bioRxiv Science⌕ Search

bioRxiv · 10.64898/2026.09.11.751023

NOTE ON RHEIFORMES (AVES: PALAEOGNATHAE) FROM A QUATERNARY CAVE IN THE LAGOA SANTA KARST, EASTERN BRAZIL

Abstract

Rheiformes are a South American lineage of large, flightless palaeognathous birds, currently represented by the genus Rhea and the two extant species R. americana and R. pennata. The fossil record of the group extends back to the Eocene, with its greatest diversification occurring during the Neogene. During the Quaternary, Rheiformes were widely distributed across southern and central South America. The Lagoa Santa region is particularly notable for its rich paleontological and archaeological record. Quaternary records of Rheiformes from caves in this region provide important evidence for understanding the distribution of the group in Brazil, although their chronological context remains uncertain owing to the absence of direct dating. Here, we describe and illustrate two rheiform bones recovered from a cave in the Lagoa Santa karst region. The material comprises a partially complete tibiotarsus and a fragmented tarsometatarsus, interpreted as belonging to a single individual. Comparative anatomical and morphometric analyses support their attribution to Rhea americana, based on morphological features and dimensions consistent with adult specimens of the species. This occurrence extends the Quaternary record of Rheiformes in the Lagoa Santa region and contributes to the fossil and subfossil record of Rhea in Brazil. The absence of stratigraphic and geochronological control precludes a precise age determination. Although the association with an extinct dasypodid indicates the presence of Late Pleistocene or Early Holocene faunal elements at the locality, a Holocene or even recent age for the rheiform remains cannot be excluded.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Chahud, A.. 2026-09-15. NOTE ON RHEIFORMES (AVES: PALAEOGNATHAE) FROM A QUATERNARY CAVE IN THE LAGOA SANTA KARST, EASTERN BRAZIL. https://doi.org/10.64898/2026.09.11.751023

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related preprints

Bone diagenesis in Iron Age Siberia: a histological and microtomographic study of Tunnug 1 (Russia, 2nd-4th c. CE)

The Siberian site of Tunnug 1, located in the Uyuk Valley (Tuva Republic, Russia), encompasses an Early Scythian burial mound (9th century BCE) and a peripheral cemetery attributed to the Kokel culture (2nd-4th centuries CE). Situated within a permafrost-affected environment, the site offers an opportunity to investigate bone preservation under long-term freeze-thaw cycle conditions and explore the relationship between funerary treatment and bone diagenesis. This study presents a combined histological and microtomographic analysis of 76 bone samples from 71 individuals across 36 burials. Transmitted light microscopy, scanning electron microscopy (SEM) and micro-computed tomography (micro-CT) were employed to document biological, chemical and physical degradation. Bone preservation was evaluated through three approaches: the traditional Oxford Histological Index (OHI), quantitative image analysis and assessment of (micro)cracking. The results revealed moderate bone preservation (OHI 2-4). Biological degradation in the form of Microscopical Focal Destruction (MFD) and chemical alteration were identified in six individuals. Enlarged canaliculi were observed in every bone sample. Microcracks were present in all individuals, visible exclusively under SEM. No clear diagenetic signatures linked to specific funerary practices were identified, though variations in preservation suggest a possible influence of burial depth. The distinct impact of permafrost and long-term freeze-thaw cycles on bone microstructure could not be isolated, underscoring the multifactorial nature of diagenesis. This study highlights the complementary value of combining multiple analytical methods assessing bone diagenesis and emphasises the need for continued experimental research into the effects of freezing environments on human remains.

paleontology↗

Nanoscale chemical tomography reveals organic and inorganic clusters in fossilised dinosaur tooth

Mineralized dental tissues are formed through biomineralization processes involving the growth and self-organisation of hydroxylapatite (HAP) nanoscale grains. There remain open questions regarding the way elements such as Mg or Na are incorporated in the organic matter between HAP grains or within the grain structure where they influence the nucleation and growth of HAP. Here, mapping the enamel structure and composition of a well-preserved ca. 150-million-year-old Giraffatitan brancai sauropod dinosaur tooth from millimeters down to the near-atomic scale, we reveal the nanoscale accumulation of Mg at HAP grain boundaries, alongside F arising from diagenesis. Within the HAP grains and at HAP grain boundaries organic matter forms clusters that we propose contribute to the fast growth rate of the tooth. Moreover, unexpected Cu3As particles are found across the entire enamel structure. These elements are not in the dentine, that exhibits empty tubules, which suggests that they were integrated during the tooth growth itself. Our multiscale analysis provides new information encouraging to reconsider aspects of the biomineralization and fossilization processes.

paleontology↗

Skeletal remains of a freshwater jalodontid chondrichthyan from the Upper Triassic Arden Sandstone Formation of Warwickshire, UK.

The Triassic was a significant period in the evolution of modern chondrichthyans (sharks, rays and chimaeras), bridging the gap between Paleozoic chondrichthyans and more recognizably modern Mesozoic forms. Although only a handful of Triassic skeletal fossils of chondrichthyans are known worldwide their calcified cartilages provide rare insight into their anatomy, evolution, and lifestyle. Here we use computed tomographic methods to describe six chondrichthyan skeletal fossils from the Carnian (Upper Triassic) Arden Sandstone Formation of Shrewley, Warwickshire, UK, consisting of a partial braincase, jaws, pectoral fin radials, caudal fin hypurals, and dorsal fin basal cartilages, and characterize their paleoenvironment. We assign the braincase and jaws, and tentatively assign the post-cranial remains, to the jalodontid taxon Keuperodus brodiei, previously described on the basis of teeth including those from the same locality. This represents the first known occurrence of articulated chondrichthyan skeletal remains from the Upper Triassic and the first interpretable cranial cartilages of the Order Jalodontiformes. The partial braincase of K. brodiei preserves an unusual basicranial circulation, almost completely embedded in the basicranium, and the jaws have an elongate extended shape; both features are akin to Paleozoic phoebodontid chondrichthyans. Phylogenetic analysis recovers K. brodiei as a stem-group elasmobranch with a close relationship to phoebodonts, one of several Paleozoic shark lineages to have independently survived the end-Permian mass extinction. However, unlike Phoebodontiformes and all other Jalodontiformes, K. brodiei occupied freshwater lake shorelines and associated fluvial feeder channels, revealing a possible freshwater refugium for Jalodontiformes towards at the end of their stratigraphic range.

paleontology↗