Community metabolomes reflect taxon-specific fingerprints of phytoplankton in the ocean
Ontology highlight
ABSTRACT:
ORGANISM(S): Marine Plankton Algae
TISSUE(S): Cultured Cells
SUBMITTER: 
Katherine Heal
PROVIDER: ST001514 | MetabolomicsWorkbench | Thu Oct 22 00:00:00 BST 2020
REPOSITORIES: MetabolomicsWorkbench
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Project description:b'Phytoplankton transform inorganic carbon into thousands of biomolecules, including polar metabolites that represent an important pool of labile fixed carbon, nitrogen, and sulfur. Metabolite production is not identical among phytoplankton, and the flux of these molecules through the microbial loop depends on compound-specific bioavailability to a wider microbial community. Yet relatively little is known about the diversity or concentration of polar metabolites within marine plankton. Here we evaluate 313 metabolites in 21 phytoplankton species and in natural marine particles across environmental gradients to show that bulk community metabolomes reflect the phytoplankton community on a chemical level.'
2021-02-15 | MSV000086875 | GNPS
Project description:In the surface ocean, carbon is fixed by phytoplankton and respired by the entire marine community at an astonishingly high rate. At any point in time, the difference between these two processes yields a carbon pool in surface particles that is a combination of both freshly fixed and partially degraded material. On a molecular level, we have a limited knowledge of the small molecules, or metabolites, within this pool. Specific metabolites have been shown to be responsible for fueling respiration, maintaining organismal interactions, and transferring energy throughout the microbial community. Metabolomics, or the direct observation and quantification of the small molecules that are the result of cellular activity, provides an important lens through which we can begin to assess the standing stocks of small compounds that likely fuel a great deal of heterotrophic activity in the surface ocean. Here we describe community metabolomes of particulate material into the North Pacific Ocean and compare the metabolomes to a variety of phytoplankton grown in the lab. Using both targeted and untargeted metabolomics, we identify metabolites in the particulate carbon pool and explore their latitudinal and phylogenetic distributions. This analysis reveals several compounds that have not been previously recognized as abundant components of the marine organic carbon pool. We found that the community metabolome showed distinct differences between the regimes that likely reflects the phytoplankton community present. The community metabolome in surface waters of the subtropical domain was remarkably consistent even when sampled weeks apart, while the northern regions showed a patichier and less reproducible community metabolome. Some individual compounds showed distinct patterns between oceanographic regimes, including homarine, an abundant molecule that can contribute up to 4\% of the total particulate carbon pool in marine surface waters. Glutamic acid and glutamine showed opposite patterns in the oceanographic regimes, suggesting differences in community-level nitrogen assimilation in these different regimes. Overall, this study offers a new perspective into particulate carbon composition in oceanographic research, reveals important carbon pools that may fuel the microbial loop, and suggests an altered community-level nitrogen assimilation capacity over the North Pacific transition zone.
2020-04-28 | ST001372 | MetabolomicsWorkbench
Project description:In the surface ocean, carbon is fixed by phytoplankton and respired by the entire marine community at an astonishingly high rate. At any point in time, the difference between these two processes yields a carbon pool in surface particles that is a combination of both freshly fixed and partially degraded material. On a molecular level, we have a limited knowledge of the small molecules, or metabolites, within this pool. Specific metabolites have been shown to be responsible for fueling respiration, maintaining organismal interactions, and transferring energy throughout the microbial community. Metabolomics, or the direct observation and quantification of the small molecules that are the result of cellular activity, provides an important lens through which we can begin to assess the standing stocks of small compounds that likely fuel a great deal of heterotrophic activity in the surface ocean. Here we describe community metabolomes of particulate material into the North Pacific Ocean and compare the metabolomes to a variety of phytoplankton grown in the lab. Using both targeted and untargeted metabolomics, we identify metabolites in the particulate carbon pool and explore their latitudinal and phylogenetic distributions. This analysis reveals several compounds that have not been previously recognized as abundant components of the marine organic carbon pool. We found that the community metabolome showed distinct differences between the regimes that likely reflects the phytoplankton community present. The community metabolome in surface waters of the subtropical domain was remarkably consistent even when sampled weeks apart, while the northern regions showed a patchier and less reproducible community metabolome. Some individual compounds showed distinct patterns between oceanographic regimes, including homarine, an abundant molecule that can contribute up to 4% of the total particulate carbon pool in marine surface waters. Glutamic acid and glutamine showed opposite patterns in the oceanographic regimes, suggesting differences in community-level nitrogen assimilation in these different regimes. Overall, this study offers a new perspective into particulate carbon composition in oceanographic research, reveals important carbon pools that may fuel the microbial loop, and suggests an altered community-level nitrogen assimilation capacity over the North Pacific transition zone.
2020-06-25 | ST001410 | MetabolomicsWorkbench
Project description:In the surface ocean, carbon is fixed by phytoplankton and respired by the entire marine community at an astonishingly high rate. At any point in time, the difference between these two processes yields a carbon pool in surface particles that is a combination of both freshly fixed and partially degraded material. On a molecular level, we have a limited knowledge of the small molecules, or metabolites, within this pool. Specific metabolites have been shown to be responsible for fueling respiration, maintaining organismal interactions, and transferring energy throughout the microbial community. Metabolomics, or the direct observation and quantification of the small molecules that are the result of cellular activity, provides an important lens through which we can begin to assess the standing stocks of small compounds that likely fuel a great deal of heterotrophic activity in the surface ocean. Here we describe community metabolomes of particulate material into the North Pacific Ocean and compare the metabolomes to a variety of phytoplankton grown in the lab. Using both targeted and untargeted metabolomics, we identify metabolites in the particulate carbon pool and explore their latitudinal and phylogenetic distributions. This analysis reveals several compounds that have not been previously recognized as abundant components of the marine organic carbon pool. We found that the community metabolome showed distinct differences between the regimes that likely reflects the phytoplankton community present. The community metabolome in surface waters of the subtropical domain was remarkably consistent even when sampled weeks apart, while the northern regions showed a patchier and less reproducible community metabolome. Some individual compounds showed distinct patterns between oceanographic regimes, including homarine, an abundant molecule that can contribute up to 4% of the total particulate carbon pool in marine surface waters. Glutamic acid and glutamine showed opposite patterns in the oceanographic regimes, suggesting differences in community-level nitrogen assimilation in these different regimes. Overall, this study offers a new perspective into particulate carbon composition in oceanographic research, reveals important carbon pools that may fuel the microbial loop, and suggests an altered community-level nitrogen assimilation capacity over the North Pacific transition zone.
2020-05-27 | ST001409 | MetabolomicsWorkbench
Project description:A functional gene microarray was developed and used to investigate phytoplankton community composition and gene expression in the English Channel. Genes encoding the CO2 fixation enzyme RuBisCO (rbcL) and the nitrate assimilation enzyme nitrate reductase (NR) representing several major groups of phytoplankton were included as oligonucleotide probes on the 'phytoarray'. Five major groups of eukaryotic phytoplankton that possess the Type 1D rbcL gene were detected, both in terms of presence (DNA) and activity (rbcL gene expression). Changes in relative signal intensity among the Type 1D rbcL probes indicated a shift from diatom dominance in the spring bloom to dominance by haptophytes and flagellates later in the summer. Because of the limitations of a smaller database, NR probes detected fewer groups, but due to the greater diversity among known NR sequences, NR probes provided higher phylogenetic resolution than did rbcL probes, and identified two uncultivated diatom phylotypes as the most abundant (DNA) and active (NR gene expression) in field samples. Unidentified chlorophytes and the diatom Phaeodactylum tricornutum were detected at both the DNA and cDNA (gene expression) levels. The reproducibility of the array was evaluated in several ways and future directions for further improvement of probe development and sensitivity are outlined. The phytoarray provides a relatively high resolution, high throughput approach to assessing phytoplankton community composition in marine environments. Keywords: seawater natural assemblages, functional gene expression Two functional genes, nitrate reductase and RuBisCO, 4 - 8 replicate features per array
2010-06-19 | E-GEOD-12742 | biostudies-arrayexpress
Project description:A functional gene microarray was developed and used to investigate phytoplankton community composition and gene expression in the English Channel. Genes encoding the CO2 fixation enzyme RuBisCO (rbcL) and the nitrate assimilation enzyme nitrate reductase (NR) representing several major groups of phytoplankton were included as oligonucleotide probes on the 'phytoarray'. Five major groups of eukaryotic phytoplankton that possess the Type 1D rbcL gene were detected, both in terms of presence (DNA) and activity (rbcL gene expression). Changes in relative signal intensity among the Type 1D rbcL probes indicated a shift from diatom dominance in the spring bloom to dominance by haptophytes and flagellates later in the summer. Because of the limitations of a smaller database, NR probes detected fewer groups, but due to the greater diversity among known NR sequences, NR probes provided higher phylogenetic resolution than did rbcL probes, and identified two uncultivated diatom phylotypes as the most abundant (DNA) and active (NR gene expression) in field samples. Unidentified chlorophytes and the diatom Phaeodactylum tricornutum were detected at both the DNA and cDNA (gene expression) levels. The reproducibility of the array was evaluated in several ways and future directions for further improvement of probe development and sensitivity are outlined. The phytoarray provides a relatively high resolution, high throughput approach to assessing phytoplankton community composition in marine environments. Keywords: seawater natural assemblages, functional gene expression
2008-09-12 | GSE12742 | GEO
Project description:Background: Marine phytoplankton are responsible for 50% of the CO2 that is fixed annually worldwide and contribute massively to other biogeochemical cycles in the oceans. Diatoms and coccolithophores play a significant role as the base of the marine food web and they sequester carbon due to their ability to form blooms and to biomineralise. To discover the presence and regulation of short non-coding RNAs (sRNAs) in these two important phytoplankton groups, we sequenced short RNA transcriptomes of two diatom species (Thalassiosira pseudonana, Fragilariopsis cylindrus) and validated them by Northern blots along with the coccolithophore Emiliania huxleyi. Results: Despite an exhaustive search, we did not find canonical miRNAs in diatoms. The most prominent classes of sRNAs in diatoms were repeat-associated sRNAs and tRNA-derived sRNAs. The latter were also present in E. huxleyi. tRNA-derived sRNAs in diatoms were induced under important environmental stress conditions (iron and silicate limitation, oxidative stress, alkaline pH), and they were very abundant especially in the polar diatom F. cylindrus (20.7% of all sRNAs) even under optimal growth conditions. Conclusions: This study provides first experimental evidence for the existence of short non-coding RNAs in marine microalgae. Our data suggest that canonical miRNAs are absent from diatoms. However, the group of tRNA-derived sRNAs seems to be very prominent in diatoms and coccolithophores and may be used for acclimation to environmental conditions. RNA-seq study of sRNA populations in two species of diatoms using Illumina GAII high-throughput sequencing
2015-03-06 | E-GEOD-57987 | biostudies-arrayexpress
Project description:Background: Marine phytoplankton are responsible for 50% of the CO2 that is fixed annually worldwide and contribute massively to other biogeochemical cycles in the oceans. Diatoms and coccolithophores play a significant role as the base of the marine food web and they sequester carbon due to their ability to form blooms and to biomineralise. To discover the presence and regulation of short non-coding RNAs (sRNAs) in these two important phytoplankton groups, we sequenced short RNA transcriptomes of two diatom species (Thalassiosira pseudonana, Fragilariopsis cylindrus) and validated them by Northern blots along with the coccolithophore Emiliania huxleyi. Results: Despite an exhaustive search, we did not find canonical miRNAs in diatoms. The most prominent classes of sRNAs in diatoms were repeat-associated sRNAs and tRNA-derived sRNAs. The latter were also present in E. huxleyi. tRNA-derived sRNAs in diatoms were induced under important environmental stress conditions (iron and silicate limitation, oxidative stress, alkaline pH), and they were very abundant especially in the polar diatom F. cylindrus (20.7% of all sRNAs) even under optimal growth conditions. Conclusions: This study provides first experimental evidence for the existence of short non-coding RNAs in marine microalgae. Our data suggest that canonical miRNAs are absent from diatoms. However, the group of tRNA-derived sRNAs seems to be very prominent in diatoms and coccolithophores and may be used for acclimation to environmental conditions.
2015-03-06 | GSE57987 | GEO
Project description:Marine phytoplankton are a diverse group of photoautotrophic organisms and key mediators in the global carbon cycle. Phytoplankton physiology and biomass accumulation are closely tied to mixed layer depth, but the intracellular metabolic pathways activated in response to changing mixed layer depths remain unexplored. Here, metatranscriptomics was used to characterize the phytoplankton community response to a mixed layer shallowing from 233 meters to 5 meters over the course of two days during the late spring in the Northwest Atlantic. Most phytoplankton genera downregulated core photosynthesis, carbon storage, and carbon fixation genes as the system transitioned from a deep to a shallow mixed layer and shifted towards catabolism of stored carbon ic pathways supportive of rapid cell growth. In contrast, phytoplankton genera exhibited divergent transcriptional strategies for photosystem light harvesting complex genes during this transition. Active infection, taken as the ratio of virus to host transcripts, increased in the Bacillariophyta (diatom) phylum and decreased in the Chlorophyta (green algae) phylum upon mixed layer shallowing. A conceptual model is proposed to provide ecophysiological context for our findings, in which light limitation during deep mixing induces populations into a transcriptional state which maximizes interrupts the oscillating levels of transcripts related to photosynthesis, carbon storage, and carbon fixation found in shallow mixed layers with relatively higher growth rates. We propose that upon sensing high light levels during mixed layer shallowing, phytoplankton resume diel oscillation of core sets of genes enabling photoprotection, biosynthesis and cell replication. Our findings highlight the shared and unique transcriptional response strategies within phytoplankton communities acclimating to the dynamic light environment associated with transient deep mixing and shallowing events during the annual North Atlantic bloom.
2023-03-22 | GSE208287 | GEO
Project description:Cross-feeding is fundamental to the diversity and function of microbial communities. However, identification of cross-fed metabolites is often challenging due to the universality of metabolic and biosynthetic intermediates. Here, we use 13C isotope tracing in peptides to elucidate cross-fed metabolites in cocultures of Saccharomyces cerevisiae and Lactococcus lactis. The community was grown on lactose as the main carbon source with either glucose or galactose fraction of the molecule labelled with 13C. Data analysis allowing for the possible mass-shifts yielded hundreds of peptides for which we could assign both species identity and labelling degree. The labelling pattern showed that the yeast utilized galactose and, to a lesser extent, lactic acid shared by L. lactis as carbon sources. While the yeast provided essential amino acids to the bacterium as expected, the data also uncovered a complex pattern of amino acid exchange. The identity of the cross-fed metabolites was further supported by metabolite labelling in the co-culture supernatant, and by diminished fitness of a galactose-negative yeast mutant in the community. Together, our results demonstrate the utility of 13C-based proteomics for uncovering microbial interactions.
2023-02-07 | PXD019952 | Pride