Stable isotope analysis of middle Miocene mammals from the Siwalik sub-Group of Pakistan

Acta Palaeontologica Polonica

Anthony Krupa¹  David L. Dettman¹  Jay Quade¹  Rana Manzoor Ahmad²  Amtur Rafeh³  Muhammad Tahir Waseem³  Abdul Majid Khan³ 

[1] Department of Geosciences, University of Arizona, Tucson AZ 85721, USA;Department of Zoology, University of Okara, Punjab 56300, Pakistan;Department of Zoology, University of the Punjab, Lahore 54590, Pakistan.;

关键词: mammalia;    paleoclimate;    paleodiet;    miocene;    chinji formation;    pakistan;   

DOI  :  10.4202/app.00788.2020

来源: DOAJ

【 摘 要 】

Stable isotope analysis is pivotal for investigating the paleodiet and paleoecology of past mammals. In this paper, we analyzed thirty fossil enamel samples belonging to the families Suidae, Rhinocerotidae, and Deinotheriidae for δ13Cenamel and δ18Oenamel composition to investigate paleodiet and paleoecology of middle Miocene mammals of the Siwalik sub-Group of Pakistan. The three mammalian groups, when combined together, yielded an average δ13Cenamel value of -12.2 ± 2‰, indicating a pure to nearly pure C3 diet. Suids show slightly higher δ13Cenamel values of -11.2 ± 1.4‰ when compared to rhinocerotids and deinotheres (-12.3 ± 0.8‰ and -12.5 ± 1.3‰, respectively), which could be explained by selective foraging on new leaf shoots or feeding from open spaces. Alternatively, the differences in δ13Cenamel could be due to different digestive physiologies and different enamel-diet enrichment factors. Members of all three families showed significant differences in δ18Oenamel values, where suids yielded higher δ18O values of -8.2 ± 1.2‰ compared to rhinocerotids and deinotheres (-11.4 ± 1.8‰ and -10.4 ± 1.7‰, respectively). Based upon these results, we assume that these mammals inhabited subtropical forests similar that of mid-Miocene of the Siwalik Group, India and Nepal. The modern analogues of such vegetation system are present in East and South of Myanmar, Nepal, and Malaya where precipitation is enough to support evergreen C3 forests. By contrast, today’s floodplain environments in Pakistan are dominated by C4 grasses, and C3 vegetation is only present in non-floodplain settings.

【 授权许可】

Unknown