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Spinal cord injury (SCI) often leads to persistent functional deficits due to loss of neurons and glia after injury. Hemisection spinal cord injury (HSCI) is a special type of SCI. The most important difference between HSCI and SCI is the occurrence of spinal cord dissection. Therefore, a calcium alginate hydrogel combined with dental pulp stem cells (DPSCs) and fibroblast growth factor 21 (FGF21) was designed based on the principle that cadherin expression is regulated by calcium ion concentration. Each element in Ca2+@Alg-FGF21 + DPSC hydrogel can exert different effects 1). calcium ions can regulate cadherin to achieve self-adhesion; 2). alginic acid can absorb calcium ions to prevent calcium overload induced injury; 3) FGF21 can regulate microenvironment; 4). DPSCs can supplement exogenous neurons. The multi-factorially comprehensive effects were hypothesized to improve the HSCI recovery. It was revealed in our study that Ca2+@Alg-FGF21 + DPSC hydrogel could effectively promote the recovery after spinal cord hemisection in mice via regulating apoptosis and autophagy, providing potential clues and cues of using Ca2+@Alg-FGF21 + DPSC hydrogel for HSCI treatment.

The loess–paleosol sequences in Shandong Province, East China, is an important aeolian archive, which can provide information for aeolian activity, palaeoclimatic change and sea level change in eastern coast of China since the last interglacial period. However, for so long, most of the studies about loess have been focused on the Chinese Loess Plateau, remaining many questions and disputes about the loess in East China. The Xianjingyuan (XJY) section on the TIA, Bohai Sea, is a representative aeolian section for islands off the eastern coast of China. In this study, optically stimulated luminescence (OSL) dating, particle size and magnetic susceptibility were applied to date and analysis the loess–paleosol sequences in this section. The results show that: (1) The OSL ages at the depths of 0.8 m, 2.5 m, and 3.9 m are 12.6 ± 1.0 ka, 19.2 ± 1.1 ka and 56.9 ± 2.6 ka, respectively, and the loess started to accumulate at ca. 86.5 ka according to the depositional rates (2) The loess accumulated mainly during the Marine Isotope Stage (MIS) 2, i.e., Last glacial maximum and deglaciation, MIS4 and MIS3b with higher depositional rate, coarser grain size, and higher magnetic susceptibility; while paleosol mainly developed during MIS3a, MIS3c and MIS5 with lower depositional rate, finer grain size and lower magnetic susceptibility. (3) The palaeoclimatic changes and aeolian sediments evolution were mainly controlled by the changes of East Asian summer monsoon and sea levels.