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Trumbore, S.

Publications and source records attributed to Trumbore, S..

2 recordsLinked to original sources

14C-age of carbon used to grow fine roots reflects tree carbon status

O_LI"Bomb" 14C ages in trees indicate the time elapsed between carbon fixation into nonstructural carbon (NSC) and its use for metabolism and growth. It remains unknown why newly grown aboveground tissues have a narrow range of young 14C-ages, while fine root ages can span decades. C_LIO_LIWe measured 14C in tissues of two coniferous species along an alpine treeline ecotone and used a mixing model to estimate the fraction of NSC that is metabolically active. We expected that greater growth limitation higher in the ecotone would supply more freshly fixed NSC to respiration, active NSC, carbohydrates, and roots, resulting in younger 14C-ages of NSC used to grow tissues. C_LIO_LIResults confirmed an increase in fresh NSC supply with elevation. Needle and branch growth was supported by young NSC (< 2 yr) with little elevation influence, while root growth was supported by older NSC that declined from 10 to 6 yr with elevation. C_LIO_LIMassive allocation of fresh NSC to needles and branches could explain their young 14C-ages. Variable fine root 14C-ages reflect tree C status, with older ages when aboveground growth limits the contribution of new C belowground, while young ages represent greater delivery of fresh NSC to roots. C_LI

ecology↗

Rates of primary production in groundwater rival those in oligotrophic marine systems

The terrestrial subsurface contains nearly all of Earths freshwater reserves1 and harbors upwards of 60% of our planets total prokaryotic biomass2,3. While genetic surveys suggest these organisms rely on in situ carbon fixation, rather than the translocation of photosynthetically derived organic carbon4-6, corroborating measurements of carbon fixation in the subsurface are absent. Using a novel ultra-low level 14C-labeling technique, we show that in situ carbon fixation rates in a carbonate aquifer reached 10% of the median rates measured in oligotrophic marine surface waters, and were up to six-fold greater than those observed in lower euphotic zone waters where deep chlorophyll levels peak. Empirical carbon fixation rates were substantiated by both nitrification and anammox rate data. Metagenomic analyses revealed a remarkable abundance of putative chemolithoautotrophic members of an uncharacterized order of Nitrospiria - the first representatives of this class expected to fix carbon via the Wood-Ljungdahl pathway. Based on these fixation rates, we extrapolate global primary production in carbonate groundwaters to be 0.11 Pg of carbon per year.

microbiology↗