Natural iron fertilization by shallow hydrothermal sources fuels diazotroph blooms in the ocean

Transcriptome remodeling drives acclimation to iron availability in the marine N2-fixing cyanobacterium Trichodesmium erythraeum IMS101

While enhanced phytoplankton growth as a result of iron (Fe) fertilization has been extensively characterized, our understanding of the underlying mechanisms remains incomplete. Here, we show in a laboratory setup mimicking Fe fertilization in the field that transcriptome remodeling is a primary driver of acclimation to Fe availability in the marine diazotrophic cyanobacterium Trichodesmium erythraeum IMS101. Fe supplementation promoted cell growth, photosynthesis and N2 fixation, and concomitant expression of the photosynthesis and N2 fixation genes. The expression of genes encoding major Fe-binding metalloproteins is tightly linked to cellular carbon and nitrogen metabolism and appears to be controlled by the ferric uptake regulator FurA, which is involved in regulating Fe uptake and homeostasis. This feedback loop is reinforced by substitutive expression of functionally equivalent or competitive genes depending on Fe availability, as well as co-expression of multiple Fe stress inducible isiA genes, an adaptive strategy evolved to elicit the Fe-responsive cascade. The study provides a genome-wide perspective on the acclimation of a prominent marine diazotroph to Fe availability, reveals an upgraded portfolio of indicator genes that can be used to better assess Fe status in the environment, and predicts scenarios of how marine diazotrophs may be affected in the future ocean.IMPORTANCEThe scarcity of trace metal iron (Fe) in global oceans has a great impact on phytoplankton growth. While enhanced primary productivity as a result of Fe fertilization has been extensively characterized, the underlying molecular mechanisms remain poorly understood. By subjecting the model marine diazotroph Trichodesmium erythraeum IMS101 to increasing concentrations of supplemented Fe, we demonstrate in it a comprehensively remodeled transcriptome that drives the mobilization of cellular Fe for coordinated carbon and nitrogen metabolism and reallocation of energy and resources. Our data provide broad genomic insight into marine diazotrophs acclimation to Fe availability, enabling the versatility and flexibility in choice of indicator genes for monitoring Fe status in the environment and having implications on how marine diazotrophs persist into the future ocean.

Shallow Hydrothermal Fluids Shape Microbial Dynamics at the Tagoro Submarine Volcano (Canary Islands, Spain)

Shallow underwater hydrothermal systems are often overlooked despite their potential contribution to marine diversity and biogeochemistry. Over a decade after its eruption, the Tagoro submarine volcano continues to emit heat, reduced compounds, and nutrients into shallow waters, serving as a model system for studying the effects of diffuse hydrothermal fluids on surface microbial communities. The impact on both phytoplankton and bacterial communities was examined through experimental manipulations mimicking dilution levels up to ~100 m from the primary crater of Tagoro. Chlorophyll a concentration doubled in the presence of hydrothermal products, with peak levels detected about a day earlier than in controls. Picoeukaryotes and Synechococcus cell abundances moderately increased, yet small eukaryotic phytoplankton (≤ 5 μm) predominated in the hydrothermally enriched bottles. Dinoflagellates, diatoms, small green algae and radiolarians particularly benefited from the hydrothermal inputs, along with phototrophic and chemoautotrophic bacteria. Our results indicate that hydrothermal products in shallow waters enhance primary production driven by phototrophic microbes, potentially triggering a secondary response associated with increased organic matter availability. Additionally, protistan grazing and parasitism emerged as key factors modulating local planktonic communities. Our findings highlight the role of shallow submarine hydrothermal systems in enhancing local primary production and element cycling.

Decoding drivers of carbon flux attenuation in the oceanic biological pump

The biological pump supplies carbon to the oceans' interior, driving long-term carbon sequestration and providing energy for deep-sea ecosystems1,2. Its efficiency is set by transformations of newly formed particles in the euphotic zone, followed by vertical flux attenuation via mesopelagic processes3. Depth attenuation of the particulate organic carbon (POC) flux is modulated by multiple processes involving zooplankton and/or microbes4,5. Nevertheless, it continues to be mainly parameterized using an empirically derived relationship, the 'Martin curve'6. The derived power-law exponent is the standard metric used to compare flux attenuation patterns across oceanic provinces7,8. Here we present in situ experimental findings from C-RESPIRE9, a dual particle interceptor and incubator deployed at multiple mesopelagic depths, measuring microbially mediated POC flux attenuation. We find that across six contrasting oceanic regimes, representing a 30-fold range in POC flux, degradation by particle-attached microbes comprised 7-29 per cent of flux attenuation, implying a more influential role for zooplankton in flux attenuation. Microbial remineralization, normalized to POC flux, ranged by 20-fold across sites and depths, with the lowest rates at high POC fluxes. Vertical trends, of up to threefold changes, were linked to strong temperature gradients at low-latitude sites. In contrast, temperature played a lesser role at mid- and high-latitude sites, where vertical trends may be set jointly by particle biochemistry, fragmentation and microbial ecophysiology. This deconstruction of the Martin curve reveals the underpinning mechanisms that drive microbially mediated POC flux attenuation across oceanic provinces.

Unsolved mysteries in marine nitrogen fixation

Biological nitrogen (N2) fixation is critical in global biogeochemical cycles and in sustaining the productivity of the oceans. There remain many unanswered questions, unresolved hypotheses, and unchallenged paradigms. The fundamental balance of N input and losses has not been fully resolved. One of the major N2-fixers, Trichodesmium, remains an enigma with intriguing biological and ecological secrets. Cyanobacterial N2 fixation, once thought to be primarily due to free-living cyanobacteria, now also appears to be dependent on microbial interactions, from microbiomes to unicellular symbioses, which remain poorly characterized. Nitrogenase genes associated with diverse non-cyanobacterial diazotrophs (NCDs) are prevalent, but their significance remains a huge knowledge gap. Answering questions, new and old, such as those discussed here, is needed to understand the ocean's N and C cycles and their responses to environmental change.

Implications of ocean acidification on micronutrient elements-iron, copper and zinc, and their primary biological impacts: A review

This review has been undertaken to understand the effectiveness of ocean acidification on oceanic micronutrient metal cycles (iron, copper and zinc) and its potential impacts on marine biota. Ocean acidification will slow down the oxidation of Fe(II) thereby retarding Fe(III) formation and subsequent hydrolysis/precipitation leading to an increase in iron bioavailability. Further, the increased primary production sustains enzymatic bacteria assisted Fe(III) reduction and subsequently the binding of weaker ligands favours the dissociation of free Fe(II) ions, thus increasing the bioavailability. The increasing pCO2 condition increases the bioavailability of copper ions by decreasing the availability of free CO32- ligand concentration. The strong complexation by dissolved organic matter may decrease the bioavailable iron and zinc ion concentration. Since ocean acidification affects the bioavailability of essential metals, studies on the uptake rates of these elements by phytoplankton should be carried out to reveal the future scenario and its effect on natural environment.