# New fossils imply a deeper origin of modern birds in the Mesozoic

## TL;DR

New fossil evidence suggests modern birds originated earlier in the Mesozoic era, challenging the idea that their diversification began after the K/Pg extinction.

## Contribution

The paper highlights new fossil discoveries that support a Cretaceous origin for modern bird lineages.

## Key findings

- Fossils from the Late Jurassic and Late Cretaceous periods indicate a deeper origin for modern birds.
- Major bird diversification likely occurred before the K/Pg boundary, during the Cretaceous Angiosperm Terrestrial Revolution.
- Phylogenomic studies and fossil data show discrepancies in divergence time estimates that need further investigation.

## Abstract

Macroevolutionary forces, such as rare catastrophes, have repeatedly disrupted and reset the evolutionary trajectories of Earth's major organismal groups. The Cretaceous–Paleogene (K/Pg) extinction event, approximately 66 Ma, resulted in the demise of ∼75% of all species at the time, yet despite its magnitude, many major organismal lineages successfully passed through this mass extinction. The evolutionary origins of modern birds (crown-group Aves) remain a subject of substantial debate, as they are often thought to have undergone their primary diversification following the K/Pg boundary. In this review, we summarize the various approaches that have been applied to understanding the timing of avian diversification. We examine the inferred divergence times derived from modern phylogenomic studies based on datasets comprising 50 to over 300 whole genomes. Additionally, we evaluate the factors contributing to the continued discrepancies in divergence time estimates. Furthermore, we discuss significant new fossil discoveries from the Late Jurassic and Late Cretaceous periods that reshape our understanding of key evolutionary events in early avian diversification. Taken together, the paleontological evidence increasingly supports a Cretaceous origin for many extant bird lineages, with the major burst of ordinal diversification likely occurring prior to the K/Pg boundary—concurrent with the early radiations of flowering plants, pollinating insects, mammals, fishes and other groups that characterized the Cretaceous Angiosperm Terrestrial Revolution.