Photosynthesis in the world's oceans by marine algae is responsible for approximately 50% of CO2 fixed into organic carbon. Aquatic primary producers are intricately linked to the climate system due to their reliance on CO2 as a substrate for photosynthesis and role in the removal and export of carbon from the surface ocean to marine sediments. The evolutionary history of marine algae was shaped by changes in the climate system. As a result, fossilized marine algae and modern representatives of ancient groups have the potential to unlock information about the Earth’s climatic past. To use this information and fully understand the role of marine algae in the carbon cycle, however, it is essential to develop an in-depth understanding of CO2 fixation in these organisms. In this thesis I look at carbon fixation in biomineralizing marine algae from a geological and a biological perspective. First I apply a carbon isotope proxy for CO2 to organic material preserved in marine diatom frustules from an extremely transformative period in geological history, the Eocene-Oligocene boundary. Subsequently, this thesis aims to address gaps in our understanding of carbon fixation in eukaryotic marine algae. I present a novel dataset of kinetics of the carbon fixing enzyme, Rubisco, in eukaryotic algae, investigate the role of a pyrenoid-based carbon concentrating mechanism, and identify plastic changes in carbon fixing machinery in response to changing CO2. The findings from this thesis refine our understanding of primary production in the oceans and how we apply algae-based CO2 proxies to understand ancient climates.

Gammaproteobacterium Thiomicrospira crunogena thrives at deep-sea vents despite extreme oscillations in the environmental supply of dissolved inorganic carbon (DIC; =CO2 + HCO3- + CO3-2). Survival in this habitat is likely aided by the presence of a carbon concentrating mechanism (CCM). Though CCMs are well-documented in cyanobacteria, based on this study T. crunogena is the first chemolithoautotroph to have a physiologically characterized CCM. T. crunogena is capable of rapid growth in the presence of 20 micrometers DIC, has the ability to use both extracellular HCO3- and CO2, and generates intracellular DIC concentrations 100-fold greater than extracellular, all of which are consistent with a CCM analogous to those present in cyanobacteria. Interestingly, however, the T.crunogena genome lacks apparent orthologs of many of the components of the cyanobacteria CCM (e.g., HCO3- transporters). However, despite this lack, several candidate genes were identified during genome annotation as likely to play a role in DIC uptake and fixation (three carbonic anhydrase genes: alpha-CA, beta-CA, and csoSCA, as well as genes encoding three RubisCO enzymes: cbbLS, CScbbLS, and cbbM, which encode a cytoplasmic form I RubisCO, a carboxysomal form I RubisCO, and a form II RubisCO, respectively). In order to clarify their possible roles in DIC uptake and fixation, alpha-CA, beta-CA and csoSCA transcription by low-DIC and high-DIC T. crunogena were assayed by qRT PCR, heterologous expression in E. coli, and potentiometric assays of low-DIC and high-DIC T. crunogena. Transcription of alpha-CA and beta-CA were not sensitive to the DIC concentration available during growth. When overexpressed in E.coli, carbonic anhydrase activity was detectable, and it was possible to measure the effects of the classical carbonic anhydrase inhibitors ethoxyzolamide and acetazolamide, as well as dithiothreitol (DTT; recently determined to be a carboxysomal CA inhibitor). The alpha-CA was sensitive to both of the classical inhibitors, but not DTT. Beta-CA was insensitive to all inhibitors tested, and the carboxysomal carbonic anhydrase was sensitive to both ethoxyzolamide and DTT. The observation that the CA activity measureable potentiometrically with intact T. crunogena cells is sensitive to classical inhibitors, but not DTT, strongly suggests the alpha-CA is extracellular. The presence of carbonic anhydrase activity in crude extracts of high-DIC cells that was resistant to classical inhibitors suggests that beta-CA may be more active in high-DIC cells. Incubating cells with ethoxyzolamide (which permeates cells rapidly) resulted in inhibition of carbon fixation, but not DIC uptake, while incubation with acetazolamide (which does not permeate cells rapidly) had no apparent effect on either carbon fixation or DIC uptake. The observations that inhibition of alpha-CA has no effect on DIC uptake and fixation, and that the beta-CA is not transcribed more frequently under low-DIC conditions, make it unlikely that either play a role in DIC uptake and fixation in low-DIC cells. Further studies are underway to determine the roles of alpha-CA and beta-CA in T. crunogena. To assay the entire genome for genes transcribed more frequently under low-DIC conditions, and therefore likely to play a role in the T. crunogena CCM, oligonucleotide arrays were fabricated using the T. crunogena genome sequence. RNA was isolated from cultures grown in the presence of both high (50 mM) and low (0.05 mM) concentrations of DIC, directly labeled with cy5 fluorophore, and hybridized to microarrays. Genes encoding the three RubisCO enzymes present in this organism demonstrated differential patterns of transcription consistent with what had been observed previously in Hydrogenovibrio marinus. Genes encoding two conserved hypothetical proteins were also found to be transcribed more frequently under low-DIC conditions, and this transcription pattern was verified by qRT-PCR. Knockout mutants are currently being generated to determine whether either gene is necessary for growth under low-DIC conditions. Identifying CCM genes and function in autotrophs beyond cyanobacteria will serve as a window into the physiology required to flourish in microbiallydominated ecosystems where noncyanobacterial primary producers dominate.

The Central Arctic Ocean is a repository of rich and diverse biota, whose major portion is one of the most important drivers of global biogeochemical cycles, including carbon cycling. In this study, the functional potential of the microbiota to fix carbon with alternative carbon fixation pathways were investigated along with their chemolithotrophic characteristics. Samples from two expeditions MOSAiC & SAS-Oden (2019-2021) resulted in metagenomic data consisting of about 1200 mOTUs (metagenomic Operational Taxonomic Units). Kofamscan based annotation explained by KEGG pathways database was analysed to explore prevalence of the alternative Carbon Fixation pathways across different taxa. From the six carbon fixation pathways, three were consolidated for their presence (rTCA, DC-HP, HP-HP). In order to explain the other metabolic processes that these organisms employ to survive, a functional annotation tool for metabolic pathways was used. that Reductive Tricarboxylic acid cycle pathway was found to be most present and observed in 5 out of 6 mOTUs selected from filtering the dataset. The taxa include bacterial phyla Proteobacteria, Actinobacteria, Chloroflexota and Marinisomatota and archaeal phyla Thermoplasmota. However, for the other pathways and less studied organisms less resolution were observed across the dataset for the presence of other pathways. These CFPs found were also supported by oxidation of inorganic compounds with high redox potentials. This study provides a glimpse of the metabolic potential of the Central Arctic Ocean microbiota, shines light on the importance of understanding and unravelling the intricacies of this rich and diverse environment.

Diatoms play a fundamental role in marine food webs, and significantly contribute to global primary production and carbon sequestration into the deep ocean. In many offshore areas of the open ocean, iron (Fe) input is low, and its availability often limits phytoplankton biomass. Recently, gene sequences encoding ferritin, a nearly ubiquitous iron storage and detoxifying protein, have been identified in pennate diatoms such as Pseudo-nitzschia, but not in other Stramenopiles (which include centric diatoms, brown algae and some protist plant parasites) or Cryptophyte relatives. Members of this genus readily bloom upon addition of iron to Fe-limited waters, and are known to produce the neurotoxin domoic acid. Until now, the reason for the success of pennate diatoms in the open ocean was uncertain; however, expressing ferritin would allow pennate species to store Fe after a transient input, using it to dominate Fe stimulated algal blooms. Here, the ferritin gene was cloned from the coastal pennate diatom Pseudonitzschia multiseries, overexpressed in Escherichia coli, and purified using liquid chromatography. The ferritin protein sequence appears to encode a non-heme, ferritinlike di-iron carboxylate protein, while gel filtration chromatography and SDS-PAGE indicate that this ferritin is part of the 24 subunit maxi-ferritins. Spectroscopically monitoring the addition of Fe(II) to a buffered ferritin solution shows that the P. multiseries protein demonstrates ferroxidase activity, binding iron and storing it as Fe(III) in excess of 600 equivalents per protein shell. In keeping with the typical stoichiometry of the ferroxidase reaction, oxygen (O₂) is consumed in a 2 Fe:O₂ratio while hydrogen peroxide is produced concurrently. iii Diatoms evolved from secondary endosymbiosis involving eukaryotic red algae; however, a broad phylogenetic comparison suggests that P. multiseries ferritin was likely acquired via lateral gene transfer from cyanobacteria – not from its ancestral endosymbionts. Until recently, no other ferritins have been identified in diatoms, and the protein characterized here is unique in that it seems to be derived from a prokaryotic organism yet it occurs in a marine eukaryote. These findings have direct implications for the success of pennate diatoms in both Fe rich coastal waters and upon Fe addition in the open ocean.

Diatoms play a fundamental role in marine food webs, and significantly contribute to global primary production and carbon sequestration into the deep ocean. In many offshore areas of the open ocean, iron (Fe) input is low, and its availability often limits phytoplankton biomass. Recently, gene sequences encoding ferritin, a nearly ubiquitous iron storage and detoxifying protein, have been identified in pennate diatoms such as Pseudo-nitzschia, but not in other Stramenopiles (which include centric diatoms, brown algae and some protist plant parasites) or Cryptophyte relatives. Members of this genus readily bloom upon addition of iron to Fe-limited waters, and are known to produce the neurotoxin domoic acid. Until now, the reason for the success of pennate diatoms in the open ocean was uncertain; however, expressing ferritin would allow pennate species to store Fe after a transient input, using it to dominate Fe stimulated algal blooms. Here, the ferritin gene was cloned from the coastal pennate diatom Pseudonitzschia multiseries, overexpressed in Escherichia coli, and purified using liquid chromatography. The ferritin protein sequence appears to encode a non-heme, ferritinlike di-iron carboxylate protein, while gel filtration chromatography and SDS-PAGE indicate that this ferritin is part of the 24 subunit maxi-ferritins. Spectroscopically monitoring the addition of Fe(II) to a buffered ferritin solution shows that the P. multiseries protein demonstrates ferroxidase activity, binding iron and storing it as Fe(III) in excess of 600 equivalents per protein shell. In keeping with the typical stoichiometry of the ferroxidase reaction, oxygen (O₂) is consumed in a 2 Fe:O₂ratio while hydrogen peroxide is produced concurrently. iii Diatoms evolved from secondary endosymbiosis involving eukaryotic red algae; however, a broad phylogenetic comparison suggests that P. multiseries ferritin was likely acquired via lateral gene transfer from cyanobacteria – not from its ancestral endosymbionts. Until recently, no other ferritins have been identified in diatoms, and the protein characterized here is unique in that it seems to be derived from a prokaryotic organism yet it occurs in a marine eukaryote. These findings have direct implications for the success of pennate diatoms in both Fe rich coastal waters and upon Fe addition in the open ocean.

Diatoms play a fundamental role in marine food webs, and significantly contribute to global primary production and carbon sequestration into the deep ocean. In many offshore areas of the open ocean, iron (Fe) input is low, and its availability often limits phytoplankton biomass. Recently, gene sequences encoding ferritin, a nearly ubiquitous iron storage and detoxifying protein, have been identified in pennate diatoms such as Pseudo-nitzschia, but not in other Stramenopiles (which include centric diatoms, brown algae and some protist plant parasites) or Cryptophyte relatives. Members of this genus readily bloom upon addition of iron to Fe-limited waters, and are known to produce the neurotoxin domoic acid. Until now, the reason for the success of pennate diatoms in the open ocean was uncertain; however, expressing ferritin would allow pennate species to store Fe after a transient input, using it to dominate Fe stimulated algal blooms. Here, the ferritin gene was cloned from the coastal pennate diatom Pseudonitzschia multiseries, overexpressed in Escherichia coli, and purified using liquid chromatography. The ferritin protein sequence appears to encode a non-heme, ferritinlike di-iron carboxylate protein, while gel filtration chromatography and SDS-PAGE indicate that this ferritin is part of the 24 subunit maxi-ferritins. Spectroscopically monitoring the addition of Fe(II) to a buffered ferritin solution shows that the P. multiseries protein demonstrates ferroxidase activity, binding iron and storing it as Fe(III) in excess of 600 equivalents per protein shell. In keeping with the typical stoichiometry of the ferroxidase reaction, oxygen (O₂) is consumed in a 2 Fe:O₂ratio while hydrogen peroxide is produced concurrently. iii Diatoms evolved from secondary endosymbiosis involving eukaryotic red algae; however, a broad phylogenetic comparison suggests that P. multiseries ferritin was likely acquired via lateral gene transfer from cyanobacteria – not from its ancestral endosymbionts. Until recently, no other ferritins have been identified in diatoms, and the protein characterized here is unique in that it seems to be derived from a prokaryotic organism yet it occurs in a marine eukaryote. These findings have direct implications for the success of pennate diatoms in both Fe rich coastal waters and upon Fe addition in the open ocean. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate

The Calvin – Benson cycle is the most widespread metabolic pathway capable of fixing CO2 in nature and a target of very high interest to metabolic engineers worldwide. In this study, 12 metabolites (ATP, AMP, NADP, NADPH, 2PG, 3PGA, FBP, RuBP, PEP, AKG, Ac-CoA and phenylalanine) were tested for protein – metabolite interactions against the proteome of Cupriavidus necator (previously Ralstonia eutropha) in the hopes of finding potential examples of allosteric regulation of the Calvin – Benson cycle. This is accomplished through the use of the LiP-SMap method, a recently developed shotgun proteomics method described by Piazza et al. capable of testing a metabolite of interest for interactions with the entire proteome of an organism at once. A functional protocol was developed and 234 protein – metabolite interactions between ATP and the proteome of C. necator are identified, 103 of which are potentially novel. Due to time constraints and setbacks in the lab, significant results were not produced for the other 11 metabolites tested. C. necator is an industrially relevant chemolithoautotroph that can be engineered to produce many valuable products and is capable of growth on CO2 and hydrogen gas. The bacteria were grown in continuous cultures after which the proteome was extracted while retaining its native state. Subsequently, the proteome was incubated with a metabolite of interest and subjected to limited, non-specific proteolysis. The resulting peptide mix was analyzed by liquid chromatography coupled tandem mass spectrometry (LC – MS/MS). / Calvin-Benson-cykeln är den mest utbredda metaboliska processen i naturen med vilken det är möjligt att fixera CO2 och en måltavla av högsta intresse för bioteknologer världen över. I den här studien testades 12 metaboliter (ATP, AMP, NADP, NADPH, 2PG, 3PGA, FBP, RuBP, PEP, AKG, Ac-CoA and phenylalanine) för interaktioner mot proteomet från Cupriavidus necator (tidigare Ralstonia eutropha) i hopp om att hitta potentiella exempel på allosterisk reglering av Calvin-Benson-cykeln. Detta uppnåddes genom användning av LiP-SMap-metoden, en nyligen utvecklad proteomikmetod beskriven av Piazza et al. kapabel av att testa en metabolit av intresse mot en organisms hela proteom simultant. Ett funktionellt protokoll utvecklades och 234 interaktioner mellan ATP och proteomet av C. necator identifierades, varav 103 potentiellt är nyupptäckta. På grund av tidsbrist och motgångar i labbet producerades inga signifikanta resultat för de resterande 11 metaboliterna som testades. C. necator är en industriellt relevant kemolitoautotrof som kan växa på CO2 och vätgas, samt manipuleras till att producera många värdefulla produkter. Bakterierna odlades i kemostater varefter proteomet extraherades i sitt naturliga tillstånd. Sedan inkuberades proteomet med en metabolit av intresse och utsattes för begränsad, icke-specifik proteolys. Den resulterande peptidblandningen analyserades via tandem masspektrometri kopplad till vätskekromatografi (LC – MS/MS).

Kolavskiljning, avlägsnande av koldioxid (CO2) från atmosfären, har fått uppmärksamhet som en metod för att mildra effekterna av den globala uppvärmningen. Växter och fototrofa mikroorganismer har den inneboende förmåganatt fånga upp kol genom fixering av CO2 för att producera biomassa. Däremot inhemska kolfixeringsvägar begränsas av nyckelenzymer med låg katalytisk aktivitet vilket resulterar i låg energieffektivitet. Rubisco är en sådan nyckelenzym, ökänt för sin dåliga prestanda. Tidigare forskning har misslyckats när det gäller att förbättra kolet fixering i Rubisco med konventionella metoder. Generativ modellering har dykt upp som en innovativ förhållningssätt till enzymteknik, dra fördel av olika arkitekturer för neurala nätverk för att föreslå en ny varianter med önskade egenskaper. Här tränas en variationsautokodare (VAE) på Rubisco-sekvensen utrymme användes för utmaningen med Rubiscos ingenjörskonst. Två modeller utbildades och med hjälp av dimensionsreduktionsegenskapen hos VAE, utforskades fitnesslandskapet i Rubisco. Sekvenser var märkt med katalytiskt relevanta data och en regressionsmodell byggdes med syftet att förutsäga dessa sekvenser med ökad katalytisk aktivitet. Nya Rubisco-sekvenser genererades efter systematiska utfrågning av det lågdimensionella rummet. Användningen av generativ modellering här ger ett nytt perspektiv på Rubisco engineering. / Carbon capture, the removal of carbon dioxide (CO2) from the atmosphere, has gained attention as a method to mitigate the effects of global warming. Plants and phototrophic microorganisms have the inherent ability to capture carbon through the fixation of CO2 to produce biomass. However, native carbon fixing pathways are limited by key enzymes with low catalytic activity resulting in low energy efficiency. Rubisco is one such key enzyme, notorious for its poor performance. Past research has been unsuccessful at enhancing carbon fixation in Rubisco through conventional methods. Generative modelling has emerged as an innovative approach to enzyme engineering, taking advantage of different neural network architectures to propose novel variants with desired characteristics. Here, a variational autoencoder (VAE) trained on the Rubisco sequence space was applied to the challenge of Rubisco engineering. Two models were trained and, using the dimensionality reduction property of VAEs, the fitness landscape of Rubisco was explored. Sequences were labelled with catalytically relevant data and a regression model was built with the aim of predicting those sequences with enhanced catalytic activity. Novel Rubisco sequences were generated following systematic interrogation of the low-dimensional space. The use of generative modelling here provides a fresh perspective on Rubisco engineering.

Die Acetyl-CoA Synthase (ACS) beinhaltet ein einzigartiges Metallcluster (Cluster A) in seinem aktiven Zentrum, welches wichtig für ein autotrophes Wachstum von Bakterien und Archaeen ist, die den reduktiven Acetyl-CoA-Weg nutzen. Der letzte Schritt dieses Syntheseweges wird von der ACS am proximal zum [4Fe-4S] Cluster liegenden Ni ion katalysiert (Nip). In meiner Arbeit wurde die ACS von Carboxydothermus hydrogenoformans (ACSCh) auf seine Ligandenbindung untersucht und in verschiedenen Konformationen kristallisiert. Zuerst wurde die ACSCh in einer neuen Konformation (ACSCh-closed) kristallisiert und deren Struktur mit einer Auflösung von 2.1 Å bestimmt. Diese wies einen geringeren Kontakt zur Solventumgebung auf als die vorher bekannte Struktur der ACSCh (ACSCh-open, PDB-ID: 1RU3). Das Cluster A der ACSCh-closed unterscheidet sich von der ACSCh-open in der Koordination des Nip, welches verzerrt tetraedrisch koordiniert in ACSCh-closed vorliegt und quadratisch planar in ACSCh-open. Eine Analyse des Modells wies einen molekularen Tunnel auf, der nur in ACSCh-closed vorhanden ist, welcher als CO-Kanal zur Substratversorgung dienen könnte. Zweitens wurde die Kristallstruktur einer CO gebunden ACSCh-closed mit einer Auflösung von 2.0 Å gelöst. Darin wurde eine Elektronendichte am Nip identifiziert, die als CO überzeugend modelliert werden konnte. CO bindet am ebenfalls verzerrt tetraedrisch koordinierten Nip. Die Konformationsänderung von ACSCh-open zu ACSCh-closed scheint der entscheidende Schritt zu sein, um CO zur Bindungsstelle zu leiten. Die dritte Struktur zeigt eine CoA gebundene ACSCh Struktur mit einer Auflösung von 2.3 Å. CoA bindet am Nip, wobei Nip quadratisch planar koordiniert wird. Die Gegenwart von CoA wurde mit Berechnungen verschiedener Elektronendichte-Karten für CoA validiert. Die Bindung von CO und CoA an ACSCh wurde zudem mittels isothermaler Titrationskalorimetrie weiter charakterisiert. Dabei bindet CoA enthalpisch getrieben mit einem KD von 3.1 µM und CO entropisch getrieben mit einem KD von 9.4 µM an ACSCh. / The acetyl-CoA synthase (ACS) harbors a unique metal cluster (cluster A) in its active site, which is important for bacteria and archaea to survive in autotrophic growth using the reductive acetyl-CoA. The last step of this pathway is catalyzed by ACS at the Nip, the Ni ion proximal to the [4Fe-4S] cluster. In my study, the monomeric ACS of Carboxydothermus hydrogenoformans (ACSCh) was studied in its ligand binding and crystallized in different forms. At first, an ACSCh structure was solved in a new conformation at dmin of 2.1 Å and less solvent exposed (called ACSCh-closed) than the known structure of ACSCh (called ACSCh-open, PDB-ID:1RU3). The cluster A of ACSCh-closed differs to that of ACSCh-open in the coordination of the proximal Ni, which is distorted tetrahedrally coordinated in ACSCh-closed and square planar coordinated in ACSCh-open. Analysis of the model revealed a molecular tunnel that is only present in ACSCh-closed, which might act as CO channel for substrate delivery. Secondly, a CO-bound ACSCh-closed crystal was obtained and solved at a resolution of 2.0 Å. An electron density fitting with a diatomic ligand at the Nip site was clearly identified and modeled as a CO molecule. CO binds at the Nip site completing the tetrahedral coordination geometry of Nip. The conformational switch between open and closed is responsible for CO migration and binding to the catalytic site. A third crystal structure depicts a CoA bound ACSCh structure at 2.3 Å resolution. CoA binds at the Nip which shows a square planar geometry. This was further supported by calculating different electron density maps for CoA. The binding of CO and CoA to ACSCh has been characterized by isothermal calorimetry experiments. While CoA binding is enthalpically driven with a KD of 3.1 µM, CO binds to ACSCh by entropic contribution with a KD of 9.4 µM.

Roots live in and have evolved in a high carbon dioxide (CO₂) environment, yet relatively little research has been conducted on the impacts of soil dissolved inorganic carbon (DIC) on root metabolism. In this thesis, I explore the impacts of root-zone DIC on whole plant biomass accumulation, water use efficiency, and above-ground gas exchange. In addition, I explore the impacts of root-zone DIC on root processes: root PEP-Carboxylase activity, root respiration rate and root exudation of Krebs cycle organic acids. Root-zone DIC did not impact biomass accumulation, leaf gas exchange parameters or water use efficiency under the growth conditions examined. Root-zone DIC did increase root PEP-Carboxylase activity, but decreased root respiration (both CO₂ production and O₂ consumption) and decreased organic acid exudation rates. Increase in measurement CO₂ partial pressure was found to cause an instantaneous decrease in root CO₂ production, and I provide evidence that changes in root metabolism (CO₂ uptake by roots) are part of the cause of this phenomenon. A hypothesized relationship between root respiration rate and Krebs cycle organic acid exudation was not supported by my data. I conclude that root-zone DIC has important impacts on critical functions of root metabolism, and should be considered as an important abiotic factor much in the same way atmospheric CO₂ is for leaves and whole plant biology.