Abstract
Carmine is a red pigment made from dried cochineal, a scale insect that has been a source of brilliant scarlet
reds in clothing and art for more than two millennia, with records dating back to 700 BC. Since the 16th century,
it has been intensely traded all over the world and was one of the most important trade goods for the Spanish
empire at its economic peak. Despite still being used on an industrial scale, with hundreds of metric tonnes
produced annually, the exact molecular and crystal structure of the dyestuff remains undetermined. Notably,
both modern-day commercial carmine and pigments prepared following historical recipes show strikingly
similar diffraction patterns, indicating a common crystalline structure. Several model structures of carmine have
been proposed, and so far spectroscopic measurements have hinted at a tetrameric complex containing the
conjugate base of carminic acid, aluminium ions, and calcium ions. Considering its commercial and historical
significance, determining the structure and composition of carmine would aid in both modern-day regulation
and identification in historical samples. Here we show that the crystal structure of carmine can at last be
determined using three-dimensional electron diffraction measurements. Our investigation reveals that carmine
is indeed comprised of a tetrameric complex, that assembles into a nanoporous supramolecular structure with pore diameters of approximately 1.8 nm, held together by intermolecular hydrogen bonding. Our results
establish a definite structure of carmine, unveiling a surprisingly complicated arrangement in a product that has
been traded around the world for centuries. We anticipate that this study will prompt further investigations of
age-old crystalline compounds and formulations using state-of-the-art electron crystallography methods, while
also highlighting the serendipitous creation of a man-made supramolecular material that dates back thousands
of years.