Early to mid-Pleistocene ostracod δ 18O and δ 13C in the central Tibetan Plateau: Implication for Indian monsoon change

MLA

Jin, Zhangdong, et al. “Early to Mid-Pleistocene Ostracod δ 18O and δ 13C in the Central Tibetan Plateau: Implication for Indian Monsoon Change.” Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 280, no. 3/4, Sept. 2009, pp. 406–14. EBSCOhost, https://doi.org/10.1016/j.palaeo.2009.06.028.

APA

Jin, Z., Bickle, M. J., Chapman, H. J., Yu, J., Wang, S., & Chen, S. (2009). Early to mid-Pleistocene ostracod δ 18O and δ 13C in the central Tibetan Plateau: Implication for Indian monsoon change. Palaeogeography, Palaeoclimatology, Palaeoecology, 280(3/4), 406–414. https://doi.org/10.1016/j.palaeo.2009.06.028

Chicago

Jin, Zhangdong, Mike J. Bickle, Hazel J. Chapman, Jimin Yu, Sumin Wang, and Shiyue Chen. 2009. “Early to Mid-Pleistocene Ostracod δ 18O and δ 13C in the Central Tibetan Plateau: Implication for Indian Monsoon Change.” Palaeogeography, Palaeoclimatology, Palaeoecology 280 (3/4): 406–14. doi:10.1016/j.palaeo.2009.06.028.