No abstract

Screening pigments are essential for vision in animals. Vertebrates use melanins bound in melanosomes as screening pigments, whereas cephalopods are assumed to use ommochromes. Preserved eye melanosomes in the controversial fossil Tullimonstrum (Mazon Creek, IL, USA) are partitioned by size and/or shape into distinct layers. These layers resemble tissue-specific melanosome populations considered unique to the vertebrate eye. Here, we show that extant cephalopod eyes also show tissue-specific size- and/or shape-specific partitioning of melanosomes; these differ from vertebrate melanosomes in the relative abundance of trace metals and in the binding environment of copper. Chemical signatures of melanosomes in the eyes of Tullimonstrum more closely resemble those of modern cephalopods than those of vertebrates, suggesting that an invertebrate affinity for Tullimonstrum is plausible. Melanosome chemistry may thus provide insights into the phylogenetic affinities of enigmatic fossils where melanosome size and/or shape are equivocal.

Brightly coloured feathers, including the brilliant reds produced by carotenoids, are sometimes shiny in appearance. Gloss is a common property of materials and usually arises through specular reflection from smooth, flat surfaces. However, the production of gloss on red feathers has never been examined. In the present study, we compared the optical and structural properties of glossy and matte carotenoid-based red feathers of multiple species to identify the proximate basis for their glossiness. Although specular reflectance did not differ between glossy and matte feathers, diffuse reflectance was lower in glossy than in matte feathers, leading to a higher contrast gloss. Compared to matte feathers, glossy red feathers had thicker barbs with a flatter and more homogeneous morphology, consistent with expectations, as well as thicker outer keratin cortices. Moreover, glossiness was predicted by a principal component regression using these same morphological traits. We demonstrate that the gloss of carotenoid-based red feathers is produced at least in part by a smooth, flattened barb microstructure and an enhanced nanostructure, illustrating a novel colour-producing interaction that neither pigment, nor microstructure could alone attain. How the ecology and evolution of species with glossy red feather differ from those with typical matte red feathers represent rich areas for future study.

Biological interactions are rarely preserved in the fossil record and where they do occur, are often difficult to discern. Therefore, the evolution of sexual systems over geologic time in animals has been difficult to investigate. The reproductively labile Spinicaudata ('clam shrimp') are a model clade for the study of sexual systems, containing dioecious (males and females), androdioecious (males and hermaphrodites) and self-fertilizing hermaphrodites. Herein we present a methodology in which mating systems can be inferred by the quantification of carapace shape differences attributable to sexual dimorphism in fossil specimens. We develop our methodology by comparing the carapaces of six species from two families of extant Spinicaudatans using eigenshape analyses. Sexual dimorphism was successfully quantified using morphometric techniques combined with discriminant analyses, correctly identifying males and females/hermaphrodites 92% of the time in extant taxa. Thirty-four specimens of the Jurassic clam shrimp Carapacetheria disgragaris were analyzed utilizing the methods developed with extant species. From these fossil data, we were able to detect two distinct carapace shapes and assign 100% of individuals to either shape. The mean carapace shapes of the fossil specimens fit well with the average outlines for males and females in the extant species, enabling us to calculate a sex ratio of 51:49 males:females and thereby assign the sexual system of dioecy. This study begins to successfully utilize the fossil record of the Spinicaudata to elucidate ancient sexual systems, which will likely have far reaching implications for our understanding of the evolutionary dynamics of sexual systems over geologic timescales.