Rhagor - Opening our national collections

Fossils in stone: acid preparation of fossils

[image: Gryphaea arcuata — Devil's toenails]

A limestone rock, from Southerndown in south Wales, containing fossil shells. (Gryphaea arcuata — Devil's toenails).

[image: Fossil shells (Gryphaea arcuata – Devil's toenails) after the rock has been dissolved in acid. ]

Fossil shells (Gryphaea arcuata – Devil's toenails) after the rock has been dissolved in acid.

[image: A fossil bivalve shell that has been partially prepared using acid]

A fossil bivalve shell that has been partially prepared using acid. The two parts of the shell (the valves) are still attached to each other, and the bottom valve is still attached to the rock.

We rarely find fossils in perfect condition. When we collect them, most of them are partially or almost completely concealed in rock. To study them in detail, or to prepare them to be displayed, we must carefully remove the rock.

It's not easy to remove the rock from the fossils, which are sometimes extremely delicate. It can be a long and painstaking process. Sometimes we use hand tools, like pins, scrapers or little chisels. We can also use specialist tools, like pneumatic pens similar to engraving devices. A third option is to use an air-abrasive machine that is little like a miniature sandblaster.

An alternative is to dissolve the rock in acid. Most fossil shells were composed originally of calcium carbonate, and many are preserved in limestone, which is the same chemical make-up. In some circumstances, however, the calcium carbonate of the shells dissolves away and is replaced by silica, but the enclosing limestone remains unchanged. Because limestone dissolves readily in acid, but silica doesn't, we can extract these specimens with chemicals.

Vinegar, no salt please

The acid we commonly use is acetic acid — the same acid that is in vinegar. We use highly concentrated acetic acid, 80%, but dilute it with water to about 5%.

We immerse the rock sample containing fossils in the diluted acetic acid, which almost immediately starts to fizz as it reacts with the limestone.

The rock can take anything from a few days to many months to dissolve completely, depending on its specific composition. The reaction with the rock gradually neutralizes the acid, which needs to be refreshed from time to time. At the end of the process all that remains is some slushy rock residue, and the silicified fossils.

Many silicified fossils are very delicate; they have to be handled with extreme care, and we often need to strengthen them with adhesives.

The fossils are now ready for research or for displaying. Many are exquisitely preserved: 450-million-year-old silicified shells sometimes look as if they have just been picked up from a modern beach!

Article by: Christian Baars, Technical Research Officer

Article Date: 7 June 2011

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