Oligocene Desmanthus (Leguminosae) from the Qaidam Basin in northeastern Tibetan Plateau, China, and its implications for paleoclimate and paleoelevation. (2nd November 2021)

• Record Type: Journal Article
• Authors: Yang, Tao; Han, Lei; Chen, Hongyu; Wang, Yong; Wang, Haojian; Bao, Lin; Li, Wenjia; Cai, Jiahao; Liang, Weiyu; Dai, Yanzhi; Zhang, Li; Xie, Sanping; Yan, Defei
• Is Part Of: Historical biology. Volume 33:Number 11(2021)
• Page Start: 2744
• Page End: 2754
• Publication Date: 2021-11-02
• Subjects: Tibetan Plateau -- Qaidam Basin -- fossil pods -- Oligocene -- paleoclimate; Paleobiology -- Periodicals; Biology -- Periodicals; Evolution -- Periodicals; Paleontology -- Periodicals; Biology -- Periodicals; Paleontology -- Periodicals; Evolution -- Periodicals; 560.5
• DOI: 10.1080/08912963.2020.1826471
• Languages: English
• ISSNs: 0891-2963

Abstract

ABSTRACT: Fossils are critical for understanding the environmental changes and uplift history of the Tibetan Plateau during the Cenozoic. As the largest inland basin located at the northeastern plateau, Qaidam Basin has been regarded as the key region to understand the climatic changes in the plateau during the Cenozoic. Herein, fossil legumes from the Oligocene Shangganchaigou Formation in northwestern Qaidam Basin have been reported and are assigned to Desmanthus cf. virgatus (L.) Willd. based on morphological comparison. Current materials represent the first megafossil record of this genus in the world. The living analogues of current fossils now live in regions with mean annual temperature values (MAT) ranging from 13.4 to 29.1°C and mean annual precipitation values (MAP) ranging from 36 to 2874 mm while the MAT and MAP of current northwestern Qaidam Basin is −1.03°C and 60.5 mm, respectively, and indicate that the Oligocene Qaidam was much warmer than today. We calculate that current fossils could grow no higher than 2492 m considering the climatic condition of the Oligocene Qaidam. The difference between estimated and modern elevation of the fossil site suggests that the elevation of the research area has increased by at least ≈1000 m since the Oligocene.