|Antarcticoolithus bradyi |
Legendre, Rubilar-Rogers, Musser, et al., 2020
Illustration: Francisco Hueichaleo
Egg size and structure reflect important constraints on the reproductive and life-history characteristics of vertebrates. More than two-thirds of all extant amniotes lay eggs. During the Mesozoic era (around 250 million to 65 million years ago), body sizes reached extremes; nevertheless, the largest known egg belongs to the only recently extinct elephant bird, which was roughly 66 million years younger than the last nonavian dinosaurs and giant marine reptiles. Here we report a new type of egg discovered in nearshore marine deposits from the Late Cretaceous period (roughly 68 million years ago) of Antarctica. It exceeds all nonavian dinosaur eggs in volume and differs from them in structure. Although the elephant bird egg is slightly larger, its eggshell is roughly five times thicker and shows a substantial prismatic layer and complex pore structure. By contrast, the new fossil, visibly collapsed and folded, presents a thin eggshell with a layered structure that lacks a prismatic layer and distinct pores, and is similar to that of most extant lizards and snakes (Lepidosauria). The identity of the animal that laid the egg is unknown, but these preserved morphologies are consistent with the skeletal remains of mosasaurs (large marine lepidosaurs) found nearby. They are not consistent with described morphologies of dinosaur eggs of a similar size class. Phylogenetic analyses of traits for 259 lepidosaur species plus outgroups suggest that the egg belonged to an individual that was at least 7 metres long, hypothesized to be a giant marine reptile, all clades of which have previously been proposed to show live birth. Such a large egg with a relatively thin eggshell may reflect derived constraints associated with body shape, reproductive investment linked with gigantism, and lepidosaurian viviparity, in which a ‘vestigial’ egg is laid and hatches immediately.
Reptilia Laurenti, 1768 (sensu Modesto and Anderson, 2004)
Sauria Macartney, 1802 (sensu Rieppel and deBraga, 1996)
Oofamily, incertae sedis
Antarcticoolithus bradyi, oogen. and oospec. nov.
Etymology. Antarctic, referring to the continent where the specimen was discovered, Antarctica; oolithus, from Ancient Greek ōión for egg and líthos for stone; bradyi, from the Ancient Greek bradús for delayed or tardy, reflecting the 160 years between the description of the first Mesozoic egg from shallow marine deposits, Testudoflexoolithus bathonicae (Buckman, 1860), and that of this new ootaxon.
Holotype. SGO.PV 25.400, an almost complete fossil egg with infilled sediment (Fig. 1), permanently reposited at the Museo Nacional de Historia Natural, Santiago, Chile.
Locality and horizon. Late Cretaceous (roughly 68 Myr) of the López de Bertodano Formation (unit Klb; Supplementary Methods), Seymour Island, Antarctica.
Diagnosis. Antarcticoolithus bradyi is diagnosed by the following combination of characters: large size (29 cm × 20 cm, preserved length × width); eggshell thickness at least 700 μm and layered with a smooth undulating exterior surface; comparatively thin calcareous layer (roughly 100 μm); and complete lack of shell units and pores.
|An artist’s interpretation of a mosasaur, an extinct marine reptile that scientists think may have laid the egg. An adult mosasaur is shown next to the egg and a hatchling. |
Illustration: Francisco Hueichaleo
Lucas J. Legendre, David Rubilar-Rogers, Grace M. Musser, Sarah N. Davis, Rodrigo A. Otero, Alexander O. Vargas and Julia A. Clarke. 2020. A Giant Soft-shelled Egg from the Late Cretaceous of Antarctica. Nature. DOI: 10.1038/s41586-020-2377-7
Egg from Antarctica is Big and Might Belong to an Extinct Sea Lizard