Phytoplankton are primarily confined to the sunlit epipelagic zone, yet intact algal cells persist in the ocean’s mesopelagic twilight zone where light is minimal. However, their survival strategies in the deeper ocean remain unknown. Here, we isolate Chaetoceros sp. DS1 from 1000 m depth and reveal its survival mechanisms under prolonged darkness and high pressure, including membrane lipid remodeling and enhanced antioxidant defenses. Importantly, DS1 maintains a latent photosynthetic reserve that activates upon exposure to dim blue light and higher pressure typical of the twilight zone, enabling photosynthesis and nutrient uptake. It exhibits metabolic flexibility by utilizing stored carbon in darkness and assimilating organic carbon under dim light. Global meta-omics data show widespread, transcriptionally active Chaetoceros-like diatoms in the twilight zone, expressing blue-light sensors and protein synthesis genes. These findings identify the ocean twilight zone as a previously overlooked niche for metabolically active phytoplankton, expanding understanding of deep-ocean microbial ecology and carbon cycling.
Marine microbes have long been regarded as central to replenishing the ocean's reservoir of recalcitrant dissolved organic matter (RDOM). However, molecular-level evidence for their role remains inconclusive because RDOM persists for years to millennia, far exceeding timescales accessible to laboratory experiments, and because conventional analytical approaches lack the resolution to discern structural isomers of RDOM that confer functionally important differences in persistence. Using polarity-based liquid chromatography coupled to ultrahigh-resolution mass spectrometry capable of discriminating RDOM isomer clusters, we reveal that marine microbial consortia rapidly (≤ 90 d) convert diverse organic substrates into RDOM with extensive structural isomerism that closely mirrors natural seawater RDOM. A subset of these microbially derived RDOM compounds exhibits near-ubiquitous occurrence (> 99%) in a global dataset and accumulates progressively in the ocean's interior. Together, our findings substantiate the direct microbial contribution to the long-lived oceanic carbon reservoir through the rapid diversification of RDOM isomers, a mechanism that contributes to sustaining the complexity and long-term persistence of the planetary-scale carbon reservoir.
Ruan-Hong Cai, O. Lechtenfeld, Andrew J. Tanentzap et al.· Proceedings of the National...· 2 citations
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