Associative learning is common way for information acquisition. Associative memory is essential to logical reasoning and associative thinking. The storages of multiple associated signals in individual neurons facilitate their integration, expand memory volume, and strengthen cognition ability. Associative memory cells that encode multiple signals have been reported, however, the mechanisms underlying their recruitment and working principle remain to be addressed. We have examined the recruitment of associative memory cells that integrate and store triple sensory signals as well as the potential mechanism of their recruitment. Paired mouse whisker, olfaction, and tail stimulations lead to odorant-induced motion and tail-induced whisker motion. In mice of expressing this cross-modal response, their barrel cortical neurons become to encode odor and tail signals alongside whisker signal. These barrel cortical neurons receive new synapse innervations from piriform and S1-tail cortical neurons. The emergence of cross-modal responses as well as the recruitments of new synapse innervations and associative memory cells in the barrel cortex need miRNA-324 and miRNA-133a, which downregulate Ttbk1 and Tet3. The co-activations of sensory cortices recruit their mutual synapse innervations and associative memory cells that integrate and store multiple associated signals through epigenetic-mediated process.

The role of sulfur cycling in arsenic behavior under reducing conditions is not well-understood in previous investigations. This study provides observations of sulfur and oxygen isotope fractionation in sulfate and evaluation of sulfur cycling-related biogeochemical processes controlling dissolved arsenic groundwater concentrations using multiple isotope approaches. As a typical basin hosting high arsenic groundwater, the western Hetao basin was selected as the study area. Results showed that, along the groundwater flow paths, groundwater δS, δO, and δC increased with increases in arsenic, dissolved iron, hydrogen sulfide and ammonium concentrations, while δC decreased with decreasing Eh and sulfate/chloride. Bacterial sulfate reduction (BSR) was responsible for many of these observed changes. The δS indicated that dissolved sulfate was mainly sourced from oxidative weathering of sulfides in upgradient alluvial fans. The high oxygen-sulfur isotope fractionation ratio (0.60) may result from both slow sulfate reduction rates and bacterial disproportionation of sulfur intermediates (BDSI). Data indicate that both the sulfide produced by BSR and the overall BDSI reduce arsenic-bearing iron(III) oxyhydroxides, leading to the release of arsenic into groundwater. These results suggest that sulfur-related biogeochemical processes are important in mobilizing arsenic in aquifer systems.

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