<?xml version="1.0" encoding="utf-8" standalone="yes"?><rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom"><channel><title>T. Koch | Amano Lab | Hokkaido University</title><link>https://amanoresearch.com/authors/t.-koch/</link><atom:link href="https://amanoresearch.com/authors/t.-koch/index.xml" rel="self" type="application/rss+xml"/><description>T. Koch</description><generator>HugoBlox Kit (https://hugoblox.com)</generator><language>en-us</language><lastBuildDate>Mon, 15 Jun 2026 00:00:00 +0000</lastBuildDate><item><title>Major contribution of anaplerosis to inorganic carbon fixation in the dark ocean</title><link>https://amanoresearch.com/publication/amano-202606-anaplerosis/</link><pubDate>Mon, 15 Jun 2026 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/amano-202606-anaplerosis/</guid><description>&lt;p&gt;While CO 2 fixation by photo- and chemolithoautotrophs is a central process of the global carbon
cycle, many organisms also incorporate inorganic carbon into organic compounds through anaplerotic
carbon fixation, a process that replenishes intermediates of central metabolic pathways. However,
the active drivers and quantitative importance of anaplerotic carbon fixation in the oceanic carbon
cycling remain poorly understood. Here, through analysis of global ocean multi-omics datasets, we
identified widespread expression of enzymes involved in this process, especially phosphoenolpyruvate
carboxylase. The heterotrophic bacterial genus Alteromonas , a globally distributed marine taxon
lacking genes for autotrophic carbon fixation pathways, exhibited particularly high transcriptional
and proteomic activity for this enzyme. Laboratory incubations confirmed that Alteromonas
assimilated dissolved inorganic carbon (DIC) into biomass, with rates regulated by temperature and
organic matter availability. Single-cell tracer analyses of the deep ocean microbial communities
quantified Alteromonas ’s contribution at about 17% of total dark DIC fixation (median; confidence
interval, 10–28%), equivalent to a potential global flux of about 0.2 PgC yr −1 . These results
reveal substantial DIC fixation via anaplerosis, indicating that dark carbon fixation is partly
supported by heterotrophic metabolism and modulated by environmental conditions, with responses that
may differ from those of canonical autotrophic processes.&lt;/p&gt;</description></item></channel></rss>