C-iTRACE

Please cite the three papers below according to your usage of CiTRACE: Gu et al., 2019, describes the physical variables and the d18O in CiTRACE. Gu et al., 2020, describes multiple isotopes at the Last Glacial Maximum in CiTRACE Gu et al., 2021, describes carbon isotopes during the deglaciation in CiTRACE. Gu, S., Liu, Z., Lynch‐Stieglitz, J., Jahn, A., Zhang, J., Lindsay, K., & Wu, L. (2019).

Assessing the Ability of Zonal d18O Contrast in Benthic Foraminifera to Reconstruct Deglacial Evolution of Atlantic Meridional Overturning Circulation. Paleoceanography and Paleoclimatology, 34(5), 800–812.doi.org/10.1029/2019PA003564 Gu, S., Liu, Z., Oppo, D. W., Lynch-Stieglitz, J., Jahn, A., Zhang, J., & Wu, L. (2020). Assessing the potential capability of reconstructing glacial Atlantic water masses and AMOC using multiple proxies in CESM.

Earth and Planetary Science Letters, 541, 116294. doi.org/10.1016/j.epsl.2020.116294" Gu, S., Z. Liu, D. W. Oppo, J. Lynch-Stieglitz, A. Jahn, J. Zhang, K. Lindsay & L. Wu (2021), Remineralization dominating the δ13C decrease in the mid-depth Atlantic during the last deglaciation, in revision for Earth and Planetary Science Letters.