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Attribution of Space-Time Variability in Global-Ocean Dissolved Inorganic Carbon.

ABSTRACT: The inventory and variability of oceanic dissolved inorganic carbon (DIC) is driven by the interplay of physical, chemical, and biological processes. Quantifying the spatiotemporal variability of these drivers is crucial for a mechanistic understanding of the ocean carbon sink and its future trajectory. Here, we use the Estimating the Circulation and Climate of the Ocean-Darwin ocean biogeochemistry state estimate to generate a global-ocean, data-constrained DIC budget and investigate how spatial and seasonal-to-interannual variability in three-dimensional circulation, air-sea CO₂ flux, and biological processes have modulated the ocean sink for 1995-2018. Our results demonstrate substantial compensation between budget terms, resulting in distinct upper-ocean carbon regimes. For example, boundary current regions have strong contributions from vertical diffusion while equatorial regions exhibit compensation between upwelling and biological processes. When integrated across the full ocean depth, the 24-year DIC mass increase of 64 Pg C (2.7 Pg C year^-1) primarily tracks the anthropogenic CO₂ growth rate, with biological processes providing a small contribution of 2% (1.4 Pg C). In the upper 100 m, which stores roughly 13% (8.1 Pg C) of the global increase, we find that circulation provides the largest DIC gain (6.3 Pg C year^-1) and biological processes are the largest loss (8.6 Pg C year^-1). Interannual variability is dominated by vertical advection in equatorial regions, with the 1997-1998 El Niño-Southern Oscillation causing the largest year-to-year change in upper-ocean DIC (2.1 Pg C). Our results provide a novel, data-constrained framework for an improved mechanistic understanding of natural and anthropogenic perturbations to the ocean sink.

SUBMITTER: Carroll D

PROVIDER: S-EPMC9286438 | biostudies-literature |

REPOSITORIES: biostudies-literature

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Project description:The hydrothermal vent gammaproteobacterium Thiomicrospira crunogena inhabits an unstable environment and must endure dramatic sweeps in habitat chemistry. This sulfur chemolithoautotroph responds to changes in dissolved inorganic carbon (DIC; = CO2 + HCO3- + CO3-2) availability with a carbon concentrating mechanism (CCM), in which whole-cell affinity for DIC, as well as the intracellular DIC concentration, increase substantially under DIC-limitation. To determine whether this CCM is regulated at the level of transcription, cells cultivated under high-DIC conditions in chemostats were resuspended in growth medium with low concentrations of DIC, and CCM development was tracked in the presence and absence of RNA polymerase inhibitor rifampicin. The induction of the CCM, as measured by silicone oil centrifugation, was hindered in the presence of rifampicin. Similar results were observed for carboxysome gene transcription and assembly, as assayed by qRT-PCR and transmission electron microscopy, respectively. Genome-wide transcription patterns, assayed via microarrays, were compared for cells grown under DIC-limitation versus ammonia limitation. In addition to carboxysome genes, two novel genes (Tcr_1019 and Tcr_1315), present in other organisms including chemolithoautotrophs, but whose function(s) have not been elucidated in any organism, were found to be upregulated under low-DIC conditions. Likewise, under ammonia limitation, in addition to the expected enhancement of ammonia transporter and PII-gene transcription, the transcription of two novel genes was measurably enhanced (Tcr_0466 and Tcr_2018). Upregulation of all four genes was verified via qRT-PCR (Tcr_1019: 4-fold; Tcr_1315: ~7-fold; Tcr_0466: >200-fold; Tcr_2018: 7-fold), suggesting novel components are part of the response to nutrient limitation by this organism. In this study Thiomicrospira crunogena cells were grown under inorganic carbon limitation and ammonia limitation (high inorganic carbon concentrations) to examine genome wide transcription responses

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Attribution of Space-Time Variability in Global-Ocean Dissolved Inorganic Carbon.

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