Chemical characterization of pterosaur melanin challenges color inferences in extinct animals.

Melanosomes (melanin-bearing organelles) are common in the fossil record occurring as dense packs of globular microbodies. The organic component comprising the melanosome, melanin, is often preserved in fossils, allowing identification of the chemical nature of the constituent pigment. In present-day vertebrates, melanosome morphology correlates with their pigment content in selected melanin-containing structures, and this interdependency is employed in the color reconstruction of extinct animals.

Probing the surface calcium binding sites of melanosomes using molecular rulers.

Melanosomes have the capacity to bind significant concentrations of calcium, suggesting there are surface binding sites that enable cations to access the interior of fully pigmented melanosomes. The surface of melanosomes is known to contain significant concentrations of carboxylate groups which likely are the initial biding sites for calcium, but their arrangement on the surface of the melanosome is not known. In various calcium proteins, a bidentate coordination by two carboxylate groups is the most common structure.

Near-infrared excited state dynamics of melanins: the effects of iron content, photo-damage, chemical oxidation, and aggregate size.

Ultrafast pump-probe measurements can discriminate the two forms of melanin found in biological tissue (eumelanin and pheomelanin), which may be useful for diagnosing and grading melanoma. However, recent work has shown that bound iron content changes eumelanin's pump-probe response, making it more similar to that of pheomelanin. Here we record the pump-probe response of these melanins at a wider range of wavelengths than previous work and show that with shorter pump wavelengths the response crosses over from being dominated by ground-state bleaching to being dominated by excited-state absorption.

Pump-Probe Microscopic Imaging of Jurassic-Aged Eumelanin.

Melanins are biological pigments found throughout the animal kingdom that have many diverse functions. Pump-probe imaging can differentiate the two kinds of melanins found in human skin, eumelanin and pheomelanin, the distributions of which are relevant to the diagnosis of melanoma. The long-term stability of the melanin pump-probe signal is central to using this technology to analyze melanin distributions in archived tissue samples to improve diagnostic procedures.

High-performance liquid chromatography estimation of cross-linking of dihydroxyindole moiety in eumelanin.

Eumelanin pigments consist of various ratios of 5,6-dihydroxyindole-2-carboxylic acid (DHICA) and 5,6-dihydroxyindole (DHI). On alkaline hydrogen peroxide oxidation, these indole moieties give rise to pyrrole-2,3,5-tricarboxylic acid (PTCA) and pyrrole-2,3-dicarboxylic acid (PDCA), respectively. In a recent study, we detected considerable amounts of other pyrrole acids, pyrrole-2,3,4,5-tetracarboxylic acid (PTeCA) and pyrrole-2,3,4-tricarboxylic acid (isoPTCA), among the oxidation products of fossil ink sacs more than 160 million years old.

Direct chemical evidence for eumelanin pigment from the Jurassic period.

Melanin is a ubiquitous biological pigment found in bacteria, fungi, plants, and animals. It has a diverse range of ecological and biochemical functions, including display, evasion, photoprotection, detoxification, and metal scavenging. To date, evidence of melanin in fossil organisms has relied entirely on indirect morphological and chemical analyses.