PP024-0012
Placing late Oligocene paleoclimate estimates for southern China into a modern climate framework

Thursday, 10 December 2020
Poster
Zachary Strasberg1, William E. Lukens1 and Brian Schubert2, (1)James Madison University, Geology and Environmental Science, Harrisonburg, VA, United States, (2)University of Louisiana at Lafayette, School of Geosciences, Lafayette, LA, United States
Abstract:
Paleoclimate records of Asian monsoons under times of elevated CO2 may help to predict future trends under anthropogenic climate change. Today, two monsoon systems influence the climate of southern China: the Indian monsoon (IM) and the East Asian monsoon (EAM). Whereas the IM is characterized by intense summer rainfall driven by the northward migration of the Inter-Tropical Convergence Zone (ITCZ) and intensified by the rain-shadow effect from the Tibetan Plateau (TP), the EAM is driven by uneven heating of the TP, with pressure reversals that advect moisture into the continental interior. Previous research suggests a pre-Miocene establishment of the IM; however, disagreements exist as to the presence of the EAM by this time. In this study, we place late Oligocene paleoclimate estimates from southern China into a modern climate framework to test for signatures of the IM vs. EAM in the Paleogene. We used the following paleoclimate estimates: 1) seasonal (6-month) rainfall from a proxy based on intra-ring δ13C variations in fossil evergreen wood from Nanning, China; 2) a range of mean annual precipitation (MAP) centered on 20th century values; 3) mean annual temperature (MAT) values from late Oligocene fossil floras in Nanning and Ningming. The estimated summer to winter precipitation ratio (Ps/Pw) from fossil wood is 5.3 (68% confidence interval of 2.5 to 11.1) consistent with a strong summer monsoon. Late Oligocene paleoclimate values were compared with records from 169 weather stations using the Euclidean distance formula and ranked to determine possible modern analogs for paleo-Nanning. Preliminary results suggest that paleo-Nanning had a climate similar to modern southern China, but cannot differentiate between the IM, EAM, or both systems. Future work will involve further sampling of fossil growth rings to better constrain paleo-Ps/Pw ratios and quantifying the sensitivity of paleo-MAT estimates on modern analog placement.