Natural Science in Archaeology
Natural Science in Archaeology
Natural Science in Archaeology
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216 9 Pigments and Colorants<br />
Central Asia (Gettens and Stout 1966). Pl<strong>in</strong>y notes the medic<strong>in</strong>al uses of orpiment<br />
(N.H. 34.56). The name comes from the Lat<strong>in</strong> auripigmentum mean<strong>in</strong>g golden pa<strong>in</strong>t.<br />
The orpiment used <strong>in</strong> ancient Egypt likely came from Persia.<br />
Realgar. The m<strong>in</strong>eral realgar, AsS, is a soft (H = 1.5–2), naturally occurr<strong>in</strong>g redorange<br />
pigment. The name comes from the Persian rahj al ghar. It was used as a<br />
cosmetic by the Akkadians (Forbes III 1965). Pl<strong>in</strong>y notes the medic<strong>in</strong>al uses of<br />
realgar and its occurrence <strong>in</strong> gold and silver m<strong>in</strong>es (N.H. 34.55). Both orpiment and<br />
realgar pigments break down on exposure to light. Orpiment whitens to arsenolite<br />
(As 2 O 3 ), and realgar changes to yellow to orange pararealgar. A pot of realgar was<br />
found <strong>in</strong> fourth century BCE ru<strong>in</strong>s at Cor<strong>in</strong>th, Greece. In Ch<strong>in</strong>ese alchemy, realgar<br />
(but not orpiment) had some importance.<br />
There is a related m<strong>in</strong>eral called pararealgar, AsS, which is thought to be a light<strong>in</strong>duced<br />
phase <strong>in</strong>version of realgar. There is some concern among art conservators<br />
regard<strong>in</strong>g its presence on pa<strong>in</strong>t<strong>in</strong>gs s<strong>in</strong>ce it is not known if it was an orig<strong>in</strong>al or<br />
altered color (Corbeil and Helwig 1995).<br />
C<strong>in</strong>nabar/Vermillion. C<strong>in</strong>nabar (HgS) has been used as a red pigment s<strong>in</strong>ce<br />
about 1500 BCE. It has been called “vermillion”, derived from the Lat<strong>in</strong> “vermes”,<br />
an <strong>in</strong>sect that was used to prepare a red dye. Theophrastus reported two types of c<strong>in</strong>nabar,<br />
likely true c<strong>in</strong>nabar plus red lead. Pl<strong>in</strong>y knew about c<strong>in</strong>nabar but confused the<br />
issue by call<strong>in</strong>g it “m<strong>in</strong>ium”. He knew the Roman supply came from Spa<strong>in</strong>, likely<br />
the m<strong>in</strong>es of Almaden. Ancient Ch<strong>in</strong>a also had an adequate supply of c<strong>in</strong>nabar.<br />
Mercury sulfide (c<strong>in</strong>nabar) was extracted from silver m<strong>in</strong>es dur<strong>in</strong>g antiquity. Red <strong>in</strong><br />
color, c<strong>in</strong>nabar was apparently used from the earliest periods. C<strong>in</strong>nabar is sensitive<br />
to light, and the color blackens over time. C<strong>in</strong>nabar has been found <strong>in</strong> a funerary sett<strong>in</strong>g<br />
at a 5000-year-old site <strong>in</strong> Spa<strong>in</strong>. It has also been discovered on human rema<strong>in</strong>s<br />
found <strong>in</strong> Peru dat<strong>in</strong>g from about 900–1000 CE (Mart<strong>in</strong>-Gil et al. 1995). Accord<strong>in</strong>g<br />
to Pl<strong>in</strong>y, the Romans regarded c<strong>in</strong>nabar with great importance and sacred associations.<br />
He quotes Verrius who “gives a list of writers of unquestionable authority<br />
who say that on holidays it was custom for the statue of Jupiter himself to be colored<br />
with c<strong>in</strong>nabar, as well as the bodies of persons go<strong>in</strong>g <strong>in</strong> triumphal procession” (N.H.<br />
33:36). Roman women used c<strong>in</strong>nabar as a cosmetic. C<strong>in</strong>nabar was called “m<strong>in</strong>ium”<br />
by Vitruvius, not to be confused with the lead oxide of the same name. In addition<br />
to Spa<strong>in</strong> and Peru, c<strong>in</strong>nabar was m<strong>in</strong>ed <strong>in</strong> Mexico, Egypt, Greece, and Ch<strong>in</strong>a.<br />
Stibnite. Stibnite (Sb 2 S 3 ), sometimes called antimonite, is a fairly soft (H = 2)<br />
m<strong>in</strong>eral often used as a pigment and colorant <strong>in</strong> antiquity. It is lead-gray to dark<br />
gray. It is known to have been used as an eye pa<strong>in</strong>t <strong>in</strong> ancient Egypt and <strong>in</strong>to the<br />
Classical Period (Forbes III 1965). The Romans may have also used roasted stibnite<br />
as a glass colorant and opacifier (Mass et al. 1997).<br />
9.9 Carbonates<br />
Calcium Carbonate. Calcium carbonate, CaCO 3 , occurs <strong>in</strong> a wide variety of m<strong>in</strong>eral<br />
sett<strong>in</strong>gs <strong>in</strong>clud<strong>in</strong>g calcite ve<strong>in</strong>s, limestone, chalk, mollusk shells, and coral.<br />
The name calcite comes from the Lat<strong>in</strong> word calx for lime. In a Bronze Age Greek