Abstract:Metabolism mediates the flow of matter and energy through the biosphere. We examined how metabolic evolution shapes ecosystems by reconstructing it in the globally abundant oceanic phytoplankter Prochlorococcus. To understand what drove observed evolutionary patterns, we interpreted them in the context of its population dynamics, growth rate, and light adaptation, and the size and macromolecular and elemental composition of cells. This multilevel view suggests that, over the course of evolution, there was a st… Show more
“…Recent molecular clock analyses have suggested that genome streamlining in Prochlorococcus occurred during the Neoproterozoic (500–1000 MYA), well after the Great Oxidation Event of ∼ 2.4 billion years ago, followed by the further differentiation of modern Prochlorococcus ecotypes during the Phanerozoic. (Sánchez‐Baracaldo ; Braakman et al ). Despite rising atmospheric O 2 levels during this time, the oceans were not uniformly oxygenated (Sperling et al ), which probably maintained large cobalt sources from anoxic sediments, as observed in the modern ocean (Hawco et al ).…”
Section: Discussionmentioning
confidence: 99%
“…Cultures growing at high Ni 0 held higher Ni quotas and experienced longer lag phases prior to exponential growth. While it is difficult to evaluate if higher Ni quotas reflect increases in intracellular or periplasmic Ni, the cbiK cobaltochelatase enzyme also has a strong affinity for Ni and is used by some organisms in the biosynthesis of the Ni containing tetrapyrrole F430 (Brindley et al 2003;Moore et al 2017). It is possible that this long lag phase is needed to upregulate Nibinding proteins to decrease competition with cobalt at the binding site of cbiK.…”
Section: Metal Competition In Prochlorococcus Cobalt Uptakementioning
In order to satisfy metabolic requirements for growth, marine cyanobacteria such as Prochlorococcus must acquire cobalt from seawater and synthesize cobalamin cofactors. Through a series of experiments with Prochlorococcus strain MIT 9215 under cobalt limiting conditions, the mechanism of Prochlorococcus' cobalt uptake was investigated. Due to low quotas, Prochlorococcus MIT 9215 can maintain growth at extremely slow rates of cobalt uptake, circa 1 atom per cell per hour. Cobalt quotas were linearly related to the concentration of inorganic cobalt species, Co′, indicating that the metal binding sites on the transporter are strongly unsaturated with respect to cobalt. When limited by cobalt, Prochlorococcus growth rates decreased at high levels of both Zn and Mn, suggesting that both metals compete with cobalt for the same transporter. This effect was not observed under a wide range of Fe, Cu, and Ni concentrations, although the onset of exponential growth was delayed at high Ni. These observations agree with prior characterizations of the periplasmic manganese binding protein MntC, which is probably the main pathway for inorganic cobalt uptake and the locus for Mn and Zn competitive inhibition. The toxicity of zinc toward cobalt limited Prochlorococcus MIT 9215 contrasts with the observation of cobalt‐zinc substitution in eukaryotic phytoplankton and is expected to occur at environmentally relevant concentrations of free zinc and cobalt ions. Thus, the ecological success of Prochlorococcus in the modern ocean may depend on access to cobalt complexed by strong organic ligands that are not subject to competitive inhibition by other metals.
“…Recent molecular clock analyses have suggested that genome streamlining in Prochlorococcus occurred during the Neoproterozoic (500–1000 MYA), well after the Great Oxidation Event of ∼ 2.4 billion years ago, followed by the further differentiation of modern Prochlorococcus ecotypes during the Phanerozoic. (Sánchez‐Baracaldo ; Braakman et al ). Despite rising atmospheric O 2 levels during this time, the oceans were not uniformly oxygenated (Sperling et al ), which probably maintained large cobalt sources from anoxic sediments, as observed in the modern ocean (Hawco et al ).…”
Section: Discussionmentioning
confidence: 99%
“…Cultures growing at high Ni 0 held higher Ni quotas and experienced longer lag phases prior to exponential growth. While it is difficult to evaluate if higher Ni quotas reflect increases in intracellular or periplasmic Ni, the cbiK cobaltochelatase enzyme also has a strong affinity for Ni and is used by some organisms in the biosynthesis of the Ni containing tetrapyrrole F430 (Brindley et al 2003;Moore et al 2017). It is possible that this long lag phase is needed to upregulate Nibinding proteins to decrease competition with cobalt at the binding site of cbiK.…”
Section: Metal Competition In Prochlorococcus Cobalt Uptakementioning
In order to satisfy metabolic requirements for growth, marine cyanobacteria such as Prochlorococcus must acquire cobalt from seawater and synthesize cobalamin cofactors. Through a series of experiments with Prochlorococcus strain MIT 9215 under cobalt limiting conditions, the mechanism of Prochlorococcus' cobalt uptake was investigated. Due to low quotas, Prochlorococcus MIT 9215 can maintain growth at extremely slow rates of cobalt uptake, circa 1 atom per cell per hour. Cobalt quotas were linearly related to the concentration of inorganic cobalt species, Co′, indicating that the metal binding sites on the transporter are strongly unsaturated with respect to cobalt. When limited by cobalt, Prochlorococcus growth rates decreased at high levels of both Zn and Mn, suggesting that both metals compete with cobalt for the same transporter. This effect was not observed under a wide range of Fe, Cu, and Ni concentrations, although the onset of exponential growth was delayed at high Ni. These observations agree with prior characterizations of the periplasmic manganese binding protein MntC, which is probably the main pathway for inorganic cobalt uptake and the locus for Mn and Zn competitive inhibition. The toxicity of zinc toward cobalt limited Prochlorococcus MIT 9215 contrasts with the observation of cobalt‐zinc substitution in eukaryotic phytoplankton and is expected to occur at environmentally relevant concentrations of free zinc and cobalt ions. Thus, the ecological success of Prochlorococcus in the modern ocean may depend on access to cobalt complexed by strong organic ligands that are not subject to competitive inhibition by other metals.
“…DOM can exit microbial cells and enter the DOM pool in several ways: sloppy feeding by grazers, lysis by virus, 'spontaneous' (i.e., abiotic-induced) cell lysis, excretion from live cells, and release of membrane vesicles (Nagata and Kirchman, 1991;Ankrah et al, 2014;Biller et al, 2014). Studies thus far indicate that Prochlorococcus can release significant amounts of DOM via excretion and vesicle formation (Bertilsson et al, 2005;Becker et al, 2014;Biller et al, 2014;Braakman et al, 2017), and this release may constitute a significant return on the investment for the HOOH-consuming heterotrophic bacteria. Studies thus far indicate that Prochlorococcus can release significant amounts of DOM via excretion and vesicle formation (Bertilsson et al, 2005;Becker et al, 2014;Biller et al, 2014;Braakman et al, 2017), and this release may constitute a significant return on the investment for the HOOH-consuming heterotrophic bacteria.…”
Hydrogen peroxide (HOOH) is a reactive oxygen species, derived from molecular oxygen, that is capable of damaging microbial cells. Surprisingly, the HOOH defence systems of some aerobes in the oxygenated marine environments are critically depleted, relative to model aerobes. For instance, the gene encoding catalase is absent in the numerically dominant photosynthetic cyanobacterium, Prochlorococcus. Accordingly, Prochlorococcus is highly susceptible to HOOH when exposed as pure cultures. Pure cultures do not exist in the marine environment, however. Catalase-positive community members can remove HOOH from the seawater medium, thus lowering the threat to Prochlorococcus and any other member that likewise lacks their own catalase. This cross-protection may constitute a loosely defined symbiosis, whereby the catalase-positive helper cells may benefit through the acquisition of nutrients released by the beneficiaries such as Prochlorococcus. Other members of the community that may be helped by the catalase-positive cells may include some lineages of Synechococcus - the sister genus of Prochlorococcus - as well as some lineages of SAR11 and ammonia oxidizing archaea and bacteria. The co-occurrence of catalase-positive and -negative members suggests that cross-protection from HOOH-mediated oxidative stress may play an important role in the construction of the marine microbial community.
“…If niche selection of genomes adapted to different niches in the water column plays a role, it is most likely to occur in the stable pycnocline where populations remain segregated over longer periods (weeks to month, or longer). Light intensity is not the only, or even the major defining difference between the periodically mixed-layer and the stable pycnocline (Braakman et al, 2017). Compared to the mixed-layer zone, the pycnocline has higher nutrient concentrations with a different composition .…”
Section: Irradiance In a Dynamic Environmentmentioning
The fluorescence and scattering properties of Prochlorococcus and Synechococcus at Station ALOHA as measured by flow cytometry (termed the FCM phenotype) vary with depth and over a variety of time scales. The variation in FCM phenotypes may reflect population selection or physiological acclimation to local conditions. Observations before, during, and after a storm with deep water mixing show a short-term homogenization of the FCM phenotypes with depth, followed by a return to the stable pattern over the time span of a few days. These dynamics indicate that, within the upper mixed-layer, the FCM phenotype distribution represents acclimation to ambient light. The populations in the pycnocline (around 100 m and below), remain stable and are invariant with light conditions. In samples where both cyanobacteria coexist, fluorescence properties of Prochlorococcus and Synechococcus are tightly correlated providing further evidence that FCM phenotype variability is caused by a common environmental factor or factors. Measurements of the dynamics of FCM phenotypes provide insights into phytoplankton physiology and adaptation. Alternatively, FCM phenotype census of a water mass may provide information about its origin and illumination history.
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