ICG2022-279, updated on 20 Jun 2022
10th International Conference on Geomorphology
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Age and source of coastal loess in the Shandong Peninsula, Bohai Sea, China

Xiaodong Miao1, Chongyi Ee2, Shujian Xu1, Qiansuo Wang3, Paul Hanson4, Haitao Chen1, and Yunkun Shi2
Xiaodong Miao et al.
  • 1School of Resource and Environmental Sciences, Linyi University, Linyi 276000, China (miaoxiaodong@lyu.edu.cn)
  • 2School of Geographic Science, Qinghai Normal University, Xining 810008, China
  • 3School of Land and Tourism, Luoyang Normal University, Luoyang 471934, China
  • 4School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE 68583, USA

Coastal loess is a unique and intriguing eolian sediment on Earth, but understanding its formation time, provenance, composition and the geomorphic processes that resulted in its accumulation is very limited compared to its inland counterpart. In this paper, we focused on a loess section at Xiazhupan (XZP) Village, Penglai City in the Shandong Peninsula, the only known coastal loess bluffs preserved in China. The coastal loess here not only has characteristics that are common to loess terrains such as being composed of predominantly silt-sized particles and the tendency to stand in vertical exposures, but it also reportedly preserves planktonic foraminifera, sizable pebbles, and volcanic glass. In addition to its peculiar near-shore locality, these features make it more unusual compared to other loess deposits. Systematic optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL and pIRIR) and radiocarbon dating reveal it was deposited mostly during 60-20 ka, Marine Isotope Stage (MIS) 4-2, which correlates to the deposition of the Malan loess (L1) in the Chinese Loess Plateau. High-resolution grain size data indicate that the coastal loess is relatively coarse-grained, suggesting a source terrain that is at least partially proximal. We argue that, given its proximal source and the geochronological evidence, this coastal loess was sourced from the exposed continental shelf during the sea-level lowstand of the last glacial period, and this hypothesis is further supported by a core collected from the Bohai Sea in which silt was present and would have been subaerially exposed during MIS 4-2. In addition, this source area of the exposed continental shelf is comparable to coastal loess in Europe. The coastal loess in Shandong can be regarded as a special type of desert or dryland loess, rather than glacial loess. Finally, future sea-level rise will likely increase the erosion potential of these vulnerable coastal loess bluffs, making it urgent to study this special landform.

How to cite: Miao, X., Ee, C., Xu, S., Wang, Q., Hanson, P., Chen, H., and Shi, Y.: Age and source of coastal loess in the Shandong Peninsula, Bohai Sea, China, 10th International Conference on Geomorphology, Coimbra, Portugal, 12–16 Sep 2022, ICG2022-279, https://doi.org/10.5194/icg2022-279, 2022.