Evaluation of Cretaceous Hinterland Weathering and Climate in the Sichuan Basin, SW China ()
1. Introduction
Reconstruction of the Cretaceous paleoclimate is important for the understanding of the Earth operating system during the greenhouse conditions. However, paleoclimatic information from continental inland-basins is scarce compared to that from continental margin marine-basins. This situation is also true in the Asian continent; Cretaceous ecosystem and paleoclimate data are accumulating in the Pacific side, while those of the Asian continental side are lacking [1] . Paleoclimate conditions in Asian inland basins are considered to be equally important in order to elucidate the land-ocean climate operating system during the Cretaceous.
In this regard, we investigated the geochemistry and clay mineralogy of the Cretaceous mudstones from the Sichuan Basin, southwestern China, for the aim of paleoclimate evaluation.
2. Geological Setting and Sampling
The Sichuan Basin is located in the western South China Block, where the Cretaceous strata are widely distributed [2] . The depositional age of studied strata ranges from Berriasian to Maastrichtian. Sediments are mostly fluvial to lacustrine origin, however, a broad distribution of aeolian dune sandstones was identified from the Cenomanian to Turonian interval [2] . 50 mudstone samples were collected from the five Cretaceous formations in the Sichuan Basin, covering the Berriasian to Maastrichtian stages. We exclusively sampled fine-grained massive mudstones in order to exclude compositional changes due to the grain-size effect.
3. Analytical Methods
Samples were pulverized using agate motor mill and fused beads were prepared for XRF analysis (ZSX Primus 2; Rigaku, Tokyo, Japan). The whole-rock major element composition acquired by XRF was used to calculate the W index [3] in order to evaluate the hinterland paleoweathering condition. Clay-mineral composition and illite crystallinity were obtained by XRD (SmartLab XRD, Rigaku, Tokyo, Japan). Oriented glass slides of clay minerals finer than 2 μm fraction were prepared for the XRD measurement.
4. Result and Discussion
Geochemical weathering indices (e.g., W value; [3] ) demonstrate a significant increase in hinterland paleoweathering from Berriasian (W = 70) to Cenomanian – Turonian (W = 95), and then slightly decrease towards the Maastrichtian (W = 80). This fluctuation pattern of the weathering indices is concordant with the Cretaceous paleotemperature reconstruction curve [4] . Therefore, the present result suggests that the hinterland paleoweathering rate in the Sichuan Basin was governed by global temperature changes. The weathering index reached the maximum value of 95 in Cenomanian-Turonian interval. Furthermore, sediments of Cenomanian-Turonian horizons contained abundant kaolinite mineral, which is a product of hydrolysis decomposition of rock-forming minerals. Both lines of evidence suggest that the Sichuan Basin was under the tropical and pluvious climate during the Cenomanian-Turonian. Note that previous study elucidated an arid climate from amalgamated sandstone facies [2] , while the present pluvious climate interpretation is derived from the analysis of intervening piled mudstone facies. When these lines of geological evidence are integrated together, it is reasonable to suggest the development of an alternating pluvious and arid paleoclimate during the Cenomanian-Turonian. The nature and trigger of this extremely oscillating pluvious/arid climate cannot be deduced solely from the present study. However, the timing of this renewed climate system matches with the Cretaceous greenhouse optimum (Cenomanian-Turonian). The development of monsoon-like pluvious/arid paleoclimate in the Sichuan Basin is possibly related to the mid-Cretaceous re-configuration in the global climate system.
5. Conclusion
In this study, the hinterland paleoweathering conditions in Sichuan Basin through the whole Cretaceous were reconstructed. We found that the fluctuation in hinterland paleoweathering intensity is highly positively correlated with the estimated global temperature trend. Therefore, the paleoweathering rate might be controlled by the global temperature. Furthermore, the present result suggests that mudstone facies intercalated in the aeolian sandstone facies record high rates of hinterland weathering intensity. The alternating mudstone and sandstone facies imply the oscillating pluvious/arid paleoclimate during the Cenomanian-Turonian greenhouse optimum.
Acknowledgements
This work was supported by JSPS (18K03787; T. Ohta), Strategic Priority Research Program of Chinese Academy of Sciences (XDB26000000) and NSFC (41572006, 41688103, 41972007). Thanks go to Prof. Y. Ogasawara of Waseda University and Mr. S. Yasutake for their help. This is a contribution to UNESCO/IUGS/IGCP 679.