Sasha C. Reed Daniela F. Cusack Avishesh Neupane 2021 <div id="abstracts" class="Abstracts u-font-serif"><div id="abs0010" class="abstract author" lang="en"><div id="abssec0010"><p id="abspara0010">Tropical forest soils contain some of the largest carbon (C) stocks on Earth, yet the effects of warming on the fate of fresh C entering tropical soils are still poorly understood. This research sought to understand how the fate of fresh C entering soils is influenced by warming, soil weathering status, and C chemistry. We hypothesized that compounds that are quickly incorporated into microbial biomass (i.e., greater C use efficiency [CUE]) subsequently have longer-term (255 days) retention in soil. We also hypothesized that relatively weathered soils with greater sorptive capacity also retain more fresh C in the short and longer-terms, and that C in these soils is more resistant to weathering loss compared with less weathered soils. We tested these hypotheses by adding two<span>&nbsp;</span>¹³C-labeled compounds (glucose and glycine) to three tropical forest soils from a weathering gradient in Hawai'i, and then incubating soils at ambient (16&nbsp;°C), +5&nbsp;°C, and +10&nbsp;°C for 255 days. We found that 255-day<span>&nbsp;</span>¹³C retention in mineral soil across sites and temperatures was best predicted by two factors: initial retention of<span>&nbsp;</span>¹³C in mineral soil and initial microbial<span>&nbsp;</span>¹³CUE (Adjusted R²&nbsp;=&nbsp;0.78). Carbon compound type influenced<span>&nbsp;</span>¹³C initial retention, with greater glucose-¹³C retention versus glycine-¹³C retention in mineral soils and microbial biomass, corresponding to greater glucose-¹³C retention in soil at 255 days. Warming had a negative longer-term effect on the retention of<span>&nbsp;</span>¹³C only in the least-weathered soil, supporting our hypothesis. These results show that initial retention of fresh C in soils via mineral sorption and microbial uptake is a strong predictor of longer-term retention, indicating that immediate C losses are a major hurdle for soil C storage. Also, retention of fresh C appears most sensitive to warming in less-weathered tropical soils, supporting the idea that mineral sorption may provide some protections against warming. Understanding the interaction between soil sorptive properties and warming for C cycling could improve predictions of forest-climate feedbacks for tropical regions.</p></div></div></div> application/pdf 10.1016/j.soilbio.2020.108080 en Elsevier Warming and microbial uptake influence the fate of added soil carbon across a Hawai'ian weathering gradient article