the ground or water. Notice in most of these limestone tempered sherds how there are holes where the temper used to be:

Pasco Plain
Pasco Plain

Despite these limitations, potters 1000 years ago figured out how to use shell and limestone to their advantage, engineering pots that would be strong for cooking or other activities, and showing deft control over very tricky firing conditions, without the benefits of modern thermometers. Truly remarkable.

7 sherds with straight and curvilinear incisions
Pensacola Incised, rims (Alabama)

Here’s our recent foray into shell-tempered pottery making: Clay Chronicles VI