Podocarpium (Leguminosae) is an extinct genus of Leguminosae widely documented in Cenozoic strata across Eurasia, but the lack of fossil evidence from key regions and critical time points limits the understanding of its evolutionary history and early dispersal patterns. In this study, we focus on the Early Oligocene Podocarpium of the Huatugou area in the western Qaidam Basin, located in the northeastern of the Qinghai-Tibet Plateau (QTP). Through detailed morphological observation and comparison, they are identified as a new species, named Podocarpium minicum C. Xie et D.-F. Yan sp. nov., characterized by irregularly oval pod shape, a sharply constricted apex, extremely small size, and the ratio of stipe/valve length ratio is more than 2. Based on the available fossil record, it is hypothesized that this genus may have originated in the Indian subcontinent. After migrating into the QTP, it underwent rapid radiation and further dispersed across Eurasia. The discovery of P. minicum sp. nov. suggests that the genus may have possessed relatively high diversity and a broad distribution in the Qaidam Basin. This fossil record reveals a potential “multi-track evolutionary mechanism” employed by the genus in response to environmental changes, while also reflecting that the EOT (Eocene–Oligocene Transition) may have indirectly influenced the climate of study area. This finding not only provides important evidence for understanding the evolutionary and distributional history of the genus but also offers further support for the hypothesis that it spread into Europe via a high-latitude route crossing the Turgai Strait.
扫码关注我们
求助内容:
应助结果提醒方式:
