Plant litter is a primary source of soil organic matter (SOM) through microbial transformation, with its quality, especially the hemicellulose and lignin content, strongly influencing litter decomposition and carbon (C) cycling. However, how the hemicellulose:lignin ratio regulates litter decomposition, transformation, and contribution to SOM remains unclear. Here, 13C-labelled litter (hemicellulose:lignin ratios of 0.42–1.02) from six maize plant parts was used to trace 13C incorporation into dissolved organic 13C (DO13C), microbial biomass 13C (MB13C), particulate organic 13C (PO13C), mineral-associated organic 13C (MAO13C), and 13C-microbial necromass during an 84-day incubation. After 84 days, 11–18 % of litter decomposed to CO